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Isotope stratigraphy of Neoproterozoic cap carbonates in the Araras Group, Brazil |
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| Authors: | Carlos JS de Alvarenga Marcel A Dardenne Roberto V Santos Emanuele R Brod Simone MCL Gioia Alcides N Sial Elton L Dantas Valderez P Ferreira |
| Institution: | aInstituto de Geociências, Universidade de Brasília, Campus Universitário, Asa Norte, CEP: 70910-900, Brasília, DF, Brazil bDepartamento de Geologia, Universidade Federal de Pernambuco, Caixa Postal: 7852, CEP: 50732-970, Recife, PE, Brazil |
| Abstract: | The Neoproterozoic carbonate sequence on the southeastern border of the Amazon Craton is divided into three lithostratigraphic units: a basal cap dolomite, an intermediate limestone, limestone-mudstone unit, and an upper dolarenite-dolorudite unit. Sections of the cap-carbonate were measured from the inner shelf to the outer shelf. Carbon isotope ratios (relative to PDB) vary between ? 10.5 and ? 1.7‰ in cap dolomite, and between ? 5.4 and + 0.1‰ in laminated limestone and mud-limestone. Limestones and mud-limestones exhibit 87Sr/86Sr ratios ranging from 0.70740 to 0.70780. A comparative isotope stratigraphy between the inner-shelf and the middle-shelf basin shows differences in carbon isotope ratios: The cap dolomite and limestones have lower δ13C ratios on the border of the basin (inner shelf) than in the middle shelf of the basin. These lower values can be related to shallower environmental conditions and to a stronger influence of the continental border. The 87Sr/86Sr ratios are the same in both areas, and are consistent with seawater composition at around 600 Ma. |
| Keywords: | Neoproterozoic Chemostratigraphy Carbonate platform Araras group Glaciation |
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