Late Wisconsinan sea levels on the Southeast U.S. Atlantic shelf based on in-place shoreline indicators

B. W. Blackwelder; O. H. Pilkey; J.D. Howard

doi:10.1126/science.204.4393.618

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Late Wisconsinan sea levels on the Southeast U.S. Atlantic shelf based on in-place shoreline indicators

B. W. Blackwelder·O. H. Pilkey·J.D. Howard

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Abstract

A new interpretation of late Pleistocene sea levels on the U.S. Atlantic continental shelf is based on in-place lagoonal and salt-marsh sediments obtained from vibra-cores. These data show sea levels during the last Wisconsinan transgression were about 30 meters shallower than is indicated by existing sea-level curves.

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Source-reported bounding extent: 24.91122077853049° to 45.29761605168801° latitude; -82.21484429397967° to -66.62540461052978° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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B. W. Blackwelder, O. H. Pilkey, J.D. Howard. 1979. Late Wisconsinan sea levels on the Southeast U.S. Atlantic shelf based on in-place shoreline indicators. https://doi.org/10.1126/science.204.4393.618

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