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Cross-shelf structure and distribution of mesozooplankton communities in the East-Siberian Sea and the adjacent Arctic Ocean

机译:东西伯利亚海和邻近北冰洋的中层浮游动物群落的跨架结构和分布

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摘要

The East-Siberian Sea (ESS) plays a significant role in circulation of surface water and biological production in the Arctic, yet due to its remote location and historically difficult sampling conditions remains the most understudied of all Arctic shelf seas, with even baseline information on biological communities absent in literature. Weaim to fill this gap by describing the distribution and community structure of mesozooplankton in the ESS and the adjacent Arctic Ocean based on recent (September 2009, 2015) as well as historical (August-September 1946, 1948)observations. We found that the overall biomass and abundance during our studies were significantly lower than in the adjacent Chukchi Sea, but higher than historical estimates from theESS, around 25-35mgDWm(-3). The diversity was low and characteristic for other Arctic shelf seas, with increasing number of species in deeper waters. Biomass was highest at the shelf break, where it approached 70mgDWm(-3), and was mainly composed of the large copepod Calanusglacialis. On the shelf, abundance and biomass were low (10-20mgDWm(-3)) andwas dominated by small copepods and chaetognaths. Several distinct assemblages of zooplankton were identified and related to the physical properties of the water masses present. A striking result was the presence of both Atlantic and Pacific expatriates in offshore waters close to the shelf break, but generally not on the shelfitself. Tracking these advected organisms could be a useful tool in determining the pathways, extent, and transit time of Atlantic and Pacific water entering the Arctic.
机译:东西伯利亚海(ESS)在北极的地表水循环和生物生产中发挥着重要作用,但是由于其偏远地区和历史上困难的采样条件仍然是所有北极陆架海中研究最多的地方,甚至有基线信息文献中缺少生物群落。我们通过根据最近(2009年9月,2015年)和历史(1946年9月至1948年9月)的观测资料来描述ESS和邻近北冰洋中型浮游动物的分布和群落结构,来填补这一空白。我们发现,在我们的研究中,总体生物量和丰度明显低于相邻的楚科奇海,但高于ESS的历史估计值,约为25-35mgDWm(-3)。多样性低,是其他北极大陆架海的特征,深海水域的物种数量增加。货架期的生物量最高,接近70mgDWm(-3),主要由大型co足类Calanusglacialis组成。在架子上,丰度和生物量较低(10-20mgDWm(-3)),并且以小型co足类和石斑鱼为主。确定了几种不同的浮游动物组合,并与存在的水团的物理性质有关。引人注目的结果是大西洋人和太平洋人都在靠近架子断裂的近海水域存在,但通常不在架子本身上。追踪这些平流生物可能是确定大西洋和太平洋水进入北极的途径,范围和传播时间的有用工具。

著录项

  • 来源
    《Polar biology》 |2019年第7期|1353-1367|共15页
  • 作者单位

    UiT Arctic Univ Norway, Fac Biosci Fisheries & Econ, Dept Arctic & Marine Biol, N-9037 Tromso, Norway|Russian Acad Sci, Shirshov Inst Oceanol, 36 Nakhimova Ave, Moscow 117997, Russia;

    Russian Acad Sci, Shirshov Inst Oceanol, 36 Nakhimova Ave, Moscow 117997, Russia;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Arctic Ocean; Zooplankton; Pelagic ecosystems; Climate change;

    机译:北冰洋;浮游生道;骨质生态系统;气候变化;

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