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The record of Pliocene sea-level change at Enewetak Atoll

Bruce R. Wardlaw·T. M. Quinn
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Abstract

Detailed seismic stratigraphy, lithostratigraphy, and chemostratigraphy indicate that atoll-wide subaerial exposure surfaces (major disconformities) developed during major sea-level lowstands form prominent seismic reflectors and are coincident with biostratigraphic breaks in the Plio-Pleistocene on Enewetak Atoll. Sea-level models based on the stratigraphic position and age of major disconformities suggest a maximum sea-level highstand elevation of 36 m above present sea level and a maximum sea-level lowstand elevation of 63 m below present sea level for the Pliocene.

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Quaternary Science ReviewsArticle
90° N90° S · 180° W ← longitude → 180° E
Source-reported bounding extent: 11.323029792807546° to 11.687677837348588° latitude; 162.11685789055355° to 162.41351792864384° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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Bruce R. Wardlaw, T. M. Quinn. 1991. The record of Pliocene sea-level change at Enewetak Atoll. https://doi.org/10.1016/0277-3791(91)90023-n

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