Response of the Methane Cycle to Climate Changes in the Past and Present
Artic permafrost environments play an important role within the global methane cycle. Thawing of permafrost and the associated release of this climate relevant trace gas, due to an increased microbial turnover of organic carbon and from ancient methane reservoirs, represent a potential risk to globa...
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ftawi:oai:epic.awi.de:20261 2024-09-15T18:29:39+00:00 Response of the Methane Cycle to Climate Changes in the Past and Present Griess, Juliane Mangelsdorf, K. Wagner, Dirk 2009 application/pdf https://epic.awi.de/id/eprint/20261/ https://epic.awi.de/id/eprint/20261/1/Gri2009c.pdf https://hdl.handle.net/10013/epic.32232 https://hdl.handle.net/10013/epic.32232.d001 unknown https://epic.awi.de/id/eprint/20261/1/Gri2009c.pdf https://hdl.handle.net/10013/epic.32232.d001 Griess, J. , Mangelsdorf, K. and Wagner, D. (2009) Response of the Methane Cycle to Climate Changes in the Past and Present , ICDP Kolloquium Potsdam, Potsdam, Germany, March 16-18 . hdl:10013/epic.32232 EPIC3ICDP Kolloquium Potsdam, Potsdam, Germany, March 16-18, 2009 p. Conference notRev 2009 ftawi 2024-06-24T04:01:09Z Artic permafrost environments play an important role within the global methane cycle. Thawing of permafrost and the associated release of this climate relevant trace gas, due to an increased microbial turnover of organic carbon and from ancient methane reservoirs, represent a potential risk to global warming. For the prediction of a future development of the permafrost environment and its contribution to the global atmospheric carbon budget, it is important to understand how this system reacted to environmental changes in the past. The Elgygytgyn lake region, Northeast Siberia, represents an ideal model system for studying the response of the methane cycle to climate change. It is supposed to be unglaciated since the time of a meteorite impact 3.6 Ma ago and since that time the permafrost went through four major climate-induced stages during the last 300,000 years. These changes in climate caused chemical and physical variations in sedimentary column and thus we expect changes in the composition of key microrganisms that were implicated in methane cycle. A 140 m long permafrost core from Elgygytgyn lake region was recovered within the ICDP project Scientific Drilling in Elgygytgyn Crater Lake in November 2008. Our studies will be conducted on combining microbial biomarker analyses and rRNA gene analyses in a high stratigraphic resolution. While rRNA gene sequences provide detailed informations on taxonomy, the extraction and analyses of microbial marker molecules are quantitative and correlate to cellular biomass. These two approaches are independent and thus can verify each others results. In addition to these studies, methane concentrations as well as the methane production and oxidation activity will be determined in the deposits. The obtained data will be interpreted in context of the results on inorganic properties in permafrost deposits of the Elgygytgyn lake region and paleoclimate reconstructions in this area provided by cooperation partners of the ICDP project Scientific Drilling at Elgygytgyn Crater ... Conference Object permafrost Siberia Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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description |
Artic permafrost environments play an important role within the global methane cycle. Thawing of permafrost and the associated release of this climate relevant trace gas, due to an increased microbial turnover of organic carbon and from ancient methane reservoirs, represent a potential risk to global warming. For the prediction of a future development of the permafrost environment and its contribution to the global atmospheric carbon budget, it is important to understand how this system reacted to environmental changes in the past. The Elgygytgyn lake region, Northeast Siberia, represents an ideal model system for studying the response of the methane cycle to climate change. It is supposed to be unglaciated since the time of a meteorite impact 3.6 Ma ago and since that time the permafrost went through four major climate-induced stages during the last 300,000 years. These changes in climate caused chemical and physical variations in sedimentary column and thus we expect changes in the composition of key microrganisms that were implicated in methane cycle. A 140 m long permafrost core from Elgygytgyn lake region was recovered within the ICDP project Scientific Drilling in Elgygytgyn Crater Lake in November 2008. Our studies will be conducted on combining microbial biomarker analyses and rRNA gene analyses in a high stratigraphic resolution. While rRNA gene sequences provide detailed informations on taxonomy, the extraction and analyses of microbial marker molecules are quantitative and correlate to cellular biomass. These two approaches are independent and thus can verify each others results. In addition to these studies, methane concentrations as well as the methane production and oxidation activity will be determined in the deposits. The obtained data will be interpreted in context of the results on inorganic properties in permafrost deposits of the Elgygytgyn lake region and paleoclimate reconstructions in this area provided by cooperation partners of the ICDP project Scientific Drilling at Elgygytgyn Crater ... |
format |
Conference Object |
author |
Griess, Juliane Mangelsdorf, K. Wagner, Dirk |
spellingShingle |
Griess, Juliane Mangelsdorf, K. Wagner, Dirk Response of the Methane Cycle to Climate Changes in the Past and Present |
author_facet |
Griess, Juliane Mangelsdorf, K. Wagner, Dirk |
author_sort |
Griess, Juliane |
title |
Response of the Methane Cycle to Climate Changes in the Past and Present |
title_short |
Response of the Methane Cycle to Climate Changes in the Past and Present |
title_full |
Response of the Methane Cycle to Climate Changes in the Past and Present |
title_fullStr |
Response of the Methane Cycle to Climate Changes in the Past and Present |
title_full_unstemmed |
Response of the Methane Cycle to Climate Changes in the Past and Present |
title_sort |
response of the methane cycle to climate changes in the past and present |
publishDate |
2009 |
url |
https://epic.awi.de/id/eprint/20261/ https://epic.awi.de/id/eprint/20261/1/Gri2009c.pdf https://hdl.handle.net/10013/epic.32232 https://hdl.handle.net/10013/epic.32232.d001 |
genre |
permafrost Siberia |
genre_facet |
permafrost Siberia |
op_source |
EPIC3ICDP Kolloquium Potsdam, Potsdam, Germany, March 16-18, 2009 p. |
op_relation |
https://epic.awi.de/id/eprint/20261/1/Gri2009c.pdf https://hdl.handle.net/10013/epic.32232.d001 Griess, J. , Mangelsdorf, K. and Wagner, D. (2009) Response of the Methane Cycle to Climate Changes in the Past and Present , ICDP Kolloquium Potsdam, Potsdam, Germany, March 16-18 . hdl:10013/epic.32232 |
_version_ |
1810471071160205312 |