Abundance and biomass of protozooplankton from the iron-induced phytoplankton bloom during the EisenEx experiment in 2000 in the Southern Ocean

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Autores principales: Henjes, Joachim, Assmy, Philipp, Klaas, Christine, Smetacek, Victor
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 2006
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author Henjes, Joachim
Assmy, Philipp
Klaas, Christine
Smetacek, Victor
author_facet Henjes, Joachim
Assmy, Philipp
Klaas, Christine
Smetacek, Victor
collection Datos científicos de ciencias marinas y ambientales
contents The responses of larger (>50 µm in diameter) protozooplankton groups to a phytoplankton bloom induced by in situ iron fertilization (EisenEx) in the Polar Frontal Zone (PFZ) of the Southern Ocean in austral spring are presented. During the 21 days of the experiment, samples were collected from seven discrete depths in the upper 150 m inside and outside the fertilized patch for the enumeration of acantharia, foraminifera, radiolaria, heliozoa, tintinnid ciliates and aplastidic thecate dinoflagellates. Inside the patch, acantharian numbers increased twofold, but only negligibly in surrounding waters. This finding is of major interest, since acantharia are suggested to be involved in the formation of barite (BaSO_4 ) found in sediments and which is a palaeoindicator of both ancient and modern high productivity regimes. Foraminifera increased significantly in abundance inside and outside the fertilized patch. However the marked increase of juveniles after a full moon event suggests a lunar periodicity in the reproduction cycle of some foraminiferan species rather than a reproductive response to enhanced food availability. In contrast, adult radiolaria showed no clear trend during the experiment, but juveniles increased threefold indicating elevated reproduction. Aplastidic thecate dinoflagellates almost doubled in numbers and biomass, but also increased outside the patch. Tintinnid numbers decreased twofold, although biomass remained constant due to a shift in the size spectrum. Empty tintinnid loricae, however, increased by a factor of two indicating that grazing pressure on this group mainly by copepods intensified during EisenEx. The results show that iron-fertilization experiments can shed light on the biology and the role of these larger protists in pelagic ecosystem which will improve their use as proxies in palaeoceanography.
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institution PANGAEA
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publishDate 2006
publisher PANGAEA
record_format pangaea
spellingShingle Abundance and biomass of protozooplankton from the iron-induced phytoplankton bloom during the EisenEx experiment in 2000 in the Southern Ocean
Henjes, Joachim
Assmy, Philipp
Klaas, Christine
Smetacek, Victor
ANT-XVIII/2; CTD/Rosette; CTD11; CTD118; CTD121; CTD125; CTD130; CTD146; CTD15; CTD150; CTD19; CTD47; CTD52; CTD55; CTD58; CTD64; CTD67; CTD71; CTD75; CTD88; CTD-RO; EisenEx; European Iron Enrichment Experiment in the Southern Ocean; Polarstern; PS58/009-6; PS58/011-3; PS58/012-4; PS58/014-6; PS58/038-7; PS58/041-5; PS58/042-5; PS58/043-4; PS58/045-9; PS58/046-5; PS58/048-5; PS58/049-5; PS58/061-3; PS58/088-7; PS58/090-2; PS58/091-3; PS58/092-6; PS58/107-6; PS58/108-3; PS58 EISENEX; South Atlantic Ocean
The responses of larger (>50 µm in diameter) protozooplankton groups to a phytoplankton bloom induced by in situ iron fertilization (EisenEx) in the Polar Frontal Zone (PFZ) of the Southern Ocean in austral spring are presented. During the 21 days of the experiment, samples were collected from seven discrete depths in the upper 150 m inside and outside the fertilized patch for the enumeration of acantharia, foraminifera, radiolaria, heliozoa, tintinnid ciliates and aplastidic thecate dinoflagellates. Inside the patch, acantharian numbers increased twofold, but only negligibly in surrounding waters. This finding is of major interest, since acantharia are suggested to be involved in the formation of barite (BaSO_4 ) found in sediments and which is a palaeoindicator of both ancient and modern high productivity regimes. Foraminifera increased significantly in abundance inside and outside the fertilized patch. However the marked increase of juveniles after a full moon event suggests a lunar periodicity in the reproduction cycle of some foraminiferan species rather than a reproductive response to enhanced food availability. In contrast, adult radiolaria showed no clear trend during the experiment, but juveniles increased threefold indicating elevated reproduction. Aplastidic thecate dinoflagellates almost doubled in numbers and biomass, but also increased outside the patch. Tintinnid numbers decreased twofold, although biomass remained constant due to a shift in the size spectrum. Empty tintinnid loricae, however, increased by a factor of two indicating that grazing pressure on this group mainly by copepods intensified during EisenEx. The results show that iron-fertilization experiments can shed light on the biology and the role of these larger protists in pelagic ecosystem which will improve their use as proxies in palaeoceanography.
title Abundance and biomass of protozooplankton from the iron-induced phytoplankton bloom during the EisenEx experiment in 2000 in the Southern Ocean
topic ANT-XVIII/2; CTD/Rosette; CTD11; CTD118; CTD121; CTD125; CTD130; CTD146; CTD15; CTD150; CTD19; CTD47; CTD52; CTD55; CTD58; CTD64; CTD67; CTD71; CTD75; CTD88; CTD-RO; EisenEx; European Iron Enrichment Experiment in the Southern Ocean; Polarstern; PS58/009-6; PS58/011-3; PS58/012-4; PS58/014-6; PS58/038-7; PS58/041-5; PS58/042-5; PS58/043-4; PS58/045-9; PS58/046-5; PS58/048-5; PS58/049-5; PS58/061-3; PS58/088-7; PS58/090-2; PS58/091-3; PS58/092-6; PS58/107-6; PS58/108-3; PS58 EISENEX; South Atlantic Ocean
url https://doi.org/10.1594/PANGAEA.552509