Department of Marine Science, University of Otago, Dunedin, New Zealand.
Scripps Institution of Oceanography, University of California at San Diego, La Jolla, California.
Glob Chang Biol. 2018 Aug;24(8):3642-3653. doi: 10.1111/gcb.14291. Epub 2018 May 16.
Organic matter produced by the sea ice microbial community (SIMCo) is an important link between sea ice dynamics and secondary production in near-shore food webs of Antarctica. Sea ice conditions in McMurdo Sound were quantified from time series of MODIS satellite images for Sept. 1 through Feb. 28 of 2007-2015. A predictable sea ice persistence gradient along the length of the Sound and evidence for a distinct change in sea ice dynamics in 2011 were observed. We used stable isotope analysis (δ C and δ N) of SIMCo, suspended particulate organic matter (SPOM) and shallow water (10-20 m) macroinvertebrates to reveal patterns in trophic structure of, and incorporation of organic matter from SIMCo into, benthic communities at eight sites distributed along the sea ice persistence gradient. Mass-balance analysis revealed distinct trophic architecture among communities and large fluxes of SIMCo into the near-shore food web, with the estimates ranging from 2 to 84% of organic matter derived from SIMCo for individual species. Analysis of patterns in density, and biomass of macroinvertebrate communities among sites allowed us to model net incorporation of organic matter from SIMCo, in terms of biomass per unit area (g/m ), into benthic communities. Here, organic matter derived from SIMCo supported 39 to 71 per cent of total biomass. Furthermore, for six species, we observed declines in contribution of SIMCo between years with persistent sea ice (2008-2009) and years with extensive sea ice breakout (2012-2015). Our data demonstrate the vital role of SIMCo in ecosystem function in Antarctica and strong linkages between sea ice dynamics and near-shore secondary productivity. These results have important implications for our understanding of how benthic communities will respond to changes in sea ice dynamics associated with climate change and highlight the important role of shallow water macroinvertebrate communities as sentinels of change for the Antarctic marine ecosystem.
海冰微生物群落(SIMCo)产生的有机物是南极近岸食物网中海冰动态和次级生产力之间的重要环节。从 2007 年至 2015 年 9 月 1 日至 2 月 28 日的 MODIS 卫星图像时间序列中量化了麦克默多海峡的海冰状况。观察到沿着海峡长度存在可预测的海冰持续时间梯度,并且 2011 年海冰动态发生明显变化。我们使用 SIMCo、悬浮颗粒有机物(SPOM)和浅水(10-20 米)大型无脊椎动物的稳定同位素分析(δC 和 δN),揭示了沿海冰持续时间梯度分布的八个地点的底栖群落中的营养结构模式和 SIMCo 有机物的纳入情况。质量平衡分析揭示了群落之间明显的营养结构,以及大量的 SIMCo 进入近岸食物网,估计从 SIMCo 中获得的单个物种的有机物占 2%至 84%。对各站点之间的大型无脊椎动物群落的密度和生物量模式进行分析,使我们能够根据单位面积的生物量(g/m )来模拟从 SIMCo 中净纳入有机物的情况。在这里,SIMCo 衍生的有机物支撑了 39%至 71%的总生物量。此外,对于六种物种,我们观察到在海冰持续时间(2008-2009 年)和海冰爆发时间(2012-2015 年)之间,SIMCo 的贡献有所下降。我们的数据表明,SIMCo 在南极洲生态系统功能中起着至关重要的作用,并且海冰动态和近岸次级生产力之间存在紧密联系。这些结果对于我们理解底栖群落将如何响应与气候变化相关的海冰动态变化以及强调浅水大型无脊椎动物群落作为南极海洋生态系统变化的哨兵具有重要意义。