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Seasonal and interannual phytoplankton production in a sub-Arctic tidewater outlet glacier fjord, SW Greenland

机译:格陵兰西南部的一个沿潮汐流出口冰川峡湾的季节性和年际浮游植物生产

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ABSTRACT: This study describes seasonal patterns and proposes likely drivers of an unusual phytoplankton primary production pattern in the outer-sill region of a tidewater outlet glacier-influenced fjord (Godth?bsfjord) in SW Greenland. It is based on monthly measurements of pelagic primary production and hydrographic conditions during a 7 yr period. Total annual primary production during 2005 to 2012 was between 84.6 and 139.1 g C m-2 yr-1. Two phytoplankton blooms of similar magnitude reoccur in the fjord every year. A ‘classical’ spring bloom of up to 1743 mg C m-2 d-1 occurred in late April/early May in a water column almost fully mixed due to tidal forces at the fjord sill. After the spring bloom, primary production decreased in June, after which a summer bloom of up to 1383 mg C m-2 d-1 built up. This bloom coincided with the development of a pycnocline caused by substantial runoff from the Greenland Ice Sheet every year during midsummer. This observation supports a hypothesis that fjord circulation modes and subglacial freshwater discharge, leading to upwelling of nutrient rich water, stimulate primary production in the fjord. Future changes in the timing or magnitude of meltwater runoff from the Greenland Ice Sheet are thus likely to affect phytoplankton dynamics in the fjord.
机译:摘要:本研究描述了季节性模式,并提出了格陵兰西南部受潮水出口冰川影响的峡湾(Godth?bsfjord)外缘区域浮游植物初级生产模式的异常驱动因素。它基于7年期间中上层初级生产和水文状况的月度测量。 2005年至2012年期间的年度初级总产量在84.6至139.1 g C m -2 yr -1 之间。每年峡湾再次出现两次浮游植物的开花。在4月底/ 5月初,由于潮汐力的作用,几乎完全混合的水柱中发生了高达1743 mg C m -2 d -1 的“经典”春季开花在峡湾。春季开花后,六月的初级产量下降,此后累积了高达1383 mg C m -2 d -1 的夏季开花。每年盛夏,格陵兰冰盖大量径流引起的碧萝oc的出现与这种花开的发展相吻合。这一观察结果支持了一个假设,即峡湾的循环模式和冰川下的淡水排放,导致营养丰富的水上升,刺激了峡湾的初级生产。因此,格陵兰冰原中融水径流的时间或幅度的未来变化可能会影响峡湾浮游植物的动态。

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