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揭示泰蒂斯深海高盐缺氧盆地卤层中微生物的活动。

Unveiling microbial activities along the halocline of Thetis, a deep-sea hypersaline anoxic basin.

机构信息

Woods Hole Oceanographic Institution, Woods Hole, MA, USA.

CNR-Institute for Coastal Marine Environment, Messina, Italy.

出版信息

ISME J. 2014 Dec;8(12):2478-89. doi: 10.1038/ismej.2014.100. Epub 2014 Jun 20.

Abstract

Deep-sea hypersaline anoxic basins (DHABs) in the Eastern Mediterranean Sea are considered some of the most hostile environments on Earth. Little is known about the biochemical adaptations of microorganisms living in these habitats. This first metatranscriptome analysis of DHAB samples provides significant insights into shifts in metabolic activities of microorganisms as physicochemical conditions change from deep Mediterranean sea water to brine. The analysis of Thetis DHAB interface indicates that sulfate reduction occurs in both the upper (7.0-16.3% salinity) and lower (21.4-27.6%) halocline, but that expression of dissimilatory sulfate reductase is reduced in the more hypersaline lower halocline. High dark-carbon assimilation rates in the upper interface coincided with high abundance of transcripts for ribulose 1,5-bisphosphate carboxylase affiliated to sulfur-oxidizing bacteria. In the lower interface, increased expression of genes associated with methane metabolism and osmoregulation is noted. In addition, in this layer, nitrogenase transcripts affiliated to uncultivated putative methanotrophic archaea were detected, implying nitrogen fixation in this anoxic habitat, and providing evidence of linked carbon, nitrogen and sulfur cycles.

摘要

深海高盐缺氧盆地(DHABs)被认为是地球上最恶劣的环境之一。对于生活在这些栖息地的微生物的生物化学适应,人们知之甚少。这是首次对 DHAB 样本进行的宏转录组分析,深入了解了微生物代谢活性随物理化学条件从深地中海海水向卤水变化而发生的变化。对忒提斯 DHAB 界面的分析表明,硫酸盐还原作用在上层(盐度为 7.0-16.3%)和下层(盐度为 21.4-27.6%)盐跃层都有发生,但在更咸的下层盐跃层中,异化硫酸盐还原酶的表达减少。在上层界面,高暗碳同化率与硫氧化细菌相关的核酮糖 1,5-二磷酸羧化酶的转录物丰度较高相一致。在下层界面,与甲烷代谢和渗透压调节相关的基因表达增加。此外,在这一层中,检测到与未培养的潜在甲烷营养古菌相关的固氮酶转录物,这意味着在这个缺氧生境中存在氮固定,并为碳、氮和硫循环的关联提供了证据。

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