Articles | Volume 16, issue 2
https://doi.org/10.5194/cp-16-487-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-16-487-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
10 Mar 2020
Research article |
| 10 Mar 2020
| 10 Mar 2020
Multiproxy evidence of the Neoglacial expansion of Atlantic Water to eastern Svalbard
Institute of Oceanology, Polish Academy of Sciences, Sopot, 81-712,
Poland
Magdalena Łącka
Institute of Oceanology, Polish Academy of Sciences, Sopot, 81-712,
Poland
Małgorzata Kucharska
Institute of Oceanology, Polish Academy of Sciences, Sopot, 81-712,
Poland
Jan Pawlowski
Institute of Oceanology, Polish Academy of Sciences, Sopot, 81-712,
Poland
Department of Genetics and Evolution, University of Geneva, Geneva, CH
1211, Switzerland
Marek Zajączkowski
Institute of Oceanology, Polish Academy of Sciences, Sopot, 81-712,
Poland
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Cited
14 citations as recorded by crossref.
- A Driftwood‐Based Record of Arctic Sea Ice During the Last 500 Years From Northern Svalbard Reveals Sea Ice Dynamics in the Arctic Ocean and Arctic Peripheral Seas G. Hole et al. 10.1029/2021JC017563
- Sedimentary Ancient DNA From the Subarctic North Pacific: How Sea Ice, Salinity, and Insolation Dynamics Have Shaped Diatom Composition and Richness Over the Past 20,000 Years H. Zimmermann et al. 10.1029/2020PA004091
- Sedimentary ancient DNA insights into foraminiferal diversity near the grounding line in the western Ross Sea, Antarctica E. Demianiuk et al. 10.5194/bg-22-2601-2025
- A late response of the sea-ice cover to Neoglacial cooling in the western Barents Sea M. Telesiński et al. 10.1177/09596836241247305
- Extending monitoring with sediment archive approaches: Comparison of biomonitoring, metabarcoding, and biomarkers to assess past phytoplankton dynamics J. Romahn et al. 10.1002/lom3.10694
- Paleoceanographic changes along the western Spitsbergen margin, evidence from planktic microfossil during the last 10 kyr BP F. Torricella et al. 10.1016/j.palaeo.2025.112940
- Identification of Atlantic water inflow on the north Svalbard shelf during the Holocene M. Peral et al. 10.1002/jqs.3374
- The maturing relationship between Quaternary paleoecology and ancient sedimentary DNA M. Edwards 10.1017/qua.2020.52
- Holocene glacial history of Svalbard: Status, perspectives and challenges W. Farnsworth et al. 10.1016/j.earscirev.2020.103249
- The development of ocean currents and the response of the cryosphere on the Southwest Svalbard shelf over the Holocene D. Devendra et al. 10.1016/j.gloplacha.2023.104213
- Marine sedimentary ancient DNA from Antarctic diatoms P. Singh et al. 10.1016/j.palaeo.2024.112090
- Marine ecosystem shifts with deglacial sea-ice loss inferred from ancient DNA shotgun sequencing H. Zimmermann et al. 10.1038/s41467-023-36845-x
- Changes in the composition of marine and sea-ice diatoms derived from sedimentary ancient DNA of the eastern Fram Strait over the past 30 000 years H. Zimmermann et al. 10.5194/os-16-1017-2020
- Sedimentary ancient DNA: a new paleogenomic tool for reconstructing the history of marine ecosystems N. Nguyen et al. 10.3389/fmars.2023.1185435
14 citations as recorded by crossref.
- A Driftwood‐Based Record of Arctic Sea Ice During the Last 500 Years From Northern Svalbard Reveals Sea Ice Dynamics in the Arctic Ocean and Arctic Peripheral Seas G. Hole et al. 10.1029/2021JC017563
- Sedimentary Ancient DNA From the Subarctic North Pacific: How Sea Ice, Salinity, and Insolation Dynamics Have Shaped Diatom Composition and Richness Over the Past 20,000 Years H. Zimmermann et al. 10.1029/2020PA004091
- Sedimentary ancient DNA insights into foraminiferal diversity near the grounding line in the western Ross Sea, Antarctica E. Demianiuk et al. 10.5194/bg-22-2601-2025
- A late response of the sea-ice cover to Neoglacial cooling in the western Barents Sea M. Telesiński et al. 10.1177/09596836241247305
- Extending monitoring with sediment archive approaches: Comparison of biomonitoring, metabarcoding, and biomarkers to assess past phytoplankton dynamics J. Romahn et al. 10.1002/lom3.10694
- Paleoceanographic changes along the western Spitsbergen margin, evidence from planktic microfossil during the last 10 kyr BP F. Torricella et al. 10.1016/j.palaeo.2025.112940
- Identification of Atlantic water inflow on the north Svalbard shelf during the Holocene M. Peral et al. 10.1002/jqs.3374
- The maturing relationship between Quaternary paleoecology and ancient sedimentary DNA M. Edwards 10.1017/qua.2020.52
- Holocene glacial history of Svalbard: Status, perspectives and challenges W. Farnsworth et al. 10.1016/j.earscirev.2020.103249
- The development of ocean currents and the response of the cryosphere on the Southwest Svalbard shelf over the Holocene D. Devendra et al. 10.1016/j.gloplacha.2023.104213
- Marine sedimentary ancient DNA from Antarctic diatoms P. Singh et al. 10.1016/j.palaeo.2024.112090
- Marine ecosystem shifts with deglacial sea-ice loss inferred from ancient DNA shotgun sequencing H. Zimmermann et al. 10.1038/s41467-023-36845-x
- Changes in the composition of marine and sea-ice diatoms derived from sedimentary ancient DNA of the eastern Fram Strait over the past 30 000 years H. Zimmermann et al. 10.5194/os-16-1017-2020
- Sedimentary ancient DNA: a new paleogenomic tool for reconstructing the history of marine ecosystems N. Nguyen et al. 10.3389/fmars.2023.1185435
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Short summary
Paleoceanographic changes in Storfjorden during the Neoglacial (the last
4000 years) were reconstructed based on microfossil and ancient DNA records. Environmental changes were steered mainly by the interaction between the inflow of Atlantic Water (AW) and sea ice cover. Warming periods were associated with AW inflow and sea ice melting, stimulating primary production. The cold phases were characterized by densely packed sea ice, resulting in limited productivity.
Paleoceanographic changes in Storfjorden during the Neoglacial (the last
4000 years) were...
