Deep material eroded from retrogressive thaw slump: case study in Peel Plateau, west Canadian Arctic
Ice-rich permafrost thaw is highly sensitive to the creation of local landscape subsidence in the Arctic, known as thermokarst structures. Upon thaw, these structures can erode, unlocking organic and mineral constituents and transferring this material downstream potentially affecting the ecosystem a...
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ftunistlouisbrus:oai:dial.uclouvain.be:boreal:224226 2024-05-12T07:59:19+00:00 Deep material eroded from retrogressive thaw slump: case study in Peel Plateau, west Canadian Arctic Thomas, Maxime Opfergelt, Sophie Monhonval, Arthur Hirst, Catherine Bröder Lisa Vonk Jorien Keskitalo Kirsi Zolkos Scott Tank Suzanne Kokelj Steve Artic Week UCL - SST/ELI/ELIE - Environmental Sciences 2019 http://hdl.handle.net/2078.1/224226 eng eng boreal:224226 http://hdl.handle.net/2078.1/224226 info:eu-repo/semantics/openAccess retrogressive thaw slump permafrost erosion mineral element release info:eu-repo/semantics/conferenceObject 2019 ftunistlouisbrus 2024-04-18T17:24:40Z Ice-rich permafrost thaw is highly sensitive to the creation of local landscape subsidence in the Arctic, known as thermokarst structures. Upon thaw, these structures can erode, unlocking organic and mineral constituents and transferring this material downstream potentially affecting the ecosystem at larger scale. Such hillslope landscape processes have recently developed in Peel Plateau, west Canadian Arctic, as Retrogressive Thaw Slumps (RTS). We investigate whether material eroded from RTS and transported downstream originates from upper or deeper soil horizons with potentially distinct organic and mineral contents. The total elemental content and soluble element fractions were determined in soils from different depths at the slump headwall (active layer, Holocene permafrost, and Pleistocene permafrost) and in downstream eroded material (mud, and debris) for eight RTS structures. We observe a similar total content in Ca, K, Al and Sr, and soluble content in Ca, K, Mg, Na between the downstream mud and debris and the Pleistocene permafrost. The data highlight that the eroded material originates from the deeper Pleistocene permafrost, and contributes solute element concentrations that are significantly higher (by at least one order of magnitude) than in previously thawed active layer or locally Holocene permafrost. We hypothesize that RTS development is responsible for horizontal transfer of perennially frozen materials downstream originating from deep Pleistocene permafrost deposits. This means that in addition to exposing deep organic carbon to mineralization, modern RTS development likely affect local ecosystem chemistry by releasing soluble elements. Conference Object Arctic Ice permafrost Thermokarst DIAL@USL-B (Université Saint-Louis, Bruxelles) Arctic |
institution |
Open Polar |
collection |
DIAL@USL-B (Université Saint-Louis, Bruxelles) |
op_collection_id |
ftunistlouisbrus |
language |
English |
topic |
retrogressive thaw slump permafrost erosion mineral element release |
spellingShingle |
retrogressive thaw slump permafrost erosion mineral element release Thomas, Maxime Opfergelt, Sophie Monhonval, Arthur Hirst, Catherine Bröder Lisa Vonk Jorien Keskitalo Kirsi Zolkos Scott Tank Suzanne Kokelj Steve Artic Week Deep material eroded from retrogressive thaw slump: case study in Peel Plateau, west Canadian Arctic |
topic_facet |
retrogressive thaw slump permafrost erosion mineral element release |
description |
Ice-rich permafrost thaw is highly sensitive to the creation of local landscape subsidence in the Arctic, known as thermokarst structures. Upon thaw, these structures can erode, unlocking organic and mineral constituents and transferring this material downstream potentially affecting the ecosystem at larger scale. Such hillslope landscape processes have recently developed in Peel Plateau, west Canadian Arctic, as Retrogressive Thaw Slumps (RTS). We investigate whether material eroded from RTS and transported downstream originates from upper or deeper soil horizons with potentially distinct organic and mineral contents. The total elemental content and soluble element fractions were determined in soils from different depths at the slump headwall (active layer, Holocene permafrost, and Pleistocene permafrost) and in downstream eroded material (mud, and debris) for eight RTS structures. We observe a similar total content in Ca, K, Al and Sr, and soluble content in Ca, K, Mg, Na between the downstream mud and debris and the Pleistocene permafrost. The data highlight that the eroded material originates from the deeper Pleistocene permafrost, and contributes solute element concentrations that are significantly higher (by at least one order of magnitude) than in previously thawed active layer or locally Holocene permafrost. We hypothesize that RTS development is responsible for horizontal transfer of perennially frozen materials downstream originating from deep Pleistocene permafrost deposits. This means that in addition to exposing deep organic carbon to mineralization, modern RTS development likely affect local ecosystem chemistry by releasing soluble elements. |
author2 |
UCL - SST/ELI/ELIE - Environmental Sciences |
format |
Conference Object |
author |
Thomas, Maxime Opfergelt, Sophie Monhonval, Arthur Hirst, Catherine Bröder Lisa Vonk Jorien Keskitalo Kirsi Zolkos Scott Tank Suzanne Kokelj Steve Artic Week |
author_facet |
Thomas, Maxime Opfergelt, Sophie Monhonval, Arthur Hirst, Catherine Bröder Lisa Vonk Jorien Keskitalo Kirsi Zolkos Scott Tank Suzanne Kokelj Steve Artic Week |
author_sort |
Thomas, Maxime |
title |
Deep material eroded from retrogressive thaw slump: case study in Peel Plateau, west Canadian Arctic |
title_short |
Deep material eroded from retrogressive thaw slump: case study in Peel Plateau, west Canadian Arctic |
title_full |
Deep material eroded from retrogressive thaw slump: case study in Peel Plateau, west Canadian Arctic |
title_fullStr |
Deep material eroded from retrogressive thaw slump: case study in Peel Plateau, west Canadian Arctic |
title_full_unstemmed |
Deep material eroded from retrogressive thaw slump: case study in Peel Plateau, west Canadian Arctic |
title_sort |
deep material eroded from retrogressive thaw slump: case study in peel plateau, west canadian arctic |
publishDate |
2019 |
url |
http://hdl.handle.net/2078.1/224226 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Ice permafrost Thermokarst |
genre_facet |
Arctic Ice permafrost Thermokarst |
op_relation |
boreal:224226 http://hdl.handle.net/2078.1/224226 |
op_rights |
info:eu-repo/semantics/openAccess |
_version_ |
1798840445353066496 |