CP - Biotic response of plankton communities to Middle to Late Miocene monsoon wind and nutrient flux changes in the Oman margin upwelling zone

Abstract. Understanding past dynamics of upwelling cells is an important aspect of assessing potential upwelling changes in future climate change scenarios. Our present understanding of nutrient fluxes throughout the world

CP - Biotic response of plankton communities to Middle to Late Miocene monsoon wind and nutrient flux changes in the Oman margin upwelling zone

CP - Relations - Warming, euxinia and sea level rise during the Paleocene–Eocene Thermal Maximum on the Gulf Coastal Plain: implications for ocean oxygenation and nutrient cycling

PDF) Biotic response of plankton communities to Middle to Late Miocene monsoon wind and nutrient flux changes in the Oman margin upwelling zone

The PhanSST global database of Phanerozoic sea surface temperature proxy data

The Marine Inorganic Carbon Cycle

PDF) Biotic response of plankton communities to Middle to Late Miocene monsoon wind and nutrient flux changes in the Oman margin upwelling zone

Montague-Judd, Danielle Dawn. 1999. Paleo-upwelling and the

CP - Relations - Global mean surface temperature and climate sensitivity of the early Eocene Climatic Optimum (EECO), Paleocene–Eocene Thermal Maximum (PETM), and latest Paleocene

Frontiers Trophic ecology of midwater zooplankton along a productivity gradient in the Southeast Pacific

JournalTOCs

Frontiers Influences of Extreme Upwelling on a Coastal Retention Zone

PDF) Late Miocene climate cooling and intensification of southeast Asian winter monsoon