Biota play an obvious key role in terrestrial and aquatic carbon cycling (Schlesinger & Bernhardt, 2013). Biotamediated carbon cycling is the consequence of basic physiological functions and refers to the transformation of CO 2 into organic matter (OM) through assimilation by primary producers (including plants, algae and autotrophic prokaryotes) and the release of CO 2 (or CH 4 ) through dissimilatory processes such as respiration by consumers (predominantly animals), microbial decomposers (including fungi, bacteria and archaea) and primary producers (Hügler & Sievert, 2011;Rosenberg et al., 2014;Thauer et al., 2008). Besides these direct biota-mediated effects on carbon cycling, biotic interactions between producers, consumers and decomposers can induce important changes in the rate of assimilatory and dissimilatory processes and thereby exert indirect