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Plankton community respiration and bacterial metabolism in a North Atlantic Shelf Sea during spring bloom development (April 2015)

机译:春季盛开期间北大西洋搁板海中的浮游生物群落呼吸作用和细菌代谢(2015年4月)

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Spring phytoplankton blooms are important events in Shelf Sea pelagic systems as the increase in carbon production results in increased food availability for higher trophic levels and the export of carbon to deeper waters and the sea-floor. It is usually accepted that the increase in phytoplankton abundance and production is followed by an increase in plankton respiration. However, this expectation is derived from field studies with a low temporal sampling resolution (5-15 days). In this study we have measured the time course of plankton abundance, gross primary production, plankton community respiration, respiration of the plankton size classes (>0.8 mu m and 0.2-0.8 mu m) and bacterial production at <= 5 day intervals during April 2015 in order to examine the phasing of plankton autotrophic and heterotrophic processes. Euphotic depth-integrated plankton community respiration increased five-fold (from 22 +/- 4 mmol O-2 m(-2) d(-1) on 4th April to 119 +/- 4 mmol O-2 m(-2) d(-1) on 15th April) at the same time as gross primary production also increased five-fold, (from 114 +/- 5 to 613 +/- 28 mmol C m(-2) d(-1)). Bacterial production began to increase during the development of the bloom, but did not reach its maximum until 5 days after the peak in primary production and plankton respiration. The increase in plankton community respiration was driven by an increase in the respiration attributable to the > 0.8 mu m size fraction of the plankton community (which would include phytoplankton, microzooplankton and particle attached bacteria). Euphotic depth-integrated respiration of the 0.2-0.8 mu m size fraction (predominantly free living bacteria) decreased and then remained relatively constant (16 +/- 3 - 11 +/- 1 mmol O-2 m(-2) d(-1)) between the first day of sampling (4th April) and the days following the peak in chlorophyll-a (20th and 25th April). Recent locally synthesized organic carbon was more than sufficient to fulfil the bacterial carbon requirement in the euphotic zone during this productive period. Changes in bacterial growth efficiencies (BGE, the ratio of bacterial production to bacterial carbon demand) were driven by changes in bacterial production rates increasing from < 30 +/- 14% on 4th April to 51 +/- 11% on 25th of April. This study therefore shows a concurrent rather than a phased increase in primary production and community respiration attributable to cells > 0.8 mu m during the development of the spring bloom, followed 5 days later by a peak in bacterial production. In addition, the size fractionated respiration rates and high growth efficiencies suggest that free living bacteria are not the major producers of CO2 before, during and a few days after this shelf sea spring phytoplankton bloom.
机译:春季浮游植物开花是架海中上层系统的重要事件,因为碳产量的增加导致更高营养层的食物供应量增加以及向更深水域和海底的碳出口。通常认为,浮游植物丰度和产量的增加是浮游生物呼吸增加的结果。但是,这种期望来自时间采样分辨率较低(5-15天)的现场研究。在这项研究中,我们测量了4月份浮游生物丰度,初级生产总值,浮游生物群落呼吸,浮游生物大小等级(> 0.8微米和0.2-0.8微米)的呼吸以及细菌产生的时间过程,间隔时间<= 5天2015年,以研究浮游生物自养和异养过程的阶段。深度共生浮游生物群落呼吸增加了五倍(从4月4日的22 +/- 4 mmol O-2 m(-2)d(-1)增加到119 +/- 4 mmol O-2 m(-2) d(-1)在4月15日),同时初级生产总值也增加了五倍(从114 +/- 5增至613 +/- 28 mmol C m(-2)d(-1))。在开花过程中,细菌的产量开始增加,但是直到初级产量和浮游生物呼吸达到峰值后的5天才达到最大值。浮游生物群落呼吸的增加是由呼吸增加所驱动的,这归因于浮游生物群落的大小> 0.8μm(包括浮游植物,微浮游植物和附着颗粒的细菌)。 0.2-0.8微米大小部分(主要是游离的活细菌)的深度共生呼吸下降,然后保持相对恒定(16 +/- 3-11 +/- 1 mmol O-2 m(-2)d(- 1))在采样的第一天(4月4日)和叶绿素a高峰之后的第二天(4月20日至25日)之间。最近的本地合成有机碳足以满足该生产期富营养区细菌碳的需求。细菌生长速率的变化从4月4日的<30 +/- 14%增加到4月25日的51 +/- 11%,驱动了细菌生长效率的变化(BGE,细菌产量与细菌碳需求的比率)。因此,这项研究表明,在春季开花过程中,一次主要产量和社区呼吸的并发而不是分阶段的增加,这归因于细胞> 0.8微米,随后5天后细菌产量达到峰值。此外,大小分级的呼吸速率和高生长效率表明,在这种架子春季浮游植物开花之前,之中和之后,游离的活菌并不是二氧化碳的主要生产者。

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