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Differences in structure of northern Australian hypolithic communities according to location rock type and gross morphology

机译:根据位置岩石类型和总体形态北澳大利亚下石器时代群落的结构差异

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摘要

Hypolithic communities (under translucent rocks) were compared between a semi-arid site (Wave Hill) and a site with considerably higher rainfall (Lake Bennett) to test the hypothesis that the communities at the higher rainfall site would be more diverse. A total of 153 cyanobacteria operational taxonomic units (OTUs) were identified, and only 50 of those were found at both sites. Of these, only two were core OTUs, as defined as being present in ≥90% of samples, highlighting the extreme differences in the cyanobacterial communities at the two sites. At Wave Hill, we compared the composition of the cyanobacterial components under two different rock types (quartz and prehnite) to determine if the different minerals would result in different hypolithic communities, but no differences were found. Of the 42 core OTUs found at Wave Hill, 22 (52%) were shared between the two rock types. As hypothesised, the diversity of both cyanobacteria and eukaryotes in the hypolithic communities was significantly higher at Lake Bennett. Some hypolithic communities were thin and tightly adhered to the rock surface, but others were thicker and could be peeled off the rock in sheets. However, the two types were not significantly different in OTU composition. Metazoans, primarily nematodes, were ubiquitous, raising the possibility that nematodes may act as vectors to transport the components of hypolithic communities from rock to rock as a mechanism of colonization.
机译:比较了半干旱地区(波丘山)和降雨量较高的地区(贝内特湖)的半透明群落(半透明岩石下),以检验高降雨部位的群落更加多样化的假设。总共确定了153个蓝细菌操作分类单位(OTU),在两个站点中仅发现了其中的50个。在这些中,只有两个是核心OTU,定义为≥90%的样品中存在OTU,这凸显了这两个位置的蓝细菌群落之间的极端差异。在Wave Hill,我们比较了两种不同岩石类型(石英和葡萄石)下的蓝细菌成分的组成,以确定不同的矿物是否会导致不同的下石器时代的群落,但未发现差异。在Wave Hill发现的42个核心OTU中,两种岩石共有22个(52%)。如所假设的,贝内特湖下石器社区的蓝细菌和真核生物的多样性明显更高。一些石器时代的群落很薄并且紧密地粘附在岩石表面,但是其他的则较厚,可以从岩石上剥落下来。但是,两种类型的OTU组成没有显着差异。后生动物(主要是线虫)无处不在,这增加了线虫可能作为媒介将次石质群落的组成成分从一个岩石运送到另一个岩石的可能性,这是一种定殖的机制。

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