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Prey fractionation in the Archaeocyatha and its implication for the ecology of the first animal reef systems

Published online by Cambridge University Press:  18 October 2019

Jonathan B. Antcliffe Open the ORCID record for Jonathan B. Antcliffe [Opens in a new window] ,
William Jessop  and
Allison C. Daley
Jonathan B. Antcliffe
Affiliation:
Oxford University Department of Zoology, South Parks Road, Oxford, U.K.; and Université de Lausanne, Institut des Sciences de la Terre, Bâtiment Géopolis, UNIL–Mouline, CH-1015 Lausanne, Switzerland. E-mail: [email protected], [email protected]
William Jessop
Affiliation:
Oxford University Department of Zoology, South Parks Road, Oxford, U.K. E-mail: [email protected]
Allison C. Daley
Affiliation:
Oxford University Department of Zoology, South Parks Road, Oxford, U.K.; and Université de Lausanne, Institut des Sciences de la Terre, Bâtiment Géopolis, UNIL–Mouline, CH-1015 Lausanne, Switzerland. E-mail: [email protected], [email protected]
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Abstract

Archaeocyaths are the most abundant sponges from the Cambrian period, having formed the first animal reef communities more than 500 million years ago. The Archaeocyatha are index fossils for correlating rocks of similar ages globally because of their abundance, extensive geographic distribution, detailed anatomy, and well-established taxonomy. Their ecological significance remains incompletely explored, yet they are known to have strongly competitively interacted, 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 into 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 understand modern reef systems and their development though time and space.

Type
Articles
Information
Paleobiology , Volume 45 , Issue 4 , September 2019 , pp. 652 - 675
Copyright
Copyright © The Paleontological Society. All rights reserved 2019 

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Footnotes

Data available from the Dryad Digital Repository:https://doi.org/10.5061/dryad.0r17c1m

References

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