Dissolved organic carbon (DOC) in Arctic ground ice, from northwest Canada, east Siberia, and Alaska ...
Thermal permafrost degradation and coastal erosion in the Arctic remobilize substantial amounts of organic carbon (OC) and nutrients which have accumulated in late Pleistocene and Holocene unconsolidated deposits. Permafrost vulnerability to thaw subsidence, collapsing coastlines and irreversible la...
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ftdatacite:10.1594/pangaea.846074 2024-09-15T18:11:23+00:00 Dissolved organic carbon (DOC) in Arctic ground ice, from northwest Canada, east Siberia, and Alaska ... Fritz, Michael Opel, Thomas Tanski, George Herzschuh, Ulrike Meyer, Hanno Eulenburg, Antje Lantuit, Hugues 2015 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.846074 https://doi.pangaea.de/10.1594/PANGAEA.846074 en eng PANGAEA https://dx.doi.org/10.5194/tc-9-737-2015 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 ground ice permafrost Event label Location of event Latitude of event Longitude of event Ice type Stratigraphy Carbon, organic, dissolved Carbon, inorganic, dissolved δ18O δ Deuterium Deuterium excess pH Conductivity, electrolytic Chloride Sulfate Nitrate Bicarbonate ion Calcium Potassium Magnesium Sodium Sampling by hand HTCO, Shimadzu TOC-V Calculated Mass spectrometer Finnigan Delta-S/equilibration device Ion chromatograph, Dionex Corporation, DX-320 Titration potentiometric, 794 Basic Titrino Metrohm ICP-OES, Perkin-Elmer, Optima 3000XL RU-Land_2007_Lena AWI Arctic Land Expedition Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn dataset Supplementary Dataset Dataset 2015 ftdatacite https://doi.org/10.1594/pangaea.84607410.5194/tc-9-737-2015 2024-08-01T10:57:14Z Thermal permafrost degradation and coastal erosion in the Arctic remobilize substantial amounts of organic carbon (OC) and nutrients which have accumulated in late Pleistocene and Holocene unconsolidated deposits. Permafrost vulnerability to thaw subsidence, collapsing coastlines and irreversible landscape change are largely due to the presence of large amounts of massive ground ice such as ice wedges. However, ground ice has not, until now, been considered to be a source of dissolved organic carbon (DOC), dissolved inorganic carbon (DIC) and other elements which are important for ecosystems and carbon cycling. Here we show, using biogeochemical data from a large number of different ice bodies throughout the Arctic, that ice wedges have the greatest potential for DOC storage, with a maximum of 28.6 mg/L (mean: 9.6 mg/L). Variation in DOC concentration is positively correlated with and explained by the concentrations and relative amounts of typically terrestrial cations such as Mg2+ and K+. DOC sequestration ... : This study was undertaken in the Helmholtz Young Investigators Group 'COPER' - Coastal permafrost erosion, organic carbon and nutrient release in the Arctic nearshore zone (Helmholtz Association grant no. VH-NG-801 to Hugues Lantuit).http://www.awi.de/forschung/nachwuchsgruppen/coper.html ... Dataset Ice permafrost wedge* Alaska Siberia DataCite |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
ground ice permafrost Event label Location of event Latitude of event Longitude of event Ice type Stratigraphy Carbon, organic, dissolved Carbon, inorganic, dissolved δ18O δ Deuterium Deuterium excess pH Conductivity, electrolytic Chloride Sulfate Nitrate Bicarbonate ion Calcium Potassium Magnesium Sodium Sampling by hand HTCO, Shimadzu TOC-V Calculated Mass spectrometer Finnigan Delta-S/equilibration device Ion chromatograph, Dionex Corporation, DX-320 Titration potentiometric, 794 Basic Titrino Metrohm ICP-OES, Perkin-Elmer, Optima 3000XL RU-Land_2007_Lena AWI Arctic Land Expedition Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn |
spellingShingle |
ground ice permafrost Event label Location of event Latitude of event Longitude of event Ice type Stratigraphy Carbon, organic, dissolved Carbon, inorganic, dissolved δ18O δ Deuterium Deuterium excess pH Conductivity, electrolytic Chloride Sulfate Nitrate Bicarbonate ion Calcium Potassium Magnesium Sodium Sampling by hand HTCO, Shimadzu TOC-V Calculated Mass spectrometer Finnigan Delta-S/equilibration device Ion chromatograph, Dionex Corporation, DX-320 Titration potentiometric, 794 Basic Titrino Metrohm ICP-OES, Perkin-Elmer, Optima 3000XL RU-Land_2007_Lena AWI Arctic Land Expedition Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn Fritz, Michael Opel, Thomas Tanski, George Herzschuh, Ulrike Meyer, Hanno Eulenburg, Antje Lantuit, Hugues Dissolved organic carbon (DOC) in Arctic ground ice, from northwest Canada, east Siberia, and Alaska ... |
topic_facet |
ground ice permafrost Event label Location of event Latitude of event Longitude of event Ice type Stratigraphy Carbon, organic, dissolved Carbon, inorganic, dissolved δ18O δ Deuterium Deuterium excess pH Conductivity, electrolytic Chloride Sulfate Nitrate Bicarbonate ion Calcium Potassium Magnesium Sodium Sampling by hand HTCO, Shimadzu TOC-V Calculated Mass spectrometer Finnigan Delta-S/equilibration device Ion chromatograph, Dionex Corporation, DX-320 Titration potentiometric, 794 Basic Titrino Metrohm ICP-OES, Perkin-Elmer, Optima 3000XL RU-Land_2007_Lena AWI Arctic Land Expedition Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn |
description |
Thermal permafrost degradation and coastal erosion in the Arctic remobilize substantial amounts of organic carbon (OC) and nutrients which have accumulated in late Pleistocene and Holocene unconsolidated deposits. Permafrost vulnerability to thaw subsidence, collapsing coastlines and irreversible landscape change are largely due to the presence of large amounts of massive ground ice such as ice wedges. However, ground ice has not, until now, been considered to be a source of dissolved organic carbon (DOC), dissolved inorganic carbon (DIC) and other elements which are important for ecosystems and carbon cycling. Here we show, using biogeochemical data from a large number of different ice bodies throughout the Arctic, that ice wedges have the greatest potential for DOC storage, with a maximum of 28.6 mg/L (mean: 9.6 mg/L). Variation in DOC concentration is positively correlated with and explained by the concentrations and relative amounts of typically terrestrial cations such as Mg2+ and K+. DOC sequestration ... : This study was undertaken in the Helmholtz Young Investigators Group 'COPER' - Coastal permafrost erosion, organic carbon and nutrient release in the Arctic nearshore zone (Helmholtz Association grant no. VH-NG-801 to Hugues Lantuit).http://www.awi.de/forschung/nachwuchsgruppen/coper.html ... |
format |
Dataset |
author |
Fritz, Michael Opel, Thomas Tanski, George Herzschuh, Ulrike Meyer, Hanno Eulenburg, Antje Lantuit, Hugues |
author_facet |
Fritz, Michael Opel, Thomas Tanski, George Herzschuh, Ulrike Meyer, Hanno Eulenburg, Antje Lantuit, Hugues |
author_sort |
Fritz, Michael |
title |
Dissolved organic carbon (DOC) in Arctic ground ice, from northwest Canada, east Siberia, and Alaska ... |
title_short |
Dissolved organic carbon (DOC) in Arctic ground ice, from northwest Canada, east Siberia, and Alaska ... |
title_full |
Dissolved organic carbon (DOC) in Arctic ground ice, from northwest Canada, east Siberia, and Alaska ... |
title_fullStr |
Dissolved organic carbon (DOC) in Arctic ground ice, from northwest Canada, east Siberia, and Alaska ... |
title_full_unstemmed |
Dissolved organic carbon (DOC) in Arctic ground ice, from northwest Canada, east Siberia, and Alaska ... |
title_sort |
dissolved organic carbon (doc) in arctic ground ice, from northwest canada, east siberia, and alaska ... |
publisher |
PANGAEA |
publishDate |
2015 |
url |
https://dx.doi.org/10.1594/pangaea.846074 https://doi.pangaea.de/10.1594/PANGAEA.846074 |
genre |
Ice permafrost wedge* Alaska Siberia |
genre_facet |
Ice permafrost wedge* Alaska Siberia |
op_relation |
https://dx.doi.org/10.5194/tc-9-737-2015 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.84607410.5194/tc-9-737-2015 |
_version_ |
1810448964850286592 |