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Endolithic Cyanobacteria in Halite Rocks from the Hyperarid Core of the Atacama Desert

机译:阿塔卡马沙漠超干旱核心地带的盐岩中的内锂蓝藻

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摘要

In the driest parts of the Atacama Desert there are no visible life forms on soil or rock surfaces. The soil in this region contains only minute traces of bacteria distributed in patches, and conditions are too dry for cyanobacteria that live under translucent stones. Here we show that halite evaporite rocks from the driest part of the Atacama Desert are colonized by cyanobacteria. This colonization takes place just a few millimeters beneath the rock surface, occupying spaces among salt crystals. Our work reveals that these communities are composed of extremely resistant Chroococcidiopsis morphospecies of cyanobacteria and associated het-erotrophic bacteria. This newly discovered endolithic environment is an extremely dry and, at the same time, saline microbial habitat. Photosynthetic microorganisms within dry evaporite rocks could be an important and previously unrecognized target for the search for life within our Solar System.
机译:在阿塔卡马沙漠最干旱的地区,在土壤或岩石表面没有可见的生命形式。该区域的土壤仅含有微量的细菌,分布在斑块中,而且对于生活在半透明结石下的蓝细菌而言,条件太干燥了。在这里,我们显示了来自阿塔卡马沙漠最干燥部分的盐岩蒸发岩被蓝细菌定殖。这种定殖发生在岩石表面以下几毫米处,占据了盐晶体之间的空间。我们的工作表明,这些群落是由蓝细菌和相关的异养细菌组成的极强的耐弯曲球菌形态。这种新近发现的石器内环境非常干燥,同时也是盐类微生物的栖息地。在我们的太阳系内寻找生命的过程中,干燥的蒸发岩中的光合微生物可能是重要且以前无法识别的目标。

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