College of Environmental Sciences and Engineering, Peking University, Key Laboratory of Water and Sediment Sciences, Ministry of Education, Beijing, PR China; State Environmental Protection Key Laboratory of All Material Fluxes in River Ecosystems, Peking University, Beijing, PR China; College of Resources and Environmental Sciences, China Agricultural University, Beijing, PR China.
College of Environmental Sciences and Engineering, Peking University, Key Laboratory of Water and Sediment Sciences, Ministry of Education, Beijing, PR China; State Environmental Protection Key Laboratory of All Material Fluxes in River Ecosystems, Peking University, Beijing, PR China.
Water Res. 2023 Dec 1;247:120829. doi: 10.1016/j.watres.2023.120829. Epub 2023 Nov 4.
Archaea, the third proposed domain of life, mediate carbon and nutrient cycling in global natural habitats. Compared with bacteria, our knowledge about archaeal ecological modes in large freshwater environments subject to varying natural and human factors is limited. By metabarcoding analysis of 303 samples, we provided the first integrate biogeography about archaeal compositions, co-existence networks, and assembling processes within a 6000 km continuum of the Yangtze River. Our study revealed that, among the major phyla, water samples owned a higher proportion of Thaumarchaeota (62.8%), while sediments had higher proportions of Euryarchaeota (33.4%) and Bathyarchaeota (18.8%). A decline of polarization in phylum abundance profile was observed from plateau/mountain/hill to basin/plain areas, which was attributed to the increase of nutrients and metals. Planktonic and benthic Bathyarchaeota tended to co-occur with both major (e.g., methanogens or Thermoplasmata) and minor (e.g., Asgard or DPANN) taxa in the non-random networks, harboring the highest richness and abundances of keystone species and contributing the most positively to edge number, node degree, and nearest neighbor degree. Furthermore, we noted significantly positive contributions of Bathyarchaeota abundance and network complexity to the dominance of deterministic process in archaeal assembly (water: 65.3%; sediments: 92.6%), since higher carbon metabolic versatility of Bathyarchaeota would benefit archaeal symbiotic relations. Stronger deterministic assembling was identified at the lower-reach plain, and higher concentrations of ammonium and aluminum separately functioning as nutrition and agglomerator were the main environmental drivers. We lastly found that the Three Gorges Dam caused a simultaneous drop of benthic Bathyarchaeota abundance, network co-existence, and deterministic effects immediately downstream due to riverbed erosion as a local interference. These findings highlight that Bathyarchaeota are a "gatekeeper" to promote fluvial archaeal diversity, stability, and predictability under varying macroscopic and microscopic factors, expanding our knowledge about microbial ecology in freshwater biogeochemical cycling globally.
古菌是生命的第三个被提出的领域,它们在全球自然栖息地中介导碳和营养物质的循环。与细菌相比,我们对受自然和人为因素变化影响的大型淡水环境中古菌生态模式的了解有限。通过对 303 个样本的 metabarcoding 分析,我们提供了关于长江 6000 公里连续体中古菌组成、共存网络和组装过程的第一个综合生物地理学信息。我们的研究表明,在主要门中,水样中拥有更高比例的泉古菌(62.8%),而沉积物中则拥有更高比例的广古菌(33.4%)和深古菌(18.8%)。从高原/山区/丘陵到盆地/平原地区,门丰度分布的极化程度下降,这归因于营养物质和金属的增加。浮游和底栖深古菌倾向于与主要类群(如产甲烷菌或热原体)和次要类群(如阿斯加德或 DPANN)在非随机网络中共存,拥有最多的丰富度和关键物种丰度,并对边缘数量、节点度和最近邻度的贡献最大。此外,我们注意到深古菌丰度和网络复杂性对古菌组装中确定性过程的主导作用有显著的积极贡献(水:65.3%;沉积物:92.6%),因为深古菌具有更高的碳代谢多功能性,有利于古菌共生关系。在下游平原地区,确定性组装更强,而分别作为营养物和团聚体的铵和铝浓度较高则是主要的环境驱动因素。最后,我们发现由于河床侵蚀导致的局部干扰,三峡大坝的建成导致下游底栖深古菌丰度、共存网络和确定性效应同时下降。这些发现强调了深古菌是促进变观宏观和微观因素下河流古菌多样性、稳定性和可预测性的“守门员”,扩展了我们对全球淡水生物地球化学循环中微生物生态学的认识。