Cycads today comprise 349 accepted species in ten genera (Calonje et al. 2017). The number of cycad species described during the last decade increased significantly as a result of intense fieldwork by botanists. Recent results of phylogenetic studies of cycads suggested a relatively recent, late Miocene radiation of cycad species along with the Paleogene appearance of most of the major clades (genera excluding Cycas L. and Dioon Lindl.) and have challenged the theory of "living fossil cycads" (Nagalingum et al. 2011, Salas-Leiva et al. 2013, Condamine et al. 2015). These studies estimated the divergence of Microcycas-Zamia to the late Eocene-early Oligocene. Zamia, with 77 currently accepted species (Calonje et al. 2017) is the second largest genus of cycads, and is the most morphologically and ecologically diverse genus in the extant Cycadales (Norstog & Nichols 1997). Furthermore it is the most speciose and broadly distributed cycad genus in the New World. The centre of diversity for the genus appears to be northern South America and Central America, as the highest species diversity occurs in Colombia (21 species) and Panama (17 species). Zamia species inhabit a great variety of habitats including areas near mangrove swamps (Zamia roezlii Linden), dry desert-like areas (Zamia encephalartoides D.W. Stev.), coastal sand dunes (Zamia lucayana Britton), 185 A review of the Cenozoic fossil record of the genus Zamia L. (Zamiaceae, Cycadales) with recognition of a new species from the late Eocene of Panamaevolution and biogeographic inferences Boglárka ErdEi, MichaEl calonjE, austin hEndy & nicolas Espinosa Modern Zamia L. is the second largest genus among cycads, however reliably identified fossil occurrences of the genus have so far been missing. Previously, fossil "Zamia" species were established in large numbers on the basis of macromorphological similarity of foliage fragments to living Zamia species. However, a reinvestigation of specimens assigned formerly to Zamia and the relevant literature provided no clear-cut evidence for their assignment to this genus. We investigated a newly recovered fossil specimen from marine sediments of the Gatuncillo Formation, near Buena Vista, Colon Province, Central Panama. It represents the first unequivocal fossil record of the genus confirmed by epidermal as well as macromorphological characters and it is described as Zamia nelliae Erdei & Calonje sp. nov. Foraminiferal and nannoplankton biostratigraphy of the locality indicates a late Eocene to earliest Oligocene age. Morphometric comparison of epidermal features of Z. nelliae with those of modern Zamia species suggests similarity with those of the Caribbean Zamia clade. The fossil record of Zamia from Panama implies that the genus appeared by the end of the Eocene or earliest Oligocene in the Central American-Caribbean region, however, the origin of the genus is still unresolved. The record of Z. nelliae may challenge former concepts on the evolution of Zamia and raises an "intermediate" hypothesis on its origin in the Cent...