In situ filamentous communities from the Ediacaran (approx. 563 Ma) of Brazil

Author:

Becker-Kerber Bruno12ORCID,de Barros Gabriel Eduardo Baréa3ORCID,Paim Paulo Sergio Gomes4ORCID,Prado Gustavo M. E. M.5ORCID,da Rosa Ana Lucia Zucatti6,El Albani Abderrazak2ORCID,Laflamme Marc7ORCID

Affiliation:

1. Programa de Pós-Graduação em Ecologia e Recursos Naturais, Universidade Federal de São Carlos, Washington Luiz, 325 km, São Carlos (SP) 13565-905, Brazil

2. Unité Mixte de Recherche (UMR), Centre National de la Recherche Scientifique (CNRS), IC2MP 7285, University of Poitiers, 86073 Poitiers, France

3. Programa de Pós-Graduação em Biologia Comparada, Departamento de Biologia, Faculdade de Filosofia, Ciências e Letras de Ribeirão Preto (FFCLRP), Universidade de São Paulo (USP), Avenue Bandeirantes, 3900-Vila Monte Alegre, 14049-900, Ribeirão Preto, São Paulo, Brazil

4. Programa de Pós-Graduação em Geologia, Universidade do Vale do Rio dos Sinos, 93.022-750, São Leopoldo (RS), Brazil

5. Programa de Pós Graduação em Geoquímica e Geotectônica, Instituto de Geociências, Universidade de São Paulo (USP), Avenue Bandeirantes, 3900-Vila Monte Alegre, 14049-900, Ribeirão Preto, São Paulo, Brazil

6. Petrobras, Santos (SP), Brazil

7. Department of Chemical and Physical Sciences, University of Toronto Mississauga, 3359 Mississauga Road, Mississauga, Ontario, Canada L5 L 1C6

Abstract

Precambrian filamentous microfossils are common and diverse. Nevertheless, their taxonomic assignment can be difficult owing to their overall simple shapes typically lacking in diagnostic features. Here, we report in situ communities of well-preserved, large filamentous impressions from the Ediacaran Itajaí Basin ( ca 563 Ma) of Brazil. The filaments are uniserial (unbranched) and can reach up to 200 µm in width and up to 44 mm in length. They occur as both densely packed or sparsely populated surfaces, and typically show a consistent orientation. Although simple in shape, their preferred orientation suggests they were tethered to the seafloor, and their overall flexibility (e.g. bent, folded and twisted) supports a biological (rather than sedimentary) affinity. Biometric comparisons with modern filamentous groups further support their biological affinity, suggesting links with either large sulfide-oxidizing bacteria (SOB) or eukaryotes. Other morphological and palaeoecological characteristics further corroborates their similarities with modern large filamentous SOB. Their widespread occurrence and association with complex Ediacaran macrobiota (e.g. frondose organisms, Palaeopascichnus ) suggest that they probably played an important role in the ecological dynamics of these early benthic communities by providing firm substrates for metazoans to inhabit. It is further hypothesized that the dynamic redox condition in the latest Ediacaran, with the non-continuous rise in oxygen concentration and periods of hypoxia, may have created ideal conditions for SOB to thrive.

Funder

Fundação de Amparo à Pesquisa do Estado de São Paulo

Publisher

The Royal Society

Subject

General Agricultural and Biological Sciences,General Environmental Science,General Immunology and Microbiology,General Biochemistry, Genetics and Molecular Biology,General Medicine

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