Sea ice and primary production proxies in surface sediments from a High Arctic Greenland fjord : Spatial distribution and implications for palaeoenvironmental studies
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 Mon...
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ftunivhelsihelda:oai:helda.helsinki.fi:10138/181218 2024-01-07T09:40:42+01:00 Sea ice and primary production proxies in surface sediments from a High Arctic Greenland fjord : Spatial distribution and implications for palaeoenvironmental studies Ribeiro, Sofia Sejr, Mikael K. Limoges, Audrey Heikkilä, Maija Andersen, Thorbjorn Joest Tallberg, Petra Weckstrom, Kaarina Husum, Katrine Forwick, Matthias Dalsgaard, Tage Masse, Guillaume Seidenkrantz, Marit-Solveig Rysgaard, Soren Environmental Sciences Aquatic Biogeochemistry Research Unit (ABRU) Environmental Change Research Unit (ECRU) Marine Ecosystems Research Group 2017-04-26T07:41:02Z 13 application/pdf http://hdl.handle.net/10138/181218 eng eng Springer 10.1007/s13280-016-0894-2 This study received financial support from the Villum Foundation, Denmark (Grant VKR 023454 to S. Ribeiro). Fieldwork was funded by the Arctic Research Center at Aarhus University, the Arctic Science Partnership, the TUNU Programme (Tromso University, Norway), and the DANCEA programme (Ministry of Environment and food of Denmark). Data from the Greenland Ecosystem Monitoring Programme were provided by the Greenland Institute of Natural Resources, Nuuk, Greenland in collaboration with Department of Bioscience, Aarhus University, Denmark. S. Rysgaard was funded by the Canada Excellence Research Chair Program, and M.-S. Seidenkrantz by the Danish Council for Independent Research vertical bar Natural Sciences (OceanHeat Project No. 12-126709/FNU). We are grateful to Egon Randa Frandsen, Aarhus University and personnel from GNRI (Nuuk, Greenland), who collected some of the sediment cores in 2014 from the small research vessel Aage V. Jensen. The captain and crew of R/V Helmer Hanssen are acknowledged, as well as Trine Dahl and Bjorn Runer Olsen for their support during data collection. Ribeiro , S , Sejr , M K , Limoges , A , Heikkilä , M , Andersen , T J , Tallberg , P , Weckstrom , K , Husum , K , Forwick , M , Dalsgaard , T , Masse , G , Seidenkrantz , M-S & Rysgaard , S 2017 , ' Sea ice and primary production proxies in surface sediments from a High Arctic Greenland fjord : Spatial distribution and implications for palaeoenvironmental studies ' , Ambio , vol. 46 , pp. S106-S118 . https://doi.org/10.1007/s13280-016-0894-2 ORCID: /0000-0002-3889-0788/work/47606213 ORCID: /0000-0003-3885-8670/work/40901756 85010310982 8bc37e48-07ed-407e-b048-eee1d9158e50 http://hdl.handle.net/10138/181218 000395124900010 cc_by openAccess info:eu-repo/semantics/openAccess Arctic sea ice Greenland fjords HBIs Primary production Proxies Silica BIOGENIC SILICA NE GREENLAND YOUNG SOUND MARINE ECOSYSTEM IDENTIFICATION OCEAN DYNAMICS COVER IP25 1172 Environmental sciences Article publishedVersion 2017 ftunivhelsihelda 2023-12-14T00:12:55Z 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 IP25 was detected at all sites but at low concentrations, indicating that IP25 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. Peer reviewed Article in Journal/Newspaper Arctic Arctic Greenland Sea ice HELDA – University of Helsinki Open Repository Arctic Greenland Tyrolerfjord ENVELOPE(-21.883,-21.883,74.517,74.517) Ambio 46 S1 106 118 |
institution |
Open Polar |
collection |
HELDA – University of Helsinki Open Repository |
op_collection_id |
ftunivhelsihelda |
language |
English |
topic |
Arctic sea ice Greenland fjords HBIs Primary production Proxies Silica BIOGENIC SILICA NE GREENLAND YOUNG SOUND MARINE ECOSYSTEM IDENTIFICATION OCEAN DYNAMICS COVER IP25 1172 Environmental sciences |
spellingShingle |
Arctic sea ice Greenland fjords HBIs Primary production Proxies Silica BIOGENIC SILICA NE GREENLAND YOUNG SOUND MARINE ECOSYSTEM IDENTIFICATION OCEAN DYNAMICS COVER IP25 1172 Environmental sciences Ribeiro, Sofia Sejr, Mikael K. Limoges, Audrey Heikkilä, Maija Andersen, Thorbjorn Joest Tallberg, Petra Weckstrom, Kaarina Husum, Katrine Forwick, Matthias Dalsgaard, Tage Masse, Guillaume Seidenkrantz, Marit-Solveig Rysgaard, Soren Sea ice and primary production proxies in surface sediments from a High Arctic Greenland fjord : Spatial distribution and implications for palaeoenvironmental studies |
topic_facet |
Arctic sea ice Greenland fjords HBIs Primary production Proxies Silica BIOGENIC SILICA NE GREENLAND YOUNG SOUND MARINE ECOSYSTEM IDENTIFICATION OCEAN DYNAMICS COVER IP25 1172 Environmental sciences |
description |
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 IP25 was detected at all sites but at low concentrations, indicating that IP25 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. Peer reviewed |
author2 |
Environmental Sciences Aquatic Biogeochemistry Research Unit (ABRU) Environmental Change Research Unit (ECRU) Marine Ecosystems Research Group |
format |
Article in Journal/Newspaper |
author |
Ribeiro, Sofia Sejr, Mikael K. Limoges, Audrey Heikkilä, Maija Andersen, Thorbjorn Joest Tallberg, Petra Weckstrom, Kaarina Husum, Katrine Forwick, Matthias Dalsgaard, Tage Masse, Guillaume Seidenkrantz, Marit-Solveig Rysgaard, Soren |
author_facet |
Ribeiro, Sofia Sejr, Mikael K. Limoges, Audrey Heikkilä, Maija Andersen, Thorbjorn Joest Tallberg, Petra Weckstrom, Kaarina Husum, Katrine Forwick, Matthias Dalsgaard, Tage Masse, Guillaume Seidenkrantz, Marit-Solveig Rysgaard, Soren |
author_sort |
Ribeiro, Sofia |
title |
Sea ice and primary production proxies in surface sediments from a High Arctic Greenland fjord : Spatial distribution and implications for palaeoenvironmental studies |
title_short |
Sea ice and primary production proxies in surface sediments from a High Arctic Greenland fjord : Spatial distribution and implications for palaeoenvironmental studies |
title_full |
Sea ice and primary production proxies in surface sediments from a High Arctic Greenland fjord : Spatial distribution and implications for palaeoenvironmental studies |
title_fullStr |
Sea ice and primary production proxies in surface sediments from a High Arctic Greenland fjord : Spatial distribution and implications for palaeoenvironmental studies |
title_full_unstemmed |
Sea ice and primary production proxies in surface sediments from a High Arctic Greenland fjord : Spatial distribution and implications for palaeoenvironmental studies |
title_sort |
sea ice and primary production proxies in surface sediments from a high arctic greenland fjord : spatial distribution and implications for palaeoenvironmental studies |
publisher |
Springer |
publishDate |
2017 |
url |
http://hdl.handle.net/10138/181218 |
long_lat |
ENVELOPE(-21.883,-21.883,74.517,74.517) |
geographic |
Arctic Greenland Tyrolerfjord |
geographic_facet |
Arctic Greenland Tyrolerfjord |
genre |
Arctic Arctic Greenland Sea ice |
genre_facet |
Arctic Arctic Greenland Sea ice |
op_relation |
10.1007/s13280-016-0894-2 This study received financial support from the Villum Foundation, Denmark (Grant VKR 023454 to S. Ribeiro). Fieldwork was funded by the Arctic Research Center at Aarhus University, the Arctic Science Partnership, the TUNU Programme (Tromso University, Norway), and the DANCEA programme (Ministry of Environment and food of Denmark). Data from the Greenland Ecosystem Monitoring Programme were provided by the Greenland Institute of Natural Resources, Nuuk, Greenland in collaboration with Department of Bioscience, Aarhus University, Denmark. S. Rysgaard was funded by the Canada Excellence Research Chair Program, and M.-S. Seidenkrantz by the Danish Council for Independent Research vertical bar Natural Sciences (OceanHeat Project No. 12-126709/FNU). We are grateful to Egon Randa Frandsen, Aarhus University and personnel from GNRI (Nuuk, Greenland), who collected some of the sediment cores in 2014 from the small research vessel Aage V. Jensen. The captain and crew of R/V Helmer Hanssen are acknowledged, as well as Trine Dahl and Bjorn Runer Olsen for their support during data collection. Ribeiro , S , Sejr , M K , Limoges , A , Heikkilä , M , Andersen , T J , Tallberg , P , Weckstrom , K , Husum , K , Forwick , M , Dalsgaard , T , Masse , G , Seidenkrantz , M-S & Rysgaard , S 2017 , ' Sea ice and primary production proxies in surface sediments from a High Arctic Greenland fjord : Spatial distribution and implications for palaeoenvironmental studies ' , Ambio , vol. 46 , pp. S106-S118 . https://doi.org/10.1007/s13280-016-0894-2 ORCID: /0000-0002-3889-0788/work/47606213 ORCID: /0000-0003-3885-8670/work/40901756 85010310982 8bc37e48-07ed-407e-b048-eee1d9158e50 http://hdl.handle.net/10138/181218 000395124900010 |
op_rights |
cc_by openAccess info:eu-repo/semantics/openAccess |
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46 |
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