A novel system for quantitative sampling of sub-ice platelet layers

Near the front of large ice shelves, outflowing seawater containing meltwater from beneath the ice shelf can become ‘supercooled’. This supports the development of ‘sub-ice platelet layers’ (SIPLs) – accumulations of ice discs, each 2-5 mm thick, that buoyantly rise through the water column until th...

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Main Authors: Robinson, N., Stewart, C., Ryan, K., Parker, S.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5016879
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5016879 2023-10-09T21:52:26+02:00 A novel system for quantitative sampling of sub-ice platelet layers Robinson, N. Stewart, C. Ryan, K. Parker, S. 2023 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5016879 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-0626 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5016879 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-0626 2023-09-10T23:43:22Z Near the front of large ice shelves, outflowing seawater containing meltwater from beneath the ice shelf can become ‘supercooled’. This supports the development of ‘sub-ice platelet layers’ (SIPLs) – accumulations of ice discs, each 2-5 mm thick, that buoyantly rise through the water column until they come to rest against the base of the sea ice. The discs coalesce to form an intricate 3-dimensional ice matrix that may extend several metres into the upper ocean. The result is a quiescent and protective marine habitat that harbours some of the highest concentrations of primary productivity on Earth, but whose viability may be threatened by subtle climate shifts. In-situ, the 3-dimensional SIPL structure can be reasonably robust. However, when samples of the SIPL are extracted the structure becomes very delicate and may disintegrate rapidly. Hence, until very recently, qualitative analysis of the integrated SIPL system – comprising the ice structure itself, the interstitial fluid, and any associated biology – has not been possible. Here we describe the development, testing, and initial deployment of a new, bespoke-engineered system for coring SIPLs. The system sequentially extracts segments of the SIPL without destroying the structure or disassociating the ice from the interstitial fluid or incorporated biology. The samples can then be analysed for ice/water fraction, physical characteristics, or biological assemblage, each of which can be related to the environmental setting. Ultimately, the system will be used to inform assessment of the Ross Sea ecosystem’s susceptibility to change as determined by the vulnerability of the unique SIPL habitat. Conference Object Ice Shelf Ice Shelves Ross Sea Sea ice GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Ross Sea
institution Open Polar
collection GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
op_collection_id ftgfzpotsdam
language English
description Near the front of large ice shelves, outflowing seawater containing meltwater from beneath the ice shelf can become ‘supercooled’. This supports the development of ‘sub-ice platelet layers’ (SIPLs) – accumulations of ice discs, each 2-5 mm thick, that buoyantly rise through the water column until they come to rest against the base of the sea ice. The discs coalesce to form an intricate 3-dimensional ice matrix that may extend several metres into the upper ocean. The result is a quiescent and protective marine habitat that harbours some of the highest concentrations of primary productivity on Earth, but whose viability may be threatened by subtle climate shifts. In-situ, the 3-dimensional SIPL structure can be reasonably robust. However, when samples of the SIPL are extracted the structure becomes very delicate and may disintegrate rapidly. Hence, until very recently, qualitative analysis of the integrated SIPL system – comprising the ice structure itself, the interstitial fluid, and any associated biology – has not been possible. Here we describe the development, testing, and initial deployment of a new, bespoke-engineered system for coring SIPLs. The system sequentially extracts segments of the SIPL without destroying the structure or disassociating the ice from the interstitial fluid or incorporated biology. The samples can then be analysed for ice/water fraction, physical characteristics, or biological assemblage, each of which can be related to the environmental setting. Ultimately, the system will be used to inform assessment of the Ross Sea ecosystem’s susceptibility to change as determined by the vulnerability of the unique SIPL habitat.
format Conference Object
author Robinson, N.
Stewart, C.
Ryan, K.
Parker, S.
spellingShingle Robinson, N.
Stewart, C.
Ryan, K.
Parker, S.
A novel system for quantitative sampling of sub-ice platelet layers
author_facet Robinson, N.
Stewart, C.
Ryan, K.
Parker, S.
author_sort Robinson, N.
title A novel system for quantitative sampling of sub-ice platelet layers
title_short A novel system for quantitative sampling of sub-ice platelet layers
title_full A novel system for quantitative sampling of sub-ice platelet layers
title_fullStr A novel system for quantitative sampling of sub-ice platelet layers
title_full_unstemmed A novel system for quantitative sampling of sub-ice platelet layers
title_sort novel system for quantitative sampling of sub-ice platelet layers
publishDate 2023
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_5016879
geographic Ross Sea
geographic_facet Ross Sea
genre Ice Shelf
Ice Shelves
Ross Sea
Sea ice
genre_facet Ice Shelf
Ice Shelves
Ross Sea
Sea ice
op_source XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-0626
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5016879
op_doi https://doi.org/10.57757/IUGG23-0626
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