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Journal of Paleontology 91(5):1069–1082
previously suspected. This reflects the general paucity of Cenozoic fossil sites from the tropical lower latitudes in North America and that the majority of our knowledge of the diversity of taxa that participated in the GABI and the timing of their dispersal into North America has been based on faunas from higher latitudes. The presence of these sloths raises interesting questions in terms of the evolutionary history of the mega- lonychid sloths and whether their appearance in North America reflects multiple separate dispersal events or a smaller number of dispersals with the subsequent evolution of these taxa occurring in the tropical portions of North America. The presence of these taxa only in North America and their absence in South America suggest this may be the case, but alternatively could simply reflect that, as in North America, there are fewer sites from the late Cenozoic in the tropical parts of northern South America. These questions cannot be resolved until additional fieldwork in the adjoining tropical regions of South and North America provides us with a more robust fossil record.
Acknowledgments
Our thanks to the Centro de Geociencias of the Universidad Nacional Autónoma de México for the support and logistics to carry out the fieldwork and preparation of the fossil material. These were possible with the economic support of the project PAPIIT IN102817. We thank W.E. Miller of Brigham Young University for his participation during the research on the sedimentary basins of central Mexico, B.Kowallis fromBYUfor description of the geology and stratigraphy and radiometric ages of the Tecolotlán Basin.We thank J. Silva Corona for the figures and photographs in this work, H. Troncoso for the preparation of the fossils collected, C. Luis Espinosa for his criticism of part of the manuscript, and C. Ortega (LA-ICPMS), Centro de Geociencias for the second analysis of ash. The Center for Field Research, and especially EarthWatch volunteers, are thanked for their support of the Fossils of the SierraMadre project, and their invaluable help collecting fossils during this project. We thank P. Holroyd, UCMP, for providing pictures of the Pliometanastes from the Siphon Canal Locality and L. Fowler for providing the measurements of this specimen. S. Bargo, D. Brandoni, and S. Hirschfeld generously provided images of specimens from their publications. We thank our reviewers, D. Croft and G. DeIuliis, for their comments, which improved the quality of the paper.
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