Liu Jiwen, Huang Fuyan, Liu Jiao, Liu Xiaoyue, Lin Ruiyun, Zhong Xiaosong, Austin Brian, Zhang Xiao-Hua
Frontiers Science Center for Deep Ocean Multispheres and Earth System, and College of Marine Life Sciences, Ocean University of China, Qingdao, 266100 China.
Laboratory for Marine Ecology and Environmental Science, Laoshan Laboratory, Qingdao, 266237 China.
Mar Life Sci Technol. 2023 Apr 7;5(2):257-270. doi: 10.1007/s42995-023-00169-y. eCollection 2023 May.
The majority of marine ammonia oxidizers belong to , a phylum of Archaea, which is distributed throughout the water column. Marine surface waters contain distinct thaumarchaeotal phylotypes compared to the deeper ocean, but spatial dynamics of the surface-associated lineages are largely unsolved. This study of 120 seawater samples from the eastern Chinese marginal seas identified contrasting distribution and association patterns among thaumarchaeotal phylotypes across different dimensions. Horizontally, -like and -like phylotypes dominated the surface water (3 m) of the Yellow Sea (YS) and East China Sea (ECS), respectively, along with increased abundance of total free-living in ECS. Similar compositional changes were observed in the surface microlayer. The spatial heterogeneity of particle-attached was less clear in surface microlayers than in surface waters. Vertically, the -like phylotype increased in abundance from surface to 90 m in ECS, which led to an increase in the proportion of relative to total prokaryotes. This occurred mainly in the free-living fraction. These results indicate a clear size-fractionated niche partitioning, which is more pronounced at lower depths than in the surface water/surface microlayer. In addition, associations of with other microbial taxa varied between phylotypes and size fractions. Our results show that a phylotype-resolved and size-fractionated spatial heterogeneity of the thaumarchaeotal community is present in surface oceanic waters and a vertical variation of the -like phylotype is present in shallow shelf waters.
The online version contains supplementary material available at 10.1007/s42995-023-00169-y.
大多数海洋氨氧化菌属于古菌门,分布于整个水柱中。与深海相比,海洋表层水含有不同的奇古菌门系统发育型,但与表层相关的谱系的空间动态在很大程度上尚未解决。这项对中国东部边缘海120个海水样本的研究确定了奇古菌门系统发育型在不同维度上的对比分布和关联模式。在水平方向上,类似 和类似 的系统发育型分别在黄海(YS)和东海(ECS)的表层水(3米)中占主导地位,同时ECS中总自由生活的 丰度增加。在表面微层中也观察到了类似的组成变化。表面微层中附着颗粒的 的空间异质性不如表层水明显。在垂直方向上,类似 的系统发育型在ECS中从表层到90米深度丰度增加,这导致 相对于总原核生物的比例增加。这主要发生在自由生活部分。这些结果表明存在明显的按大小分级的生态位划分,在较深深度比在表层水/表面微层中更明显。此外, 与其他微生物类群的关联在系统发育型和大小分级之间有所不同。我们的结果表明,在海洋表层水中存在奇古菌群落的系统发育型解析和按大小分级的空间异质性,在浅海大陆架水域中存在类似 的系统发育型的垂直变化。
在线版本包含可在10.1007/s42995-023-00169-y获取的补充材料。