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Global-scale carbon and energy flows through the marine planktonic food web: An analysis with a coupled physical–biological model
•Global ecosystem model captures biome-scale carbon flows through plankton food web.•Quantitative, holistic global planktonic food web carbon budgets derived.•Respiration/remineralization highly distributed across the planktonic food web.•Muted cross-biome differences in mesozooplankton trophic leve...
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Published in: | Progress in oceanography 2014-01, Vol.120, p.1-28 |
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Main Authors: | , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | •Global ecosystem model captures biome-scale carbon flows through plankton food web.•Quantitative, holistic global planktonic food web carbon budgets derived.•Respiration/remineralization highly distributed across the planktonic food web.•Muted cross-biome differences in mesozooplankton trophic level.•Step toward more quantitative planktonic food web predictions in changing climate.
Global-scale planktonic ecosystem models exhibit large differences in simulated net primary production (NPP) and assessment of planktonic food web fluxes beyond primary producers has been limited, diminishing confidence in carbon flux estimates from these models. In this study, a global ocean-ice-ecosystem model was assessed against a suite of observation-based planktonic food web flux estimates, many of which were not considered in previous modeling studies. The simulation successfully captured cross-biome differences and similarities in these fluxes after calibration of a limited number of highly uncertain yet influential parameters. The resulting comprehensive carbon budgets suggested that shortened food webs, elevated growth efficiencies, and tight consumer-resource coupling enable oceanic upwelling systems to support 45% of pelagic mesozooplankton production despite accounting for only 22% of ocean area and 34% of NPP. In seasonally stratified regions (42% of ocean area and 40% of NPP), weakened consumer-resource coupling tempers mesozooplankton production to 41% and enhances export below 100m to 48% of the global total. In oligotrophic systems (36% of ocean area and 26% of NPP), the dominance of small phytoplankton and low consumer growth efficiencies supported only 14% of mesozooplankton production and 17% of export globally. Bacterial production, in contrast, was maintained in nearly constant proportion to primary production across biomes through the compensating effects of increased partitioning of NPP to the microbial food web in oligotrophic ecosystems and increased bacterial growth efficiencies in more productive areas. Cross-biome differences in mesozooplankton trophic level were muted relative to those invoked by previous work such that significant differences in consumer growth efficiencies and the strength of consumer-resource coupling were needed to explain sharp cross-biome differences in mesozooplankton production. Lastly, simultaneous consideration of multiple flux constraints supports a highly distributed view of respiration across the planktonic food web r |
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ISSN: | 0079-6611 1873-4472 |
DOI: | 10.1016/j.pocean.2013.07.001 |