Large benthic foraminifera (LBF) are important components of tropical shallow-marine
ecosystems, in which they are abundant on both coral reefs and in the inter-reef areas …

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 …

The SE Asian carbonate record allows insight into the poorly known response of equatorial
marine systems to regional and global change during the Cenozoic. There is a marked …

The central part of the Indo-West Pacific (IWP) harbours the highest marine biodiversity, but
only few data of its origin are available. In this paper the Cenozoic records of large benthic …

Fault-associated dolomitized carbonates are proven hydrocarbon reservoirs in the
subsurface; yet their origins and spatial variability in reservoir quality are poorly understood …

Most studies of Cenozoic shallow-water, mixed carbonate–siliciclastic depositional systems
have focused on their sedimentology. To date, however, comprehensive analyses of biotas …

We discuss the ages of twelve (clusters of) localities along the northeastern margin of the
Kutai Basin (East Kalimantan, Indonesia). These localities form the basis for a large-scale …

Only three species of alveolinoidean larger foraminifera occur in present-day tropical
shallow-water marine settings. Alveolinella quoyi thrives in the Central Indo-Pacific and …

The larger benthic foraminiferal family Lepidocyclinidae has been described extensively in
the literature, with occurrences ranging from the middle Eocene in the Americas to the late …

To provide a comprehensive palaeoenvironmental reconstruction based on larger benthic
foraminifera (LBF), a quantitative analysis of their assemblage composition is needed …