Stable carbon and oxygen isotope ratios of foraminifera and organic carbon of ODP Hole 188-1167A (Table 2)

• Main Authors: Theissen, Kevin M, Dunbar, Robert G, Cooper, Alan K, Mucciarone, David A, Hoffmann, Dirk L
• Format: Dataset
• Language: English
• Published: PANGAEA 2003
• Subjects: 188-1167A; Carbon; organic; total; DEPTH; sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Element analyser CNS; Carlo Erba NA1500; Globocassidulina crassa; δ13C; δ18O; Joides Resolution; Leg188; Mass spectrometer Finnigan Delta Plus; Mass spectrometer Finnigan MAT 252; Neogloboquadrina pachyderma sinistral; Ocean Drilling Program; ODP; Prydz Bay; Sample code/label; organic carbon; Amery Ice Shelf; Antarc*; Antarctic; Antarctica; East Antarctica; Ice Sheet; Ice Shelf; Lambert Glacier; Neogloboquadrina pachyderma
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.742618; https://doi.org/10.1594/PANGAEA.742618

Ocean Drilling Program Leg 188, Prydz Bay, East Antarctica is part of a larger initiative to explore the Cenozoic history of the Antarctic Ice Sheet through direct drilling and sampling of the continental margins. In this paper, we present stable isotopic results from Ocean Drilling Program (ODP) Site 1167 located on the Prydz Channel Trough Mouth Fan (TMF), the first Antarctic TMF to be drilled. The foraminifer-based d18O record is interpreted along with sedimentary and downhole logging evidence to reconstruct the Quaternary glacial history of Prydz Bay and the adjacent Lambert Glacier Amery Ice Shelf System (LGAISS). We report an electron spin resonance age date of 36.9±3.3 ka at 0.45 m below sea floor and correlate suspected glacial–interglacial cycles with the global isotopic stratigraphy to improve the chronology for Site 1167. The d18O record based on planktonic (Neogloboquadrina pachyderma (s.)) and limited benthic results (Globocassidulina crassa), indicates a trend of ice sheet expansion that was interrupted by a period of reduced ice volume and possibly warmer conditions during the early–mid-Pleistocene (0.9–1.38 Ma). An increase in d18O values after ~900 ka appears to coincide with the mid-Pleistocene climate transition and the expansion of the northern hemisphere ice sheet. The d18O record in the upper 50 m of the stratigraphic section indicates as few as three glacial–interglacial cycles, tentatively assigned as marine isotopic stages (MIS) 16–21, are preserved since the Brunhes/Matuyama paleomagnetic reversal (780 ka). This suggests that there is a large unconformity near the top of the section and/or that there may have been few extreme advances of the ice sheet since the mid-Pleistocene climate transition resulting in lowered sedimentation rates on the Prydz Channel TMF. The stable isotopic record from Site 1167 is one of the few available from the area south of the Antarctic Polar Front that has been linked with the global isotopic stratigraphy. Our results suggest the potential for the recovery ...