The North Atlantic Ocean plays an important role in the uptake of anthropogenic CO 2 and the global carbon cycle (Friedlingstein et al., 2022;Sarmiento et al., 1995;Takahashi et al., 2009). The northward carbon flux through the Florida Straits is a major contributor to the North Atlantic Ocean carbon budget (Rosón et al., 2003). The quantification of natural and anthropogenic carbon transport across the Florida Straits contributes to the estimation and understanding of the North Atlantic and global carbon budget (Brown et al., 2021;Rosón et al., 2003).In the Florida Straits, the Florida Current passes through productive and diverse marine ecosystems, including extensive shallow and deep coral reef ecosystems (Lee et al., 1992;Schmitz & Richardson, 1991;Sponaugle et al., 2005). Therefore, understanding both the physical and chemical dynamics in the Florida Straits has important biological and ecosystem implications. Within our study region, recent numerical model results suggest that