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Origin of the white shark Carcharodon (Lamniformes: Lamnidae) based on recalibration of the Upper Neogene Pisco Formation of Peru
Authors:DANA J EHRET  BRUCE J MACFADDEN  DOUGLAS S JONES  THOMAS J DEVRIES  DAVID A FOSTER  RODOLFO SALAS‐GISMONDI
Institution:1. Monmouth University, West Long Branch, NJ, 07764, USA;2. e‐mail: dehret@monmouth.edu;3. Florida Museum of Natural History, University of Florida, Gainesville, FL 32611, USA;4. e‐mails: bmacfadd@flmnh.ufl.edu, dsjones@flmnh.ufl.edu;5. Burke Museum of Natural History and Culture, University of Washington, Seattle, WA 98195, USA;6. e‐mail: tomdevrie@aol.com;7. Department of Geological Sciences, University of Florida, Gainesville, FL 32611, USA;8. e‐mail: dafoster@ufl.edu;9. Departmento de Paleontologia de Vertebrados, Museo de Historia Natural Javier Prado, Universidad Nacional Mayor de San Marcos, Lima 11, Peru;10. e‐mail: rodsalasgis@yahoo.com
Abstract:Abstract: The taxonomic origin of the white shark, Carcharodon, is a highly debated subject. New fossil evidence presented in this study suggests that the genus is derived from the broad‐toothed ‘mako’, Carcharodon (Cosmopolitodus) hastalis, and includes the new species C. hubbelli sp. nov. – a taxon that demonstrates a transition between Chastalis and Carcharodon carcharias. Specimens from the Pisco Formation clearly demonstrate an evolutionary mosaic of characters of both recent C. carcharias and fossil C. hastalis. Characters diagnostic to C. carcharias include the presence tooth serrations and a symmetrical first upper anterior tooth that is the largest in the tooth row, while those indicative of C. hastalis include a mesially slanted third anterior (intermediate) tooth. We also provide a recalibration of critical fossil horizons within the Pisco Formation, Peru using zircon U‐Pb dating and strontium‐ratio isotopic analysis. The recalibration of the absolute dates suggests that Carcharodon hubbelli sp. nov. is Late Miocene (6–8 Ma) in age. This research revises and elucidates lamnid shark evolution based on the calibration of the Neogene Pisco Formation.
Keywords:Carcharocles  Cosmopolitodus  geochronology  Miocene  Isurus  strontium
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