Downward fluxes of particulate organic matter in coastal and oceanic areas off Chile: The role of the OMZ and functional groups of the plankton

Vertical fluxes of particles have been estimated during the last decade in coastal and oceanic systems off central-southern Chile. Free-drifting, cylindrical sediment traps have been deployed below the mixing layer from coastal areas, while automatic, cone-shaped sediment traps have been anchored in...

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Autores principales: González,H E, Daneri,G, Menschel,E, Marchant,M, Pantoja,S, Hebbeln,D, Barria,C, Vera,R, Iriarte,J
Lenguaje:English
Publicado: Facultad de Ciencias Naturales y Oceanográficas, Universidad de Concepción 2006
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Acceso en línea:http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0717-65382006000300007
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spelling oai:scielo:S0717-653820060003000072007-10-30Downward fluxes of particulate organic matter in coastal and oceanic areas off Chile: The role of the OMZ and functional groups of the planktonGonzález,H EDaneri,GMenschel,EMarchant,MPantoja,SHebbeln,DBarria,CVera,RIriarte,J Particulate organic matter fluxes oxygen minimum zone zooplankton functional groups sediment traps central Chile Vertical fluxes of particles have been estimated during the last decade in coastal and oceanic systems off central-southern Chile. Free-drifting, cylindrical sediment traps have been deployed below the mixing layer from coastal areas, while automatic, cone-shaped sediment traps have been anchored in deep oceanic areas. Vertical fluxes toward 2300 m depth off Coquimbo were dominated by calcium carbonate (~70 mg m-2 d-1) instead of particulate organic carbon (POC ~7 mg m-2 d-1), where foraminifers (Neogloboquadrina pachyderma) and faecal pellets of Euphausia mucronata and Oikopleura spp, played important roles as vehicles for carbonate and carbon, respectively. In coastal upwelling systems, (i. e. Concepción), the dominant vertical flux was POC, mainly driven by euphausiids faecal strings and diatoms of the genera Thalassiosira, Chaetoceros and Skeletonema. Bacterial degradation of exported POC towards deeper layer of the ocean seems not to be significantly affected by the oxic versus hypoxic levels of dissolved oxygen characteristics of different water masses.info:eu-repo/semantics/openAccessFacultad de Ciencias Naturales y Oceanográficas, Universidad de ConcepciónGayana (Concepción) v.70 suppl.1 20062006-10-01text/htmlhttp://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0717-65382006000300007en10.4067/S0717-65382006000300007
institution Scielo Chile
collection Scielo Chile
language English
topic Particulate organic matter
fluxes
oxygen minimum zone
zooplankton functional groups
sediment traps
central Chile
spellingShingle Particulate organic matter
fluxes
oxygen minimum zone
zooplankton functional groups
sediment traps
central Chile
González,H E
Daneri,G
Menschel,E
Marchant,M
Pantoja,S
Hebbeln,D
Barria,C
Vera,R
Iriarte,J
Downward fluxes of particulate organic matter in coastal and oceanic areas off Chile: The role of the OMZ and functional groups of the plankton
description Vertical fluxes of particles have been estimated during the last decade in coastal and oceanic systems off central-southern Chile. Free-drifting, cylindrical sediment traps have been deployed below the mixing layer from coastal areas, while automatic, cone-shaped sediment traps have been anchored in deep oceanic areas. Vertical fluxes toward 2300 m depth off Coquimbo were dominated by calcium carbonate (~70 mg m-2 d-1) instead of particulate organic carbon (POC ~7 mg m-2 d-1), where foraminifers (Neogloboquadrina pachyderma) and faecal pellets of Euphausia mucronata and Oikopleura spp, played important roles as vehicles for carbonate and carbon, respectively. In coastal upwelling systems, (i. e. Concepción), the dominant vertical flux was POC, mainly driven by euphausiids faecal strings and diatoms of the genera Thalassiosira, Chaetoceros and Skeletonema. Bacterial degradation of exported POC towards deeper layer of the ocean seems not to be significantly affected by the oxic versus hypoxic levels of dissolved oxygen characteristics of different water masses.
author González,H E
Daneri,G
Menschel,E
Marchant,M
Pantoja,S
Hebbeln,D
Barria,C
Vera,R
Iriarte,J
author_facet González,H E
Daneri,G
Menschel,E
Marchant,M
Pantoja,S
Hebbeln,D
Barria,C
Vera,R
Iriarte,J
author_sort González,H E
title Downward fluxes of particulate organic matter in coastal and oceanic areas off Chile: The role of the OMZ and functional groups of the plankton
title_short Downward fluxes of particulate organic matter in coastal and oceanic areas off Chile: The role of the OMZ and functional groups of the plankton
title_full Downward fluxes of particulate organic matter in coastal and oceanic areas off Chile: The role of the OMZ and functional groups of the plankton
title_fullStr Downward fluxes of particulate organic matter in coastal and oceanic areas off Chile: The role of the OMZ and functional groups of the plankton
title_full_unstemmed Downward fluxes of particulate organic matter in coastal and oceanic areas off Chile: The role of the OMZ and functional groups of the plankton
title_sort downward fluxes of particulate organic matter in coastal and oceanic areas off chile: the role of the omz and functional groups of the plankton
publisher Facultad de Ciencias Naturales y Oceanográficas, Universidad de Concepción
publishDate 2006
url http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0717-65382006000300007
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