Department of Geological Sciences, Stockholm University, Stockholm, Sweden.
Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden.
Geobiology. 2024 Sep-Oct;22(5):e12618. doi: 10.1111/gbi.12618.
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.
嗜热孢子是嗜热细菌的休眠静止阶段,已被证明是世界各地冷海洋沉积物中常见但神秘的组成部分。已经提出了多种假设来解释它们的分布,强调它们作为通过洋流研究微生物扩散的模型生物的潜力。在北极海洋中,以前假设嗜热孢子的丰度和多样性较低。然而,这种评估主要基于来自斯瓦尔巴西部峡湾的数据,因此大部分北极地区尚未得到探索。在这里,我们通过调查拉普捷夫海外部三个地点加热架沉积物中嗜热孢子的丰度和多样性,扩展了对北极海洋中嗜热孢子分布的了解。其中两个地点位于甲烷排放冷渗出物的区域,具有热成因来源特征,暗示其起源于深部碳氢化合物储层,而第三个地点是一个已知不受渗出物影响的参考点。我们发现,在一个调查的渗出物地点,有活力的嗜热孢子种群的活性更为明显。这一发现得到了放射性示踪剂生长实验的支持,该实验表明加热会触发嗜热、硫酸盐还原活性,以及 16S 基因序列分析的支持,该分析表明,在高温孵育后,与厚壁菌门密切相关的 ASV 显著富集。与未加热的样品相比,加热样品中还观察到硫酸盐还原、内生孢子形成类别的脱硫梭菌的富集。此外,在渗出物地点鉴定的几个 ASV 与与深部生物圈相关的产嗜热孢子细菌密切相关,包括碳氢化合物和热液系统。基于诱导活性、估计丰度和使用 16S rRNA 基因测序的系统发育组成的综合信息,我们提出了北极海洋中嗜热孢子的可能来源环境和扩散载体。