(Table 1) Age control points of sediment cores JM97-948/2A and MD95-2011, supplement to: Andersson, Carin; Risebrobakken, Bjørg; Jansen, Eystein; Dahl, Svein Olaf (2003): Late Holocene surface ocean conditions of the Norwegian Sea (Voring Plateau). Paleoceanography, 18(2), 1044

• Main Authors: Andersson, Carin, Risebrobakken, Bjørg, Jansen, Eystein, Dahl, Svein Olaf
• Format: Dataset
• Language: English
• Published: PANGAEA - Data Publisher for Earth & Environmental Science 2003
• Subjects: Event label; DEPTH, sediment/rock; Age, dated; Age, dated standard deviation; Calendar age; Age, minimum/young; Age, maximum/old; Age, comment; Giant box corer; Calypso Corer; Age, 14C AMS; MD101; Marion Dufresne 1995; Norwegian Sea; Vøring Plateau; Fennoscandian; Neogloboquadrina pachyderma; North Atlantic
• Online Access: https://dx.doi.org/10.1594/pangaea.841543; https://doi.pangaea.de/10.1594/PANGAEA.841543

Late Holocene sea surface ocean conditions of the eastern Norwegian Sea (Vøring Plateau) are inferred from planktic stable isotopes and planktic foraminiferal assemblage changes in cores JM97-948/2A and MD95-2011 (66.97°N, 7.64°E). Strong covariance between the planktic stable oxygen isotopic record and abundance changes of N. pachyderma (sin) show that major changes in surface ocean conditions are reflected both in the geochemical composition of the foraminiferal tests as well as in the composition of the foraminiferal fauna. Surface ocean conditions warmer than present were common during the past 3000 years. During the so-called Medieval Warm Period, surface conditions were highly variable with marked changes in sea surface temperature. The warmest sea surface temperatures during this period occurred between 800 and 550 years BP (0 BP = AD 2000). Climatic deterioration, recorded as decreases in sea surface temperature, occurred at about 2750, 1550, 400, and 100 years BP. The cooling events at about 2750 and 1550 years BP appear to correlate with increases in ice-rafted debris in the North Atlantic. Based on the results from JM97-948/2A and MD95-2011, the onset of the Little Ice Age cooling trend seems to have occurred around 700-600 years BP. Faunal changes indicate two cooling events during the Little Ice Age (at 400 and 100 years BP) that correspond to decreases in Fennoscandian summer temperatures and increases in ice-rafted debris in the eastern North Atlantic. : AMS dating on the planktonic foraminifer Neogloboquadrina pachyderma (dextral). Radiocarbon ages were calibrated using CALIB 4.3 in conjunction with INTCAL98 (Stuiver et al., 1998). A 400-year correction for the marine reservoir effect was applied. Samples KIA5600 and KIA3927 not used in the age-depth model.