The middle Cretaceous was a period characterized by elevated sea-floor spreading rates,
enhanced volcanism, high atmospheric CO 2 levels, warming temperatures, and the peak …

Major carbon cycle disturbances reflected by carbon isotope excursions (CIE) have been
reported in the Jurassic successions of Euro-Boreal and Mediterranean basins. However …

In the Western Alps, the Penninic Frontal Thrust (PFT) is the main crustal-scale tectonic
structure of the belt. This thrust transported the high-pressure metamorphosed internal units …

Sedimentary gaps are a major obstacle in the reconstruction of a carbonate platform's
history. In order to improve the understanding of the early diagenesis and the succession of …

Little is known about the impact of the mid-Cretaceous Oceanic Anoxic Events (OAEs) on the
neritic carbonate systems in South America. In order to fill this knowledge gap, the present …

An integrated lithofacies and mineralogical assemblage was used to describe a depositional
model and sequence stratigraphic framework of the Maastrichtian–Danian succession in the …

Quantitative palynological, sedimentological, and geophysical data analyses of the
Cretaceous Abu Tunis 1X well from the Matruh Basin, northwestern Egypt indicate …

Abstract The Upper Cretaceous of central India is represented by a thin transgressive-
regressive succession of tropical marine sediments deposited on a Precambrian basement …

The present paper reports on the sedimentological and geochemical record of Albian–
Turonian neritic carbonates from the eastern subequatorial Pacific domain in Peru. The …

The sedimentary record of fossil coastal lagoons is an under-explored archive of
environmental change in ancient coastal domains. The significant continentality of coastal …