XRF down-core scanning and bulk chemistry measurements of sediments from the high latitude sectors of Pacific Ocean ...

Thirty marine sediment cores were collected from the subarctic Northwest Pacific (cruise SO264 with R/V SONNE in 2018), the central Drake Passage (cruise PS97 with RV Polarstern in 2016), the Pacific sector of the Southern Ocean (cruise PS75 in 2009/2010) and the Okhotsk Sea (cruise KOMEX I and KOME...

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Main Authors: Chao, Weng-si, Lee, An-Sheng, Tiedemann, Ralf, Lembke-Jene, Lester, Lamy, Frank
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2022
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.949225
https://doi.pangaea.de/10.1594/PANGAEA.949225
id ftdatacite:10.1594/pangaea.949225
record_format openpolar
spelling ftdatacite:10.1594/pangaea.949225 2024-06-09T07:45:37+00:00 XRF down-core scanning and bulk chemistry measurements of sediments from the high latitude sectors of Pacific Ocean ... Chao, Weng-si Lee, An-Sheng Tiedemann, Ralf Lembke-Jene, Lester Lamy, Frank 2022 application/zip https://dx.doi.org/10.1594/pangaea.949225 https://doi.pangaea.de/10.1594/PANGAEA.949225 en eng PANGAEA https://dx.doi.org/10.1038/s41598-022-25377-x Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CaCO3 content machine learning Marine Sediment Core Pacific Ocean Quantification total organic carbon TOC XRF scanning article Collection Bundled Publication of Datasets 2022 ftdatacite https://doi.org/10.1594/pangaea.94922510.1038/s41598-022-25377-x 2024-05-13T12:44:57Z Thirty marine sediment cores were collected from the subarctic Northwest Pacific (cruise SO264 with R/V SONNE in 2018), the central Drake Passage (cruise PS97 with RV Polarstern in 2016), the Pacific sector of the Southern Ocean (cruise PS75 in 2009/2010) and the Okhotsk Sea (cruise KOMEX I and KOMEX II with R/V Akademik Lavrentyev in 1998 and cruise SO178 in 2004). The cover area is mainly spreading over the high- to mid-latitude Northwest Pacific (37°N-52°N) and the Pacific sector of the Southern Ocean (53°S-63°S), with a water depth coverage from 1211 m to 4853 m. These cores are dominated by pelagic sediments and mainly consist of calcareous and siliceous ooze and non-carbonaceous fine-grained sediments. The drilling locates at the pelagic ocean rather than the nearby area to the shore to avoid too much influence of coastal erosion and fluvial input. The age range of the majority of the sediments spans from Holocene to mid-Pleistocene. All XRF-scanning measurements were carried out with an Avaatech XRF ... Article in Journal/Newspaper Drake Passage okhotsk sea Southern Ocean Subarctic DataCite Metadata Store (German National Library of Science and Technology) Drake Passage Okhotsk Pacific Southern Ocean
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic CaCO3 content
machine learning
Marine Sediment Core
Pacific Ocean
Quantification
total organic carbon TOC
XRF scanning
spellingShingle CaCO3 content
machine learning
Marine Sediment Core
Pacific Ocean
Quantification
total organic carbon TOC
XRF scanning
Chao, Weng-si
Lee, An-Sheng
Tiedemann, Ralf
Lembke-Jene, Lester
Lamy, Frank
XRF down-core scanning and bulk chemistry measurements of sediments from the high latitude sectors of Pacific Ocean ...
topic_facet CaCO3 content
machine learning
Marine Sediment Core
Pacific Ocean
Quantification
total organic carbon TOC
XRF scanning
description Thirty marine sediment cores were collected from the subarctic Northwest Pacific (cruise SO264 with R/V SONNE in 2018), the central Drake Passage (cruise PS97 with RV Polarstern in 2016), the Pacific sector of the Southern Ocean (cruise PS75 in 2009/2010) and the Okhotsk Sea (cruise KOMEX I and KOMEX II with R/V Akademik Lavrentyev in 1998 and cruise SO178 in 2004). The cover area is mainly spreading over the high- to mid-latitude Northwest Pacific (37°N-52°N) and the Pacific sector of the Southern Ocean (53°S-63°S), with a water depth coverage from 1211 m to 4853 m. These cores are dominated by pelagic sediments and mainly consist of calcareous and siliceous ooze and non-carbonaceous fine-grained sediments. The drilling locates at the pelagic ocean rather than the nearby area to the shore to avoid too much influence of coastal erosion and fluvial input. The age range of the majority of the sediments spans from Holocene to mid-Pleistocene. All XRF-scanning measurements were carried out with an Avaatech XRF ...
format Article in Journal/Newspaper
author Chao, Weng-si
Lee, An-Sheng
Tiedemann, Ralf
Lembke-Jene, Lester
Lamy, Frank
author_facet Chao, Weng-si
Lee, An-Sheng
Tiedemann, Ralf
Lembke-Jene, Lester
Lamy, Frank
author_sort Chao, Weng-si
title XRF down-core scanning and bulk chemistry measurements of sediments from the high latitude sectors of Pacific Ocean ...
title_short XRF down-core scanning and bulk chemistry measurements of sediments from the high latitude sectors of Pacific Ocean ...
title_full XRF down-core scanning and bulk chemistry measurements of sediments from the high latitude sectors of Pacific Ocean ...
title_fullStr XRF down-core scanning and bulk chemistry measurements of sediments from the high latitude sectors of Pacific Ocean ...
title_full_unstemmed XRF down-core scanning and bulk chemistry measurements of sediments from the high latitude sectors of Pacific Ocean ...
title_sort xrf down-core scanning and bulk chemistry measurements of sediments from the high latitude sectors of pacific ocean ...
publisher PANGAEA
publishDate 2022
url https://dx.doi.org/10.1594/pangaea.949225
https://doi.pangaea.de/10.1594/PANGAEA.949225
geographic Drake Passage
Okhotsk
Pacific
Southern Ocean
geographic_facet Drake Passage
Okhotsk
Pacific
Southern Ocean
genre Drake Passage
okhotsk sea
Southern Ocean
Subarctic
genre_facet Drake Passage
okhotsk sea
Southern Ocean
Subarctic
op_relation https://dx.doi.org/10.1038/s41598-022-25377-x
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.1594/pangaea.94922510.1038/s41598-022-25377-x
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