Excess carbon in aquatic organisms and ecosystems: physiological, ecological, and evolutionary implications
Excess carbon in aquatic organisms and ecosystems: physiological, ecological, and evolutionary implications
Cells and organisms, both autotrophs and heterotrophs, commonly face imbalanced access to and uptake of
elements relative to their requirements. C is often in excess relative to key nutrient elements like N or P in photoautotrophs. Likewise, one of the lessons from ecological stoichiometry is that the growth of consumers, especially herbivores and detritivores, is commonly limited by N or P such that they also experience C in excess in relative terms. ‘‘Excess’’ implies wastage, yet this definition, which is consistent with purely stoichiometric arguments, is by no means straightforward. In fact, many organisms put this apparently surplus C to good use for fitness-promoting purposes like storage, structure, and defense or mutualistic goals like symbiosis. Nevertheless,
genuine excesses do occur, in which case the remaining ‘‘leftover C’’ must be disposed of, either in organic or
inorganic form via increased metabolic activity and respiration. These fluxes of C in various forms have major effects on the C balance of organisms, as well as governing the energy flux and C pathways at the ecosystem level. We here discuss evolutionary and ecological implications of ‘‘excess C’’ both at the organism and ecosystem level.
carbon cycle, marine ecosystems, dissolved organic carbon, excess carbon
1685-1696
Hessen, D.O.
57c22fb0-cd1a-49bb-b998-5e653710d748
Anderson, T.R.
dfed062f-e747-48d3-b59e-2f5e57a8571d
July 2008
Hessen, D.O.
57c22fb0-cd1a-49bb-b998-5e653710d748
Anderson, T.R.
dfed062f-e747-48d3-b59e-2f5e57a8571d
Hessen, D.O. and Anderson, T.R.
(2008)
Excess carbon in aquatic organisms and ecosystems: physiological, ecological, and evolutionary implications.
Limnology and Oceanography, 53 (4), .
(doi:10.4319/lo.2008.53.4.1685).
Abstract
Cells and organisms, both autotrophs and heterotrophs, commonly face imbalanced access to and uptake of
elements relative to their requirements. C is often in excess relative to key nutrient elements like N or P in photoautotrophs. Likewise, one of the lessons from ecological stoichiometry is that the growth of consumers, especially herbivores and detritivores, is commonly limited by N or P such that they also experience C in excess in relative terms. ‘‘Excess’’ implies wastage, yet this definition, which is consistent with purely stoichiometric arguments, is by no means straightforward. In fact, many organisms put this apparently surplus C to good use for fitness-promoting purposes like storage, structure, and defense or mutualistic goals like symbiosis. Nevertheless,
genuine excesses do occur, in which case the remaining ‘‘leftover C’’ must be disposed of, either in organic or
inorganic form via increased metabolic activity and respiration. These fluxes of C in various forms have major effects on the C balance of organisms, as well as governing the energy flux and C pathways at the ecosystem level. We here discuss evolutionary and ecological implications of ‘‘excess C’’ both at the organism and ecosystem level.
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Published date: July 2008
Keywords:
carbon cycle, marine ecosystems, dissolved organic carbon, excess carbon
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Local EPrints ID: 54649
URI: http://eprints.soton.ac.uk/id/eprint/54649
ISSN: 0024-3590
PURE UUID: 9ecd479f-20cc-4ac2-92f9-781093eadaa3
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Date deposited: 17 Jul 2008
Last modified: 15 Mar 2024 10:49
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Author:
D.O. Hessen
Author:
T.R. Anderson
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