We aimed to understand how phytoplankton are transported to the bathypelagic zone of the Sea of Japan. We collected sinking particles by sediment traps moored at 387 m and 890 m depths and phytoplankt
Collection of smear slide microscopy images from the above given hole of International Ocean Discovery Program (IODP) Expedition 386 (Japan Trench Paleoseismology). The offshore phase of this expediti
Presence of FTIR spectra of clinopyroxenes, orthopyroxenes and garnets of French Massif Central (France) and Adamawa Volcanic Plateau (Cameroon) pyroxenites. In the table, there is the integral absorp