Breithaupt et al. (2020), addressed a blue carbon knowledge gap about apparently increasing rates of coastal wetland organic carbon (OC) burial that had been identified by Breithaupt et al. (2014), concluding that increasing OC burial rates during the past century represent a net acceleration. In Breithaupt et al. (2014), dated mangrove soil cores from southwest Florida showed that rates of sediment accumulation, OC burial, and vertical accretion had all increased in the past century. At that time an explanation for these increases could only be surmised as representing: "(a) a recent increase in delivery, (b) a recent increase in preservation, (c) the regular occurrence of ongoing degradation at each depth over the past century, or (d) some combination of the above including a recent increase combined with ongoing degradation" (Breithaupt et al., 2014). We subsequently applied a combination of radiochemical, geomorphological, and biogeochemical analyses to "determine whether previously documented increases in OC burial rates over the past century represent real acceleration or whether the increases can be attributed to post-depositional degradation of older material or to artifacts of the methods used to measure soil accumulation" (Breithaupt et al., 2020). Our findings indicated the trend of increasing OC burial rates could not be explained by the use of different dating methods, nor by the occurrence of preferential degradation of OC at different soil depths, leading to