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DOI10.1126/science.aat1327
Temperature-dependent hypoxia explains biogeography and severity of end-Permian marine mass extinction
Penn J.L.; Deutsch C.; Payne J.L.; Sperling E.A.
发表日期2018
ISSN0036-8075
卷号362期号:6419
英文摘要Rapid climate change at the end of the Permian Period (~252 million years ago) is the hypothesized trigger for the largest mass extinction in Earth’s history. We present model simulations of the Permian/Triassic climate transition that reproduce the ocean warming and oxygen (O2) loss indicated by the geologic record. The effect of these changes on animal survival is evaluated using the Metabolic Index (F), a measure of scope for aerobic activity governed by organismal traits sampled in diverse modern species. Modeled loss of aerobic habitat predicts lower extinction intensity in the tropics, a pattern confirmed with a spatially explicit analysis of the marine fossil record. The combined physiological stresses of ocean warming and O2 loss can account for more than half the magnitude of the “Great Dying.” 2017 © The Authors.
英文关键词oxygen; animal community; biogeography; climate change; fossil record; geological record; hypoxic conditions; index method; marine environment; mass extinction; Permian; Permian-Triassic boundary; physiological response; survival; Triassic; aerobic capacity; aerobic metabolism; Article; astronomy; biodiversity; biogeography; carbon footprint; climate change; ecophysiology; end Permian mass extinction; fossil; geochemical analysis; greenhouse effect; greenhouse gas; hypoxia; marine environment; marine fossil; marine species; metabolic index; metabolic parameters; nonhuman; oxygen consumption; oxygen supply; physical tolerance; prediction; priority journal; sea surface temperature; species difference; species habitat; survival rate; temperature dependence; anaerobic growth; animal; aquatic species; climate change; greenhouse effect; heat; metabolism; species extinction; Animalia; Anaerobiosis; Animals; Aquatic Organisms; Biodiversity; Climate Change; Extinction, Biological; Greenhouse Effect; Hot Temperature; Oxygen
语种英语
来源期刊Science
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/245039
作者单位School of Oceanography, University of Washington, Seattle, WA 98195, United States; Department of Biology, University of Washington, Seattle, WA 98195, United States; Department of Geological Sciences, Stanford University, Stanford, CA 94305, United States
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Penn J.L.,Deutsch C.,Payne J.L.,et al. Temperature-dependent hypoxia explains biogeography and severity of end-Permian marine mass extinction[J],2018,362(6419).
APA Penn J.L.,Deutsch C.,Payne J.L.,&Sperling E.A..(2018).Temperature-dependent hypoxia explains biogeography and severity of end-Permian marine mass extinction.Science,362(6419).
MLA Penn J.L.,et al."Temperature-dependent hypoxia explains biogeography and severity of end-Permian marine mass extinction".Science 362.6419(2018).
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