Organic matter, such as detritus, occurs naturally in marine sediments. However, anthropogenic activities, such as historical timber industry practices and nutrient enrichment (eutrophication) leading to algal blooms, have enriched organic matter in marine sediments, compromising the stability of benthic communities. Added organic material can facilitate microorganisms, which alter the chemistry of the water in marine sediment. This study focused on factors associated with the success of benthic anaerobic bacteria that reduce sulfate into sulfide, which can be detrimental to organisms living in and on the sediment. We investigated if wood or algae would be a more productive carbon source for sulfate reducing bacteria and if grain size, fine versus coarse, would affect the amount of sulfide produced by anaerobic bacteria. Sediment microbial communities were cultivated in a four-week long mesocosm experiment in which wood or algae carbon sources were mixed in fine or coarse sediment. We measured sulfide levels throughout the experiment to determine which treatments were most productive. We found that algae led to earlier and higher sulfide levels within four weeks, as compared to wood. Furthermore, fine grained sediment produced higher concentrations of sulfide, particularly in the presence of algae. Our findings suggest organic material in the form of algae, such as from algal blooms, is a more readily available source of carbon for sulfate reducing bacteria. Future research could extend the timeline of an experiment to investigate what sulfide levels may be produced with wood in sediment.