Temporal variability of microbial communities during the past 600 years in a Tibetan lake sediment core

Over the past decades, the Tibetan Plateau has been experiencing rapid climate change and increasing anthropogenic disturbance. The existing multi-proxy sediment records highlight the complex interplay of physical and ecological changes as a response to past climate changes on the Tibetan Plateau. Yet, it remains an open question of how sedimentary microbial communities respond to past climate changes and anthropogenic interventions. Using high-throughput Illumina sequencing, this study investigated the temporal changes of prokaryotic and eukaryotic communities in a Tibetan lake sediment core spanning the last 600 years. There were obvious temporal distributions of prokaryotic and eukaryotic indicator taxa, and these temporal patterns were mainly influenced by mean annual temperature (MAT), total phosphorus (TP) and nitrogen:phosphorus ratio (N:P). The alpha diversity of eukaryotic communities significantly increased with time (P