Comparison of lacustrine successions and their palaeohydrological implications in two sub‐basins of the Triassic Cuyana rift, Argentina

Abstract

Continental carbonates are rich in palaeoclimatic, palaeoenvironmental and palaeontological information. While carbonate accumulation mechanisms have been described for many types of continental environments, especially in extensional basins, there are still uncertainties that existing facies models fail to address. The Triassic Cerro de las Cabras and Cerro Puntudo formations are alluvial-fluvial-lacustrine sequences that represent a part of the sedimentary infill of two sub-basins of the Cuyana Basin during the early stages of the Triassic rift in west-central Argentina. Previous work has provided absolute dates, confirming that these deposits are coeval (Anisian) allowing a comparative study of carbonate sedimentation in an extensional tectonic context. The description and origin of freshwater carbonate deposits and their surrounding siliciclastic sediments in specific areas of the Cuyana rift, gives insight into the major factors that control carbonate precipitation in all rift basins, including the characterization of the palaeohydrology and the importance of provenance. The Cerro de las Cabras Formation represents an ephemeral, playa-lake depositional system with subaerial exposure and pedogenesis. Its aggradational succession corresponds to the evaporative facies association lake type, diagnostic of underfilled lake basins where persistently closed surface hydrology can lead to thick evaporites. However, this formation lacks thick evaporites and has microbialitic limestones, pointing to an open groundwater supply. The Cerro Puntudo Formation represents an alkaline playa-lake system fed by groundwater and ephemeral surface-water input. The unit is an aggradational-minor progradational succession, pointing to a fluctuating profundal facies association, suggesting a balanced-filled lake type. These two synchronous, lacustrine depositional systems were influenced by tectonics and climate. Provenance and hydrology are key controls in carbonate accumulation in continental rift basins that must be included in future facies models for continental carbonates. Comparison with other rift basins suggests that application of lake-type characterizations coupled with palaeohydrology and provenance patterns will aid in developing new sedimentation models for freshwater limestones in extensional settings.

Depositional processes and sedimentation pattern in an intermontane basin: Insights from the Imphal Basin, Indo‐Myanmar Range, NE India

“…Deposited through suspension fallout in relatively shallow stagnant waterbodies, and subsequently altered by pedogenic activities (Benavente et al, 2015;Reineck & Singh, 1980). Peat (P) 1 -1.8 m thick, laterally persistent, deposits of dark greyish to deep brownish peat, containing traces of roots, rootlets, rhizomes, tiny stems, and leaves ( Figure 5d).…”

“…Deposited through suspension fallout in relatively shallow stagnant waterbodies, and subsequently altered by pedogenic activities (Benavente et al, 2015;Reineck & Singh, 1980).…”

“…Deposited through suspension in deeper waters under reducing conditions (Chakraborty & Sarkar, 2005; Reineck & Singh, 1980; Shukla, Bora, & Singh, 2010). (Continues)the Mc facies deposited in deeper parts of the lake under anaerobic conditions, whereas the silty mud of the Mn facies deposited in mudflats from suspension fall out and later altered by pedogenesis(Benavente, Mancuso, Cabaleri, & Gierlowski-Kordesch, 2015). The peat (P) formed in swamps wherein occasional floodwaters deposited mud and silt through suspension settle out.…”

Increasing the fish diversity of the Triassic faunas of Gondwana: a new redfieldiiform (Actinopterygii) from the Middle Triassic of Argentina and its palaeobiogeographical implications

“…This interpretation agrees with the tectonic and climatic setting described for the Triassic Cuyo rift Basin (Benavente et al . , and references therein).…”

“…Benavente et al . () described in detail the middle part of the Cerro de Las Cabras Formation at its type locality, composed mainly of carbonates associated with volcaniclastic deposits. They interpreted that section of the unit as being a freshwater carbonate shallow palustrine–lacustrine depositional systems fed mainly by an open groundwater supply, as confirmed by geochemical data (Benavente ).…”