Old Organic Matter in Siberian Permafrost Deposits and its Degradation Features
Introduction During the late Quaternary, a large pool of organic matter (OM) accumulated in the arctic permafrost zone. Because of the potential re-introduction into the biogeochemical cycle from degrading permafrost, the OC inventory of ice-rich permafrost deposits and its degradation features are...
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ftawi:oai:epic.awi.de:30849 2023-05-15T15:15:07+02:00 Old Organic Matter in Siberian Permafrost Deposits and its Degradation Features Strauss, Jens Schirrmeister, Lutz Wetterich, Sebastian Mangelsdorf, Kai 2012-06-26 application/pdf https://epic.awi.de/id/eprint/30849/ https://epic.awi.de/id/eprint/30849/1/Strauss_abstract_TICOP.pdf https://hdl.handle.net/10013/epic.39819 https://hdl.handle.net/10013/epic.39819.d001 unknown The Fort Dialog-Iset Publisher https://epic.awi.de/id/eprint/30849/1/Strauss_abstract_TICOP.pdf https://hdl.handle.net/10013/epic.39819.d001 Strauss, J. orcid:0000-0003-4678-4982 , Schirrmeister, L. orcid:0000-0001-9455-0596 , Wetterich, S. orcid:0000-0001-9234-1192 and Mangelsdorf, K. (2012) Old Organic Matter in Siberian Permafrost Deposits and its Degradation Features , Tenth International Conference on Permafrost - Resources and Risks of Permafrost Areas in a Changing World, Salekhard, Russia, 25 June 2012 - 29 June 2012 . hdl:10013/epic.39819 EPIC3Tenth International Conference on Permafrost - Resources and Risks of Permafrost Areas in a Changing World, Salekhard, Russia, 2012-06-25-2012-06-29Tyumen, Ekaterinburg, The Fort Dialog-Iset Publisher Conference notRev 2012 ftawi 2022-10-02T23:12:31Z Introduction During the late Quaternary, a large pool of organic matter (OM) accumulated in the arctic permafrost zone. Because of the potential re-introduction into the biogeochemical cycle from degrading permafrost, the OC inventory of ice-rich permafrost deposits and its degradation features are relevant to current concerns about the effects of global warming. The objectives of this paper are (1) to deduce the quality and quantity of OM stored in the studied sedi-ments and (2) to infer the paleoenvironmental condi-tions of the source biota. Therefore, standard sedimentological and a molecular marker (biomarker) approach are applied. Methods The study site is located on the west coast of the Buor Khaya Peninsula (N 71.6°, E 132.2°, Fig. 1), Yakutia (Russia). In Table 1 the used methods are summarized. Table 1. Applied methods Parameter Analyses and methods Radiocarbon age AMS 14C Grain size Diffraction Particle Size Ana-lyzer Bulk density Gas pycnometer OM characteristics (TOC, C/N, δ13C) Element analyses Mass -spectrometry Isotope signature of ground ice (δ18O, δ2H) Mass -spectrometry Biomarkers (brGDGT, archaeol, n-alkanes) HPLC-MS GC-MS Hydrobiochemistry (Acetate) Ion chromatography Results and Discussion Stratigraphically, two sediment units are distin-guished. The first unit is composed of late Pleistocene ice-rich permafrost (Yedoma). The second unit consists of Holocene thermokarst deposits. The mean bulk den-sity is ca. 1 10³kg/m³. The average total organic carbon (TOC) content is 2.4 wt% for Yedoma, 2.8 wt% for thermokarst deposits. The OM is low degraded (mean C/N 10) for mineral sediments. Hence, the deposits ac-cumulated at relatively fast rates and the OM underwent a short time of decomposition before it was incorporated into permafrost. The volumetric organic carbon contents of the Yedoma and thermokarst deposits are 13 ± 11 kg/m³ and 22 ± 11 kg/m³, re-spectively. This quantity is inside the range of comparable deposits studied by Schirrmeister et al. (2011). δ13C reveal a terrestrial signal ... Conference Object Arctic Global warming Ice permafrost Thermokarst Yakutia Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Arctic Khaya ENVELOPE(135.167,135.167,60.567,60.567) Buor-Khaya ENVELOPE(127.803,127.803,72.287,72.287) |
institution |
Open Polar |
collection |
Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
op_collection_id |
ftawi |
language |
unknown |
description |
Introduction During the late Quaternary, a large pool of organic matter (OM) accumulated in the arctic permafrost zone. Because of the potential re-introduction into the biogeochemical cycle from degrading permafrost, the OC inventory of ice-rich permafrost deposits and its degradation features are relevant to current concerns about the effects of global warming. The objectives of this paper are (1) to deduce the quality and quantity of OM stored in the studied sedi-ments and (2) to infer the paleoenvironmental condi-tions of the source biota. Therefore, standard sedimentological and a molecular marker (biomarker) approach are applied. Methods The study site is located on the west coast of the Buor Khaya Peninsula (N 71.6°, E 132.2°, Fig. 1), Yakutia (Russia). In Table 1 the used methods are summarized. Table 1. Applied methods Parameter Analyses and methods Radiocarbon age AMS 14C Grain size Diffraction Particle Size Ana-lyzer Bulk density Gas pycnometer OM characteristics (TOC, C/N, δ13C) Element analyses Mass -spectrometry Isotope signature of ground ice (δ18O, δ2H) Mass -spectrometry Biomarkers (brGDGT, archaeol, n-alkanes) HPLC-MS GC-MS Hydrobiochemistry (Acetate) Ion chromatography Results and Discussion Stratigraphically, two sediment units are distin-guished. The first unit is composed of late Pleistocene ice-rich permafrost (Yedoma). The second unit consists of Holocene thermokarst deposits. The mean bulk den-sity is ca. 1 10³kg/m³. The average total organic carbon (TOC) content is 2.4 wt% for Yedoma, 2.8 wt% for thermokarst deposits. The OM is low degraded (mean C/N 10) for mineral sediments. Hence, the deposits ac-cumulated at relatively fast rates and the OM underwent a short time of decomposition before it was incorporated into permafrost. The volumetric organic carbon contents of the Yedoma and thermokarst deposits are 13 ± 11 kg/m³ and 22 ± 11 kg/m³, re-spectively. This quantity is inside the range of comparable deposits studied by Schirrmeister et al. (2011). δ13C reveal a terrestrial signal ... |
format |
Conference Object |
author |
Strauss, Jens Schirrmeister, Lutz Wetterich, Sebastian Mangelsdorf, Kai |
spellingShingle |
Strauss, Jens Schirrmeister, Lutz Wetterich, Sebastian Mangelsdorf, Kai Old Organic Matter in Siberian Permafrost Deposits and its Degradation Features |
author_facet |
Strauss, Jens Schirrmeister, Lutz Wetterich, Sebastian Mangelsdorf, Kai |
author_sort |
Strauss, Jens |
title |
Old Organic Matter in Siberian Permafrost Deposits and its Degradation Features |
title_short |
Old Organic Matter in Siberian Permafrost Deposits and its Degradation Features |
title_full |
Old Organic Matter in Siberian Permafrost Deposits and its Degradation Features |
title_fullStr |
Old Organic Matter in Siberian Permafrost Deposits and its Degradation Features |
title_full_unstemmed |
Old Organic Matter in Siberian Permafrost Deposits and its Degradation Features |
title_sort |
old organic matter in siberian permafrost deposits and its degradation features |
publisher |
The Fort Dialog-Iset Publisher |
publishDate |
2012 |
url |
https://epic.awi.de/id/eprint/30849/ https://epic.awi.de/id/eprint/30849/1/Strauss_abstract_TICOP.pdf https://hdl.handle.net/10013/epic.39819 https://hdl.handle.net/10013/epic.39819.d001 |
long_lat |
ENVELOPE(135.167,135.167,60.567,60.567) ENVELOPE(127.803,127.803,72.287,72.287) |
geographic |
Arctic Khaya Buor-Khaya |
geographic_facet |
Arctic Khaya Buor-Khaya |
genre |
Arctic Global warming Ice permafrost Thermokarst Yakutia |
genre_facet |
Arctic Global warming Ice permafrost Thermokarst Yakutia |
op_source |
EPIC3Tenth International Conference on Permafrost - Resources and Risks of Permafrost Areas in a Changing World, Salekhard, Russia, 2012-06-25-2012-06-29Tyumen, Ekaterinburg, The Fort Dialog-Iset Publisher |
op_relation |
https://epic.awi.de/id/eprint/30849/1/Strauss_abstract_TICOP.pdf https://hdl.handle.net/10013/epic.39819.d001 Strauss, J. orcid:0000-0003-4678-4982 , Schirrmeister, L. orcid:0000-0001-9455-0596 , Wetterich, S. orcid:0000-0001-9234-1192 and Mangelsdorf, K. (2012) Old Organic Matter in Siberian Permafrost Deposits and its Degradation Features , Tenth International Conference on Permafrost - Resources and Risks of Permafrost Areas in a Changing World, Salekhard, Russia, 25 June 2012 - 29 June 2012 . hdl:10013/epic.39819 |
_version_ |
1766345492009058304 |