Taxonomic Composition and Growth Rates of Phytoplankton Assemblages at the Subtropical Convergence East of New Zealand

Off the eastern coast of New Zealand, warm, saline, nutrient-poor Subtropical Waters (STW) are separated from cool, fresher, relatively nutrient-rich Sub-Antarctic Waters (SAW) by the Subtropical Convergence (STC). The Chatham Rise, a submarine rise, restricts the latitudinal movement of the STC as...

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Published in:Journal of Plankton Research
Main Authors: Delizo, Liza, Smith, Walker O., Hall, Julie
Format: Text
Language:English
Published: Oxford University Press 2007
Subjects:
Online Access:http://plankt.oxfordjournals.org/cgi/content/short/fbm047v1
https://doi.org/10.1093/plankt/fbm047
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spelling fthighwire:oai:open-archive.highwire.org:plankt:fbm047v1 2023-05-15T13:57:29+02:00 Taxonomic Composition and Growth Rates of Phytoplankton Assemblages at the Subtropical Convergence East of New Zealand Delizo, Liza Smith, Walker O. Hall, Julie 2007-06-02 05:54:04.0 text/html http://plankt.oxfordjournals.org/cgi/content/short/fbm047v1 https://doi.org/10.1093/plankt/fbm047 en eng Oxford University Press http://plankt.oxfordjournals.org/cgi/content/short/fbm047v1 http://dx.doi.org/10.1093/plankt/fbm047 Copyright (C) 2007, Oxford University Press Article TEXT 2007 fthighwire https://doi.org/10.1093/plankt/fbm047 2016-11-16T18:35:37Z Off the eastern coast of New Zealand, warm, saline, nutrient-poor Subtropical Waters (STW) are separated from cool, fresher, relatively nutrient-rich Sub-Antarctic Waters (SAW) by the Subtropical Convergence (STC). The Chatham Rise, a submarine rise, restricts the latitudinal movement of the STC as well as mixing of STW and SAW. Due to this restriction, this sector of the STC is characterized by sharp gradients in temperature, macro- (nitrate, silicate, and phosphate) and micro- (iron) nutrient concentrations. Shipboard incubations were conducted during austral spring 2000 and 2001 to test the hypothesis that these gradients affect the taxonomic composition and/or growth rates of phytoplankton on either side of and at the STC. Maximum chlorophyll a concentrations during 2000 were 0.39 μg L−1, but were an order of magnitude higher in 2001. During both years STC phytoplankton were dominated by diatoms (77% of the total chlorophyll a during austral spring 2000 and 70% during spring 2001), whereas cryptophytes and prasinophytes dominated STW assemblages (27 and 36% during 2000, and 63 and 17% during 2001). Chlorophyll in the SAW was dominated by procaryotes and photosynthetic nanoflagellates during 2000 (17% procaryotes, 68% nanoflagellates), and by diatoms during the austral spring 2001 cruise (53%). Growth rates of the phytoplankton assemblage were determined by 14C-labeling of chlorophyll a and photosynthetic pigments. During 2000 temperature-normalized growth rates were near maximal at the STC, and decreased on average to less than half of the maximum north and south of that front, whereas in 2001 both absolute and relative growth rates were low at all stations. Growth rates did not closely parallel biomass of the various taxa, suggesting that nutrient limitation and/or grazing were significantly impacting standing stocks. It appeared that growth was strongly influenced by nutrients and light, but that biomass was more strongly influenced by grazing. The Subtropical Convergence is a globally important region of ... Text Antarc* Antarctic HighWire Press (Stanford University) Antarctic Austral New Zealand Journal of Plankton Research 29 8 655 670
institution Open Polar
collection HighWire Press (Stanford University)
op_collection_id fthighwire
language English
topic Article
spellingShingle Article
Delizo, Liza
Smith, Walker O.
Hall, Julie
Taxonomic Composition and Growth Rates of Phytoplankton Assemblages at the Subtropical Convergence East of New Zealand
topic_facet Article
description Off the eastern coast of New Zealand, warm, saline, nutrient-poor Subtropical Waters (STW) are separated from cool, fresher, relatively nutrient-rich Sub-Antarctic Waters (SAW) by the Subtropical Convergence (STC). The Chatham Rise, a submarine rise, restricts the latitudinal movement of the STC as well as mixing of STW and SAW. Due to this restriction, this sector of the STC is characterized by sharp gradients in temperature, macro- (nitrate, silicate, and phosphate) and micro- (iron) nutrient concentrations. Shipboard incubations were conducted during austral spring 2000 and 2001 to test the hypothesis that these gradients affect the taxonomic composition and/or growth rates of phytoplankton on either side of and at the STC. Maximum chlorophyll a concentrations during 2000 were 0.39 μg L−1, but were an order of magnitude higher in 2001. During both years STC phytoplankton were dominated by diatoms (77% of the total chlorophyll a during austral spring 2000 and 70% during spring 2001), whereas cryptophytes and prasinophytes dominated STW assemblages (27 and 36% during 2000, and 63 and 17% during 2001). Chlorophyll in the SAW was dominated by procaryotes and photosynthetic nanoflagellates during 2000 (17% procaryotes, 68% nanoflagellates), and by diatoms during the austral spring 2001 cruise (53%). Growth rates of the phytoplankton assemblage were determined by 14C-labeling of chlorophyll a and photosynthetic pigments. During 2000 temperature-normalized growth rates were near maximal at the STC, and decreased on average to less than half of the maximum north and south of that front, whereas in 2001 both absolute and relative growth rates were low at all stations. Growth rates did not closely parallel biomass of the various taxa, suggesting that nutrient limitation and/or grazing were significantly impacting standing stocks. It appeared that growth was strongly influenced by nutrients and light, but that biomass was more strongly influenced by grazing. The Subtropical Convergence is a globally important region of ...
format Text
author Delizo, Liza
Smith, Walker O.
Hall, Julie
author_facet Delizo, Liza
Smith, Walker O.
Hall, Julie
author_sort Delizo, Liza
title Taxonomic Composition and Growth Rates of Phytoplankton Assemblages at the Subtropical Convergence East of New Zealand
title_short Taxonomic Composition and Growth Rates of Phytoplankton Assemblages at the Subtropical Convergence East of New Zealand
title_full Taxonomic Composition and Growth Rates of Phytoplankton Assemblages at the Subtropical Convergence East of New Zealand
title_fullStr Taxonomic Composition and Growth Rates of Phytoplankton Assemblages at the Subtropical Convergence East of New Zealand
title_full_unstemmed Taxonomic Composition and Growth Rates of Phytoplankton Assemblages at the Subtropical Convergence East of New Zealand
title_sort taxonomic composition and growth rates of phytoplankton assemblages at the subtropical convergence east of new zealand
publisher Oxford University Press
publishDate 2007
url http://plankt.oxfordjournals.org/cgi/content/short/fbm047v1
https://doi.org/10.1093/plankt/fbm047
geographic Antarctic
Austral
New Zealand
geographic_facet Antarctic
Austral
New Zealand
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_relation http://plankt.oxfordjournals.org/cgi/content/short/fbm047v1
http://dx.doi.org/10.1093/plankt/fbm047
op_rights Copyright (C) 2007, Oxford University Press
op_doi https://doi.org/10.1093/plankt/fbm047
container_title Journal of Plankton Research
container_volume 29
container_issue 8
container_start_page 655
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