Microbial activities along a 20 million-year-old pristine oil reservoir

Lisa Voskuhl, Hannah Möhlen, Christian Schlautmann, Sadjad Mohammadian, Ann-Christin Severmann, Johannes Koch, John Köhne, Erling Rykkelid, Joachim Rinna, Rainer Meckenstock
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Abstract

Studies on oil reservoir microbiology typically take samples from producing reservoirs and sample fluids that have been pumped to the surface. This comes with problems since producing oil reservoirs are affected by production processes leading to changes in environmental conditions and the natural microbiome. Hence, pumped samples do not display an unaltered picture of the spatial distribution and composition of the microorganisms in the reservoir. We took 13 samples from a freshly drilled sediment core of a pristine, heavily biodegraded oil reservoir in the North Sea. Core samples originated from above, within, and below the reservoir. 16S rRNA gene amplicon sequencing of the microbiome revealed distinct differences between sediments and formation water, indicating that studies on microbiomes from formation water alone are not necessarily representative for the microbial processes in an oil reservoir. Fluorescence microscopy showed that microorganisms live in small microcolonies on the sediment surface. CT-scanning with image analysis visualized the water phase distribution inside the reservoir sediments and clearly indicated water-filled voids that might be habitable for microorganisms, enlarging the surface for potential biodegradation. Employing microcosm experiments and reverse isotope labelling, we were able to determine the first degradation rates measured from cores above, within, and below a reservoir ranging from no activity up to 1 mM CO 2 /(g sediment x year) , Results indicate significant degradation potential from autochthonous microorganisms in the reservoir above the water-contact-zone. Evading the general issues of produced oil samples for studying microbiomes results in a more realistic picture of an oil reservoir unaffected by production artefacts.
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微生物沿着两千万年前的原始油藏活动
油层微生物学研究通常从生产油藏和泵送到地面的样品流体中取样。这就带来了一些问题,因为生产油藏受到生产过程的影响,导致环境条件和天然微生物群的变化。因此,泵送的样品不能显示储层中微生物的空间分布和组成不变的图像。我们从北海一个原始的、严重生物降解的油藏新钻探的沉积物岩心中提取了13个样本。岩心样品来自储层上方、内部和下方。微生物组的16S rRNA基因扩增子测序显示沉积物和地层水之间存在明显差异,表明仅对地层水微生物组进行研究并不一定能代表油藏中的微生物过程。荧光显微镜显示微生物生活在沉积物表面的小微菌落中。ct扫描和图像分析可视化了水库沉积物内部的水相分布,并清楚地指出了可能适合微生物居住的充满水的空隙,扩大了潜在生物降解的表面。通过微观实验和反同位素标记,我们能够确定从储层上方、内部和下方的岩心中测量到的第一次降解率,范围从无活动到1 mM CO 2 /(g沉积物x年),结果表明水接触带上方储层中的本地微生物具有显著的降解潜力。为了研究微生物组,避免了采出油样品的一般问题,从而获得了不受生产人工制品影响的油藏的更真实的图像。
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