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Arctic spring awakening - Steering principles behind the phenology of vernal ice algal blooms

机译:北极春季觉醒-春季冰藻水华的物候学背后的指导原则

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Marine ecosystems at high latitudes are characterized by extreme seasonal changes in light conditions, as well as a limited period of high primary production during spring and early summer. As light returns at the end of winter to Arctic ice-covered seas, a first algal bloom takes place in the bottom layer of the sea ice. This bottom ice algae community develops through three distinct phases in the transition from winter to spring, starting with phase I, a predominantly net heterotroph community that has limited interaction with the pelagic or benthic realms. Phase II begins in the spring once light for photosynthesis becomes available at the ice bottom, although interaction with the water column and benthos remains limited. The transition to the final phase III is then mainly driven by a balance of atmospheric and oceanographic forcing that induce structural changes in the sea ice and ultimately the removal of algal biomass from the ice. Due to limited data availability an incomplete understanding exists of all the processes determining ice algal bloom phenology and the considerable geographic differences in sympagic algal standing stocks and primary production. We present here the first pan-Arctic compilation of available time-series data on vernal sea ice algal bloom development and identify the most important factors controlling its development and termination. Using data from the area surrounding Resolute Bay (Nunavut, Canada) as an example, we support previous investigations that snow cover on top of the ice influences sea ice algal phenology, with highest biomass development, but also earliest termination of blooms, under low snow cover. We also provide a pan-Arctic overview of sea ice algae standing stocks and primary production, and discuss the pertinent processes behind the geographic differences we observed. Finally, we assess potential future changes in vernal algal bloom phenology as a consequence of climate change, including their importance to different groups of grazers. (C) 2015 Elsevier Ltd. All rights reserved.
机译:高纬度地区的海洋生态系统的特征是光照条件的极端季节性变化,以及春季和初夏期间有限的高初级生产期。随着冬季结束时光返回北极冰雪覆盖的海域,海冰的底层首次出现藻华。从冬季到春季,这个底层冰藻群落经历了三个不同的阶段,从第一阶段开始,该阶段主要是净异养群落,与上层或底栖生物的相互作用有限。尽管与水柱和底栖生物的相互作用仍然受到限制,但一旦冰底有光合作用的光,第二阶段便从春季开始。然后,到最后阶段III的过渡主要是由大气和海洋强迫之间的平衡驱动的,这促使海冰发生结构变化,并最终从冰中去除藻类生物质。由于有限的数据可用性,对确定冰藻水华物候的所有过程以及有症状的藻类常备种群和初级生产的巨大地理差异尚不完全了解。我们在这里展示了有关春季海冰藻类繁殖的可用时间序列数据的第一个泛北极汇编,并确定了控制其发育和终止的最重要因素。以来自Resolute Bay(加拿大努纳武特)周边地区的数据为例,我们支持先前的研究,即冰层上的积雪影响海冰藻类物候,其生物量发育最高,但在低雪条件下最早终止了开花覆盖。我们还提供了北冰洋海藻常规种群和初级生产的概览,并讨论了我们观察到的地理差异背后的相关过程。最后,我们评估了由于气候变化而导致的未来藻类藻类物候变化的潜在变化,包括它们对不同种类的放牧者的重要性。 (C)2015 Elsevier Ltd.保留所有权利。

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  • 来源
    《Progress in Oceanography》 |2015年第12期|151-170|共20页
  • 作者单位

    Helmholtz Ctr Polar & Marine Res, Alfred Wegener Inst, D-27570 Bremerhaven, Germany;

    Univ Manitoba, Dept Geog & Environm, CEOS, Winnipeg, MB R3T 2N2, Canada;

    Norwegian Polar Res Inst, Fram Ctr, N-9296 Tromso, Norway;

    Univ Manitoba, Dept Geog & Environm, CEOS, Winnipeg, MB R3T 2N2, Canada;

    Univ Ctr Svalbard, N-9171 Longyearbyen, Norway|Univ Bergen, Dept Biol, N-5020 Bergen, Norway;

    Univ Quebec, Inst Sci Mer Rimouski Quebec Ocean, Rimouski, PQ G5L 3A1, Canada;

    Greenland Inst Nat Resources, Greenland Climate Res Ctr, Nuuk 3900, Greenland;

    Univ Alaska Fairbanks, Sch Fisheries & Ocean Sci, Fairbanks, AK 99775 USA|Inst Marine Res, N-9294 Tromso, Norway;

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