Multiple trophic levels fueled by recirculation in the Columbia River plume: Columbia river bulge acts as bioreactor
Multiple trophic levels fueled by recirculation in the Columbia River plume: Columbia river bulge acts as bioreactor
Large rivers represent gateways for the transport of terrigenous and anthropogenic material to the coastal ocean. Here we document a ∼700 km2 recirculation or bulge associated with the Columbia River plume that retains recently discharged river water sufficiently to create a regional bioreactor. Fueled by a fluvial nitrate source, this feature stimulated growth across three trophic levels and may buffer this gateway system during periods of increased warming and stratification that lead to decreased ocean productivity, potentially enhancing production at multiple trophic levels and enriching surface waters far from the river mouth.
Kudela, Raphael M.
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Horner-devine, Alexander R.
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Banas, Neil S.
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Hickey, Barbara M.
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Peterson, Tawnya D.
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Mccabe, Ryan M.
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Lessard, Evelyn J.
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Frame, Elizabeth
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Bruland, Kenneth W.
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Jay, David A.
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Peterson, Jay O.
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Peterson, William T.
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Kosro, P. Michael
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Palacios, Sherry L.
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Lohan, Maeve C.
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Dever, Edward P.
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1 September 2010
Kudela, Raphael M.
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Horner-devine, Alexander R.
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Banas, Neil S.
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Hickey, Barbara M.
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Peterson, Tawnya D.
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Mccabe, Ryan M.
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Lessard, Evelyn J.
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Frame, Elizabeth
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Bruland, Kenneth W.
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Jay, David A.
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Peterson, Jay O.
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Peterson, William T.
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Kosro, P. Michael
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Palacios, Sherry L.
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Lohan, Maeve C.
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Dever, Edward P.
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Kudela, Raphael M., Horner-devine, Alexander R., Banas, Neil S., Hickey, Barbara M., Peterson, Tawnya D., Mccabe, Ryan M., Lessard, Evelyn J., Frame, Elizabeth, Bruland, Kenneth W., Jay, David A., Peterson, Jay O., Peterson, William T., Kosro, P. Michael, Palacios, Sherry L., Lohan, Maeve C. and Dever, Edward P.
(2010)
Multiple trophic levels fueled by recirculation in the Columbia River plume: Columbia river bulge acts as bioreactor.
Geophysical Research Letters, 37 (18).
(doi:10.1029/2010GL044342).
Abstract
Large rivers represent gateways for the transport of terrigenous and anthropogenic material to the coastal ocean. Here we document a ∼700 km2 recirculation or bulge associated with the Columbia River plume that retains recently discharged river water sufficiently to create a regional bioreactor. Fueled by a fluvial nitrate source, this feature stimulated growth across three trophic levels and may buffer this gateway system during periods of increased warming and stratification that lead to decreased ocean productivity, potentially enhancing production at multiple trophic levels and enriching surface waters far from the river mouth.
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Published date: 1 September 2010
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Local EPrints ID: 414071
URI: http://eprints.soton.ac.uk/id/eprint/414071
ISSN: 1944-8007
PURE UUID: 8462cc51-f2ad-42f4-a30d-282c38f7da05
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Date deposited: 13 Sep 2017 16:31
Last modified: 16 Mar 2024 04:13
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Contributors
Author:
Raphael M. Kudela
Author:
Alexander R. Horner-devine
Author:
Neil S. Banas
Author:
Barbara M. Hickey
Author:
Tawnya D. Peterson
Author:
Ryan M. Mccabe
Author:
Evelyn J. Lessard
Author:
Elizabeth Frame
Author:
Kenneth W. Bruland
Author:
David A. Jay
Author:
Jay O. Peterson
Author:
William T. Peterson
Author:
P. Michael Kosro
Author:
Sherry L. Palacios
Author:
Edward P. Dever
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