According to the prevailing view in literature, two Eocene carbonate platform belts
developed on northern and southern margins of the Tethys Ocean. However, Eocene …

Orthophragmines are a group of discoidal, lenticular or stellate 'orbitoidal'larger benthic
foraminifera that thrived in shallow-marine environments in low-to-middle latitudes during …

A study of the paleoenvironmental evolution of the middle Eocene platforms recognized in
the westernmost Tethys has been carried out in the well-exposed middle Eocene …

ABSTRACT Thirteen Paleocene-Eocene sections have been studied along the Prebetic
Domain (South Iberian Margin) in the Alicante, Murcia, Granada, and Jaen Sectors. The …

Eocene Nummulites banks play a significant role as potential hydrocarbon reservoirs.
However, the impact of biological accumulation and sedimentary and diagenetic alterations …

Timing of seawater retreat from the Tethyan Himalaya is of great importance, as it provides a
minimum age control on the initial India-Asia collision. In south Tibet, however, it is still in …

This paper analyses the lower to middle Eocene carbonate succession exposed at the
Island of Pag (Croatia), in the External Dinarides, providing its palaeoenvironmental …

Rotaliids are one of the groups of larger foraminifera that quickly recolonized the shallow-
water environments after the mass extinction at the end of the Cretaceous. Here we present …

Larger benthic foraminifera (LBF) experienced rapid evolution during the Paleogene,
reaching a widespread distribution in both northern and southern Tethys during the Eocene …

The forearc basin in Myanmar is significant in understanding the development of continental
forearc basins. We present stratigraphic, sandstone petrographic, and U-Pb detrital data …