“…Like modern lacustrine ecosystems (e.g., Odum, 1971;De Santo, 1978;Ward, 1992), Morrison siliciclastic and carbonate lacustrine ecosystems were probably supported by primary productivity generated by autotrophs, such as plankton, algae, charophytes, and plants, which had little or no fossil record in the Morrison but are likely to have been present and from terrestrial inputs as CPOM, FPOM, and DOM. Here, the food web was detritivore and autotroph based, the detritivores supported by CPOM and FPOM and the autotrophs supported by DOM and photosynthesis.…”