“…There is a difference between the decomposition of a marine and a terrestrial biomass, since they are from different environments; a marine biomass has resistance to salinity, and consequently different microbial ecosystems are involved in the stages of their degradation [45,46]. In this digestion, there is an assimilation of the main sources of proteins, carbohydrates, and fatty acids, where, in addition to generating a liquid fraction with soluble organic matter, a biogas is generated in the last phases, which is a mixture composed of CH 4 and CO 2 , and to a lesser extent H 2 S, O 2 , and H 2 [47]. The composition of the organic matter dissolved in a leachate generated by decomposition, as well as the proportions of the gases generated, may vary depending on the composition of the decomposing organic matter, rate, and microbial activity, as well as the conditions of the environment; in the case of Sargassum sp.…”