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Cited by 704

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Worldwide Initiation of Holocene Marine Deltas by Deceleration of Sea-Level Rise

Stanley, Daniel Jean, Warne, Andrew G.·1994·Science

Abstract

Radiocarbon-dated deltaic sequences of Holocene age from different parts of the world began to accumulate within a restricted time range, from about 8500 to 6500 years ago. Evaluation of major delta processes indicates that deceleration in sea-level rise was the key factor in Holocene delta formation. Within many deltas, there is as much as a 2000-year age range between basal deposits in seaward and landward cores. This age difference records the progressive landward migration of near mean sea-level depositional environments during the lower to mid-Holocene. Establishment of a chronostratigraphic framework for Holocene delta development provides a fundamental global baseline for distinguishing sea-level change from vertical land motion by tectonism and isostasy, and for evaluating rates of future marine incursion into low-lying deltas.

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Metadata

Authors
Stanley, D. J., & Warne, A. G.
Venue
Science
Published
1994-07-08
Volume
265
Issue
5169
Pages
228-231
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W2084014771
Cited by
704
References
0
FWCI
14.92
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Worldwide Initiation of Holocene Marine Deltas by Deceleration of Sea-Level Rise. https://app.cochat.ai/papers/10.1126/science.265.5169.228
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Stanley, D. J., & Warne, A. G. (1994). Worldwide Initiation of Holocene Marine Deltas by Deceleration of Sea-Level Rise. Science. https://doi.org/10.1126/science.265.5169.228

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.