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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Published in:Biogeosciences
Main Authors: 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
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2013
Subjects:
Online Access:https://doi.org/10.5194/bg-10-3109-2013
https://doaj.org/article/53709b9f1c4b4a4597fbb0d794c6bc15
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spelling 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
institution Open Polar
collection 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
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container_issue 5
container_start_page 3109
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