Isotopic and micropaleontological record of sediments of the Baffin Bay

• Main Authors: Hillaire-Marcel, Claude, de Vernal, Anne, Aksu, Ali E, Macko, Stephen A
• Format: Other/Unknown Material
• Language: English
• Published: PANGAEA 1989
• Subjects: 105-645; Baffin Bay; COMPCORE; Composite Core; HUD76-029-033; HUD85-027-16; HUD85-027-16TC; Hudson Bay; Joides Resolution; Labrador Sea; Leg105; Ocean Drilling Program; ODP; PC; Piston corer; TC; Trigger corer; Baffin; Ice Sheet; Neogloboquadrina pachyderma; Sea ice
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.744850; https://doi.org/10.1594/PANGAEA.744850

The oxygen and carbon isotopic compositions of the planktonic foraminifer, Neogloboquadrina pachyderma (sinistral), were determined at 20-cm intervals through the 'composite' top ~ 22 m of sediments at ODP Site 645 (Holes 645B, 645C, 645F, and 645G) and at 10-cm intervals through a 9-m piston core (85-027-016) collected during the Hudson site survey. Quantitative analyses of palynomorphs, notably dinocysts, and of planktonic foraminifers were performed. Organic and nitrogen contents and isotopic composition of nitrogen and carbon in organic matter also were determined. These data provide a high-resolution record of changes that occurred in surface-water masses during the last glacial cycle in Baffin Bay. The basin experienced low planktonic productivity during most of the late Pleistocene, either from dilution in surface water by meltwater discharges from the surrounding ice-sheet or from the presence of a relatively dense sea-ice cover. Peaks of meltwater discharge are indicated by d18O values as low as about 1.5 per mil, correlative d13C- d18O shifts, low concentration of planktonic foraminifers, high concentrations of glacially reworked pre-Quaternary palynomorphs, and low-salinity dinocyst assemblages. As a whole, d18O values ranging between 4.5 and 2.5 per mil allow the establishment of an 18O stratigraphy spanning isotopic stages 5 to 1. Because of the poor core recovery, the general paucity of microflora and microfauna, and the possible occurrence of slumping or debris flow at Site 645, further interpretation remains problematic.