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Christof Pearce

Marine conditions and development of the Sirius Water polynya on the North-East Greenland shelf during the Younger Dryas-Holocene

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  • Rebecca Jackson, Geological Survey of Denmark and Greenland, University of Copenhagen
  • ,
  • Nanna Andreasen, Geological Survey of Denmark and Greenland, University of Copenhagen
  • ,
  • Mimmi Oksman, Geological Survey of Denmark and Greenland
  • ,
  • Thorbjørn J. Andersen, University of Copenhagen
  • ,
  • Christof Pearce
  • Marit Solveig Seidenkrantz
  • Sofia Ribeiro, Geological Survey of Denmark and Greenland

The Fram Strait is one of the largest gateways through which meltwater and sea ice are exported to the subarctic North Atlantic, transiting the North-East Greenland shelf via the southward flowing East Greenland Current. Observations indicate a recent freshening of the East Greenland Current that may have implications for wider oceanic circulation regimes. The North-East Greenland shelf is an opportune region to assess these changes back through time. Paleoceanographic reconstructions from the North-East Greenland shelf are sparse and their temporal coverage is limited to the Holocene, limiting our ability to assess the impact of rapid climatic variations on marine conditions, such as during the Younger Dryas/Holocene transition. Here, we present data from a well-dated marine sediment core retrieved from the North-East Greenland shelf (74°N; east of Young Sound-Tyrolerfjord system) that captures the late Younger Dryas Stadial through to the Mid-Holocene at sub-centennial resolution. We apply a multi-proxy approach to reconstruct changes in productivity, surface and bottom ocean conditions. We show that at 74° N the presence of warm Atlantic waters on the inner North-East Greenland shelf was limited to the late Younger Dryas, as the Greenland Ice Sheet retreated landward and isostatic rebound caused the area to uplift. A unique dimension to this record is its location within one of the few biological hotspots on the East Greenland shelf today; the Sirius Water polynya. Archaeological studies indicate the polynya was forming as early as 4500 years ago, but nothing is known about its evolution from a marine perspective. Cooling of bottom waters, increasing sea-surface productivity and more frequent open water conditions indicate an Early Holocene onset of the Sirius Water (ca. 10–8.7 ka BP).

Original languageEnglish
Article number107647
JournalQuaternary Science Reviews
Publication statusPublished - 1 Sep 2022

Bibliographical note

Publisher Copyright:
© 2022 The Authors

    Research areas

  • Dinocysts, Foraminifera, Greenland, Holocene, Micropaleontology, North-East Greenland, Paleoceanography, Polynyas, Sirius water polynya, Younger dryas

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