Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA.
Nature. 2013 Jul 11;499(7457):205-8. doi: 10.1038/nature12230. Epub 2013 Jun 12.
Scientific ocean drilling has revealed a deep biosphere of widespread microbial life in sub-seafloor sediment. Microbial metabolism in the marine subsurface probably has an important role in global biogeochemical cycles, but deep biosphere activities are not well understood. Here we describe and analyse the first sub-seafloor metatranscriptomes from anaerobic Peru Margin sediment up to 159 metres below the sea floor, represented by over 1 billion complementary DNA (cDNA) sequence reads. Anaerobic metabolism of amino acids, carbohydrates and lipids seem to be the dominant metabolic processes, and profiles of dissimilatory sulfite reductase (dsr) transcripts are consistent with pore-water sulphate concentration profiles. Moreover, transcripts involved in cell division increase as a function of microbial cell concentration, indicating that increases in sub-seafloor microbial abundance are a function of cell division across all three domains of life. These data support calculations and models of sub-seafloor microbial metabolism and represent the first holistic picture of deep biosphere activities.
科学大洋钻探揭示了海底沉积物中广泛存在的微生物生命的深海生物圈。海洋地下的微生物代谢可能在全球生物地球化学循环中起着重要作用,但深海生物圈的活动还不太清楚。在这里,我们描述和分析了来自秘鲁大陆架海底以下 159 米的海底沉积物的第一批海底宏转录组,这些沉积物由超过 10 亿个互补 DNA (cDNA) 序列读数代表。氨基酸、碳水化合物和脂质的厌氧代谢似乎是主要的代谢过程,并且异化亚硫酸盐还原酶 (dsr) 转录本的特征与孔隙水硫酸盐浓度特征一致。此外,参与细胞分裂的转录本随着微生物细胞浓度的增加而增加,这表明海底微生物丰度的增加是所有三个生命领域细胞分裂的函数。这些数据支持了对海底微生物代谢的计算和模型,代表了对深海生物圈活动的第一个整体描述。