Stable isotopes of carbon (δ13C-DIC) and oxygen (δ18O-H2O) in the western Arctic Ocean (2021)

Stable isotopes of carbon (δ13C-DIC) and oxygen (δ18O-H2O) are two essential tracers that help understand the changing Arctic water masses and carbon cycles. However, the interplay of physical, chemical, and biological factors and their influence on δ13C-DIC in the Arctic Ocean are poorly understood...

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Main Authors: Zhangxian Ouyang, Wei-Jun Cai
Format: Dataset
Language:unknown
Published: Arctic Data Center 2023
Subjects:
Online Access:https://doi.org/10.18739/A27659H17
id dataone:doi:10.18739/A27659H17
record_format openpolar
spelling dataone:doi:10.18739/A27659H17 2023-11-08T14:14:16+01:00 Stable isotopes of carbon (δ13C-DIC) and oxygen (δ18O-H2O) in the western Arctic Ocean (2021) Zhangxian Ouyang Wei-Jun Cai The sampling stations mainly cover the central and eastern Chukchi Sea, extending from the Bering Strait to the southwestern Canada Basin. ENVELOPE(-175.0,-150.0,75.0,64.0) BEGINDATE: 2021-09-12T00:00:00Z ENDDATE: 2021-10-02T00:00:00Z 2023-01-01T00:00:00Z https://doi.org/10.18739/A27659H17 unknown Arctic Data Center δ13C-DIC δ18O-H2O western Arctic Ocean Dataset 2023 dataone:urn:node:ARCTIC https://doi.org/10.18739/A27659H17 2023-11-08T13:48:47Z Stable isotopes of carbon (δ13C-DIC) and oxygen (δ18O-H2O) are two essential tracers that help understand the changing Arctic water masses and carbon cycles. However, the interplay of physical, chemical, and biological factors and their influence on δ13C-DIC in the Arctic Ocean are poorly understood. Therefore, we investigated the distributions of δ13C-DIC and δ18O-H2O in the western Arctic Ocean during the Mirai 2021 cruise from September 12th to October 2nd under the framework of the Arctic Challenge for Sustainability II Project (ArCS II). Here we present the dataset of δ13C-DIC and δ18O-H2O, which covers the central and eastern Chukchi Sea, extending from the Bering Strait to the southwestern Canada Basin. Combined with other hydrographic and biogeochemical parameters, δ18O-H2O samples could be used to decipher and quantify the contributions of source water masses in each sample. δ13C-DIC samples could be helpful to better understand the carbon export pathways and partition of potential carbon sources. The observations of δ18O-H2O and δ13C-DIC facilitate a better understanding of the carbon flows, exports, and degradation from highly productive shelves to oligotrophic basins, and thus a better prediction of future changes in the Arctic carbon dynamics. Dataset Arctic Arctic Ocean Bering Strait canada basin Chukchi Chukchi Sea Arctic Data Center (via DataONE) Arctic Arctic Ocean Chukchi Sea Bering Strait Canada ENVELOPE(-175.0,-150.0,75.0,64.0)
institution Open Polar
collection Arctic Data Center (via DataONE)
op_collection_id dataone:urn:node:ARCTIC
language unknown
topic δ13C-DIC
δ18O-H2O
western Arctic Ocean
spellingShingle δ13C-DIC
δ18O-H2O
western Arctic Ocean
Zhangxian Ouyang
Wei-Jun Cai
Stable isotopes of carbon (δ13C-DIC) and oxygen (δ18O-H2O) in the western Arctic Ocean (2021)
topic_facet δ13C-DIC
δ18O-H2O
western Arctic Ocean
description Stable isotopes of carbon (δ13C-DIC) and oxygen (δ18O-H2O) are two essential tracers that help understand the changing Arctic water masses and carbon cycles. However, the interplay of physical, chemical, and biological factors and their influence on δ13C-DIC in the Arctic Ocean are poorly understood. Therefore, we investigated the distributions of δ13C-DIC and δ18O-H2O in the western Arctic Ocean during the Mirai 2021 cruise from September 12th to October 2nd under the framework of the Arctic Challenge for Sustainability II Project (ArCS II). Here we present the dataset of δ13C-DIC and δ18O-H2O, which covers the central and eastern Chukchi Sea, extending from the Bering Strait to the southwestern Canada Basin. Combined with other hydrographic and biogeochemical parameters, δ18O-H2O samples could be used to decipher and quantify the contributions of source water masses in each sample. δ13C-DIC samples could be helpful to better understand the carbon export pathways and partition of potential carbon sources. The observations of δ18O-H2O and δ13C-DIC facilitate a better understanding of the carbon flows, exports, and degradation from highly productive shelves to oligotrophic basins, and thus a better prediction of future changes in the Arctic carbon dynamics.
format Dataset
author Zhangxian Ouyang
Wei-Jun Cai
author_facet Zhangxian Ouyang
Wei-Jun Cai
author_sort Zhangxian Ouyang
title Stable isotopes of carbon (δ13C-DIC) and oxygen (δ18O-H2O) in the western Arctic Ocean (2021)
title_short Stable isotopes of carbon (δ13C-DIC) and oxygen (δ18O-H2O) in the western Arctic Ocean (2021)
title_full Stable isotopes of carbon (δ13C-DIC) and oxygen (δ18O-H2O) in the western Arctic Ocean (2021)
title_fullStr Stable isotopes of carbon (δ13C-DIC) and oxygen (δ18O-H2O) in the western Arctic Ocean (2021)
title_full_unstemmed Stable isotopes of carbon (δ13C-DIC) and oxygen (δ18O-H2O) in the western Arctic Ocean (2021)
title_sort stable isotopes of carbon (δ13c-dic) and oxygen (δ18o-h2o) in the western arctic ocean (2021)
publisher Arctic Data Center
publishDate 2023
url https://doi.org/10.18739/A27659H17
op_coverage The sampling stations mainly cover the central and eastern Chukchi Sea, extending from the Bering Strait to the southwestern Canada Basin.
ENVELOPE(-175.0,-150.0,75.0,64.0)
BEGINDATE: 2021-09-12T00:00:00Z ENDDATE: 2021-10-02T00:00:00Z
long_lat ENVELOPE(-175.0,-150.0,75.0,64.0)
geographic Arctic
Arctic Ocean
Chukchi Sea
Bering Strait
Canada
geographic_facet Arctic
Arctic Ocean
Chukchi Sea
Bering Strait
Canada
genre Arctic
Arctic Ocean
Bering Strait
canada basin
Chukchi
Chukchi Sea
genre_facet Arctic
Arctic Ocean
Bering Strait
canada basin
Chukchi
Chukchi Sea
op_doi https://doi.org/10.18739/A27659H17
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