CP - Biotic response of plankton communities to Middle to Late Miocene monsoon wind and nutrient flux changes in the Oman margin upwelling zone
Por um escritor misterioso
Last updated 31 março 2025

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

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

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

Phytoplankton community changes in a coastal upwelling system during the last century - ScienceDirect

Microbial biogeochemistry of coastal upwelling regimes in a changing ocean

The PhanSST global database of Phanerozoic sea surface temperature proxy data

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

2965 PDFs Review articles in OXYGEN MINIMUM ZONES

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The PhanSST global database of Phanerozoic sea surface temperature proxy data

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

2965 PDFs Review articles in OXYGEN MINIMUM ZONES
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