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Two distinct Pleistocene assemblages from SE SantiagoIsland are comparable to modern analogues elsewhere inthe Cape Verde Islands. A low-diversity Siderastrea radiansassemblage lived atop basalt knobs surrounded by sand on aslope below a cliff. A Millepora alcicornis–Megabalanusazoricus assemblage occupied the cliff. The latter was atypical rocky-shore assemblage from a high-energy settingbelowthe tidal zone.Bioerosion structures in basalt producedby Circolites kotoncensis and Gastrochaenolites isp. alsooccur there. Despite extensive studies on local limestonedeposits in 1832 and 1836, lack of exposure preventedDarwin from seeing these fossils.Funding for fieldwork on Santiago Island in June 2011 was provided under grant CGL2010-15372-BTE from the Spanish Ministry of Science and Innovation to project leader Eduardo Mayoral (University of Huelva). Financial support to A. Santos came from the Spanish Ministry of Science and Technology (Juan de la Cierva subprogram, Ref: JCI-2008-2431). Additional support by the Junta de Andalucia (Spanish government) to the Research Group RNM276 is also acknowledged. Partial funding to J. Ledesma-Vazquez on this project came from the Programma Integral de Fortalecimiento Institucional 2010. We thank Christopher K. Pham, Department of Oceanography and Fisheries, University of the Azores, Portugal, for help with identification of the fossil barnacles and Ricardo Ramalho, Institut fur Geophysik, Westphalishe-Wilhelms Universitat, Germany, for discussions about bioerosion by sea urchins on basalt surfaces

What Darwin did not see: Pleistocene fossil assemblages on a high-energy coast at Ponta das Bicudas, Santiago, Cape Verde Islands