Borehole temperature, submarine permafrost methane concentrations and pore water chemistry measured on borehole BK-2, central Laptev Sea shelf ...
Submarine permafrost degradation has been invoked as a cause for recent observations of methane emissions from the seabed to the water column and atmosphere of the East Siberian shelf. Sediment drilled 52 m down from the sea ice in Buor Khaya Bay, central Laptev Sea revealed unfrozen sediment overly...
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ftdatacite:10.1594/pangaea.846279 2024-09-15T18:11:21+00:00 Borehole temperature, submarine permafrost methane concentrations and pore water chemistry measured on borehole BK-2, central Laptev Sea shelf ... Overduin, Pier Paul Liebner, Susanne Knoblauch, Christian Günther, Frank Wetterich, Sebastian Schirrmeister, Lutz Hubberten, Hans-Wolfgang Grigoriev, Mikhail N 2015 application/zip https://dx.doi.org/10.1594/pangaea.846279 https://doi.pangaea.de/10.1594/PANGAEA.846279 en eng PANGAEA https://dx.doi.org/10.1002/2014jg002862 https://dx.doi.org/10.2312/bzpm_0664_2013 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn article Collection Supplementary Publication Series of Datasets 2015 ftdatacite https://doi.org/10.1594/pangaea.84627910.1002/2014jg00286210.2312/bzpm_0664_2013 2024-08-01T10:57:41Z Submarine permafrost degradation has been invoked as a cause for recent observations of methane emissions from the seabed to the water column and atmosphere of the East Siberian shelf. Sediment drilled 52 m down from the sea ice in Buor Khaya Bay, central Laptev Sea revealed unfrozen sediment overlying ice-bonded permafrost. Methane concentrations in the overlying unfrozen sediment were low (mean 20 µM) but higher in the underlying ice-bonded submarine permafrost (mean 380 µM). In contrast, sulfate concentrations were substantially higher in the unfrozen sediment (mean 2.5 mM) than in the underlying submarine permafrost (mean 0.1 mM). Using deduced permafrost degradation rates, we calculate potential mean methane efflux from degrading permafrost of 120 mg/m**2 per year at this site. However, a drop of methane concentrations from 190 µM to 19 µM and a concomitant increase of methane d13C from -63 per mil to -35 per mil directly above the ice-bonded permafrost suggest that methane is effectively oxidized ... : Supplement to: Overduin, Pier Paul; Liebner, Susanne; Knoblauch, Christian; Günther, Frank; Wetterich, Sebastian; Schirrmeister, Lutz; Hubberten, Hans-Wolfgang; Grigoriev, Mikhail N (2015): Methane oxidation following submarine permafrost degradation: Measurements from a central Laptev Sea shelf borehole. Journal of Geophysical Research: Biogeosciences, 120(5), 965-978 ... Article in Journal/Newspaper Ice laptev Laptev Sea permafrost Sea ice DataCite |
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Open Polar |
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DataCite |
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ftdatacite |
language |
English |
topic |
Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn |
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Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn Overduin, Pier Paul Liebner, Susanne Knoblauch, Christian Günther, Frank Wetterich, Sebastian Schirrmeister, Lutz Hubberten, Hans-Wolfgang Grigoriev, Mikhail N Borehole temperature, submarine permafrost methane concentrations and pore water chemistry measured on borehole BK-2, central Laptev Sea shelf ... |
topic_facet |
Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn |
description |
Submarine permafrost degradation has been invoked as a cause for recent observations of methane emissions from the seabed to the water column and atmosphere of the East Siberian shelf. Sediment drilled 52 m down from the sea ice in Buor Khaya Bay, central Laptev Sea revealed unfrozen sediment overlying ice-bonded permafrost. Methane concentrations in the overlying unfrozen sediment were low (mean 20 µM) but higher in the underlying ice-bonded submarine permafrost (mean 380 µM). In contrast, sulfate concentrations were substantially higher in the unfrozen sediment (mean 2.5 mM) than in the underlying submarine permafrost (mean 0.1 mM). Using deduced permafrost degradation rates, we calculate potential mean methane efflux from degrading permafrost of 120 mg/m**2 per year at this site. However, a drop of methane concentrations from 190 µM to 19 µM and a concomitant increase of methane d13C from -63 per mil to -35 per mil directly above the ice-bonded permafrost suggest that methane is effectively oxidized ... : Supplement to: Overduin, Pier Paul; Liebner, Susanne; Knoblauch, Christian; Günther, Frank; Wetterich, Sebastian; Schirrmeister, Lutz; Hubberten, Hans-Wolfgang; Grigoriev, Mikhail N (2015): Methane oxidation following submarine permafrost degradation: Measurements from a central Laptev Sea shelf borehole. Journal of Geophysical Research: Biogeosciences, 120(5), 965-978 ... |
format |
Article in Journal/Newspaper |
author |
Overduin, Pier Paul Liebner, Susanne Knoblauch, Christian Günther, Frank Wetterich, Sebastian Schirrmeister, Lutz Hubberten, Hans-Wolfgang Grigoriev, Mikhail N |
author_facet |
Overduin, Pier Paul Liebner, Susanne Knoblauch, Christian Günther, Frank Wetterich, Sebastian Schirrmeister, Lutz Hubberten, Hans-Wolfgang Grigoriev, Mikhail N |
author_sort |
Overduin, Pier Paul |
title |
Borehole temperature, submarine permafrost methane concentrations and pore water chemistry measured on borehole BK-2, central Laptev Sea shelf ... |
title_short |
Borehole temperature, submarine permafrost methane concentrations and pore water chemistry measured on borehole BK-2, central Laptev Sea shelf ... |
title_full |
Borehole temperature, submarine permafrost methane concentrations and pore water chemistry measured on borehole BK-2, central Laptev Sea shelf ... |
title_fullStr |
Borehole temperature, submarine permafrost methane concentrations and pore water chemistry measured on borehole BK-2, central Laptev Sea shelf ... |
title_full_unstemmed |
Borehole temperature, submarine permafrost methane concentrations and pore water chemistry measured on borehole BK-2, central Laptev Sea shelf ... |
title_sort |
borehole temperature, submarine permafrost methane concentrations and pore water chemistry measured on borehole bk-2, central laptev sea shelf ... |
publisher |
PANGAEA |
publishDate |
2015 |
url |
https://dx.doi.org/10.1594/pangaea.846279 https://doi.pangaea.de/10.1594/PANGAEA.846279 |
genre |
Ice laptev Laptev Sea permafrost Sea ice |
genre_facet |
Ice laptev Laptev Sea permafrost Sea ice |
op_relation |
https://dx.doi.org/10.1002/2014jg002862 https://dx.doi.org/10.2312/bzpm_0664_2013 |
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.84627910.1002/2014jg00286210.2312/bzpm_0664_2013 |
_version_ |
1810448932472356864 |