Alternations of open and closed lakes in the Lower Aptian Codó Formation (Parnaíba Basin, Brazil)

• Published in: Sedimentary geology Vol. 455; p. 106478
• Main Authors: Bobco, Fabia Emanuela Rafaloski, Trombetta, Mariane Cristina, Ferreira, Laís de Oliveira, Silveira, Luís Fernando, Kroth, Mateus, Mendonça, Joalice de Oliveira, Mendonça Filho, João Graciano, Sedorko, Daniel, Araujo, Bruno César, Borghi, Leonardo
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01-09-2023
• Subjects: Evaporites; Geochemistry; Lacustrine carbonates; Palynofacies; Evaporites; Geochemistry; Lacustrine carbonates; Palynofacies
• ISSN: 0037-0738; 1879-0968
• DOI: 10.1016/j.sedgeo.2023.106478

Lakes can be classified as open, semi-closed, and closed based on the balance between accommodation space and sediment–water fill. Different lake types can coexist in adjacent basins and rapidly change throughout time from one type to another. Understanding the processes that result from shifts in a lake's hydrological properties can be challenging, as well as characterizing its sedimentary products. The Aptian Codó Formation, in the Parnaíba Basin, north–northeast Brazil, contains in its record a complex facies succession deposited in a continental lacustrine system. In order to better understand the depositional aspects of different lake types, we characterized the lower portion of the Codó Formation using a multi-proxy approach. We combined litho- and microfacies analysis, ichnology, bulk chemical data, mineralogy, isotopic geochemistry, and organic matter analysis in the recently drilled, fully recovered borehole, 2-CO-1-MA. We defined eight lithofacies: bioturbated siltstones, dark gray mudstones, laminites, stratiform and domal stromatolites, heterolites rich in ostracods and organic muddy, and anhydrite and gypsum rocks. The isotopic data and the palynofacies analysis pointed out the existence of restricted conditions (TOC up to 19.6 wt%) with intermittent connections with seawater. Integrating all techniques, we interpreted five depositional stages: expanded lake, brackish ephemeral lake, perennial shallow lake, evaporitic sabkha, and stratified lake. These stages were influenced by the relation between inflow and evaporation rate, which were the main controls on sedimentation in the lacustrine-sabkha system studied. Our findings provide a detailed description and interpretation of the paleoenvironmental conditions related to the alternation from open to closed lakes, combining sedimentological, geochemical, and palynological characteristics of an inland lake system.