Foraminifera and coccolithophorid assemblage changes in the Panama Basin during the last deglaciation: Response to sea-surface productivity induced by a transient climate change
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Martínez I, Rincon D, Yokoyama Y & Barrows T
Eds: Martinez I, Spero HJ & Berrio JC
Palaeogeography, Palaeoclimatology, Palaeoecology, vol. 234(1), 114-126, 2006https://doi.org/10.1016/j.palaeo.2005.10.022
This article is in the special issue "Late Quaternary Climates of Tropical America and Adjacent Seas"; a publication of PAGES PEP I (Pole-Equator-Pole transect through the Americas), a former Working Group. The aim was to integrate the research findings of climatologists and marine and continental paleoscientists studying paleoclimatic changes in and around tropical South America.