Four years of climate warming reduced dark carbon fixation in coastal wetlands.

However, in other seasons, TOC content showed a decreasing trend ( Fig.

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However, nearly all ASVs of Crenarchaeota (99.5 and 95.7% in the Ah and Bh layers, respectively) exhibited an increasing trend under experimental warming, whereas almost all ASVs of Firmicutes (98.3 and 96.0% in the Ah and Bh layers, respectively) were negatively affected by warming ( Fig. 1c–d ).

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