Sea ice and primary production proxies in surface sediments from a High Arctic Greenland fjord: Spatial distribution and implications for palaeoenvironmental studies

• Published in: Ambio
• Main Authors: Ribeiro, Sofia, Sejr, Mikael K., Limoges, Audrey, Heikkilä, Maija, Andersen, Thorbjørn Joest, Tallberg, Petra, Weckström, Kaarina, Husum, Katrine, Forwick, Matthias, Dalsgaard, Tage, Massé, Guillaume, Seidenkrantz, Marit-Solveig, Rysgaard, Søren
• Format: Article in Journal/Newspaper
• Language: English
• Published: Springer Verlag (Germany) 2017
• Subjects: VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Sedimentologi: 456; VDP::Mathematics and natural science: 400::Geosciences: 450::Sedimentology: 456; Arctic sea ice; Greenland fjords; HBIs; Primary production; Proxies; Silica; Arctic; Greenland; Tyrolerfjord; Sea ice
• Online Access: https://hdl.handle.net/10037/13484; https://doi.org/10.1007/s13280-016-0894-2

Source at https://doi.org/10.1007/s13280-016-0894-2 . In order to establish a baseline for proxy-based reconstructions for the Young Sound–Tyrolerfjord system (Northeast Greenland), we analysed the spatial distribution of primary production and sea ice proxies in surface sediments from the fjord, against monitoring data from the Greenland Ecosystem Monitoring Programme. Clear spatial gradients in organic carbon and biogenic silica contents reflected marine influence, nutrient availability and river-induced turbidity, in good agreement with in situ measurements. The sea ice proxy IPz 25 was detected at all sites but at low concentrations, indicating that IP 25 records from fjords need to be carefully considered and not directly compared to marine settings. The sea ice-associated biomarker HBI III revealed an open-water signature, with highest concentrations near the mid-July ice edge. This proxy evaluation is an important step towards reliable palaeoenvironmental reconstructions that will, ultimately, contribute to better predictions for this High Arctic ecosystem in a warming climate.