Ren Ze, Luo Wei, Zhang Cheng
Research and Development Center for Watershed Environmental Eco-Engineering, Advanced Institute of Natural Sciences, Beijing Normal University, Zhuhai, China.
School of Environment, Beijing Normal University, Beijing, China.
Front Microbiol. 2022 Jul 25;13:944646. doi: 10.3389/fmicb.2022.944646. eCollection 2022.
Thermokarst lakes are widely distributed in cold regions as a result of ice-rich permafrost thaw. Disentangling the biogeography of abundant and rare microbes is essential to understanding the environmental influences, assembly mechanisms, and responses to climate change of bacterial communities in thermokarst lakes. In light of this, we assessed the abundant and rare bacterial subcommunities in sediments from thermokarst lakes across the Qinghai-Tibet Plateau (QTP). The operational taxonomic unit (OTU) richness was more strongly associated with location and climate factors for abundant subcommunities, while more strongly associated with physicochemical variables for rare subcommunities. The relative abundance of abundant and rare taxa showed opposite patterns with abundant taxa having greater relative abundance at higher latitude and pH, but at lower mean annual precipitation and nutrients. Both the abundant and rare subcommunities had a clear distribution pattern along the gradient of latitude and mean annual precipitation. Abundant subcommunities were dominantly shaped by dispersal limitation processes (80.9%), while rare subcommunities were shaped almost equally by deterministic (47.3%) and stochastic (52.7%) processes. The balance between stochastic and deterministic processes was strongly environmentally adjusted for rare subcommunities, while not associated with environmental changes for abundant subcommunities. The results shed light on biogeography patterns and structuring mechanisms of bacterial communities in thermokarst lakes, improving our ability to predict the influences of future climate change on these lakes.
热喀斯特湖由于富含冰的永久冻土融化而广泛分布于寒冷地区。解析丰富和稀有微生物的生物地理学对于理解热喀斯特湖细菌群落的环境影响、组装机制以及对气候变化的响应至关重要。鉴于此,我们评估了青藏高原热喀斯特湖沉积物中丰富和稀有的细菌亚群落。对于丰富的亚群落,操作分类单元(OTU)丰富度与位置和气候因素的相关性更强,而对于稀有的亚群落,与物理化学变量的相关性更强。丰富和稀有分类群的相对丰度呈现相反的模式,丰富分类群在较高纬度和pH值下相对丰度更高,但在年平均降水量和养分较低时相对丰度更高。丰富和稀有的亚群落沿纬度和年平均降水量梯度均有明显的分布模式。丰富的亚群落主要受扩散限制过程影响(80.9%),而稀有的亚群落几乎由确定性(47.3%)和随机性(52.7%)过程同等塑造。对于稀有的亚群落,随机和确定性过程之间的平衡受到强烈的环境调节,而对于丰富的亚群落则与环境变化无关。这些结果揭示了热喀斯特湖细菌群落的生物地理学模式和构建机制,提高了我们预测未来气候变化对这些湖泊影响的能力。