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Eugene W. Domack

Researcher at University of South Florida

Publications -  119
Citations -  8837

Eugene W. Domack is an academic researcher from University of South Florida. The author has contributed to research in topics: Ice shelf & Glacial period. The author has an hindex of 53, co-authored 119 publications receiving 8220 citations. Previous affiliations of Eugene W. Domack include Rice University & University of South Florida St. Petersburg.

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Late Pleistocene–Holocene retreat of the West Antarctic Ice-Sheet system in the Ross Sea: Part 1—Geophysical results

TL;DR: In this paper, a high-resolution database of the Ross Sea seafloor has been used for the reconstruction of the last glacial maximum and the relative retreat history of the ice sheet.
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Late Pleistocene–Holocene retreat of the West Antarctic Ice-Sheet system in the Ross Sea: Part 2—Sedimentologic and stratigraphic signature

TL;DR: Sedimentologic, geotechnical, geochemical and accelerator mass spectrometer (AMS) radiocarbon data from two marine geologic cruises in the Ross Sea have allowed us to constrain facies relationships and temporal changes in the West Antarctic Ice Sheet.
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Stability of the Larsen B ice shelf on the Antarctic Peninsula during the Holocene epoch

TL;DR: It is suggested that the recent prolonged period of warming in the Antarctic Peninsula region, in combination with the long-term thinning of the Larsen B ice shelf has led to collapse of the ice shelf.
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Marine Ecosystem Sensitivity to Climate Change

TL;DR: In this paper, the authors summarize the available data on climate variability and trends in the western Antarctic Peninsula (WAP) region and discuss these data in the context of long-term climate variability during the last 8000 years of the Holocene.
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A community-based geological reconstruction of Antarctic Ice Sheet deglaciation since the Last Glacial Maximum

Michael J. Bentley, +76 more
TL;DR: In this paper, the authors present a series of timeslice maps for 20 ka, 15 ka, 10 ka and 5 ka, including grounding line position and ice sheet thickness changes, along with a clear assessment of levels of confidence.