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Evidence for Biotic Perchlorate Reduction in Naturally Perchlorate-Rich Sediments of Pilot Valley Basin, Utah

机译:犹他州的飞行员盆地天然高氯酸盐沉积物生物高氯酸盐的证据

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The presence of perchlorate on Mars suggests a possible energy source for sustaining microbial life. Perchlorate-reducing microbes have been isolated from perchlorate-contaminated soils and sediments on the Earth, but to date, never from an environment that is naturally enriched in perchlorate. The arid Pilot Valley paleolake basin in Utah is a Mars analog environment whose sediments are naturally enriched with up to similar to 6.5 mu g kg(-1) perchlorate oxyanions. Here, we present results of field and laboratory studies indicating that perchlorate-reducing microorganisms co-occur with this potential electron acceptor. Biogeochemical data suggest ongoing perchlorate reduction; phylogenetic data indicate the presence of diverse microbial communities; and laboratory enrichments using Pilot Valley sediments show that resident microbes can reduce perchlorate. This is the first article of the co-existence of perchlorate-reducing microbes in an environment where perchlorate occurs naturally, arguing for Pilot Valley's utility as an analog for studying biogeochemical processes that may have occurred, and may yet still be occurring, in ancient martian lacustrine sediments.
机译:MARS上高氯酸盐表明可能的能量来源用于维持微生物寿命。已经从高氯酸盐污染的土壤和地球上的沉积物中分离出高氯酸盐的微生物,但到目前为止,从未来自富含高氯酸盐的环境。在犹他州的干旱试点谷古醇盆地是一个MARS模拟环境,其沉积物自然富集,最多至类似于6.5μgkg(-1)高氯酸盐氧基。在这里,我们存在现场和实验室研究的结果,表明在该潜在的电子受体中还原过氯酸盐还原微生物。生物地球化学数据表明正在进行的高氯酸盐;系统发育数据表明存在不同的微生物社区;使用先导谷沉积物的实验室浓缩表明常驻微生物可以减少高氯酸盐。这是第一个在高氯酸盐发生自然发生的环境中加入高氯酸盐减少微生物的第一个文章,以试验谷的效用作为研究可能发生的生物地球化学过程,并且仍然可能发生在古代火星湖泊沉积物。

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