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Temporal and spatial variation of the phytoplankton assemblage in the eastern Indian sector of the Southern Ocean in summer 2001/2002

机译:2001/2002年夏季南印度洋东部印度洋浮游植物群落的时空变化

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摘要

The abundance and species composition of phytoplankton were investigated at stations in a permanently ice-free (61°S) and seasonally ice-covered area (64°S and 66°30′S) in the eastern Indian sector of the Southern Ocean between November 2001 and March 2002. Although a phytoplankton bloom occurred just after retreat of the sea ice at both stations in the seasonally ice-covered area, vertical stability of the water column during the bloom was weak at the most southerly station. This shows that a bloom can form even under weak vertical stability. In the bloom, diatoms dominated under weak vertical stability and Phaeocystis under strong vertical stability. In the latter case, ice algae largely contributed to development of the bloom. In the later observation period, a subsurface chlorophyll maximum (SCM) was observed at 61°S and 64°S. Species composition was different between the mixed layer and SCM at 64°S, but was uniform with depth at 61°S, indicating that the SCM is formed by different mechanisms.
机译:在十一月之间,在印度洋南部东部的永久无冰区(61°S)和季节性覆冰区(64°S和66°30′S),对站内浮游植物的丰度和物种组成进行了调查。 2001年和2002年3月。尽管在季节性冰雪覆盖地区的两个站都在海冰撤退后立即发生浮游植物开花,但在最南端的站,开花期间水柱的垂直稳定性较弱。这表明即使在较弱的垂直稳定性下也可以形成水华。在花期中,硅藻在垂直稳定性较弱的情况下占主导地位,而藻囊藻在垂直稳定性较弱的情况下占主导地位。在后一种情况下,冰藻在很大程度上促进了水华的形成。在随后的观察期中,在61°S和64°S观察到了地下叶绿素最大值(SCM)。混合层和SCM的物种组成在64°S时有所不同,但在61°S时深度均匀,表明SCM是由不同的机制形成的。

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