北极陆快海冰中微藻群落的时空动态

IF 3.8 3区 地球科学 Q1 OCEANOGRAPHY
Rebecca J. Duncan , Janne E. Søreide , Øystein Varpe , Józef Wiktor , Vanessa Pitusi , Elaine Runge , Katherina Petrou
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引用次数: 0

摘要

海冰微藻是极地海洋食物网的重要能量来源,是浮游植物大量繁殖之前的主要碳源。在此,我们研究了春季(4 月至 5 月)挪威斯瓦尔巴特高纬度北极地区六个不同峡湾的陆地快速海冰中的海冰微藻群落动态。我们发现,光照(0.1 - 23% 入射 PAR / 0.1 - 193 μmol 光子 m-2s-1)在决定群落组成方面起着核心作用,在底层冰群落透射光照较多的地点观察到了更多样化的群落。四月份,当冰下透光率相近时,微藻群落相似,与地理位置无关,但五月份群落结构的这种光源分离现象并不明显。在所有地点,集合体都以羽状硅藻为主,其中最丰富的类群是 Nitzschia frigida。然而,随着冰下透光率的增加,我们发现叶绿藻、纤毛藻(Navicula spp.)和纤毛藻(Thalassiosira spp.)的相对丰度也在增加。光照与冰藻生物量中的δ13C富集度和C:N比值之间的正相关关系表明了光照对冰藻生物化学组成的影响。光照与细胞丰度或叶绿素 a 浓度无关。随着气候变化对北极海冰范围和积雪覆盖的预期改变,我们将看到传输到冰底生物群落的光照发生变化。这些变化,无论是雪盖增加导致透光率降低,还是冰层变薄、雪深或降雨量增加导致透光率增加,都可能改变海冰微藻群落的组成,进而影响极地水域二次生产和生物地球化学循环的成败。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Spatio-temporal dynamics in microalgal communities in Arctic land-fast sea ice

Sea ice microalgae are an important source of energy for the polar marine food web, representing the primary carbon source prior to pelagic phytoplankton blooms. Here we investigate community dynamics of sea ice microalgal communities in land-fast sea ice across six different fjords in high-Arctic Svalbard, Norway, during Spring (April – May). We found that light (0.1 – 23% incoming PAR / 0.1 – 193 μmol photons m-2s-1) played a central role in determining community composition, with more diverse assemblages observed in sites with more light transmitted to the bottom ice community. In April, microalgal assemblages were similar when under-ice light transmittance was similar, independent of geographical location, however this light-derived separation of community structure was not evident in May. At all sites, assemblages were dominated by pennate diatoms, with the most abundant taxon being Nitzschia frigida. However, with increasing under-ice light transmittance, we saw an increase in the relative abundance of Dinophyceae, Navicula spp. and Thalassiosira spp.. A positive relationship between light and δ13C enrichment and C:N ratios in the ice algal biomass demonstrated the effect of light on the biochemical composition of ice algae. Light did not correlate with cell abundance or chlorophyll a concentration. With anticipated changes to Arctic sea ice extent and snow cover as a result of climate change, we will see shifts in the light transmitted to the bottom ice community. These shifts, whether caused by reduced light transmittance from increased snow cover or increased light transmittance from thinning ice, snow depth or increased rainfall, will likely alter sea ice microalgal community composition, which in turn, may influence the success of secondary production and biogeochemical cycling in polar waters.

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来源期刊
Progress in Oceanography
Progress in Oceanography 地学-海洋学
CiteScore
7.20
自引率
4.90%
发文量
138
审稿时长
3 months
期刊介绍: Progress in Oceanography publishes the longer, more comprehensive papers that most oceanographers feel are necessary, on occasion, to do justice to their work. Contributions are generally either a review of an aspect of oceanography or a treatise on an expanding oceanographic subject. The articles cover the entire spectrum of disciplines within the science of oceanography. Occasionally volumes are devoted to collections of papers and conference proceedings of exceptional interest. Essential reading for all oceanographers.
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