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对南极制度转变的底栖生物响应:食物颗粒大小和补充生物学。

Benthic responses to an Antarctic regime shift: food particle size and recruitment biology.

机构信息

Scripps Institution of Oceanography, La Jolla, California, 92093, USA.

Moss Landing Marine Laboratories, Moss Landing, California, 95039 , USA.

出版信息

Ecol Appl. 2019 Jan;29(1):e01823. doi: 10.1002/eap.1823.

DOI:10.1002/eap.1823
PMID:30601593
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC6850755/
Abstract

Polar ecosystems are bellwether indicators of climate change and offer insights into ecological resilience. In this study, we describe contrasting responses to an apparent regime shift of two very different benthic communities in McMurdo Sound, Antarctica. We compared species-specific patterns of benthic invertebrate abundance and size between the west (low productivity) and east (higher productivity) sides of McMurdo Sound across multiple decades (1960s-2010) to depths of 60 m. We present possible factors associated with the observed changes. A massive and unprecedented shift in sponge recruitment and growth on artificial substrata observed between the 1980s and 2010 contrasts with lack of dramatic sponge settlement and growth on natural substrata, emphasizing poorly understood sponge recruitment biology. We present observations of changes in populations of sponges, bryozoans, bivalves, and deposit-feeding invertebrates in the natural communities on both sides of the sound. Scientific data for Antarctic benthic ecosystems are scant, but we gather multiple lines of evidence to examine possible processes in regional-scale oceanography during the eight years in which the sea ice did not clear out of the southern portion of McMurdo Sound. We suggest that large icebergs blocked currents and advected plankton, allowed thicker multi-year ice, and reduced light to the benthos. This, in addition to a possible increase in iron released from rapidly melting glaciers, fundamentally shifted the quantity and quality of primary production in McMurdo Sound. A hypothesized shift from large to small food particles is consistent with increased recruitment and growth of sponges on artificial substrata, filter-feeding polychaetes, and some bryozoans, as well as reduced populations of bivalves and crinoids that favor large particles, and echinoderms Sterechinus neumayeri and Odontaster validus that predominantly feed on benthic diatoms and large phytoplankton mats that drape the seafloor after spring blooms. This response of different guilds of filter feeders to a hypothesized shift from large to small phytoplankton points to the enormous need for and potential value of holistic monitoring programs, particularly in pristine ecosystems, that could yield both fundamental ecological insights and knowledge that can be applied to critical conservation concerns as climate change continues.

摘要

极地生态系统是气候变化的晴雨表,为生态弹性提供了深入的了解。在这项研究中,我们描述了两种截然不同的南极麦克默多海峡海底生物群落对明显的生态系统状态转变的截然不同的反应。我们比较了 20 世纪 60 年代至 2010 年期间,麦克默多海峡东西两侧(西侧生产力较低,东侧生产力较高)至 60 米深处的底栖无脊椎动物丰度和大小的物种特异性模式。我们提出了与观察到的变化相关的可能因素。在 20 世纪 80 年代至 2010 年期间,人工基质上的海绵繁殖和生长出现了大规模的、前所未有的转变,而天然基质上的海绵定植和生长却没有明显的变化,这强调了海绵繁殖生物学的认识不足。我们提出了在海峡两侧的自然群落中,海绵、苔藓动物、双壳类动物和滤食性无脊椎动物种群变化的观察结果。南极底栖生态系统的科学数据很少,但我们收集了多条证据,以检查在 8 年期间,当海冰没有从麦克默多海峡南部清除时,区域尺度海洋学中可能发生的过程。我们认为,大冰山阻止了海流并输运了浮游生物,使多年冰更厚,并减少了底栖生物的光照。除了从快速融化的冰川中释放出的铁可能增加之外,这从根本上改变了麦克默多海峡的初级生产力的数量和质量。从大食物颗粒向小食物颗粒的假设转变与人工基质上海绵的繁殖和生长、滤食多毛类动物和一些苔藓动物的增加以及滤食双壳类动物和海胆的减少以及 Sterechinus neumayeri 和 Odontaster validus 相一致,这些动物主要以底栖硅藻和在春季水华后覆盖海底的大型浮游植物垫为食。不同滤食者群体对从大到小的浮游植物的假设转变的反应表明,特别是在原始生态系统中,对整体监测计划的巨大需求和潜在价值,这不仅可以提供基本的生态见解,还可以为应对气候变化带来的关键保护问题提供知识。

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