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An extraterrestrial trigger for the mid-Ordovician ice age: Dust from the breakup of the L-chondrite parent body
Schmitz, Birger1; Farley, Kenneth A.2; Goderis, Steven3; Heck, Philipp R.4,5; Bergstrom, Stig M.6; Boschi, Samuele1; Claeys, Philippe7; Debaille, Vinciane8; Dronov, Andrei9,10; van Ginneken, Matthias11
刊名SCIENCE ADVANCES
2019-09-01
卷号5期号:9页码:10
ISSN号2375-2548
DOI10.1126/sciadv.aax4184
通讯作者Schmitz, Birger(birger.schmitz@nuclear.lu.se)
英文摘要The breakup of the L-chondrite parent body in the asteroid belt 466 million years (Ma) ago still delivers almost a third of all meteorites falling on Earth. Our new extraterrestrial chromite and He-3 data for Ordovician sediments show that the breakup took place just at the onset of a major, eustatic sea level fall previously attributed to an Ordovician ice age. Shortly after the breakup, the flux to Earth of the most fine-grained, extraterrestrial material increased by three to four orders of magnitude. In the present stratosphere, extraterrestrial dust represents 1% of all the dust and has no climatic significance. Extraordinary amounts of dust in the entire inner solar system during >2 Ma following the L-chondrite breakup cooled Earth and triggered Ordovician icehouse conditions, sea level fall, and major faunal turnovers related to the Great Ordovician Biodiversification Event.
WOS关键词ASTEROID BREAKUP ; OXYGEN-ISOTOPE ; SPARGING OSO4 ; NOBLE-GASES ; BIODIVERSIFICATION ; RECORD ; EARTH ; CHEMOSTRATIGRAPHY ; MICROMETEORITES ; METEORITES
WOS研究方向Science & Technology - Other Topics
语种英语
出版者AMER ASSOC ADVANCEMENT SCIENCE
WOS记录号WOS:000491128800054
内容类型期刊论文
源URL[http://libir.pmo.ac.cn/handle/332002/28278]  
专题中国科学院紫金山天文台
通讯作者Schmitz, Birger
作者单位1.Lund Univ, Dept Phys, Astrogeobiol Lab, Lund, Sweden
2.CALTECH, Div Geol & Planetary Sci, Pasadena, CA 91125 USA
3.Vrije Univ Brussel, Dept Chem, Brussels, Belgium
4.Robert A Pritzker Ctr Meteorit & Polar Studies, Field Museum Nat Hist, Chicago, IL USA
5.Univ Chicago, Dept Geophys Sci, Chicago, IL USA
6.Ohio State Univ, Sch Earth Sci, Columbus, OH 43210 USA
7.Vrije Univ Brussel, Analyt Environm & GeoChem, Brussels, Belgium
8.Univ Libre Bruxelles, Lab GTime, Brussels, Belgium
9.Russian Acad Sci, Geol Inst, Moscow, Russia
10.Kazan Volga Reg Fed Univ, Inst Geol & Oil & Gas Technol, Kazan, Russia
推荐引用方式
GB/T 7714
Schmitz, Birger,Farley, Kenneth A.,Goderis, Steven,et al. An extraterrestrial trigger for the mid-Ordovician ice age: Dust from the breakup of the L-chondrite parent body[J]. SCIENCE ADVANCES,2019,5(9):10.
APA Schmitz, Birger.,Farley, Kenneth A..,Goderis, Steven.,Heck, Philipp R..,Bergstrom, Stig M..,...&Terfelt, Fredrik.(2019).An extraterrestrial trigger for the mid-Ordovician ice age: Dust from the breakup of the L-chondrite parent body.SCIENCE ADVANCES,5(9),10.
MLA Schmitz, Birger,et al."An extraterrestrial trigger for the mid-Ordovician ice age: Dust from the breakup of the L-chondrite parent body".SCIENCE ADVANCES 5.9(2019):10.
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