Archaeocyaths are the most abundant sponges from the Cambrian period, forming the first animal reef communities over 500 million years ago. The Archaeocyatha are index fossils for correlating rocks of similar ages globally, because of their abundance, extensive geographic distribution, their detailed anatomy and well established taxonomy. Their ecological significance remains incompletely explored yet they are known to strongly competitively interact unlike modern sponges. This study examines the feeding ecology of the fossil remains of Siberian archaeocyath assemblages. As suspension feeders, archaeocyaths filtered plankton from the water column through pores in their outer wall. Here we outline a new method to estimate the limit on the upper size of plankton that could be consumed by an archaeocyath during life. The archaeocyaths examined were predominantly feeding on nanoplankton and microplankton such as phytoplankton and protozooplankton. Size-frequency distributions of pore sizes from six different Siberian archaeocyath assemblages, ranging from Tommotian to Botoman in age, reveal significantly different upper limits to the prey consumed at each locality. Some of the assemblages contain specimens that could have fed on larger organisms extending in to the mesoplankton including micro-invertebrates as a possible food resource. These results show that during the establishment of the first animal reef systems, prey partitioning was established as a way of reducing competition. This method has applicability for understanding the construction and the functioning of the first reef systems, as well as helping to understanding modern reef systems and their development though time and space.

Data table SI Archaeo ecology Antcliffe et alAdditional data on Achaeocyatha pore sizes