The Cretaceous oceanic red bed (CORB) is a newly opened window on global oceanic and
climate changes during the Cretaceous greenhouse world. As a result of the International …

Different pathways can be proposed to explain the origin of the red pigmentation present in
many Phanerozoic limestones. We investigate three possible models:(1) telogenetic …

Seaward progradation of several kilometers has been documented mostly for leeward
margin low-angle carbonate slope systems with a dominant platform top sediment source …

The Carboniferous, particularly during the Serpukhovian and Bashkirian time, was a period
of scarce shallow-water calcimicrobial-microbialite reef growth. Organic frameworks …

The Rimicaris exoculata shrimp is considered as a primary consumer that dominates the
fauna of most Mid-Atlantic Ridge (MAR) hydrothermal ecosystems. These shrimps harbour …

Marine sediments featuring special colors have always played an important role in
disclosing regional or global environmental transitions and geological evolution. A deep …

Ironstones and iron-rich limestones regularly occur as components of time-specific intervals
of the Palaeozoic as well as in younger times (Brett et al., 2012--this issue). Silurian …

Integrated analyses of ferruginous laminated crusts and macro-oncoids associated with
Middle Jurassic (Bathonian-Callovian) hardgrounds and condensed horizons crop** out …

This paper provides a synthetic sedimentological overview of the middle Frasnian carbonate
platform of Belgium and associated carbonate mounds. Carbonate mounds started usually …

A petrographic and biosedimentological study of the Rosso Ammonitico Veronese from the
Trento Plateau (north-eastern Italy) shows that diagenetic (neomorphism, recrystallization) …