Assesses microbial recovery patterns in estuarine ecosystems after a typhoon, suggesting salinity's critical role in stability.
Extreme weather events are increasing pressure on coastal ecosystems and the biogeochemical services they sustain, but the factors shaping microbial resistance and recovery after typhoons remain unclear. Here we tracked bacterioplankton community dynamics across the Jinjiang River–Quanzhou Bay estuary before and after Typhoon Haikui and analysed seven additional storm-event datasets. Preexisting salinity gradients were strongly associated with poststorm community stability. Low-salinity riverine communities showed a prolonged compositional shift, expansion of fast-growing opportunistic taxa, and reduced co-occurrence network complexity. In contrast, high-salinity bay communities showed greater compositional resistance and faster apparent recovery, patterns consistent with stronger environmental filtering, rare-taxon responses, and more connected co-occurrence networks. A meta-analysis of additional storm-event datasets supported the broader relevance of this pattern. Together, these findings suggest that poststorm microbial recovery is temporally delayed and spatially heterogeneous, and that salinity gradients may help identify relatively stable and vulnerable zones in coastal ecosystems. Preexisting salinity gradients shape coastal ecosystem stability after typhoons, with low-salinity communities undergoing prolonged state shifts and high-salinity communities showing strong resistance, based on bacterioplankton time-series observations and an analysis of multiple storm events.
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Du et al. (2026) studied this question.
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