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Abstract: Terrestrial paleotemperature and paleobotanical records point to late Miocene cooling and wetter Neotropical climates (AGU25)

Terrestrial paleotemperature and paleobotanical records point to late Miocene cooling and wetter Neotropical climates

Elena Stiles1,2, Katharine W Huntington3, Carmala Garzione4, Caroline A E Strömberg5, Camilo Montes6, Jaime Escobar7, Carlos Jaramillo8, Andrés Felipe Vanegas9, César Perdomo10, Andrew J Schauer5, Zhennan Wang11, Daniel Esteban Góngora12, Lin Li13, Federico Moreno14, David L Dettman15, Lina C Pérez-Angel, PhD16, René López Camacho17 and Andrés Felipe Torrejano18, (1)Burke Museum of Natural History and Culture, Seattle, United States, (2)University of Washington Seattle Campus, Biology, Seattle, United States, (3)University of Washington, Department of Earth and Space Sciences, Seattle, United States, (4)University of Arizona, Geoscience, Tucson, AZ, United States, (5)University of Washington, Seattle, United States, (6)Universidad de los Andes, Bogotá, Colombia, (7)Universidad del Norte, Ingeniería Civil y Ambiental, Barranquilla, Colombia, (8)Smithsonian Tropical Research Institute, Panama, Panama, (9)Museo de Historia Natural La Tatacoa, La Victoria, Colombia, (10)Museo La Tormenta, Villavieja, Colombia, (11)University of Arizona, Tucson, AZ, United States, (12)Instituto Geográfico Agustín Codazzi, Bogotá, Colombia, (13)University of Arizona, Tucson, United States, (14)University of Rochester, Rochester, NY, United States, (15)University of Arizona, Department of Geosciences, Tucson, AZ, United States, (16)University of Colorado at Boulder, Department of Geological Sciences and the Institute of Arctic and Alpine Research, Boulder, CO, United States, (17)Universidad Distrital Francisco José de Caldas, Bogota, Colombia, (18)Instituto Humboldt, Bogotá, Colombia