Whole‐lake mineralization of allochthonous and autochthonous organic carbon in a large humic lake (örträsket, N. Sweden)
Organic carbon mineralization was studied in a large humic lake (Lake Ortrasket) in northern Sweden during a well‐defined summer stratification period following high water flow during snowmelt. Several independent methods including plankton counts, measurements of bacterioplankton and phytoplankton...
Published in: | Limnology and Oceanography |
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Online Access: | http://dx.doi.org/10.4319/lo.2001.46.7.1691 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.2001.46.7.1691 https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lo.2001.46.7.1691 |
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crwiley:10.4319/lo.2001.46.7.1691 2024-09-15T18:26:09+00:00 Whole‐lake mineralization of allochthonous and autochthonous organic carbon in a large humic lake (örträsket, N. Sweden) Jonsson, Anders Meili, Markus Bergström, Ann-Kristin Jansson, Mats 2001 http://dx.doi.org/10.4319/lo.2001.46.7.1691 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.2001.46.7.1691 https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lo.2001.46.7.1691 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Limnology and Oceanography volume 46, issue 7, page 1691-1700 ISSN 0024-3590 1939-5590 journal-article 2001 crwiley https://doi.org/10.4319/lo.2001.46.7.1691 2024-07-18T04:26:40Z Organic carbon mineralization was studied in a large humic lake (Lake Ortrasket) in northern Sweden during a well‐defined summer stratification period following high water flow during snowmelt. Several independent methods including plankton counts, measurements of bacterioplankton and phytoplankton production, stable isotope monitoring, sediment trapping, and mass balance calculations were used. Total organic carbon mineralization showed a summer mean of 0.3 g C m −2 d −1 and was partitioned about equally between water and sediment. In the water column, organic matter was mineralized by bacteria (60%) and protozoan and metazoan zooplankton (30%), as well as by photooxidation (10%). Most of the mineralized organic carbon was of allochthonous origin. Primary production in the lake contributed at most 5% of the total organic carbon input and about 20% of the total organic carbon mineralization. Total carbon mineralization in the epilimnion and metalimnion agreed well with an estimate of CO 2 evasion from the stratified lake, while CO 2 accumulation in the hypolimnion matched the O 2 consumption and resulted in a very negative dδ 13 C of DIC before autumn overturn (−23‰). Isotopic compositions of DIC and POC confirmed the dominant influence of terrestrial organic input on the cycling of both organic and inorganic carbon in the lake. Article in Journal/Newspaper Northern Sweden Wiley Online Library Limnology and Oceanography 46 7 1691 1700 |
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Open Polar |
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Wiley Online Library |
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crwiley |
language |
English |
description |
Organic carbon mineralization was studied in a large humic lake (Lake Ortrasket) in northern Sweden during a well‐defined summer stratification period following high water flow during snowmelt. Several independent methods including plankton counts, measurements of bacterioplankton and phytoplankton production, stable isotope monitoring, sediment trapping, and mass balance calculations were used. Total organic carbon mineralization showed a summer mean of 0.3 g C m −2 d −1 and was partitioned about equally between water and sediment. In the water column, organic matter was mineralized by bacteria (60%) and protozoan and metazoan zooplankton (30%), as well as by photooxidation (10%). Most of the mineralized organic carbon was of allochthonous origin. Primary production in the lake contributed at most 5% of the total organic carbon input and about 20% of the total organic carbon mineralization. Total carbon mineralization in the epilimnion and metalimnion agreed well with an estimate of CO 2 evasion from the stratified lake, while CO 2 accumulation in the hypolimnion matched the O 2 consumption and resulted in a very negative dδ 13 C of DIC before autumn overturn (−23‰). Isotopic compositions of DIC and POC confirmed the dominant influence of terrestrial organic input on the cycling of both organic and inorganic carbon in the lake. |
format |
Article in Journal/Newspaper |
author |
Jonsson, Anders Meili, Markus Bergström, Ann-Kristin Jansson, Mats |
spellingShingle |
Jonsson, Anders Meili, Markus Bergström, Ann-Kristin Jansson, Mats Whole‐lake mineralization of allochthonous and autochthonous organic carbon in a large humic lake (örträsket, N. Sweden) |
author_facet |
Jonsson, Anders Meili, Markus Bergström, Ann-Kristin Jansson, Mats |
author_sort |
Jonsson, Anders |
title |
Whole‐lake mineralization of allochthonous and autochthonous organic carbon in a large humic lake (örträsket, N. Sweden) |
title_short |
Whole‐lake mineralization of allochthonous and autochthonous organic carbon in a large humic lake (örträsket, N. Sweden) |
title_full |
Whole‐lake mineralization of allochthonous and autochthonous organic carbon in a large humic lake (örträsket, N. Sweden) |
title_fullStr |
Whole‐lake mineralization of allochthonous and autochthonous organic carbon in a large humic lake (örträsket, N. Sweden) |
title_full_unstemmed |
Whole‐lake mineralization of allochthonous and autochthonous organic carbon in a large humic lake (örträsket, N. Sweden) |
title_sort |
whole‐lake mineralization of allochthonous and autochthonous organic carbon in a large humic lake (örträsket, n. sweden) |
publisher |
Wiley |
publishDate |
2001 |
url |
http://dx.doi.org/10.4319/lo.2001.46.7.1691 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.2001.46.7.1691 https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lo.2001.46.7.1691 |
genre |
Northern Sweden |
genre_facet |
Northern Sweden |
op_source |
Limnology and Oceanography volume 46, issue 7, page 1691-1700 ISSN 0024-3590 1939-5590 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.4319/lo.2001.46.7.1691 |
container_title |
Limnology and Oceanography |
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46 |
container_issue |
7 |
container_start_page |
1691 |
op_container_end_page |
1700 |
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1810466595438329856 |