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    Current protected areas provide limited benefits for European river biodiversity

    AbstractProtected areas are a principal conservation tool for addressing biodiversity loss. Such protection is especially needed in freshwaters, given their greater biodiversity losses compared to terrestrial and marine ecosystems. However, broad-scale evaluations of protected area effectiveness for freshwater biodiversity are lacking. Here, we provide a continental-scale analysis of the relationship between protected areas and freshwater biodiversity using 1,754 river invertebrate community time series sampled between 1986 and 2022 across ten European countries. Protected areas primarily benefited poor-quality communities (indicative of higher human impacts) that were protected, or that gained protection, across a substantial proportion of their upstream catchment. Protection had little to no influence on moderate- and high-quality communities, although high-quality communities potentially provide less scope for effect. Our results reveal the overall limited effectiveness of current protected areas for freshwater biodiversity, likely because they are typically designed and managed to achieve terrestrial conservation goals. Broadly improving effectiveness for freshwater biodiversity requires catchment-scale management approaches involving larger and more continuous upstream protection, and efforts to address remaining stressors. These approaches would also benefit connected terrestrial and coastal ecosystems, thus generally helping bend the curve of global biodiversity loss.

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    IntroductionBiodiversity is in crisis owing to human-induced global change1,2,3. Extensive actions have been implemented to address these losses, including legislation and agreements to expand the cover of protected areas (PAs), such as the EU Habitats Directive (92/43/EEC) and the Kunming-Montreal Global Biodiversity Framework, which sets a target of 30% global PA coverage by 20304. PAs restrict or reduce human activity in designated locations, such as national parks, nature reserves, or marine sanctuaries, with the aim of maintaining and restoring biodiversity. Whether PAs generally achieve this aim remains unclear. Several broad-scale (i.e., global or continental) studies have investigated the effectiveness of terrestrial and marine PAs, providing insights into their potential for reducing biodiversity loss5,6,7, exploitation8, and habitat loss9,10. However, similar broad-scale perspectives are currently lacking for freshwaters. This knowledge gap is particularly concerning given that freshwater ecosystems harbor a disproportionate amount of global biodiversity by area, and this biodiversity is declining faster compared to terrestrial and marine ecosystems11,12,13. Evidence of PA effectiveness for individual freshwater ecosystems, or freshwaters in individual regions, is currently mixed14, with some PAs generally benefitting freshwater biodiversity15,16 whereas others exhibit little to no effect17,18,19. This variability highlights the need for research that evaluates the general effectiveness of PAs for freshwater biodiversity at broader spatial scales.Inland (i.e., non-marine) PAs may broadly fail to protect freshwater biodiversity because their boundaries and management typically prioritize terrestrial habitats and charismatic taxa20,21, lack explicit goals for freshwaters, and neglect the needs of freshwater taxa22,23,24. For example, most inland PAs are small, with ~85% less than 10 square kilometers25. However, many freshwater ecosystems, particularly larger rivers, can extend across tens to hundreds of kilometers with catchments encompassing thousands of square kilometers26. Thus, local river communities can be impacted by upstream terrestrial pollutants and other inputs across broad spatial scales27,28,29. Small-scale protection of a river site can therefore be compromised by inputs arriving from upstream, unprotected areas30,31. Small PAs may also only succeed at protecting local habitat, while other key upstream and downstream habitats used by mobile freshwater taxa remain unprotected32,33,34.Evaluating the benefits of inland PAs for freshwaters requires appropriate counterfactuals, i.e., unprotected areas, for comparison. Studies often rely on spatial comparisons of protected and unprotected sites17,19,35,36, but this may produce biased results due to spatial biases in PA placement. For example, PAs tend to be designated in less impacted, forested, higher elevation areas with little human development37,38, which may already have high and/or stable biodiversity compared to unprotected sites. These biases often cannot be fully controlled, which makes it difficult to distinguish the effects of protection from pre-existing differences between sites39. An alternative approach is to incorporate a temporal component into the spatial comparisons, specifically by comparing the rate of biodiversity change between protected and unprotected sites6. This method better evaluates PA effectiveness by using earlier years within sites as the baseline, thus helping determine whether establishing or expanding protection affected biodiversity, and whether biodiversity was lost (or gained) at a faster rate in unprotected sites. However, such temporal comparisons are hindered by the scarcity of high-resolution time-series data.To address the need for broad-scale, temporal evaluations of PA effectiveness for freshwater biodiversity, we examine 1,754 time series of river invertebrate communities collected between 1986 and 2022 across ten European countries (Fig. 1 and Supplementary Table 1). We focus on river invertebrates because they are key components of freshwater biodiversity that provide important ecosystem functions and services40, and they exhibit consistent compositional responses to human pressures41. These taxa are therefore commonly used as bioindicators and have been monitored globally for decades, including in countries across Europe. Consequently, analysis of European, long-term river invertebrate community data can address the need for broad-scale, temporal evaluations of PA effectiveness for freshwater biodiversity.Fig. 1: Locations of the 1754 sampled European river sites.Sites are in Belgium, Czechia, Denmark, Finland, France, Hungary, Lithuania, Spain, Sweden, and the UK. Sites are colored based on the presence of a protected area in the full upstream catchment (no = red; yes = blue). Point sizes for sites with upstream protected areas are based on the proportion of the catchment covered by protected areas.Full size imageWe first quantify biodiversity change as site-specific temporal changes in invertebrate abundance, taxonomic richness, and ecological quality (a measure of human impacts based on similarity to communities in least-impacted conditions; see “Methods” section). We then determine whether the rate of biodiversity change differs between sites with and without upstream PAs (as in ref. 6 for terrestrial and marine ecosystems), under the expectation that protection would better maintain biodiversity and lead to greater increases in biodiversity through time. To compare the effects of protection close to a river site versus across its broader catchment, we investigate relationships at four progressively larger upstream distances, ranging from PAs up to 1 km upstream (i.e., the immediate vicinity of a site) 10 km, 100 km, and the full upstream catchment. Lastly, for sites with upstream PAs, we determine whether biodiversity change depends on the amount of PA cover, or the degree of PA gain, and whether it varies with river size and initial ecological quality. Regarding river size, as discussed above, larger rivers integrate inputs across longer distances, thus potentially exposing their communities to cumulative pollutants from rural and urban sources, so we expect that biodiversity in larger rivers primarily responds to PA cover that spans larger upstream scales. Regarding ecological quality, PAs tend to be designated in already less impacted areas (i.e., better initial ecological quality), and we expect that the effectiveness of such PAs differs from those established in poorer quality sites, which generally have lower biodiversity42 and thus more scope for improvement.Here, we show that upstream PAs primarily benefit poor-quality communities where PAs encompass a larger proportion of the catchment. These communities exhibit much higher rates of biodiversity recovery than likely would have occurred in the absence of protection. In contrast, PAs have little to no effect on biodiversity in moderate- and high-quality communities, although the latter group may have been unaffected because human impacts in such rivers are generally low regardless of protection status. Our results underscore the need to broadly improve PA effectiveness in freshwaters by ensuring PA design and management explicitly consider freshwater biodiversity and integrate the needs of freshwater ecosystems.ResultsProtected and unprotected sitesProtected and unprotected sites only differed in the rate of ecological quality change (represented as the Ecological Quality Ratio; EQR), and only when protections encompassed smaller upstream scales, specifically when PAs were within 1-km (based on a significant Likelihood ratio test or LRT, n = 1754, L = 23.4, df = 1, P < 0.001) and 10-km upstream distances from a river site (LRT, n = 1754, L = 5.97, df = 1, P = 0.039; Fig. 2a–c). However, these changes were always greater (i.e., better) in unprotected sites, which was the opposite of our expectations. For example, the rate of EQR change for protected sites at the 1-km upstream scale was +1.1% year−1, whereas it was +1.9% year−1 for unprotected sites (Fig. 2c). For all other metrics and upstream scales, we found no differences in biodiversity change between protected and unprotected sites (Fig. 2a–c; Supplementary Table 2), with similar proportions of sites in these groups both gaining and losing biodiversity (Supplementary Fig. 1).Fig. 2: Overall effects of protected areas on river biodiversity.Rate of temporal change in a, d abundance, b, e richness, and c, f ecological quality (as the Ecological Quality Ratio; EQR) in (a–c) protected and unprotected sites, and (d–f) in sites that gained and did not gain upstream PA cover, for the 1-km, 10-km, 100-km, and full upstream scales. Points show the predicted group mean based on the respective linear mixed model, with lines as 95% confidence intervals. Asterisks indicate significant differences between groups based on Likelihood Ratio Tests and corrected for multiple comparisons using the Benjamini–Hochberg false discovery rate (c, 1 km: P < 0.001, 10 km: P = 0.021; e, 1 km: P = 0.039). Numbers in (c, f) indicate the number of sites out of 1754 total in each group, and these same sample sizes apply to (a, b) and (d, e).Full size imageFor sites with upstream PAs, higher PA cover was related to greater increases in taxon richness and ecological quality, but the nature of these relationships depended on initial ecological quality and upstream scale, as evidenced by significant PA cover*ecological quality interactions from generalized additive mixed models (Supplementary Table 3), and differences in effect sizes among upstream scales. Richness primarily increased with higher PA cover close to a site (i.e., at smaller upstream scales), and primarily in initially degraded communities (i.e., lower initial ecological quality; Fig. 3). For example, considering richness at the 1-km upstream scale and an initially poor ecological quality of 0.2 (i.e., 20% similarity to reference conditions), increasing PA cover from <1% to 100% almost tripled the rate at which richness increased, from +2.8% year−1 to +8.2% year−1 (Fig. 3a). These effects weakened as the upstream scale and initial ecological quality increased (Fig. 3b–d) to the point that, at the full upstream scale and an initially high ecological quality of 0.8, increasing PA cover from <1% to 100% only increased the rate at which richness increased from +0.7% to +1.1% year−1 (Fig. 3d). Similar to richness, ecological quality also increased with higher PA cover primarily in initially poorer quality communities. However, the effect of upstream scale was the opposite to that observed for richness, with greater improvements in ecological quality when PA cover increased at larger upstream scales (Supplementary Fig. 2), indicating ecological quality primarily responded to the amount of protection across the catchment.Fig. 3: Effects of the amount of protected area on taxon richness.Relationship between increasing the amount of protected area (PA) cover and the rate of temporal change in richness for only sites with PAs at the a 1-km, b 10-km, c 100-km, and d full upstream scales. Lines show the best-fit relationships, with shaded areas as 95% confidence intervals, based on generalized additive mixed models. Line and shading color illustrate how relationships depend on initial ecological quality (as the initial Ecological Quality Ratio, EQR) using examples of 0.2 (red), 0.4 (orange), 0.6 (light blue), and 0.8 (dark blue), which respectively indicate higher to lower human impacts.Full size imageIncreasing PA cover did not affect the rate of change in abundance at any upstream scale, and we found no evidence for effects of river size (Supplementary Table 3).Sites that gained and did not gain protected areasSimilar to the protected and unprotected sites, sites that gained and did not gain PA cover only differed in the rate of ecological quality change, and only at the 1-km upstream scale (LRT, n = 1754, L = 7.79, df = 1, P = 0.021), with greater increases in sites that did not gain PA cover (Fig. 2d–f). For all other metrics and upstream scales, we found no differences in biodiversity change between sites that gained and did not gain PA cover (Fig. 2d–f; Supplementary Table 2), with similar proportions of sites in these groups both gaining and losing biodiversity (Supplementary Fig. 1).For sites that gained upstream PAs, higher gains translated to greater increases in richness and ecological quality, primarily in initially poorer quality communities and only at larger upstream scales (richness: full only, Supplementary Fig. 3; EQRs: 10 km, 100 km, and full, Fig. 4). These increases were stronger for ecological quality and weaker for richness. For example, at the full upstream scale and an initially poor ecological quality of 0.2, increasing the rate of PA gain from <1% year−1 to the maximum observed value of 7.5% year−1 more than tripled the rate of EQR gain, from +4.1% year−1 to +14% year−1 (Fig. 4d). The rate of richness gain almost doubled under the same conditions, from +2.3% year−1 to +4.5% year−1 (Supplementary Fig. 3). Furthermore, as initial ecological quality increased, we found some instances where higher PA gains translated to slightly lower rates of increase in both ecological quality and richness. Using the full upstream scale as an example and an initially high ecological quality of 0.8, increasing the rate of PA gain from <1% to 7.5% year−1 decreased the rate of EQR gain from +0.32% to +0.19% year−1 (Fig. 4d).Fig. 4: Effects of the rate of protected area gain on ecological quality.Relationship between gain of upstream protected area (PA) cover and the rate of temporal change in ecological quality (represented as the Ecological Quality Ratio; EQR) for only sites that gained PA cover at the a 1-km, b 10-km, c 100-km, and d full upstream scales. Lines show the best-fit relationships, with shaded areas as the 95% confidence intervals, based on generalized additive mixed models. Line and shading color illustrate how relationships depend on initial ecological quality using example initial EQRs of 0.2 (red), 0.4 (orange), 0.6 (light blue), and 0.8 (dark blue), which respectively indicate higher to lower human impacts. Black lines and grey shading indicate non-significant (P > 0.05) relationships based on Wald-type tests. Best-fit relationships are shown up to the maximum rate of PA gain observed at each upstream scale.Full size imageIncreasing PA gain did not affect the rate of change in abundance at any upstream scale, and we found no evidence for effects of river size (Supplementary Table 3).DiscussionA principal question for evaluating the effectiveness of protection for nature conservation is to determine what would have happened in its absence39. Our results show that, broadly speaking, the same changes in river invertebrate biodiversity occurred regardless of the presence or degree of upstream protection, although PAs improved biodiversity outcomes in a subset of poor-quality communities that had or gained PA cover across a larger proportion of their upstream catchment. Additionally, some rivers lost invertebrate biodiversity during our 1986 to 2022 study period, which occurred in a comparable proportion of protected and unprotected sites. We therefore found no consistent evidence that inland PAs have generally benefited European river invertebrate biodiversity, suggesting that PAs may have not benefited water or habitat quality, given that invertebrates are key indicators of both43. These findings provide continental-scale support for similar results from individual freshwater ecosystems and specific regions for invertebrates18,31, other taxonomic groups (e.g., fish17,18,19), and water quality18. This conclusion should not be misconstrued as suggesting that PAs are ineffective, particularly given that it is based on a subset of total freshwater biodiversity and does not address whether PAs achieved the terrestrial conservation goals they are typically designed and managed for, such as reducing habitat loss9,10. We also found that PAs increased the rate of improvement in biodiversity and ecological quality for some river invertebrate communities, and other studies have shown PAs benefiting certain, individual freshwater ecosystems and taxonomic groups14,44. Our findings do, however, highlight the need to broadly improve the capacity of inland PAs to support freshwater biodiversity.Our results for poor-quality communities (e.g., around an initial EQR of 0.2 or 20% similarity to reference conditions) suggest that PAs led to greater increases in biodiversity in these sites than would have occurred without protection. The lesser influence of protection on higher quality communities potentially reflects the already low human impacts in these sites, thus biodiversity remained high and stable regardless of protection status. This explanation fits with our results showing low PA effectiveness in high-quality communities (e.g., initial EQR around 0.8) where biodiversity was likely already high, and may explain why protection was sometimes associated with lower biodiversity gains, which may occur if PAs are placed in areas with a lower scope for improvement (e.g., remote, forested catchments37,38). However, it does not explain why PAs were less effective for moderate-quality communities (e.g., initial EQR around 0.4–0.6), which have considerable potential for further improvement. A more likely explanation for these communities is that current approaches to implementing inland PAs, which typically focus on management of terrestrial habitats23, can address some stressors affecting poor-quality rivers, but not other stressors that may be more relevant in higher quality ecosystems. For example, land-use change and pollution are among the principal stressors driving freshwater biodiversity loss45. PAs have some capacity to address these stressors by reducing the human activities that cause them, such as deforestation, urban expansion, intensive agriculture, and tourism10,46. Doing so can subsequently improve water and habitat quality in hydrologically connected rivers47,48. However, as communities recover, other unaddressed stressors may become more relevant, such as upstream flow alterations or climate change49, thereby limiting PA effectiveness. Maximizing the benefits of PAs for freshwater biodiversity requires that existing management regimes consider both terrestrial- and freshwater-focused actions23,50, and set specific goals to address the most important stressors in each freshwater ecosystem. Preventing degradation, including in higher quality rivers, also requires conservation actions beyond establishing PAs, such as better wastewater treatment, habitat restoration, and further improvements to land management practices, including reducing micropollutants11,51.PA benefits in initially poor-quality communities varied among upstream scales and community metrics, suggesting that the spatial scale of protection determined which community components were affected. Richness primarily responded to the amount of PA cover close to a site (i.e., at smaller upstream scales), whereas ecological quality primarily responded when protection encompassed and expanded across the broader catchment (i.e., at larger upstream scales). Abundance exhibited no response to protection whatsoever. Increases in richness that neither affect abundance nor substantially alter compositional metrics, such as ecological quality, can occur when only numerically rare species increase52. Similarly, compositional changes may not affect richness or abundance if new taxa replace previous taxa53. Our results could therefore be explained by protection at smaller scales primarily increasing rare taxa, and protection across larger scales producing stronger compositional recovery by replacing tolerant with sensitive taxa. Increasing rare taxa can provide some benefits, including potentially diversifying and stabilizing ecosystem functions54,55, but may represent a less desirable outcome compared to substantially improving invertebrate ecological quality, which is a principal indicator of European river health. Therefore, our results suggest that protecting the broader catchment, or at least a large proportion of the catchment and a river’s lateral buffer zones, may elicit greater biodiversity benefits. This conclusion supports the value of catchment-scale rather than local-scale approaches to freshwater protection22,56, including PAs that are configured to protect and connect key longitudinal (upstream to downstream), lateral (riparian and floodplain), and vertical habitats (surface to groundwater)14,33,57.An additional solution to improving PA effectiveness for freshwaters could be to further limit human activities within current PA boundaries, given that many still permit continued human use58, such as land development and resource extraction. Designating stricter PAs that do not allow such activities may reduce human impacts46, thus potentially benefiting downstream freshwaters. However, evidence that the strictness of a PA’s designation determines its conservation benefits is equivocal59, including in freshwater ecosystems16,44. Stricter protection can also counterintuitively lead to worse conservation outcomes by disenfranchising local communities and promoting illegal use of protected resources60. Integrating terrestrial with freshwater approaches to PA design and management may be an alternative approach for improving freshwater conservation outcomes14,50. Freshwater-focused PAs (e.g., Ramsar wetlands or river PAs61) can be designed based on the distribution of both terrestrial and freshwater biodiversity while accounting for habitat connectivity and downstream impacts22,30,50. Effective, adequately funded, and co-produced management is also key to PA effectiveness14,60. We therefore advocate that freshwater ecosystems would further benefit from inclusion in PA management priorities that integrate the freshwater needs of local communities and stakeholders.Inland PAs are increasing globally, supported by the 30% by 2030 coverage target set by the Kunming-Montreal Global Biodiversity Framework4. These PAs typically prioritize the needs of terrestrial habitats and taxa, raising questions about their benefits for freshwater biodiversity. Our findings, based on European river invertebrate communities, show that PAs have benefited certain freshwater communities, specifically poor-quality communities where protection encompassed a larger proportion of the upstream catchment. All other communities exhibited more limited (or no) effects of protection, although the lack of effect in high-quality communities may have occurred because these communities are less impacted regardless of whether they are protected or not. Improving overall PA effectiveness, particularly in impacted rivers, requires design and management strategies that explicitly integrate the needs of freshwater ecosystems14,57, including actions that address multiple stressors and continuous coverage that extends over larger upstream distances and lateral buffer zones. Accordingly, a holistic, catchment-scale framework for managing freshwaters is required14,22,23,62. Such a framework would better support freshwater biodiversity, including aquatic invertebrates and the ecosystem functions they provide (e.g., prey, nutrient cycling, and decomposition40), and would benefit terrestrial ecosystems via aquatic-terrestrial linkages63 and marine ecosystems via freshwater-marine linkages64. Consequently, improving freshwater protection is a critical issue relevant to all ecosystems and is essential to bend the curve of global biodiversity loss.MethodsRiver invertebrate biodiversityWe collated river invertebrate time series from ref. 42 and from data provided by European freshwater researchers and managers. We defined the following criteria for data inclusion: (i) time series must span a duration of ≥10 years with ≥7 individual sampling years to enable robust estimation of biodiversity change; (ii) within a time series, samples in different years must be collected using the same methods and from the same three-month season; (iii) data were available at the community-level with taxa identified to a consistent taxonomic level through time (if inconsistent levels were used then taxa were adjusted to the most temporally consistent level); and (iv) ecological quality values could be calculated for each community following methods compliant with the EU Water Framework Directive (see Supplementary Table 4). These criteria allowed the inclusion of data from ten European countries (Fig. 1). Included data encompassed 1754 sites and 24,245 individual years collected between 1986 and 2022. Included time series spanned a mean total duration of 19.7 ± 5.7 years (mean ± SD) with 13.8 ± 5.5 sampling years (Supplementary Table 1). Taxonomic resolution varied among sites, with 57% (993 sites) identified only to the family level or higher, and 43% (761 sites) identified to a mixed resolution, typically a combination of families, genera, and species, with some classified to intermediate (e.g., subfamily) or higher levels (e.g., Oligochaeta at subclass). These taxonomic differences among sites did not influence our results (see Supplementary Fig. 4). Identifications higher than species level introduce some uncertainty, given that we cannot detect potential species shifts occurring within these groups. However, such identifications still reliably reflect overall community responses to environmental change65,66 and are common in invertebrate research in which many taxa cannot be reliably identified to the species level.We quantified biodiversity for each site and year based on three community metrics: (i) abundance (total number of individuals), (ii) richness (total number of taxa), and (iii) ecological quality, quantified as the Ecological Quality Ratio (EQR). Ecological quality is commonly used in Europe as a community-based indicator of human impacts, particularly organic pollutants and general environmental degradation67. It reflects the compositional similarity of sensitive and tolerant taxa to expected values from least-impacted reference communities, which are defined based on country-specific criteria (Supplementary Table 4). EQRs are a continuous observed-to-expected ratio of this similarity, ranging from 0 (low similarity indicating high human impacts) to 1 (equal to reference conditions indicating low human impacts), although EQRs for some communities can be above 1, reflecting conditions better than the average reference state. We chose EQRs over other compositional metrics, such as temporal β-diversity, because they provide meaningful information not just about whether communities changed, but also how they changed.Rates of temporal change in each community metric were quantified for each site by relating site-specific abundance, richness, and EQRs to sampling year using the gls function from the nlme package in R68,69, then extracting the slope of this relationship. We included a first-order autoregressive structure in each model to control for temporal autocorrelation between successive years. All slopes were converted to percent change per year by log-transforming all metrics prior to modeling, then exponentiating the slopes, subtracting 1, and multiplying by 100. This transformation ensured all rates of biodiversity change had the same units across sites and metrics.Protected areas and upstream scalesWe obtained vectorial cartographic polygons for inland PAs from Protected Planet25. We excluded 2% of European PAs (accounting for 6% of total cover) for which the year of establishment was unknown. We further excluded all point data due to analytical errors that arise when inferring the dimensions of PAs with unknown boundaries70. The majority of point data in our included countries (1171 points out of 1247 total or 94%) were natural monuments in Sweden. These PAs have a registered area of 0 km2 because they are individual features, such as a single tree or rock formation, thus contributing marginally to total protected area cover. Of the remaining 76 excluded points, 20 were Ramsar wetlands with a total area of 296 km2, and 50 were large biosphere reserves with a total area of 94,188 km2. To fill the biosphere information gap, we used data on European biosphere boundaries from ref. 71, although we excluded the outer transition zones, which are not considered protected. Polygons for all included PAs were dissolved into a single layer, with no distinctions made between different PA types (discussed further in Supplementary Note 1).In addition to the PA polygons, for each site, we produced upstream polygons representing four different spatial scales. The four scales included: lateral buffer zones extending up the main channel and all tributaries to (i) 1-, (ii) 10-, and (iii) 100-km longitudinal distances; and (iv) the full upstream contributing area, i.e., the upstream catchment including all terrestrial areas that drain into a site. Each upstream scale was selected to account for the potential effects of PAs at progressively greater distances from each site, with the full upstream scale also accounting for PA effects outside the lateral buffer zones. Upstream distances were delineated using the Hydrography90m river network and the hydrographr package72,73. Buffer zone widths for 1–100-km upstream scales were quantified as 100 m multiplied by the Strahler order of each segment, plus half the predicted river width based on its order from ref. 74 (see Fig. 5). We used this approach because human activities adjacent to a river typically exert the strongest influence on local communities, and 100-m lateral buffer zones effectively capture these effects75,76,77. Additionally, our data encompassed sites from rivers of Strahler orders 1–11, representing small streams to very large rivers, and larger lateral areas are needed to capture the larger surface and ground water inputs to higher-order rivers78. Lastly, including river width as part of the buffer zones captured PAs that encompass rivers. The full upstream contributing area was delineated using the get_upstream_catchment function from the hydrographr package.Fig. 5: Illustrated example of the four upstream scales.A river site (red circle) and the upstream scales captured by lateral buffer zones (dashed lines) extending up to 1-km (purple), 10-km (pink), and 100-km (yellow) upstream distances. The solid black outline represents the full upstream contributing area. Note the decline in buffer zone thickness from higher (larger) to lower (smaller) order rivers.Full size imageBased on the PA and upstream polygons, we calculated the percent of each upstream scale covered by PAs to represent both the presence (>0% cover) and degree (total % cover) of protection. We also calculated the rate of temporal change in percent PA cover to capture biodiversity responses to PA expansion. PA cover was calculated for the year before the first and last year of each invertebrate time series, which allowed invertebrate communities ≥1 year to respond to environmental changes resulting from PA establishment. Percent PA cover was quantified as the mean percent cover between the first and last years (always ranging from 0 to 100% across sites). Temporal changes in percent PA cover (% year−1) for each site were quantified as the slope of the relationship between PA cover and year, which ranged from 0 to 9% year−1 depending on the upstream scale (1 km: 0–9%; 10 km: 0–8.6%; 100 km: 0–7.5%; Full: 0–7.5% year−1). PA cover changes were only neutral or positive because Protected Planet data cannot represent PA cover declines79, although PA cover has generally increased globally58.In addition to PA cover, we quantified the size (in km2) of each full upstream area to represent river size, given that larger rivers have larger upstream areas. Size was calculated based on the number of 90 m by 90 m pixels in the full upstream area, derived from the Hydrography90m river network. Sites primarily encompassed medium- to larger-sized rivers, with 671 sites out of 1754 total having an upstream catchment size between 10 and 100 km2 and 701 sites between 100 and 1000 km2, with the remainder comprised of very small (135 sites <10 km2) and very large rivers (247 sites >1000 km2).Statistical analysesWe conducted two sets of analyses: (1) categorical comparisons of changes in abundance, richness, and EQRs between protected and unprotected sites (i.e., those with and without upstream PAs), and between sites that did or did not gain upstream PA cover; and (2) for sites with upstream PAs, we related the rate of biodiversity change to the amount of upstream PA cover and the rate of PA gain using regression. The first set of analyses provided a broad overview of the effects of having or gaining any upstream PA cover. The second set determined whether the degree of protection, or its rate of gain, influenced biodiversity change. We also used the second set of analyses to test the influence of river size and initial ecological quality (detailed below). These temporal trend comparisons have some strengths compared to other potential approaches, such as before-and-after comparisons or spatial comparisons of protected and environmentally similar unprotected sites. Specifically, using temporal trends of percent biodiversity change enables comparison of sites that differ in total biodiversity, and allows for variation in protection timing (e.g., sites can be already protected at the start of their time series or can become protected later). Temporal analyses also allow for changes in protection effectiveness through time, such as lagged effects, and capture the potential compounding effects of establishing multiple PAs in subsequent years.For our first set of analyses, we compared sites with upstream PAs (>0% cover; ‘protected’) versus those without (0% cover; ‘unprotected’), and those that gained upstream PAs (>0% cover year−1; ‘gain’) versus those that did not (0% cover year−1; ‘no gain’). Sites were assigned to these categories separately for each upstream scale, given that sites could change assignments across scales (e.g., an upstream PA is present within 10 km but not 1 km). We then related the continuous, site-level rates of biodiversity change to these categories using linear mixed models (LMMs) conducted in the lme4 package80. Additionally, each model included fixed continuous terms for site latitude and longitude to control for broad-scale spatial trends, a fixed continuous term for time-series length to control for slope differences among shorter to longer time series, and a random intercept term designating the provider of each dataset to control for differences in sampling methods among providers (see Supplementary Table 1). We tested the significance (P < 0.05) of the fixed categorical PA term by dropping it from each model and comparing the reduced versus fuller models using Likelihood ratio tests81. We ran separate models for each upstream scale. To control for conducting multiple models using the same response variables, we corrected all P-values using the Benjamini–Hochberg false discovery rate82.For our second set of analyses, we used generalized additive mixed models (GAMMs) to relate biodiversity change to the amount of upstream PA cover for sites with upstream PAs, and to the rate of PA gain for sites that gained upstream PAs. Models were conducted in the mgcv package83. PA cover and rates of gain were converted to proportions and square-root transformed prior to analyses to produce a more even distribution of values. To determine the influence of river size, we included an interaction between the PA term and a continuous term for the size of the full upstream area (log10-transformed km2). To determine the influence of initial ecological quality, we included an interaction between the PA term and a continuous term for the EQR averaged across the first three sampling years to represent the initial status of the community. The individual PA, river size, and quality terms were modeled as fixed smoothed terms using thin-plate regression splines, with all fixed interactions modeled using tensor product smooths. Additionally, we included the same fixed and random control variables as for the LMMs. All smoothed terms used the default basis dimensions, and we checked model diagnostics, including the need for higher basis dimensions, using the gam.check function. All GAMMs used a Gaussian distribution (identity link function). The significance (P < 0.05) of interactions, and if needed the individual PA term, were determined using Wald-type tests83. We corrected all P-values as above when conducting multiple models using the same response variables.Reporting summaryFurther information on research design is available in the Nature Portfolio Reporting Summary linked to this article.

    Data availability

    All data needed to repeat our analyses are publicly available from https://doi.org/10.6084/m9.figshare.25245430.
    Code availability

    All code needed to repeat our analyses is publicly available from https://doi.org/10.6084/m9.figshare.25245430.
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L.K. received funding from Formas (#2023-00284) and sourced data from the Swedish University of Agricultural Sciences database (Miljödata). A.L. received funding from the Spanish Ministry of Science and Innovation (#PID2020-115830GB-100). P.P. was funded by the Czech Science Foundation (#GA23-05268S), and thanks to CHMI and the Povodí enterprises for the provided data.FundingOpen Access funding enabled and organized by Projekt DEAL.Author informationAuthors and AffiliationsDepartment of River Ecology and Conservation, Senckenberg Research Institute and Natural History Museum Frankfurt, Gelnhausen, GermanyJames S. Sinclair & Peter HaaseSchool of Science and Technology, Nottingham Trent University, Nottingham, UKRachel StubbingtonDivision of Biology, Kansas State University, Manhattan, KS, USAEllen A. R. WeltiFreshwater and Marine Solutions, Finnish Environment Institute, Oulu, FinlandJukka AroviitaState Scientific Research Institute Nature Research Centre, Vilnius, LithuaniaNathan J. BakerSHE2 Research Group, FEHM-Lab (Freshwater Ecology, Hydrology and Management), Institute of Environmental Assessment and Water Research (IDAEA), CSIC, Barcelona, SpainMiguel Cañedo-ArgüellesDepartment of Hydrobiology, University of Pécs, Pécs, HungaryZoltán CsabaiHUN-REN Balaton Limnological Research Institute, Tihany, HungaryZoltán CsabaiInstitute of Aquatic Ecology, HUN-REN Centre for Ecological Research, Budapest, HungaryDavid Cunillera-MontcusíIFREMER–DYNECO/LEBCO, Centre de Bretagne, Plouzané, FranceDavid Cunillera-MontcusíLeibniz Institute of Freshwater Ecology and Inland Fisheries (IGB), Berlin, GermanySami DomischINRAE, UR RiverLy, centre de Lyon-Villeurbanne, Villeurbanne, Cedex, FranceMartial Ferréol & Mathieu FlouryUniversity of Paris-Saclay, INRAE, UR HYCAR, Antony, FranceMathieu FlouryDepartment of Animal Sciences and Aquatic Ecology, Ghent University, Ghent, BelgiumMarie Anne Eurie Forio & Peter L. M. GoethalsIHCantabria – Instituto de Hidráulica Ambiental de la Universidad de Cantabria, Santander, SpainAlexia M. González-FerrerasNature Solutions, Finnish Environment Institute, Oulu, FinlandKaisa-Leena HuttunenEcology and Genetics Research Unit, University of Oulu, Oulu, FinlandKaisa-Leena Huttunen & Timo MuotkaDepartment of Aquatic Sciences and Assessment, Swedish University of Agricultural Sciences, Uppsala, SwedenRichard K. JohnsonDepartment of Forest Ecology and Management, Swedish University of Agricultural Sciences, Umeå, SwedenLenka KuglerováDepartment of Plant Biology and Ecology, University of the Basque Country (UPV/EHU), Leioa, Bilbao, SpainAitor LarrañagaOulanka Research Station, University of Oulu Infrastructure Platform, Kuusamo, FinlandRiku PaavolaWater, Energy and Environmental Engineering Research Unit, Faculty of Technology, University of Oulu, Oulu, FinlandRiku PaavolaDepartment of Botany and Zoology, Faculty of Science, Masaryk University, Brno, Czech RepublicPetr PařilDepartment of Ecoscience, Aarhus University, Aarhus, DenmarkJes J. RasmussenResearch Center One Health Ruhr, University Alliance Ruhr & Faculty for Biology, University of Duisburg-Essen, Essen, GermanyRalf B. SchäferFlanders Environment Agency (VMM), Aalst, BelgiumRudy VannevelDepartment of Tisza Research, Institute of Aquatic Ecology, HUN-REN Centre for Ecological Research, Debrecen, HungaryGábor VárbíróSchool of Life Sciences, University of Essex, Colchester, UKMartin WilkesFaculty of Biology, University of Duisburg-Essen, Essen, GermanyPeter HaaseAuthorsJames S. SinclairView author publicationsSearch author on:PubMed Google ScholarRachel StubbingtonView author publicationsSearch author on:PubMed Google ScholarEllen A. R. WeltiView author publicationsSearch author on:PubMed Google ScholarJukka AroviitaView author publicationsSearch author on:PubMed Google ScholarNathan J. BakerView author publicationsSearch author on:PubMed Google ScholarMiguel Cañedo-ArgüellesView author publicationsSearch author on:PubMed Google ScholarZoltán CsabaiView author publicationsSearch author on:PubMed Google ScholarDavid Cunillera-MontcusíView author publicationsSearch author on:PubMed Google ScholarSami DomischView author publicationsSearch author on:PubMed Google ScholarMartial FerréolView author publicationsSearch author on:PubMed Google ScholarMathieu FlouryView author publicationsSearch author on:PubMed Google ScholarMarie Anne Eurie ForioView author publicationsSearch author on:PubMed Google ScholarPeter L. M. GoethalsView author publicationsSearch author on:PubMed Google ScholarAlexia M. González-FerrerasView author publicationsSearch author on:PubMed Google ScholarKaisa-Leena HuttunenView author publicationsSearch author on:PubMed Google ScholarRichard K. JohnsonView author publicationsSearch author on:PubMed Google ScholarLenka KuglerováView author publicationsSearch author on:PubMed Google ScholarAitor LarrañagaView author publicationsSearch author on:PubMed Google ScholarTimo MuotkaView author publicationsSearch author on:PubMed Google ScholarRiku PaavolaView author publicationsSearch author on:PubMed Google ScholarPetr PařilView author publicationsSearch author on:PubMed Google ScholarJes J. RasmussenView author publicationsSearch author on:PubMed Google ScholarRalf B. SchäferView author publicationsSearch author on:PubMed Google ScholarRudy VannevelView author publicationsSearch author on:PubMed Google ScholarGábor VárbíróView author publicationsSearch author on:PubMed Google ScholarMartin WilkesView author publicationsSearch author on:PubMed Google ScholarPeter HaaseView author publicationsSearch author on:PubMed Google ScholarContributionsJ.S.S. and P.H. conceived the study. J.A., S.D., and R.B.S. contributed to planning and methods. J.S.S. and P.H. wrote most of the manuscript with contributions from all authors, particularly R.S. and E.A.R.W. J.A., N.J.B., M.C.-A., Z.C., D.C.-M,. M.Fe., M.Fl., M.A.E.F., P.L.M.G., A.M.G.-F., K.-L.H., R.K.J., L.K., A.L., T.M., R.P., P.P., J.J.R., R.V., G.V., and M.W. provided invertebrate data or contributed to calculating ecological quality values for their respective countries.Corresponding authorCorrespondence to
    James S. Sinclair.Ethics declarations

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    Since April 16th, 2025, Miguel Cañedo-Argüelles has been seconded to the ERC Executive agency. The views expressed in this paper are purely those of the author. They do not necessarily reflect the views or official positions of the European Commission, the ERC Executive Agency, or the ERC Scientific Council. The other authors declare no competing interests.

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    The impact of tropical cyclones Pam, Harold, Winston and Yasa on tree cover loss in Vanuatu and Fiji

    AbstractMany Pacific Small Island Developing States are vulnerable to Tropical Cyclones (TCs) leading to an estimated average annual loss of USD 1.08 billion. The study quantifies the impacts of tropical cyclones on tree cover and associated ecosystem services, beginning with coastal protection and the loss of carbon, for inclusion in Post Disaster Needs Assessment (PDNAs), Nationally Determined Contributions (NDCs), catastrophe risk insurance payments and loss and damage accounting. The study focuses on the impacts of tree cover loss resulting from four separate category five tropical cyclones in Fiji and Vanuatu: Pam, Harold, Winston and Yasa. Compared to national average annual tree cover losses between 2000 and 2023, TCs Pam and Harold increased tree cover loss 4.6 and 5.2-fold in Vanuatu and TCs Winston and Yasa increased tree cover loss 3.6 and 3.1-fold in Fiji, respectively. The resulting loss of carbon storage adds an estimated 23.4–25.0% in economic losses based on IPCC Tier II emissions factors and 37.2% for IPCC Tier I emissions factors to the Vanuatu and Fiji PDNA economic loss estimates, respectively. The focus on carbon emissions is a first step towards a quantification of the loss of ecosystem services in countries whose people depend on natural resources for daily subsistence. The study makes a case for inclusion of environmental damage in both PDNA and loss and damage estimates to justify additional financial investments in disaster recovery.

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    Data availability

    All data supporting the findings of this analysis are freely available within the analysis and its supplementary information as well as via the GitHub repository: [https://github.com/nicholasmetherall/tropical-cyclone-impact-analysis]. These data may be used if cited appropriately. The workflows were all undertaken through open access and open-source software and reproducible programming environments. https://figshare.com/articles/dataset/tropical-cyclone-tree-cover-loss-github-repo_tar_gz/28759697.
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    Download referencesAcknowledgementsPacific Centre for Environment and Sustainability Development (PaCE) at the University of the South Pacific: Dr Hilda Sakiti Waqa, Dr Awnesh Singh, Mrs Harmindar Kaur. The Fenner School of Environment and Society, The Australian National University: Dr Bruce Doran and from the Statistics Unit (ANU) Mrs Alice Richardson. The Pacific Community (SPC): the Geoscience Energy and Maritime Division, Committee on Earth Observation Satellites (CEOS): Dr Brian Killough. Department of Environment and Conservation and the Department of Forestry of Vanuatu as well as the Ministry of Forestry-Silviculture and Research of Fiji. Dr Michelle Sims, Dr Nancy Harris and Professor Matthew Hansen from the World Resources Institute whose work and advice inspired and guided this study.Author informationAuthor notesNicholas Metherall and Elisabeth Holland contributed equally to this work.Authors and AffiliationsFenner School of Environment and Society, Australian National University, Canberra, ACT, 0200, AustraliaNicholas Metherall & Sara BeavisPacific Centre for Sustainability Futures, University of the South Pacific, Lower Campus Road E, Central Division, Suva, FijiNicholas Metherall, Salote Nasalo & Ceceilia Carol LouisInstitute at Brown for Environment and Society, Brown University, Waterman Street, Providence, RI, 02912, USAElisabeth HollandGeoscience Energy and Maritime (GEM) Division, The Pacific Community (SPC), Ratu Mara Road, Central Division, Suva, FijiMoleni Tu’uholoakiAuthorsNicholas MetherallView author publicationsSearch author on:PubMed Google ScholarElisabeth HollandView author publicationsSearch author on:PubMed Google ScholarMoleni Tu’uholoakiView author publicationsSearch author on:PubMed Google ScholarSara BeavisView author publicationsSearch author on:PubMed Google ScholarSalote NasaloView author publicationsSearch author on:PubMed Google ScholarCeceilia Carol LouisView author publicationsSearch author on:PubMed Google ScholarContributionsN.M. and E.H. conceived of the study. N.M., E.H., M.T. and S.B. designed the study. C.L. undertook the synthesis of TC information for Vanuatu. S.N. undertook the synthesis of TC information for Fiji. M.T. and E.H. provided guidance about the main tropical cyclone parameters to include in the analysis. N.M. collated the GFW and IBTrACS data together for analysis and developed the code base for these workflows to be replicated. M.T., C.L. and S.N. reviewed the code base. N.M. and E.H. produced the results and figures, wrote the original draft of the paper and responded to reviewers’ comments. All authors helped with interpretation of the data and contributed to reviewing and editing the paper.Corresponding authorCorrespondence to
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    Simulation study on the impact of check dams on water and sand in Xiliugou Basin and inner Mongolia section of the Yellow River

    AbstractSevere soil erosion on the Loess Plateau has led to a reduction in the area of agricultural land as well as an increase in the risk of flooding in the lower reaches of the Yellow River. Ten Kongdui (Mongolian for “Kongdui”, meaning “Great Mountain Gully”) is located in the upper reaches of the arsenic sandstone hilly and gully area. It is located in the heart of the Kubuqi sandstorm area. This area is one of the sandy and coarse sand production areas in the middle reaches of the Yellow River. It is also the main sand source area of the Inner Mongolia section of the Yellow River. The Ten Major Kongdui Xiliugou Basin is located in the upper and middle reaches of the Yellow River in the coarse sand-producing area. The gullies are deep and steep, with exposed arsenic sandstone. The chain reaction of heavy rain, flood and sediment is intense, making it a key channel for coarse sand from the Yellow River to flow into the river. To effectively address soil erosion in this area, curb the expansion of pyrite sandstone gully erosion and reduce the amount of sediment flowing into the Yellow River, it is proposed to establish an integrated engineering system of “soil and water conservation – sediment interception” within the basin. Through the measure of check dam local sediment storage will be achieved, the ecosystem functions will be restored, and the healthy life of the Yellow River will be maintained. Using distributed hydrologic modeling to explore the effects of a sand detention project in the Xiliugou watershed on watershed runoff and sand transport, the SWAT model was calibrated (1990–1999) and validated (2000–2020) using observed runoff and sediment data at Longtouguai Station, the simulated runoff and sand transport at Longtouguai Hydrological Station were found to fit well with the measured values through model simulation. The linear fitting coefficient R2 exceeds 0.6, it is considered that the linear relationship between the simulated values and the measured values is reasonable, which indicates that the reservoir model in SWAT model can be used for check dam simulation, and the water and sand impacts of water and sand reduction of the new check dam project on the Xiliugou watershed are analyzed through the results of the SWAT model calculations and the impacts of further calculations on the channel siltation of the Inner Mongolia section of the Yellow River are further calculated. The results show that: 1, the construction of check dams can affect the runoff volume of the basin to a certain extent, and intercepts part of the runoff, the average annual water reduction of the newly built 79 check dams is 2.44 × 106 m3. 2, it has a great influence on the sand transport in the basin, and the effect of sand reduction is obvious, the average annual sand reduction of the newly built 79 check dams is 4.09 × 105 t. 3, Reduces sand content in the Yellow River and enhances flushing of existing sediment in the Nei Mongol section of the river, and reduces water demand for sediment transport. The results of this study provide reference for promoting the construction of water sand replacement project in Xiliugou Basin and the high-quality development of the Yellow River Basin.

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    Data available on request from the authors. The data that support thefindings of this study are available from the corresponding author upon reasonable request.
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    Download referencesFundingThis research was supported by Key Special Project of the “Science and Technology Revitalization of Mongolia” Action (grant number 2022EEDSKJXM004-4), National Natural Science Foundation of China (grant number 42401022), Key Research and Development and Technology Transfer Program Project of Inner Mongolia Autonomous Region (2025SYFHH0219), Ordos Major Science and Technology Project – Research on the Integrated Scheduling Technology of Recycled Water and Other Multiple Sources in Ordos City (ZD20232323), Special project of basic scientific research business expenses of China Academy of water resources and hydropower (Grant No.MK0145B012021), Key R&D and Achievement Transformation Program of Inner Mongolia Autonomous Region (2025YFHH0005).Author informationAuthors and AffiliationsChina Institute of Water Resources and Hydropower Research, Yinshanbeilu Grassland Eco-Hydrology National Observation and Research Station, Beijing, 100038, ChinaWeijie Zhang, Wei Hu, Yingjie Wu, Pengcheng Tang & Wei LiInstitute of Water Resources of Pastoral Area Ministry of Water Resources, Hohhot, 010020, ChinaWeijie Zhang, Wei Hu, Yingjie Wu, Pengcheng Tang & Wei LiNorth China University of Water Resources and Electric Power, Zhengzhou, 450046, ChinaQingqing Qi, Xinyu Zhang, Fei Wang & Zezhong ZhangOrdos Development Center of Water Conservancy, Ordos, 017001, ChinaYong Liu, Rong Hao & Dequan ZhangAuthorsWeijie ZhangView author publicationsSearch author on:PubMed Google ScholarQingqing QiView author publicationsSearch author on:PubMed Google ScholarXinyu ZhangView author publicationsSearch author on:PubMed Google ScholarFei WangView author publicationsSearch author on:PubMed Google ScholarZezhong ZhangView author publicationsSearch author on:PubMed Google ScholarWei HuView author publicationsSearch author on:PubMed Google ScholarYingjie WuView author publicationsSearch author on:PubMed Google ScholarPengcheng TangView author publicationsSearch author on:PubMed Google ScholarWei LiView author publicationsSearch author on:PubMed Google ScholarYong LiuView author publicationsSearch author on:PubMed Google ScholarRong HaoView author publicationsSearch author on:PubMed Google ScholarDequan ZhangView author publicationsSearch author on:PubMed Google ScholarContributionsConceptualization, W.Z.; Z.Z.; Q.Q. and W.F.; data interpretation and methodology, X.Z. and W.F.; validation, W.H.; Y.W.; P.T. and Y.L.; software, W.L. and W.F.; original draft preparation, X.Z.; funding acquisition, R.H.; D.Z. and W.Z.; All authors have read and agreed to the published version of the manuscript.Corresponding authorCorrespondence to
    Xinyu Zhang.Ethics declarations

    Competing interests
    The authors declare no competing interests.

    Additional informationPublisher’s noteSpringer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.Rights and permissions
    Open Access This article is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License, which permits any non-commercial use, sharing, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if you modified the licensed material. You do not have permission under this licence to share adapted material derived from this article or parts of it. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by-nc-nd/4.0/.
    Reprints and permissionsAbout this articleCite this articleZhang, W., Qi, Q., Zhang, X. et al. Simulation study on the impact of check dams on water and sand in Xiliugou Basin and inner Mongolia section of the Yellow River.
    Sci Rep (2025). https://doi.org/10.1038/s41598-025-32381-4Download citationReceived: 27 June 2025Accepted: 09 December 2025Published: 17 December 2025DOI: https://doi.org/10.1038/s41598-025-32381-4Share this articleAnyone you share the following link with will be able to read this content:Get shareable linkSorry, a shareable link is not currently available for this article.Copy shareable link to clipboard
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    KeywordsCheck damRunoffSediment transportSoil and water assessment tool (SWAT) More

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    Large-scale experimental assessment of coyote behavior across urban and rural landscapes

    AbstractCarnivores must navigate the complexities of human modifications to their environment. Natural resources and biodiversity decline in urban areas, while people in rural areas often pose greater direct risk through actions such as hunting. To evaluate if carnivore populations adapt their behavior to local risks in rural and urban environments, we compared behavioral responses to novel objects in coyotes (Canis latrans). We placed an attractant at arrays of 30 camera-trap stations at 16 pairs of urban and rural field sites across the USA, with a novel object placed at half of the stations. Coyotes exhibited more cautious behavior and remained farther from the attractant at all sites with the novel object; however, urban coyotes got closer to the attractant than rural coyotes. There were few behavioral differences between urban and rural coyotes and none between eastern and western coyotes. Coyotes across the USA exhibit neophobic behavior but urban coyotes, especially western coyotes, are willing to take more risk (i.e., be closer to the attractant). The consistency in most metrics of coyote behavior suggest that solutions developed in one area could be universally useful. This study also demonstrates the effectiveness of a large, collaborative approach to studying broad-scale patterns in behavioral traits.

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    Data availability

    The datasets generated and analyzed during the current study are available from the corresponding author on reasonable request.
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    Download referencesAcknowledgementsWe thank Catherine Escamilla, Ashley Kimmel, Azana Cochran, Patricia Monzon, Sofia Monzon, Antonio Pepe, Nathan Folkerts, students of the Conservation Biology class at the University of Utah, and many others for their help in the field. Funding was provided by Utah State University, USDA-National Wildlife Research Center, Sageland Collaborative, University of Utah’s Global Change and Sustainability Center, the National Science Foundation (awards 1950350 and 1835410), the School of Natural Resources, University of Nebraska-Lincoln, Max McGraw Wildlife Foundation, Cook County Animal and Rabies Control, University of Wyoming, and University of Georgia Warnell School of Forestry and Natural Resources.FundingFunding was provided by Utah State University, USDA-National Wildlife Research Center, Sageland Collaborative, University of Utah’s Global Change and Sustainability Center, the National Science Foundation (awards 1950350 and 1835410), the School of Natural Resources, University of Nebraska-Lincoln, Max McGraw Wildlife Foundation, Cook County Animal and Rabies Control, University of Wyoming, and University of Georgia Warnell School of Forestry and Natural Resources. Author informationAuthors and AffiliationsDepartment of Wildland Resources & Ecology Center, Utah State University, Logan, UT, 84322, USAJulie K. YoungNorth Carolina Museum of Natural Sciences, Raleigh, NC 27612, USA & Dept. Forestry and Environmental Resources, North Carolina State University, Raleigh, NC, 27612, USARoland KaysUniversity of Utah, Salt Lake City, UT, 84112, USAAustin M. GreenDepartment of Natural Resources and the Environment, University of New Hampshire, Durham, NH, 03824, USARemington J. MollUSDA-National Wildlife Research Center, Predator Research Facility, Millville, UT, 84326, USAJeffrey T. Schultz, Stephanie Keller & Stewart W. BreckSchool of Natural Resources, University of Nebraska, Lincoln, NE, 68583, USAJohn F. Benson & Kyle D. DoughertyDepartment of Forest and Conservation Sciences, Department of Zoology, University of British Columbia, Vancouver, BC, V6T 1Z4, CanadaSarah Benson-AmramNational Park Service, Santa Monica Mountains National Recreation Area, 1 Baxter Way, Suite 180, Thousand Oaks, CA, 91362, USAJustin Brown & Seth P. D. RileySchool of Environment and Natural Resources, The Ohio State University, Columbus, OH, 43210, USAGrayson Cahal & Stan D. GehrtWarnell School of Forestry and Natural Resources, University of Georgia, Athens, GA, 30622, USABenjamin S. Carr & Michel T. KohlNatural Resources, Cleveland Metroparks, Strongsville, OH, 44149, USAJonathon D. CepekZoology & Physiology Department, University of Wyoming, Laramie, WY, 82071, USAEmily DavisDepartment of Environmental Science and Technology, University of Maryland, College Park, MD, USATravis GalloUrban Wildlife Program, Department of Natural Resources – Wildlife Resources Division, 30025, Social Circle, GA, USAKaitlin O. GoodeSchool of Biological Sciences, University of Utah, Salt Lake City, UT, 84112, USATrayl Grace, Sam Raber & Çağan H. ŞekercioğluSchool of Environmental and Forest Sciences, University of Washington, Seattle, WA, 98195, USAMolly Henling & Laura R. PrughNatural Science Division, Pepperdine University, Malibu, CA, USALucian Himes & Javier MonzónBlack Rock Forest, Cornwall, NY, 12518, USAScott LaPointMianus River Gorge, Inc, New York City, NY, USAChristopher NagyBarnard College, New York City, NY, 10027, USAEmma PalmerDepartment of Environmental Science and Policy, George Mason University, Fairfax, VA, 22030, USAKate RitzelDepartment of Environmental Science, Policy, and Management, University of California Berkeley, 130 Mulford Hall, Berkeley, CA, 94720-3114, USAChristopher J. Schell & Lauren StantonAuthorsJulie K. YoungView author publicationsSearch author on:PubMed Google ScholarRoland KaysView author publicationsSearch author on:PubMed Google ScholarAustin M. GreenView author publicationsSearch author on:PubMed Google ScholarRemington J. MollView author publicationsSearch author on:PubMed Google ScholarJeffrey T. SchultzView author publicationsSearch author on:PubMed Google ScholarJohn F. BensonView author publicationsSearch author on:PubMed Google ScholarSarah Benson-AmramView author publicationsSearch author on:PubMed Google ScholarJustin BrownView author publicationsSearch author on:PubMed Google ScholarGrayson CahalView author publicationsSearch author on:PubMed Google ScholarBenjamin S. CarrView author publicationsSearch author on:PubMed Google ScholarJonathon D. CepekView author publicationsSearch author on:PubMed Google ScholarEmily DavisView author publicationsSearch author on:PubMed Google ScholarKyle D. DoughertyView author publicationsSearch author on:PubMed Google ScholarTravis GalloView author publicationsSearch author on:PubMed Google ScholarStan D. GehrtView author publicationsSearch author on:PubMed Google ScholarKaitlin O. GoodeView author publicationsSearch author on:PubMed Google ScholarTrayl GraceView author publicationsSearch author on:PubMed Google ScholarMolly HenlingView author publicationsSearch author on:PubMed Google ScholarLucian HimesView author publicationsSearch author on:PubMed Google ScholarStephanie KellerView author publicationsSearch author on:PubMed Google ScholarMichel T. KohlView author publicationsSearch author on:PubMed Google ScholarScott LaPointView author publicationsSearch author on:PubMed Google ScholarJavier MonzónView author publicationsSearch author on:PubMed Google ScholarChristopher NagyView author publicationsSearch author on:PubMed Google ScholarEmma PalmerView author publicationsSearch author on:PubMed Google ScholarLaura R. PrughView author publicationsSearch author on:PubMed Google ScholarSam RaberView author publicationsSearch author on:PubMed Google ScholarKate RitzelView author publicationsSearch author on:PubMed Google ScholarSeth P. D. RileyView author publicationsSearch author on:PubMed Google ScholarChristopher J. SchellView author publicationsSearch author on:PubMed Google ScholarÇağan H. ŞekercioğluView author publicationsSearch author on:PubMed Google ScholarLauren StantonView author publicationsSearch author on:PubMed Google ScholarStewart W. BreckView author publicationsSearch author on:PubMed Google ScholarContributionsJY, SB, and RK conceived of the idea. JY, RK, SB, and JS wrote the manuscript text. JS and SK coded data, RM, AG, and JY conducted data analysis and made statistical figures. RK made the map. JB, SBA, JB, GC, BC, JC, KD, TG, SG, KG, TG, MH, LH, MK, SL, JM, CN, EP, KR, SR, CS, CS, LS, JY, SB, JS, RK, AG, and RM collected field data and reviewed the manuscript.Corresponding authorCorrespondence to
    Julie K. Young.Ethics declarations

    Competing interests
    The authors declare no competing interests.

    Additional informationPublisher’s noteSpringer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.Supplementary InformationBelow is the link to the electronic supplementary material.Supplementary Material 1Rights and permissions
    Open Access This article is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License, which permits any non-commercial use, sharing, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if you modified the licensed material. You do not have permission under this licence to share adapted material derived from this article or parts of it. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by-nc-nd/4.0/.
    Reprints and permissionsAbout this articleCite this articleYoung, J.K., Kays, R., Green, A.M. et al. Large-scale experimental assessment of coyote behavior across urban and rural landscapes.
    Sci Rep (2025). https://doi.org/10.1038/s41598-025-33189-yDownload citationReceived: 05 August 2025Accepted: 16 December 2025Published: 17 December 2025DOI: https://doi.org/10.1038/s41598-025-33189-yShare this articleAnyone you share the following link with will be able to read this content:Get shareable linkSorry, a shareable link is not currently available for this article.Copy shareable link to clipboard
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    KeywordsBayesian statisticsBehaviorCanis latransDetectionNovel objectUrbanization More

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    Evaluation of synergistic and regulatory effects of carbon-reduction and water-saving in the Yangtze River Delta Urban Agglomeration

    AbstractRealizing the synergistic effect of urban carbon-reduction and water-saving (CRWS) is of great significance for improving the urban carbon-water nexus and promoting urban sustainable development. From the perspective of the synergistic impact of intensive water resource utilization on carbon emissions, a theoretical framework is constructed. The relevant data on water resources and carbon emissions of the Yangtze River Delta Urban Agglomeration (YRDUA) from 2014 to 2023 are taken as the research objects for analysis. And a series of fixed effect models are adopted to evaluate the synergistic and regulatory effects of urban CRWS. Results show that the production water supply intensity has a positive impact on carbon emission intensity, while production water-saving intensity and ecological water intensity have negative impacts on carbon emission intensity in the YRDUA. Technical factors negatively regulate the synergy of carbon emission intensity and production water supply intensity. Structural factors negatively regulate the synergy between carbon emission intensity and water resource intensive utilization intensity. Technology, structure and scale factors have more significant effects on the synergistic effect of CRWS in areas with higher urban development level.

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    IntroductionIn recent years, the level of urban development has been continuously expanding globally1. As the main carbon emitters and water consumers, the improvement of the development level of cities has led to a series of problems such as increased carbon emission, water resource consumption, and worsening water pollution2. This has had a negative impact on the synergy and virtuous cycle of carbon emission and water resource utilization3. Carbon emission and water resource scarcity have gradually become important bottlenecks for the sustainable development of urban systems, and the two have affect and interact with each other4,5,6. Water resources development, transportation, and sewage treatment will cause carbon dioxide emissions, and the climate change caused by carbon emission will also have a profound impact on the improvement of water resource utilization level7. Therefore, it is worth considering about how to realizing synergistic development of low carbon emission and water resource utilization, improve the urban carbon–water nexus and promote the sustainable development of urban economy.At present, the carbon emission issue characterized by the increasing concentration of carbon dioxide in the atmosphere and the water utilization issue characterized by water resource scarcity are the key research focuses in the current theory of urban carbon–water correlation. In industrialized countries, energy consumption leads to large greenhouse gas emissions. In order to achieve low-carbon development, the promotion and utilization of energy technology are essential, and the consumption of water resources also increases accordingly8. Byers et al.9 and Konadu et al.10 analyzed the implementation path of low-carbon development in the UK. The results suggested that the UK might face significant water stress in the future to enable high carbon capture and storage (CCS) for thermal power generation. However, in the long run, improving the utilization rate of water resources is the most marginal measure to reduce emissions and balance economic development with environmental improvement11. Therefore, water-saving can lead to cascading energy saving, thus achieving carbon reduction12. For a water plant with a conventional water supply of 105 t/d, saving 10% of water is 104 t/d, and based on the carbon emission of 0.3 kg per ton of water supply, it is preliminarily estimated that carbon emission can be reduced by more than 1095 t/year. Meanwhile, the sustainable utilization of water resources will have an impact on carbon emission13. Relevant studies have shown that carbon footprint exists in the construction of water source projects, water supply, and water pollution treatment14,15,16,17. Wang et al.18 found that industrial water consumed the most energy and emitted the most carbon during China’s economic and social water cycle. The aforementioned studies indicate that there is a close correlation between water resource utilization and carbon emissions. Therefore, it is necessary to formulate relevant policies to determine and balance the carbon-reduction and water-saving goals on the premise of ensuring the normal operation of the economy and society19. Factors such as total energy consumption, industrial structure, technological progress and population size has produced significant regulatory effect on urban carbon emission and water resource utilization20,21,22. In addition, the differences in urban development level also have different impacts on controlling carbon emission and improving the efficiency of water resource intensive utilization23,24.In 2001, the Intergovernmental Panel on Climate Change (IPCC) defined synergies as the economic and social benefits brought about by the realization of greenhouse gas emission reduction targets, such as technological innovation and progress, air quality improvement, ecological environment improvement, etc. Relevant studies mainly involve the synergistic effect of low-carbon development and production technology development25, the synergistic effect between pollution reduction and carbon reduction26,27, and the synergistic effect of energy, climate and environmental policies28. The impact of technological progress on carbon emission has a dual characteristic. On the one hand, the progress of production technology can first be reflected in the reduction of fossil fuel demand, thereby achieving a reduction in carbon emission. On the other hand, technological progress can promote economic growth and lead to more energy consumption and carbon dioxide emissions29. Climate and environmental policies can effectively reduce carbon emission and energy consumption, and exhibit regional heterogeneity characteristics30. At present, research methods for synergistic effects mainly include cross elasticity analysis of collaborative control31, regression analysis of synergistic effects32, general equilibrium model33, STIRPAT model34, physiological process model35. In recent years, quantitative research on the synergy of carbon–water relationships has been continuously deepened. Jiang et al.36 took Tianjin in China as the research object and used a system dynamics model to study the feedback mechanism between water resource utilization and urban carbon emissions. The results showed that carbon emissions existed throughout the entire life cycle of water resource supply, allocation, and utilization. Danish7 analyzed the relationship between water productivity and carbon emissions using the auto-regressive distributed lag method. The results indicated that there was a causal relationship between the two in both the long term and the short term. Zhao et al.37 constructed a policy evaluation model to analyze the energy-carbon–water correlation in China. The results indicated that the environmental effects brought about by water conservation were significant.There are rich achievements in the research of the synergistic effects brought about by carbon-reduction goals, but research on the synergistic effects of urban carbon emission based on the perspective of water resource intensive utilization is still lacking. Therefore, this study constructs a theoretical framework for evaluating the synergistic effect of urban carbon-reduction and water-saving (CRWS) based on the synergistic impact of water resource intensive utilization on carbon emission. On this basis, the fixed effect panel model and multiple parallel regulation effect model are introduced to analyze the synergistic effect and explore the regulatory effect of urban CRWS under the development level of heterogeneous cities. Finally, the Yangtze River Delta Urban Agglomeration (YRDUA) is taken as the research object for quantitative analysis. The research hypotheses are as follows: (1) The impacts of production water supply, production water-saving, and ecological water use on carbon emissions are different or even opposite. (2) The moderating effects of technical, structural, and scale factors on the synergistic effect of CRWS in the YRDUA vary significantly. (3) Moderating variables such as technical, structural, and scale factors have a more obvious impact on the synergistic effect of CRWS in areas with a higher level of urban development.This study contributes to the existing literature in three aspects: (1) Three indexes including production water supply intensity, production water-saving intensity and ecological water intensity are adopted to comprehensively reflect the water resource intensive utilization intensity. (2) The synergistic impact of water resource intensive utilization intensity on carbon emission is analyzed. (3) The regulatory effects model of technology, structure, and scale factors on the synergy of urban CRWS are established. In addition, this study takes heterogeneity of urban development level into account to explore whether the synergistic and regulatory effects of CRWS are different under the heterogeneity of city size and urbanization rate. The research on the synergistic and regulatory effects of urban CRWS is helpful to reveal the effective ways of low carbon emission, water resource intensive utilization and urban carbon neutrality, and improve the urban carbon–water nexus from the small and medium-sized regional scale.Materials and methodsAnalysis framework for the synergistic and regulatory effects of urban carbon-reduction and water-savingAs shown in Fig. 1, the impact of water resource intensive utilization on carbon emission can be decomposed into the synergistic effects of the intensive utilization of production water resources and ecological water resources, as well as the role of regulatory variables such as technology, structure, and scale factors.Fig. 1The synergistic impact mechanism of water resource intensive utilization on carbon emission.Full size imageFirstly, the improvement of the production water intensive level brings opportunities for urban low-carbon development. In the process of soc-economic development, human production activities inevitably generate a large amount of carbon dioxide, among which industrial production industries such as cement and steel with high energy consumption are the main carbon emitting industries. Water resources, as a medium or green energy, provide important support for reducing carbon sources38. On the one hand, the strengthening of production water supply intensity helps to improve the carbon utilization efficiency of carbon-containing resources and reduce carbon emission per unit output39. On the other hand, water conservation in production can not only reduce water costs but also decrease the discharge of wastewater, thereby effectively reducing the actual carbon emissions generated during the production process. 40.Secondly, the improvement of ecological water intensive level is the basis for ensuring the low-carbon development of soc-economy. Plants in ecosystems including woodland, grassland, wetland convert carbon dioxide in the air into organic carbon through photosynthesis, with a carbon sequestration capacity of up to 90%41. As a crucial environmental factor, water resources can promote the ecological environment system to give full play to the function of carbon sink. By ensuring that ecological water is not occupied by production water, the utilization intensity of ecological water can be enhanced. It helps to achieve the protection and restoration of natural ecological landscapes such as forests and wetlands, as well as the construction and maintenance of artificial ecological landscapes such as economic forests, green spaces, and parks. While improving residents’ living environment and quality of life, urban carbon absorption capacity can be enhanced to reduce atmospheric carbon dioxide concentration42.Finally, with the premise of water resource intensive utilization and ecological environment protection, giving full play to the regulatory role of energy-related technologies, structures, and scale factors is an important way to achieve low-carbon development goals. Specifically, strengthening the innovation and promotion of energy utilization technology and reducing energy consumption intensity are conducive to reducing the actual carbon emission generated in the production process43. Reducing the consumption of coal in industrial production, appropriately promoting the use of clean energy represented by hydropower, and optimizing the energy structure and industrial structure can promote the formation of a production mode with high output, low consumption and low emission44. In addition, relevant studies show that industrial fixed asset investment has a long-term and stable correlation with energy consumption and carbon emission. Therefore, the investment scale of industrial fixed investment is also an important factor affecting low-carbon development45.In order to analyze and evaluate the synergistic and regulatory effects of urban CRWS, we proposes a four-stage analysis framework (as shown in Fig. 2). The first stage is to quantitatively analyze the change trend of urban carbon emission intensity and water resource intensive utilization intensity. The second stage is to analyze the synergistic and regulatory effects of urban CRWS. Firstly, production water supply intensity, production water-saving intensity, and ecological water intensity are used to reflect the water resource intensive utilization intensity. A fixed effect model is adopted to analyze the synergistic impact of water resource intensive utilization intensity on carbon emission. Then, a multiple parallel regulation effect model is introduced to analyze the regulation effects of energy-related technology, structure and scale factors on the synergistic effect of urban CRWS. Finally, taking the level of urban development into account, we explore the differences in the synergistic and regulatory effects of CRWS under the heterogeneity of city size and urbanization rate. The third stage is to take the YRDUA as an example to conduct empirical research. The fourth stage is to propose the policy implications of the research.Fig. 2Urban carbon-reduction and water-saving synergistic effects analysis framework.Full size imageStudy area and data sourcesThe YRDUA is located on the alluvial plain at the mouth of the Yangtze River, with a total area of 211,700 square kilometers and a population of 225 million. The YRDUA consists of Shanghai, 9 cities including Nanjing, Wuxi, Changzhou, Suzhou, Nantong, Yangzhou, Zhenjiang, Yancheng and Taizhou in Jiangsu Province, 9 cities including Hangzhou, Ningbo, Wenzhou, Huzhou, Jiaxing, Shaoxing, Jinhua, Zhoushan and Taizhou in Zhejiang Province, and 8 cities including Hefei, Wuhu, Ma’anshan, Tongling, Anqing, Chuzhou, Chizhou and Xuancheng in Anhui Province. With the proposal of the integrated development strategy for the YRDUA in 2018, coupled with the development strategy of the Yangtze River Economic Belt, the YRDUA is facing significant development opportunities. However, due to the rapid population growth and the accelerated urbanization process, the YRDUA still faces huge dual pressures of resource and environment. Therefore, conducting relevant research on the synergistic and regulatory effects of CRWS can provide a basis for improving the utilization level of water resources and enhancing environmental quality in the YRDUA. And it has guiding significance for the management practice of promoting the green and low-carbon development of the YRDUA. In view of this, the study takes 27 cities in the YRDUA as the basic research area.The panel data involved in this study spans from 2014 to 2023. Statistical data such as GDP and population of each city are acquired from the China Urban Statistical Yearbook, and the statistical data such as carbon emission intensity, production water consumption, production water-saving, and energy consumption are sourced from the China Urban Construction Yearbook. Statistical data such as industrial structure and industrial fixed investment are obtained from the Shanghai Statistical Yearbook, Jiangsu Statistical Yearbook, Zhejiang Statistical Yearbook, and Anhui Statistical Yearbook. For a small portion of missing data, interpolation method is used to fill in.Variable selectionCarbon emission intensityThe carbon emission intensity represents the amount of CO2 emitted per unit of output. It can be expressed as Eq. (1):$$CAR_{j} = T_{j} /GDP_{j}$$
    (1)
    where CARj refers to the carbon emission intensity of city j, Tj refers to the total carbon emission of the city j, and GDPj refers to the gross domestic product of the city j.We draw on the method of Xu et al.46, which calculates the carbon emission of different types of energy consumption separately and then accumulates them to obtain the total CO2 emissions. It can be expressed as follows:$$T_{j} = sumlimits_{i = 1}^{8} {E_{ji} times f_{i} }$$
    (2)
    where i represents the types of fossil fuels, namely coal, coke, crude oil, gasoline, kerosene, diesel, fuel oil and natural gas. Eji represents the consumption of energy i by the city j. fi is the carbon emission coefficient of energy i, mainly derived from the National Greenhouse Gas Inventory Guidelines published by the Intergovernmental Panel on Climate Change (IPCC) in 2006. The carbon emission coefficients of the above five fossil fuels are 0.5714, 0.8550, 0.5857, 0.6185 and 0.4483 respectively.Water resource intensive utilization intensityThe water resource intensive utilization intensity is a concept that balances the production and ecological benefits of water resources. We adopt the production water supply intensity, production water-saving intensity, and ecological water intensity to describe the water resource intensive utilization intensity. Specifically, the production water supply intensity refers to the amount of water consumed per unit of output. The production water-saving intensity refers to the proportion of water saved per unit of water consumption. Ecological water intensity refers to the per capita water consumption in the ecological environment. They are expressed in Eqs. (3) ~ (5):$$WU_{j} = WC_{j} /GDP_{j}$$
    (3)
    $$WS_{j} = PW_{j} /WC_{j}$$
    (4)
    $$EW_{j} = EE_{j} /POP_{j}$$
    (5)
    where WUj, WSj, and EWj respectively represent the production water supply intensity, production water-saving intensity, and ecological water intensity of the city j. WCj, PWj, and EEj respectively represent the total amount of production water, production water-saving, and ecological environment water used of the city j. GDPj and POPj respectively represent the gross national product and total population of the city j.Regulatory variablesEnergy consumption intensityEnergy consumption intensity reflects the progress of regional energy utilization technology. The lower the energy consumption intensity, the stronger the urban energy rational utilization capacity and the higher the energy technology level47. We adopt the total amount of energy consumed per unit of output to represent the energy consumption intensity, which can be calculated as follows:$$ECI_{j} = EC_{j} /GDP_{j}$$
    (6)
    where ECIj and ECj represent the energy consumption intensity and total energy consumption of the city j, respectively.Energy consumption structureCoal consumption is the main source of CO2 emissions, and could have a significant impact on atmospheric carbon emission. Therefore, we use the proportion of coal consumption in total energy consumption to represent the energy consumption structure, which can be calculated as follows:$$ECS_{j} = CC_{j} /EC_{j}$$
    (7)
    where ECSj and CCj represent the energy consumption structure and total coal consumption of the city j, respectively.Industrial structureAs the main sector of energy consumption, industry has a significant impact on carbon emission intensity48,49. We use the industrial output as a proportion of the gross national product to express the industrial structure, which can be calculated as follows:$$IS_{j} = IO_{j} /GDP_{j}$$
    (8)
    where ISj and IOj represent the industrial structure and industrial output of the city j, respectively.Industrial investment scaleThe increase in industrial investment scale represents the expansion of industrial production scale, which can exacerbate the expansion effect of carbon emission to some extent50. We use the per capita fixed industrial investment to represent the scale of industrial investment, which can be calculated as follows:$$IIS_{j} = IIA_{j} /POP_{j}$$
    (9)
    where IISj and IIAj represent the industrial investment scale and total industrial fixed assets investment of the city j, respectively.Synergistic effect analysis modelThe synergistic effect of urban CRWS is analyzed from a quantifiable perspective using a panel fixed effect model. Taking into account the characteristics of the carbon–water nexus and combining with the theoretical mechanism analysis mentioned earlier, we divide the regulatory variables related to energy into three categories: technical, structural and scale factors. The energy consumption intensity is adopted to reflect technical factor, energy consumption structure and industrial structure are adopted to reflect structural factors, and industrial investment scale is adopted to reflect scale factors. On this basis, a fixed effect model is constructed to analyze the synergistic effect of water resource intensive utilization on carbon emission. The model can be constructed as follows:$$CAR_{jt} = alpha_{01} + alpha_{11} WU_{jt} + alpha_{21} ECI_{jt} + alpha_{31} ECS_{jt} + alpha_{41} IS_{jt} + alpha_{51} IIS_{jt} + lambda_{j1} + mu_{t1} + varepsilon_{jt1}$$
    (10)
    $$CAR_{jt} = alpha_{02} + alpha_{12} WS_{jt} + alpha_{22} ECI_{jt} + alpha_{32} ECS_{jt} + alpha_{42} IS_{jt} + alpha_{52} IIS_{jt} + lambda_{j2} + mu_{t2} + varepsilon_{jt2}$$
    (11)
    $$CAR_{jt} = alpha_{03} + alpha_{13} EW_{jt} + alpha_{23} ECI_{jt} + alpha_{33} ECS_{jt} + alpha_{43} IS_{jt} + alpha_{53} IIS_{jt} + lambda_{j3} + mu_{t3} + varepsilon_{jt3}$$
    (12)
    where (alpha_{0m}) ~ (alpha_{5m}) (m = 1, 2, 3) are the parameters to be estimated. (lambda_{j}),(mu_{t}) and (varepsilon_{jt}) represent individual fixed effects, time fixed effects and random error terms, respectively.Multiple parallel regulatory effect modelThe regulatory effect means that the direction and degree of the influence of the regulatory variable on the main effect can be different due to individual characteristics or environmental conditions51,52. In empirical studies, the regulatory effect is specifically manifested as the strengthening or weakening of the relationship between the explanatory variable and the explained variable by the regulatory variable53. In general, the regulatory effect is based on the main effect. By constructing corresponding interaction terms and combining the symbols of the main effect and the regulatory effect, the direction and degree of the influence of the regulatory variables on the main effect are judged and analyzed (as shown in Fig. 3).Fig. 3Schematic diagram of the regulatory effect.Full size imageThe water resource intensive utilization intensity indicators (i.e. WUjt, WSjt, and EWjt) are adopted as the main effect to carbon emission intensity (CARjt), and ECIjt, ECSjt, ISjt, and IISjt are adopted as regulatory variables. By introducing the interaction terms between the four regulatory variables mentioned above and the intensity variable of water resource intensive utilization, a multiple parallel regulatory effect model is constructed as follows:$$begin{gathered} CAR_{jt} = alpha_{01} + alpha_{11} WU_{jt} + alpha_{21} ECI_{jt} + alpha_{31} ECS_{jt} + alpha_{41} IS_{jt} + alpha_{51} IIS_{jt} + beta_{{{11}}} WU_{jt} times ECI_{jt} + hfill \ , beta_{21} WU_{jt} times ECS_{jt} + beta_{31} WU_{ji} times IS_{jt} + beta_{{{41}}} WU_{jt} times IIS_{jt} + lambda_{j1} + mu_{t1} + varepsilon_{jt1} hfill \ end{gathered}$$
    (13)
    $$begin{gathered} CAR_{jt} = alpha_{02} + alpha_{12} WS_{jt} + alpha_{22} ECI_{jt} + alpha_{32} ECS_{jt} + alpha_{42} IS_{jt} + alpha_{52} IIS_{jt} + beta_{{{12}}} WS_{jt} times ECI_{jt} + hfill \ , beta_{22} WS_{jt} times ECS_{jt} + beta_{32} WS_{ji} times IS_{jt} + beta_{{{42}}} WS_{jt} times IIS_{jt} + lambda_{j2} + mu_{t2} + varepsilon_{jt2} hfill \ end{gathered}$$
    (14)
    $$begin{gathered} CAR_{jt} = alpha_{03} + alpha_{13} EW_{jt} + alpha_{23} ECI_{jt} + alpha_{33} ECS_{jt} + alpha_{43} IS_{jt} + alpha_{53} IIS_{jt} + beta_{{{13}}} EW_{jt} times ECI_{jt} + hfill \ , beta_{23} EW_{jt} times ECS_{jt} + beta_{33} EW_{ji} times IS_{jt} + beta_{{{43}}} EW_{jt} times IIS_{jt} + lambda_{j3} + mu_{t3} + varepsilon_{jt3} hfill \ end{gathered}$$
    (15)
    where (alpha_{0m}) ~ (alpha_{5m}) (m = 1, 2, 3), (beta_{1n}) ~ (beta_{4n}) (n = 1, 2, 3) are the parameters to be estimated. (lambda_{j}),(mu_{t}) and (varepsilon_{jt}) represent individual fixed effects, time fixed effects and random error terms, respectively.In order to further analyze whether the regulatory effects of energy-related technology, structure and scale factors as regulatory variables would be different due to different levels of urban development, we group the study regions according to urban development scale and urbanization level. The synergistic and regulatory effects of CRWS based on the heterogeneity of urban development levels are studied. Specifically, the scale of urban development is defined according to the range of the permanent population of the city. The level of urbanization is defined based on the size of the urbanization rate. The groups are shown in (Tables 1, 2).Table 1 Classification of urban development scale.Full size tableTable 2 Classification of urbanization levels.Full size tableResultsTrends of carbon emission and water resource intensive utilization intensityThe trends of carbon emission intensity and water resource intensive utilization intensity in 27 cities of the YRDUA from 2014 to 2023 are shown in Fig. 4. The averages of carbon emission intensity and production water supply intensity show decreasing trend year by year. Specifically, the average of carbon emission intensity decreased from 0.229 tons/104 yuan in 2014 to 0.149 tons/104 yuan in 2023 (Fig. 4a). The average of production water supply intensity decreased from 4826 m3/104 yuan in 2014 to 3708 m3/104 yuan in 2023 (Fig. 4b). The average of production water-saving intensity increased year by year, from 9.528% in 2014 to 12.925% in 2023 (Fig. 4c). The average of ecological water intensity showed a fluctuating upward trend, decreasing from 8.451m3/person in 2014 to 8.356m3/person, and gradually increasing to 10.961m3/person in 2023 (Fig. 4d). Overall, during the study period, the carbon emission per unit output of the YRDUA continued to decrease, while the level of water resource intensive utilization improved.Fig. 4Evolution trends of the intensity of carbon emission and water resource intensive utilization in the YRDUA.Full size imageThe trends of carbon emission intensity and water resource intensive utilization intensity in Shanghai, Jiangsu, Zhejiang, and Anhui are shown in Fig. 5. During the study period, the carbon emission intensity in Shanghai, Jiangsu, Zhejiang and Anhui showed a fluctuating downward trend (Fig. 5a). However, in 2018, carbon emissions in various provinces showed an upward trend, mainly attributed to the stable growth of coal consumption and the continuous increase in the use of oil and natural gas. The production water supply intensity in Shanghai showed a significant downward trend and was significantly higher than that of other three provinces (Fig. 5b). The production water-saving intensity in Shanghai and Jiangsu has been continuously improving, while that in Zhejiang and Anhui has not changed much (Fig. 5c). Except for Shanghai, the ecological water intensity in Jiangsu, Zhejiang and Anhui decreased before 2016 and gradually increased after that. It might be because in the early years, in order to expand production, production water has encroached upon ecological water. However, with the development of the economy and the deterioration of the ecological environment, the government has realized the importance of ecological protection and thus gradually increased ecological water consumption (Fig. 5d).Fig. 5Trends of carbon emission intensity and water resource intensive utilization intensity at the provincial level.Full size imageThe synergistic effect of CRWS in the YRDUABefore the synergistic effect analysis, the appropriate model form is selected and analyzed by F-test and Hausman test. The results show that F-value is 4.193 and (chi^{2}) is 123.779, both of which pass the significance test at 1% level. Therefore, the fixed effect model (FE model) should be selected as the most appropriate model. Based on Eqs. (10) ~ (12), the regression results of the synergy effect of CRWS in 27 cities of the YRDUA are obtained, as shown in Table 3.Table 3 Regression results of synergistic effect of CRWS in the YRDUA.Full size tableAs can be seen from models (1) to (3) in Table 3, the production water supply intensity has a positive impact on carbon emission intensity. With the increase of production water supply intensity, the carbon emission intensity also increase, and both have the same change trend. However, the production water-saving intensity has a negative impact on carbon emission intensity, indicating that the increase of production water-saving intensity weakens the increase of carbon emission to a certain extent. The ecological water intensity has a significant negative impact on carbon emission intensity, indicating that the increase in ecological water consumption contributes to the reduction of carbon emission. The adjusted R2values in Table 3 range from 0.367 to 0.417, indicating a relatively low goodness-of-fit of the model. This may be because the model only considers the impacts of the level of intensive water resource utilization and moderating factors on carbon emissions, without taking into account the impact of the interaction between them on carbon emissions. In addition, the heterogeneity in urban development levels can also lead to differences in the impact of the level of intensive water resource utilization.In addition, except for the industrial fixed asset investment, the regression coefficients of energy consumption intensity, energy consumption structure and industrial structure are significantly positive. It indicates that, with the increase of energy consumption, coal consumption and industrial output, carbon emission of the YRDUA also increase.To further verify the reliability of the conclusion, this paper adopts two methods for robustness test: changing the sample size and replacing the core independent variables. First of all, the Shanghai area holds a special political and economic status in China, and there may be particularities in water resource utilization and carbon emission control. Therefore, Shanghai is excluded and the relevant data of the remaining 26 cities are used for regression analysis again. Second, the industrial water-saving intensity is used to replace the production water-saving intensity for regression analysis. The results of the robustness test are shown in models (4) to (7) in Table 3. It can be known that whether special samples are excluded or core explanatory variables are replaced, the synergy effect exists. Meanwhile, the coefficients and significance levels of other variables have not changed significantly, further indicating that the regression results are robust.The regulation effect of CRWS in the YRDUACollinearity diagnosis is conducted on four moderating variables: energy consumption intensity, energy consumption structure, industrial structure, and industrial investment scale. Pairwise comparison of the above four variables revealed that the maximum correlation coefficient is 0.2498 (i.e., the correlation coefficient between industrial structure and industrial investment scale). Therefore, it can be considered that there is almost no collinearity among the moderating variables. On this basis, multiple parallel regulatory model is introduced to explore the regulatory effects of technical factors, structural factors and scale factors on the synergistic effect of CRWS in the YRDUA, and the results are shown in Table 4. From the perspective of technology, the increase in energy consumption has a negative effect on the synergy between carbon emission and production water supply intensity. The energy consumption intensity does not have a significant regulatory effect on the synergy dominated by production water-saving intensity and ecological water intensity. From the perspective of structure, compared with the adjustment of industrial structure, the optimization of energy consumption structure has a more significant regulatory effect on the synergy dominated by production water supply intensity and production water-saving intensity in the YRDUA. From the perspective of scale, the industrial investment scale has no significant regulatory effect on the synergistic effect of CRWS in the YRDUA.Table 4 Regression results of CRWS regulatory effect in the YRDUA.Full size tableThe synergistic and regulatory effects of CRWS in the YRDUA based on the heterogeneity of urban development levelAnalysis based on the heterogeneity of urban scaleAccording to the urban resident population, 27 cities in the YRDUA are divided into large scale cities, medium scale cities and small scale cities. The synergistic effect and the regulatory effects of technology, structure and scale factors of CRWS are analyzed respectively, and the results are shown in Table 5.Table 5 Analysis of regulatory effect of CRWS in the YRDUA based on urban scale heterogeneity.Full size tableFrom models (1) to (3) in Table 5, it can be seen that the production water supply intensity and production water-saving intensity of large scale cities have a significant positive impact on the carbon emission intensity. In addition to the scale of industrial investment, energy consumption intensity, energy consumption structure and industrial structure have a negative regulatory effect on the synergy dominated by production water supply intensity in large cities. The energy consumption structure and industrial investment scale have negative regulating effects on the synergy of carbon emission and production water-saving intensity in large cities.From models (4) to (6) in Table 5, it can be seen that production water supply intensity and ecological water intensity of medium scale cities have significant positive and negative impacts on carbon emission intensity, respectively. With the increasing of production water consumption and decreasing of ecological water consumption, carbon emission of medium-sized cities increases significantly. In terms of the regulatory effect of technology, structure and scale factors on the synergistic effect of CRWS, industrial structure has a positive regulatory effect on the synergy of carbon emission and production water supply intensity of medium scale cities. The industrial investment scale also has a positive regulatory effect on the synergy of carbon emission and ecological water intensity in medium scale cities.From models (7) to (9) in Table 5, it can be seen that with the increase of water consumption in production, the carbon emission of small scale cities also increases. In terms of the regulatory effect of technology, structure and scale factors, only the scale factor (industrial investment scale) has a positive regulatory effect on the synergy of carbon emission and production water supply intensity.Analysis based on the heterogeneity of urbanization levelAccording to the urbanization rate, 27 cities in the YRDUA are divided into cities with high urbanization rate, medium urbanization rate and low urbanization rate. The synergistic effect of urban CRWS and the regulatory effect of technology, structure and scale factors are analyzed respectively, and the results are shown in (Table 6).Table 6 Analysis of regulating effect of CRWS in the YRDUA based on urbanization level heterogeneity.Full size tableFrom models (1) to (3) in Table 6, it can be seen that the production water-saving intensity and ecological water consumption intensity of cities with high urbanization rate have a significant positive impact on carbon emission intensity. It indicates that the increase of production water-saving amount and ecological water consumption have a positive impact on the increase of carbon emission of cities with high urbanization rate. In terms of the regulatory effects of technology, structure and scale factors, energy consumption structure weakens the synergistic effect of production water-saving intensity in cities with high urbanization rate. Energy consumption intensity and industrial investment scale have a negative regulatory effect on the synergy of carbon emission and ecological water intensity in cities with high urbanization rate.From models (4) to (6) in Table 6, it can be seen that the increase of production water consumption and the decrease of ecological water consumption have positive impacts on the increase of carbon emission in cities with medium urbanization rate. In terms of the regulatory effects of technology, structure and scale factors, energy consumption intensity has a negative regulatory effect on the synergy of production water supply intensity in cities with medium urbanization rate. The industrial investment scale has a strong effect on the synergy of carbon emission and ecological water intensity in cities with medium urbanization rate.From models (7) to (9) in Table 6, it can be seen that the increase of water consumption in production has a positive impact on the increase of carbon emission in cities with low urbanization rate. In terms of the regulatory effects of technology, structure and scale factors, only the scale of industrial investment has a positive regulatory effect on the synergy of carbon emission and production water supply intensity.DiscussionAnalysis of carbon emission and water resource intensive utilizationIn recent years, the diversification of energy structure and non-fossil energy types in the production process has contributed to the continuous reduction of carbon emission intensity in the YRDUA54. However, the pressure of carbon emission reduction in the YRDUA is still great, and the energy structure and industrial structure need to be further optimized and adjusted to meet the national emission reduction targets55. The water resource intensive utilization in the YRDUA has been improved, which is partly attributed to the strictest water resource management system implemented in China. The reduction of supply has promoted the innovation of production technology and water-saving technology, and effectively reduced the demand for production water and increased the production water-saving amount56. In addition, some areas are indeed in the state of “no water available”, and a large number of virtual water imports have led to changes in China’s water consumption pattern, which has inhibited the growth of production water demand (Wang and Ge, 202057). Therefore, the water resource management policies adopted must effectively improve the level of water resource intensive utilization from multiple aspects such as improving the water utilization efficiency and increasing the amount of water-saving in production. For example, innovations in water recycling and sewage treatment technologies can not only improve the efficiency and effectiveness of production water use, promote water conservation in production, but also ensure the amount of ecological water use. Guaranteeing the construction of green facilities such as urban green spaces, parks, and artificial forests through the ecological supply of water resources is conducive to enhancing the carbon sequestration capacity of the region.The synergistic impact of water resource intensive utilization on carbon emission intensityThe synergistic effect of intensive water utilization intensity on carbon emission intensity in the YRDUA is significant (Fig. 6). Specifically, the production water supply intensity, production water-saving intensity and ecological water intensity are significant at the levels of 10%, 5% and 1% respectively. The regression coefficient of production water supply intensity is 0.003, indicating that it has the same changing trend as carbon emissions. The regression coefficients of production water-saving intensity and ecological water intensity are both -0.001, indicating that their changing trends are opposite to that of carbon emission intensity.This means that appropriate reduction of production water consumption, improvement of production water-saving level, and protection of ecological water consumption can improve the level of water resource intensive utilization and help reduce carbon emission58.Fig. 6Analysis of synergistic effect of CRWS in the YRDUA. The red arrow refers to the influence of the regulatory variables with the main effect of production water supply intensity. The green arrow refers to the impact of the regulatory variables with the main effect of water-saving intensity in production. The purple arrow refers to the impact of the regulatory variables with the main effect of ecological water intensity. + refers to the positive influence, W, M and S represent the degree of weak, medium and strong influence, and the scope of corresponding regression coefficients are (0.00, 0.05), [0.05, 0.10) and [0.10, (infty)).—refers to the negative influence, W, M and S represent the degree of weak, medium and strong influence, respectively, and scope of the corresponding regression coefficients are (-0.05, 0.00), (-0.10, -0.05], (-(infty), -0.10].The same below.Full size imageTechnology and structural factors have improved the carbon emission intensity of the YRDUA to a certain extent, indicating that while technological progress has brought about the improvement of production efficiency, its rebound effect on carbon emission reduction and water-saving has gradually emerged, resulting in the decrease of the synergy of CRWS59. On the one hand, technological progress can effectively improve the efficiency of water resource utilization, reduce carbon emissions per unit of water used, and achieve water conservation. On the other hand, technological progress will lead to the further expansion of production scale, the production water consumption and its carbon emissions will also increase accordingly, thereby generating a rebound effect. The foundation of energy structure and industrial structure is relatively weak, and the secondary industry characterized by high-pollution and high-emission still occupies a dominant position. It not only intensifies the contradiction between production water and ecological water, but also weakens the synergistic effect of CRWS60. However, if only a single carbon emission reduction target is set, it would cause excessive emission reduction burden on the traditional industries that support economic development, and weaken the power of urban economic development. Therefore, the adoption of total water resource management measures from the perspectives of water resource intensive utilization, combined with the appropriate adjustment and improvement of energy structure and industrial structure, can help to promote the synergistic effect of CRWS.Heterogeneity analysis and policy implications of CRWS regulatory effectsCompared with areas with lower urban development level, regulatory variables such as technology, structure and scale factors have more obvious influences on the synergistic effect of CRWS in areas with higher urban development level (Fig. 7). For cities with large scale and high urbanization level, energy consumption intensity, energy consumption structure, industrial structure and industrial investment scale all negatively regulate the synergistic effect of CRWS. This is because in cities with a higher level of development, highly developed industrial production has an increasing demand for water resources and high-emission fuels such as coal, which leads to more severe problems of water resource consumption and carbon emission61. In addition, policies and measures dominated by command-based environmental regulations make industrial production more inclined to adopt end-treatment methods to reduce water utilization and carbon emission, rather than innovation and promotion of production technology62. The status quo of high energy and water consumption industries has not been fundamentally improved, resulting in the inability to achieve synergies of CRWS. The scale of industrial investment has a strong regulatory effect on the synergy of CRWS in cities with low development level. Compared with large cities, small cities have relatively sparse population and abundant energy resources. With the rapid expansion of industrial investment scale, water resource and carbon emission are concentrated in a small number of industries with high water consumption and energy consumption, which is more conducive to the concentration and consistency of management objectives, thus promoting the synergy of CRWS63. Therefore, according to the difference of urban development level, management measures based on the regulatory effect of technology, structure and scale factors should be adopted to promote the synergistic effect of urban CRWS.Fig. 7Analysis of regulatory effect of CRWS in the YRDUA.Full size imageWe acknowledge that there are some limitations to the data used in the current research. For example, data on production water-saving for certain years are unavailable (the proportion of missing data does not exceed 5%). The interpolation method has been used to predict the missing data, which may lead to uncertainties in subsequent analyses. In addition, the research scale is only limited to small and medium-sized cities, and further refinement is needed, especially in the study of synergy effect of CRWS at the industry and enterprise levels in different regions, which needs to be further strengthened. This is of great significance for supplementing relevant policies to improve and balance the regional carbon–water relationship. Therefore, the above limitations can be addressed by improving research data at a more detailed level through field research and government consultation in the future.ConclusionsThis study designs an analytical framework to evaluate the synergistic and regulatory effects of urban CRWS, and applies it to the study of the YRDUA. The fixed effect analysis model is used to evaluate the synergistic effect of CRWS. The regulatory effects of technology, structure and scale factors on the synergy of CRWS are analyzed by adopting multiple parallel regulation model. Based on the heterogeneity of urban development level, the differences of synergistic and regulatory effects of CRWS are analyzed. The results indicate that the urban carbon emission intensity shows a downward trend, while the water resource intensive utilization intensity shows an upward trend in the YRDUA. Production water supply intensity has a positive impact on carbon emission intensity, production water-saving intensity and ecological water intensity have a negative impact on carbon emission intensity. Technical and structural factors negatively regulate the synergy of carbon emission intensity and production water supply intensity. Structural factors negatively regulate the synergy of carbon emission intensity and production water-saving intensity, and the synergy of carbon emission intensity and ecological water intensity. Compared with areas with lower urban development level, regulatory variables such as technology, structure and scale factors have more obvious impacts on the synergistic effect of CRWS in areas with higher urban development level. Therefore, the government should formulate targeted policies to achieve synergies of CRWS and promote sustainable economic development.

    Data availability

    The datasets used and/or analyzed during the current study are available from the corresponding author on reasonable request.
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    Download referencesFundingThis research was supported by the Natural Science Research of Jiangsu Higher Education Institutions of China (Grant No. 23KJB630003), the Huai’an City Science and Technology Project (Grant No. HAB202357), the National Natural Science Foundation Project of China (Grant No. 42001250), Scientific Research Initiation Fund of Huaiyin Normal University (Grant No. 31WQ001) .Author informationAuthors and AffiliationsSchool of Mathematics and Statistics, Huaiyin Normal University, No. 111 Changjiang West Road, Huaiyin District, Huaian, 223300, Jiangsu Province, ChinaQian Wang & Zuqin DingNanjing Water Group Co., Ltd, Nanjing, 210000, Jiangsu Province, ChinaShouqiang XuAuthorsQian WangView author publicationsSearch author on:PubMed Google ScholarShouqiang XuView author publicationsSearch author on:PubMed Google ScholarZuqin DingView author publicationsSearch author on:PubMed Google ScholarContributionsQian Wang: Conceptualization, Methodology, Formal analysis, Investigation, Software, Validation, Writing—original draft, Writing—review & editing, Supervision. Shouqiang Xu: Data curation, Resources, Investigation, Visualization. Zuqin Ding: Investigation, Visualization. All authors reviewed the manuscript.Corresponding authorCorrespondence to
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    Reprints and permissionsAbout this articleCite this articleWang, Q., Xu, S. & Ding, Z. Evaluation of synergistic and regulatory effects of carbon-reduction and water-saving in the Yangtze River Delta Urban Agglomeration.
    Sci Rep 15, 43998 (2025). https://doi.org/10.1038/s41598-025-27779-zDownload citationReceived: 27 June 2025Accepted: 05 November 2025Published: 17 December 2025Version of record: 17 December 2025DOI: https://doi.org/10.1038/s41598-025-27779-zShare this articleAnyone you share the following link with will be able to read this content:Get shareable linkSorry, a shareable link is not currently available for this article.Copy shareable link to clipboard
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    KeywordsSynergistic and regulatory effectsCarbon-water nexusCarbon emission intensityYangtze River Delta Urban AgglomerationCarbon-reduction and water-saving More

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    Reconstructing Late Quaternary coastal landscapes by a machine-learning framework

    AbstractCoastal landforms, particularly sea cliffs and associated wave-cut platforms, preserve key evidence of past sea-level fluctuations, tectonic activity, and paleoclimate variability. In this study, we implement a supervised machine learning approach, trained on an original, expert-labeled geomorphological dataset, to detect and classify inherited and active coastal features – such as paleo-sea cliffs and polycyclic sea cliffs – along the south-Tyrrhenian. Using DTM and morphometric indicators, our model, based on a RandomForestClassifier trained on expert-based cartography and independently validated, accurately identifies the spatial signatures of Quaternary coastal evolution. These results are cross validated against independent geomorphological mapping and sea-level reconstruction datasets. The integration of geomorphological classification with sea level markers enables us to reconstruct coastal morphogenesis in relation to the last interglacial cycle. Our findings highlight the potential of machine learning to automate the identification of coastal paleo-landscapes, providing insight into the imprint of climatic forcing on their morphology. This approach offers a scalable framework for investigating past climate–landscape interactions and for supporting future coastal hazard assessments under changing climate conditions.

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    Efficient and scalable training set generation for automated pollen monitoring with Hirst-type samplers

    AbstractAutomated pollen detection is essential for ecological monitoring, allergy forecasting, and biodiversity research. However, existing methods rely heavily on manual or semi-automated annotations, limiting scalability and broader applicability. We introduce a highly automated training dataset generation pipeline that combines one-shot detection with systematic refinement, producing tens of thousands of high-quality annotations from bright-field microscopy while significantly reducing manual effort and annotation costs. Using multi-regional datasets from France, Hungary, and Sweden, we trained object detection models on seven pollen taxa and evaluated their performance on both external pure and mixed species slides and real-world airborne samples. We assessed the reusability of pretrained vision models for pollen detection, aiming to reduce the need for extensive retraining. Using linear probing, we identified foundational Vision Transformers (ViTs) as the most effective feature extractors and integrated them into Faster R-CNN detection models. We benchmarked these models against ResNet50, a widely adopted backbone in biological imaging. On held-out regions of the training datasets, our models achieved high performance in both classification and detection tasks. On independent reference slides from other datasets, ViTs continued to outperform ResNet50 in classification. However, in full object detection and under real deployment conditions, ResNet50-based models remained competitive and achieved the highest accuracy for detecting Ambrosia, a major allergen with public health significance. Cross-dataset generalization remains a challenge, underscoring the need for domain adaptation techniques such as stain normalization and data augmentation. This study establishes a scalable framework for AI-assisted pollen monitoring, supporting large-scale slide digitization and enabling applications in long-term ecological research, allergen surveillance, and automated biodiversity assessment.

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    Data availability

    All datasets used in this study, including digitized slides and corresponding hand annotations are available upon request. For additional information or specific requests, please contact the corresponding author.
    Code availability

    The source code utilized in this study is available from our GitHub repository at https://github.com/abiricz/pollen-auto-annot-init-paper. This repository includes all scripts and comprehensive documentation required to replicate the experiments and evaluations described in this work.
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    Download referencesAcknowledgementsThis work was primarily supported by Information in Images Ltd. Special thanks to Michael Broderick, the director of the company, whose support was instrumental in restarting this research. We also acknowledge Zsolt Bedőházi for his contributions to the initial software development and preliminary prototyping. We are grateful to the teams at the National Public Health Center, the Swedish Museum of Natural History, and the Réseau National de Surveillance Aérobiologique in Lyon for their efforts in preparing the data and providing reference samples. A special acknowledgment is extended to János Fillinger and his team for providing access to their facility for scanning the samples. Their expertise in pathology brought a valuable external perspective beyond the field of pollen monitoring, further enriching this study. We thank Viktor Varga for his valuable input in the final refinement of the manuscript, including suggestions for minor corrections and additional evaluations that improved the clarity and completeness of the work. The authors thank the Wigner Scientific Computing Laboratory (WSCLAB) for providing computational resources that enabled large-scale evaluations and experiments for this publication. All code development was conducted independently prior to these computations, ensuring the integrity of proprietary research and potential industrial applications.FundingThis work was further supported by the National Research, Development, and Innovation Office of Hungary within the framework of the MILAB Artificial Intelligence National Laboratory (RRF-2.3.1-21-2022-00004) (I.C.) and the Data-Driven Health Division of National Laboratory for Health Security (RRF-2.3.1-21-2022-00006) (P.P.) and under grant No. 2020-1.1.2-PIACI-KFI-2021-00298 (A.B.). Finally, we sincerely thank Semmelweis University for generously covering the publication fee for this paper.Author informationAuthors and AffiliationsDepartment of Physics of Complex Systems, ELTE Eötvös Loránd University, Budapest, HungaryAndrás Biricz & István CsabaiNational Center for Public Health and Pharmacy, Budapest, HungaryDonát MagyarThe Palynological Laboratory at the Swedish Museum of Natural History, Stockholm, SwedenBjörn GeddaINRAE, UR 546 BioSP, Site Agroparc, Avignon, FranceAntonio SpanuNational Korányi Institute for Pulmonology, Budapest, HungaryJános FillingerDepartment of Pathology, Forensic and Insurance Medicine, Semmelweis University, Budapest, HungaryAdrián PestiData-Driven Health Division, National Laboratory for Health Security, Health Services Management Training Centre, Budapest, HungaryPéter PollnerDepartment of Biological Physics, ELTE Eötvös Loránd University, Budapest, HungaryPéter PollnerAuthorsAndrás BiriczView author publicationsSearch author on:PubMed Google ScholarDonát MagyarView author publicationsSearch author on:PubMed Google ScholarBjörn GeddaView author publicationsSearch author on:PubMed Google ScholarAntonio SpanuView author publicationsSearch author on:PubMed Google ScholarJános FillingerView author publicationsSearch author on:PubMed Google ScholarAdrián PestiView author publicationsSearch author on:PubMed Google ScholarIstván CsabaiView author publicationsSearch author on:PubMed Google ScholarPéter PollnerView author publicationsSearch author on:PubMed Google ScholarContributionsAll authors read and approved the final version of the manuscript. András Biricz: conceptualization, data curation, formal analysis, investigation, methodology, project administration, software, validation, writing – original draft Donát Magyar: resources, project administration, validation, writing – review & editing Björn Gedda: resources, project administration, validation, writing – review & editing Antonio Spanu: resources, validation, writing – review & editing János Fillinger: data curation, resources, project administration, validation Adrián Pesti: data curation, resources, validation István Csabai: conceptualization, funding acquisition, project administration, supervision, writing – review & editing Péter Pollner: conceptualization, funding acquisition, project administration, supervision, writing – review & editingCorresponding authorsCorrespondence to
    András Biricz or Péter Pollner.Ethics declarations

    Competing interests
    András Biricz reports contractual work with Information in Images Ltd., directed by Michael Broderick, which supported this study and is engaged in the commercial sale of microscopy devices. The company may potentially benefit from findings related to digital microscopy and dataset generation. All other authors declare no competing interests.

    Additional informationPublisher’s noteSpringer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.Supplementary InformationSupplementary Information.Rights and permissions
    Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.
    Reprints and permissionsAbout this articleCite this articleBiricz, A., Magyar, D., Gedda, B. et al. Efficient and scalable training set generation for automated pollen monitoring with Hirst-type samplers.
    Sci Rep (2025). https://doi.org/10.1038/s41598-025-31646-2Download citationReceived: 03 June 2025Accepted: 04 December 2025Published: 17 December 2025DOI: https://doi.org/10.1038/s41598-025-31646-2Share this articleAnyone you share the following link with will be able to read this content:Get shareable linkSorry, a shareable link is not currently available for this article.Copy shareable link to clipboard
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    KeywordsAirborne allergen analysisAutomated pollen detectionDeep learningHirst-type samplerOpen-vocabulary object detectionPollen monitoringVision Transformer More

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    Integrated assessment of greenhouse gas emissions in extensive livestock farming systems

    AbstractExtensive livestock farming has been described only in part, with previous studies focusing mainly on individual aspects such as the breeds reared, economic profitability, or environmental impact. However, the current scenario of increasing climate uncertainty highlights the need for a more comprehensive description of typologies of extensive production systems. In this study, 52 dehesa farms were analysed between 2021 and 2022 using technical, economic and environmental indicators. To determine their main characteristics, a Principal Component Analysis was conducted, followed by Cluster Analysis. Three factors were identified: (i) level of intensification and emissions, (ii) land tenure and labour and (iii) dependence on CAP subsidies. These factors explained 67.63% of total variance, and based on them, four farm types were classified. Results showed that less intensive farms had lower environmental impact (cluster 1, 2, 3: 991.99, 727.20 and 1049.87 kg CO2eq ha-1 year-1, respectively) and lower dependence on external inputs. More intensified farms (cluster 4: 2183.58 kg CO2eq ha-1 year-1), although emissions were higher, showed better economic performance. Cluster 3 represented the most sustainable model since farms combined good technical and economic performance while applying regenerative environmental management practices. This classification can support the development of tailored management strategies to guide extensive livestock systems towards improved sustainability and resilience.

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    Data availability

    The datasets generated during and/or analysed during the current study are available from the corresponding author on reasonable request. Corresponding author: [email protected].
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    Download referencesAcknowledgmentsThis paper has been jointly funded (85%) by the European Union, European Regional Development Fund and the Regional Government of Extremadura. Managing Authority: Ministry of Finance. Grant Ref. GR24147.FundingThe funding was provided by the Junta de Extremadura and FEDER Funds (Grant GR24147).Author informationAuthors and AffiliationsDepartment of Animal Production and Food Science, Faculty of Veterinary, University of Extremadura, Cáceres, SpainAndrés Horrillo & Miguel EscribanoDepartment of Animal Production and Food Science, School of Agricultural Engineering, University of Extremadura, Badajoz, SpainPaula Gaspar & Antonio Rodríguez-LedesmaAuthorsAndrés HorrilloView author publicationsSearch author on:PubMed Google ScholarPaula GasparView author publicationsSearch author on:PubMed Google ScholarAntonio Rodríguez-LedesmaView author publicationsSearch author on:PubMed Google ScholarMiguel EscribanoView author publicationsSearch author on:PubMed Google ScholarContributionsConceptualization, A.H., M.E., P.G. and A.R.L.; methodology, A.H. and M.E.; formal analysis, A.H. and M.E.; investigation, A.H., M.E., P.G. and A.R.L.; data curation, A.H. and M.E.; writing—original draft preparation, A.H., A.R.L. and M.E.; writing—review and editing, A.H., M.E., P.G. and A.R.L.; visualization, A.H. and M.E.; supervision, M.E. and P.G.; project administration, M.E. and P.G.; funding acquisition, M.E., A.R.L. and P.G. All authors have read and agreed to the published version of the manuscript.Corresponding authorCorrespondence to
    Andrés Horrillo.Ethics declarations

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    The authors declare no competing interests.

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    Reprints and permissionsAbout this articleCite this articleHorrillo, A., Gaspar, P., Rodríguez-Ledesma, A. et al. Integrated assessment of greenhouse gas emissions in extensive livestock farming systems.
    Sci Rep (2025). https://doi.org/10.1038/s41598-025-32814-0Download citationReceived: 24 July 2025Accepted: 12 December 2025Published: 17 December 2025DOI: https://doi.org/10.1038/s41598-025-32814-0Share this articleAnyone you share the following link with will be able to read this content:Get shareable linkSorry, a shareable link is not currently available for this article.Copy shareable link to clipboard
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    KeywordsExtensive farmsDehesaClimate changeClusterCarbon footprintRegenerative management practices More