Atualização da informação geológica e estratigráfica das jazidas de dinossáurios de La Rioja. Paleodiversidade do Cretácico Inferior do Grupo Enciso em Peña Cárcena (Igea, Espanha)

ABSTRACT: The discovery of new vertebrate fossil sites with skeletal remains in the Enciso Group of Igea (La Rioja) is showing the relevance of the area to study the palaeobiodiversity of Early Cretaceous vertebrate faunas from the Iberian Peninsula. At Peña Cárcena hill two sedimentary environments have been inferred: a mixed siliciclastic-carbonate lacustrine environment that is dominant at the outcrops, overlaid by a splay delta in an avulsion-belt. The vertebrate remains are especially abundant in the mixed siliciclastic-carbonate lacustrine deposits with two partially articulated skeletons (a theropod and a large-sized dinosaur), teeth and a fragment of a left maxilla of baryonychines, a pterosaur tooth that differs from those of Prejanopterus, a Goniopholis tooth, chelonian shell fragments that might belong to Camerochelys, a fairly complete lepisosteiform, teeth and dorsal fin spines of hybodontiforms. At the delta deposits, vertebrate fossils are rather scarce, with a single lepisosteiform skeleton and indeterminate bone fragments.RESUMO: A descoberta de novas jazidas com restos osteológicos de vertebrados no Grupo Enciso em Igea (La Rioja) comprova a importância da região para o estudo da paleobiodiversidade das faunas de vertebrados do Cretácico Inferior da Península Ibérica. Na colina de Peña-Cárcena, tem-se inferido dois ambientes sedimentares: o predominante nos afloramentos corresponde a um ambiente lacustre, siliciclástico-carbonatado misto, que se encontra sobreposto por depósitos de transbordo deltaico em cinturão abandonado. Restos de vertebrados são abundantes nos depósitos lacustres, incluindo dois esqueletos parciais articulados (de um terópode e de outro dinossáurio de grande porte), dentes e um fragmento de maxila esquerda de barionicinos, um dente de pterossáurio distinto de Prejanopterus, um dente de Goniopholis, fragmentos da carapaça de quelónios que poderão pertencer a Camerochelys, um lepisosteiforme praticamente completo, dentes e espinhos de barbatanas de hybodontiformes. Fósseis de vertebrados são escassos nos depósitos deltaicos, com apenas um esqueleto de lepisosteiforme e fragmentos indeterminados.info:eu-repo/semantics/publishedVersio

El registro fósil de vertebrados y patrimonio paleontológico más representativo de los pirineos occidentales

Los Pirineos occidentales son un territorio con una notable diversidad geológica y un importante registro fósil, que constituye un gran archivo de paleobiodiversidad. En lo que respecta al registro fósil de vertebrados, los Pirineos occidentales (Región Vasco-Cantábrica, Cuenca de Pamplona y sector noroccidental de la Cuenca del Ebro) son relevantes tanto desde el punto de vista de los yacimientos paleontológicos como de las colecciones de fósiles procedentes de ellos. Varios yacimientos de vertebrados forman parte del Inventario de Lugares de Interés Geológico (LIG) con alto o muy alto interés paleontológico en la Comunidad Autónoma del País Vasco. Destacan los yacimientos de peces cretácicos de Zeanuri en Bizkaia, mamíferos eocenos de Zambrana e icnitas miocenas de Salinas de Añana en Álava/Araba y la asociación de vertebrados pleistocenos de Kiputz cerca de Mutriku, en Gipuzkoa. Otros yacimientos notables en el área de estudio deberían ser objeto de iniciativas de geoconservación: es el caso de la cantera de Laño (Condado de Treviño), con asociaciones fi nicretácicas de vertebrados continentales y marinos, los afloramientos con icnitas de aves y mamíferos del Eoceno al Mioceno inferior de Navarra/Nafarroa y la cueva vizcaína de Santa Isabel de Ranero (Pleistoceno), por citar únicamente los ejemplos más sobresalientes. Asimismo, existen colecciones de fósiles de vertebrados en los Pirineos occidentales que destacan por su elevado interés paleontológico, aunque algunos no provengan de LIG reconocidos. Estas colecciones están depositadas en diversos centros e instituciones de Bilbao, Irún, Leioa, Pamplona-Iruñea, y Vitoria-Gasteiz. La valoración de la paleobiodiversidad y el registro fósil es un paso importante para el conocimiento del patrimonio paleontológico de un territorio y la creación de fi guras de geoconservación (e.g., LIG, geosites). Sin embargo, la mera inclusión de los yacimientos paleontológicos en estas fi guras no garantiza su protección y conservación, ni la adecuada gestión de las colecciones de fósiles procedentes de ellos. Por lo tanto, es necesario diseñar estrategias de conservación transversales teniendo en cuenta las particularidades de cada yacimiento y/o colección. La divulgación científi ca y cultural del patrimonio paleontológico de un territorio, como el aquí estudiado, debe contar con una mayor colaboración entre los paleontólogos que han valorado los bienes paleontológicos y los técnicos que los gestionan. Para ello, es necesaria la disposición de partidas presupuestarias específicas que posibiliten el desarrollo de diferentes acciones encaminadas a la investigación, conservación y difusión social de este patrimonio.The western Pyrenees is a territory with a remarkable geodiversity and an important fossil record, which constitutes a large archive of palaeobiodiversity. With respect to the vertebrate fossil record, the western Pyrenees (Basque-Cantabrian Region, Pamplona Basin and the north-western sector of the Ebro Basin) are relevant both from the point of view of palaeontological sites and fossil collections. Several vertebrate fossil sites are integrated into the Inventory of Geological Interest Sites (LIG) with high to very high palaeontological interest of the Autonomous Community of the Basque Country. It is worth highlighting the Cretaceous fish sites of Zeanuri in Biscay, Eocene mammals of Zambrana and Miocene ichnites of Salinas de Añana in Araba, and the Pleistocene vertebrate fossil assemblage of Kiputz near Mutriku, in Gipuzkoa. Other highly significant sites in the study area should be subject to geoconservation initiatives. This is the case of the Laño quarry in the Condado de Treviño, which has provided continental and marine vertebrate fossil assemblages from the latest Cretaceous, Eocene to Early Miocene sites with bird and mammal tracks in Navarre, and the Pleistocene cave deposits of Santa Isabel de Ranero in Biscay, to mention only the most outstanding examples. There are also vertebrate fossil collections in the western Pyrenees that stand out for their high palaeontological interest, although some do not come from recognized LIG. These collections are deposited in several centres and institutions of Bilbao, Irun, Leioa, Pamplona-Iruñea and Vitoria-Gasteiz. The valuation of the palaeobiodiversity and fossil record is an important step for the study of palaeontological heritage of a territory and the set-up of geoconservation designations (e.g., LIG, geosites). However, the mere inclusion of the palaeontological assents in these geoconservation designations does not guarantee either their protection and conservation or the suitable management of the fossil collection. Therefore, it is necessary to design conservation strategies taking into account the particularities of each palaeontological site and/or fossil collection. The scientific and cultural dissemination of the palaeontological heritage of a territory like one studied here should have greater collaboration between the palaeontologists that have valued the palaeontological assets and the technicians and institutions that manage them. This requires the provision of specific budgetary items that enable the development of the different activities of research, conservation and social dissemination of this heritage.Fil: Badiola, Ainara. Universidad del País Vasco; EspañaFil: Arlegi, Mikel. Universidad del País Vasco; España. Université de Bordeaux; FranciaFil: Astibia, Humberto. Universidad del País Vasco; EspañaFil: Bardet, Nathalie. Centre National de la Recherche Scientifique; Francia. Muséum National d'Histoire Naturelle; Francia. Université Pierre et Marie Curie; FranciaFil: Berreteaga, Ana. Universidad del País Vasco; EspañaFil: Corral, J. Carmelo. Museo de Ciencias Naturales de Álava/; EspañaFil: Díaz Martínez, Ignacio. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigación en Paleobiología y Geología; Argentina. Universidad Nacional de Río Negro. Sede Alto Valle. Instituto de Investigaciones en Paleobiología y Geología; ArgentinaFil: Gómez Olivencia, Asier. Universidad del País Vasco; España. IKERBASQUE. Basque Foundation for Science; España. Universidad Carlos III de Madrid. Instituto de Salud; EspañaFil: Lopez Horgue, Mikel A.. Universidad del País Vasco; EspañaFil: Perales Gogenola, Leire. Universidad del País Vasco; EspañaFil: Pereda Suberbiola, Xabier. Universidad del País Vasco; Españ

Coralline Algae in a Changing Mediterranean Sea: How Can We Predict Their Future, if We Do Not Know Their Present?

In this review we assess the state of knowledge for the coralline algae of the Mediterranean Sea, a group of calcareous seaweeds imperfectly known and considered highly vulnerable to long-term climate change. Corallines have occurred in the Mediterranean area for ∼140 My and are well-represented in the subsequent fossil record; for some species currently common the fossil documentation dates back to the Oligocene, with a major role in the sedimentary record of some areas. Some Mediterranean corallines are key ecosystem engineers that produce or consolidate biogenic habitats (e.g., coralligenous concretions, Lithophyllum byssoides rims, rims of articulated corallines, maerl/rhodolith beds). Although bioconstructions built by corallines exist virtually in every sea, in the Mediterranean they reach a particularly high spatial and bathymetric extent (coralligenous concretions alone are estimated to exceed 2,700 km2 in surface). Overall, composition, dynamics and responses to human disturbances of coralline-dominated communities have been well-studied; except for a few species, however, the biology of Mediterranean corallines is poorly known. In terms of diversity, 60 species of corallines are currently reported from the Mediterranean. This number, however, is based on morphological assessments and recent studies incorporating molecular data suggest that the correct estimate is probably much higher. The responses of Mediterranean corallines to climate change have been the subject of several recent studies that documented their tolerance/sensitivity to elevated temperatures and pCO2. These investigations have focused on a few species and should be extended to a wider taxonomic set

Tectonic lowstand wedges of a carbonate platform-basin transition (Lower Albian of Lanestosa, N Spain)

Lopez-Horgue M., Garcia-Mondejar J., Fernandez-Mendiola P.A. Tectonic lowstand wedges of a carbonate platform-basin transition (Lower Albian of Lanestosa, N Spain). In: Géologie Méditerranéenne. Tome 21, numéro 3-4, 1994. Perimediterranean carbonate platforms. First International Meeting. Marseille – France (5-8 septembre 1994) sous la direction de Jean-Pierre Masse. pp. 105-107

Distributions of C-22-C-30 even-carbon-number n-alkanes in ocean anoxic event 1 samples from the Basque-Cantabrian Basin

The Ocean Anoxic Event 1 (OAE-1) in central sites of the Basque-Cantabrian Basin exhibits very reducing depositional conditions of sedimentation. These sedimentation events have left a distinct mixture of hydrocarbons that are represented by C22-C30 n-alkanes with a predominance of the even-carbon-number homologues, high relative proportions of squalane and C16-C24 n-alkylcyclopentanes predominated by n-undecyl-, n-tridecyl- and n-pentadecylcyclopentane. Other minor compounds encompass a series of C18-C21 n-alkylcyclohexanes and C18-C24 dimethyl n-alkylcyclohexanes maximized by the even-carbon-number homologues as well as iso- and anteiso-alkanes. This unusual distribution of n-alkanes in this environment provides a new case for comparison with previously reported hypersaline and phosphorite sedimentary deposits where the occurrence of similar n-alkane distributions was reported. In the present case, these major n-alkanes and squalane are indicative of transformation under strong reducing conditions. In contrast, the occurrence of the alkylcyclopentanes, irrespective of the presence of even-carbon-number n-alkanes or squalane, suggests that reductive cyclization of fatty acids is less dependent on strong reducing conditions

Distributions of C-22-C-30 even-carbon-number n-alkanes in ocean anoxic event 1 samples from the Basque-Cantabrian Basin

The Ocean Anoxic Event 1 (OAE-1) in central sites of the Basque-Cantabrian Basin exhibits very reducing depositional conditions of sedimentation. These sedimentation events have left a distinct mixture of hydrocarbons that are represented by C22-C30 n-alkanes with a predominance of the even-carbon-number homologues, high relative proportions of squalane and C16-C24 n-alkylcyclopentanes predominated by n-undecyl-, n-tridecyl- and n-pentadecylcyclopentane. Other minor compounds encompass a series of C18-C21 n-alkylcyclohexanes and C18-C24 dimethyl n-alkylcyclohexanes maximized by the even-carbon-number homologues as well as iso- and anteiso-alkanes. This unusual distribution of n-alkanes in this environment provides a new case for comparison with previously reported hypersaline and phosphorite sedimentary deposits where the occurrence of similar n-alkane distributions was reported. In the present case, these major n-alkanes and squalane are indicative of transformation under strong reducing conditions. In contrast, the occurrence of the alkylcyclopentanes, irrespective of the presence of even-carbon-number n-alkanes or squalane, suggests that reductive cyclization of fatty acids is less dependent on strong reducing conditions

Report on the 7th International Meeting of the IUGS Lower Cretaceous Ammonite Working Group, the Kilian Group (Warsaw, Poland, 21st August 2022): state of the art on the current Standard Ammonite Zonation of the Western Tethyan Mediterranean Province

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