Scott, A. The pre-Quaternary history of fire. Palaeogeogr. Palaeoclimatol. Palaeoecol. 164, 281–329 (2000).
Jones, T. P., Ash, S. & Figueiral, I. Late Triassic charcoal from Petrified Forest National Park, Arizona USA. Palaeogeogr. Palaeoclimatol. Palaeoecol. https://doi.org/10.1016/S0031-0182(02)00549-7 (2002).
Uhl, D. & Montenari, M. Charcoal as evidence of palaeo-wildfires in the Late Triassic of SW Germany. Geol. J. 46, 34–41 (2011).
Pointer, R. Fire & Global Change During Key Intervals of the Late Triassic & Early Jurassic with a Focus 325 on the Central Polish Basin (University of Exeter, Exeter, 2018).
Marynowski, L. & Simoneit, B. R. T. Widespread Upper Triassic to Lower Jurassic wildfire records from Poland: Evidence from charcoal and pyrolytic plycylic aromatic hydrocarbons. Palaios 24, 785–798 (2009).
Petersen, H. I. & Lindström, S. Synchronous wildfire activity rise and mire deforestation at the triassic-jurassic boundary. PLoS ONE https://doi.org/10.1371/journal.pone.0047236 (2012).
Whiteside, J. H. et al. Extreme ecosystem instability suppressed tropical dinosaur dominance for 30 million years. Proc. Natl. Acad. Sci. U. S. A. https://doi.org/10.1073/pnas.1505252112 (2015).
Atchley, S. C. et al. A linkage among Pangean tectonism, cyclic alluviation, climate change, and biologic turnover in the Late Triassic: the record from the chinle formation Southwestern United States. J. Sediment. Res. https://doi.org/10.2110/jsr.2013.89 (2014).
Ramezani, J. et al. High-precision U-Pb zircon geochronology of the Late Triassic Chinle Formation, Petrified Forest National Park (Arizona, USA): Temporal constraints on the early evolution of dinosaurs. Bull. Geol. Soc. Am. https://doi.org/10.1130/B30433.1 (2011).
Baranyi, V., Reichgelt, T., Olsen, P. E., Parker, W. G. & Kürschner, W. M. Norian vegetation history and related environmental changes: New data from the Chinle Formation, Petrified Forest National Park (Arizona, SW USA). Bull. Geol. Soc. Am. https://doi.org/10.1130/B31673.1 (2018).
Belcher, C. M. et al. Increased fire activity at the Triassic/Jurassic boundary in Greenland due to climate-driven floral change. Nat. Geosci. 3, 426–429 (2010).
Agee, James K. Fire regimes and approaches for determining fire history. In: Hardy, Colin C.; Arno, Stephen F., eds. The use of fire in forest restoration. Gen. Tech. Rep. INT-GTR-341. Ogden, UT: U.S. Department of Agriculture, Forest Service, Intermountain Research Station, 12–13 (1996)
Morgan, P., Hardy, C. C., Swetnam, T. W., Rollins, M. G. & Long, D. G. Mapping fire regimes across time and space: understanding coarse and fine-scale fire patterns. Int. J. Wildl. Fire 10, 329–342 (2001).
He, T., Belcher, C. M., Lamont, B. B. & Lim, S. L. A 350-million-year legacy of fire adaptation among conifers. J. Ecol. 104, 352–363 (2016).
Lamont, B. B. & He, T. Fire-Proneness as a prerequisite for the evolution of fire-adapted traits. Trends Plant Sci. 22, 278–288 (2017).
Keeley, J. E., Pausas, J. G., Rundel, P. W., Bond, W. J. & Bradstock, R. A. Fire as an evolutionary pressure shaping plant traits. Trends Plant Sci. 16, 406–411 (2011).
Falk, D. A. et al. Multi-scale controls of historical forest-fire regimes: new insights from fire-scar networks. Front Ecol. Environ. https://doi.org/10.1890/100052 (2011).
Marlon, J. R. et al. Long-term perspective on wildfires in the western USA. Proc. Natl. Acad. Sci. USA 109(9), E535–E543. https://doi.org/10.1073/pnas.1112839109 (2012).
Gutsell, S. L. & Johnson, E. A. How fire scars are formed: coupling a disturbance process to its ecological effects. Can. J. For. Res. 26, 166–174 (1996).
Ortloff, W., Goldammer, J. G., Schweingruber, F. H. & Swetnam, T. W. Jahrringanalytische Untersuchungen zur Feuergeschichte eines Bestandes von Pinus ponderosa DOUGL. ex LAWS. in den Santa Rita Mountains, Arizona, USA. Forstarchiv 66, 206–214 (1995).
Byers, B. A., Ash, S. R., Chaney, D. & DeSoto, L. First known fire scar on a fossil tree trunk provides evidence of Late Triassic wildfire. Palaeogeogr. Palaeoclimatol. Palaeoecol. 411, 180–187 (2014).
Arbellay, E., Stoffel, M., Sutherland, E. K., Smith, K. T. & Falk, D. A. Changes in tracheid and ray traits in fire scars of North American conifers and their ecophysiological implications. Ann. Bot. 114, 223–232 (2014).
Arbellay, E., Stoffel, M., Sutherland, E. K., Smith, K. T. & Falk, D. A. Resin duct size and density as ecophysiological traits in fire scars of Pseudotsuga menziesii and Larix occidentalis. Ann. Bot. 114, 973–980 (2014).
Swetnam, T. W. et al. Multi-millennial fire history of the giant forest, Sequoia National Park, California, USA. Fire Ecol. 5, 120–150 (2009).
Brown, P. M. & Swetnam, T. W. A cross-dated fire history from coast redwood near Redwood National Park California. Can. J. For. Res. https://doi.org/10.1139/x94-004 (1994).
Lombardo, K. J., Swetnam, T. W., Baisan, C. H. & Borchert, M. I. Using bigcone Douglas-fir fire scars and tree rings to reconstruct interior chaparral fire history. Fire Ecol. 5, 35–56 (2009).
Lageard, J. G. A., Thomas, P. A. & Chambers, F. M. Using fire scars and growth release in subfossil Scots pine to reconstruct prehistoric fires. Palaeogeogr. Palaeoclimatol. Palaeoecol. 164, 87–99 (2000).
Mutch, L. S. & Swetnam, T. W. Effects of Fire Severity and Climate on Ring-Width Growth of Giant Sequoia After Fire. Symp. Fire Wilderness Park Manag. Past Lessons Futur. Oppor. March 30-April 1, 1993 Missoula, MT Gen Tech Rep INT-GTR-320 Ogden, UT; US Dep. Agric. For. Serv. Intermt. Res. Stn. (1995).
Xu, J., Lu, J., Evans, R. & Downes, G. M. Relationship between ring width and tracheid characteristics in Picea crassifolia: implication in dendroclimatology. BioResources https://doi.org/10.15376/biores.9.2.2203-2213 (2014).
Kitzberger, T., Veblen, T. T. & Villalba, R. Climatic influences on fire regimes along a rain forest-to-xeric woodland gradient in northern Patagonia Argentina. J. Biogeogr. 24, 35–47 (1997).
González, M. E., Veblen, T. T. & Sibold, J. S. Fire history of Araucaria-Nothofagus forests in Villarrica National Park Chile. J. Biogeogr. 32, 1187–1202 (2005).
Littell, J. S., Peterson, D. L., Riley, K. L., Liu, Y. & Luce, C. H. A review of the relationships between drought and forest fire in the United States. Glob. Change Biol. 22, 2353–2369 (2016).
Mundo, I. A., Kitzberger, T., Roig Juñent, F. A., Villalba, R. & Barrera, M. D. Fire history in the Araucaria araucana forests of Argentina: human and climate influences. Int. J. Wildl. Fire 22, 194–206 (2013).
Mundo, I. A., Juñent, F. A. R., Villalba, R., Kitzberger, T. & Barrera, M. D. Araucaria araucana tree-ring chronologies in Argentina: spatial growth variations and climate influences. Trees Struct. Funct. 26, 443–458 (2012).
Abe, H. & Nakai, T. Effect of the water status within a tree on tracheid morphogenesis in Cryptomeria japonica D Don. Trees 14, 124–129 (1999).
DeSoto, L., De la Cruz, M. & Fonti, P. Intra-annual patterns of tracheid size in the Mediterranean tree Juniperus thurifera as an indicator of seasonal water stress. Can. J. For. Res. 41, 1280–1294 (2011).
Martin-Benito, D., Beeckman, H. & Cañellas, I. Influence of drought on tree rings and tracheid features of Pinus nigra and Pinus sylvestris in a mesic Mediterranean forest. Eur. J. For. Res. 132, 33–45 (2013).
Markesteijn, L., Poorter, L., Paz, H., Sack, L. & Bongers, F. Ecological differentiation in xylem cavitation resistance is associated with stem and leaf structural traits. Plant Cell Environ. 34, 137–148 (2011).
Rosner, S. Wood density as a proxy for vulnerability to cavitation: Size matters. J. Plant Hydraul. 4, 001 (2017).
Ash, S. D. The Black Forest Bed, a distinctive rock unit in the Upper Triassic Chinle Formation, northeastern Arizona. Bull. Arizona-Nevada Acad. Sci. 24–25, 59–73 (1992).
Martz, J. W., Kirkland, J. I., Milner, A. R. C., Parker, W. G. & Santucci, V. L. Upper Triassic lithostratigraphy, depositional systems, and vertebrate paleontology across southern Utah. Geol. Intermt. West 4, 99–180 (2017).
Kent, Dennis V., Paul E. Olsen, Cornelia Rasmussen, Christopher Lepre, Roland Mundil, Randall B. Irmis, George E. Gehrels, Dominique Giesler, John W. Geissman, and William G. Parker. Empirical evidence for stability of the 405-kiloyear Jupiter–Venus eccentricity cycle over hundreds of millions of years. Proc. Natl. Acad. Sci. USA. (2018). https://www.pnas.org/content/115/24/6153
Kent, D. V. et al. Magnetochronology of the Entire Chinle Formation (Norian Age) in a Scientific Drill Core from Petrified Forest National Park (Arizona, USA) and Implications for Regional and Global Correlations in the Late Triassic. Geochem. Geophys. Geosyst. 20, 4654–4664 (2019).
Nordt, L., Atchley, S. & Dworkin, S. Collapse of the Late Triassic megamonsoon in western equatorial Pangea, present-day American Southwest. Bull. Geol. Soc. Am. 127, 1798–1815 (2015).
Riggs, N. R., Lehman, T. M., Gehrels, G. E. & Dickinson, W. R. Detrital zircon link between headwaters and terminus of the Upper Triassic Chinle-Dockum Paleoriver System. Science 273, 97–100 (1996).
Dickinson, W. R. & Gehrels, G. E. U-Pb Ages of detrital zircons in relation to paleogeography: Triassic Paleodrainage Networks and sediment dispersal across Southwest Laurentia. J. Sediment. Res. 78, 745–764 (2008).
Ash, S. R. & Creber, G. T. Palaeoclimatic interpretation of the wood structures of the trees in the Chinle Formation (Upper Triassic), Petrified Forest National Park, Arizona USA. Palaeogeogr. Palaeoclimatol. Palaeoecol. 96, 299–317 (1992).
Savidge, R. A. Wood anatomy of Late Triassic trees in Petrified Forest National Park, Arizona, USA, in relation to Araucarioxylon arizonicum Knowlton, 1889. Bull. Geosci. 82, 301–328 (2007).
Ash, S. R. & Creber, G. T. The late Triassic Araucarioxylon arizonicum trees of the Petrified Forest National Park, Arizona, USA. Palaeontology 43, 15–28 (2000).
West, A. G., Nel, J. A., Bond, W. J. & Midgley, J. J. Experimental evidence for heat plume-induced cavitation and xylem deformation as a mechanism of rapid post-fire tree mortality. New Phytol. https://doi.org/10.1111/nph.13979 (2016).
Luthardt, L., Rößler, R. & Schneider, J. W. Tree-ring analysis elucidating palaeo-environmental effects captured in an in situ fossil forest—The last 80 years within an early Permian ecosystem. Palaeogeogr. Palaeoclimatol. Palaeoecol. 487, 278–295 (2017).
Ash, S. R. & Savidge, R. A. The bark of the late triassic Araucarioxylon arizonicum tree from petrified forest National Park Arizona. IAWA J. 25, 349–368 (2004).
Gottesfeld, A. S. Paleoecology of the Lower Part of the Chinle Formation in the Petrified Forest. Museum North. Arizona Bull. 117, 59–73 (1972).
Creber, G. T. & Ash, S. R. The Late Triassic Schilderia adamanica and Woodworthia arizonica trees of the Petrified Forest National Park, Arizona, USA. Palaeontology https://doi.org/10.1111/j.0031-0239.2004.00345.x (2004).
Creber, G. T. & Collinson, M. E. Epicormic shoot traces in the secondary xylem of the Triassic and Permian fossil conifer species Woodworthia arizonica – Short communication. IAWA J. https://doi.org/10.1163/22941932-90000151 (2006).
Axsmith, B. J. & Ash, S. R. Two rare fossil cones from the Upper Triassic Chinle Formation in Petrified Forest National Park, Arizona, and New Mexico. Museum North. Arizona Bull. 62, 82–94 (2006).
He, T., Pausas, J. G., Belcher, C. M., Schwilk, D. W. & Lamont, B. B. Fire-adapted traits of Pinus arose in the fiery Cretaceous. New Phytol. 194, 751–759 (2012).
Midgley, J. & Bond, W. Pushing back in time: The role of fire in plant evolution. New Phytol. 191, 5–7 (2011).
Crisp, M. D., Burrows, G. E., Cook, L. G., Thornhill, A. H. & Bowman, D. M. J. S. Flammable biomes dominated by eucalypts originated at the Cretaceous-Palaeogene boundary. Nat. Commun. https://doi.org/10.1038/ncomms1191 (2011).
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