| Full text | |
| Author(s): |
de Almeida, Renato Paes
;
Althaus, Camila Eliza
;
Janikian, Liliane
;
Gomes, Pedro Victor Oliveira
;
Figueiredo, Felipe Torres
;
Sawakuchi, Andre Oliveira
;
Freitas, Bernardo Tavares
;
da Silva, Leonardo Henrique Gomes
Total Authors: 8
|
| Document type: | Journal article |
| Source: | CRETACEOUS RESEARCH; v. 163, p. 12-pg., 2024-07-15. |
| Abstract | |
Cretaceous and possibly Paleogene strata, originally defined as the Alter do Chao Formation, are extensively exposed in the Amazonas Basin. While theoretical considerations suggest that the eastern Amazon has been draining into the Atlantic since pre-Miocene times, the limited published field data indicate a significant continental-scale reversal of drainage, transitioning from westward flow during the Cretaceous to the current eastward regional flow. This hypothesis has a significant impact on accepted paleogeographic reconstructions and has implications for the origin of the Amazon River and the associated biotic environments. Nevertheless, the observational database to support that hypothesis is still very scarce. To address this problem, the present study presents data from a basin-transverse profile where the entire stratigraphic succession of Cretaceous and Paleogene ages in the Amazonas Basin is exposed, namely the Jazida da Fazendinha and Alter do Chao formations. Facies analysis of cliff outcrops along the Tapajos River margins, including the type area of the units, reveals associations interpreted as fluvial deposits dominated by sandy bars. Paleocurrents were interpreted from more than 2000 individual measurements of fluvial cross-strata from various stratigraphic levels. The findings indicate that the regional flow direction during the deposition of both units was eastward across the entire basin transect. Integrating our dataset into the existing data on provenance reveals that, unlike the modern Andean-derived system, the primary sources for the Alter do Chao Formation were limited to the Amazon Craton. Our findings offer compelling empirical evidence to support the scenario proposed by previous numerical models. The findings also suggest that the rock record does not support the poorly documented and highly influential model of a significant westward-flowing river in Amazonia during the Cretaceous and the Paleogene. (c) 2024 Published by Elsevier Ltd. (AU) | |
| FAPESP's process: | 21/02994-0 - Survey and integration of outcrop, core and well data for the interpretation of paleogeography, stratigraphy and sedimentary sources of Cretaceous-Cenozoic section from Amazon Basin. |
| Grantee: | Camila Eliza Althaus |
| Support Opportunities: | Scholarships in Brazil - Doctorate |
| FAPESP's process: | 18/23899-2 - Trans-Amazon Drilling Project: origin and evolution of the forests, climate, and hydrology of the South American tropics |
| Grantee: | André Oliveira Sawakuchi |
| Support Opportunities: | Research Program on Global Climate Change - Thematic Grants |
| FAPESP's process: | 16/19736-5 - Quantitative approaches for big river deposits: integrated field geology and 3D photogrammetric models |
| Grantee: | Bernardo Tavares Freitas |
| Support Opportunities: | Regular Research Grants |