Clay minerals in response to the Pleistocene climate change on the Yermak Plateau, Arctic Ocean (ODP, Site 911)
Abstract The Arctic plays an important role in controlling the Earth's climate and ocean circulation. Studies of past climate conditions in high latitudes are important to understand this role more precisely. Clay mineralogy of sediments was detected to be comparative with cyclic changes in cli...
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Cambridge University Press (CUP)
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Online Access: | http://dx.doi.org/10.1017/s0032247400017770 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0032247400017770 |
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crcambridgeupr:10.1017/s0032247400017770 2024-03-03T08:41:33+00:00 Clay minerals in response to the Pleistocene climate change on the Yermak Plateau, Arctic Ocean (ODP, Site 911) Ruikka, Mattiina Strand, Kari 2002 http://dx.doi.org/10.1017/s0032247400017770 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0032247400017770 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Polar Record volume 38, issue 206, page 241-248 ISSN 0032-2474 1475-3057 General Earth and Planetary Sciences Ecology Geography, Planning and Development journal-article 2002 crcambridgeupr https://doi.org/10.1017/s0032247400017770 2024-02-08T08:29:13Z Abstract The Arctic plays an important role in controlling the Earth's climate and ocean circulation. Studies of past climate conditions in high latitudes are important to understand this role more precisely. Clay mineralogy of sediments was detected to be comparative with cyclic changes in climatic conditions during the past 0.8 Ma in the northernmost Atlantic-Arctic gateway (Ocean Drilling Program, Site 911). Clay minerals are transported by sea ice, icebergs, glaciofluvially, or by ocean currents. Smectite is assumed to be transported predominantly during interglacial periods. Its content decreases from about 0.4 Ma to the present, which may indicate lesser eroded smectite in the provenance area, assumed to be mostly in the Laptev Sea. Illite is due to erosion from Svalbard during glacial periods, and shows a negative correlation with smectite. Chlorite is not a good climate indicator because of its high frequency in the northern regions. Zemlya Frantsa-Iosifa (Franz Josef Land) is the most likely source area of kaolinite and the output seems to have slightly increased from 0.5 to 0.4 Ma. The correlation of kaolinite and chlorite means coincidental sedimentation. Kaolinite and chlorite are negatively correlated with illite, which indicates transportation during the more open ocean conditions that prevailed between repeated Pleistocene glaciations. Article in Journal/Newspaper Arctic Arctic Ocean Atlantic Arctic Atlantic-Arctic Climate change Franz Josef Land Iceberg* Polar Record Sea ice Svalbard Yermak plateau Cambridge University Press Arctic Arctic Ocean Svalbard Laptev Sea Yermak Plateau ENVELOPE(5.000,5.000,81.250,81.250) Franz Josef Land ENVELOPE(55.000,55.000,81.000,81.000) Polar Record 38 206 241 248 |
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Open Polar |
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Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
General Earth and Planetary Sciences Ecology Geography, Planning and Development |
spellingShingle |
General Earth and Planetary Sciences Ecology Geography, Planning and Development Ruikka, Mattiina Strand, Kari Clay minerals in response to the Pleistocene climate change on the Yermak Plateau, Arctic Ocean (ODP, Site 911) |
topic_facet |
General Earth and Planetary Sciences Ecology Geography, Planning and Development |
description |
Abstract The Arctic plays an important role in controlling the Earth's climate and ocean circulation. Studies of past climate conditions in high latitudes are important to understand this role more precisely. Clay mineralogy of sediments was detected to be comparative with cyclic changes in climatic conditions during the past 0.8 Ma in the northernmost Atlantic-Arctic gateway (Ocean Drilling Program, Site 911). Clay minerals are transported by sea ice, icebergs, glaciofluvially, or by ocean currents. Smectite is assumed to be transported predominantly during interglacial periods. Its content decreases from about 0.4 Ma to the present, which may indicate lesser eroded smectite in the provenance area, assumed to be mostly in the Laptev Sea. Illite is due to erosion from Svalbard during glacial periods, and shows a negative correlation with smectite. Chlorite is not a good climate indicator because of its high frequency in the northern regions. Zemlya Frantsa-Iosifa (Franz Josef Land) is the most likely source area of kaolinite and the output seems to have slightly increased from 0.5 to 0.4 Ma. The correlation of kaolinite and chlorite means coincidental sedimentation. Kaolinite and chlorite are negatively correlated with illite, which indicates transportation during the more open ocean conditions that prevailed between repeated Pleistocene glaciations. |
format |
Article in Journal/Newspaper |
author |
Ruikka, Mattiina Strand, Kari |
author_facet |
Ruikka, Mattiina Strand, Kari |
author_sort |
Ruikka, Mattiina |
title |
Clay minerals in response to the Pleistocene climate change on the Yermak Plateau, Arctic Ocean (ODP, Site 911) |
title_short |
Clay minerals in response to the Pleistocene climate change on the Yermak Plateau, Arctic Ocean (ODP, Site 911) |
title_full |
Clay minerals in response to the Pleistocene climate change on the Yermak Plateau, Arctic Ocean (ODP, Site 911) |
title_fullStr |
Clay minerals in response to the Pleistocene climate change on the Yermak Plateau, Arctic Ocean (ODP, Site 911) |
title_full_unstemmed |
Clay minerals in response to the Pleistocene climate change on the Yermak Plateau, Arctic Ocean (ODP, Site 911) |
title_sort |
clay minerals in response to the pleistocene climate change on the yermak plateau, arctic ocean (odp, site 911) |
publisher |
Cambridge University Press (CUP) |
publishDate |
2002 |
url |
http://dx.doi.org/10.1017/s0032247400017770 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0032247400017770 |
long_lat |
ENVELOPE(5.000,5.000,81.250,81.250) ENVELOPE(55.000,55.000,81.000,81.000) |
geographic |
Arctic Arctic Ocean Svalbard Laptev Sea Yermak Plateau Franz Josef Land |
geographic_facet |
Arctic Arctic Ocean Svalbard Laptev Sea Yermak Plateau Franz Josef Land |
genre |
Arctic Arctic Ocean Atlantic Arctic Atlantic-Arctic Climate change Franz Josef Land Iceberg* Polar Record Sea ice Svalbard Yermak plateau |
genre_facet |
Arctic Arctic Ocean Atlantic Arctic Atlantic-Arctic Climate change Franz Josef Land Iceberg* Polar Record Sea ice Svalbard Yermak plateau |
op_source |
Polar Record volume 38, issue 206, page 241-248 ISSN 0032-2474 1475-3057 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0032247400017770 |
container_title |
Polar Record |
container_volume |
38 |
container_issue |
206 |
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241 |
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248 |
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1792497245615030272 |