Optical properties and bioavailability of dissolved organic matter along a flow-path continuum from soil pore waters to the Kolyma River mainstem, East Siberia
The Kolyma River in northeast Siberia is among the six largest Arctic rivers and drains a region underlain by vast deposits of Holocene-aged peat and Pleistocene-aged loess known as yedoma, most of which is currently stored in ice-rich permafrost throughout the region. These peat and yedoma deposits...
Published in: | Biogeosciences |
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Language: | English |
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Copernicus Publications
2016
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article Verlagsveröffentlichung Frey, Karen E. Sobczak, William V. Mann, Paul J. Holmes, Robert M. Optical properties and bioavailability of dissolved organic matter along a flow-path continuum from soil pore waters to the Kolyma River mainstem, East Siberia |
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article Verlagsveröffentlichung |
description |
The Kolyma River in northeast Siberia is among the six largest Arctic rivers and drains a region underlain by vast deposits of Holocene-aged peat and Pleistocene-aged loess known as yedoma, most of which is currently stored in ice-rich permafrost throughout the region. These peat and yedoma deposits are important sources of dissolved organic matter (DOM) to inland waters that in turn play a significant role in the transport and ultimate remineralization of organic carbon to CO2 and CH4 along the terrestrial flow-path continuum. The turnover and fate of terrigenous DOM during offshore transport largely depends upon the composition and amount of carbon released to inland and coastal waters. Here, we measured the ultraviolet-visible optical properties of chromophoric DOM (CDOM) from a geographically extensive collection of waters spanning soil pore waters, streams, rivers, and the Kolyma River mainstem throughout a ∼ 250 km transect of the northern Kolyma River basin. During the period of study, CDOM absorption coefficients were found to be robust proxies for the concentration of DOM, whereas additional CDOM parameters such as spectral slopes (S) were found to be useful indicators of DOM quality along the flow path. In particular, the spectral slope ratio (SR) of CDOM demonstrated statistically significant differences between all four water types and tracked changes in the concentration of bioavailable DOC, suggesting that this parameter may be suitable for clearly discriminating shifts in organic matter characteristics among water types along the full flow-path continuum across this landscape. However, despite our observations of downstream shifts in DOM composition, we found a relatively constant proportion of DOC that was bioavailable ( ∼ 3–6 % of total DOC) regardless of relative water residence time along the flow path. This may be a consequence of two potential scenarios allowing for continual processing of organic material within the system, namely (a) aquatic microorganisms are acclimating to a downstream shift in DOM composition and/or (b) photodegradation is continually generating labile DOM for continued microbial processing of DOM along the flow-path continuum. Without such processes, we would otherwise expect to see a declining fraction of bioavailable DOC downstream with increasing residence time of water in the system. With ongoing and future permafrost degradation, peat and yedoma deposits throughout the northeast Siberian region will become more hydrologically active, providing greater amounts of DOM to fluvial networks and ultimately to the Arctic Ocean. The ability to rapidly and comprehensively monitor shifts in the quantity and quality of DOM across the landscape is therefore critical for understanding potential future feedbacks within the Arctic carbon cycle. |
format |
Article in Journal/Newspaper |
author |
Frey, Karen E. Sobczak, William V. Mann, Paul J. Holmes, Robert M. |
author_facet |
Frey, Karen E. Sobczak, William V. Mann, Paul J. Holmes, Robert M. |
author_sort |
Frey, Karen E. |
title |
Optical properties and bioavailability of dissolved organic matter along a flow-path continuum from soil pore waters to the Kolyma River mainstem, East Siberia |
title_short |
Optical properties and bioavailability of dissolved organic matter along a flow-path continuum from soil pore waters to the Kolyma River mainstem, East Siberia |
title_full |
Optical properties and bioavailability of dissolved organic matter along a flow-path continuum from soil pore waters to the Kolyma River mainstem, East Siberia |
title_fullStr |
Optical properties and bioavailability of dissolved organic matter along a flow-path continuum from soil pore waters to the Kolyma River mainstem, East Siberia |
title_full_unstemmed |
Optical properties and bioavailability of dissolved organic matter along a flow-path continuum from soil pore waters to the Kolyma River mainstem, East Siberia |
title_sort |
optical properties and bioavailability of dissolved organic matter along a flow-path continuum from soil pore waters to the kolyma river mainstem, east siberia |
publisher |
Copernicus Publications |
publishDate |
2016 |
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https://doi.org/10.5194/bg-13-2279-2016 https://noa.gwlb.de/receive/cop_mods_00013583 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00013539/bg-13-2279-2016.pdf https://bg.copernicus.org/articles/13/2279/2016/bg-13-2279-2016.pdf |
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ENVELOPE(161.000,161.000,69.500,69.500) |
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Arctic Arctic Ocean Kolyma |
geographic_facet |
Arctic Arctic Ocean Kolyma |
genre |
Arctic Arctic Ocean Ice kolyma river permafrost Siberia |
genre_facet |
Arctic Arctic Ocean Ice kolyma river permafrost Siberia |
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Biogeosciences -- http://www.bibliothek.uni-regensburg.de/ezeit/?2158181 -- http://www.copernicus.org/EGU/bg/bg.html -- 1726-4189 https://doi.org/10.5194/bg-13-2279-2016 https://noa.gwlb.de/receive/cop_mods_00013583 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00013539/bg-13-2279-2016.pdf https://bg.copernicus.org/articles/13/2279/2016/bg-13-2279-2016.pdf |
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uneingeschränkt info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.5194/bg-13-2279-2016 |
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Biogeosciences |
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ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00013583 2023-05-15T15:01:00+02:00 Optical properties and bioavailability of dissolved organic matter along a flow-path continuum from soil pore waters to the Kolyma River mainstem, East Siberia Frey, Karen E. Sobczak, William V. Mann, Paul J. Holmes, Robert M. 2016-04 electronic https://doi.org/10.5194/bg-13-2279-2016 https://noa.gwlb.de/receive/cop_mods_00013583 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00013539/bg-13-2279-2016.pdf https://bg.copernicus.org/articles/13/2279/2016/bg-13-2279-2016.pdf eng eng Copernicus Publications Biogeosciences -- http://www.bibliothek.uni-regensburg.de/ezeit/?2158181 -- http://www.copernicus.org/EGU/bg/bg.html -- 1726-4189 https://doi.org/10.5194/bg-13-2279-2016 https://noa.gwlb.de/receive/cop_mods_00013583 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00013539/bg-13-2279-2016.pdf https://bg.copernicus.org/articles/13/2279/2016/bg-13-2279-2016.pdf uneingeschränkt info:eu-repo/semantics/openAccess article Verlagsveröffentlichung article Text doc-type:article 2016 ftnonlinearchiv https://doi.org/10.5194/bg-13-2279-2016 2022-02-08T22:55:33Z The Kolyma River in northeast Siberia is among the six largest Arctic rivers and drains a region underlain by vast deposits of Holocene-aged peat and Pleistocene-aged loess known as yedoma, most of which is currently stored in ice-rich permafrost throughout the region. These peat and yedoma deposits are important sources of dissolved organic matter (DOM) to inland waters that in turn play a significant role in the transport and ultimate remineralization of organic carbon to CO2 and CH4 along the terrestrial flow-path continuum. The turnover and fate of terrigenous DOM during offshore transport largely depends upon the composition and amount of carbon released to inland and coastal waters. Here, we measured the ultraviolet-visible optical properties of chromophoric DOM (CDOM) from a geographically extensive collection of waters spanning soil pore waters, streams, rivers, and the Kolyma River mainstem throughout a ∼ 250 km transect of the northern Kolyma River basin. During the period of study, CDOM absorption coefficients were found to be robust proxies for the concentration of DOM, whereas additional CDOM parameters such as spectral slopes (S) were found to be useful indicators of DOM quality along the flow path. In particular, the spectral slope ratio (SR) of CDOM demonstrated statistically significant differences between all four water types and tracked changes in the concentration of bioavailable DOC, suggesting that this parameter may be suitable for clearly discriminating shifts in organic matter characteristics among water types along the full flow-path continuum across this landscape. However, despite our observations of downstream shifts in DOM composition, we found a relatively constant proportion of DOC that was bioavailable ( ∼ 3–6 % of total DOC) regardless of relative water residence time along the flow path. This may be a consequence of two potential scenarios allowing for continual processing of organic material within the system, namely (a) aquatic microorganisms are acclimating to a downstream shift in DOM composition and/or (b) photodegradation is continually generating labile DOM for continued microbial processing of DOM along the flow-path continuum. Without such processes, we would otherwise expect to see a declining fraction of bioavailable DOC downstream with increasing residence time of water in the system. With ongoing and future permafrost degradation, peat and yedoma deposits throughout the northeast Siberian region will become more hydrologically active, providing greater amounts of DOM to fluvial networks and ultimately to the Arctic Ocean. The ability to rapidly and comprehensively monitor shifts in the quantity and quality of DOM across the landscape is therefore critical for understanding potential future feedbacks within the Arctic carbon cycle. Article in Journal/Newspaper Arctic Arctic Ocean Ice kolyma river permafrost Siberia Niedersächsisches Online-Archiv NOA Arctic Arctic Ocean Kolyma ENVELOPE(161.000,161.000,69.500,69.500) Biogeosciences 13 8 2279 2290 |