Coastal Upwelling Under Anthropogenic Influence Drives the Community Change, Assembly Process, and Co‐Occurrence Pattern of Coral Associated Microorganisms

Abstract

AbstractSummer upwelling areas may serve as a thermal refuge for coral reefs under climate change, and the environmental adaptation of scleractinian coral to upwelling environments remains to be further understood. In this work, we systematically analyzed how the coral holobionts of Galaxea fascicularis respond to different environments between the Qiongdong upwelling and non‐upwelling regions. The presence of colder and more saline water was found in seasonal upwelling region east of Hainan Island. Compared with the corals in the non‐upwelling environment, the corals from the upwelling environment generally had higher Symbiodiniaceae density, tissue biomass, and protein content. Evident spatial differences existed in Symbiodiniaceae composition among different regions, and the corals in the upwelling region had remarkably higher symbiont diversity. Importantly, the coastal upwelling under anthropogenic influence (i.e., nutrient pollution and coastal development) shaped coral bacterial communities significantly and decreased their diversity. Local adaptations of coral to environmental changes can be inferred from the flexibility and ecological functions of the coral core microbiome. In particular, the coastal upwelling environment led assembly of coral‐associated bacteria more deterministic rather than stochastic. In the upwelling region, microbial co‐occurrences had more positive interactions but the ecological network structure had a lower stability. These findings deepen the understanding of the ecological impact of upwelling on coral adaptation in the Anthropocene.