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Benthic foraminifera (BF) typically constitute around 50% of the eukaryotic biomass of seafloor environments and are excellent recorders of bottom water environmental and geochemical changes in the past. In the last 27.000 years, major climatic oscil
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::74e88b1fef32312ceca73a075b0e6af4
https://doi.org/10.5194/egusphere-egu23-2109
https://doi.org/10.5194/egusphere-egu23-2109
