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DOI10.1126/science.adg1366
Oxygen isotope ensemble reveals Earth's seawater, temperature, and carbon cycle history
Isson, Terry; Rauzi, Sofia
发表日期2024
ISSN0036-8075
EISSN1095-9203
起始页码383
结束页码6683
卷号383期号:6683
英文摘要Earth's persistent habitability since the Archean remains poorly understood. Using an oxygen isotope ensemble approach-comprising shale, iron oxide, carbonate, silica, and phosphate records-we reconcile a multibillion-year history of seawater delta O-18, temperature, and marine and terrestrial clay abundance. Our results reveal a rise in seawater delta O-18 and a temperate Proterozoic climate distinct to interpretations of a hot early Earth, indicating a strongly buffered climate system. Precambrian sediments are enriched in marine authigenic clay, with prominent reductions occurring in concert with Paleozoic and Cenozoic cooling, the expansion of siliceous life, and the radiation of land plants. These findings support the notion that shifts in the locus and extent of clay formation contributed to seawater O-18 enrichment, clement early Earth conditions, major climate transitions, and climate stability through the reverse weathering feedback.
语种英语
WOS研究方向Science & Technology - Other Topics
WOS类目Multidisciplinary Sciences
WOS记录号WOS:001183256400027
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/292120
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Isson, Terry,Rauzi, Sofia. Oxygen isotope ensemble reveals Earth's seawater, temperature, and carbon cycle history[J],2024,383(6683).
APA Isson, Terry,&Rauzi, Sofia.(2024).Oxygen isotope ensemble reveals Earth's seawater, temperature, and carbon cycle history.SCIENCE,383(6683).
MLA Isson, Terry,et al."Oxygen isotope ensemble reveals Earth's seawater, temperature, and carbon cycle history".SCIENCE 383.6683(2024).
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