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Using detrital zircon and rutile to constrain sedimentary provenance of Early Paleozoic fluvial systems of the Araripe Basin, Western Gondwana

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Author(s):
Cerri, Rodrigo, I ; Warren, Lucas, V ; Spencer, Christopher J. ; Varejao, Filipe G. ; Promenzio, Paloma ; Luvizotto, George L. ; Assine, Mario L.
Total Authors: 7
Document type: Journal article
Source: Journal of South American Earth Sciences; v. 116, p. 17-pg., 2022-04-26.
Abstract

The Early Paleozoic of the NE Brazilian sedimentary basins are key to understanding the primeval depositional environments and paleogeography of Western Gondwana after its final assembly. In this context, determining the sedimentary provenance of the Early Paleozoic Cariri Formation (basal unit of the Araripe Basin) may improve paleogeographic reconstructions and stratigraphic correlations. Despite the Araripe Basin being one of the beststudied interior basins of northeastern Brazil, the Cariri Formation lacks detailed geochronological and sedimentary provenance analyses, which hamper precise definitions of its depositional age, sedimentary source areas and paleogeography. Considering this scenario, we performed a combined multiproxy approach, including sedimentologic and stratigraphic analysis, detrital zircon U-Pb dating and provenance studies based on trace elements in detrital rutile. The maximum depositional age for the Cariri Formation suggests that its sedimentation started after the Late Cambrian. Detrital zircon ages and detrital rutile provenance indicate that the primary source areas for the Cariri Formation fluvial system were the orogenic terranes related to the Brasiliano Orogeny, located at the SE of the Borborema Province (e.g., Sergipano Belt), with secondary, but also important, the contribution of Cambrian sources. Records of this event are also found in northern Africa, where units related to the Neoproterozoic East African-Antarctic and Pan African orogens provided sediments for basin-scale fluvial systems. (AU)

FAPESP's process: 14/00519-9 - Centralities of night-time leisure in the city of São Carlos-SP and the interface relations
Grantee:Tiago Ferreira Lopes Machado
Support Opportunities: Scholarships in Brazil - Scientific Initiation
FAPESP's process: 17/19550-1 - Jaibaras tectonossequence genesis (Ediacarano - Ordoviciano) and its inheritance in the sedimentation of Serra Grande sequence (Ordoviciano - Siluriano), Northeast edge of Parnaíba Basin
Grantee:Rodrigo Irineu Cerri
Support Opportunities: Scholarships in Brazil - Doctorate
FAPESP's process: 20/10739-7 - Geochronology and provenance of the Parnaíba, Araripe, Jatobá and Tucano Norte Basins lower successions: implications on the origin of Western Gondwana intracratonic basins
Grantee:Rodrigo Irineu Cerri
Support Opportunities: Scholarships in Brazil - Post-Doctoral