Phytoplankton chemotaxonomy in the Atlantic sector of the Southern Ocean during late summer 2009

Copyright: 2013 Elsevier. This is an ABSTRACT ONLY. The definitive version is published in Deep-Sea Research Part 1: Oceanographic Research Papers, vol. 78, pp 70-78 A chemotaxonomic investigation of surface phytoplankton was undertaken on a research cruise to the Atlantic sector of the Southern Oce...

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Bibliographic Details
Main Authors: Gibberd, M-J, Kean, E, Barlow, R, Thomalla, Sandy J, Lucas, M
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2013
Subjects:
Online Access:http://hdl.handle.net/10204/7463
http://ac.els-cdn.com/S0967063713000861/1-s2.0-S0967063713000861-main.pdf?_tid=2e5bd630-ebd0-11e3-ac59-00000aacb35f&acdnat=1401876691_47f13ba4be6529c7a06c5c6ee21a7268
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Summary:Copyright: 2013 Elsevier. This is an ABSTRACT ONLY. The definitive version is published in Deep-Sea Research Part 1: Oceanographic Research Papers, vol. 78, pp 70-78 A chemotaxonomic investigation of surface phytoplankton was undertaken on a research cruise to the Atlantic sector of the Southern Ocean during late austral summer 2009. Based on pigment signatures, several distinct regions emerged that were delineated by physical features. CHEMTAX analysis of high performance liquid chromatography (HPLC) pigment data indicated that diatoms generally dominated communities south of the Antarctic Polar Front (APF), particularly in regions of elevated biomass where chlorophyll-a (chl-a) was 41.5 mg l(sup-1) and diatoms comprised 480% of biomass. Pigment signatures representative of haptophytes-8, indicative of Phaeocystis antarctica, were dominant near the ice shelf. Chl-a concentrations were 0.2–0.6 mg l(sup-1) between the APF and the Subtropical Front (STF) and outputs suggested that chlorophytes, haptophytes-8 and haptophyte-6, in the form of coccolithophores, were the major constituents. Very low chl-a levels (o0.2 mg l(sup-1) were observed north of the STF and the prokaryotes Synechococcus spp. and Prochlorococcus spp. were the dominant groups in these oligotrophic waters.