More stories

  • in

    Tracking late Pleistocene Neandertals on the Iberian coast

    1.
    Bennett, M. R. & Morse, S. A. Human Footprints: Fossilised Locomotion? (Springer International Publishing, Berlin, 2014).
    Google Scholar 
    2.
    Leakey, M. D. & Hay, R. L. Pliocene footprints in the Laetolil Beds at Laetoli, northern Tanzania. Nature 278, 317–323 (1979).
    ADS  Article  Google Scholar 

    3.
    Mietto, P., Avanzini, M. & Rolandi, G. Palaeontology: Human footprints in Pleistocene volcanic ash. Nature 422, 133 (2003).
    ADS  CAS  PubMed  Article  PubMed Central  Google Scholar 

    4.
    Ashton, N. et al. Hominin footprints from early Pleistocene deposits at Happisburgh, UK. PLoS ONE 9, e88329 (2014).
    ADS  PubMed  PubMed Central  Article  CAS  Google Scholar 

    5.
    Duveau, J. et al. The composition of a Neandertal social group revealed by the hominin footprints at Le Rozel (Normandy, France). PNAS 116, 19409–19414 (2019).
    CAS  PubMed  Article  PubMed Central  Google Scholar 

    6.
    Masao, F. T. et al. New footprints from Laetoli (Tanzania) provide evidence for marked body size variation in early hominins. eLife 5, e19568 (2016).
    PubMed  PubMed Central  Article  Google Scholar 

    7.
    Altamura, F. et al. Archaeology and ichnology at Gombore II-2, Melka Kunture, Ethiopia: Everyday life of a mixed-age hominin group 700,000 years ago. Sci. Rep. 8, 2815 (2018).
    ADS  PubMed  PubMed Central  Article  CAS  Google Scholar 

    8.
    Bustos, D. et al. Footprints preserve terminal Pleistocene hunt? Human-sloth interactions in North America. Sci. Adv. 4, eaar7621 (2018).
    ADS  PubMed  PubMed Central  Article  Google Scholar 

    9.
    Stewart, M. et al. Human footprints provide snapshot of last interglacial ecology in the Arabian interior. Sci. Adv. 6, eaba8940 (2020).
    ADS  CAS  PubMed  PubMed Central  Article  Google Scholar 

    10.
    Barton, C. M. Stone tools and paleolithic settlement in the Iberian Peninsula. Proc. Prehist. Soc. 56, 15–32 (1990).
    Article  Google Scholar 

    11.
    Garralda, M. D. The Neandertals from the Iberian Peninsula. MUNIBE 57, 289–314 (2005).
    Google Scholar 

    12.
    Ruiz, M. N. et al. Last Neandertal occupations at Central Iberia: The lithic industry of Jarama VI rock shelter (Valdesotos, Guadalajara, Spain). Archaeol. Anthropol. Sci. 12, 45 (2020).
    Article  Google Scholar 

    13.
    Muñiz, F. et al. Following the last Neandertals: Mammal tracks in Late Pleistocene coastal dunes of Gibraltar (S Iberian Peninsula). Quat. Sci. Rev. 217, 297–309 (2019).
    ADS  Article  Google Scholar 

    14.
    Neto de Carvalho, C. et al. First vertebrate tracks and palaeoenvironment in a MIS-5 context in the Doñana National Park (Huelva, SW Spain). Quat. Sci. Rev. 243, 106508 (2020).
    Article  Google Scholar 

    15.
    Neto de Carvalho, C. et al. Paleoecological implications of large-sized wild boar tracks recorded during the last interglacial (Mis 5) at Huelva (Sw Spain). Palaios 35, 512–523 (2020).
    ADS  Article  Google Scholar 

    16.
    Rodríguez-Ramírez, A. et al. The role of neo-tectonics in the sedimentary infilling and geomorphological evolution of the Guadalquivir estuary (Gulf of Cadiz, SW Spain) during the Holocene. Geomorphology 219, 126–140 (2014).
    ADS  Article  Google Scholar 

    17.
    Rodríguez-Rámirez, A. Geomorfología del Parque Nacional de Doñana y su Entorno. (ed Organismo Autónomo Parques Nacionales) (Ministerio de Medio Ambiente, Madrid, 1998).

    18.
    Pérez Muñoz, A. B. et al. Parque Nacional de Doñana. Guía Geológica. (ed Rodríguez Fernández, R.) (Instituto Geológico y Minero de España & Organismo Autónomo Parques Nacionales, Madrid, 2020).

    19.
    Instituto Hidrográfico de la Marina. Derrotero N° 2-Tomo 2 (Costas de Portugal y SO de España, Cádiz, 1992).
    Google Scholar 

    20.
    Rodríguez-Ramírez, A. et al. Analysis of the recent storm record in the southwestern spanish coast: Implications for littoral management. Sci. Total Environ. 303, 189–201 (2003).
    ADS  PubMed  Article  CAS  PubMed Central  Google Scholar 

    21.
    Gibbard, P. L., Head, M. J., Walker, M. J. C. & The Subcommission on Quaternary Stratigraphy. Formal ratification of the Quaternary System/Period and the Pleistocene Series/Epoch with a base at 2.58 Ma. J. Quat. Sci. 25, 96–102 (2010).
    Article  Google Scholar 

    22.
    Zazo, C. et al. Landscape evolution and geodynamic controls in the Gulf of Cadiz (Huelva coast, SW Spain) during the Late Quaternary. Geomorphology 68, 269–290 (2005).
    ADS  Article  Google Scholar 

    23.
    Duveau, J. Les empreintes de pieds du Rozel (Manche). Instantanés de groupes humains au Pléistocène supérieur. Approche combinée morphométrique et expérimentale. (Ph. D. dissertation. Muséum national d’Histoire naturelle, Paris, 2020).

    24.
    Manolis, S., Aiello, L., Henessy, R., Kyparissi-Apostolika, N. Middle Palaeolithic Footprints from Theopetra Cave (Thessaly, Greece) (ed Kyparissi-Apostolika, N.) 87–93 (Greek Ministry of Culture and Institute for Aegean Prehistory, Athens, 2000).

    25.
    Onac, B. P. et al. U-Th ages constraining the Neanderthal footprint at Vârtop Cave, Romania. Quat. Sci. Rev. 24, 1151–1157 (2005).
    ADS  Article  Google Scholar 

    26.
    Duveau, J., Berillon, G., Verna, C. 11-On the tracks of Neandertals: The ichnological assemblage from Le Rozel (Normandy, France). (eds Pastoors, A. & Lenssen-Erz, T.) (Springer Nature, in Press).

    27.
    Citton, P., Romano, M., Salvador, I. & Avanzini, M. Reviewing the upper Pleistocene human footprints from the ‘Sala dei Misteri’in the Grotta della Basura (Toirano, northern Italy) cave: An integrated morphometric and morpho-classificatory approach. Quat. Sci. Rev. 169, 50–64 (2017).
    ADS  Article  Google Scholar 

    28.
    Helm, C. W. et al. A New Pleistocene Hominin Tracksite from the Cape South Coast, South Africa. Sci. Rep. 8, 3772 (2018).
    ADS  PubMed  PubMed Central  Article  CAS  Google Scholar 

    29.
    Dingwall, H. L., Hatala, K. G., Wunderlich, R. E. & Richmond, B. G. Hominin stature, body mass, and walking speed estimates based on 1.5 million-year-old fossil footprints at Ileret, Kenya. J. Hum. Evol. 64, 556–568 (2013).
    PubMed  Article  PubMed Central  Google Scholar 

    30.
    Krishan, K. Estimation of stature from footprint and foot outline dimensions in Gujjars of North India. Forensic Sci. Int. 175, 93–101 (2008).
    PubMed  Article  PubMed Central  Google Scholar 

    31.
    Fawzy, I. A. & Kamal, N. N. Stature and body weight estimation from various footprint measurements among Egyptian population. J. Forensic Sci. 55, 884–888 (2010).
    PubMed  Article  PubMed Central  Google Scholar 

    32.
    Reel, S., Rouse, S., Obe, W. V. & Doherty, P. Estimation of stature from static and dynamic footprints. Forensic Sci. Int. 219, 283-e1 (2012).
    PubMed  Article  PubMed Central  Google Scholar 

    33.
    Hemy, N., Flavel, A., Ishak, N. I. & Franklin, D. Sex estimation using anthropometry of feet and footprints in a Western Australian population. Forensic Sci. Int. 231, 402-e1 (2013).
    PubMed  Article  PubMed Central  Google Scholar 

    34.
    Aiello, L. & Dean, C. An Introduction to Human Evolutionary Anatomy (Academic Press Inc., London, 1990).
    Google Scholar 

    35.
    Klenerman, L. & Wood, B. The Human Foot: A Companion to Clinical Studies (Springer, London, 2006).
    Google Scholar 

    36.
    Elftman, H. & Manter, J. Chimpanzee and human feet in bipedal walking. Am. J. Phys. Anthropol. 20, 69–79 (1935).
    Article  Google Scholar 

    37.
    Alexander, R. M. Principles of Animal Locomotion (Princeton University Press, Princeton, 2003).
    Google Scholar 

    38.
    Ruff, C. B., Trinkaus, E. & Holliday, T. W. Body mass and encephalization in Pleistocene Homo. Nature 387, 173 (1997).
    ADS  CAS  PubMed  Article  PubMed Central  Google Scholar 

    39.
    Carretero, J. M. et al. Stature estimation from complete long bones in the Middle Pleistocene humans from the Sima de los Huesos, Sierra de Atapuerca (Spain). J. Hum. Evol. 62, 242–255 (2012).
    PubMed  Article  PubMed Central  Google Scholar 

    40.
    Benazzi, S. et al. Early dispersal of modern humans in Europe and implications for Neandertal behaviour. Nature 479, 525–528 (2011).
    ADS  CAS  PubMed  Article  PubMed Central  Google Scholar 

    41.
    Hublin, J. J. The modern human colonization of western Eurasia: When and where?. Quat. Sci. Rev. 118, 194–210 (2015).
    ADS  Article  Google Scholar 

    42.
    Karavanić, I. et al. Paleolithic hominins and settlement in Croatia from MIS 6 to MIS 3: Research history and current interpretations. Quat. Int. 494, 152–166 (2018).
    Article  Google Scholar 

    43.
    Vallespi, E., Alvarez, G., Perez Sindreu, F. & Rufete, P. Nuevas atribuciones onubenses al Paleolitico Inferior y Medio. Huelva en su Historia I, 43–56 (1986).

    44.
    Viehmann, I. Prehistoric Human Footprints in Romania’s Caves. Theor. Appl. Karstol. 3, 229–234 (1987).
    Google Scholar 

    45.
    Harvati, K. The human fossil record from Romania: Early Upper Paleolithic European Mandibles and Neanderthal. (eds Harvati, K. & Roksandic, M.) 51–68 (Springer Netherlands, 2016).

    46.
    Zazo, C. et al. Pleistocene and Holocene Aeolian facies along the Huelva coast (southern Spain): Climatic and neotectonic implications. Geol. Mijn. 77, 209–224 (1999).
    Article  Google Scholar 

    47.
    Zazo, C. et al. El complejo eólico de El Abalario (Huelva) (eds Sanjaume, E., Gracia, F. J.) 407–425 (Sociedad Española de Geomorfología, Madrid, 2011)

    48.
    Paerl, H. W. & Yanarell, A. C. Environmental dynamics, community structure and function in a hypersaline microbial mat (eds Seckbach, J. & Oren, A.) 421–442, (Springer Netherlands, 2010).

    49.
    Porada, H. & Bouougri, E. Wrinkle structures—a critical review (eds Schieber, J. et al.) 135–144 (Elsevier, 2007).

    50.
    Gerdes, G. What Are Microbial Mats? (eds Seckbach, J. & Oren, A.) 3–25, (Springer Netherlands, 2010).

    51.
    Eriksson, P. G. et al. Paleoenvironmental Context Of Microbial Mat-Related Structures In Siliciclastic Rocks. (eds Seckbach, J. & Oren, A.) 71–108 (Springer Netherlands, 2010).

    52.
    Zilhão, J. et al. Last Interglacial Iberian Neandertals as fisher-hunter-gatherers. Science 367, 1443 (2020).
    ADS  Article  CAS  Google Scholar 

    53.
    Hardy, B. L. & Moncel, M.-H. Neanderthal use of fish, mammals, birds, starchy plants and wood 125–250,000 years ago. PLoS ONE 6, e23768 (2011).
    ADS  CAS  PubMed  PubMed Central  Article  Google Scholar 

    54.
    Wall-Scheffler, C. M., Wagnild, J. & Wagler, E. Human footprint variation while performing load bearing tasks. PLoS ONE 10, e0118619 (2015).
    PubMed  PubMed Central  Article  CAS  Google Scholar 

    55.
    Romagnoli, F., Martini, F. & Sarti, L. Neanderthal use of Callista chione shells as raw material for retouched tools in South-East Italy: Analysis of Grotta del Cavallo layer l assemblage with a new methodology. J. Archaeol. Method Theory 22, 1007–1037 (2015).
    Article  Google Scholar 

    56.
    Benito, B. M. et al. The ecological niche and distribution of Neanderthals during the Last Interglacial. J. Biogeogr. 44, 51–61 (2017).
    Article  Google Scholar 

    57.
    Villa, P. et al. Neandertals on the beach: Use of marine resources at Grotta dei Moscerini (Latium, Italy). PLoS ONE 15, e0226690 (2020).
    CAS  PubMed  PubMed Central  Article  Google Scholar 

    58.
    Cortés-Sánchez, M. et al. Shellfish collection on the westernmost Mediterranean, Bajondillo cave (~ 160–35 cal kyr BP): A case of behavioral convergence?. Quat. Sci. Rev. 217, 284–196 (2019).
    ADS  Article  Google Scholar 

    59.
    Stringer, C. B. et al. Neandertal exploitation of marine mammals in Gibraltar. PNAS 105, 14319–14324 (2008).
    ADS  CAS  PubMed  Article  PubMed Central  Google Scholar  More

  • in

    Eco-evolutionary interaction between microbiome presence and rapid biofilm evolution determines plant host fitness

    1.
    Slobodkin, L. B. Growth and regulation of animal populations (Holt, Rinehart and Winston, 1961).
    2.
    Thompson, J. N. Rapid evolution as an ecological process. Trends Ecol. Evol. 13, 329–332 (1998).
    CAS  PubMed  Article  Google Scholar 

    3.
    Hendry, A. P. A critique for eco-evolutionary dynamics. Funct. Ecol. 33, 84–94 (2019).
    Article  Google Scholar 

    4.
    Turcotte, M. M., Reznick, D. N. & Hare, J. D. The impact of rapid evolution on population dynamics in the wild: experimental test of eco-evolutionary dynamics. Ecol. Lett. 14, 1084–1092 (2011).
    PubMed  Article  Google Scholar 

    5.
    Hairston, N. G. Jr, Ellner, S. P., Geber, M. A., Yoshida, T. & Fox, J. A. Rapid evolution and the convergence of ecological and evolutionary time. Ecol. Lett. 8, 1114–1127 (2005).
    Article  Google Scholar 

    6.
    Tan, J., Rattray, J. B., Yang, X. & Jiang, L. Spatial storage effect promotes biodiversity during adaptive radiation. Proc. R. Soc. Lond. B 284, 20170841 (2017).
    Google Scholar 

    7.
    Hart, S. P., Turcotte, M. M. & Levine, J. M. Effects of rapid evolution on species coexistence. Proc. Natl Acad. Sci. USA 116, 2112–2117 (2019).
    CAS  PubMed  Article  Google Scholar 

    8.
    Faillace, C. A. & Morin, P. J. Evolution alters the consequences of invasions in experimental communities. Nat. Ecol. Evol. 1, 0013 (2017).
    Article  Google Scholar 

    9.
    Vanbergen, A. J., Espíndola, A. & Aizen, M. A. Risks to pollinators and pollination from invasive alien species. Nat. Ecol. Evol. 2, 16–25 (2018).
    PubMed  Article  Google Scholar 

    10.
    Hendry, A. P. Eco-evolutionary dynamics (Princeton Univ. Press, 2016).

    11.
    Garud, N. R., Good, B. H., Hallatschek, O. & Pollard, K. S. Evolutionary dynamics of bacteria in the gut microbiome within and across hosts. PLoS Biol. 17, e3000102 (2019).
    PubMed  PubMed Central  Article  Google Scholar 

    12.
    Zhao, S. et al. Adaptive evolution within gut microbiomes of healthy people. Cell Host Microbe 25, 656–667 (2019).
    CAS  PubMed  PubMed Central  Article  Google Scholar 

    13.
    terHorst, C. P. & Zee, P. C. Eco-evolutionary dynamics in plant–soil feedbacks. Funct. Ecol. 30, 1062–1072 (2016).
    Article  Google Scholar 

    14.
    Soto, M. J., Domínguez‐Ferreras, A., Pérez‐Mendoza, D., Sanjuán, J. & Olivares, J. Mutualism versus pathogenesis: the give‐and‐take in plant–bacteria interactions. Cell. Microbiol. 11, 381–388 (2009).
    CAS  PubMed  Article  Google Scholar 

    15.
    Marchetti, M. et al. Experimental evolution of a plant pathogen into a legume symbiont. PLoS Biol. 8, e1000280 (2010).
    PubMed  PubMed Central  Article  CAS  Google Scholar 

    16.
    Saikkonen, K., Wäli, P., Helander, M. & Faeth, S. H. Evolution of endophyte–plant symbioses. Trends Plant Sci. 9, 275–280 (2004).
    CAS  PubMed  Article  Google Scholar 

    17.
    Reese, A. T. & Dunn, R. R. Drivers of microbiome biodiversity: a review of general rules, feces, and ignorance. mBio 9, e01294-18 (2018).
    PubMed  PubMed Central  Article  Google Scholar 

    18.
    Miller, E. T., Svanbäck, R. & Bohannan, B. J. Microbiomes as metacommunities: understanding host-associated microbes through metacommunity ecology. Trends Ecol. Evol. 33, 926–935 (2018).
    PubMed  Article  Google Scholar 

    19.
    Griffin, E. A. et al. Plant host identity and soil macronutrients explain little variation in sapling endophyte community composition: is disturbance an alternative explanation? J. Ecol. 107, 1876–1889 (2019).
    CAS  Article  Google Scholar 

    20.
    Acosta, K. et al. Duckweed hosts a taxonomically similar bacterial assemblage as the terrestrial leaf microbiome. PLoS ONE 15, e0228560 (2020).
    CAS  PubMed  PubMed Central  Article  Google Scholar 

    21.
    Sandler, G., Bartkowska, M., Agrawal, A. F. & Wright, S. I. Estimation of the SNP mutation rate in two vegetatively propagating species of duckweed. G3 10, 4191–4200 (2020).
    PubMed  Article  Google Scholar 

    22.
    Ishizawa, H., Kuroda, M., Morikawa, M. & Ike, M. Evaluation of environmental bacterial communities as a factor affecting the growth of duckweed Lemna minor. Biotechnol. Biofuels 10, 62 (2017).
    PubMed  PubMed Central  Article  CAS  Google Scholar 

    23.
    Zhang, Y. et al. Duckweed (Lemna minor) as a model plant system for the study of human microbial pathogenesis. PLoS ONE 5, e13527 (2010).
    PubMed  PubMed Central  Article  CAS  Google Scholar 

    24.
    Rainey, P. B. & Travisano, M. Adaptive radiation in a heterogeneous environment. Nature 394, 69–72 (1998).
    CAS  PubMed  PubMed Central  Article  Google Scholar 

    25.
    Tan, J., Yang, X., He, Q., Hua, X. & Jiang, L. Earlier parasite arrival reduces the repeatability of host adaptive radiation. ISME J. 14, 2358–2360 (2020).
    PubMed  PubMed Central  Article  Google Scholar 

    26.
    Tan, J., Yang, X. & Jiang, L. Species ecological similarity modulates the importance of colonization history for adaptive radiation. Evolution 71, 1719–1727 (2017).
    PubMed  Article  Google Scholar 

    27.
    Meyer, J. R., Schoustra, S. E., Lachapelle, J. & Kassen, R. Overshooting dynamics in a model adaptive radiation. Proc. R. Soc. Lond. B 278, 392–398 (2011).
    Google Scholar 

    28.
    Tan, J., Kelly, C. K. & Jiang, L. Temporal niche promotes biodiversity during adaptive radiation. Nat. Commun. 4, 2102 (2013).
    PubMed  Article  CAS  Google Scholar 

    29.
    Spiers, A. J., Buckling, A. & Rainey, P. B. The causes of Pseudomonas diversity. Microbiology 146, 2345–2350 (2000).
    CAS  PubMed  Article  Google Scholar 

    30.
    Spiers, A. J., Bohannon, J., Gehrig, S. M. & Rainey, P. B. Biofilm formation at the air–liquid interface by the Pseudomonas fluorescens SBW25 wrinkly spreader requires an acetylated form of cellulose. Mol. Microbiol. 50, 15–27 (2003).
    CAS  PubMed  Article  Google Scholar 

    31.
    Bantinaki, E. et al. Adaptive divergence in experimental populations of Pseudomonas fluorescens. III. Mutational origins of wrinkly spreader diversity. Genetics 176, 441–453 (2007).
    CAS  PubMed  PubMed Central  Article  Google Scholar 

    32.
    McDonald, M. J., Gehrig, S. M., Meintjes, P. L., Zhang, X.-X. & Rainey, P. B. Adaptive divergence in experimental populations of Pseudomonas fluorescens. IV. Genetic constraints guide evolutionary trajectories in a parallel adaptive radiation. GENETICS 183, 1041–1053 (2009).
    CAS  PubMed  PubMed Central  Article  Google Scholar 

    33.
    Bailey, S. F., Dettman, J. R., Rainey, P. B. & Kassen, R. Competition both drives and impedes diversification in a model adaptive radiation. Proc. R. Soc. Lond. B 280, 20131253 (2013).
    Google Scholar 

    34.
    Hansen, S. K., Rainey, P. B., Haagensen, J. A. & Molin, S. Evolution of species interactions in a biofilm community. Nature 445, 533–536 (2007).
    CAS  PubMed  Article  Google Scholar 

    35.
    Flemming, H.-C. et al. Biofilms: an emergent form of bacterial life. Nat. Rev. Microbiol. 14, 563–575 (2016).
    CAS  PubMed  Article  Google Scholar 

    36.
    Ahmad, F., Ahmad, I. & Khan, M. S. Screening of free-living rhizospheric bacteria for their multiple plant growth promoting activities. Microbiol. Res. 163, 173–181 (2008).
    CAS  PubMed  Article  Google Scholar 

    37.
    El-Sayed, W. S., Akhkha, A., El-Naggar, M. Y. & Elbadry, M. In vitro antagonistic activity, plant growth promoting traits and phylogenetic affiliation of rhizobacteria associated with wild plants grown in arid soil. Front. Microbiol. 5, 651 (2014).
    PubMed  PubMed Central  Article  Google Scholar 

    38.
    Gómez, P. & Buckling, A. Real-time microbial adaptive diversification in soil. Ecol. Lett. 16, 650–655 (2013).
    PubMed  Article  Google Scholar 

    39.
    Spor, A., Koren, O. & Ley, R. Unravelling the effects of the environment and host genotype on the gut microbiome. Nat. Rev. Microbiol. 9, 279–290 (2011).
    CAS  PubMed  Article  Google Scholar 

    40.
    Walters, W. A. et al. Large-scale replicated field study of maize rhizosphere identifies heritable microbes. Proc. Natl Acad. Sci. USA 115, 7368–7373 (2018).
    PubMed  PubMed Central  Article  Google Scholar 

    41.
    Veach, A. M. et al. Rhizosphere microbiomes diverge among Populus trichocarpa plant-host genotypes and chemotypes, but it depends on soil origin. Microbiome 7, 76 (2019).
    PubMed  PubMed Central  Article  Google Scholar 

    42.
    Lennon, J. T. & Martiny, J. B. Rapid evolution buffers ecosystem impacts of viruses in a microbial food web. Ecol. Lett. 11, 1178–1188 (2008).
    PubMed  Article  Google Scholar 

    43.
    Pantel, J. H., Duvivier, C. & Meester, L. D. Rapid local adaptation mediates zooplankton community assembly in experimental mesocosms. Ecol. Lett. 18, 992–1000 (2015).
    PubMed  Article  Google Scholar 

    44.
    Faillace, C. A. & Morin, P. J. Evolution alters post-invasion temporal dynamics in experimental communities. J. Anim. Ecol. 89, 285–298 (2020).
    PubMed  Article  Google Scholar 

    45.
    Omilian, A. R., Cristescu, M. E. A., Dudycha, J. L. & Lynch, M. Ameiotic recombination in asexual lineages of Daphnia. Proc. Natl Acad. Sci. USA 103, 18638–18643 (2006).
    CAS  PubMed  Article  Google Scholar 

    46.
    Mao, Y., Botella, J. R., Liu, Y. & Zhu, J.-K. Gene editing in plants: progress and challenges. Natl Sci. Rev. 6, 421–437 (2019).
    CAS  Article  Google Scholar 

    47.
    Horvath, P. & Barrangou, R. CRISPR/Cas, the immune system of Bacteria and Archaea. Science 327, 167–170 (2010).
    CAS  PubMed  Article  Google Scholar 

    48.
    Yang, L. et al. Promotion of plant growth and in situ degradation of phenol by an engineered Pseudomonas fluorescens strain in different contaminated environments. Soil Biol. Biochem. 43, 915–922 (2011).
    CAS  Article  Google Scholar 

    49.
    Zabłocka-Godlewska, E., Przystaś, W. & Grabińska-Sota, E. Decolourization of diazo Evans blue by two strains of Pseudomonas fluorescens isolated from different wastewater treatment plants. Water Air Soil Pollut. 223, 5259–5266 (2012).
    PubMed  PubMed Central  Article  CAS  Google Scholar 

    50.
    Paulsen, I. T. et al. Complete genome sequence of the plant commensal Pseudomonas fluorescens Pf-5. Nat. Biotechnol. 23, 873–878 (2005).
    CAS  PubMed  PubMed Central  Article  Google Scholar 

    51.
    Rainey, P. B. Adaptation of Pseudomonas fluorescens to the plant rhizosphere. Environ. Microbiol. 1, 243–257 (1999).
    CAS  PubMed  Article  Google Scholar 

    52.
    Gilbert, S. et al. Bacterial production of indole related compounds reveals their role in association between duckweeds and endophytes. Front. Chem. 6, 265 (2018).
    PubMed  PubMed Central  Article  CAS  Google Scholar 

    53.
    Bailey, M. J., Lilley, A. K., Thompson, I. P., Rainey, P. B. & Ellis, R. J. Site directed chromosomal marking of a fluorescent pseudomonad isolated from the phytosphere of sugar beet; stability and potential for marker gene transfer. Mol. Ecol. 4, 755–764 (1995).
    CAS  PubMed  Article  Google Scholar 

    54.
    Spiers, A. J. & Rainey, P. B. The Pseudomonas fluorescens SBW25 wrinkly spreader biofilm requires attachment factor, cellulose fibre and LPS interactions to maintain strength and integrity. Microbiology 151, 2829–2839 (2005).
    CAS  PubMed  Article  Google Scholar 

    55.
    Lind, P. A., Libby, E., Herzog, J. & Rainey, P. B. Predicting mutational routes to new adaptive phenotypes. eLife 8, e38822 (2019).
    PubMed  PubMed Central  Article  Google Scholar 

    56.
    O’Brien, P. A., Webster, N. S., Miller, D. J. & Bourne, D. G. Host–microbe coevolution: applying evidence from model systems to complex marine invertebrate holobionts. mBio 10, e02241-18 (2019).
    PubMed  PubMed Central  Article  Google Scholar 

    57.
    Theis, K. R. et al. Getting the hologenome concept right: an eco-evolutionary framework for hosts and their microbiomes. mSystems 1, e00028-16 (2016).
    PubMed  PubMed Central  Article  Google Scholar 

    58.
    Landolt, E. Biosystematic Investigations in the Family of Duckweeds (Lemnaceae), Volume 2. The Family of Lemnaceae, A Monographic Study, Volume 1 (Geobotanical Institute, ETH Zurich, 1986).

    59.
    Ziegler, P., Sree, K. S. & Appenroth, K.-J. Duckweeds for water remediation and toxicity testing. Toxicol. Environ. Chem. 98, 1127–1154 (2016).
    CAS  Article  Google Scholar  More

  • in

    Urbanization can benefit agricultural production with large-scale farming in China

    1.
    Gu, B., Zhang, X., Bai, X., Fu, B. & Chen, D. Four steps to food security for swelling cities. Nature 566, 31–33 (2019).
    ADS  CAS  Article  Google Scholar 
    2.
    Godfray, H. C. et al. Food security: the challenge of feeding 9 billion people. Science 327, 812–818 (2010).
    ADS  CAS  Article  Google Scholar 

    3.
    Bren D Amour, C. et al. Future urban land expansion and implications for global croplands. Proc. Natl Acad. Sci. USA 114, 8939–8944 (2017).
    Article  Google Scholar 

    4.
    Gardi, C., Panagos, P., Van Liedekerke, M., Bosco, C. & De Brogniez, D. Land take and food security: assessment of land take on the agricultural production in Europe. J. Environ Plann. Manag. 58, 898–912 (2015).
    Article  Google Scholar 

    5.
    Shi, K. et al. Urban expansion and agricultural land loss in China: a multiscale perspective. Sustainability 8, 790 (2016).
    Article  Google Scholar 

    6.
    Bai, X., Shi, P. & Liu, Y. Society: realizing China’s urban dream. Nature 509, 158–160 (2014).
    Article  Google Scholar 

    7.
    World Urbanization Prospects 2018 (United Nations, 2018); https://population.un.org/wup/Download/

    8.
    Zhai, Z., Chen, J. & Li, L. Future trends of China’s population and aging from 2015 to 2100 [in Chinese]. Popul. Res. 41, 60–71 (2017).
    Google Scholar 

    9.
    Van Vliet, J., Eitelberg, D. A. & Verburg, P. H. A global analysis of land take in cropland areas and production displacement from urbanization. Glob. Environ. Change 43, 107–115 (2017).
    Article  Google Scholar 

    10.
    Chen, J. Rapid urbanization in China: a real challenge to soil protection and food security. Catena 69, 1–15 (2007).
    Article  Google Scholar 

    11.
    Martellozzo, F. et al. Urbanization and the loss of prime farmland: a case study in the Calgary–Edmonton corridor of Alberta. Reg. Environ. Change 15, 881–893 (2015).
    Article  Google Scholar 

    12.
    Yan, H., Liu, J., He, Q. H., Bo, T. & Cao, M. Assessing the consequence of land use change on agricultural productivity in China. Glob. Planet. Change 67, 13–19 (2009).
    ADS  Article  Google Scholar 

    13.
    Bai, X., Chen, J. & Shi, P. Landscape urbanization and economic growth in China: positive feedbacks and sustainability dilemmas. Environ. Sci. Technol. 46, 132–139 (2012).
    ADS  CAS  Article  Google Scholar 

    14.
    Statistical yearbooks of prefecture-level cities in 2015 [in Chinese]. National Bureau of Statistics http://www.stats.gov.cn/tjsj/ (2016).

    15.
    Zuo, L. et al. Progress towards sustainable intensification in China challenged by land-use change. Nat. Sustain. 1, 304–313 (2018).
    Article  Google Scholar 

    16.
    Lal, R. Soil carbon sequestration impacts on global climate change and food security. Science 304, 1623–1627 (2004).
    ADS  CAS  Article  Google Scholar 

    17.
    Zhang, X. et al. Effects of enhancing soil organic carbon sequestration in the topsoil by fertilization on crop productivity and stability: evidence from long-term experiments with wheat–maize cropping systems in China. Sci. Total Environ. 562, 247–259 (2016).
    ADS  CAS  Article  Google Scholar 

    18.
    Wu, Y. et al. Policy distortions, farm size, and the overuse of agricultural chemicals in China. Proc. Natl Acad. Sci. USA 115, 7010–7015 (2018).
    ADS  CAS  Article  Google Scholar 

    19.
    Zou, B., Mishra, A. K. & Luo, B. Aging population, farm succession, and farmland usage: evidence from rural China. Land Use Policy 77, 437–445 (2018).
    Article  Google Scholar 

    20.
    Guidance on Accelerating the Development of Agricultural Productive Services (Ministry of Agriculture and Rural Affairs of the People’s Republic of China, 2017).

    21.
    Ju, X., Gu, B., Wu, Y. & Galloway, J. N. Reducing China’s fertilizer use by increasing farm size. Glob. Environ. Change 41, 26–32 (2016).
    Article  Google Scholar 

    22.
    Ren, C. et al. The impact of farm size on agricultural sustainability. J. Clean Prod. 220, 357–367 (2019).
    Article  Google Scholar 

    23.
    Adamopoulos, T. & Restuccia, D. The size distribution of farms and international productivity differences. Am. Econ. Rev. 104, 1667–1697 (2014).
    Article  Google Scholar 

    24.
    Wang, J., Chen, K. Z., Gupta, S. D. & Huang, Z. Is small still beautiful? A comparative study of rice farm size and productivity in China and India. China Agr. Econ. Rev. 7, 484–509 (2015).
    Article  Google Scholar 

    25.
    Lu, H., Xie, H., He, Y., Wu, Z. & Zhang, X. Assessing the impacts of land fragmentation and plot size on yields and costs: a translog production model and cost function approach. Agr. Syst. 161, 81–88 (2018).
    Article  Google Scholar 

    26.
    Syp, A., Faber, A., Borzecka-Walker, M. & Osuch, D. Assessment of greenhouse gas emissions in winter wheat farms using data envelopment analysis approach. Pol. J. Environ. Stud. 24, 2197–2203 (2015).
    CAS  Article  Google Scholar 

    27.
    Li, G., Feng, Z., You, L. & Fan, L. Re-examining the inverse relationship between farm size and efficiency. China Agr. Econ. Rev. 5, 473–488 (2013).
    Article  Google Scholar 

    28.
    Fan, L. et al. Decreasing farm number benefits the mitigation of agricultural non-point source pollution in China. Environ. Sci. Pollut. Res. 26, 464–472 (2019).
    Article  Google Scholar 

    29.
    Cassman, K. G., Dobermann, A., Walters, D. T. & Yang, H. Meeting cereal demand while protecting natural resources and improving environmental quality. Annu. Rev. Env. Resour. 28, 315–358 (2003).
    Article  Google Scholar 

    30.
    Pellegrini, P. & Fernández, R. J. Crop intensification, land use, and on-farm energy-use efficiency during the worldwide spread of the green revolution. Proc. Natl Acad. Sci. USA 115, 2335–2340 (2018).
    CAS  Article  Google Scholar 

    31.
    Resource and Environment Data Cloud Platform (Resource and Environment Science and Data Center, 2018); http://www.resdc.cn/Default.aspx

    32.
    Laborde, D., Martin, W., Swinnen, J. & Vos, R. COVID-19 risks to global food security. Science 369, 500–502 (2020).
    ADS  CAS  Article  Google Scholar 

    33.
    Shi, Q., Jin, H. & Zhuo, J. Does land expropriation definitely reduce farmers’ income: a survey of 7 villages in Shanghai: the defects and reforms of the current land expropriation system [in Chinese]. Manage. World 3, 77–82 (2011).
    Google Scholar 

    34.
    Liu, Y. & Li, Y. Revitalize the world’s countryside. Nature 548, 275–277 (2017).
    ADS  CAS  Article  Google Scholar 

    35.
    Liu, Y., Fang, F. & Li, Y. Key issues of land use in China and implications for policy making. Land Use Policy 40, 6–12 (2014).
    CAS  Article  Google Scholar 

    36.
    Measures for Land Acquisition Compensation and Social Security for Land-Expropriated Farmers in Jiangsu Province Provincial Government Order No. 93 (Jiangsu Provincial People’s Government, 2013).

    37.
    Wu, Y., Chen, Y., Deng, X. & Hui, E. C. M. Development of characteristic towns in China. Habitat Int. 77, 21–31 (2018).
    Article  Google Scholar 

    38.
    Yu, Y., Huang, Y. & Zhang, W. Modeling soil organic carbon change in croplands of China, 1980–2009. Glob. Planet Change 82–83, 115–128 (2012).
    ADS  Article  Google Scholar 

    39.
    No. 1 Central Document (Ministry of Agriculture and Rural Affairs of the People’s Republic of China, 2020); http://www.moa.gov.cn/ztzl/jj2020zyyhwj/

    40.
    Güneralp, B. et al. Global scenarios of urban density and its impacts on building energy use through 2050. Proc. Natl Acad. Sci. USA 114, 8945–8950 (2017).
    Article  Google Scholar  More

  • in

    No projected global drylands expansion under greenhouse warming

    1.
    D’Odorico, P. & Porporato, A. Dryland Ecohydrology (Springer, 2019).
    2.
    Smith, W. K. et al. Remote sensing of dryland ecosystem structure and function: progress, challenges, and opportunities. Remote Sens. Environ. 233, 111401 (2019).
    Article  Google Scholar 

    3.
    Reynolds, J. F. et al. Global desertification: building a science for dryland development. Science 316, 847–851 (2007).
    CAS  Article  Google Scholar 

    4.
    Ahlström, A. et al. The dominant role of semi-arid ecosystems in the trend and variability of the land CO2 sink. Science 348, 895–899 (2015).
    Article  CAS  Google Scholar 

    5.
    Middleton, N. & Thomas, D. S. G. World Atlas of Desertification 2nd edn (Wiley, 1997).

    6.
    Budyko, M. I. & Miller, D. H. International Geophysics Series: Climate and Life Vol. 18 (Academic Press, 1974).

    7.
    Feng, S. & Fu, Q. Expansion of global drylands under a warming climate. Atmos. Chem. Phys. 13, 10081–10094 (2013).
    CAS  Article  Google Scholar 

    8.
    Fu, Q. & Feng, S. Responses of terrestrial aridity to global warming. J. Geophys. Res. Atmos. 119, 7863–7875 (2014).
    Article  Google Scholar 

    9.
    Scheff, J. & Frierson, D. M. W. Terrestrial aridity and its response to greenhouse warming across CMIP5 climate models. J. Clim. 28, 5583–5600 (2015).
    Article  Google Scholar 

    10.
    Huang, J., Yu, H., Guan, X., Wang, G. & Guo, R. Accelerated dryland expansion under climate change. Nat. Clim. Change 6, 166–171 (2016).
    Google Scholar 

    11.
    Huang, J., Yu, H., Dai, A., Wei, Y. & Kang, L. Drylands face potential threat under 2 °C global warming target. Nat. Clim. Change 7, 417–422 (2017).
    Article  Google Scholar 

    12.
    Park, C.-E. et al. Keeping global warming within 1.5 °C constrains emergence of aridification. Nat. Clim. Change 8, 70–74 (2018).
    Article  Google Scholar 

    13.
    Koutroulis, A. G. Dryland changes under different levels of global warming. Sci. Total Environ. 655, 482–511 (2019).
    CAS  Article  Google Scholar 

    14.
    Park, C. E. et al. Inequal responses of drylands to radiative forcing geoengineering methods. Geophys. Res. Lett. 46, 14011–14020 (2019).
    Article  Google Scholar 

    15.
    Wei, Y. et al. Drylands climate response to transient and stabilized 2 °C and 1.5 °C global warming targets. Clim. Dyn. 53, 2375–2389 (2019).
    Article  Google Scholar 

    16.
    Yao, J. et al. Accelerated dryland expansion regulates future variability in dryland gross primary production. Nat. Commun. 11, 1665 (2020).
    CAS  Article  Google Scholar 

    17.
    Berdugo, M. et al. Global ecosystem thresholds driven by aridity. Science 367, 787–790 (2020).
    CAS  Article  Google Scholar 

    18.
    Rajaud, A. & de Noblet-Ducoudré, N. Tropical semi-arid regions expanding over temperate latitudes under climate change. Climatic Change 144, 703–719 (2017).
    Article  Google Scholar 

    19.
    Yang, Y. et al. Disconnection between trends of atmospheric drying and continental runoff. Water Resour. Res. 54, 4700–4713 (2018).
    Article  Google Scholar 

    20.
    Greve, P., Roderick, M. L., Ukkola, A. M. & Wada, Y. The aridity index under global warming. Environ. Res. Lett. 14, 124006 (2019).
    CAS  Article  Google Scholar 

    21.
    Milly, P. C. D. & Dunne, K. A. Potential evapotranspiration and continental drying. Nat. Clim. Change 6, 946–949 (2016).
    Article  Google Scholar 

    22.
    Yang, Y., Roderick, M. L., Zhang, S., McVicar, T. R. & Donohue, R. J. Hydrologic implications of vegetation response to elevated CO2 in climate projections. Nat. Clim. Change 9, 44–48 (2019).
    Article  CAS  Google Scholar 

    23.
    Norby, R. J. & Zak, D. R. Ecological lessons from free-air CO2 enrichment (FACE) experiments. Annu. Rev. Ecol. Evol. Syst. 42, 181–203 (2011).
    Article  Google Scholar 

    24.
    Berg, A. & Sheffield, J. Soil moisture–evapotranspiration coupling in CMIP5 models: relationship with simulated climate and projections. J. Clim. 31, 4865–4878 (2018).
    Article  Google Scholar 

    25.
    Mahowald, N. et al. Projections of leaf area index in Earth system models. Earth Syst. Dyn. 7, 211–229 (2016).
    Article  Google Scholar 

    26.
    Sherwood, S. & Fu, Q. A drier future? Science 343, 737–739 (2014).
    CAS  Article  Google Scholar 

    27.
    Berg, A. et al. Land–atmosphere feedbacks amplify aridity increase over land under global warming. Nat. Clim. Change 6, 869–874 (2016).
    Article  Google Scholar 

    28.
    Berg, A. & Sheffield, J. Climate change and drought: the soil moisture perspective. Curr. Clim. Change Rep. 4, 180–191 (2018).
    Article  Google Scholar 

    29.
    Lavergne, A. et al. Observed and modelled historical trends in the water‐use efficiency of plants and ecosystems. Glob. Change Biol. 25, 2242–2257 (2019).
    Article  Google Scholar 

    30.
    Friedlingstein, P. Carbon cycle feedbacks and future climate change. Phil. Trans. R. Soc. A 373, 20140421 (2015).
    Article  CAS  Google Scholar 

    31.
    Swann, A. L., Hoffman, F. M., Koven, C. D. & Randerson, J. T. Plant responses to increasing CO2 reduce estimates of climate impacts on drought severity. Proc. Natl Acad. Sci. USA 113, 10019–10024 (2016).
    CAS  Article  Google Scholar 

    32.
    Lemordant, L., Gentine, P., Swann, A. S., Cook, B. I. & Scheff, J. Critical impact of vegetation physiology on the continental hydrologic cycle in response to increasing CO2. Proc. Natl Acad. Sci. USA 115, 4093–4098 (2018).
    CAS  Article  Google Scholar 

    33.
    Berg, A. & Sheffield, J. Evapotranspiration partitioning in CMIP5 models: uncertainties and future projections. J. Clim. 32, 2653–2671 (2019).
    Article  Google Scholar 

    34.
    Cao, L., Bala, G., Caldeira, K., Nemani, R. & Ban-Weiss, G. Importance of carbon dioxide physiological forcing to future climate change. Proc. Natl Acad. Sci. USA 107, 9513–9518 (2010).
    CAS  Article  Google Scholar 

    35.
    Skinner, C. B., Poulsen, C. J. & Mankin, J. S. Amplification of heat extremes by plant CO2 physiological forcing. Nat. Commun. 9, 1094 (2018).
    Article  CAS  Google Scholar 

    36.
    Kooperman, G. J. et al. Forest response to rising CO2 drives zonally asymmetric rainfall change over tropical land. Nat. Clim. Change 8, 434–440 (2018).
    Article  Google Scholar 

    37.
    Frieler, K. et al. Assessing the impacts of 1.5 °C global warming—simulation protocol of the Inter-sectoral Impact Model Intercomparison Project (ISIMIP2b). Geosci. Model Dev. 10, 4321–4345 (2017).
    Article  Google Scholar 

    38.
    Zhu, Z. et al. Greening of the Earth and its drivers. Nat. Clim. Change 6, 791–795 (2016).
    CAS  Article  Google Scholar 

    39.
    He, B., Wang, S., Guo, L. & Wu, X. Aridity change and its correlation with greening over drylands. Agric. For. Meteorol. 278, 107663 (2019).
    Article  Google Scholar 

    40.
    Brandt, M. et al. Human population growth offsets climate-driven increase in woody vegetation in sub-Saharan Africa. Nat. Ecol. Evol. 1, 0081 (2017).
    Article  Google Scholar 

    41.
    Burrell, A. L., Evans, J. P. & De Kauwe, M. G. Anthropogenic climate change has driven over 5 million km2 of drylands towards desertification. Nat. Commun. 11, 3853 (2020).
    CAS  Article  Google Scholar 

    42.
    Berg, A., Sheffield, J. & Milly, P. C. D. Divergent surface and total soil moisture projections under global warming. Geophys. Res. Lett. 44, 236–244 (2017).
    Article  Google Scholar 

    43.
    Mankin, J. S., Seager, R., Smerdon, J. E., Cook, B. I. & Williams, A. P. Mid-latitude freshwater availability reduced by projected vegetation responses to climate change. Nat. Geosci. 12, 983–988 (2019).
    CAS  Article  Google Scholar 

    44.
    Liu, Y. et al. Field-experiment constraints on the enhancement of the terrestrial carbon sink by CO2 fertilization. Nat. Geosci. 12, 809–814 (2019).
    CAS  Article  Google Scholar 

    45.
    Zeng, Z. et al. Responses of land evapotranspiration to Earth’s greening in CMIP5 Earth System Models. Environ. Res. Lett. 11, 104006 (2016).
    Article  Google Scholar 

    46.
    Peñuelas, J. et al. Shifting from a fertilization-dominated to a warming-dominated period. Nat. Ecol. Evol. 1, 1438–1445 (2017).
    Article  Google Scholar 

    47.
    Brodribb, T. J., Powers, J., Cochard, H. & Choat, B. Hanging by a thread? Forests and drought. Science 368, 261–266 (2020).
    CAS  Article  Google Scholar 

    48.
    Scheff, J., Seager, R., Liu, H. & Coats, S. Are glacials dry? Consequences for paleoclimatology and for greenhouse warming. J. Clim. 30, 6593–6609 (2017).
    Article  Google Scholar 

    49.
    Ault, T. R. On the essentials of drought in a changing climate. Science 368, 256–260 (2020).
    CAS  Article  Google Scholar 

    50.
    Berg, A. & Sheffield, J. Historic and projected changes in coupling between soil moisture and evapotranspiration (ET) confounded by the role of different ET components. J. Geophys. Res. Atmos. 124, 5791–5806 (2019).
    Google Scholar 

    51.
    Berg, A. & McColl, K. R code for ‘No global drylands expansion under greenhouse warming’. Zenodo https://doi.org/10.5281/zenodo.4490414 (2021). More

  • in

    Bioinformatic analysis of chromatin organization and biased expression of duplicated genes between two poplars with a common whole-genome duplication

    An improved reference genome of P. alba var. pyramidalis
    To identify the major structural variation between the genomes of these two species, we first produced a chromosome-level genome assembly of P. alba var. pyramidalis using single-molecule sequencing and chromosome conformation capture (Hi-C) technologies, and then performed comparative genomic analysis with a recently published genome assembly of P. euphratica37. The resulting assembly of P. alba var. pyramidalis consisted of 131 contigs spanning 408.08 Mb, 94.74% (386.61 Mb) of which were anchored onto 19 chromosomes (Supplementary Fig. S1 and Supplementary Tables S1–S3). A total of 40,215 protein-coding genes were identified in this assembly (Supplementary Table S4). The content of repetitive elements in the genome of P. alba var. pyramidalis (138.17 Mb, 33.86% of the genome) is 188.94 Mb less than that of P. euphratica (327.11 Mb, 56.95% of the genome), which contributes greatly to their differences in genome size (Supplementary Table S5).
    3D organization of the poplar genomes
    To characterize the spatial organization and evolution of poplar 3D genomes at a high resolution, we performed Hi-C experiments using HindIII for P. euphratica and P. alba var. pyramidalis, generating a total of 482.95 million sequencing read pairs. These data were mapped to their respective reference genome sequences. After stringent filtering, 81.72 and 94.61 million usable valid read pairs were obtained in P. euphratica and P. alba var. pyramidalis, respectively, and used for subsequent comparative 3D genome analysis (Supplementary Table S6). In addition, we profiled the DNA methylation and transcriptomes of the same tissue samples to provide a framework for understanding the relationships among epigenetic features and 3D chromatin architecture in poplar.
    We first examined genome packing at the chromosomal level with a genome-wide Hi-C map at 50 kb binning resolution for P. euphratica and P. alba var. pyramidalis. As expected, the normalized Hi-C map from both species showed intense signals on the main diagonal (Fig. 1, and Supplementary Figs. S2 and S3) and a rapid decrease in the frequency of intrachromosomal interactions with increasing genomic distance, indicating frequent interactions between sequences close to each other in the linear genome (Supplementary Fig. S4). Strong intrachromosomal and interchromosomal interactions were also observed on the chromosome arms, implying the presence of chromosome territories in the nucleus, in which each chromosome occupies a limited, exclusive nuclear space16,38.
    Fig. 1: Hi-C heatmaps with compartment region analysis results at 50-kb resolution of P. euphratica chromosome 1 (left) and P. alba var. pyramidalis chromosome 1 (right).

    The heatmaps at the top are Hi-C contact maps at 50-kb resolution, which show global patterns of chromatin interaction in the chromosome. The chromosome is shown from top to bottom and left to right. The ICE-normalized interaction intensity is shown on the color scale on the right side of the heatmap. The track below the Hi-C heatmap shows the partition of A (red histogram, PC1  > 0) and B (green histogram, PC1 5 kb) structural variants ranging from 5 to 446 kb in length in the alignment of the two genomes, including 719 inversions, 476 translocations, and 7947 and 10,093 unique regions in P. alba var. pyramidalis and P. euphratica, respectively (Supplementary Tables S10 and S11).
    To characterize the relationship between structural variation and spatial organization of the poplar genomes, we first analyzed the conservation of A/B compartments between P. alba var. pyramidalis and P. euphratica, using a 50-kb Hi-C matrix. The results showed that 71.52% (145.75 Mb in P. euphratica and 145.63 Mb in P. alba var. pyramidalis) of the total length of the syntenic regions have the same compartment status between the two species, while 43.68 and 43.71 Mb of the genomic regions exhibit A/B compartment switching in P. alba var. pyramidalis and P. euphratica, respectively (Fig. 3a). For the regions with structural variation, we found that 77% of the inversion events between the two genomes had no effects on their compartment status, while 61% of the translocation events occurred within the regions exhibiting compartment switching (Fig. 4a and Supplementary Table S10). Moreover, we also found that 38.59% and 33.39% of the nonsyntenic regions were identified as A compartments in P. alba var. pyramidalis and P. euphratica, respectively, indicating that the large-scale insertions and/or deletions are biased to occur at heterochromatic regions (Fig. 4b). We further assessed the conservation of genome organization at the TAD level by examining whether the orthologous genes within the same TAD in one species could still be located within the TAD in another species19,21,23. The results indicated that only 48.04% of TADs from P. alba var. pyramidalis and 40.95% from P. euphratica were substantially shared between the two species (Figs. 3b, c). Taken together, these results indicated that the 3D genome organization shows surprisingly low conservation across poplar species at both the compartmental and TAD levels.
    Fig. 3: Evolutionary conservation of compartment status and TADs across P. euphratica and P. alba var. pyramidalis.

    a Overlap of compartment status between syntenic regions in P. euphratica and P. alba var. pyramidalis. b Overlap of TADs between syntenic regions in P. euphratica and P. alba var. pyramidalis. c Example of conserved TAD structures across a syntenic region between P. euphratica and P. alba var. pyramidalis. The TADs are outlined by black triangles in the heatmaps, and the position of the TAD domains is indicated by alternating blue-green line segments. The mean cf value used to identify the domains is also shown. The orthology tracks of these conserved domains are shown at the bottom

    Full size image

    Fig. 4: Relationship between structural variation and spatial organization of the genomes of P. euphratica and P. alba var. pyramidalis.

    a Analysis of compartment inversion (left) and translocation (right) across P. euphratica and P. alba var. pyramidalis. b Analysis of compartments of species-specific regions in P. euphratica (left) and P. alba var. pyramidalis (right)

    Full size image

    Relationship between chromatin interactions and expression divergence of WGD-derived paralogs
    Poplar species have undergone a recent WGD event followed by diploidization, a process of genome fractionation that leads to functional and expression divergence of the duplicated gene pairs27,28,33. Although no biased gene loss or expression dominance was found between the two poplar subgenomes, there is evidence that nearly half of the WGD-derived paralogs have diverged in expression32,33. To explore the potential role of chromatin dynamics on the observed expression patterns of duplicated genes, we examined their differences in chromatin interaction patterns for both species. We first identified a total of 10,438 and 9754 paralogous gene pairs showing interchromosomal interactions in P. euphratica and P. alba var. pyramidalis, respectively. After correlating the frequency of chromatin interactions with their differences in expression, we found that gene pairs with biased expression (more than twofold differences in expression levels) interacted less frequently than gene pairs with similar expression levels in both species (P = 1.71 × 10−6 and 7.20 × 10−7 for P. euphratica and P. alba var. pyramidalis, respectively, Mann–Whitney U test; Fig. 5a). We also estimated the interaction score (the average of the distance-normalized interaction frequencies) for bins involved in the paralogous gene pairs and quantified their differences in interaction strength (Supplementary Fig. S7 and Supplementary Table S12)3,23. Our results showed that for gene pairs with biased expression, highly expressed gene copies have stronger interaction strengths than weakly expressed copies (P = 2.10 × 10−12 and 2.74 × 10−2 for P. alba var. pyramidalis and P. euphratica, respectively, Mann–Whitney U test), while no significant differences were observed for gene pairs with similar expression levels (Fig. 5b). We further investigated these phenomena at the level of high-order chromatin architecture and found that the gene pairs located in conserved TADs had similar expression levels (P = 2.68 × 10−3 and 7.86 × 10−6 for P. euphratica and P. alba var. pyramidalis, respectively, Mann–Whitney U test; Supplementary Fig. S8). Overall, our analyses indicate that the extensive expression divergence between WGD-derived paralogs in Populus is associated with the differences in their chromatin dynamics and 3D genome organization, and suggest that this organization may function as a key regulatory layer underlying expression divergence during diploidization.
    Fig. 5: Comparison of interaction levels between WGD-derived paralogs with biased/similar expression in P. euphratica and P. alba var. pyramidalis.

    a The box plot shows that the interaction frequency of WGD-derived paralogs with biased (fold change  > 2) and similar (fold change  More

  • in

    Seeing biodiversity from a Chinese perspective

    Zoologist Alice Hughes leads the landscape-ecology research group at Xishuangbanna Tropical Botanical Garden in Menglun, Yunnan province, China.Credit: Michael C. Orr

    British zoologist Alice Hughes has been working at the Xishuangbanna Tropical Botanical Garden in Menglun, Yunnan province, in southern China, for nearly eight years. She reveals what she has learnt about the country’s approach to ecological conservation ahead of its first United Nations biodiversity conference in Kunming, Yunnan, in May.
    What is your current role?
    I lead the landscape-ecology research group at one of China’s most diverse botanical gardens. My team aims to better understand the lives of animals and how they interact with their environments. This helps us to create more effective methods of conserving a biodiverse environment.
    The 18-person team, which is part of the Chinese Academy of Sciences (CAS), does everything from mapping biodiversity to researching the illegal and legal trade in different species, to find out where and why our natural world is changing. We then develop actionable measures to help stem the worst effects of those changes.
    For example, many members of my team are working on the various species of Rhinolophus bats. Our genetic research suggests that around 70% of the Rhinolophus bat species haven’t been described in scientific literature. If you can’t describe a species, then you can’t conserve it.
    How did you come to work in China, and what’s it like?
    In 2011, I moved to Thailand from the United Kingdom as part of my postdoctoral research, before heading to Australia and finally taking a position in China in 2013.
    At first, I was naive about how different the culture might be in Asian countries and it’s definitely been a steep learning curve. Adaptability is important. I think that many people in the West are much too ready to disbelieve or find fault with actions from China, and Chinese scientists. As a result, there is sensitivity in China’s research community, especially around things that have frequently been an issue, such as the regulation of the trade of exotic wildlife. As a foreigner, it is a challenging balance to provide advice without it being seen as overly critical. I can participate in these discussions at a high level because I have worked here long enough: people know I will listen and provide my perspectives based on fact, rather than prejudice.

    I’ve worked on some difficult and potentially sensitive topics, such as endangered species, wildlife trade and the Belt and Road Initiative, which aims to link global trade routes to China through international infrastructure development, for example. I focus on the possible impacts these might have on biodiversity and how to minimize them. China is wary of being accused of driving extensive biodiversity loss, especially as it is investing in scientific research to avert it.
    I’ve been invited to join a variety of both central and regional government working groups. It’s a privilege to be in those groups and work with some of the country’s top scientists, especially when it comes to international or UN meetings.
    Working for CAS is the equivalent to being an employee of the government. Many people outside China still find it surprising that foreigners work in scientific institutes here, even though the number is growing.
    I’m also unusual because I’m a foreign woman. In the time I have worked here I don’t think I have met any other European women with full-time faculty positions in China. In my institute there are more than ten foreign men with such positions. It’s not easy for Chinese women either. At the institute, we have 43 research groups; only 3 are led by women.
    It’s important for all conservation scientists to be open minded and willing to find out what’s going to work in any country and culture to help tackle the global problem of biodiversity loss, and develop solutions that work in that societal context. A good example of that came last year, when some specialists called for a global ban on wild-meat consumption, amid fears over new diseases that originate in wild animals and cause outbreaks in humans. Now that might sound like a great idea, but in many parts of Africa there is not enough water to raise livestock, and people depend on wild meat for food.
    This means that rather than recommending a blanket ban, a better solution might be a system that monitors what is traded, and provides recommendations as to which species can be eaten safely and sustainably.

    Xishuanganna tropical botanic garden in southwest China’s Yunnan Province.Credit: Xinhua/eyevine

    Do foreign scientists need to speak Chinese to work in China?
    For most of my team, neither English nor Chinese is their first language. We have around 12 different nationalities, so discussions take place predominantly in English, as a default.
    I work closely with my Chinese colleagues to make sure that our research work is properly communicated when it’s published in Chinese. In meetings with Chinese colleagues, someone will translate pertinent points to me, or I’ll translate my slides into Chinese and present in English. I also have my reports and briefs translated, and with advances in translation software, we can get what is needed done.
    It’s easy to have misunderstandings when you’re translating ideas between different languages, so we’re careful to look for any linguistic nuances that might change the perceived meaning.
    How is China balancing urbanization with conservation?
    It’s an ongoing challenge. The concept of an ecological civilization — the government’s vision for environmentally sustainable growth in China — was written into the country’s constitution in 2018 after it was made a national priority in 2012, which is a huge commitment to sustainability.
    A principal policy is the ecological conservation red-line plan, an idea that has been developed over the past decade. Across China, large areas of land are now being protected from industrial and urban development, in part to ensure that crucial ecosystems, such as wetlands that limit floods, can continue to function effectively. Multimillion-dollar developments have been torn down during its roll-out. China is one of few countries to have enacted such a science-based, top-down vision of how to balance human need with the maintenance of ecological services and preservation of biodiversity.

    It’s not all perfect, though: I know that on paper, these ecological red lines now exist and in certain biodiversity hotspots they have been enforced. But not every region is the same. Areas have high levels of autonomy and in Yunnan, where I live, there have been more challenges for the local government to work with provincial governments for many practical and political reasons. The saying goes, ‘The mountains are high, and the emperor is far away’: places that are far away from Beijing feel less pressure to enact centralized policies because there is less supervision.
    The south of China has seen lots of deforestation, which is hugely damaging to biodiversity. Natural forests have been replaced with for-profit tree plantations, usually planted with rubber or eucalyptus, which have had a hugely negative impact on biodiversity. Sustainable forestry is a real issue across Asia.
    China is leading an important biodiversity conference in May. What are your expectations?
    It’s the first time that China will host the UN biodiversity conference and this puts the spotlight on what they are doing to help the situation.
    I know there are a number of senior Chinese officials who would like to see China take on more of an international leadership role, in addition to making efforts to preserve biodiversity domestically.
    The current set of UN goals for global biodiversity expired last year and the next set, which is planned to be agreed at the convention, must encourage countries to plant diverse, native species. Currently, there is no pressure coming from politicians to do that, even though we know we suffer biodiversity loss as a result: we’re often hung up on targets, even if those targets are virtue signalling, rather than real change.
    Also, governments tend to try to meet their targets in the easiest and most economically beneficial way. So they meet their tree-planting targets by planting by just a few, non-diverse species that are often not even native to the country.
    We still need to include more practical goals in policy documents, such as enabling sustainable supply chains, to focus on the mechanisms behind biodiversity loss.
    What strikes you as unique about the Chinese ecological-research environment?
    A Chinese ecologist needs to be fast to act. The time frame to submit an application for a grant can be very quick. Often you have less than 24 hours to respond. Also, most initiatives are tied to the government’s five-year plans, so our priorities need to adapt to reflect those five-year cycles.
    In the past two years, there has been a complete inventory of all China’s marine and terrestrial protected areas so they can be accurately mapped and future targets can be based on them. That really is an unparalleled effort.
    This involved mapping 400 marine protected areas, and 13,600 terrestrial ones. I haven’t heard of anything equivalent to this scale and speed in any other country.
    The most positive thing for me is that science matters here. The annual budget for scientific research is increasing and the findings from our applied research inform national policy. That is something the West would do well to remember. More

  • in

    Nitrogen addition decreases methane uptake caused by methanotroph and methanogen imbalances in a Moso bamboo forest

    1.
    Ni, X. & Groffman, P. M. Declines in methane uptake in forest soils. Proc. Natl. Acad. Sci. USA 115, 8587–8590 (2018).
    CAS  PubMed  Article  Google Scholar 
    2.
    IPCC. Climate change 2013: the physical science basis Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change (Cambridge University Press, 2013).

    3.
    Kirschke, S. et al. Three decades of global methane sources and sinks. Nat. Geosci. 6, 813–823 (2013).
    ADS  CAS  Article  Google Scholar 

    4.
    Turner, A. J., Frankenberg, C. & Kort, E. A. Interpreting contemporary trends in atmospheric methane. Proc. Natl. Acad. Sci. USA 116, 2805–2813 (2019).
    CAS  PubMed  Article  Google Scholar 

    5.
    Tate, K. R. Soil methane oxidation and land-use change–from process to mitigation. Soil Biol. Biochem. 80, 260–272 (2015).
    CAS  Article  Google Scholar 

    6.
    Thauer, R. K., Anne-Kristin, K., Henning, S., Wolfgang, B. & Reiner, H. Methanogenic archaea: ecologically relevant differences in energy conservation. Nat. Rev. Microbiol. 6, 579–591 (2008).
    CAS  PubMed  Article  Google Scholar 

    7.
    Banger, K., Tian, H. & Lu, C. Do nitrogen fertilizers stimulate or inhibit methane emissions from rice fields?. Glob. Change Biol. 18, 3259–3267 (2012).
    ADS  Article  Google Scholar 

    8.
    Murase, J. & Kimura, M. Methane production and its fate in paddy fields. IV. Sources of microorganisms and substrates responsible for anaerobic CH4 oxidation in subsoil. Soil Sci. Plant Nutr. 40, 57–61 (1994).
    CAS  Article  Google Scholar 

    9.
    Zhang, M., Huang, J., Sun, S., Rehman, M. & He, S. Depth-specific distribution and significance of nitrite-dependent anaerobic methane oxidation process in tidal flow constructed wetlands used for treating river water. Sci. Total Environ. 716, 107354 (2020).
    Google Scholar 

    10.
    Yu, X. et al. Sonneratia apetala introduction alters methane cycling microbial communities and increases methane emissions in mangrove ecosystems. Soil Biol. Biochem. 144, 107775 (2020).
    CAS  Article  Google Scholar 

    11.
    Hanson, R. S. & Hanson, T. E. Methanotrophic bacteria. Microbiol. Rev. 60, 439–471 (1996).
    CAS  PubMed  PubMed Central  Article  Google Scholar 

    12.
    Knief, C. Diversity and habitat preferences of cultivated and uncultivated aerobic methanotrophic bacteria evaluated based on pmoA as molecular marker. Front. Microbiol. 6, 1346 (2015).
    PubMed  PubMed Central  Article  Google Scholar 

    13.
    Dunfield, P., Knowles, R., Dumont, R. & Moore, T. R. Methane production and consumption in temperate and subarctic peat soils: response to temperature and pH. Soil Biol. Biochem. 25, 321–326 (1993).
    CAS  Article  Google Scholar 

    14.
    Mer, J. L. & Roger, P. Production, oxidation, emission and consumption of methane by soils: a review. Eur. J. Soil Biol. 37, 25–50 (2001).
    Article  Google Scholar 

    15.
    Aronson, E. L., Dubinsky, E. A. & Helliker, B. R. Effects of nitrogen addition on soil microbial diversity and methane cycling capacity depend on drainage conditions in a pine forest soil. Soil Biol. Biochem. 62, 119–128 (2013).
    CAS  Article  Google Scholar 

    16.
    Bodelier, P. L. E. & Laanbroek, H. J. Nitrogen as a regulatory factor of methane oxidation in soils and sediments. FEMS Microbiol. Ecol. 47, 265–277 (2004).
    CAS  PubMed  Article  Google Scholar 

    17.
    Galloway, J. N. et al. Transformation of the nitrogen cycle: recent trends, questions, and potential solutions. Science 320, 889–892 (2008).
    ADS  CAS  PubMed  PubMed Central  Article  Google Scholar 

    18.
    Liu, L. & Greaver, T. L. A review of nitrogen enrichment effects on three biogenic GHGs: the CO2 sink may be largely offset by stimulated N2O and CH4 emission. Ecol. Lett. 12, 1103–1117 (2009).
    CAS  PubMed  Article  Google Scholar 

    19.
    Fowler, D., Coyle, M., Skiba, U., Sutton, M. A. & Voss, M. The global nitrogen cycle in the twenty-first century. Philos. Trans. R. Soc. B. 368, 20130164 (2013).
    Article  CAS  Google Scholar 

    20.
    Reay, D. S., Dentener, F., Smith, P., Grace, J. & Feely, R. A. Global nitrogen deposition and carbon sinks. Nat. Geosci. 1, 430–437 (2008).
    ADS  CAS  Article  Google Scholar 

    21.
    Ackerman, D., Millet, D. B. & Chen, X. Global estimates of inorganic nitrogen deposition across four decades. Glob. Biogeochem. Cycles 33, 100–107 (2019).
    ADS  CAS  Article  Google Scholar 

    22.
    Liu, X. et al. Enhanced nitrogen deposition over China. Nature 494, 459–462 (2013).
    ADS  CAS  PubMed  Article  Google Scholar 

    23.
    Li, Q. et al. Nitrogen depositions increase soil respiration and decrease temperature sensitivity in a Moso bamboo forest. Agric. For. Meteorol. 268, 48–54 (2019).
    ADS  Article  Google Scholar 

    24.
    Steudler, P. A., Bowden, R. D., Melillo, J. M. & Aber, J. D. Influence of nitrogen fertilization on methane uptake in temperate forest soils. Nature 341, 314–316 (1989).
    ADS  Article  Google Scholar 

    25.
    Hütsch, B. W., Webster, C. P. & Powlson, D. S. Methane oxidation in soil as affected by land use, soil pH and N fertilization. Soil Biol. Biochem. 26, 1613–1622 (1994).
    Article  Google Scholar 

    26.
    Bodelier, P. L. E., Roslev, P., Henckel, T. & Frenzel, P. Stimulation by ammonium-based fertilizers of methane oxidation in soil around rice roots. Nature 403, 421–424 (2000).
    ADS  CAS  PubMed  Article  Google Scholar 

    27.
    Kruger, M. & Frenzel, P. Effects of N-fertilisation on CH4 oxidation and production, and consequences for CH4 emissions from microcosms and rice fields. Glob. Change Biol. 9, 773–784 (2003).
    ADS  Article  Google Scholar 

    28.
    Delgado, J. A. & Mosier, A. R. Mitigation alternatives to decrease nitrous oxides emissions and urea-nitrogen loss and their effect on methane flux. J. Environ. Qual. 25, 1105–1111 (1996).
    CAS  Article  Google Scholar 

    29.
    Shang, Q. et al. Net annual global warming potential and greenhouse gas intensity in Chinese double rice-cropping systems: a 3-year field measurement in long-term fertilizer experiments. Glob. Change Biol. 17, 2196–2210 (2011).
    ADS  Article  Google Scholar 

    30.
    Cai, Z. et al. Methane and nitrous oxide emissions from rice paddy fields as affected by nitrogen fertilizers and water management. Plant Soil 196, 7–14 (1997).
    CAS  Article  Google Scholar 

    31.
    Malghani, S., Reim, A., Fischer, J. V., Conrad, R. & Trumbore, S. E. Soil methanotroph abundance and community composition are not influenced by substrate availability in laboratory incubations. Soil Biol. Biochem. 101, 184–194 (2016).
    CAS  Article  Google Scholar 

    32.
    Schnyder, E., Bodelier, P. L. E., Hartmann, M., Henneberger, R. & Niklaus, P. A. Positive diversity-functioning relationships in model communities of methanotrophic bacteria. Ecology 99, 714–723 (2018).
    PubMed  Article  Google Scholar 

    33.
    Wang, C., Liu, D. & Bai, E. Decreasing soil microbial diversity is associated with decreasing microbial biomass under nitrogen addition. Soil Biol. Biochem. 120, 126–133 (2018).
    CAS  Article  Google Scholar 

    34.
    Shrestha, M., Shrestha, P. M., Frenzel, P. & Conrad, R. Effect of nitrogen fertilization on methane oxidation, abundance, community structure, and gene expression of methanotrophs in the rice rhizosphere. ISME J. 4, 1545–1556 (2010).
    CAS  PubMed  Article  Google Scholar 

    35.
    Liu, H. et al. Responses of soil methanogens, methanotrophs, and methane fluxes to land-use conversion and fertilization in a hilly red soil region of southern China. Environ. Sci. Pollut. Res. 24, 8731–8743 (2017).
    CAS  Article  Google Scholar 

    36.
    Bao, Q., Ding, L. J., Huang, Y. & Xiao, K. Effect of rice straw and/or nitrogen fertiliser inputs on methanogenic archaeal and denitrifying communities in a typical rice paddy soil. Earth Environ. Sci. Trans. R. Soc. Edinb. 109, 375–386 (2019).
    CAS  Google Scholar 

    37.
    Ho, A. et al. The more, the merrier: heterotroph richness stimulates methanotrophic activity. ISME J. 8, 1945–1948 (2014).
    PubMed  PubMed Central  Article  Google Scholar 

    38.
    Dan, H. et al. The response of methanotrophs to additions of either ammonium, nitrate or urea in alpine swamp meadow soil as revealed by stable isotope probing. FEMS Microbiol. Ecol. 7, fiz077 (2019).
    Google Scholar 

    39.
    Zhang, D., Mo, L., Chen, X., Zhang, L. & Xu, X. Effect of nitrogen addition on methanotrophs in temperate forest soil. Acta Ecol. Sin. 37, 8254–8263 (2017).
    Google Scholar 

    40.
    Mohanty, S. R., Bodelier, P. L. E., Floris, V. & Conrad, R. Differential effects of nitrogenous fertilizers on methane-consuming microbes in rice field and forest soils. Appl. Environ. Microbiol. 72, 1346–1354 (2006).
    CAS  PubMed  PubMed Central  Article  Google Scholar 

    41.
    Hu, A. & Lu, Y. The differential effects of ammonium and nitrate on methanotrophs in rice field soil. Soil Biol. Biochem. 85, 31–38 (2015).
    CAS  Article  Google Scholar 

    42.
    Shrestha, P. M. et al. Linking activity, composition and seasonal dynamics of atmospheric methane oxidizers in a meadow soil. ISME J. 6, 1115–1126 (2012).
    CAS  PubMed  Article  Google Scholar 

    43.
    Jang, I., Lee, S., Zoh, K. D. & Kang, H. Methane concentrations and methanotrophic community structure influence the response of soil methane oxidation to nitrogen content in a temperate forest. Soil Biol. Biochem. 43, 620–627 (2011).
    CAS  Article  Google Scholar 

    44.
    Song, X., Chen, X., Zhou, G., Jiang, H. & Peng, C. Observed high and persistent carbon uptake by Moso bamboo forests and its response to environmental drivers. Agric. For. Meteorol. 247, 467–475 (2017).
    ADS  Article  Google Scholar 

    45.
    Song, X. et al. Carbon sequestration by Chinese bamboo forests, and their ecological benefits: assessment of potential, problems, and future challenges. Environ. Rev. 19, 418–428 (2011).
    CAS  Article  Google Scholar 

    46.
    Jia, Y. et al. Spatial and decadal variations in inorganic nitrogen wet deposition in China induced by human activity. Sci. Rep. 4, 3763 (2014).
    PubMed  PubMed Central  Article  CAS  Google Scholar 

    47.
    Song, X., Zhou, G., Gu, H. & Qi, L. Management practices amplify the effects of N deposition on leaf litter decomposition of the Moso bamboo forest. Plant Soil 395, 391–400 (2015).
    CAS  Article  Google Scholar 

    48.
    Mo, J., Fang, Y., Xu, G., Li, D. & Xue, J. The short-term responses of soil CO2 emission and CH4 uptake to simulated N deposition in nursery and forests of Dinghushan in subtropical China. Acta Ecol. Sin. 25, 682–690 (2005).
    CAS  Google Scholar 

    49.
    Zhang, W. et al. Methane uptake responses to nitrogen deposition in three tropical forests in southern China. J. Geophys. Res. 113, D11116 (2008).
    ADS  Article  CAS  Google Scholar 

    50.
    Song, X. et al. Nitrogen addition increased CO2 uptake more than non-CO2 greenhouse gases emissions in a Moso bamboo forest. Sci. Adv. 6, eaaw5790 (2020).
    ADS  CAS  PubMed  PubMed Central  Article  Google Scholar 

    51.
    Knief, C., Lipski, A. & Dunfield, P. F. Diversity and activity of methanotrophic bacteria in different upland soils. Appl. Environ. Microbiol. 69, 6703–6714 (2003).
    CAS  PubMed  PubMed Central  Article  Google Scholar 

    52.
    Wang, M., Xu, X., Wang, W., Wang, G. & Su, C. Effects of slag and biochar amendments on methanogenic community structures in paddy fields. Acta Ecol. Sin. 38, 2816–2818 (2018).
    Article  Google Scholar 

    53.
    Zeikus, J. G. Biology of methanogenic bacteria. Bacteriol. Rev. 41, 514–541 (1977).
    CAS  PubMed  PubMed Central  Article  Google Scholar 

    54.
    Täumer, J. et al. Divergent drivers of the microbial methane sink in temperate forest and grassland soils. Glob. Change Biol. 27, 929–940 (2021).

    55.
    Pratscher, J., Vollmers, J., Wiegand, S., Dumont, M. G. & Kaster, A. K. Unravelling the identity, metabolic potential and global biogeography of the atmospheric methane-oxidizing upland soil cluster α. Environ. Microbiol. 20(3), 1016–1029 (2018).
    CAS  PubMed  PubMed Central  Article  Google Scholar 

    56.
    Knief, C. Diversity and habitat preferences of cultivated and uncultivated aerobic methanotrophic bacteria evaluated based on pmoA as molecular marker. Front. Microbiol. 6, 487 (2015).
    Article  Google Scholar 

    57.
    Deng, Y. et al. Upland soil cluster gamma dominates methanotrophic communities in upland grassland soils. Sci. Total Environ. 670, 826–836 (2019).
    ADS  CAS  PubMed  Article  Google Scholar 

    58.
    Henckel, T., Friedrich, M. & Conrad, R. Molecular analyses of the methane-oxidizing microbial community in rice field soil by targeting the genes of the 16S rRNA, particulate methane monooxygenase, and methanol dehydrogenase. Appl. Environ. Microbiol. 65, 1980–1990 (1999).
    CAS  PubMed  PubMed Central  Article  Google Scholar 

    59.
    Lieberman, R. L. & Rosenzweig, A. C. Biological methane oxidation: regulation, biochemistry, and active site structure of particulate methane monooxygenase. Crit. Rev. Biochem. Mol. Biol. 39, 147–164 (2004).
    CAS  PubMed  Article  Google Scholar 

    60.
    Freitag, T. E. & Prosser, J. I. Correlation of methane production and functional gene transcriptional activity in a peat soil. Appl. Environ. Microbiol. 75, 6679–6687 (2009).
    CAS  PubMed  PubMed Central  Article  Google Scholar 

    61.
    Thauer, R. K. Biochemistry of methanogenesis: a tribute to Marjory Stephenson: 1998 Marjory Stephenson prize lecture. Microbiology 144, 2377–2406 (1998).
    CAS  PubMed  Article  Google Scholar 

    62.
    Schnell, S. & King, G. M. Mechanistic analysis of ammonium inhibition of atmospheric methane consumption in forest soils. Appl. Environ. Microbiol. 60, 3514–3521 (1994).
    CAS  PubMed  PubMed Central  Article  Google Scholar 

    63.
    Chao, A. Nonparametric estimation of the number of classes in a population. Scand. J. Stat. 11, 265–270 (1984).
    MathSciNet  Google Scholar 

    64.
    Shannon, C. E. A. mathematical theory of communication. Bell Syst. Tech. J. 27, 379–423 (1948).
    MathSciNet  MATH  Article  Google Scholar 

    65.
    Li, Q. et al. Biochar amendment decreases soil microbial biomass and increases bacterial diversity in Moso bamboo (Phyllostachys edulis) plantations under simulated nitrogen deposition. Environ. Res. Lett. 13, 044029 (2018).
    ADS  Article  CAS  Google Scholar 

    66.
    Li, Q., Song, X., Gu, H. & Gao, F. Nitrogen deposition and management practices increase soil microbial biomass carbon but decrease diversity in Moso bamboo plantations. Sci. Rep. 6, 28235 (2016).
    ADS  PubMed  PubMed Central  Article  Google Scholar 

    67.
    Frey, S. D., Knorr, M., Parrent, J. L. & Simpson, R. T. Chronic nitrogen enrichment affects the structure and function of the soil microbial community in temperate hardwood and pine forests. For. Ecol. Manag. 196, 159–171 (2004).
    Article  Google Scholar 

    68.
    Lin, Y. et al. Long-term application of lime or pig manure rather than plant residues suppressed diazotroph abundance and diversity and altered community structure in an acidic ultisol. Soil Biol. Biochem. 123, 218–228 (2018).
    CAS  Article  Google Scholar 

    69.
    Rousk, J. et al. Soil bacterial and fungal communities across a pH gradient in an arable soil. ISME J. 4, 1340–1351 (2010).
    PubMed  Article  Google Scholar 

    70.
    Zhou, X., Guo, Z., Chen, C. & Jia, Z. Soil microbial community structure and diversity are largely influenced by soil pH and nutrient quality in 78-year-old tree plantations. Biogeosciences 14, 2101–2111 (2017).
    ADS  CAS  Article  Google Scholar 

    71.
    Nicol, G. W., Leininger, S., Schleper, C. & Prosser, J. I. The influence of soil pH on the diversity, abundance and transcriptional activity of ammonia oxidizing archaea and bacteria. Environ. Microbiol. 10, 2966–2978 (2008).
    CAS  PubMed  Article  Google Scholar 

    72.
    Vitousek, P. M. et al. Technical report: human alteration of the global nitrogen cycle: sources and consequences. Ecol. Appl. 7, 737 (1997).
    Google Scholar 

    73.
    Treseder, K. K. Nitrogen additions and microbial biomass: a meta-analysis of ecosystem studies. Ecol. Lett. 11, 1111–1120 (2008).
    PubMed  Article  Google Scholar 

    74.
    Serna-Chavez, H. M. & Bodegom, P. M. V. Global drivers and patterns of microbial abundance in soil. Glob. Ecol. Biogeogr. 22, 1162–1172 (2013).
    Article  Google Scholar 

    75.
    Rosso, L., Lobry, J. R., Bajard, S. & Flandrois, J. P. Convenient model to describe the combined effects of temperature and pH on microbial growth. Appl. Environ. Microbiol. 61, 610–616 (1995).
    CAS  PubMed  PubMed Central  Article  Google Scholar 

    76.
    Högberg, M. N., Högberg, P. & Myrold, D. D. Is microbial community composition in boreal forest soils determined by pH, C-to-N ratio, the trees, or all three?. Oecologia 150, 590–601 (2007).
    ADS  PubMed  Article  Google Scholar 

    77.
    Sterner, R. W. & Elser, J. J. Ecological Stoichiometry: The Biology of Elements from Molecules to the Biosphere (Princeton University Press, Princeton, 2002).
    Google Scholar 

    78.
    Kolb, S. The quest for atmospheric methane oxidizers in forest soils. Environ. Microbiol. Rep. 1, 336–346 (2009).
    CAS  PubMed  Article  Google Scholar 

    79.
    Topp, E. & Pettey, E. Soils as sources and sinks for atmospheric methane. Can. J. Soil Sci. 77, 167–177 (1997).
    CAS  Article  Google Scholar 

    80.
    Bender, M. & Conrad, R. Effect of CH4 concentrations and soil conditions on the induction of CH4 oxidation activity. Soil Biol. Biochem. 27, 1517–1527 (1995).
    CAS  Article  Google Scholar 

    81.
    Kolb, S., Knief, C., Dunfield, P. F. & Conrad, R. Abundance and activity of uncultured methanotrophic bacteria involved in the consumption of atmospheric methane in two forest soils. Environ. Microbiol. 7(8), 1150–1161 (2005).
    CAS  PubMed  Article  Google Scholar 

    82.
    Degelmann, D. M., Borken, W., Drake, H. L. & Kolb, S. Different atmospheric methane-oxidizing communities in European Beech and Norway Spruce Soils. Appl. Environ. Microbiol. 76(10), 3228–3235 (2010).
    CAS  PubMed  PubMed Central  Article  Google Scholar 

    83.
    Li, S., Yu, Y. & He, S. Summary of research on dissolved organic carbon (DOC). Soil Environ. Sci. 11, 422–429 (2002).
    Google Scholar 

    84.
    Zhang, R. et al. Nitrogen deposition enhances photosynthesis in Moso bamboo but increases susceptibility to other stress factors. Front. Plant Sci. 8, 1975 (2017).
    PubMed  PubMed Central  Article  Google Scholar 

    85.
    Wan, X. et al. Soil C:N ratio is the major determinant of soil microbial community structure in subtropical coniferous and broadleaf forest plantations. Plant Soil 387, 103–116 (2015).
    CAS  Article  Google Scholar 

    86.
    Demoling, F., Figueroa, D. & Bååth, E. Comparison of factors limiting bacterial growth in different soils. Soil Biol. Biochem. 39, 485–2495 (2007).
    Article  CAS  Google Scholar 

    87.
    Aronson, E. L. & Helliker, B. R. Methane flux in non-wetland soils in response to nitrogen addition: a meta-analysis. Ecology 91, 3242–3251 (2010).
    CAS  Article  Google Scholar 

    88.
    Cheng, S. et al. The primary factors controlling methane uptake from forest soils and their responses to increased atmospheric nitrogen deposition: a review. Acta Ecol. Sin. 32, 4914–4923 (2012).
    ADS  CAS  Article  Google Scholar 

    89.
    Fierer, N. et al. Comparative metagenomic, phylogenetic and physiological analyses of soil microbial communities across nitrogen gradients. ISME J. 6, 1007–1017 (2012).
    CAS  PubMed  Article  Google Scholar 

    90.
    Ramirez, K. S., Craine, J. M. & Fierer, N. Consistent effects of nitrogen amendments on soil microbial communities and processes across biomes. Glob. Change Biol. 18, 1918–1927 (2012).
    ADS  Article  Google Scholar 

    91.
    Song, X., Li, Q. & Gu, H. Effect of nitrogen deposition and management practices on fine root decomposition in Moso bamboo plantations. Plant Soil 410, 207–215 (2017).
    CAS  Article  Google Scholar 

    92.
    Vance, E. D., Brookes, P. C. & Jenkinson, D. S. An extraction method for measuring soil microbial biomass C. Soil Biol. Biochem. 19, 703–707 (1987).
    CAS  Article  Google Scholar 

    93.
    Li, Y. et al. Biochar reduces soil heterotrophic respiration in a subtropical plantation through increasing soil organic carbon recalcitrancy and decreasing carbon-degrading microbial activity. Soil Biol. Biochem. 122, 173–185 (2018).
    CAS  Article  Google Scholar 

    94.
    Lu, R. Methods for Soil Agro-chemistry Analysis (China Agricultural Science and Technology Press, Beijing, 2000).
    Google Scholar 

    95.
    Bourne, D. G., Mcdonald, I. R. & Murrell, J. C. Comparison of pmoA PCR primer sets as tools for investigating methanotroph diversity in three Danish soils. Appl. Environ. Microbiol. 67, 3802 (2001).
    CAS  PubMed  PubMed Central  Article  Google Scholar 

    96.
    Angel, R., Claus, P. & Conrad, R. Methanogenic archaea are globally ubiquitous in aerated soils and become active under wet anoxic conditions. ISME J. 6, 847–862 (2011).
    PubMed  PubMed Central  Article  CAS  Google Scholar 

    97.
    Caporaso, J. G. et al. QIIME allows analysis of high-throughput community sequencing data. Nat. Methods 7, 335–336 (2010).
    CAS  PubMed  PubMed Central  Article  Google Scholar 

    98.
    Wang, Q. et al. Ecological patterns of nifH genes in four terrestrial climatic zones explored with targeted metagenomics using FrameBot, a new informatics tool. mBio 4, e00592-e613 (2013).
    PubMed  PubMed Central  Google Scholar 

    99.
    Kou, Y. et al. Scale-dependent key drivers controlling methane oxidation potential in Chinese grassland soils. Soil Biol. Biochem. 111, 104–114 (2017).
    CAS  Article  Google Scholar 

    100.
    Kou, Y. et al. Climate and soil parameters are more important than denitrifier abundances in controlling potential denitrification rates in Chinese grassland soils. Sci. Total Environ. 669, 62–69 (2019).
    ADS  CAS  PubMed  Article  Google Scholar 

    101.
    Wei, H. et al. Contrasting soil bacterial community, diversity, and function in two forests in China. Front. Microbiol. 9, 1693 (2018).
    PubMed  PubMed Central  Article  Google Scholar 

    102.
    Liu, W. et al. Critical transition of soil bacterial diversity and composition triggered by nitrogen enrichment. Ecology 101, e03053 (2020).
    PubMed  Google Scholar 

    103.
    Tang, X., Liu, S., Zhou, G., Zhang, D. & Zhou, C. Soil-atmospheric exchange of CO2, CH4, and N2O in three subtropical forest ecosystems in southern China. Glob. Change Biol. 12, 546–560 (2006).
    ADS  Article  Google Scholar  More

  • in

    The flight of the hornbill: drift and diffusion in arboreal avian movement

    A mathematical model to simulate movement
    For ‘attracting features’, such as nesting or roosting sites, we employ potential terms that are logarithmic in distance. Logarithmic potentials have been employed in diffusion models7 such as those involving long-range interactions8. The forces due to these are inversely proportional to distance from the features. Given a choice between locations, an animal would invariably drift towards ones that are closer. Additionally, they also command some influence for longer distances. We did consider alternatives such as a potential that corresponds to an inverse squared force but it diminishes much faster as the distance to the source increases. The ‘repulsive features’ such as human dominated areas are incorporated using Gaussian type potentials that would have an influence only when the animal is close to them. Such forces fall off exponentially fast as one goes away from the source location.
    The corresponding Langevin equations can be written as:

    $$begin{aligned} frac{dx}{dt}= & {} -gamma sum _{i}frac{ 2alpha times (x – x_{i})}{(x – x_{i})^2 + (y – y_{i})^2} nonumber \&+,gamma sum _{j}Big ((x-x_{j}) e^{-((x-x_{j})^2 + (y-y_{j})^2)}Big ) + root 2 of {2D}xi _x(t) end{aligned}$$
    (1)

    $$begin{aligned} frac{dy}{dt}= & {} -gamma sum _{i}frac{ 2alpha times (y – y_{i})}{(x – x_{i})^2 + (y – y_{i})^2} nonumber \&+,gamma sum _{j}Big ((y-y_{j}) e^{-((x-x_{j})^2 + (y-y_{j})^2)}Big ) + root 2 of {2D}xi _y(t) end{aligned}$$
    (2)

    where x and y denote the coordinates of an animal’s location. ((x_{i}), (y_{i})) and ((x_{j}), (y_{j})) denote locations of i attracting and j repelling features respectively. We only choose nests as points of attraction for breeding hornbills since their diurnal movements are strongly centred around the nests. The white noise terms (xi _x) and (xi _y) are Gaussian in nature and delta correlated—which means that no correlations exist between the noise values at different instances of time. (gamma ) and D denote the drift and diffusion coefficients respectively. The drift coefficient (gamma ) represents the directedness of motion, which could be interpreted as strength of bias towards/against certain features in the landscape. In contrast, D quantifies the strength of random undirected motion. The force term with coefficient (-gamma ) results from negative gradient of the logarithmic potential, whose choice we explained earlier:

    $$begin{aligned} U = gamma sum _{i} log left{ (x – x_{i})^2 + (y – y_{i})^2 right} ^{alpha } ,,,. end{aligned}$$
    (3)

    The value of (alpha ) is determined from calculation of first passage times of the birds (discussed in the following section) and comparison of the values so obtained with observational (telemetry) data. We find that (alpha ) = 8 gives biologically sensible first passage times for hornbills (see “Calculating First Passage Times” in Methods section, Table 3 and Supplementary Tables 1, 2). If one observes an animal’s movement for a very long time, the probability of finding the animal would decrease more drastically away from a central feature for lower values of (alpha ). Such variations are captured by the steady-state probability distributions of space-use that we describe in the following section.
    Fokker–Planck methods
    Although the Langevin equations can generate trajectories of movement, the corresponding simulations need to be run for very long times to infer reliable information about spatial use. The time steps are further much smaller than the frequency of data recorded by the GPS. The step-lengths thus generated from simulated trajectories do not lend themselves to comparison against those from the recorded data. A convenient alternative is to solve a Fokker–Planck equation which has a direct correspondence with the Langevin equations. For our model, this takes the form:

    $$begin{aligned} frac{ partial P(x,y,t)}{partial t}&= frac{partial }{partial x} left{ F_x + D frac{partial }{partial x} right} P(x,y,t) nonumber \&quad +, frac{partial }{partial y} left{ F_y + D frac{partial }{partial y}.right} P(x,y,t) end{aligned}$$
    (4)

    where

    $$begin{aligned} F_x&= -gamma sum _{i} frac{ 2 alpha times (x – x_{i})}{(x – x_{i})^2 + (y – y_{i})^2} nonumber \&quad+, gamma sum _{j} (x – x_{j}) times e^{-( (x – x_{j})^2 + (y – y_{j})^2)} nonumber \ F_y&= -gamma sum _{i} frac{ 2 alpha times (y – y_{i})}{(x – x_{i})^2 + (y – y_{i})^2} nonumber \&quad+ gamma sum _{j} (y – y_{j}) times e^{-( (x – x_{j})^2 + (y – y_{j})^2)} end{aligned}$$
    (5)

    The Fokker–Planck equation describes the evolution of the probabilities of occurrence over a given region. The probability distribution eventually reaches a ‘steady state’ which captures the long-term occurrence probabilities for a given bird, and it does not change beyond this point in time. This steady-state probability distribution can be computed by setting the time derivative term to zero in Eq. (4). The numerical solution of the Fokker–Planck equation involves discretizing the spatial derivatives involved. The steady state probability distribution is consequently obtained on a spatial domain of discretized grids.
    Interestingly, Giuggioli et al.9 considered logarithmic potentials in their work on home range estimation, where an exponent of 8 was found to have a very similar steady state distribution to that from a harmonic potential. Harmonic potential has been utilized in analyzing home ranges of Peromyscus maniculatus10.
    Using the steady-state solution of the Fokker–Planck equation, we compute the mean square displacement averaged over different possible starting locations using the steady state distribution. A discrete version of the mean-square displacement (MSD) can be defined as:

    $$begin{aligned} MSD = sum _i^N langle (x – x_i)^2 + (y – y_i)^2 rangle P_{0}(x_i,y_i) end{aligned}$$
    (6)

    where (P_0(x_i,y_i)) is the distribution of starting locations (x_i) and (y_i) from where displacements are calculated. The inner angular brackets represent a similar weighted average of the mid-points of all grids over the steady-state probability distribution (P_{text {st}}(x,y)). Many of the grids that we define to perform simulations lie outside the known home range of the birds. The probability of choosing a starting location is defined using a Gaussian distribution centred around the nest or the most visited roost site.
    The square root of the MSD defines a characteristic length scale. This could be interpreted as home range length when the steady state distribution is computed over an infinite extent9. A logarithmic potential does not lend itself to such computations since it decays much more slowly such that the characteristic length continues to grow with the size of the area considered. We evaluate the characteristic length scale (L) on a domain that is not much larger in size compared to the observed home range.
    We also calculate L from empirical data by using the probability of occurrence over space inferred from two-dimensional histograms of location data. The MSD in this case is evaluated in the same vein as above but now the displacements from initial locations are weighted over the probabilities of occurrence derived from the histograms. Since these probabilities are only available for each grid, we choose only the mid-points of grids as possible locations to find the result. The starting locations are chosen from a uniform distribution over the mid-points of the grids. This is definitely a crude way of evaluating L but it does give us some way of comparing our numerical solutions against data. Finding a joint-probability distribution over the two dimensions would have been ideal but it is complicated by the fact that the distribution over space is multi-modal owing to multiple roosts for some hornbills. When inferring MSD from the location coordinates directly, it increases before saturating as the sampling frequency is decreased. For very high sampling frequency (or very small time intervals), diffusion effects dominate which leads to an almost linear increase in MSD. The effects of drift are more prominent compared to diffusion for lower sampling frequencies which marks the saturation of the MSD values10.
    A first-passage time model for heterogeneous environments
    The temporal information about an animal’s whereabouts is highly scrambled in the data. An important quantity of interest that could be extracted from movement data is the search time to reach a given target. A very useful measure of search times is the ‘first passage time’. Very generally, first passage time is the time taken for a given state variable to reach a particular value. In the case of animal movement, it can be interpreted as the time taken to reach a particular target location. McKenzie et al.11 derived an interesting first passage time model which had a direct correspondence with a Fokker–Planck equation. We use the prescription of Moorcroft et al.12,13 to estimate the drift and diffusion coefficients. This assumes a movement kernel that is a product of exponential distribution of step lengths and von Mises distribution for the turning angles. (This may be seen in the “goodness of fit tests” section in Methods where we assess fit of our data to claimed distributions.) It can be expressed as:

    $$begin{aligned} K({mathbf{X}} ,{mathbf{X}}’ ,tau )=, & {} frac{1}{rho } f_tau (rho ) k_tau (phi ) end{aligned}$$
    (7)

    $$begin{aligned} {rm{where}},,,,,,,,,,,, ,f_tau (rho )=, & {} lambda e^{-lambda rho }end{aligned}$$
    (8)

    $$begin{aligned} k_tau (phi )=, & {} frac{1}{2 pi I_0(kappa _tau )} exp [kappa _tau cos (phi )] end{aligned}$$
    (9)

    Here, ({mathbf{X}} ), ({mathbf{X}}’ ) denote the current and previous locations respectively, f is the exponential distribution of step lengths (rho ) with rate parameter (lambda ) and mean (bar{rho }_{tau } = 1/lambda ), and (k_{tau }) is the von Mises distribution of turning angles (phi ). (tau ) refers to the time taken to complete a given step. The turning angles are computed with respect to the nest/roost sites. (kappa _tau ) is the concentration parameter of the von Mises distribution which signifies the departure from a uniform distribution of movement directions. The normalizing factor (I_0(kappa _tau )) is a modified Bessel function of the first kind and of zeroth order. The drift and diffusion coefficients can be reliably estimated as:

    $$begin{aligned} gamma= & {} lim _{tau rightarrow 0} frac{bar{rho }_{tau } kappa _tau }{2tau } end{aligned}$$
    (10)

    $$begin{aligned} D= & {} lim _{tau rightarrow 0} frac{bar{{rho _{tau }}^2}}{4tau } end{aligned}$$
    (11)

    Employing the formalism in McKenzie11 to derive the equation for the first passage time T, we obtain the following equation:

    $$begin{aligned}&gamma sum _{i} left{ frac{ 2alpha times ({mathbf{X}} – {mathbf{X}} _{i})}{(x – x_{i})^2 + (y – y_{i})^2} right} cdot nabla T nonumber \&quad -, gamma sum _{j} left{ ({mathbf{X}} – {mathbf{X}} _{j}) e^{-( (x – x_{j})^2 + (y – y_{j})^2)} right} cdot nabla T nonumber \&quad +, D nabla ^2 T + 1 = 0 end{aligned}$$
    (12)

    The terms in dot product with (nabla T) are simply the drift coefficients with spatial dependence.
    McKenzie et al.11 had a simpler version of the first passage time equation that only accounted for bias towards the home range centre. The authors mention that the task of solving the first passage time equation is computationally harder with terms that account for more complex types of heterogeneities. We transform the partial differential equation in (12) into polar coordinates which simplifies the process of solving it (see First Passage Time calculation in Methods). The first passage times obtained from this solution also help us fix the value of (alpha ) in the equation above and subsequently in the logarithmic potential in (3), and in Eqs. (1) and (2). On performing this analysis for different hornbills, we see that (alpha ) = 8 works very well for them irrespective of the species and distribution of heterogeneities around them (see First Passage Time calculation in Methods). First passage times are calculated from the roosting/nesting site that lies closest to the home range centre. In case of GHNBr2, we calculate the first passage times from the approximate home range centre where no roosts exist. This ensures that most points considered for computations lie within the actual extent of the bird’s recorded locations. We used the Minimum Convex Polygon method to estimate the approximate home range centre14. This helped in identifying a location for each bird—which was a roost/nest in most cases—from where first passage times were subsequently computed. The method used for home range estimation is not relevant in the context of our proposed model and results presented, and therefore we do not consider other alternatives. More