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Mapping the lithic colonization at the boundaries of life in Northern Victoria Land, Antarctica

机译:绘制南极维多利亚州北部维多利亚州生活边界的石器殖民地

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The endolithic microbial communities of the Antarctic represent a borderline lifestyle in the most hostile ice-free areas of the continent. The extreme adaptation of microbes in these communities renders them very sensitive to environmental changes. To date, the actual distribution of these communities has never been investigated; yet, this information would define the geographic limits for life at present and supply a useful tool for monitoring any possible future variation related to climate change. In this study, most of the outcrops of Northern and of one site in Southern Victoria Land were recorded by altitudinal and sea distance gradients. The presence of endolithic life was determined by in situ observation, by microscopic observation of rock fragments in the laboratory, and, for doubtful samples, by culture experiment. Colonizers were present in more than 87 % of the visited sites. The presence of lithic life in Victoria Land appears to be wider than that reported 14 years earlier. The colonization trend follows climatic variation, with epiliths prevailing in coastal sites and decreasing towards the interior, while chasmoendoliths and cryptoendoliths increase and become predominant from the coast towards the inland sites. Typical cryptoendolithic colonization was exclusive on porous rocks as sandstone, chasmoendolithic colonization occurred even in less porous but translucent rocks as granite and quartz. Multivariate analysis of the combined results clearly indicates the pivotal role of the rock type in the colonization of endolithic micro-organisms; sandstone allows lithobionts to push themselves towards areas characterized by harsher conditions.
机译:在该大陆最不利的无冰地区,南极的石器时代微生物群落代表了一种边缘化的生活方式。这些社区中微生物的极端适应使它们对环境变化非常敏感。迄今为止,尚未调查这些社区的实际分布。但是,这些信息将定义当前生命的地理限制,并提供有用的工具来监视与气候变化有关的任何未来可能的变化。在这项研究中,北部的大部分露头和南部维多利亚地区的一个露头都是通过海拔和海域距离梯度记录的。通过现场观察,在实验室中通过显微镜观察岩石碎片以及对于可疑样品通过培养实验来确定内膜生命的存在。在超过87%的访问地点中都存在定居者。维多利亚州土地上的石器生活似乎比14年前报道的要广泛。殖民化趋势随气候变化而变化,表石在沿海地区盛行,向内逐渐减少,而滑石和隐隐石则增加,并从沿海到内陆地区占主导地位。典型的隐岩质殖民化是砂岩等多孔岩石所独有的,甚至在孔隙度较低但半透明的岩石(如花岗岩和石英)中也发生了异岩质殖民化。综合结果的多变量分析清楚地表明了岩石类型在内生微生物定殖中的关键作用。砂岩可以使石锂离子将自身推向条件更恶劣的地区。

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