Abstract Abstract: Anatomically preserved conifer-like leaves from the Middle Jurassic La Matilde Formation at the Barda Blanca locality in the Gran Bajo de San Julián area, southern Patagonia are described here. Leaves are assigned to conifers based on the following foliar features: thick-walled epidermal cells, a sclerenchymatic hypodermis, resin canals and transfusion tracheids associated with the vascular bundle. General mesophyll anatomy and inferred foliar morphology suggest a similarity to large, broad, linear-lanceolate, multi-veined conifer-like leaves. The general foliar habit indicates an affinity with the large, multi-veined leaves of the Araucariaceae; especially with those exhibited by the species of the Araucaria sections, Araucaria and Bunya. Anatomically, the permineralized leaves exhibit xeromorphic foliar features, including thick-walled epidermal cells, an isobilateral mesophyll with well-developed palisade cells and mechanical tissue. The general leaf anatomy shown by the Patagonian specimens along with sedimentological data may suggest that during the deposition of the La Matilde Formation at the Barda Blanca locality, the parent plant was well adapted to the environmental conditions, which probably consisted of a high light intensity with an adequate quantity of water in the soil, which increased the maximum leaf conductance of CO2.

Asterozoans are free living, star-shaped echinoderms which are important components of benthic marine faunas worldwide. Their fossil record is, however, poor and fragmentary, probably due to dissarticulation of ossicles. In particular, fossil asteroids are infrequent in South America. A new species of starfish is reported from the early Valanginian of the Mulichinco Formation, Neuquén Basin, in the context of a shallow-water, storm-dominated shoreface environment. The specimen belongs to the Astropectinidae, and was assigned to a new species within the genus Tethyaster Sladen, T. antares sp. nov., characterized by a R:r ratio of 2.43:1, rectangular marginals wider in the interbrachial angles, inferomarginals (28 pairs along a median arc) with slightly convex profile and flat spines (one per ossicle in the interbrachials and two per ossicle in the arms). Both the sedimentologic features of the bearing bed, and the taphonomic signature point to a rapid burial. Considering the presence of well-developed fascioles, it is likely that the specimen was already half buried at the beginning of its taphonomic pathway. This record represents the oldest finding of Astropectinidae in the Southern Hemisphere and the first record of the genus Tethyaster for the Lower Cretaceous of South America.

Los asterozoos son echinodermos de vida libre, con forma de estrella, y componentes importantes de las faunas marinas bentónicas a nivel mundial. Su registro fósil, sin embargo, es pobre y fragmentario, probablemente debido a la desarticulación de los osículos. En particular, los asteroideos fósiles son poco frecuentes en América del Sur. Se presenta aquí una nueva especie de estrella de mar de edad valanginiana proveniente de la Formación Mulichinco (cuenca Neuquina), en un contexto de ambiente somero de 'shoreface' dominado por tormentas. El espécimen pertenece a la Familia Astropectinidae y fue asignado al género Tethyaster Sladen. T. antares sp. nov., se caracteriza por una relación R:r de 2.43:1, marginales rectangulares más anchos en los ángulos interbraquiales, inferomarginales (28 pares a lo largo de un arco medial) con perfil ligeramente convexo y espinas planas (una por osículo en las áreas interbraquiales y dos por osículo en los brazos). Las características sedimentológicas y tafonómicas indican un enterramiento rápido. La presencia de fasciolas bien desarrolladas sugiere la posibilidad de que el espécimen se hallara parcialmente enterrado al comienzo de su ruta tafonómica. Este registro representa el hallazgo más antiguo de Astropectinidae en el Hemisferio Sur y el primer registro del género Tethyaster en el Cretácico Inferior de Sudamérica.