Evidence for significant protein-like dissolved organic matter accumulation in Sea of Okhotsk sea ice
Absorption and fluorescence of chromophoric dissolved organic matter (CDOM) in sea ice and surface waters in the southern Sea of Okhotsk was examined. Sea-water CDOM had featureless absorption increasing exponentially with shorter wavelengths. Sea ice showed distinct absorption peaks in the ultravio...
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Online Access: | http://hdl.handle.net/2115/70587 https://doi.org/10.3189/2015AoG69A002 |
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fthokunivhus:oai:eprints.lib.hokudai.ac.jp:2115/70587 2023-05-15T13:29:12+02:00 Evidence for significant protein-like dissolved organic matter accumulation in Sea of Okhotsk sea ice Granskog, Mats A. Nomura, Daiki Müller, Susann Krell, Andreas Toyota, Takenobu Hattori, Hiroshi http://hdl.handle.net/2115/70587 https://doi.org/10.3189/2015AoG69A002 eng eng Cambridge University Press https://www.igsoc.org/ http://hdl.handle.net/2115/70587 Annals of Glaciology, 56(69): 1-8 http://dx.doi.org/10.3189/2015AoG69A002 © 2015 The Authors http://creativecommons.org/licenses/by/4.0/ CC-BY sea ice sea-ice ecology 660 article fthokunivhus https://doi.org/10.3189/2015AoG69A002 2022-11-18T01:04:56Z Absorption and fluorescence of chromophoric dissolved organic matter (CDOM) in sea ice and surface waters in the southern Sea of Okhotsk was examined. Sea-water CDOM had featureless absorption increasing exponentially with shorter wavelengths. Sea ice showed distinct absorption peaks in the ultraviolet, especially in younger ice. Older first-year sea ice had relatively flat absorption spectra in the ultraviolet range. Parallel factor analysis (PARAFAC) identified five fluorescent CDOM components, two humic-like and three protein-like. Sea water was largely governed by humic-like fluorescence. In sea ice, protein-like fluorescence was found in considerable excess relative to sea water. The accumulation of protein-like CDOM fluorescence in sea ice is likely a result of biological activity within the ice. Nevertheless, sea ice does not contribute excess CDOM during melt, but the material released will be of different composition than that present in the underlying waters. Thus, at least transiently, the CDOM introduced during sea-ice melt might provide a more labile source of fresher protein-like DOM to surface waters in the southern Sea of Okhotsk. Article in Journal/Newspaper Annals of Glaciology okhotsk sea Sea ice Hokkaido University Collection of Scholarly and Academic Papers (HUSCAP) Okhotsk Annals of Glaciology 56 69 1 8 |
institution |
Open Polar |
collection |
Hokkaido University Collection of Scholarly and Academic Papers (HUSCAP) |
op_collection_id |
fthokunivhus |
language |
English |
topic |
sea ice sea-ice ecology 660 |
spellingShingle |
sea ice sea-ice ecology 660 Granskog, Mats A. Nomura, Daiki Müller, Susann Krell, Andreas Toyota, Takenobu Hattori, Hiroshi Evidence for significant protein-like dissolved organic matter accumulation in Sea of Okhotsk sea ice |
topic_facet |
sea ice sea-ice ecology 660 |
description |
Absorption and fluorescence of chromophoric dissolved organic matter (CDOM) in sea ice and surface waters in the southern Sea of Okhotsk was examined. Sea-water CDOM had featureless absorption increasing exponentially with shorter wavelengths. Sea ice showed distinct absorption peaks in the ultraviolet, especially in younger ice. Older first-year sea ice had relatively flat absorption spectra in the ultraviolet range. Parallel factor analysis (PARAFAC) identified five fluorescent CDOM components, two humic-like and three protein-like. Sea water was largely governed by humic-like fluorescence. In sea ice, protein-like fluorescence was found in considerable excess relative to sea water. The accumulation of protein-like CDOM fluorescence in sea ice is likely a result of biological activity within the ice. Nevertheless, sea ice does not contribute excess CDOM during melt, but the material released will be of different composition than that present in the underlying waters. Thus, at least transiently, the CDOM introduced during sea-ice melt might provide a more labile source of fresher protein-like DOM to surface waters in the southern Sea of Okhotsk. |
format |
Article in Journal/Newspaper |
author |
Granskog, Mats A. Nomura, Daiki Müller, Susann Krell, Andreas Toyota, Takenobu Hattori, Hiroshi |
author_facet |
Granskog, Mats A. Nomura, Daiki Müller, Susann Krell, Andreas Toyota, Takenobu Hattori, Hiroshi |
author_sort |
Granskog, Mats A. |
title |
Evidence for significant protein-like dissolved organic matter accumulation in Sea of Okhotsk sea ice |
title_short |
Evidence for significant protein-like dissolved organic matter accumulation in Sea of Okhotsk sea ice |
title_full |
Evidence for significant protein-like dissolved organic matter accumulation in Sea of Okhotsk sea ice |
title_fullStr |
Evidence for significant protein-like dissolved organic matter accumulation in Sea of Okhotsk sea ice |
title_full_unstemmed |
Evidence for significant protein-like dissolved organic matter accumulation in Sea of Okhotsk sea ice |
title_sort |
evidence for significant protein-like dissolved organic matter accumulation in sea of okhotsk sea ice |
publisher |
Cambridge University Press |
url |
http://hdl.handle.net/2115/70587 https://doi.org/10.3189/2015AoG69A002 |
geographic |
Okhotsk |
geographic_facet |
Okhotsk |
genre |
Annals of Glaciology okhotsk sea Sea ice |
genre_facet |
Annals of Glaciology okhotsk sea Sea ice |
op_relation |
https://www.igsoc.org/ http://hdl.handle.net/2115/70587 Annals of Glaciology, 56(69): 1-8 http://dx.doi.org/10.3189/2015AoG69A002 |
op_rights |
© 2015 The Authors http://creativecommons.org/licenses/by/4.0/ |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.3189/2015AoG69A002 |
container_title |
Annals of Glaciology |
container_volume |
56 |
container_issue |
69 |
container_start_page |
1 |
op_container_end_page |
8 |
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1765999239546011648 |