“…The spatial heterogeneity of intertidal mudflats, as well as the high degree of temporal variability in process rates, adds to the challenges of accurately quantifying carbon stocks and flows in coastal areas (Legge et al, 2020). MPB spatiotemporal distribution is highly variable, as it is driven by highly variable physical [photosynthetically active radiation (PAR), mud surface temperature (MST), tides, and waves] and biological (grazing, biostabilization, and bioturbation) factors (e.g., Pinckney and Zingmark, 1991;Kingston, 2002;Cohn et al, 2003;Consalvey et al, 2004;Spilmont et al, 2007;Coelho et al, 2009Coelho et al, , 2011Serôdio et al, 2012;Savelli et al, 2018).…”