Clastic sedimentary record impacted by carbonate bioclasts in the Late Ediacaran

Abstract Clastic sedimentary systems and their characteristics are assumed not to have been modified by carbonate bioclastic grains until the Phanerozoic. Here, we show that the presence of carbonate bioclasts produced by disintegrated biomineralizing metazoans modified fine-grained siliciclastic facies in the Late Ediacaran Tamengo Formation, Brazil, ca. 555–542 Ma. The analysis of both polished sections and thin sections shows that sand-sized carbonate bioclasts (< 2 mm) derived from the Ediacaran metazoan Corumbella created diverse sedimentary features later found in the Phanerozoic record, such as bioclastic-rich horizontal and low-angle cross-laminations, erosive pods and lenses, bioclastic syneresis cracks, ripples preserved by bioclastic caps, microbial lamination eroded and filled with bioclasts, and entrapped bioclasts within microbial mats. These sedimentary features would have hardly been recorded in fine siliciclastic facies without the sand-sized bioclasts. Based on these features, together with other sedimentary evidence, Corumbella depositional settings in the Tamengo Fm. are reinterpreted as mid-ramp, subtidal settings. The multi-component organization of the skeleton of Corumbella favoured disarticulation to yield a sand-sized bioclast, so in turn creating a new complexity to shallow marine clastic settings typical of Phanerozoic marine depositional systems.

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Publication Details

Journal
Geological Magazine
Published
2025-01-01
DOI
https://doi.org/10.1017/s0016756824000335
Citations
2
Primary Topic
Paleontology and Stratigraphy of Fossils
Type
article
Field-Weighted Citation Impact
8.66

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article

Clastic sedimentary record impacted by carbonate bioclasts in the Late Ediacaran

Gustavo Paula-Santos, Sérgio Caetano-Filho, Gabriel Ladeira Osés, Jhon Willy Lopes Afonso et al.
2 citations
Geological Magazine
Paleontology and Stratigraphy of Fossils
8.66
article

Clastic sedimentary record impacted by carbonate bioclasts in the Late Ediacaran

Gustavo Paula-Santos, Sérgio Caetano-Filho, Gabriel Ladeira Osés, Jhon Willy Lopes Afonso, Tiago Fiorini da Silva, C. L. Rodrigues, Rachel A. Wood, Kamilla Borges Amorim, Guilherme Raffaeli Romero, Mírian Liza Alves Forancelli Pacheco, Bernardo T. Freitas
article en
2 citations

Abstract

Abstract Clastic sedimentary systems and their characteristics are assumed not to have been modified by carbonate bioclastic grains until the Phanerozoic. Here, we show that the presence of carbonate bioclasts produced by disintegrated biomineralizing metazoans modified fine-grained siliciclastic facies in the Late Ediacaran Tamengo Formation, Brazil, ca. 555–542 Ma. The analysis of both polished sections and thin sections shows that sand-sized carbonate bioclasts (< 2 mm) derived from the Ediacaran metazoan Corumbella created diverse sedimentary features later found in the Phanerozoic record, such as bioclastic-rich horizontal and low-angle cross-laminations, erosive pods and lenses, bioclastic syneresis cracks, ripples preserved by bioclastic caps, microbial lamination eroded and filled with bioclasts, and entrapped bioclasts within microbial mats. These sedimentary features would have hardly been recorded in fine siliciclastic facies without the sand-sized bioclasts. Based on these features, together with other sedimentary evidence, Corumbella depositional settings in the Tamengo Fm. are reinterpreted as mid-ramp, subtidal settings. The multi-component organization of the skeleton of Corumbella favoured disarticulation to yield a sand-sized bioclast, so in turn creating a new complexity to shallow marine clastic settings typical of Phanerozoic marine depositional systems.

Geological MagazineVol. 162
Universidade Federal de São Carlos (BR), Universidade de São Paulo (BR), University of Bremen (DE), Universidade Estadual de Campinas (UNICAMP) (BR), Universidade Federal de Mato Grosso (BR), Valongo Observatory (BR), National Observatory (BR), Universidade Estadual Paulista (Unesp) (BR), University of Edinburgh (GB)
UK Research and Innovation, Fundação de Amparo à Pesquisa do Estado de São Paulo, Coordenação de Aperfeiçoamento de Pessoal de Nível Superior, Conselho Nacional de Desenvolvimento Científico e Tecnológico, Universidade de São Paulo, Centro Nacional de Pesquisa em Energia e Materiais, Natural Environment Research Council, Laboratório Nacional de Luz Síncrotron
Life below water
Openalex Percentile: Top 5%
Paleontology and Stratigraphy of Fossils
8.66
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