1. Dawn of diverse shelled and carbonaceous animal microfossils at ~ 571 Ma.
- Author
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Morais L, Freitas BT, Fairchild TR, Clavijo Arcos RE, Guillong M, Vance D, de Campos MDR, Babinski M, Pereira LG, Leme JM, Boggiani PC, Osés GL, Rudnitzki ID, Galante D, Rodrigues F, and Trindade RIF
- Subjects
- Animals, Brazil, Animal Shells anatomy & histology, Animal Shells chemistry, Biological Evolution, Paleontology methods, Fossils
- Abstract
The Ediacaran-Cambrian transition documents a critical stage in the diversification of animals. The global fossil record documents the appearance of cloudinomorphs and other shelled tubular organisms followed by non-biomineralized small carbonaceous fossils and by the highly diversified small shelly fossils between ~ 550 and 530 Ma. Here, we report diverse microfossils in thin sections and hand samples from the Ediacaran Bocaina Formation, Brazil, separated into five descriptive categories: elongate solid structures (ES); elongate filled structures (EF); two types of equidimensional structures (EQ 1 and 2) and elongate hollow structures with coiled ends (CE). These specimens, interpreted as diversified candidate metazoans, predate the latest Ediacaran biomineralized index macrofossils of the Cloudina-Corumbella-Namacalathus biozone in the overlying Tamengo Formation. Our new carbonate U-Pb ages for the Bocaina Formation, position this novel fossil record at 571 ± 9 Ma (weighted mean age). Thus, our data point to diversification of metazoans, including biomineralized specimens reminiscent of sections of cloudinids, protoconodonts, anabaritids, and hyolithids, in addition to organo-phosphatic surficial coverings of animals, demonstrably earlier than the record of the earliest known skeletonized metazoan fossils., (© 2024. The Author(s).)
- Published
- 2024
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