Boletín de la RSEHN. Sección Geológica

La icnotaxonomía de las esqueletizaciones hasta el momento está pobremente desarrollada. Esto quizá sea el resultado de un escaso registro en comparación a otros tipos de trazas halladas en hojas fósiles. Aquí se dan a conocer nuevas evidencias de esqueletizaciones identificadas en hojas procedentes de la Formación Palo Pintado (Mioceno tardío-Plioceno), que aflora en el centro-sur de la Provincia de Salta, Argentina. Del mismo modo, se propone una nueva nomenclatura para separar las esqueletizaciones de las escisiones marginales, y así contribuir al ordenamiento de la icnotaxonomía de las trazas en hojas fósiles. Se da a conocer el primer hallazgo de esqueletizaciones en helechos neógenos, y que constituye el segundo caso en todo el registro fósil. Por último, este trabajo provee información sobre el comportamiento y preferencias alimenticias de los insectos fitófagos durante este periodo de tiempo.

The ichnotaxonomy of skeletonizations is poorly developed. These are the unique type of fossil traces, in the category of external foliage feeding, that do not count with a clearly established classification. This may be the result of a poor record compared to other types of traces found in fossil leaves. In this work, 856 impressions of angiosperms and ferns were examined, 288 of them showed some evidence of phytophagy damages, among the latter 20 corresponded to skeletonizations. The leaves carrying the traces come from the Quebrada del Horno, Quebrada de Alfredo and Peñas Blancas outcrops. These are located in the center-south of the Salta province, Argentina. The Palo Pintado Fm crops out in these localities, both the stratigraphic correlation and the radiometric dating confer to Palo Pintado Fm a late Miocene - lower Pliocene age. It contacts in the lower section with Angastaco Fm and its upper part with San Felipe Fm. Lithologically, it is composed of sandstones alternating with siltstones and to a lesser degree wtih conglomerates. Sandstones present a brownish coloration while siltstones exhibit yellow and brown hues that merge to greenish sediments. Throughout the formation, there is a disposition in successive finer-grained sedimentary cycles. The layers of limolite are abundant at the base of the formation and become more sporadic towards the upper section. As result of this study, new evidence of skeletonizations identified in leaves from the Palo Pintado Fm are revealed. On the other hand, a new nomenclature is proposed to separate the skeletonizations from the marginal excisions, and thus contribute to the ordering of the ichnotaxonomy of phytophagy traces on fossil leaves. The reason for this proposal is due to that only two ichnospecies of skeletonizations are currently known and they are included in the ichnogenus Phagophytichnus van Amerom, 1966, which was originally established to group the marginal excisions. These types of traces (marginal excisions and skeletonizations) have different morphological and ecological characteristics; the skeletonizations present intact leaf veins inside the traces; instead, the marginal excisions frequently remove all the tissues, including the veins. On the other hand, skeletonizations are exclusively the result of a feeding process and the marginal excisions are also indirect evidence of other types of behavior, for instance, the tissue removed from the leaves can be used by some insects to build nests or as a substrate for the proliferation of fungi. By the above explained, herein is established the ichnogenus Osteophytichnus nov. ichnogen. to include all skeletonizations. In addition, this study reports for the first time skeletonizations on ferns of Neogene age, which also constitute the second case in the entire fossil record. It was not possible to compare the fossil traces found in Acrostichum paleoaureum Beauchamp, Lemoigne & Petrescu, 1973 with extant skeletonizations, since the scarse record of ferns attacked by skeletonizer insects. In the same way, in the extant species related to A. paleoaureum, only non-marginal excisions and window excisions have been reported, which did not allow to establish comparisons or infer possible producer insects for the traces reported in this work. Finally, herein is provided information about the behavior and food preferences of insects during the Neogene of South America.