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 - Relations - Dynamics of sediment flux to a bathyal continental margin section through the Paleocene–Eocene Thermal Maximum

CP - Relations - Palaeo-environmental evolution of Central Asia during the Cenozoic: new insights from the continental sedimentary archive of the Valley of Lakes (Mongolia)

Figure 1 from Decadal resolution record of Oman upwelling indicates solar forcing of the Indian summer monsoon (9-6 ka)

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

Decadal-resolution record of winter monsoon intensity over the last two millennia from planktic foraminiferal assemblages in the northeastern Arabian Sea - Philipp M Munz, Michael Siccha, Andreas Lückge, Anna Böll, Michal Kucera

2965 PDFs Review articles in OXYGEN MINIMUM ZONES

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

Decadal-resolution record of winter monsoon intensity over the last two millennia from planktic foraminiferal assemblages in the northeastern Arabian Sea - Philipp M Munz, Michael Siccha, Andreas Lückge, Anna Böll, Michal Kucera

Late Cenozoic cooling restructured global marine plankton communities

2965 PDFs Review articles in OXYGEN MINIMUM ZONES

Geographical differences in seasonality of CZCS-derived phytoplankton pigment in the Arabian Sea for 1978–1986 - ScienceDirect