2007 GSA Denver Annual Meeting (2831 October 2007)
Paper No. 216-5
Presentation Time: 2:30 PM-2:45 PM


CALVILLO CANADELL, Laura, Departamento de Paleontologia, Instituto de Geologia, UNAM, Ciudad Universitaria, Delegacion Coyoacan, Distrito Federal, Mexico, 04510, Mexico, lauretacc@hotmail.com, GANDOLFO, Maria A., Department of Plant Biology, Cornell Univ, L. H. Bailey Hortorium, Mann Library, Ithaca, NY 14853, ZAMALOA, Maria C., Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Ciudad Universitaria, Intendente Guiraldes 2620, Buenos Aires, 1428, Argentina, CUNEO, Ruben N., Paleobotany, MEF, Av. Fontana 140, Trelew, 9100, Argentina, WILF, Peter, Dept. of Geosciences, Pennsylvania State University, University Park, PA 16802, and JOHNSON, Kirk

The Early Eocene Laguna del Hunco flora from Chubut, Patagonia, Argentina is one of the world's most diverse Tertiary assemblages of angiosperms. This paleoflora was deposited in tuffaceous mudstones and sandstones of the Tufolitas Laguna del Hunco, which are described as a lacustrine unit of the middle Chubut River volcanic-pyroclastic complex. The flora is even more interesting because its paleofloristic association is composed of tropical elements (i.e. Akania, and Gymnostoma) restricted today to temperate and tropical Australasia; other elements (i.e. Anacardiaceae and Melastomataceae) that are considered to be modern pantropical, and elements of austral origin (i.e. Proteaceae and Podocarpaceae). In this contribution, we describe fossil taxa with affinities to Leguminosae, a family of cosmopolitan distribution. Leguminosae or Fabaceae comprises more than 700 genera and 17000 species belonging to three subfamilies (Papilionoideae, Caesalpinioideae and Mimosoideae) The morphotypes presented here are based on compressions of leaves and a single fruit, and correspond to members of the subfamilies Papilionoideae and Caesalpinioideae.The subfamily Papilionoideae is represented by fossils assignable to the tribes Swarztieae (Zollernia), Brongniartieae (Hovea), Phaseoleae (Rhynchosia), and Desmodieae (Desmodium), while the subfamily Caesalpinioideae is confirmed by the presence of the tribes Detarieae (Hymenaea), Cercideae (Cercis), and Caesalpinieae (Sclerolobium). The tribe Caesalpinieae is also represented by a fossil fruit probably belonging to the genus Caesalpinia. These fossils allow confirmation of the presence of Leguminosae in Patagonia at least since the early Eocene. The presence of two of the three subfamilies by the early Eocene also suggest that the legumes probably already diversified at the subfamilial level in Argentina by the Paleogene. Although the center of origin for the family is uncertain, the presence of these taxa further highlights the diversity and varied biogeographic relationships of the family, adding information for future discussions of its hypothetical origin.

2007 GSA Denver Annual Meeting (2831 October 2007)
General Information for this Meeting
Session No. 216
Paleontology IX: Paleoclimate and Paleoenvironmental Change
Colorado Convention Center: 405
1:30 PM-5:30 PM, Wednesday, 31 October 2007

Geological Society of America Abstracts with Programs, Vol. 39, No. 6, p. 585

© Copyright 2007 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.