Freshwater peat on the continental shelf

K.O. Emery; R. L. Wigley; A.S. Bartlett; M. Rubin; E.S. Barghoorn

doi:10.1126/science.158.3806.1301

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Freshwater peat on the continental shelf

K.O. Emery·R. L. Wigley·A.S. Bartlett·M. Rubin·E.S. Barghoorn

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Abstract

Freshwater peats from the continental shelf off northeastern United States contain the same general pollen sequence as peats from ponds that are above sea level and that are of comparable radiocarbon ages. These peats indicate that during glacial times of low sea level terrestrial vegetation covered the region that is now the continental shelf in an unbroken extension from the adjacent land areas to the north and west.

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Source-reported bounding extent: 37.67242518679933° to 45.59295017118643° latitude; -75.98845493237955° to -66.84637765114445° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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K.O. Emery, R. L. Wigley, A.S. Bartlett, M. Rubin, E.S. Barghoorn. 1967. Freshwater peat on the continental shelf. https://doi.org/10.1126/science.158.3806.1301

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