Departments of Marine Microbiology and Biogeochemistry and Ocean Systems, NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University, Den Burg, The Netherlands.
Department of Earth Sciences, Faculty of Geosciences, University of Utrecht, Utrecht, The Netherlands.
Geobiology. 2019 Jan;17(1):91-109. doi: 10.1111/gbi.12316. Epub 2018 Oct 3.
Archaea are important players in marine biogeochemical cycles, and their membrane lipids are useful biomarkers in environmental and geobiological studies. However, many archaeal groups remain uncultured and their lipid composition unknown. Here, we aim to expand the knowledge on archaeal lipid biomarkers and determine the potential sources of those lipids in the water column of the euxinic Black Sea. The archaeal community was evaluated by 16S rRNA gene amplicon sequencing and by quantitative PCR. The archaeal intact polar lipids (IPLs) were investigated by ultra-high-pressure liquid chromatography coupled to high-resolution mass spectrometry. Our study revealed both a complex archaeal community and large changes with water depth in the IPL assemblages. In the oxic/upper suboxic waters (<105 m), the archaeal community was dominated by marine group (MG) I Thaumarchaeota, coinciding with a higher relative abundance of hexose phosphohexose crenarchaeol, a known marker for Thaumarchaeota. In the suboxic waters (80-110 m), MGI Nitrosopumilus sp. dominated and produced predominantly monohexose glycerol dibiphytanyl glycerol tetraethers (GDGTs) and hydroxy-GDGTs. Two clades of MGII Euryarchaeota were present in the oxic and upper suboxic zones in much lower abundances, preventing the detection of their specific IPLs. In the deep sulfidic waters (>110 m), archaea belonging to the DPANN Woesearchaeota, Bathyarchaeota, and ANME-1b clades dominated. Correlation analyses suggest that the IPLs GDGT-0, GDGT-1, and GDGT-2 with two phosphatidylglycerol (PG) head groups and archaeol with a PG, phosphatidylethanolamine, and phosphatidylserine head groups were produced by ANME-1b archaea. Bathyarchaeota represented 55% of the archaea in the deeper part of the euxinic zone and likely produces archaeol with phospho-dihexose and hexose-glucuronic acid head groups.
古菌是海洋生物地球化学循环中的重要参与者,其膜脂是环境和地球生物学研究中的有用生物标志物。然而,许多古菌群体仍然未被培养,其脂质组成也未知。在这里,我们旨在扩大对古菌脂质生物标志物的认识,并确定在缺氧黑海水柱中这些脂质的潜在来源。通过 16S rRNA 基因扩增子测序和定量 PCR 评估古菌群落。通过超高压液相色谱与高分辨率质谱联用研究古菌完整极性脂(IPL)。我们的研究揭示了一个复杂的古菌群落,以及 IPL 组合随水深的巨大变化。在有氧/上层亚缺氧水域(<105 m),古菌群落主要由海洋组(MG)I 泉古菌门 Thaumarchaeota 主导,同时六糖磷酸己糖焦磷酸岩藻糖古菌醇的相对丰度较高,这是 Thaumarchaeota 的已知标志物。在亚缺氧水域(80-110 m),MGI Nitrosopumilus sp. 占主导地位,主要产生单糖甘油二磷酸二植烷甘油四醚(GDGTs)和羟基-GDGTs。MGII 广古菌的两个分支在有氧和上层亚缺氧带中存在,但丰度较低,无法检测到其特定的 IPL。在深硫水域(>110 m),属于 DPANN Woesearchaeota、Bathyarchaeota 和 ANME-1b 类群的古菌占主导地位。相关分析表明,具有两个磷脂酰甘油(PG)头基团的 IPLs GDGT-0、GDGT-1 和 GDGT-2 和具有 PG、磷脂乙醇胺和磷脂丝氨酸头基团的 archaeol 由 ANME-1b 古菌产生。Bathyarchaeota 在缺氧区较深部分的古菌中占 55%,可能产生具有磷酸二己糖和己糖-葡糖醛酸头基团的 archaeol。