Paleontological reconstructions of plankton community structure during warm periods of the
Cenozoic (last 66 million years) reveal that deep-dwelling 'twilight zone'(200–1000 m) …

Pelagic barite (BaSO 4) and related proxies are useful tools for reconstructing the marine
carbon cycle. The factors controlling pelagic barite dissolution in the ocean water column …

The marine biological carbon pump, which exports organic carbon out of the surface ocean,
plays an essential role in sequestering carbon from the atmosphere, thus impacting climate …

Carbonate‐forming organisms play an integral role in the marine inorganic carbon cycle, yet
the links between carbonate production and the environment are insufficiently understood …

Abstract At the Gebel Kilabiya area, studies on foraminifera and isotopes were conducted
during the Paleocene. The data revealed that the lowest part of the P2 Zone and the oldest …

This study aimed to characterize the spatial distribution and composition of living Benthic
Foraminifera (BF) and to comprehend how environmental conditions (eg, organic matter) …

Abstract The Paleocene‐Eocene Thermal Maximum (PETM,∼ 56 Ma) presents a past
analog for future global warming. Previous studies provided evidence for major loss of …

Long-term climatic trends of the Paleogene were interrupted by global perturbations of the
carbon cycle, commonly associated with warming of surface and bottom waters and …

Paleontological reconstructions of plankton community structure during warm periods of the
Cenozoic (last 66 million years) reveal that deep-dwelling twilight zone (200-1000 m) …

Marine barite is commonly used as a proxy to reconstruct past ocean productivity. Its
distribution in the water column mirrors organic carbon fluxes since it precipitates within …