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DOI10.1126/science.aap8525
Postimpact earliest Paleogene warming shown by fish debris oxygen isotopes (El Kef, Tunisia)
MacLeod K.G.; Quinton P.C.; Sepúlveda J.; Negra M.H.
发表日期2018
ISSN0036-8075
起始页码1467
结束页码1469
卷号360期号:6396
英文摘要Greenhouse warming is a predicted consequence of the Chicxulub impact, but supporting data are sparse. This shortcoming compromises understanding of the impact’s effects, and it has persisted due to an absence of sections that both contain suitable material for traditional carbonate- or organic-based paleothermometry and are complete and expanded enough to resolve changes on short time scales. We address the problem by analyzing the oxygen isotopic composition of fish debris, phosphatic microfossils that are relatively resistant to diagenetic alteration, from the Global Stratotype Section and Point for the Cretaceous/Paleogene boundary at El Kef, Tunisia. We report an ~1 per mil decrease in oxygen isotopic values (~5°C warming) beginning at the boundary and spanning ~300 centimeters of section (~100,000 years). The pattern found matches expectations for impact-initiated greenhouse warming. 2017 © The Authors.
英文关键词carbonic acid; oxygen 18; phosphate; oxygen; Cretaceous; Cretaceous-Paleogene boundary; diagenesis; isotopic composition; microfossil; oxygen isotope; Paleogene; warming; animal tissue; Article; environmental impact; environmental impact assessment; fish; greenhouse effect; microfossil; molecular genetics; nonhuman; Paleogene; priority journal; thermometry; Tunisia; warming; animal; fish; fossil; species extinction; temperature; Kef; Tunisia; Animals; Extinction, Biological; Fishes; Fossils; Global Warming; Greenhouse Effect; Oxygen Isotopes; Temperature; Tunisia
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/244613
作者单位Department of Geological Sciences, University of Missouri, Columbia, MO, United States; Department of Geology, SUNY Potsdam, Potsdam, NY, United States; Department of Geological Sciences, Institute of Arctic and Alpine Research, University of Colorado Boulder, Boulder, CO, United States; Department of Geology, Faculty of Sciences of Tunis, University of Tunis El Manar, 2092 Manar II, Tunis, Tunisia
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MacLeod K.G.,Quinton P.C.,Sepúlveda J.,et al. Postimpact earliest Paleogene warming shown by fish debris oxygen isotopes (El Kef, Tunisia)[J],2018,360(6396).
APA MacLeod K.G.,Quinton P.C.,Sepúlveda J.,&Negra M.H..(2018).Postimpact earliest Paleogene warming shown by fish debris oxygen isotopes (El Kef, Tunisia).Science,360(6396).
MLA MacLeod K.G.,et al."Postimpact earliest Paleogene warming shown by fish debris oxygen isotopes (El Kef, Tunisia)".Science 360.6396(2018).
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