A Spatially Restricted Distribution of Thermophilic Endospores in Laptev Sea Shelf Sediments Suggests a Limited Dispersal by Local Geofluids

IF 2.7 2区 地球科学 Q2 BIOLOGY
Geobiology Pub Date : 2024-09-11 DOI:10.1111/gbi.12618
Emelie Ståhl, Anna Linderholm, Volker Brüchert
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Abstract

Thermospores, the dormant resting stages of thermophilic bacteria, have been shown to be frequent but enigmatic components of cold marine sediments around the world. Multiple hypotheses have been proposed to explain their distribution, emphasizing their potential as model organisms for studying microbial dispersal via ocean currents. In the Arctic Ocean, the abundance and diversity of thermospores have previously been assumed to be low. However, this assessment has been based on data mainly from the western fjords of Svalbard, thus leaving most of the Arctic unexplored. Here, we expand the knowledge about the distribution of thermospores in the Arctic Ocean by investigating the abundance and diversity of thermospores in heated shelf sediments from three sites in the outer Laptev Sea. Two of the sites are located in an area with methane-emitting cold seeps with a thermogenic source signature suggestive of an origin in a deep hydrocarbon reservoir, while the third site is a reference site not known to be impacted by seepage. We found that activity of viable thermospore populations was more prominent at one of the investigated seep sites. This finding is supported by both radiotracer growth experiments showing thermophilic, sulfate-reducing activity triggered by heating, as well as 16S gene sequence analyses showing significantly enriched ASVs affiliated to the phylum Firmicutes following high-temperature incubations. An enrichment of the sulfate-reducing, endospore-forming class Desulfotomaculia in heated samples compared to unheated samples was also observed. Furthermore, several ASVs identified at the seep site are closely related to thermospore-producing bacteria associated with the deep biosphere, including hydrocarbon and hydrothermal systems. Based on the combined information from induced activity, estimated abundance, and phylogenetic composition using 16S rRNA gene sequencing, we propose likely source environments and dispersal vectors for thermospores in the Arctic Ocean.

Abstract Image

拉普捷夫海大陆架沉积物中嗜热内生孢子的空间限制性分布表明当地地质流体的传播有限
热孢子是嗜热细菌的休眠静止阶段,已被证明是世界各地寒冷海洋沉积物中经常出现的神秘成分。人们提出了多种假说来解释它们的分布,强调了它们作为研究微生物通过洋流扩散的模式生物的潜力。在北冰洋,热孢子的丰度和多样性以前一直被认为很低。然而,这种评估主要基于斯瓦尔巴群岛西部峡湾的数据,因此北极大部分地区尚未被探索。在这里,我们通过研究拉普捷夫海外海三个地点的加热陆架沉积物中热孢子的丰度和多样性,扩大了对北冰洋热孢子分布的了解。其中两个地点位于有甲烷排放冷渗漏的区域,其热源特征表明该渗漏源于深层碳氢化合物储层,而第三个地点则是一个参考地点,没有受到渗漏的影响。我们发现,有活力的热孢子种群的活动在其中一个调查过的渗漏点更为突出。这一发现得到了放射性示踪剂生长实验的支持,实验显示加热会引发嗜热的硫酸盐还原活动,16S 基因序列分析也显示高温培养后属于真菌门的 ASVs 显著富集。与未加热的样本相比,加热样本中富含硫酸盐还原、内生孢子形成类 Desulfotomaculia。此外,在渗漏点发现的几种 ASV 与深层生物圈(包括碳氢化合物和热液系统)中产生热孢子的细菌密切相关。根据诱导活动、估计丰度和使用 16S rRNA 基因测序的系统发育组成等综合信息,我们提出了北冰洋热孢子的可能来源环境和传播载体。
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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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