The Great Lakes of East Africa are collectively the earth's most remarkable and species-rich
freshwater feature. Intrinsic biological factors and extrinsic ecological opportunities allowed …

Abstract Barremian–Aptian (Lower Cretaceous) Pre-Salt lacustrine carbonates host large
petroleum reservoirs in South Atlantic rift basins, yet remain poorly studied, in part due to the …

The 'wet'early to mid-Holocene of tropical Africa, with its enhanced monsoon, ended with an
abrupt shift toward drier conditions and was ultimately replaced by a drier climate that has …

Abstract The Piceance Creek basin formed as a continental foreland basin ca 53 to 48 Ma in
the early to middle Eocene. On a global basis, the basin contains one of the richest oil shale …

Abstract The Itapema Formation in the Santos Basin is described as a carbonate coquina
interval, a type of sedimentary rock composed mainly by shells and their fragments. These …

In light of a modern understanding of early Eocene greenhouse climate fluctuations and new
highly seasonal fluvial system faces models, the role of climate in the evolution of one …

Abstract In the Early to Middle Miocene, the post‐orogenic intramontane lacustrine Sinj
Basin that belonged to the Dinarides Lake System evolved in the area of the External …

Abstract The Yacoraite Formation (Cretaceous–Paleogene) is a mixed carbonate–
siliciclastic microbialite-bearing lacustrine succession deposited in the intra-continental …

Fine-grained sedimentary rocks are well developed in a salinized lacustrine basin in the
Junggar Basin, China. Understanding the sedimentary characteristics and process of these …

Lacustrine carbonates of the Eocene Green River Formation crop out on the western margin
of the Piceance Basin and the eastern margin of the Uinta Basin, in western Colorado. This …