单一酸杆菌对温度、pH和O2的响应产生多种brGDGT,为brGDGT的代用物和生物合成提供了培养视角

IF 2.7 2区 地球科学 Q2 BIOLOGY
Geobiology Pub Date : 2022-09-23 DOI:10.1111/gbi.12525
Toby A. Halamka, Jonathan H. Raberg, Jamie M. McFarlin, Adam D. Younkin, Christopher Mulligan, Xiao-Lei Liu, Sebastian H. Kopf
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引用次数: 34

摘要

支链甘油二烷基甘油四醚(brGDGTs)是一种细菌膜脂,由于其相对丰度与环境温度和ph之间存在很强的经验相关性,因此经常被用作古环境指标。尽管brGDGTs在现代和古环境中无处不在,但这些神秘化合物的来源生物仍然难以捉摸,要求古环境应用仅依赖于观察到的环境相关性。以往的实验室和环境研究表明,全球丰富的酸杆菌门可能是自然界中重要的brdgt产生菌。在这里,我们报告了一种培养的酸杆菌,孤杆菌的实验,它的细胞膜的很大一部分(在所有实验中占24±9%)是由一组结构多样的四醚组成的,包括常见的brdgts Ia, IIa, IIIa, Ib和IIb。在温度为15至30°C、pH为5.0至6.5、O2为1%至21%的条件下培养孤杆菌,并在这些生长条件下显示出brGDGT甲基化程度的显著变化。培养中的温度响应与发表的环境数据集中观察到的趋势密切一致,为brGDGT甲基化数与温度之间的经验关系提供了生理基础。然而,brGDGT在较低温度(15°C和20°C)下的甲基化受到培养pH的调节,pH越高甲基化程度越高。相比之下,pH对brGDGT环化几乎没有影响,这支持了细菌群落组成的变化可能是环境样品中观察到的环化数量与pH之间联系的基础。氧浓度同样影响brGDGT甲基化,突出了该环境参数影响古温度重建的潜力。低氧培养条件进一步导致产生罕见的brGDGT异构体,这可能是O2限制的指标。最后,除了先前发现的基于isoc15的单醚和二醚外,在S. usitatus中还产生了brGTGTs(三烷基四醚),这表明brGTGTs的潜在生物合成途径是利用古菌四醚合成酶(Tes)酶的同源物从二醚合成四醚。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Production of diverse brGDGTs by Acidobacterium Solibacter usitatus in response to temperature, pH, and O2 provides a culturing perspective on brGDGT proxies and biosynthesis

Branched glycerol dialkyl glycerol tetraethers (brGDGTs) are bacterial membrane lipids that are frequently employed as paleoenvironmental proxies because of the strong empirical correlations between their relative abundances and environmental temperature and pH. Despite the ubiquity of brGDGTs in modern and paleoenvironments, the source organisms of these enigmatic compounds have remained elusive, requiring paleoenvironmental applications to rely solely on observed environmental correlations. Previous laboratory and environmental studies have suggested that the globally abundant bacterial phylum of the Acidobacteria may be an important brGDGT producer in nature. Here, we report on experiments with a cultured Acidobacterium, Solibacter usitatus, that makes a large portion of its cellular membrane (24 ± 9% across all experiments) out of a structurally diverse set of tetraethers including the common brGDGTs Ia, IIa, IIIa, Ib, and IIb. Solibacter usitatus was grown across a range of conditions including temperatures from 15 to 30°C, pH from 5.0 to 6.5, and O2 from 1% to 21%, and demonstrated pronounced shifts in the degree of brGDGT methylation across these growth conditions. The temperature response in culture was in close agreement with trends observed in published environmental datasets, supporting a physiological basis for the empirical relationship between brGDGT methylation number and temperature. However, brGDGT methylation at lower temperatures (15 and 20°C) was modulated by culture pH with higher pH systematically increasing the degree of methylation. In contrast, pH had little effect on brGDGT cyclization, supporting the hypothesis that changes in bacterial community composition may underlie the link between cyclization number and pH observed in environmental samples. Oxygen concentration likewise affected brGDGT methylation highlighting the potential for this environmental parameter to impact paleotemperature reconstruction. Low O2 culture conditions further resulted in the production of uncommon brGDGT isomers that could be indicators of O2 limitation. Finally, the production of brGTGTs (trialkyl tetraethers) in addition to the previously discovered iso-C15-based mono- and diethers in S. usitatus suggests a potential biosynthetic pathway for brGDGTs that uses homologs of the archaeal tetraether synthase (Tes) enzyme for tetraether synthesis from diethers.

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来源期刊
Geobiology
Geobiology 生物-地球科学综合
CiteScore
6.80
自引率
5.40%
发文量
56
审稿时长
3 months
期刊介绍: The field of geobiology explores the relationship between life and the Earth''s physical and chemical environment. Geobiology, launched in 2003, aims to provide a natural home for geobiological research, allowing the cross-fertilization of critical ideas, and promoting cooperation and advancement in this emerging field. We also aim to provide you with a forum for the rapid publication of your results in an international journal of high standing. We are particularly interested in papers crossing disciplines and containing both geological and biological elements, emphasizing the co-evolutionary interactions between life and its physical environment over geological time. Geobiology invites submission of high-quality articles in the following areas: Origins and evolution of life Co-evolution of the atmosphere, hydrosphere and biosphere The sedimentary rock record and geobiology of critical intervals Paleobiology and evolutionary ecology Biogeochemistry and global elemental cycles Microbe-mineral interactions Biomarkers Molecular ecology and phylogenetics.
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