Abstract

Two distinct pathways of carbon flow are currently recognized in deep sea aquatic food webs: a short pathway based on phytoplankton production known as planktonic and a longer one, which also includes bacteria, protozoans, and the process known as the microbial loop, referred to collectively as the microbial food web. Considering the microbial loop complements the current vision of aquatic food webs, which today continues to be limited in this respect. In this sense, the analysis of natural abundance of the steady isotopes of carbon and nitrogen in aquatic organisms is a technique which permits the definition of the role of the trophic groups which are part of food web. The proportion of isotopes of carbon indicates the autotrophic energy source of an organism while the proportion of nitrogen isotopes, permits to infer, based on the process of trophic breaking, the level of the organisms studied.

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