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Phytoplankton abundance and community structure in the Antarctic polar frontal region during austral summer of 2009

Phytoplankton abundance and community structure in the Antarctic polar frontal region during austral summer of 2009
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摘要 The Antarctic polar front region in the Southern Ocean is known to be most productive. We studied the phytoplankton community structure in the Indian sector at this frontal location during late austral summer (February, 2009) onboard R/V Akademic Boris Petrov. We used the phytoplankton and microheterotrophs abundance, as also the associated physico-chemical parameters to explain the low phytoplankton abundance in the study region. This study emphasizes the shift of phytoplankton, from large (>10 μm) to small (<10 μm) size. The phytoplankton abundance appears to be controlled by physical parameters and by nutrient concentrations and also by the microheterotrophs (ciliates and dinoflagellates) which exert a strong grazing pressure. This probably reduces small (<10 μm) and large (>10 μm) phytoplankton abundance during the late austral summer. This study highlights the highly productive polar front nevertheless becomes a region of low phytoplankton abundance, due to community shifts towards pico-phytoplankton (<10 μm) during late austral summer. The Antarctic polar front region in the Southern Ocean is known to be most productive. We studied the phytoplankton community structure in the Indian sector at this frontal location during late austral summer (February, 2009) onboard R/V Akademic Boris Petrov. We used the phytoplankton and microheterotrophs abundance, as also the associated physico-chemical parameters to explain the low phytoplankton abundance in the study region. This study emphasizes the shift of phytoplankton, from large (〉10μm) to small (〈10μm) size. The phytoplankton abundance appears to be controlled by physical parameters and by nutrient concentrations and also by the microheterotrophs (ciliates and dinoflagellates) which exert a strong grazing pressure. This probably reduces small (〈10 μm) and large (〉10 μm) phytoplankton abundance during the late austral summer. This study highlights the highly productive polar front nevertheless becomes a region of low phytoplankton abundance, due to community shifts towards pico-phytoplankton (〈 10μm) during late austral summer.
出处 《Chinese Journal of Oceanology and Limnology》 SCIE CAS CSCD 2013年第1期21-30,共10页 中国海洋湖沼学报(英文版)
基金 Supported by the Ministry of Earth Science(MoES),New Delhi,India one of the ongoing projects in National Centre for Antarctic and Ocean Research(NCAOR)(No.36/2012)
关键词 微型浮游植物 植物群落结构 南半球 丰度 夏季 南极 额叶 物理化学参数 Southern Ocean polar front diatom ciliate dinoflagellate
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