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Transcriptomic evidence for microbial sulfur cycling in the eastern tropical North Pacific oxygen minimum zone

机译:转录组证据,证明了东部热带北太平洋氧气最低带中微生物的硫循环

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摘要

Microbial communities play central roles in ocean biogeochemical cycles, and are particularly important in in oceanic oxygen minimum zones (OMZs). However, the key carbon, nitrogen, and sulfur (S) cycling processes catalyzed by OMZ microbial communities are poorly constrained spatially, temporally, and with regard to the different microbial groups involved. Here we sample across dissolved oxygen (DO) gradients in the oceans’ largest OMZ by volume—the eastern tropical North Pacific ocean, or ETNP—and quantify 16S rRNA and functional gene transcripts to detect and constrain the activity of different S-cycling groups. Based on gene expression profiles, putative dissimilatory sulfite reductase (dsrA) genes are actively expressed within the ETNP OMZ. dsrA expression was limited almost entirely to samples with elevated nitrite concentrations, consistent with previous observations in the Eastern Tropical South Pacific OMZ. dsrA and ‘reverse’ dissimilatory sulfite reductase (rdsrA) genes are related and the associated enzymes are known to operate in either direction—reducing or oxidizing different S compounds. We found that rdsrA genes and soxB genes were expressed in the same samples, suggestive of active S cycling in the ETNP OMZ. These data provide potential thresholds for S cycling in OMZs that closely mimic recent predictions, and indicate that S cycling may be broadly relevant in OMZs.
机译:微生物群落在海洋生物地球化学循环中起着重要作用,在海洋最小氧区(OMZs)中尤其重要。但是,由OMZ微生物群落催化的关键碳,氮和硫(S)循环过程在空间,时间和涉及的不同微生物组方面受到的约束较弱。在这里,我们对海洋中最大的OMZ(体积)(东部热带北太平洋或ETNP)中的溶解氧(DO)梯度进行采样,并量化16S rRNA和功能性基因转录本,以检测和限制不同S循环群的活动。根据基因表达谱,推定的异化亚硫酸盐还原酶(dsrA)基因在ETNP OMZ中活跃表达。 dsrA表达几乎完全限于亚硝酸盐浓度升高的样品,这与先前在东部热带南太平洋OMZ中的观察结果一致。 dsrA和“反向”异化亚硫酸盐还原酶(rdsrA)基因是相关的,并且已知相关的酶可在任一方向上起作用-还原或氧化不同的S化合物。我们发现rdsrA基因和soxB基因在相同的样品中表达,提示在ETNP OMZ中有活跃的S循环。这些数据为OMZ中的S循环提供了潜在的阈值,这些阈值紧密模拟了最近的预测,并表明S循环在OMZ中可能广泛相关。

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