Global climate change significantly increased the duration
of droughts
in intermittent rivers, impacting benthic microbial-mediated biogeochemical
processes. However, the impact of prolonged droughts on the carbon
contribution of intermittent rivers remains poorly understood. In
this study, we investigated the potential effects of varying drought
gradients (ranging from 20 to 130 days) on benthic biofilms community
structure (algae, bacteria, and fungi) and their carbon metabolism
functions (ecosystem metabolism and carbon dioxide (CO2) emission fluxes) using mesocosm experiments. Our findings indicate
that longer drought durations lead to reduced alpha diversity and
community heterogeneity, tighter interdomain networks, and an increased
role of stochastic processes in community assembly, with a discernible
threshold at around 60 days. Concurrently, the biofilm transforms
into a carbon sink following a drought period of 60 days, as evidenced
by the transformation of CO2 emission fluxes from 633.25
± 194.69 to −349.61 ± 277.79 mg m–2 h–1. Additionally, the partial least-squares path
model revealed that the resilience of algal communities and network
stability may drive biofilm’s transformation into a carbon
sink, primarily through the heightened resilience of autotrophic metabolism.
This study underscores the significance of the carbon contribution
from intermittent rivers, as the shift in carbon metabolism functions
with increasing droughts could lead to skewed estimations of current
riverine carbon fluxes.