Clay Mineral Cycles Identified by Diffuse Spectral Reflectance in Quaternary Sediments From the Northwind Ridge: Implications for Glacial-Interglacial Sedimentation Patterns in the Arctic Ocean
A Quaternary record of fine-grained sediment composition is used to investigate Arctic Ocean climate variability on glacial-interglacial time scales. Diffuse spectral reflectance data from sediment core P1-92AR-P25 from the Northwind Ridge, north of Alaska, demonstrates cyclic variations in mineralo...
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2010
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ftolddominionuni:oai:digitalcommons.odu.edu:oeas_fac_pubs-1035 2023-06-11T04:08:20+02:00 Clay Mineral Cycles Identified by Diffuse Spectral Reflectance in Quaternary Sediments From the Northwind Ridge: Implications for Glacial-Interglacial Sedimentation Patterns in the Arctic Ocean Yurco, Lyanne N. Ortiz, Joseph D. Polyak, Leonid Darby, Dennis A. Crawford, Kevin A. 2010-08-01T07:00:00Z application/pdf https://digitalcommons.odu.edu/oeas_fac_pubs/31 https://doi.org/10.1111/j.1751-8369.2010.00160.x https://digitalcommons.odu.edu/context/oeas_fac_pubs/article/1035/viewcontent/Yurco_2010_Clay_mineral_cycles.pdf unknown ODU Digital Commons https://digitalcommons.odu.edu/oeas_fac_pubs/31 doi:10.1111/j.1751-8369.2010.00160.x https://digitalcommons.odu.edu/context/oeas_fac_pubs/article/1035/viewcontent/Yurco_2010_Clay_mineral_cycles.pdf OES Faculty Publications Arctic Ocean Quaternary palaeoclimate Arctic oscillation Clay mineral provenance Glacial interglacial cycles Diffuse spectral reflectance R mode factor analysis Sea-ice motion Surface sediments Late Pleistocene Extratropical circulation Thermohaline circulation Atlantic oscillation Transport pathways Chukchi Borderland Northern Eurasia Mendeleev Ridge Environmental Sciences Geology Oceanography article 2010 ftolddominionuni https://doi.org/10.1111/j.1751-8369.2010.00160.x 2023-05-08T17:59:31Z A Quaternary record of fine-grained sediment composition is used to investigate Arctic Ocean climate variability on glacial-interglacial time scales. Diffuse spectral reflectance data from sediment core P1-92AR-P25 from the Northwind Ridge, north of Alaska, demonstrates cyclic variations in mineralogy. Varimax-rotated R-mode factor analysis of down-core data revealed three major mineralogical assemblages, which were then compared with the content of manganese, a proxy for basin ventilation, and thus glacial-interglacial cycles. Results indicate that factor 1, a smectite + chlorite clay assemblage, was delivered to the core site during interglacials, either by fluvial discharge or sea-ice drift from Siberian rivers or inflow from the Bering Sea. Factor 2, an illite + goethite assemblage, is related to glacial periods, and was probably transported from the Laurentide Ice Sheet by icebergs or meltwater. Factor 3, glauconite, might have been sourced from the North Slope region of Alaska during deglacial intervals, or from dolomites associated with Laurentide iceberg-discharge pulses. The observed variations in sediment source and transport mechanisms arise from glacial-interglacial changes in sea level, the size of the terrestrial ice sheets surrounding the Arctic Ocean, the extent of sea-ice cover and altered atmospheric circulation. The reconstructed glacial-interglacial circulation patterns from the Late Quaternary show some similarity with modern circulation changes presumably related to the monthly- to decadally-fluctuating Arctic Oscillation. However, because the Arctic Oscillation operates on much shorter time scales, further research is necessary to better understand the driving mechanism for the changes observed over glacial-interglacial cycles, and the potential role of ocean-atmospheric interaction. Article in Journal/Newspaper Arctic Arctic Ocean Bering Sea Chukchi Ice Sheet Iceberg* north slope Sea ice Alaska Old Dominion University: ODU Digital Commons Arctic Arctic Ocean Bering Sea Chukchi Borderland ENVELOPE(-165.000,-165.000,77.000,77.000) Polar Research 29 2 176 197 |
institution |
Open Polar |
collection |
Old Dominion University: ODU Digital Commons |
op_collection_id |
ftolddominionuni |
language |
unknown |
topic |
Arctic Ocean Quaternary palaeoclimate Arctic oscillation Clay mineral provenance Glacial interglacial cycles Diffuse spectral reflectance R mode factor analysis Sea-ice motion Surface sediments Late Pleistocene Extratropical circulation Thermohaline circulation Atlantic oscillation Transport pathways Chukchi Borderland Northern Eurasia Mendeleev Ridge Environmental Sciences Geology Oceanography |
spellingShingle |
Arctic Ocean Quaternary palaeoclimate Arctic oscillation Clay mineral provenance Glacial interglacial cycles Diffuse spectral reflectance R mode factor analysis Sea-ice motion Surface sediments Late Pleistocene Extratropical circulation Thermohaline circulation Atlantic oscillation Transport pathways Chukchi Borderland Northern Eurasia Mendeleev Ridge Environmental Sciences Geology Oceanography Yurco, Lyanne N. Ortiz, Joseph D. Polyak, Leonid Darby, Dennis A. Crawford, Kevin A. Clay Mineral Cycles Identified by Diffuse Spectral Reflectance in Quaternary Sediments From the Northwind Ridge: Implications for Glacial-Interglacial Sedimentation Patterns in the Arctic Ocean |
topic_facet |
Arctic Ocean Quaternary palaeoclimate Arctic oscillation Clay mineral provenance Glacial interglacial cycles Diffuse spectral reflectance R mode factor analysis Sea-ice motion Surface sediments Late Pleistocene Extratropical circulation Thermohaline circulation Atlantic oscillation Transport pathways Chukchi Borderland Northern Eurasia Mendeleev Ridge Environmental Sciences Geology Oceanography |
description |
A Quaternary record of fine-grained sediment composition is used to investigate Arctic Ocean climate variability on glacial-interglacial time scales. Diffuse spectral reflectance data from sediment core P1-92AR-P25 from the Northwind Ridge, north of Alaska, demonstrates cyclic variations in mineralogy. Varimax-rotated R-mode factor analysis of down-core data revealed three major mineralogical assemblages, which were then compared with the content of manganese, a proxy for basin ventilation, and thus glacial-interglacial cycles. Results indicate that factor 1, a smectite + chlorite clay assemblage, was delivered to the core site during interglacials, either by fluvial discharge or sea-ice drift from Siberian rivers or inflow from the Bering Sea. Factor 2, an illite + goethite assemblage, is related to glacial periods, and was probably transported from the Laurentide Ice Sheet by icebergs or meltwater. Factor 3, glauconite, might have been sourced from the North Slope region of Alaska during deglacial intervals, or from dolomites associated with Laurentide iceberg-discharge pulses. The observed variations in sediment source and transport mechanisms arise from glacial-interglacial changes in sea level, the size of the terrestrial ice sheets surrounding the Arctic Ocean, the extent of sea-ice cover and altered atmospheric circulation. The reconstructed glacial-interglacial circulation patterns from the Late Quaternary show some similarity with modern circulation changes presumably related to the monthly- to decadally-fluctuating Arctic Oscillation. However, because the Arctic Oscillation operates on much shorter time scales, further research is necessary to better understand the driving mechanism for the changes observed over glacial-interglacial cycles, and the potential role of ocean-atmospheric interaction. |
format |
Article in Journal/Newspaper |
author |
Yurco, Lyanne N. Ortiz, Joseph D. Polyak, Leonid Darby, Dennis A. Crawford, Kevin A. |
author_facet |
Yurco, Lyanne N. Ortiz, Joseph D. Polyak, Leonid Darby, Dennis A. Crawford, Kevin A. |
author_sort |
Yurco, Lyanne N. |
title |
Clay Mineral Cycles Identified by Diffuse Spectral Reflectance in Quaternary Sediments From the Northwind Ridge: Implications for Glacial-Interglacial Sedimentation Patterns in the Arctic Ocean |
title_short |
Clay Mineral Cycles Identified by Diffuse Spectral Reflectance in Quaternary Sediments From the Northwind Ridge: Implications for Glacial-Interglacial Sedimentation Patterns in the Arctic Ocean |
title_full |
Clay Mineral Cycles Identified by Diffuse Spectral Reflectance in Quaternary Sediments From the Northwind Ridge: Implications for Glacial-Interglacial Sedimentation Patterns in the Arctic Ocean |
title_fullStr |
Clay Mineral Cycles Identified by Diffuse Spectral Reflectance in Quaternary Sediments From the Northwind Ridge: Implications for Glacial-Interglacial Sedimentation Patterns in the Arctic Ocean |
title_full_unstemmed |
Clay Mineral Cycles Identified by Diffuse Spectral Reflectance in Quaternary Sediments From the Northwind Ridge: Implications for Glacial-Interglacial Sedimentation Patterns in the Arctic Ocean |
title_sort |
clay mineral cycles identified by diffuse spectral reflectance in quaternary sediments from the northwind ridge: implications for glacial-interglacial sedimentation patterns in the arctic ocean |
publisher |
ODU Digital Commons |
publishDate |
2010 |
url |
https://digitalcommons.odu.edu/oeas_fac_pubs/31 https://doi.org/10.1111/j.1751-8369.2010.00160.x https://digitalcommons.odu.edu/context/oeas_fac_pubs/article/1035/viewcontent/Yurco_2010_Clay_mineral_cycles.pdf |
long_lat |
ENVELOPE(-165.000,-165.000,77.000,77.000) |
geographic |
Arctic Arctic Ocean Bering Sea Chukchi Borderland |
geographic_facet |
Arctic Arctic Ocean Bering Sea Chukchi Borderland |
genre |
Arctic Arctic Ocean Bering Sea Chukchi Ice Sheet Iceberg* north slope Sea ice Alaska |
genre_facet |
Arctic Arctic Ocean Bering Sea Chukchi Ice Sheet Iceberg* north slope Sea ice Alaska |
op_source |
OES Faculty Publications |
op_relation |
https://digitalcommons.odu.edu/oeas_fac_pubs/31 doi:10.1111/j.1751-8369.2010.00160.x https://digitalcommons.odu.edu/context/oeas_fac_pubs/article/1035/viewcontent/Yurco_2010_Clay_mineral_cycles.pdf |
op_doi |
https://doi.org/10.1111/j.1751-8369.2010.00160.x |
container_title |
Polar Research |
container_volume |
29 |
container_issue |
2 |
container_start_page |
176 |
op_container_end_page |
197 |
_version_ |
1768381560627658752 |