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Evolution of the Ratio of Strontium-87 to Strontium-86 in Seawater from Cretaceous to Present

Hess, Jennifer, Bender, Michael L., Schilling, Jean-Guy·1986·Science

Abstract

A detailed record of the strontium-87 to strontium-86 ratio in seawater during the last 100 million years was determined by measuring this ratio in 137 well-preserved and well-dated fossil foraminifera samples. Sample preservation was evaluated from scanning electron microscopy studies, measured strontium-calcium ratios, and pore water strontium isotope ratios. The evolution of the strontium isotopic ratio in seawater offers a means to evaluate long-term changes in the global strontium isotope mass balance. Results show that the marine strontium isotope composition can be used for correlating and dating well-preserved authigenic marine sediments throughout much of the Cenozoic to a precision of ±1 million years. The strontium-87 to strontium-86 ratio in seawater increased sharply across the Cretaceous/Tertiary boundary, but this feature is not readily explained as strontium input from a bolide impact on land.

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Metadata

Authors
Hess, J., Bender, M. L., & Schilling, J.-G.
Venue
Science
Published
1986-02-28
Volume
231
Issue
4741
Pages
979-984
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W1968545963
Cited by
444
References
0
FWCI
21.70
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Evolution of the Ratio of Strontium-87 to Strontium-86 in Seawater from Cretaceous to Present. https://app.cochat.ai/papers/10.1126/science.231.4741.979
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Hess, J., Bender, M. L., & Schilling, J.-G. (1986). Evolution of the Ratio of Strontium-87 to Strontium-86 in Seawater from Cretaceous to Present. Science. https://doi.org/10.1126/science.231.4741.979

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