Not logged in
PANGAEA.
Data Publisher for Earth & Environmental Science

Riethdorf, Jan-Rainer; Nürnberg, Dirk; Max, Lars; Tiedemann, Ralf; Gorbarenko, Sergey A; Malakhov, Mikhail I (2013): Stable isotopes, core logging data, relative paleointensity, dry bulk density, biogenic opal, CN-data (TC, TOC, CaCO3, TN), element concentrations, and coarse fraction of three sediment cores from the western Bering Sea [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.786307, Supplement to: Riethdorf, J-R et al. (2013): Millennial-scale variability of marine productivity and terrigenous matter supply in the western Bering Sea over the past 180 kyr. Climate of the Past, 9(3), 1345-1373, https://doi.org/10.5194/cp-9-1345-2013

Always quote citation above when using data! You can download the citation in several formats below.

RIS CitationBibTeX CitationShow MapGoogle Earth

Abstract:
We used piston cores recovered in the western Bering Sea to reconstruct millennial-scale changes in marine productivity and terrigenous matter supply over the past ~180 kyr. Based on a geochemical multi-proxy approach, our results indicate closely interacting processes controlling marine productivity and terrigenous matter supply comparable to the situation in the Okhotsk Sea. Overall, terrigenous inputs were high, whereas export production was low. Minor increases in marine productivity occurred during intervals of Marine Isotope Stage 5 and interstadials, but pronounced maxima were recorded during interglacials and Termination I. The terrigenous material is suggested to be derived from continental sources on the eastern Bering Sea shelf and to be subsequently transported via sea ice, which is likely to drive changes in surface productivity, terrigenous inputs, and upper-ocean stratification. From our results we propose glacial, deglacial, and interglacial scenarios for environmental change in the Bering Sea. These changes seem to be primarily controlled by insolation and sea-level forcing which affect the strength of atmospheric pressure systems and sea-ice growth. The opening history of the Bering Strait is considered to have had an additional impact. High-resolution core logging data (color b*, XRF scans) strongly correspond to the Dansgaard-Oeschger climate variability registered in the NGRIP ice core and support an atmospheric coupling mechanism of Northern Hemisphere climates.
Coverage:
Median Latitude: 57.367867 * Median Longitude: 170.249387 * South-bound Latitude: 53.881667 * West-bound Longitude: 162.089667 * North-bound Latitude: 58.875333 * East-bound Longitude: 170.698833
Date/Time Start: 2009-09-09T00:06:00 * Date/Time End: 2009-09-22T00:06:00
Size:
25 datasets

Download Data

Download ZIP file containing all datasets as tab-delimited text — use the following character encoding:

Datasets listed in this publication series

  1. Riethdorf, J-R; Nürnberg, D; Max, L et al. (2013): (Table A3) Age-depth points for core SO201-2-101. https://doi.org/10.1594/PANGAEA.825247
  2. Riethdorf, J-R; Nürnberg, D; Max, L et al. (2013): (Table A1) Age-depth points for core SO201-2-77. https://doi.org/10.1594/PANGAEA.825261
  3. Riethdorf, J-R; Nürnberg, D; Max, L et al. (2013): (Table A2) Age-depth points for core SO201-2-85. https://doi.org/10.1594/PANGAEA.825249
  4. Riethdorf, J-R; Nürnberg, D; Max, L et al. (2013): Bulk components of sediment core SO201-2-77. https://doi.org/10.1594/PANGAEA.786276
  5. Riethdorf, J-R; Nürnberg, D; Max, L et al. (2013): Color measurements on sediment core SO201-2-77. https://doi.org/10.1594/PANGAEA.786273
  6. Riethdorf, J-R; Nürnberg, D; Max, L et al. (2013): Stable isotopes measured on benthic foraminifers of sediment core SO201-2-77. https://doi.org/10.1594/PANGAEA.786282
  7. Riethdorf, J-R; Nürnberg, D; Max, L et al. (2013): Dry bulk density of sediment core SO201-2-77. https://doi.org/10.1594/PANGAEA.786285
  8. Riethdorf, J-R; Nürnberg, D; Max, L et al. (2013): Geochemical composition of sediment core SO201-2-77. https://doi.org/10.1594/PANGAEA.786295
  9. Riethdorf, J-R; Nürnberg, D; Max, L et al. (2013): Opal of sediment core SO201-2-77. https://doi.org/10.1594/PANGAEA.786291
  10. Riethdorf, J-R; Nürnberg, D; Max, L et al. (2013): Coarse-fraction analysis of sediment core SO201-2-77. https://doi.org/10.1594/PANGAEA.786270
  11. Riethdorf, J-R; Nürnberg, D; Max, L et al. (2013): Bulk components of sediment core SO201-2-85. https://doi.org/10.1594/PANGAEA.786278
  12. Riethdorf, J-R; Nürnberg, D; Max, L et al. (2013): Color measurements on sediment core SO201-2-85. https://doi.org/10.1594/PANGAEA.786274
  13. Riethdorf, J-R; Nürnberg, D; Max, L et al. (2013): Stable isotopes measured on benthic foraminifers of sediment core SO201-2-85. https://doi.org/10.1594/PANGAEA.786283
  14. Riethdorf, J-R; Nürnberg, D; Max, L et al. (2013): Dry bulk density of sediment core SO201-2-85. https://doi.org/10.1594/PANGAEA.786287
  15. Riethdorf, J-R; Nürnberg, D; Max, L et al. (2013): Geochemical composition of sediment core SO201-2-85. https://doi.org/10.1594/PANGAEA.786296
  16. Riethdorf, J-R; Nürnberg, D; Max, L et al. (2013): Opal of sediment core SO201-2-85. https://doi.org/10.1594/PANGAEA.786292
  17. Riethdorf, J-R; Nürnberg, D; Max, L et al. (2013): Paleomagnetic of sediment core SO201-2-85. https://doi.org/10.1594/PANGAEA.786293
  18. Riethdorf, J-R; Nürnberg, D; Max, L et al. (2013): Coarse-fraction analysis of sediment core SO201-2-85. https://doi.org/10.1594/PANGAEA.786271
  19. Riethdorf, J-R; Nürnberg, D; Max, L et al. (2013): Bulk components of sediment core SO201-2-101. https://doi.org/10.1594/PANGAEA.786275
  20. Riethdorf, J-R; Nürnberg, D; Max, L et al. (2013): Color measurements on sediment core SO201-2-101. https://doi.org/10.1594/PANGAEA.786272
  21. Riethdorf, J-R; Nürnberg, D; Max, L et al. (2013): Stable isotopes measured on benthic foraminifers of sediment core SO201-2-101. https://doi.org/10.1594/PANGAEA.786280
  22. Riethdorf, J-R; Nürnberg, D; Max, L et al. (2013): Dry bulk density of sediment core SO201-2-101. https://doi.org/10.1594/PANGAEA.786284
  23. Riethdorf, J-R; Nürnberg, D; Max, L et al. (2013): Geochemical composition of sediment core SO201-2-101. https://doi.org/10.1594/PANGAEA.786294
  24. Riethdorf, J-R; Nürnberg, D; Max, L et al. (2013): Opal of sediment core SO201-2-101. https://doi.org/10.1594/PANGAEA.786290
  25. Riethdorf, J-R; Nürnberg, D; Max, L et al. (2013): Coarse-fraction analysis of sediment core SO201-2-101. https://doi.org/10.1594/PANGAEA.786268