title: Late wisconsinan sea levels on the southeast u.s. Atlantic shelf based on in-place shoreline indicators.
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.
authors.forename: B W
authors.initials: BW
authors.lastname: Blackwelder
authors.forename: O H
authors.initials: OH
authors.lastname: Pilkey
authors.forename: J D
authors.initials: JD
authors.lastname: Howard