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

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

CP - Recent

PDF) Decadal resolution record of Oman upwelling indicates solar forcing of the Indian summer monsoon (9–6 ka)

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

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

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

Jing Lyu (@hangyi_lyu) / X

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

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

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

Gerald Auer (@GeraldAuer) / X

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

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