Journal of Paleontology, 87(5), 2013, p. 755–774 Copyright Ó 2013, The Paleontological Society 0022-3360/13/0087-755$03.00 DOI: 10.1666/12-117 SHARKS AND RAYS (CHONDRICHTHYES, ELASMOBRANCHII) FROM THE LATE MIOCENE GATUN FORMATION OF PANAMA CATALINA PIMIENTO,1,2,3 GERARDO GONZA´ LEZ-BARBA,4 DANA J. EHRET,5 AUSTIN J. W. HENDY,1,2 1 2 BRUCE J. MACFADDEN, AND CARLOS JARAMILLO 1Florida Museum of Natural History, University of Florida, Gainesville, FL 32611, USA, ,
[email protected].; ,
[email protected].; ,
[email protected].; 2Smithsonian Tropical Research Institute, Center for Tropical Paleoecology and Archaeology, Box 2072, Panama, Republic of Panama, ,
[email protected].; 3Department of Biology, University of Florida, Gainesville, FL 32611, USA; 4Museo de Historia Natural, Area de Ciencias del Mar, La Paz, Universidad Autonoma de Baja California Sur, AP 23080, Mexico, ,
[email protected].; and 5Alabama Museum of Natural History, University of Alabama, Tuscaloosa, Alabama, 35487, USA, ,
[email protected]. ABSTRACT—The late Miocene Gatun Formation of northern Panama contains a highly diverse and well sampled fossil marine assemblage that occupied a shallow-water embayment close to a purported connection between the Pacific and Atlantic (Caribbean) oceans. However, the diverse chondrichthyan fauna has been poorly documented. Based on recent field discoveries and further analysis of existing collections, the chondrichthyan fauna from this unit comprises at least 26 taxa, of which four species are extinct today. The remaining portion of the total chondrichthyan biodiversity has affinities with modern taxa and is therefore comprised of long-lived species. Based on known records of the modern geographic distribution range of the Gatun chondrichthyans, the fauna has mixed biogeographic affinities suggesting that around 10 million yr ago, a connection likely occurred between the Pacific Ocean and the Caribbean Sea.