An astronomical timescale for the Permian-Triassic mass extinction reveals a two-step, million-year-long terrestrial crisis in South China
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L. Shao | D. Bond | J. Hilton | Jing Lu | Juan Wang | Zhiming Yan | Xuetian Wang | Tianchang Zhang | Fanghui Hua
[1] P. Wignall,et al. End Permian to Middle Triassic plant species richness and abundance patterns in South China: Coevolution of plants and the environment through the Permian–Triassic transition , 2022, Earth-Science Reviews.
[2] L. Shao,et al. Diachronous end-Permian terrestrial ecosystem collapse with its origin in wildfires , 2022, Palaeogeography, Palaeoclimatology, Palaeoecology.
[3] S. Grasby,et al. Environmental crises at the Permian–Triassic mass extinction , 2022, Nature Reviews Earth & Environment.
[4] Peter A. Cawood,et al. Anomalous weathering trends indicate accelerated erosion of tropical basaltic landscapes during the Permo-Triassic warming , 2022, Earth and Planetary Science Letters.
[5] D. Erwin,et al. Felsic volcanism as a factor driving the end-Permian mass extinction , 2021, Science advances.
[6] Liu Guoshan,et al. Two pulses of increasing terrestrial input to marine environment during the Permian–Triassic transition , 2021, Palaeogeography, Palaeoclimatology, Palaeoecology.
[7] Zhong‐Qiang Chen,et al. Biotic and palaeoecological variations in the Permian-Triassic boundary microbialite (Xiejiacao, South China): Implication for a two-phase ecological crisis in microbialite ecosystems , 2021, Global and Planetary Change.
[8] K. Kaiho,et al. End-Permian terrestrial disturbance followed by the complete plant devastation, and the vegetation proto-recovery in the earliest-Triassic recorded in coastal sea sediments , 2021 .
[9] Ying Cui,et al. Massive and rapid predominantly volcanic CO2 emission during the end-Permian mass extinction , 2021, Proceedings of the National Academy of Sciences.
[10] Chengshan Wang,et al. Organic carbon burial is paced by a ~173-ka obliquity cycle in the middle to high latitudes , 2021, Science Advances.
[11] K. Angielczyk,et al. Evidence from South Africa for a protracted end-Permian extinction on land , 2021, Proceedings of the National Academy of Sciences.
[12] Zhuo Feng,et al. Intensive Wildfire Associated With Volcanism Promoted the Vegetation Changeover in Southwest China During the Permian−Triassic Transition , 2021, Frontiers in Earth Science.
[13] S. Dai,et al. Environmental perturbations during the latest Permian: Evidence from organic carbon and mercury isotopes of a coal-bearing section in Yunnan Province, southwestern China , 2020 .
[14] L. Shao,et al. Evolution of a plume-influenced source-to-sink system: An example from the coupled central Emeishan large igneous province and adjacent western Yangtze cratonic basin in the Late Permian, SW China , 2020 .
[15] B. Bomfleur,et al. Palynology and vegetation dynamics across the Permian–Triassic boundary in southern Tibet , 2020 .
[16] L. Shao,et al. Sequence stratigraphy, paleogeography, and coal accumulation regularity of major coal-accumulating periods in China , 2020, International Journal of Coal Science & Technology.
[17] Zhuo Feng,et al. From rainforest to herbland: New insights into land plant responses to the end-Permian mass extinction , 2020 .
[18] P. Wignall,et al. Death in the shallows: The record of Permo-Triassic mass extinction in paralic settings, southwest China , 2020, Global and Planetary Change.
[19] D. Kemp,et al. A robust geochronology of the Yangtze River Delta based on magnetostratigraphy and cyclostratigraphy of sediment core ZKA2 , 2020 .
[20] R. Roessler,et al. Late Palaeozoic red beds elucidate fluvial architectures preserving large woody debris in the seasonal tropics of central Pangaea , 2020, Sedimentology.
[21] Gaojun Li,et al. Weathering dynamics of Large Igneous Provinces (LIPs): A case study from the Lesotho Highlands , 2020 .
[22] S. Grasby,et al. Ecological disturbance in tropical peatlands prior to marine Permian-Triassic mass extinction , 2020, Geology.
[23] N. Planavsky,et al. Mercury evidence of intense volcanic effects on land during the Permian-Triassic transition , 2019, Geology.
[24] S. Grasby,et al. Mercury as a proxy for volcanic emissions in the geologic record , 2019, Earth-Science Reviews.
[25] L. Shao,et al. Frequent and intense fires in the final coals of the Paleozoic indicate elevated atmospheric oxygen levels at the onset of the End-Permian Mass Extinction Event , 2019, International Journal of Coal Geology.
[26] Mingsong Li,et al. Acycle: Time-series analysis software for paleoclimate research and education , 2019, Comput. Geosci..
[27] C. Fielding,et al. Age and pattern of the southern high-latitude continental end-Permian extinction constrained by multiproxy analysis , 2019, Nature Communications.
[28] M. Mann,et al. Tracking variable sedimentation rates and astronomical forcing in Phanerozoic paleoclimate proxy series with evolutionary correlation coefficients and hypothesis testing , 2018, Earth and Planetary Science Letters.
[29] Donghai Zhang,et al. Paleomagnetic constraints on the paleogeography of the East Asian blocks during Late Paleozoic and Early Mesozoic times , 2018, Earth-Science Reviews.
[30] D. Erwin,et al. A sudden end-Permian mass extinction in South China , 2018, GSA Bulletin.
[31] L. Shao,et al. SHRIMP zircon U–Pb ages from coal beds across the Permian–Triassic boundary, eastern Yunnan, southwestern China , 2018 .
[32] H. Bucher,et al. Palynofloral associations before and after the Permian–Triassic mass extinction, Kap Stosch, East Greenland , 2017 .
[33] Chao Ma,et al. Theory of chaotic orbital variations confirmed by Cretaceous geological evidence , 2017, Nature.
[34] L. Hinnov,et al. Astronomical tuning of the end-Permian extinction and the Early Triassic Epoch of South China and Germany , 2016 .
[35] Xiao-Lei Liu,et al. The terrestrial end-Permian mass extinction in South China , 2016 .
[36] D. Erwin,et al. High-resolution SIMS oxygen isotope analysis on conodont apatite from South China and implications for the end-Permian mass extinction , 2016 .
[37] Daoliang Chu,et al. Vegetation changeover across the Permian–Triassic Boundary in Southwest China: Extinction, survival, recovery and palaeoclimate: A critical review , 2015 .
[38] Jianxin Yu,et al. Terrestrial paleoenvironment characterization across the Permian-Triassic boundary in South China , 2015 .
[39] Yigang Xu,et al. Triggers of Permo-Triassic boundary mass extinction in South China: The Siberian Traps or Paleo-Tethys ignimbrite flare-up? , 2014 .
[40] M. Benton,et al. Impacts of global warming on Permo-Triassic terrestrial ecosystems , 2014 .
[41] S. Bowring,et al. High-precision timeline for Earth’s most severe extinction , 2014, Proceedings of the National Academy of Sciences.
[42] L. Hinnov. Cyclostratigraphy and its revolutionizing applications in the earth and planetary sciences , 2013 .
[43] L. Hinnov,et al. Time-calibrated Milankovitch cycles for the late Permian , 2013, Nature Communications.
[44] Shao Long-y. Sequence-Palaeogeography and Coal Aaccumulation of Late Permian in Southwestern China , 2013 .
[45] P. Wignall,et al. Two pulses of extinction during the Permian–Triassic crisis , 2012, Nature Geoscience.
[46] D. Erwin,et al. Calibrating the End-Permian Mass Extinction , 2011, Science.
[47] L. Hinnov,et al. Did the great dying of life take 700 k.y.? Evidence from global astronomical correlation of the Permian-Triassic boundary interval , 2011 .
[48] B. Jones,et al. Multiple Early Triassic greenhouse crises impeded recovery from Late Permian mass extinction , 2011 .
[49] C. Xiong,et al. Permian–Triassic land-plant diversity in South China: Was there a mass extinction at the Permian/Triassic boundary? , 2011, Paleobiology.
[50] J. Pearce. Geochemical fingerprinting of oceanic basalts with applications to ophiolite classification and the search for Archean oceanic crust , 2008 .
[51] R. Pancost,et al. Changes in the global carbon cycle occurred as two episodes during the Permian–Triassic crisis , 2007 .
[52] Yigang Xu,et al. Distinct mantle sources of low-Ti and high-Ti basalts from the western Emeishan large igneous province, SW China: implications for plume–lithosphere interaction , 2004 .
[53] G. M. Young,et al. Behavior of major and trace elements (including REE) during Paleoproterozoic pedogenesis and diagenetic alteration of an Archean granite near Ville Marie, Québec, Canada , 2000 .
[54] G. M. Young,et al. Unraveling the effects of potassium metasomatism in sedimentary rocks and paleosols, with implications for paleoweathering conditions and provenance , 1995 .
[55] N. Schofield,et al. Effects of partial deforestation on hydrology and salinity in high salt storage landscapes. II. Strip, soils and parkland clearing , 1991 .
[56] W. McDonough,et al. Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes , 1989, Geological Society, London, Special Publications.
[57] J. Winchester,et al. Geochemical discrimination of different magma series and their differentiation products using immobile elements , 1977 .