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Full-Text Articles in Physical Sciences and Mathematics
West Antarctic Ice Sheet Retreat Chronology Of Two Middle-Shelf Grounding-Zone Wedges In Eastern Basin, Ross Sea, Antarctica, Lenora Nicole Copeland
West Antarctic Ice Sheet Retreat Chronology Of Two Middle-Shelf Grounding-Zone Wedges In Eastern Basin, Ross Sea, Antarctica, Lenora Nicole Copeland
LSU Master's Theses
This study isolated a small number of large, in situ and reworked foraminifera from diamicts deposited in two grounding zone wedges on the middle continental shelf in Eastern Basin, Ross Sea, Antarctica. All samples were of sufficient weight to yield Holocene dates if the samples were indeed of Holocene age. Of the twelve small samples sent for radiocarbon analysis, the two heaviest were for reworked foraminifera which yielded dates of >22,200 14C BP and >22,500 14C BP. None of the other ten samples yielded radiocarbon dates. The lack of Holocene radiocarbon dates for the six in situ and four reworked …
Evaluating The Duration Of Post-Lgm Grounding Events In The Glomar Challenger Basin Paleotrough, Eastern Basin Antarctica, Using Sediment Flux Calculations, Boluwatife Owolana
Evaluating The Duration Of Post-Lgm Grounding Events In The Glomar Challenger Basin Paleotrough, Eastern Basin Antarctica, Using Sediment Flux Calculations, Boluwatife Owolana
LSU Master's Theses
Previously acquired geological and geophysical data from the eastern Ross Sea outer shelf support the view that the West Antarctic Ice Sheet (WAIS) deposited three large-volume grounding zone wedges (GZWs) during the relatively short time since the onset of ice sheet retreat began at approximately 11 ka 14C BP. Here, GZW sediment volumes were estimated from seismic data correlations to evaluate the different possible durations of the individual grounding events. The two end-member fluxes used correspond to 1) a modern flux active at Whillans Ice Stream and 2) a larger flux accounting for the larger size of the drainage basin …
Antarctic Plant And Phytoplankton Response To The First Phase Of The Mid Miocene Climatic Optimum At South Mcmurdo Sound, Lee Foersterling
Antarctic Plant And Phytoplankton Response To The First Phase Of The Mid Miocene Climatic Optimum At South Mcmurdo Sound, Lee Foersterling
LSU Master's Theses
The Antarctic Drilling Program (ANDRILL) recovered 1138.54 m of sub-seafloor marine sediments with 98% core recovery at the AND2-2A drill site in South McMurdo Sound. Biostratigraphy, magnetostratigraphy, and isotopic dating (Acton et al., 2008) indicated that an Early to Middle Miocene section (223-1138.54 mbsf) was recovered. This study focuses on an interval with high concentrations of palynomorphs, located between 460.57 and 403.48 mbsf and dated to 16.7 Ma to 16.2 Ma according to the updated Acton et al. (2008) ANDRILL SMS age model. Palynological results show a pronounced increase in organic microfossils between 434.01 and 431.91 mbsf, compared to levels …