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</o:shapelayout></xml><![endif]--></head><body lang=es-419 link="#0563C1" vlink="#954F72" style='word-wrap:break-word'><div class=WordSection1><h2 style='mso-margin-top-alt:0cm;margin-right:0cm;margin-bottom:15.0pt;margin-left:0cm;line-height:22.5pt'><span style='font-size:12.0pt;font-weight:normal'>Estimados colegas,<o:p></o:p></span></h2><h2 style='mso-margin-top-alt:0cm;margin-right:0cm;margin-bottom:15.0pt;margin-left:0cm;line-height:22.5pt;box-sizing: border-box;display:inline-block;background-image:initial;background-position:initial;background-size: initial;background-repeat:initial;background-attachment:initial;background-origin: initial;background-clip: initial;color:rgba(0, 0, 0, 0.54)'><span style='font-size:12.0pt;font-weight:normal'>Nos es grato comunicarles que ha sido publicado un nuevo número de la Revista de la Asociación Geológica Argentina. Les recordamos que la gestión editorial de la RAGA se está llevando a cabo a través de la nueva plataforma: <a href="https://revista.geologica.org.ar/raga">https://revista.geologica.org.ar/raga</a> <o:p></o:p></span></h2><h2 style='mso-margin-top-alt:0cm;margin-right:0cm;margin-bottom:15.0pt;margin-left:0cm;line-height:22.5pt;box-sizing: border-box;display:inline-block;background-image:initial;background-position:initial;background-size: initial;background-repeat:initial;background-attachment:initial;background-origin: initial;background-clip: initial;color:rgba(0, 0, 0, 0.54)'><span style='font-size:12.0pt;font-weight:normal'>Cordiales saludos,<o:p></o:p></span></h2><p class=MsoNoSpacing><span style='font-size:12.0pt'>Subcomisión de Publicaciones<o:p></o:p></span></p><p class=MsoNoSpacing><span style='font-size:12.0pt'>Asociación Geológica Argentina<o:p></o:p></span></p><h2 style='mso-margin-top-alt:0cm;margin-right:0cm;margin-bottom:15.0pt;margin-left:0cm;line-height:22.5pt'><span style='font-size:12.0pt;font-family:"Segoe UI",sans-serif'><o:p> </o:p></span></h2><h2 style='mso-margin-top-alt:0cm;margin-right:0cm;margin-bottom:15.0pt;margin-left:0cm;line-height:22.5pt'><span style='font-size:12.0pt;font-family:"Segoe UI",sans-serif'>Vol. 77 Núm. 3 (2020): Desarrollos recientes en icnología argentina<o:p></o:p></span></h2><h2 style='mso-margin-top-alt:0cm;margin-right:0cm;margin-bottom:15.0pt;margin-left:0cm;line-height:22.5pt'><span style='font-size:11.0pt;font-family:"Segoe UI",sans-serif;font-weight:normal'>Editoras invitadas: Graciela S. Bressan y Diana E. Fernández<o:p></o:p></span></h2><h2 style='mso-margin-top-alt:0cm;margin-right:0cm;margin-bottom:15.0pt;margin-left:0cm;line-height:22.5pt'><span style='font-size:12.0pt;font-family:"Segoe UI",sans-serif;font-weight:normal'>Artículos</span><span style='font-size:12.0pt;font-family:"Segoe UI",sans-serif'><o:p></o:p></span></h2><h3 style='margin:0cm;line-height:15.0pt'><span lang=EN-US style='font-size:10.5pt;font-family:"Segoe UI",sans-serif'>Petrographic analysis of crowded Rosselia ichnofabrics from the Tremadocian of Northwestern Argentina: Ethologic meaning and diagenesis <o:p></o:p></span></h3><h3 style='margin:0cm;line-height:15.0pt'><span style='font-size:10.0pt;font-family:"Segoe UI",sans-serif;font-weight:normal'>María Duperron, Roberto A Scasso <o:p></o:p></span></h3><h3 style='margin:0cm;line-height:15.0pt'><span style='font-size:10.0pt;font-family:"Segoe UI",sans-serif;border:solid #007AB2 1.0pt;padding:0cm;font-weight:normal'><a href="https://revista.geologica.org.ar/raga/article/view/216/613"><span style='text-decoration:none'>PDF</span></a></span><span style='font-size:10.5pt;font-family:"Segoe UI",sans-serif;font-weight:normal'> </span><span style='font-size:10.5pt;font-family:"Segoe UI",sans-serif'><o:p></o:p></span></h3><h3 style='margin:0cm;line-height:15.0pt'><span lang=EN-US style='font-size:10.5pt;font-family:"Segoe UI",sans-serif'><o:p> </o:p></span></h3><h3 style='margin:0cm;line-height:15.0pt'><span lang=EN-US style='font-size:10.5pt;font-family:"Segoe UI",sans-serif'>Palaxius chosmalalensis n. isp., a new crustacean microcoprolite from the Lower Cretaceous of Argentina and new criteria for the classification of ichnospecies of Palaxius<o:p></o:p></span></h3><h3 style='margin:0cm;line-height:15.0pt'><span style='font-size:10.0pt;font-family:"Segoe UI",sans-serif;font-weight:normal'>Diego A. Kietzmann, Mariana S. Olivo<o:p></o:p></span></h3><h3 style='margin:0cm;line-height:15.0pt'><span style='font-size:10.5pt;font-family:"Segoe UI",sans-serif;font-weight:normal'><a href="https://revista.geologica.org.ar/raga/article/view/14/610"><span lang=EN-US style='font-size:10.0pt;color:#007AB2;border:solid #007AB2 1.0pt;padding:0cm;text-decoration:none'>PDF</span></a></span><span lang=EN-US style='font-size:10.5pt;font-family:"Segoe UI",sans-serif;font-weight:normal'><o:p></o:p></span></h3><h3 style='margin:0cm;line-height:15.0pt'><span lang=EN-US style='font-size:10.5pt;font-family:"Segoe UI",sans-serif'><o:p> </o:p></span></h3><h3 style='margin:0cm;line-height:15.0pt'><span lang=EN-US style='font-size:10.5pt;font-family:"Segoe UI",sans-serif'>Taphonomy of decapod-bearing concretions and their associated trace fossils from the Agrio Formation (Lower Cretaceous, Neuquén Basin), with paleobiological implications for axiid shrimps<o:p></o:p></span></h3><h3 style='margin:0cm;line-height:15.0pt'><span style='font-size:10.0pt;font-family:"Segoe UI",sans-serif;font-weight:normal'>A. Mariel Andrada, Graciela S Bressan, Darío G Lazo<o:p></o:p></span></h3><h3 style='margin:0cm;line-height:15.0pt'><span style='font-size:10.5pt;font-family:"Segoe UI",sans-serif;font-weight:normal'><a href="https://revista.geologica.org.ar/raga/article/view/217/612"><span lang=EN-US style='font-size:10.0pt;color:#007AB2;border:solid #007AB2 1.0pt;padding:0cm;text-decoration:none'>PDF</span></a></span><span lang=EN-US style='font-size:10.5pt;font-family:"Segoe UI",sans-serif;font-weight:normal'><o:p></o:p></span></h3><h3 style='margin:0cm;line-height:15.0pt'><span lang=EN-US style='font-size:10.5pt;font-family:"Segoe UI",sans-serif'><o:p> </o:p></span></h3><h3 style='margin:0cm;line-height:15.0pt'><span lang=EN-US style='font-size:10.5pt;font-family:"Segoe UI",sans-serif'>Analysis of Asteriacites von Schlotheim 1820 from Mulichinco Formation (Lower Cretaceous, Neuquén Basin) and ichnotaxonomic implications<o:p></o:p></span></h3><h3 style='margin:0cm;line-height:15.0pt'><span style='font-size:10.0pt;font-family:"Segoe UI",sans-serif;font-weight:normal'>Luciana M Giachetti, Diana E Fernández, Marcos Comerio<o:p></o:p></span></h3><h3 style='margin:0cm;line-height:15.0pt'><span style='font-size:10.5pt;font-family:"Segoe UI",sans-serif'><a href="https://revista.geologica.org.ar/raga/article/view/218/614"><span lang=EN-US style='font-size:10.0pt;color:#007AB2;border:solid #007AB2 1.0pt;padding:0cm;font-weight:normal;text-decoration:none'>PDF</span></a></span><span lang=EN-US style='font-size:10.5pt;font-family:"Segoe UI",sans-serif;font-weight:normal'><o:p></o:p></span></h3><h3 style='margin:0cm;line-height:15.0pt'><span lang=EN-US style='font-size:10.5pt;font-family:"Segoe UI",sans-serif'><o:p> </o:p></span></h3><h3 style='margin:0cm;line-height:15.0pt'><span lang=EN-US style='font-size:10.5pt;font-family:"Segoe UI",sans-serif'>Vertebrate tracks of the Río Negro province, Patagonia, Argentina: stratigraphy, palaeobiology and environmental contexts<o:p></o:p></span></h3><h3 style='margin:0cm;line-height:15.0pt'><span style='font-size:10.0pt;font-family:"Segoe UI",sans-serif;font-weight:normal'>Silvina De Valais, Ignacio Díaz-Martínez, Paolo Citton, Carlos Cónsole-Gonella<o:p></o:p></span></h3><h3 style='margin:0cm;line-height:15.0pt'><span style='font-size:10.5pt;font-family:"Segoe UI",sans-serif;font-weight:normal'><a href="https://revista.geologica.org.ar/raga/article/view/215/615"><span style='font-size:10.0pt;color:#007AB2;border:solid #007AB2 1.0pt;padding:0cm;text-decoration:none'>PDF</span></a><o:p></o:p></span></h3><h3 style='margin:0cm;line-height:15.0pt'><span style='font-size:10.5pt;font-family:"Segoe UI",sans-serif'><o:p> </o:p></span></h3><h3 style='margin:0cm;line-height:15.0pt'><span style='font-size:10.5pt;font-family:"Segoe UI",sans-serif'>Sedimentología e icnología del intervalo medio de la Formación Agua del Jagüel, Carbonífero de la Precordillera de Mendoza: implicancias paleoambientales de la transgresión postglacial<o:p></o:p></span></h3><h3 style='margin:0cm;line-height:15.0pt'><span style='font-size:10.0pt;font-family:"Segoe UI",sans-serif;font-weight:normal'>Pablo J Alonso-Muruaga, Carlos O Limarino, Luis A Buatois, Cecilia A Pirrone<o:p></o:p></span></h3><h3 style='margin:0cm;line-height:15.0pt'><span style='font-size:10.5pt;font-family:"Segoe UI",sans-serif;font-weight:normal'><a href="https://revista.geologica.org.ar/raga/article/view/219/616"><span style='font-size:10.0pt;color:#007AB2;border:solid #007AB2 1.0pt;padding:0cm;text-decoration:none'>PDF</span></a><o:p></o:p></span></h3><h3 style='margin:0cm;line-height:15.0pt'><span style='font-size:10.5pt;font-family:"Segoe UI",sans-serif'><o:p> </o:p></span></h3><h3 style='margin:0cm;line-height:15.0pt'><span style='font-size:10.5pt;font-family:"Segoe UI",sans-serif'>Dinosaur tracks at Cañadón de las Campanas and Villa El Chocón area (Late Cretaceous, Candeleros Formation), Patagonia, Argentina<o:p></o:p></span></h3><h3 style='margin:0cm;line-height:15.0pt'><span style='font-size:10.0pt;font-family:"Segoe UI",sans-serif;font-weight:normal'>Verónica Krapovickas , Alberto C Garrido, Juan I Canale<o:p></o:p></span></h3><h3 style='margin:0cm;line-height:15.0pt'><span style='font-size:10.5pt;font-family:"Segoe UI",sans-serif;font-weight:normal'><a href="https://revista.geologica.org.ar/raga/article/view/220/617"><span lang=EN-US style='font-size:10.0pt;color:#007AB2;border:solid #007AB2 1.0pt;padding:0cm;text-decoration:none'>PDF</span></a></span><span lang=EN-US style='font-size:10.5pt;font-family:"Segoe UI",sans-serif;font-weight:normal'><o:p></o:p></span></h3><h3 style='margin:0cm;line-height:15.0pt'><span lang=EN-US style='font-size:10.5pt;font-family:"Segoe UI",sans-serif'><o:p> </o:p></span></h3><h3 style='margin:0cm;line-height:15.0pt'><span lang=EN-US style='font-size:10.5pt;font-family:"Segoe UI",sans-serif'>Trace fossils as tools to unravel oxygen conditions: A case study from Los Molles Formation (Toarcian-lower Callovian)<o:p></o:p></span></h3><h3 style='margin:0cm;line-height:15.0pt'><span style='font-size:10.0pt;font-family:"Segoe UI",sans-serif;font-weight:normal'>Débora Mical Campetella, Noelia Beatriz Carmona, Juan José Ponce, Andreas Wetzel, Maximiliano Rodríguez, Martin Nazareno Parada<o:p></o:p></span></h3><h3 style='margin:0cm;line-height:15.0pt'><span style='font-size:10.5pt;font-family:"Segoe UI",sans-serif;font-weight:normal'><a href="https://revista.geologica.org.ar/raga/article/view/221/618"><span style='font-size:10.0pt;color:#007AB2;border:solid #007AB2 1.0pt;padding:0cm;text-decoration:none'>PDF</span></a><o:p></o:p></span></h3><p class=MsoNormal><o:p> </o:p></p></div></body></html>