Sediment sources and transport pathways on shelves of the Chukchi and East Siberian Seas: Evidence from the heavy minerals and garnet geochemistry
Study of sediment sources and transport pathways in the Chukchi and East Siberian Seas is vital for understanding the interaction of fluvial, ocean, and sea-ice dynamics. In this study, 42 samples were analyzed for heavy minerals and 23 were analyzed for garnet geochemistry. These analyses suggest t...
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ftnipr:oai:nipr.repo.nii.ac.jp:00016972 2023-05-15T13:24:37+02:00 Sediment sources and transport pathways on shelves of the Chukchi and East Siberian Seas: Evidence from the heavy minerals and garnet geochemistry 2022-09 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16972 http://id.nii.ac.jp/1291/00016841/ en eng https://doi.org/10.1016/j.polar.2022.100873 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16972 http://id.nii.ac.jp/1291/00016841/ Polar Science, 33, 100873(2022-09) 18739652 Heavy minerals Geochemistry of garnet Surface sediment Chukchi Sea East Siberian Sea Journal Article 2022 ftnipr https://doi.org/10.1016/j.polar.2022.100873 2022-12-03T19:43:26Z Study of sediment sources and transport pathways in the Chukchi and East Siberian Seas is vital for understanding the interaction of fluvial, ocean, and sea-ice dynamics. In this study, 42 samples were analyzed for heavy minerals and 23 were analyzed for garnet geochemistry. These analyses suggest that the surface sediment is mainly sourced from the surrounding rivers. There are distinctive performances between the heavy minerals and garnet geochemistry of sediments in the Chukchi Sea and the East Siberian Sea. The content of hypersthene increased significantly on the outer shelf of the Chukchi Sea. The garnet was derived from volcanic rocks of the Okhotsk-Chukotka volcanic province and transported from the Gulf of Anadyr by the Pacific inflow. Coastal erosion materials dominated in the inner shelf of the Chukchi Sea. A significant amount of river input occurred in the western, middle, and eastern parts of the East Siberian Sea. The inputs from the Indigirka River and Kolyma River tend to be distributed eastward. The garnet geochemistry shows that there was a mixed sedimentary zone located south of Wrangel Island. The sediments in the outer shelf of the East Siberian Sea show a stable mixed sedimentary environment. Article in Journal/Newspaper Anadyr Anadyr' Chukchi Chukchi Sea Chukotka East Siberian Sea kolyma river Polar Science Polar Science Sea ice Wrangel Island National Institute of Polar Research Repository, Japan Okhotsk Chukchi Sea Pacific Kolyma ENVELOPE(161.000,161.000,69.500,69.500) East Siberian Sea ENVELOPE(166.000,166.000,74.000,74.000) Wrangel Island ENVELOPE(-179.385,-179.385,71.244,71.244) Anadyr ENVELOPE(177.510,177.510,64.734,64.734) Anadyr’ ENVELOPE(176.233,176.233,64.882,64.882) Indigirka ENVELOPE(149.609,149.609,70.929,70.929) Polar Science 33 100873 |
institution |
Open Polar |
collection |
National Institute of Polar Research Repository, Japan |
op_collection_id |
ftnipr |
language |
English |
topic |
Heavy minerals Geochemistry of garnet Surface sediment Chukchi Sea East Siberian Sea |
spellingShingle |
Heavy minerals Geochemistry of garnet Surface sediment Chukchi Sea East Siberian Sea Sediment sources and transport pathways on shelves of the Chukchi and East Siberian Seas: Evidence from the heavy minerals and garnet geochemistry |
topic_facet |
Heavy minerals Geochemistry of garnet Surface sediment Chukchi Sea East Siberian Sea |
description |
Study of sediment sources and transport pathways in the Chukchi and East Siberian Seas is vital for understanding the interaction of fluvial, ocean, and sea-ice dynamics. In this study, 42 samples were analyzed for heavy minerals and 23 were analyzed for garnet geochemistry. These analyses suggest that the surface sediment is mainly sourced from the surrounding rivers. There are distinctive performances between the heavy minerals and garnet geochemistry of sediments in the Chukchi Sea and the East Siberian Sea. The content of hypersthene increased significantly on the outer shelf of the Chukchi Sea. The garnet was derived from volcanic rocks of the Okhotsk-Chukotka volcanic province and transported from the Gulf of Anadyr by the Pacific inflow. Coastal erosion materials dominated in the inner shelf of the Chukchi Sea. A significant amount of river input occurred in the western, middle, and eastern parts of the East Siberian Sea. The inputs from the Indigirka River and Kolyma River tend to be distributed eastward. The garnet geochemistry shows that there was a mixed sedimentary zone located south of Wrangel Island. The sediments in the outer shelf of the East Siberian Sea show a stable mixed sedimentary environment. |
format |
Article in Journal/Newspaper |
title |
Sediment sources and transport pathways on shelves of the Chukchi and East Siberian Seas: Evidence from the heavy minerals and garnet geochemistry |
title_short |
Sediment sources and transport pathways on shelves of the Chukchi and East Siberian Seas: Evidence from the heavy minerals and garnet geochemistry |
title_full |
Sediment sources and transport pathways on shelves of the Chukchi and East Siberian Seas: Evidence from the heavy minerals and garnet geochemistry |
title_fullStr |
Sediment sources and transport pathways on shelves of the Chukchi and East Siberian Seas: Evidence from the heavy minerals and garnet geochemistry |
title_full_unstemmed |
Sediment sources and transport pathways on shelves of the Chukchi and East Siberian Seas: Evidence from the heavy minerals and garnet geochemistry |
title_sort |
sediment sources and transport pathways on shelves of the chukchi and east siberian seas: evidence from the heavy minerals and garnet geochemistry |
publishDate |
2022 |
url |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16972 http://id.nii.ac.jp/1291/00016841/ |
long_lat |
ENVELOPE(161.000,161.000,69.500,69.500) ENVELOPE(166.000,166.000,74.000,74.000) ENVELOPE(-179.385,-179.385,71.244,71.244) ENVELOPE(177.510,177.510,64.734,64.734) ENVELOPE(176.233,176.233,64.882,64.882) ENVELOPE(149.609,149.609,70.929,70.929) |
geographic |
Okhotsk Chukchi Sea Pacific Kolyma East Siberian Sea Wrangel Island Anadyr Anadyr’ Indigirka |
geographic_facet |
Okhotsk Chukchi Sea Pacific Kolyma East Siberian Sea Wrangel Island Anadyr Anadyr’ Indigirka |
genre |
Anadyr Anadyr' Chukchi Chukchi Sea Chukotka East Siberian Sea kolyma river Polar Science Polar Science Sea ice Wrangel Island |
genre_facet |
Anadyr Anadyr' Chukchi Chukchi Sea Chukotka East Siberian Sea kolyma river Polar Science Polar Science Sea ice Wrangel Island |
op_relation |
https://doi.org/10.1016/j.polar.2022.100873 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=16972 http://id.nii.ac.jp/1291/00016841/ Polar Science, 33, 100873(2022-09) 18739652 |
op_doi |
https://doi.org/10.1016/j.polar.2022.100873 |
container_title |
Polar Science |
container_volume |
33 |
container_start_page |
100873 |
_version_ |
1766380592035790848 |