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Cited by 736

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Long-Term Sea-Level Fluctuations Driven by Ocean Basin Dynamics

Müller, R. Dietmar, Sdrolias, Maria, Gaina, Carmen, Steinberger, Bernhard, Heine, Christian·2008·Science

Abstract

Earth's long-term sea-level history is characterized by widespread continental flooding in the Cretaceous period (∼145 to 65 million years ago), followed by gradual regression of inland seas. However, published estimates of the Late Cretaceous sea-level high differ by half an order of magnitude, from ∼40 to ∼250 meters above the present level. The low estimate is based on the stratigraphy of the New Jersey margin. By assimilating marine geophysical data into reconstructions of ancient ocean basins, we model a Late Cretaceous sea level that is 170 (85 to 270) meters higher than it is today. We use a mantle convection model to suggest that New Jersey subsided by 105 to 180 meters in the past 70 million years because of North America's westward passage over the subducted Farallon plate. This mechanism reconciles New Jersey margin–based sea-level estimates with ocean basin reconstructions.

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Metadata

Authors
Müller, R. D., Sdrolias, M., Gaina, C., Steinberger, B., & Heine, C.
Venue
Science
Published
2008-03-07
Volume
319
Issue
5868
Pages
1357-1362
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W1993774943
Cited by
736
References
1
FWCI
69.85
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Long-Term Sea-Level Fluctuations Driven by Ocean Basin Dynamics. https://app.cochat.ai/papers/10.1126/science.1151540
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Müller, R. D., Sdrolias, M., Gaina, C., Steinberger, B., & Heine, C. (2008). Long-Term Sea-Level Fluctuations Driven by Ocean Basin Dynamics. Science. https://doi.org/10.1126/science.1151540

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