Data on dissolved organic matter, sea ice and environment in surface water of Antarctic Ocean

On behalf of my coauthors, I am pleased to submit a manuscript entitled “Sea ice melting is a factor driving dissolved organic matter change in surface waters of Antarctic Ocean close to the Prydz Bay”. The South Ocean (or Antarctic Ocean) is the largest sink for atmospheric CO2, and is sensitive to...

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Bibliographic Details
Main Authors: Xu, Yunping, Yu, Jianchun
Format: Dataset
Language:unknown
Published: figshare 2021
Subjects:
Online Access:https://dx.doi.org/10.6084/m9.figshare.17086862
https://figshare.com/articles/dataset/Data_on_dissolved_organic_matter_sea_ice_and_environment_in_surface_water_of_Antarctic_Ocean/17086862
id ftdatacite:10.6084/m9.figshare.17086862
record_format openpolar
spelling ftdatacite:10.6084/m9.figshare.17086862 2023-05-15T13:40:29+02:00 Data on dissolved organic matter, sea ice and environment in surface water of Antarctic Ocean Xu, Yunping Yu, Jianchun 2021 https://dx.doi.org/10.6084/m9.figshare.17086862 https://figshare.com/articles/dataset/Data_on_dissolved_organic_matter_sea_ice_and_environment_in_surface_water_of_Antarctic_Ocean/17086862 unknown figshare Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY Oceanography FOS Earth and related environmental sciences 40502 Chemical Oceanography dataset Dataset 2021 ftdatacite https://doi.org/10.6084/m9.figshare.17086862 2022-02-08T14:21:14Z On behalf of my coauthors, I am pleased to submit a manuscript entitled “Sea ice melting is a factor driving dissolved organic matter change in surface waters of Antarctic Ocean close to the Prydz Bay”. The South Ocean (or Antarctic Ocean) is the largest sink for atmospheric CO2, and is sensitive to current global warming, characterized by rapid changes in sea ice. Here we measured the concentration and composition of dissolved organic matter (DOM) in surface waters from Antarctic Ocean close to the Prydz Bay, and tried to understand their changes in relation to sea ice melting processes. Our data based on optical spectra and high-resolution mass spectra revealed distinct differences in concentration and composition of DOM during sea ice melting and post-melting periods. Overall, with continuous sea ice melting, the underlying surface water had higher DOM concentration, lower chromophoric DOM concentration, and more protein-like labile components that were attributed to significant contributions of sea ice algae DOM, whereas the water during post-sea ice melting period had lower DOM concentration, higher chromophoric DOM concentration and more humid-like refractory components that were derived from microbial transformation of labile DOM. Dataset Antarc* Antarctic Antarctic Ocean ice algae Prydz Bay Sea ice DataCite Metadata Store (German National Library of Science and Technology) Antarctic Antarctic Ocean Prydz Bay
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic Oceanography
FOS Earth and related environmental sciences
40502 Chemical Oceanography
spellingShingle Oceanography
FOS Earth and related environmental sciences
40502 Chemical Oceanography
Xu, Yunping
Yu, Jianchun
Data on dissolved organic matter, sea ice and environment in surface water of Antarctic Ocean
topic_facet Oceanography
FOS Earth and related environmental sciences
40502 Chemical Oceanography
description On behalf of my coauthors, I am pleased to submit a manuscript entitled “Sea ice melting is a factor driving dissolved organic matter change in surface waters of Antarctic Ocean close to the Prydz Bay”. The South Ocean (or Antarctic Ocean) is the largest sink for atmospheric CO2, and is sensitive to current global warming, characterized by rapid changes in sea ice. Here we measured the concentration and composition of dissolved organic matter (DOM) in surface waters from Antarctic Ocean close to the Prydz Bay, and tried to understand their changes in relation to sea ice melting processes. Our data based on optical spectra and high-resolution mass spectra revealed distinct differences in concentration and composition of DOM during sea ice melting and post-melting periods. Overall, with continuous sea ice melting, the underlying surface water had higher DOM concentration, lower chromophoric DOM concentration, and more protein-like labile components that were attributed to significant contributions of sea ice algae DOM, whereas the water during post-sea ice melting period had lower DOM concentration, higher chromophoric DOM concentration and more humid-like refractory components that were derived from microbial transformation of labile DOM.
format Dataset
author Xu, Yunping
Yu, Jianchun
author_facet Xu, Yunping
Yu, Jianchun
author_sort Xu, Yunping
title Data on dissolved organic matter, sea ice and environment in surface water of Antarctic Ocean
title_short Data on dissolved organic matter, sea ice and environment in surface water of Antarctic Ocean
title_full Data on dissolved organic matter, sea ice and environment in surface water of Antarctic Ocean
title_fullStr Data on dissolved organic matter, sea ice and environment in surface water of Antarctic Ocean
title_full_unstemmed Data on dissolved organic matter, sea ice and environment in surface water of Antarctic Ocean
title_sort data on dissolved organic matter, sea ice and environment in surface water of antarctic ocean
publisher figshare
publishDate 2021
url https://dx.doi.org/10.6084/m9.figshare.17086862
https://figshare.com/articles/dataset/Data_on_dissolved_organic_matter_sea_ice_and_environment_in_surface_water_of_Antarctic_Ocean/17086862
geographic Antarctic
Antarctic Ocean
Prydz Bay
geographic_facet Antarctic
Antarctic Ocean
Prydz Bay
genre Antarc*
Antarctic
Antarctic Ocean
ice algae
Prydz Bay
Sea ice
genre_facet Antarc*
Antarctic
Antarctic Ocean
ice algae
Prydz Bay
Sea ice
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.6084/m9.figshare.17086862
_version_ 1766136093184360448