An ichthyosaurian forefin from the Lower Cretaceous Zapata Formation of southern Chile: implications for morphological variability within Platypterygius

Fil: Pardo-Pérez, Judith. Institut für Geowissenschaften. Ruprecht Karls Universität Heidelberg. Heidelberg; GermanyFil: Frey, Eberhard. Staatliches Museum für Naturkunde Karlsruhe; GermanyFil: Stinnesbeck, Wolfgang. Institut für Geowissenschaften. Ruprecht Karls Universität Heidelberg. Heidelberg; GermanyFil: Fernández, Marta Susana. División Paleontología Vertebrados. Facultad de Ciencias Naturales y Museo. Universidad Nacional de La Plata; ArgentinaFil: Rivas, Luis. Departamento Ciencias de la Tierra. Universidad de Concepción; ChileFil: Salazar, Christian. Institut für Geowissenschaften. Ruprecht Karls Universität Heidelberg. Heidelberg; GermanyFil: Leppe, Marcelo. Instituto Antártico Chileno. Punta Arenas; Chil

New cladotherian mammal from southern Chile and the evolution of mesungulatid meridiolestidans at the dusk of the Mesozoic era

In the last decades, several discoveries have uncovered the complexity of mammalian evolution during the Mesozoic Era, including important Gondwanan lineages: the australosphenidans, gondwanatherians, and meridiolestidans (Dryolestoidea). Most often, their presence and diversity is documented by isolated teeth and jaws. Here, we describe a new meridiolestidan mammal, Orretherium tzen gen. et sp. nov., from the Late Cretaceous of southern Chile, based on a partial jaw with five cheek teeth in locis and an isolated upper premolar. Phylogenetic analysis places Orretherium as the earliest divergence within Mesungulatidae, before other forms such as the Late Cretaceous Mesungulatum and Coloniatherium, and the early Paleocene Peligrotherium. The in loco tooth sequence (last two premolars and three molars) is the first recovered for a Cretaceous taxon in this family and suggests that reconstructed tooth sequences for other Mesozoic mesungulatids may include more than one species. Tooth eruption and replacement show that molar eruption in mesungulatids is heterochronically delayed with regard to basal dryolestoids, with therian-like simultaneous eruption of the last premolar and last molar. Meridiolestidans seem endemic to Patagonia, but given their diversity and abundance, and the similarity of vertebrate faunas in other regions of Gondwana, they may yet be discovered in other continents.Fil: Martinelli, Agustín Guillermo. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Parque Centenario. Museo Argentino de Ciencias Naturales "Bernardino Rivadavia"; Argentina. Universidad de Chile; ChileFil: Soto Acuña, Sergio. Universidad de Chile; ChileFil: Goin, Francisco Javier. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Paleontología Vertebrados; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; ArgentinaFil: Kaluza, Jonatan Ezequiel. Universidad Maimónides; Argentina. Universidad de Chile; Chile. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; ArgentinaFil: Bostelmann, J. Enrique. Universidad Austral de Chile; ChileFil: Fonseca, Pedro H. M.. Universidade Federal do Rio Grande do Sul; BrasilFil: Reguero, Marcelo Alfredo. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Paleontología Vertebrados; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; ArgentinaFil: Leppe, Marcelo. Instituto Antártico Chileno; ChileFil: Vargas, Alexander O.. Universidad de Chile; Chil

Evolution of Climatic Related Leaf Traits in the Family Nothofagaceae

The current relationship between leaf traits and environmental variables has been widely used as a proxy for climate estimates. However, it has been observed that the phylogenetic relationships between taxa also influence the evolution of climatic related leaf traits, implying that the direct use of the physiognomy–climate relation should be corrected by their ancestor–descendant relations. Here, we analyze the variation of 20 leaf traits during the evolution of 27 species in the Gondwana family Nothofagaceae. We evaluate whether the evolution of these traits is exclusively associated with past climate variations or whether they are restricted by phylogenetic relationships. Our results indicate that four leaf traits, associated with size and shape, had consistently a phylogenetic independent evolution, suggesting adaptive variation with the environment. While three of the traits, presented consistently phylogenetic signal and fit a Brownian motion or Ornstein-Uhlenbeck model of evolution, suggesting that the evolution of these traits is restrained by phylogenetic relationships and implying that phylogenetic corrections should be made for the family Nothofagaceae to use them as climatic proxy. Finally, this study highlights the importance of evaluating the evolutionary history of climatic related leaf traits before conducting paleoclimate estimates

Primer mamífero Mesozoico de Chile: el registro más austral de un gondwanaterio del Cretácico tardío

Se describe a Magallanodon baikashkenke gen. et. sp. nov., un nuevo mamífero gondwanaterio del Cretácico tardío de la Región de Magallanes, en el sur de Chile (Valle del Río de Las Chinas, Estancia Cerro Guido, norte de Puerto Natales, Provincia de Última Esperanza). Las capas portadoras se ubican entre los niveles del Campaniano tardío-Maastrichtiano temprano de la Formación Dorotea (Cuenca de Magallanes/Austral). Los nuevos restos constituyen el registro más austral de un mamífero gondwanaterio del Mesozoico, como así también el primer mamífero Mesozoico conocido para Chile. El nuevo taxón es comparable en tamaño a las formas hipsodontes Gondwanatherium (Cretácico tardío) y Sudamerica (Paleoceno temprano), pero con molares notoriamente braquidontes soportados por cuatro a cinco raíces. Como en otros gondwanaterios, posee al menos un incisivo superior rodentiforme en la serie superior. Se diagnostica y describe brevemente el nuevo taxón, considerado tentativamente como un ferugliotérido (Ferugliotheriidae). De confirmarse esta asignación, este nuevo taxón representaría el miembro de mayor tamaño para la familia. El patrón oclusal de los molariformes, con el desgaste, se semeja también al de otros gondwanaterios, en particular al de los ferugliotéridos y al del sudamerícido Gondwanatherium, agregando en consecuencia más evidencias en favor de la proximidad filogenética entre ambas familias. Se llevó a cabo un análisis de la microestructura del esmalte del incisivo superior de Magallanodon; como resultado, se encontraron varias similitudes importantes con el patrón existente en Gondwanatherium (Sudamericidae). Se discute la significación de Magallanodon en la adquisición, entre los gondwanaterios, de un patrón molariforme caracterizado por la presencia de lofos transversos. Finalmente, se discute la significación del nuevo hallazgo en el contexto de las biotas australes, incluyendo aquellas de Patagonia y Antártica.We describe Magallanodon baikashkenke gen. et. sp. nov., a new gondwanatherian mammal from the Late Cretaceous of the Magallanes Region in southern Chile (Río de Las Chinas Valley, Estancia Cerro Guido, north of Puerto Natales city, Última Esperanza Province). The mammal-bearing layer is placed within the Late Campanian-Early Maastrichtian levels of the Dorotea Formation (Magallanes/ Austral Basin). The new remains constitute the southernmost record of a Mesozoic gondwanatherian mammal, as well as the first Mesozoic mammal from Chile. This taxon is comparable in size to the hypsodont-toothed Gondwanatherium (Late Cretaceous) and Sudamerica (Early Paleocene) but with noticeably brachyodont molariforms supported by four to five roots. As in other gondwanatherians, it has at least one hypertrophied, rodent-like incisor in the upper jaw. The new taxon is here diagnosed and described, and is regarded as a possible ferugliotheriid (?Ferugliotheriidae). If confirmed, it would represent the largest known taxon for this family. Its molariform occlusal crown pattern, after wear, resembles that of other gondwanatherians, particularly ferugliotheriids and that of the sudamericid Gondwanatherium. This adds new evidence on the phylogenetic proximity of ferugliotheriid and sudamericid gondwanatherians. An analysis of the enamel microstructure of the upper incisor of Magallanodon was performed demonstrating several crucial similarities with the pattern shown by Gondwanatherium (Sudamericidae). We discuss the significance of Magallanodon for understanding the acquisition, within gondwanatherians, of a lophed molariform pattern. Finally, we discuss the significance of the new finding in the context of southern biotas, including those of Patagonia and Antarctica.Fil: Goin, Francisco Javier. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Paleontología Vertebrados; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; ArgentinaFil: Martinelli, Agustín Guillermo. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Parque Centenario. Museo Argentino de Ciencias Naturales "Bernardino Rivadavia"; ArgentinaFil: Soto Acuña, Sergio. Universidad de Santiago de Chile. Facultad de Ciencias; ChileFil: Vieytes, Emma Carolina. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Zoología de Vertebrados; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; ArgentinaFil: Manriquez, Leslie. Universidad de Vale do Rio dos Sinos; BrasilFil: Fernandez, Roy A.. Universidad de Santiago de Chile. Facultad de Ciencias; ChileFil: Pino, Juan Pablo. Instituto Antártico Chileno; ChileFil: Trevisan Cristine. Instituto Antártico Chileno; ChileFil: Kaluza, Jonatan Ezequiel. Universidad de Santiago de Chile. Facultad de Ciencias; Chile. Fundación de Historia Natural Félix de Azara; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Reguero, Marcelo Alfredo. Museo Nacional de Historia Natural de Santiago; Chile. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; ArgentinaFil: Leppe, Marcelo. Instituto Antártico Chileno; ChileFil: Ortiz, Hector. Universidad de Santiago de Chile. Facultad de Ciencias; ChileFil: Rubilar Rogers, David. Museo Nacional de Historia Natural de Santiago; ChileFil: Vargas, Alexander. Universidad de Santiago de Chile. Facultad de Ciencias; Chil

Multiple late-Pleistocene colonisation events of the Antarctic pearlwort Colobanthus quitensis (Caryophyllaceae) reveal the recent arrival of native Antarctic vascular flora

Aim: Antarctica's remote and extreme terrestrial environments are inhabited by only two species of native vascular plants. We assessed genetic connectivity amongst Antarctic and South American populations of one of these species, Colobanthus quitensis, to determine its origin and age in Antarctica. Location: Maritime Antarctic, sub‐Antarctic islands, South America. Taxon: Antarctic pearlwort Colobanthus quitensis (Caryophyllaceae). Methods: Four chloroplast markers and one nuclear marker were sequenced from 270 samples from a latitudinal transect spanning 21–68° S. Phylogeographic, population genetic and molecular dating analyses were used to assess the demographic history of C. quitensis and the age of the species in Antarctica. Results: Maritime Antarctic populations consisted of two different haplotype clusters, occupying the northern and southern Maritime Antarctic. Molecular dating analyses suggested C. quitensis to be a young (<1 Ma) species, with contemporary population structure derived since the late‐Pleistocene. Main conclusions: The Maritime Antarctic populations likely derived from two independent, late‐Pleistocene dispersal events. Both clusters shared haplotypes with sub‐Antarctic South Georgia, suggesting higher connectivity across the Southern Ocean than previously thought. The overall findings of multiple colonization events by a vascular plant species to Antarctica, and the recent timing of these events, are of significance with respect to future colonizations of the Antarctic Peninsula by vascular plants, particularly with predicted increases in ice‐free land in this area. This study fills a significant gap in our knowledge of the age of the contemporary Antarctic terrestrial biota. Adding to previous inferences on the other Antarctic vascular plant species (the grass Deschampsia antarctica), we suggest that both angiosperm species are likely to have arrived on a recent (late‐Pleistocene) time‐scale. While most major groups of Antarctic terrestrial biota include examples of much longer‐term Antarctic persistence, the vascular flora stands out as the first identified terrestrial group that appears to be of recent origin

Relict duck-billed dinosaurs survived into the last age of the dinosaurs in subantarctic Chile

In the dusk of the Mesozoic, advanced duck-billed dinosaurs (Hadrosauridae) were so successful that they likely outcompeted other herbivores, contributing to declines in dinosaur diversity. From Laurasia, hadrosaurids dispersed widely, colonizing Africa, South America, and, allegedly, Antarctica. Here, we present the first species of a duck-billed dinosaur from a subantarctic region, Gonkoken nanoi, of early Maastrichtian age in Magallanes, Chile. Unlike duckbills further north in Patagonia, Gonkoken descends from North American forms diverging shortly before the origin of Hadrosauridae. However, at the time, non-hadrosaurids in North America had become replaced by hadrosaurids. We propose that the ancestors of Gonkoken arrived earlier in South America and reached further south, into regions where hadrosaurids never arrived: All alleged subantarctic and Antarctic remains of hadrosaurids could belong to non-hadrosaurid duckbills like Gonkoken. Dinosaur faunas of the world underwent qualitatively different changes before the Cretaceous-Paleogene asteroid impact, which should be considered when discussing their possible vulnerability

The South Shetland Islands, Antarctica: unified lithostratigraphy and geological map

Over the last few decades, numerous geological studies have been carried out in the South Shetland Islands, which have greatly contributed to a better understanding of its geological evolution. However, few attempts have been conducted to correlate the geological units throughout this archipelago. We present herein a lithostratigraphical correlation, which constitutes a coherent and unified stratigraphy for the main Mesozoic and Cenozoic units rocks of the South Shetland Islands along with a new geological map. The lithostratigraphical correlation shows that the geological evolution comprises three main stages: (i) deep marine sedimentation from ~164 to 140 Ma, (ii) subaerial volcanism and sedimentation with a proliferation of plants and fauna from ~140 to 35 Ma and (iii) glacial and interglacial deposits from ~35 Ma. The lithostratigraphical correlation also shows a broad geographical trend of decreasing age of volcanism from southwest to northeast, which has been previously suggested. However, this spatial age trend is disrupted by the presence of Eocene magmatism in Livingston Island, located in the centre of the archipelago. We suggest that the migration of volcanism occurred from the Late Cretaceous until the early Eocene. Subsequently, enhanced magmatic activity took place from the mid-Eocene until the Miocene, which we associate with processes related with the waning of subduction, such as roll-back. Finally, constraining the protolith age of the metamorphic complex of Smith Island remains challenging, yet holds key implications for the tectonic and accretionary evolution of the Antarctic Peninsula. The rocks recording the glaciation of this sector of Antarctica are well exposed in the northern South Shetland Islands and hold critical information for understanding the timings and processes that lead to the greenhouse-icehouse transition towards the Eocene end. Contemporaneous rocks to the breakup of Antarctic Peninsula from Patagonia, which led to the Drake Passage opening and the development of the Scotia Sea, are exposed in the north-centre of the archipelago. A better age constrain of these units may lead to further understanding the paleontological evolution of this region. The dataset containing the geological map is shared as a shapefile and KML file

Sustained Antarctic Research: A 21st Century Imperative

The view from the south is, more than ever, dominated by ominous signs of change. Antarctica and the Southern Ocean are intrinsic to the Earth system, and their evolution is intertwined with and influences the course of the Anthropocene. In turn, changes in the Antarctic affect and presage humanity's future. Growing understanding is countering popular beliefs that Antarctica is pristine, stable, isolated, and reliably frozen. An aspirational roadmap for Antarctic science has facilitated research since 2014. A renewed commitment to gathering further knowledge will quicken the pace of understanding of Earth systems and beyond. Progress is already evident, such as addressing uncertainties in the causes and pace of ice loss and global sea-level rise. However, much remains to be learned. As an iconic global “commons,” the rapidity of Antarctic change will provoke further political action. Antarctic research is more vital than ever to a sustainable future for this One Earth

Asedios al archivo, la literatura, los territorios, las pedagogías y la creación

Lenguajes de la memoria y los Derechos Humanos III. Asedios al archivo, la literatura, los territorios, las pedagogías y la creación está integrado por un conjunto de trabajos cuyos ejes temáticos son auscultados desde el suelo presente, necesario, insistente, heteroglósico, en continua redefinición. El libro fue concebido en un momento atravesado por el influjo del abismo producido por el gobierno de la derecha en Argentina y en América Latina, en el interregno 2015-2019, y culminado durante la pandemia Covid 19, que azota al mundo con millones de muertos e infectados.Fil: Ares, María Cristina. Universidad de Buenos Aires. Departamento de Letras; Argentina.Fil: Bracaccini Acevedo, María. Universidad Nacional de Córdoba. Facultad de Filosofía y Humanidades; Argentina.Fil: Cella, Susana. Universidad de Buenos Aires. Facultad de Filosofía y Letras; Argentina.Fil: Cornavaca, María Trinidad. Universidad Nacional de Córdoba. Facultad de Lenguas; Argentina.Fil: Corral, María Manuela. Universidad Nacional de Córdoba. Facultad de Lenguas; Argentina.Fil: Crenzel, Emilio. Universidad de Buenos Aires. Facultad de Ciencias Sociales; Argentina.Fil: Da Silva Catela, Ludmila. Universidad Federal de Río de Janeiro; Brasil.Fil: Díaz, Marcelo. Universidad Nacional de Río Cuarto; Argentina.Fil: Ferraro, Paula Daniela. Universidad Federal Fluminense; Brasil.Fil: Ferrada Rau, Rocío Nili. Universidad de Chile; Chile.Fil: Garbero, Vanesa. Universidad de Buenos Aires; Argentina.Fil: García, Díaz. Universidad Nacional Autónoma de México; México.Fil: Giraldi Dei Cas, Norah. Universidad de Lille; Francia.Fil: Gutiérrez, Carlos Arturo. Universidad Nacional de Colombia; Colombia.Fil: Kozameh, Alicia. Chapman University. Departamento de Inglés; Estados Unidos.Fil: Magrin, Natalia. Universidad Nacional de Córdoba. Facultad de Psicología; Argentina.Fil: Inchauspe, Leandro. Universidad Nacional de Córdoba. Facultad de Filosofía y Humanidades. Escuela de Historia; Argentina.Fil: Martínez, Carlos Dámaso. Universidad Nacional de Córdoba. Facultad de Filosofía y Humanidades. Escuela de Letras; Argentina.Fil: Mercado, Mónica. Universidad Nacional de Córdoba. Facultad de Artes. Departamento Académico de Artes Visuales; Argentina.Fil: Merro, Agustina. Universidad Nacional de Córdoba. Facultad de Filosofía y Humanidades. Escuela de Letras; Argentina.Fil: Mohaded, Ana. Universidad Nacional de Córdoba. Facultad de Artes. Departamento Académico de Cine y Televisión; Argentina.Fil: Montes, Alicia. Universidad de Buenos Aires. Facultad de Filosofía y Letras; Argentina.Fil: Muñoz Leppe, Olga Elvira. Universidad Metropolitana de Ciencias de la Educación; Chile.Fil: Palma Solís, Jennifer Luz. Universidad de Chile; Chile.Fil: Pino, Mirian. Universidad Nacional de Córdoba. Facultad de Filosofía y Humanidades. Escuela de Letras; Argentina.Fil: Rabanal Gatica, Damaso. Universidad Austral de Chile; Chile.Fil: Reati, Fernando. Georgia State University; Estados Unidos.Fil: Reyes, Manuela. Universidad Nacional de Villa María; Argentina.Fil: Rocchietti, Luciana. Universidad Nacional de Córdoba. Facultad de Ciencias de la Comunicación; Argentina.Fil: Saint Bonet, María Virginia. Universidad Nacional de Córdoba. Facultad de Filosofía y Humanidades. Escuela de Letras; Argentina.Fil: Schwenke, Gonzalo. Universidad Austral de Chile; Chile.Fil: Semilla Durán, María Angélica. Universidad Central de Barcelona; España.Fil: Solis, Ana Carol. Universidad Nacional de Córdoba. Facultad de Filosofía y Humanidades. Escuela de Historia; Argentina.Fil: Sosa San Martín, Gabriela. Universidad de la República. Facultad de Humanidades y Ciencias de la Educación; Uruguay.Fil: Suppo, Carina Noemí. Universidad Nacional de Rosario; Argentina.Fil: Vásquez, Malva Marina. Universidad de Chile; Chile.Fil: Vassallo, Celeste. Universidad Nacional de Córdoba. Facultad de Filosofía y Humanidades. Escuela de Letras; Argentina.Fil: Wild, Carolina. Universidad Nacional de Córdoba. Facultad de Ciencias de la Comunicación; Argentina