Evolution of Precambrian life in the Brazilian geological record


Autoria(s): Fairchild, Thomas Rich; Sanchez, Evelyn A. M.; Pacheco, Mirian Liza A. F.; Leme, Juliana de Moraes
Contribuinte(s)

UNIVERSIDADE DE SÃO PAULO

Data(s)

01/11/2013

01/11/2013

2012

Resumo

Precambrian rocks comprise nearly one-quarter of the surface of Brazil and range from Paleoarchean (ca. 3.6 Ga) to the latest Ediacaran (0.542 Ga) in age. Except for controversial phosphatized 'embryo-like' microfossils like those from the lower Ediacaran Doushantuo Formation, China and complex rangeomorphs, Brazilian research has revealed all major categories of Precambrian life forms described elsewhere - microbialites, biomarkers, silicified microfossils, palynomorphs, vase-shaped microfossils, macroalgae, metazoans, vendobionts and ichnofossils - but the paleobiological significance of this record has been little explored. At least four occurrences of these fossils offer promise for increased understanding of the following aspects of Precambrian biospheric evolution: (i) the relationship of microbialites in 2.1-2.4 Ga old carbonates of the Minas Supergroup in the Quadrilatero Ferrifero, Minas Gerais (the oldest Brazilian fossils) to the development of the early oxygenic atmosphere and penecontemporaneous global tectonic and climatic events; (ii) the evolutionary and biostratigraphic significance of Mesoproterozoic to Ediacaran organic-walled microfossils in central-western Brazil; (iii) diversity and paleoecological significance of vase-shaped heterotrophic protistan microfossils in the Urucum Formation (Jacadigo Group) and possibly the Bocaina Formation (Corumba Group), of Mato Grosso do Sul; and (iv) insights into the record of skeletogenesis and paleoecology of latest Ediacaran metazoans as represented by the abundant organic carapaces of Corumbella and calcareous shells of the index fossil Cloudina, of the Corumba Group, Mato Grosso do Sul. Analysis of the Brazilian Precambrian fossil record thus holds great potential for augmenting paleobiological knowledge of this crucial period on Earth and for developing more robust hypotheses regarding possible origins and evolutionary pathways of biospheres on other planets. Received 26 February 2012, accepted 17 May 2012, first published online 18 June 2012

Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)

Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)

Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)

Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)

Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)

Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)

Identificador

INTERNATIONAL JOURNAL OF ASTROBIOLOGY, NEW YORK, v. 11, n. 4, Special Issue, supl. 1, Part 2, pp. 309-323, OCT, 2012

1473-5504

http://www.producao.usp.br/handle/BDPI/37598

10.1017/S1473550412000183

http://dx.doi.org/10.1017/S1473550412000183

Idioma(s)

eng

Publicador

CAMBRIDGE UNIV PRESS

NEW YORK

Relação

INTERNATIONAL JOURNAL OF ASTROBIOLOGY

Direitos

closedAccess

Copyright CAMBRIDGE UNIV PRESS

Palavras-Chave #PRECAMBRIAN #EVOLUTION #FOSSIL RECORD #BRAZIL #ASTROBIOLOGY #PALEOPROTEROZOIC SNOWBALL EARTH #PROTEROZOIC OCEAN CHEMISTRY #ARCHEAN MOLECULAR FOSSILS #VASE-SHAPED MICROFOSSILS #GRAND-CANYON #CHUAR GROUP #CARBONATE PLATFORM #SHELLY FOSSILS #SOUTH CHINA #NEOPROTEROZOIC GLACIATIONS #ASTRONOMY & ASTROPHYSICS #BIOLOGY #GEOSCIENCES, MULTIDISCIPLINARY
Tipo

article

original article

publishedVersion