Werner, Kirstin; Spielhagen, Robert F; Bauch, Dorothea; Hass, H Christian; Kandiano, Evgenia S (2013): Age determination, planktic foraminifera and stable istopes of sediment core MSM05/5_712-2. PANGAEA, https://doi.org/10.1594/PANGAEA.810415, Supplement to: Werner, K et al. (2013): Atlantic Water advection versus sea-ice advances in the eastern Fram Strait during the last 9 ka: Multiproxy evidence for a two-phase Holocene. Paleoceanography, 28(2), 283-295, https://doi.org/10.1002/palo.20028
Always quote above citation when using data! You can download the citation in several formats below.
A sediment core from the West Spitsbergen continental margin was studied to reconstruct climate and paleoceanographic variability during the last ~9 ka in the eastern Fram Strait. Our multiproxy evidence suggests that the establishment of the modern oceanographic configuration in the eastern Fram Strait occurred stepwise, in response to the postglacial sea-level rise and the related onset of modern sea-ice production on the shallow Siberian shelves. The late Early and Mid Holocene interval (9 to 5 ka) was generally characterized by relatively unstable conditions. High abundance of the subpolar planktic foraminifer species Turborotalita quinqueloba implies strong intensity of Atlantic Water (AW) inflow with high productivity and/or high AW temperatures, resulting in a strong heat flux to the Arctic. A series of short-lived cooling events (8.2, 6.9. and 6.1 ka) occurred superimposed on the warm late Early and Mid Holocene conditions. Our proxy data imply that simultaneous to the complete postglacial flooding of Arctic shallow shelves and the initiation of modern sea-ice production, strong advance of polar waters initiated modern oceanographic conditions in the eastern Fram Strait at ~5.2 ka. The Late Holocene was marked by the dominance of the polar planktic foraminifer species Neogloboquadrina pachyderma, a significant expansion of sea ice/icebergs, and strong stratification of the water column. Although planktic foraminiferal assemblages as well as sea surface and subsurface temperatures suggest a return of slightly strengthened advection of subsurface Atlantic Water after 3 ka, a relatively stable cold-water layer prevailed at the sea surface and the study site was probably located within the seasonally fluctuating marginal ice zone during the Neoglacial period.
Latitude: 78.915662 * Longitude: 6.767167
Date/Time Start: 2007-08-04T10:00:00 * Date/Time End: 2007-08-04T10:00:00
Datasets listed in this publication series
- Werner, K; Spielhagen, RF; Bauch, D et al. (2013): Age determination of sediment core MSM05/5_712-2. https://doi.org/10.1594/PANGAEA.810414
- Werner, K; Spielhagen, RF; Bauch, D et al. (2013): Distribution of planktic foraminifera and stable istopes of sediment core MSM05/5_712-2. https://doi.org/10.1594/PANGAEA.770168
- Werner, K; Spielhagen, RF; Bauch, D et al. (2013): Globigerinita spp. in sediment core MSM05/5_712-2. https://doi.org/10.1594/PANGAEA.810636
- Werner, K; Spielhagen, RF; Bauch, D et al. (2013): Grain size analysis of sediment core MSM05/5_712-2. https://doi.org/10.1594/PANGAEA.810417
- Werner, K; Spielhagen, RF; Bauch, D et al. (2013): Granulometry of sediment core MSM05/5_712-2. https://doi.org/10.1594/PANGAEA.733674
- Werner, K; Spielhagen, RF; Bauch, D et al. (2013): Sea surface temperature and salinity calculated for sediment core MSM05/5_712-2. https://doi.org/10.1594/PANGAEA.810418
- Werner, K; Spielhagen, RF; Bauch, D et al. (2013): Sortable silt mean of sediment core MSM05/5_712-2. https://doi.org/10.1594/PANGAEA.810419