Abstract
Complex animals first evolved during the Ediacaran period, between 635 and 542 million years ago, when the oceans were just becoming fully oxygenated. In situ fossils of the mobile forms of these animals are associated with microbial sedimentary structures1,2,3, and the animal’s trace fossils generally were formed parallel to the surface of the seabed, at or below the sediment–water interface4,5. This evidence suggests the earliest mobile animals inhabited settings with high microbial populations, and may have mined microbially bound sediments for food resources6,7,8. Here we report the association of mobile animals—insect larvae, oligochaetes and burrowing shore crabs—with microbial mats in a modern hypersaline lagoon in Venezuela. The lagoon is characterized by low concentrations of dissolved O2 and pervasive biomats dominated by oxygen-producing cyanobacteria, both analogous to conditions during the Ediacaran. We find that, during the day, O2 levels in the biomats are four times higher than in the overlying water column. We therefore conclude that the animals harvest both food and O2 from the biomats. In doing so, the animals produce horizontal burrows similar to those found in Ediacaran-aged rocks. We suggest that early mobile animals may have evolved in similar environments during the Ediacaran, effectively exploiting oases rich in O2 that formed within low oxygen settings.
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Acknowledgements
S. G. Pemberton, N. Butterfield and S. Jensen are thanked for their technical input and evaluation. M.G. and K.O.K. thank the Natural Sciences and Engineering Research Council of Canada for ongoing support.
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M.G. and K.O.K. conceived the study and led field operations: S.V.L., E.P. and D.P. executed different aspects of the data gathering and data analysis: J.W.H. and A.S. provided ancient rock-record examples. All of the authors contributed to the writing of the final manuscript.
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Gingras, M., Hagadorn, J., Seilacher, A. et al. Possible evolution of mobile animals in association with microbial mats. Nature Geosci 4, 372–375 (2011). https://doi.org/10.1038/ngeo1142
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DOI: https://doi.org/10.1038/ngeo1142
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