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极地海区浮游动物对全球气候变化的响应极其敏感,其群落结构已成为研究全球变化对海洋生态系统影响的重要指标,而DNA条形码则是浮游动物种类鉴定的有效工具。采用线粒体细胞色素c氧化酶第一亚基编码基因(mtCOI)特异扩增测序的方法,分析了南大洋32种常见浮游动物的94条DNA条形码序列,其长度分布在830碱基到1050碱基之间。发现南极常见浮游动物种内遗传差异均值为0.67%,分布在0—2.6%之间;同属近源种间遗传差异均值为14.3%,分布在0.1%—29.3%之间。哲水蚤属的近缘哲水蚤(Calanus propinquus)和C.simillimus遗传相似度非常高。考虑到上述两者在形态和遗传上的相似性,本研究认为两种可能为同种异名,有待开展深入研究确认C.simillimus种的地位。除了哲水蚤属的两种外,所有样品种内、种间遗传差异显著,且同种的不同样品都聚到一起形成单系群。结果表明mtCOI序列可以作为DNA条形码实现南极浮游动物常见种的准确鉴定(水母和海樽等胶质浮游动物的有效性未验证)。以上结果也得到了示踪向量分析的证实。本研究新增的DNA条形码数据以及新提供的兼并引物必将推动南极浮游动物环境样品的宏基因组学研究。 相似文献
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Nitrous oxide （N2O） distribution patterns in the Bering Sea basin （BSB） and Indian Sector of the Southern Ocean （ISSO） were described and compared. In both sites, the waters were divided into four layers： surface layer, subsurface layer, N2O maximum layer, and deep water. Simulations were made to find out the most important factors that regulate the N2O distribution patterns in different layers of both sites. The results showed that in the surface water, N2O was more understaturated in the ISSO than the BSB. This phenom- enon in the surface water of ISSO may result from ice melt water intrusion and northeastward transport of the Antarctic surface water. Results of the rough estimation of air-sea fluxes during the expedition were （-0.34±0.07）-（-0.64±0.13） μmol/（m2·d） and （-1.47±0.42）-（-1.77±0.51） μmol/（m-2·d） for the BSB and the ISSO, respectively. Strongly stratified surface layer and temperature minimum layer restricted exchange across the thermocline. The N2O maximum existed in higher concentration and deeper in the BSB than the ISSO, but their contribution to the upper layer by eddy diffusions was negligible. In deep waters, a concentration difference of 5 nmol/L N2O between these two sites was found, which suggested that N2O production occurred during thermohaline circulation. N2O may be a useful tracer to study important large-scale hydrographic processes. 相似文献
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Angelika Brandt Huw Griffiths Julian Gutt Katrin Linse Stefano Schiaparelli Tosca Ballerini Bruno Danis Olaf Pfannkuche 《极地研究(英文版)》2014,(3):204-212
Despite recent progress in deep-sea biodiversity assessments in the Southern Ocean （SO）, there remain gaps in our knowledge that hamper efficient deep-sea monitoring in times of rapid climate change. These include geographical sampling bias, depth and size-dependent faunal gaps in biology, ecology, distribution, and phylogeography, and the evolution of SO species. The phenomena of species patchiness and rarity are still not well understood, possibly because of our limited understanding of physiological adaptations and thresholds. Even though some shallow water species have been investigated physiologically, community-scale studies on the effects of multiple stressors related to ongoing environmental change, including temperature rise, ocean acidification, and shifts in deposition of phytoplankton, are completely unknown for deep-sea organisms. Thus, the establishment of long-term and coordinated monitoring programs, such as those rapidly growing under the umbrella of the Southern Ocean Observing System （SOOS） or the Deep Ocean Observing Strategy （DOOS）, may represent unique tools for measuring the status and trends of deep-sea and SO ecosystems. 相似文献
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这是一个难忘的南极夏季,濒临南大洋普里兹湾东南极大陆拉斯曼丘陵的中山站随着2011年2月底中国第27次南极考察队圆满完成任务安全返航,这里又恢复了平日的寂静,就在撤离的1周前,他们完成了1个战略和战术上都具有重要意义的漂亮行动。 相似文献