You are not currently logged in.
Access your personal account or get JSTOR access through your library or other institution:
Preview not available
In temperate coastal waters, it is generally assumed that carbon cycling is primarily supported by phytoplankton production, having δ13 C values ranging from -22 to -18%.. In a transect leading out from the Mississippi River, riverine and seawater δ13 C endmembers of particulate organic matter have previously been measured at -25.5 and -20.0%., respectively. In addition, $\detal^13 C$ values of dissolved organic carbon in the northern Gulf of Mexico range from -24.7 to -19.6%., with the more 13 C-depleted values from fresher waters. Assumptions about coastal transport of dissolved organic matter predict that the bacterial δ13 C values hsould fall along the conservative salinity mixing line between terrestrial marine carbon sources. However, in the field survey presented here, δ13 C values of bacteria in coastal regions of the Gulf of Mexico adjacent to the Mississippi River are considerably 13 C-depleted, with values as low as -33%.. These isotope values suggest that carbon from sources other than phytoplankton production or terrestrial organic matter are supporting the production of the bacterial semblage. Possibilities include the incorporation of carbon derived from light hydrocarbons from seep areas and the chemoautotrophic processes of methane oxidation and nitrification. These 13 C-depleted stable isotope data are evidence that bacterially assimilated carbon in the northern Gulf of Mexico may be seasonally uncoupled to surface phytoplankton production.
Limnology and Oceanography