On the biogeochemistry of dissolved carbohydrates in the Greenland Sea (Arctic)

Dissolved organic matter (DOM) was isolated with XAD-2 and 4 resins in different water masses of the Greenland Sea and Fram Strait. The contribution of XAD-extractable dissolved organic carbon (DOC), operationally defined as recalcitrant or humic substances, to total DOC ranged between 45±9% in surf...

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Published in:Organic Geochemistry
Main Authors: Engbrodt, R., Kattner, Gerhard
Format: Article in Journal/Newspaper
Language:unknown
Published: 2005
Subjects:
Online Access:https://epic.awi.de/id/eprint/10840/
https://doi.org/10.1016/j.orggeochem.2004.12.007
https://hdl.handle.net/10013/epic.21309
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spelling ftawi:oai:epic.awi.de:10840 2023-09-05T13:15:44+02:00 On the biogeochemistry of dissolved carbohydrates in the Greenland Sea (Arctic) Engbrodt, R. Kattner, Gerhard 2005 https://epic.awi.de/id/eprint/10840/ https://doi.org/10.1016/j.orggeochem.2004.12.007 https://hdl.handle.net/10013/epic.21309 unknown Engbrodt, R. and Kattner, G. (2005) On the biogeochemistry of dissolved carbohydrates in the Greenland Sea (Arctic) , Organic geochemistry, 36 , pp. 937-948 . doi:10.1016/j.orggeochem.2004.12.007 <https://doi.org/10.1016/j.orggeochem.2004.12.007> , hdl:10013/epic.21309 EPIC3Organic geochemistry, 36, pp. 937-948, ISSN: 0146-6380 Article isiRev 2005 ftawi https://doi.org/10.1016/j.orggeochem.2004.12.007 2023-08-22T19:48:58Z Dissolved organic matter (DOM) was isolated with XAD-2 and 4 resins in different water masses of the Greenland Sea and Fram Strait. The contribution of XAD-extractable dissolved organic carbon (DOC), operationally defined as recalcitrant or humic substances, to total DOC ranged between 45±9% in surface waters and 60±6% in deep waters. The concentration and composition of carbohydrates was determined using the L-tryptophan / sulphuric acid method (for the bulk carbohydrate concentration, TCHO) and high-performance anion-exchange chromatography with pulsed amperometric detection after sulphuric acid hydrolysis (for the distribution of total hydrolysable neutral sugars, THNS). Carbohydrates contributed up to 6.8% to both total and recalcitrant DOC. TCHO contribution to total DOC decreased with depth from on average 4.1±1.2% in surface waters to 2.2±1.0% in deep waters, whereas the THNS contribution was similar in both layers accounting for 2.5±1.6% (surface) and 2.4±0.2% (at depth). TCHO contribution to XAD-extractable DOC also decreased with depth from 4.5±1.7% to 2.1±1.0%, whereas THNS contribution was almost constant with yields of 0.5±0.3% in surface samples and 0.6±0.1% at depth. The molecular size distribution of the recalcitrant DOM derived from selective resin fractionation of XAD-2 and XAD-4 showed in all fractions a clear trend towards small molecules in the deep sea. More than half of the XAD-extractable carbohydrates of surface samples and more than 70% of deep sea samples were found in the unpolar fraction of XAD, which was eluted with methanol. Glucose was the dominant carbohydrate in the surface water samples, whereas in the deep sea the composition was more uniform. In the XAD extracts the compositions were less variable than in the original samples. The neutral sugar composition, in particular glucose and the deoxysugars, are indicatives of the diagenetic state of the extracted DOM. The molar ratio (fucose+rhamnose) / (arabinose+xylose) was lowest for deep sea extractable DOM indicating a high ... Article in Journal/Newspaper Arctic Arctic Fram Strait Greenland Greenland Sea Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Arctic Greenland Organic Geochemistry 36 6 937 948
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language unknown
description Dissolved organic matter (DOM) was isolated with XAD-2 and 4 resins in different water masses of the Greenland Sea and Fram Strait. The contribution of XAD-extractable dissolved organic carbon (DOC), operationally defined as recalcitrant or humic substances, to total DOC ranged between 45±9% in surface waters and 60±6% in deep waters. The concentration and composition of carbohydrates was determined using the L-tryptophan / sulphuric acid method (for the bulk carbohydrate concentration, TCHO) and high-performance anion-exchange chromatography with pulsed amperometric detection after sulphuric acid hydrolysis (for the distribution of total hydrolysable neutral sugars, THNS). Carbohydrates contributed up to 6.8% to both total and recalcitrant DOC. TCHO contribution to total DOC decreased with depth from on average 4.1±1.2% in surface waters to 2.2±1.0% in deep waters, whereas the THNS contribution was similar in both layers accounting for 2.5±1.6% (surface) and 2.4±0.2% (at depth). TCHO contribution to XAD-extractable DOC also decreased with depth from 4.5±1.7% to 2.1±1.0%, whereas THNS contribution was almost constant with yields of 0.5±0.3% in surface samples and 0.6±0.1% at depth. The molecular size distribution of the recalcitrant DOM derived from selective resin fractionation of XAD-2 and XAD-4 showed in all fractions a clear trend towards small molecules in the deep sea. More than half of the XAD-extractable carbohydrates of surface samples and more than 70% of deep sea samples were found in the unpolar fraction of XAD, which was eluted with methanol. Glucose was the dominant carbohydrate in the surface water samples, whereas in the deep sea the composition was more uniform. In the XAD extracts the compositions were less variable than in the original samples. The neutral sugar composition, in particular glucose and the deoxysugars, are indicatives of the diagenetic state of the extracted DOM. The molar ratio (fucose+rhamnose) / (arabinose+xylose) was lowest for deep sea extractable DOM indicating a high ...
format Article in Journal/Newspaper
author Engbrodt, R.
Kattner, Gerhard
spellingShingle Engbrodt, R.
Kattner, Gerhard
On the biogeochemistry of dissolved carbohydrates in the Greenland Sea (Arctic)
author_facet Engbrodt, R.
Kattner, Gerhard
author_sort Engbrodt, R.
title On the biogeochemistry of dissolved carbohydrates in the Greenland Sea (Arctic)
title_short On the biogeochemistry of dissolved carbohydrates in the Greenland Sea (Arctic)
title_full On the biogeochemistry of dissolved carbohydrates in the Greenland Sea (Arctic)
title_fullStr On the biogeochemistry of dissolved carbohydrates in the Greenland Sea (Arctic)
title_full_unstemmed On the biogeochemistry of dissolved carbohydrates in the Greenland Sea (Arctic)
title_sort on the biogeochemistry of dissolved carbohydrates in the greenland sea (arctic)
publishDate 2005
url https://epic.awi.de/id/eprint/10840/
https://doi.org/10.1016/j.orggeochem.2004.12.007
https://hdl.handle.net/10013/epic.21309
geographic Arctic
Greenland
geographic_facet Arctic
Greenland
genre Arctic
Arctic
Fram Strait
Greenland
Greenland Sea
genre_facet Arctic
Arctic
Fram Strait
Greenland
Greenland Sea
op_source EPIC3Organic geochemistry, 36, pp. 937-948, ISSN: 0146-6380
op_relation Engbrodt, R. and Kattner, G. (2005) On the biogeochemistry of dissolved carbohydrates in the Greenland Sea (Arctic) , Organic geochemistry, 36 , pp. 937-948 . doi:10.1016/j.orggeochem.2004.12.007 <https://doi.org/10.1016/j.orggeochem.2004.12.007> , hdl:10013/epic.21309
op_doi https://doi.org/10.1016/j.orggeochem.2004.12.007
container_title Organic Geochemistry
container_volume 36
container_issue 6
container_start_page 937
op_container_end_page 948
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