Implications of elevated CO 2 on pelagic carbon fluxes in an Arctic mesocosm study – an elemental mass balance approach
Recent studies on the impacts of ocean acidification on pelagic communities have identified changes in carbon to nutrient dynamics with related shifts in elemental stoichiometry. In principle, mesocosm experiments provide the opportunity of determining temporal dynamics of all relevant carbon and nu...
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ftdoajarticles:oai:doaj.org/article:53709b9f1c4b4a4597fbb0d794c6bc15 2023-05-15T15:01:48+02:00 Implications of elevated CO 2 on pelagic carbon fluxes in an Arctic mesocosm study – an elemental mass balance approach J. Czerny K. G. Schulz T. Boxhammer R. G. J. Bellerby J. Büdenbender A. Engel S. A. Krug A. Ludwig K. Nachtigall G. Nondal B. Niehoff A. Silyakova U. Riebesell 2013-05-01T00:00:00Z https://doi.org/10.5194/bg-10-3109-2013 https://doaj.org/article/53709b9f1c4b4a4597fbb0d794c6bc15 EN eng Copernicus Publications http://www.biogeosciences.net/10/3109/2013/bg-10-3109-2013.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 doi:10.5194/bg-10-3109-2013 1726-4170 1726-4189 https://doaj.org/article/53709b9f1c4b4a4597fbb0d794c6bc15 Biogeosciences, Vol 10, Iss 5, Pp 3109-3125 (2013) Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 article 2013 ftdoajarticles https://doi.org/10.5194/bg-10-3109-2013 2022-12-30T21:26:11Z Recent studies on the impacts of ocean acidification on pelagic communities have identified changes in carbon to nutrient dynamics with related shifts in elemental stoichiometry. In principle, mesocosm experiments provide the opportunity of determining temporal dynamics of all relevant carbon and nutrient pools and, thus, calculating elemental budgets. In practice, attempts to budget mesocosm enclosures are often hampered by uncertainties in some of the measured pools and fluxes, in particular due to uncertainties in constraining air–sea gas exchange, particle sinking, and wall growth. In an Arctic mesocosm study on ocean acidification applying KOSMOS (Kiel Off-Shore Mesocosms for future Ocean Simulation), all relevant element pools and fluxes of carbon, nitrogen and phosphorus were measured, using an improved experimental design intended to narrow down the mentioned uncertainties. Water-column concentrations of particulate and dissolved organic and inorganic matter were determined daily. New approaches for quantitative estimates of material sinking to the bottom of the mesocosms and gas exchange in 48 h temporal resolution as well as estimates of wall growth were developed to close the gaps in element budgets. However, losses elements from the budgets into a sum of insufficiently determined pools were detected, and are principally unavoidable in mesocosm investigation. The comparison of variability patterns of all single measured datasets revealed analytic precision to be the main issue in determination of budgets. Uncertainties in dissolved organic carbon (DOC), nitrogen (DON) and particulate organic phosphorus (POP) were much higher than the summed error in determination of the same elements in all other pools. With estimates provided for all other major elemental pools, mass balance calculations could be used to infer the temporal development of DOC, DON and POP pools. Future elevated p CO 2 was found to enhance net autotrophic community carbon uptake in two of the three experimental phases but did not ... Article in Journal/Newspaper Arctic Ocean acidification Directory of Open Access Journals: DOAJ Articles Arctic Biogeosciences 10 5 3109 3125 |
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Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 |
spellingShingle |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 J. Czerny K. G. Schulz T. Boxhammer R. G. J. Bellerby J. Büdenbender A. Engel S. A. Krug A. Ludwig K. Nachtigall G. Nondal B. Niehoff A. Silyakova U. Riebesell Implications of elevated CO 2 on pelagic carbon fluxes in an Arctic mesocosm study – an elemental mass balance approach |
topic_facet |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 |
description |
Recent studies on the impacts of ocean acidification on pelagic communities have identified changes in carbon to nutrient dynamics with related shifts in elemental stoichiometry. In principle, mesocosm experiments provide the opportunity of determining temporal dynamics of all relevant carbon and nutrient pools and, thus, calculating elemental budgets. In practice, attempts to budget mesocosm enclosures are often hampered by uncertainties in some of the measured pools and fluxes, in particular due to uncertainties in constraining air–sea gas exchange, particle sinking, and wall growth. In an Arctic mesocosm study on ocean acidification applying KOSMOS (Kiel Off-Shore Mesocosms for future Ocean Simulation), all relevant element pools and fluxes of carbon, nitrogen and phosphorus were measured, using an improved experimental design intended to narrow down the mentioned uncertainties. Water-column concentrations of particulate and dissolved organic and inorganic matter were determined daily. New approaches for quantitative estimates of material sinking to the bottom of the mesocosms and gas exchange in 48 h temporal resolution as well as estimates of wall growth were developed to close the gaps in element budgets. However, losses elements from the budgets into a sum of insufficiently determined pools were detected, and are principally unavoidable in mesocosm investigation. The comparison of variability patterns of all single measured datasets revealed analytic precision to be the main issue in determination of budgets. Uncertainties in dissolved organic carbon (DOC), nitrogen (DON) and particulate organic phosphorus (POP) were much higher than the summed error in determination of the same elements in all other pools. With estimates provided for all other major elemental pools, mass balance calculations could be used to infer the temporal development of DOC, DON and POP pools. Future elevated p CO 2 was found to enhance net autotrophic community carbon uptake in two of the three experimental phases but did not ... |
format |
Article in Journal/Newspaper |
author |
J. Czerny K. G. Schulz T. Boxhammer R. G. J. Bellerby J. Büdenbender A. Engel S. A. Krug A. Ludwig K. Nachtigall G. Nondal B. Niehoff A. Silyakova U. Riebesell |
author_facet |
J. Czerny K. G. Schulz T. Boxhammer R. G. J. Bellerby J. Büdenbender A. Engel S. A. Krug A. Ludwig K. Nachtigall G. Nondal B. Niehoff A. Silyakova U. Riebesell |
author_sort |
J. Czerny |
title |
Implications of elevated CO 2 on pelagic carbon fluxes in an Arctic mesocosm study – an elemental mass balance approach |
title_short |
Implications of elevated CO 2 on pelagic carbon fluxes in an Arctic mesocosm study – an elemental mass balance approach |
title_full |
Implications of elevated CO 2 on pelagic carbon fluxes in an Arctic mesocosm study – an elemental mass balance approach |
title_fullStr |
Implications of elevated CO 2 on pelagic carbon fluxes in an Arctic mesocosm study – an elemental mass balance approach |
title_full_unstemmed |
Implications of elevated CO 2 on pelagic carbon fluxes in an Arctic mesocosm study – an elemental mass balance approach |
title_sort |
implications of elevated co 2 on pelagic carbon fluxes in an arctic mesocosm study – an elemental mass balance approach |
publisher |
Copernicus Publications |
publishDate |
2013 |
url |
https://doi.org/10.5194/bg-10-3109-2013 https://doaj.org/article/53709b9f1c4b4a4597fbb0d794c6bc15 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Ocean acidification |
genre_facet |
Arctic Ocean acidification |
op_source |
Biogeosciences, Vol 10, Iss 5, Pp 3109-3125 (2013) |
op_relation |
http://www.biogeosciences.net/10/3109/2013/bg-10-3109-2013.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 doi:10.5194/bg-10-3109-2013 1726-4170 1726-4189 https://doaj.org/article/53709b9f1c4b4a4597fbb0d794c6bc15 |
op_doi |
https://doi.org/10.5194/bg-10-3109-2013 |
container_title |
Biogeosciences |
container_volume |
10 |
container_issue |
5 |
container_start_page |
3109 |
op_container_end_page |
3125 |
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1766333807907045376 |