VARIATION OF GLACIAL-INTERGLACIAL MARINE SILICON ISOTOPIC COMPOSITIONS AND ITS POSSIBLE IMPLICATIONS—A MODELING STUDY
Silicon isotopic composition (δ30Si) is a promising proxy for reconstruction of marine silicic acid utilization and Si cycling in the geological past. It has been applied extensively in the Southern Ocean in order to investigate the glacial-interglacial physical and biological cycles and the pCO2 va...
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ftawi:oai:epic.awi.de:35332 2024-09-15T18:37:13+00:00 VARIATION OF GLACIAL-INTERGLACIAL MARINE SILICON ISOTOPIC COMPOSITIONS AND ITS POSSIBLE IMPLICATIONS—A MODELING STUDY Gao, Shuang Völker, Christoph Lohmann, Gerrit Butzin, Martin Wolf-Gladrow, Dieter 2014-02-25 https://epic.awi.de/id/eprint/35332/ http://www.sgmeet.com/osm2014/viewabstract.asp?AbstractID=16048 https://hdl.handle.net/10013/epic.43334 unknown Gao, S. , Völker, C. orcid:0000-0003-3032-114X , Lohmann, G. orcid:0000-0003-2089-733X , Butzin, M. orcid:0000-0002-9275-7304 and Wolf-Gladrow, D. orcid:0000-0001-9531-8668 (2014) VARIATION OF GLACIAL-INTERGLACIAL MARINE SILICON ISOTOPIC COMPOSITIONS AND ITS POSSIBLE IMPLICATIONS—A MODELING STUDY , Ocean Sciences Meeting, Honolulu, Hawaii, USA, 24 February 2014 - 28 February 2014 . hdl:10013/epic.43334 EPIC3Ocean Sciences Meeting, Honolulu, Hawaii, USA, 2014-02-24-2014-02-28 Conference notRev 2014 ftawi 2024-06-24T04:09:53Z Silicon isotopic composition (δ30Si) is a promising proxy for reconstruction of marine silicic acid utilization and Si cycling in the geological past. It has been applied extensively in the Southern Ocean in order to investigate the glacial-interglacial physical and biological cycles and the pCO2 variations. Our aim is to compare the glacial-interglacial δ30Si distributions of silicic acid and biogenic opal in the oceans and in marine sediments and to further evaluate the influence on δ30Si by the glacial-interglacial variations of ocean circulation, dust deposition, riverine Si flux and its δ30Si. To simulate the Si biogeochemical cycle and Si isotopic compositions under the Last Glacial Maximum (LGM) conditions, we applied the Ocean General Circulation Model (MPI-OM) under the LGM atmospheric forcing and dust deposition and applied the Hamburg Ocean Carbon Cycle Model (HAMOCC5.1) which includes an interactive sediment module. Finally, the pre-industrial and glacial water masses are identified and the Si cycling (including δ30Si) is compared to proxy data. Conference Object Southern Ocean 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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ftawi |
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description |
Silicon isotopic composition (δ30Si) is a promising proxy for reconstruction of marine silicic acid utilization and Si cycling in the geological past. It has been applied extensively in the Southern Ocean in order to investigate the glacial-interglacial physical and biological cycles and the pCO2 variations. Our aim is to compare the glacial-interglacial δ30Si distributions of silicic acid and biogenic opal in the oceans and in marine sediments and to further evaluate the influence on δ30Si by the glacial-interglacial variations of ocean circulation, dust deposition, riverine Si flux and its δ30Si. To simulate the Si biogeochemical cycle and Si isotopic compositions under the Last Glacial Maximum (LGM) conditions, we applied the Ocean General Circulation Model (MPI-OM) under the LGM atmospheric forcing and dust deposition and applied the Hamburg Ocean Carbon Cycle Model (HAMOCC5.1) which includes an interactive sediment module. Finally, the pre-industrial and glacial water masses are identified and the Si cycling (including δ30Si) is compared to proxy data. |
format |
Conference Object |
author |
Gao, Shuang Völker, Christoph Lohmann, Gerrit Butzin, Martin Wolf-Gladrow, Dieter |
spellingShingle |
Gao, Shuang Völker, Christoph Lohmann, Gerrit Butzin, Martin Wolf-Gladrow, Dieter VARIATION OF GLACIAL-INTERGLACIAL MARINE SILICON ISOTOPIC COMPOSITIONS AND ITS POSSIBLE IMPLICATIONS—A MODELING STUDY |
author_facet |
Gao, Shuang Völker, Christoph Lohmann, Gerrit Butzin, Martin Wolf-Gladrow, Dieter |
author_sort |
Gao, Shuang |
title |
VARIATION OF GLACIAL-INTERGLACIAL MARINE SILICON ISOTOPIC COMPOSITIONS AND ITS POSSIBLE IMPLICATIONS—A MODELING STUDY |
title_short |
VARIATION OF GLACIAL-INTERGLACIAL MARINE SILICON ISOTOPIC COMPOSITIONS AND ITS POSSIBLE IMPLICATIONS—A MODELING STUDY |
title_full |
VARIATION OF GLACIAL-INTERGLACIAL MARINE SILICON ISOTOPIC COMPOSITIONS AND ITS POSSIBLE IMPLICATIONS—A MODELING STUDY |
title_fullStr |
VARIATION OF GLACIAL-INTERGLACIAL MARINE SILICON ISOTOPIC COMPOSITIONS AND ITS POSSIBLE IMPLICATIONS—A MODELING STUDY |
title_full_unstemmed |
VARIATION OF GLACIAL-INTERGLACIAL MARINE SILICON ISOTOPIC COMPOSITIONS AND ITS POSSIBLE IMPLICATIONS—A MODELING STUDY |
title_sort |
variation of glacial-interglacial marine silicon isotopic compositions and its possible implications—a modeling study |
publishDate |
2014 |
url |
https://epic.awi.de/id/eprint/35332/ http://www.sgmeet.com/osm2014/viewabstract.asp?AbstractID=16048 https://hdl.handle.net/10013/epic.43334 |
genre |
Southern Ocean |
genre_facet |
Southern Ocean |
op_source |
EPIC3Ocean Sciences Meeting, Honolulu, Hawaii, USA, 2014-02-24-2014-02-28 |
op_relation |
Gao, S. , Völker, C. orcid:0000-0003-3032-114X , Lohmann, G. orcid:0000-0003-2089-733X , Butzin, M. orcid:0000-0002-9275-7304 and Wolf-Gladrow, D. orcid:0000-0001-9531-8668 (2014) VARIATION OF GLACIAL-INTERGLACIAL MARINE SILICON ISOTOPIC COMPOSITIONS AND ITS POSSIBLE IMPLICATIONS—A MODELING STUDY , Ocean Sciences Meeting, Honolulu, Hawaii, USA, 24 February 2014 - 28 February 2014 . hdl:10013/epic.43334 |
_version_ |
1810481561564348416 |