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| DOI | 10.1080/03115518.2018.1517222 | ||
| Año | 2019 | ||
| Tipo | artículo de investigación |
Citas Totales
Autores Afiliación Chile
Instituciones Chile
% Participación
Internacional
Autores
Afiliación Extranjera
Instituciones
Extranjeras
A new podocarpaceous conifer is described from the early Danian Salamanca Formation (southern Chubut, Patagonia, Argentina) based on compressions of leafy branches with cuticular remains. Kirketapel salamanquensis gen. et sp. nov. has amphistomatic, scale-like leaves with marginal frills distinguishable at the apex; stomata oriented randomly in relation to the major axis of the leaf with four to five subsidiary cells and extremely reduced Florin rings; and irregularly shaped epidermal cells. We compare K. salamanquensis with extant and extinct members of the imbricate-leaved podocarps, among which it closely resembles Florin's Dacrydium group C genera (i.e., Lagarostrobos, Manoao, Lepidothamnus and Halocarpus). Among these genera, only Lepidothamnus has a living representative in South America, the Chilean L. fonkii, whose leaf macro- and micromorphological characters are described in detail for comparison. Overall, the Patagonian fossil species is most similar to the extant and extinct members of Lagarostrobos in its cuticular micromorphology; however, macromorphological characters, such as the leaf size, apex curvature and mode of flattening, clearly differentiate it from all four genera of Dacrydium group C. We include Kirketapel salamanquensis in a combined molecular and morphological phylogenetic analysis conducted under the maximum parsimony criterion. The new, early Paleocene fossil taxon is confidently recovered as part of the scale-leaved clade as defined herein, which also includes Halocarpus, Phyllocladus, Lepidothamnus, Parasitaxus, Lagarostrobos and Manoao, and it constitutes the oldest record known for the group by at least 17 million years as well as its first fossil occurrence outside Australasia, establishing a widespread Gondwanan history. Furthermore, based on its oldest locality of occurrence, K. salamanquensis shows that the divergence of the total group of the scale-leaved podocarps occurred by at least 65 million years ago, adding to the growing systematic knowledge of earliest Cenozoic macrofloras in the Southern Hemisphere.
| Ord. | Autor | Género | Institución - País |
|---|---|---|---|
| 1 | Andruchow-Colombo, Ana | Mujer |
Museo Paleontol Egidio Feruglio - Argentina
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| 2 | Escapa, Ignacio H. | Hombre |
Museo Paleontol Egidio Feruglio - Argentina
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| 3 | Carpenter, Raymond J. | Hombre |
Univ Tasmania - Australia
Univ Adelaide - Australia |
| 4 | Hill, Robert S. | Hombre |
Univ Adelaide - Australia
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| 5 | Iglesias, Ari | - |
UNIV NACL COMAHUE - Argentina
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| 6 | ABARZUA-VASQUEZ, ANA MARIA | Mujer |
Universidad Austral de Chile - Chile
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| 7 | Wilf, Peter | Hombre |
PENN STATE UNIV - Estados Unidos
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| Fuente |
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| NSF |
| National Science Foundation (NSF) |
| Argentinean National Scientific and Technical Research Council (CONICET) |
| Agradecimiento |
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| The authors thank L. Reiner and E. Ruigomez for helping with the curation of the fossil specimens, A. Vilela for the curation of the L. fonkii specimens at PBP Herbarium, I. Davie for his help in cuticle preparation, Aluar Aluminio Argentino SAIC and Servicio de Microscopia de Barrido del Museo de La Plata for providing access to the SEM, and M. Luquet and P. Sarmiento for technical support. Thanks to the Secretaria de Cultura and Secretaria de Turismo y areas Protegidas from Chubut Province, to A. Balercia, Bochatey Family, and H. Visser for facilitating land access, and to P. Puerta, K. R. Johnson, M. Caffa, L. Canessa and many others for help in the field. We are indebted to M. Gandolfo, K. Nixon, A. Stalter and P. Fraissinet for providing access to the herbarium and plant anatomy collection of the L.H. Bailey Hortorium at Cornell University; to M. Pole, who kindly provided images of New Zealand fossil material; to L. Aagesen, N.B. Degiani, I. Schonberger, and M. Tomescu for providing podocarp material; and to M. Krause and W. Clyde for their help with the geology. We are indebted to C. Mays and two anonymous reviewers for their remarks and suggestions that greatly improved the quality of the manuscript. Recent support for this research came from National Science Foundation (NSF) grant DEB-1556666, and prior support came from NSF grants DEB-0919071 and DEB-0345750. We also thank the Argentinean National Scientific and Technical Research Council (CONICET) for research funding. |