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Cited by 665

The DOI matches its Crossref record; 131 of the 131 references it cites were found in a registry or an index.

Lithium Isotope History of Cenozoic Seawater: Changes in Silicate Weathering and Reverse Weathering

Misra, Sambuddha, Froelich, Philip N.·2012·Science

Abstract

Life of Li: Because lithium primarily exists in silicate minerals on continents, the variations of Li isotopes in marine sedimentary rocks reflect the degree of silicate weathering and formation of new sediments on the seafloor, which in turn are largely controlled by climate and tectonic forces over geologic time. By analyzing sedimentary cores from eight drill sites around the world's oceans, Misra and Froelich (p. 818 , published online 26 January; see the cover; see the Perspective by Paytan ) assembled a 68-million-year record of the Li isotope composition of seawater. The record reveals a stepwise change in the Li isotopic ratio, suggesting that several intense episodes of tectonic uplift increased continental weathering rates and delivery of sediments to the oceans. Abrupt swings in the record at specific points in Earth's history, for example, around the time when dinosaurs became extinct, imply major changes in ocean chemistry—but their mechanisms remain enigmatic.

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Metadata

Authors
Misra, S., & Froelich, P. N.
Venue
Science
Published
2012-02-17
Volume
335
Issue
6070
Pages
818-823
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W1984117161
Cited by
665
References
131
FWCI
22.25
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Lithium Isotope History of Cenozoic Seawater: Changes in Silicate Weathering and Reverse Weathering. https://app.cochat.ai/papers/10.1126/science.1214697
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Misra, S., & Froelich, P. N. (2012). Lithium Isotope History of Cenozoic Seawater: Changes in Silicate Weathering and Reverse Weathering. Science. https://doi.org/10.1126/science.1214697

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