Age determination and stable isotope composition of sediment cores from the Arctic Ocean, supplement to: Nørgaard-Pedersen, Niels; Spielhagen, Robert F; Erlenkeuser, Helmut; Grootes, Pieter Meiert; Heinemeier, Jan; Knies, Jochen (2003): Arctic Ocean during the Last Glacial Maximum: atlantic and polar domains of surface water mass distribution and ice cover. Paleoceanography, 18(3), 1063

• Main Authors: Nørgaard-Pedersen, Niels, Spielhagen, Robert F, Erlenkeuser, Helmut, Grootes, Pieter Meiert, Heinemeier, Jan, Knies, Jochen
• Format: Article in Journal/Newspaper
• Language: English
• Published: PANGAEA - Data Publisher for Earth & Environmental Science 2003
• Subjects: GLAMAP; Gravity corer Kiel type; Gravity corer; MultiCorer; Giant box corer; Kasten corer; Fram-I; ODEN-96; ARK-II/4; ARK-III/3; ARK-IV/3; ARK-VII/1; ARK-VIII/2; ARK-VIII/3; ARK-IX/3; ARK-IX/4; ARK-XIII/2; ARK-XIII/3; Ice drift station; Oden; Polarstern; Glacial Atlantic Ocean Mapping GLAMAP2000; Arctic; Arctic Ocean; Barents Sea; Pedersen; Fram Strait; Ice Sheet; Iceberg*; Sea ice
• Online Access: https://dx.doi.org/10.1594/pangaea.735802; https://doi.pangaea.de/10.1594/PANGAEA.735802

On the basis of 52 sediment cores, analyzed and dated at high resolution, the paleoceanography and climate of the Last Glacial Maximum (LGM) were reconstructed in detail for the Fram Strait and the eastern and central Arctic Ocean. Sediment composition and stable isotope data suggest three distinct paleoenvironments: (1) a productive region in the eastern to central Fram Strait and along the northern Barents Sea continental margin characterized by Atlantic Water advection, frequent open water conditions, and occasional local meltwater supply and iceberg calving from the Barents Sea Ice Sheet; (2) an intermediate region in the southwestern Eurasian Basin (up to 84-85°N) and the western Fram Strait characterized by subsurface Atlantic Water advection and recirculation, a moderately high planktic productivity, and a perennial ice cover that breaks up only occasionally; and (3) a central Arctic region (north of 85°N in the Eurasian Basin) characterized by a low-salinity surface water layer and a thick ice cover that strongly reduces bioproduction and bulk sedimentation rates. Although the total inflow of Atlantic Water into the Arctic Ocean may have been reduced during the LGM, its impact on ice coverage and halocline structure in the Fram Strait and southwestern Eurasian Basin was strong.