Modest net autotrophy in the oligotrophic ocean

The metabolic state of the oligotrophic subtropical ocean has long been debated. Net community production (NCP) represents the balance of autotrophic carbon fixation with heterotrophic respiration. Many in vitro NCP estimates based on oxygen incubation methods and the corresponding scaling relations...

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Published in:Global Biogeochemical Cycles
Main Authors: Letscher, Robert T., Moore, J. Keith
Language:unknown
Published: 2022
Subjects:
Online Access:http://www.osti.gov/servlets/purl/1465338
https://www.osti.gov/biblio/1465338
https://doi.org/10.1002/2016GB005503
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spelling ftosti:oai:osti.gov:1465338 2023-07-30T04:05:32+02:00 Modest net autotrophy in the oligotrophic ocean Letscher, Robert T. Moore, J. Keith 2022-01-03 application/pdf http://www.osti.gov/servlets/purl/1465338 https://www.osti.gov/biblio/1465338 https://doi.org/10.1002/2016GB005503 unknown http://www.osti.gov/servlets/purl/1465338 https://www.osti.gov/biblio/1465338 https://doi.org/10.1002/2016GB005503 doi:10.1002/2016GB005503 54 ENVIRONMENTAL SCIENCES 58 GEOSCIENCES 2022 ftosti https://doi.org/10.1002/2016GB005503 2023-07-11T09:28:17Z The metabolic state of the oligotrophic subtropical ocean has long been debated. Net community production (NCP) represents the balance of autotrophic carbon fixation with heterotrophic respiration. Many in vitro NCP estimates based on oxygen incubation methods and the corresponding scaling relationships used to predict the ecosystem metabolic balance have suggested the ocean gyres to be net heterotrophic; however, all in situ NCP methods find net autotrophy. Reconciling net heterotrophy requires significant allochthonous inputs of organic carbon to the oligotrophic gyres to sustain a preponderance of respiration over in situ production. Here we use the first global ecosystem-ocean circulation model that contains representation of the three allochthonous carbon sources to the open ocean, to show that the five oligotrophic gyres exhibit modest net autotrophy throughout the seasonal cycle. Annually integrated rates of NCP vary in the range ~1.5–2.2 mol O 2 m -2 yr -1 across the five gyre systems; however, seasonal NCP rates are as low as ~1 ± 0.5 mmol O2 m -2 d -1 for the North Atlantic. Volumetric NCP rates are heterotrophic below the 10% light level; however, they become net autotrophic when integrated over the euphotic zone. Observational uncertainties when measuring these modest autotrophic NCP rates as well as the metabolic diversity encountered across space and time complicate the scaling up of in vitro measurements to the ecosystem scale and may partially explain the previous reports of net heterotrophy. The oligotrophic ocean is autotrophic at present; however, it could shift toward seasonal heterotrophy in the future as rising temperatures stimulate respiration. Other/Unknown Material North Atlantic SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy) Global Biogeochemical Cycles 31 4 699 708
institution Open Polar
collection SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy)
op_collection_id ftosti
language unknown
topic 54 ENVIRONMENTAL SCIENCES
58 GEOSCIENCES
spellingShingle 54 ENVIRONMENTAL SCIENCES
58 GEOSCIENCES
Letscher, Robert T.
Moore, J. Keith
Modest net autotrophy in the oligotrophic ocean
topic_facet 54 ENVIRONMENTAL SCIENCES
58 GEOSCIENCES
description The metabolic state of the oligotrophic subtropical ocean has long been debated. Net community production (NCP) represents the balance of autotrophic carbon fixation with heterotrophic respiration. Many in vitro NCP estimates based on oxygen incubation methods and the corresponding scaling relationships used to predict the ecosystem metabolic balance have suggested the ocean gyres to be net heterotrophic; however, all in situ NCP methods find net autotrophy. Reconciling net heterotrophy requires significant allochthonous inputs of organic carbon to the oligotrophic gyres to sustain a preponderance of respiration over in situ production. Here we use the first global ecosystem-ocean circulation model that contains representation of the three allochthonous carbon sources to the open ocean, to show that the five oligotrophic gyres exhibit modest net autotrophy throughout the seasonal cycle. Annually integrated rates of NCP vary in the range ~1.5–2.2 mol O 2 m -2 yr -1 across the five gyre systems; however, seasonal NCP rates are as low as ~1 ± 0.5 mmol O2 m -2 d -1 for the North Atlantic. Volumetric NCP rates are heterotrophic below the 10% light level; however, they become net autotrophic when integrated over the euphotic zone. Observational uncertainties when measuring these modest autotrophic NCP rates as well as the metabolic diversity encountered across space and time complicate the scaling up of in vitro measurements to the ecosystem scale and may partially explain the previous reports of net heterotrophy. The oligotrophic ocean is autotrophic at present; however, it could shift toward seasonal heterotrophy in the future as rising temperatures stimulate respiration.
author Letscher, Robert T.
Moore, J. Keith
author_facet Letscher, Robert T.
Moore, J. Keith
author_sort Letscher, Robert T.
title Modest net autotrophy in the oligotrophic ocean
title_short Modest net autotrophy in the oligotrophic ocean
title_full Modest net autotrophy in the oligotrophic ocean
title_fullStr Modest net autotrophy in the oligotrophic ocean
title_full_unstemmed Modest net autotrophy in the oligotrophic ocean
title_sort modest net autotrophy in the oligotrophic ocean
publishDate 2022
url http://www.osti.gov/servlets/purl/1465338
https://www.osti.gov/biblio/1465338
https://doi.org/10.1002/2016GB005503
genre North Atlantic
genre_facet North Atlantic
op_relation http://www.osti.gov/servlets/purl/1465338
https://www.osti.gov/biblio/1465338
https://doi.org/10.1002/2016GB005503
doi:10.1002/2016GB005503
op_doi https://doi.org/10.1002/2016GB005503
container_title Global Biogeochemical Cycles
container_volume 31
container_issue 4
container_start_page 699
op_container_end_page 708
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