Planktonic Foraminifera have a uniquely complete fossil record that enables high resolution analyses of how they reacted to past environmental change. 125,000 BP the Mediterranean Sea experienced a sharp change in ocean circulation, providing an excellent

Modern observations of planktic foraminifera from sediment trap studies help to constrain the regional ecology of paleoceanographically valuable species. Results from a weekly-resolved sediment trap time series (2008–2014) in the northern Gulf of Mexico

Despite the pivotal role of the fossil record of planktonic foraminifera in revealing past climates and studying plankton evolution, the origin of the group remains elusive. Conflicting evidence exists between paleontological and molecular studies on

The isolating effect of water mass partitioning of populations on the morphology, stratigraphic distribution and extinction of planktonic foraminifera is assessed from the Pliocene–Quaternary record of Globorotalia puncticulata. Southern Hemisphere,