Vaca Muerta Shale—Taming a Giant
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Palaxius Chosmalalensis N. Isp., a New Crustacean Microcoprolite from The
Volumen 77 (3): REVISTA DE LA DESARROLLOS RECIENTES EN ICNOLOGÍA ARGENTINA ASOCIACIÓN GEOLÓGICA ARGENTINA www.geologica.org.ar Septiembre 2020 Palaxius chosmalalensis n. isp., a new crustacean microcoprolite from the Lower Cretaceous of Argentina and new criteria for the classification of ichnospecies of Palaxius Diego A. KIETZMANN1,2 and Mariana S. OLIVO1,2 1Universidad de Buenos Aires, Facultad de Ciencias Exactas y Naturales, Departamento de Ciencias Geológicas, Ciudad Autónoma de Buenos Aires. 2CONICET-Universidad de Buenos Aires, Instituto de Geociencias Básicas, Ambientales y Aplicadas de Buenos Aires (IGeBA). Email: [email protected] Editor: Graciela S. Bressan y Diana E. Fernández Recibido: 12 de mayo de 2019 Aceptado: 2 de agosto de 2019 ABSTRACT Crustacean microcoprolites are abundant constituents in the Upper Jurassic–Lower Cretaceous of the Neuquén Basin (Argentina). A new record of these particles is described from the lowermost Olcostephanus (O.) atherstoni ammonite Zone (lower Valanginian) in the Mulichinco Formation at Puerta Curacó section, north of the Neuquén province. Coprolites come from shallow-water oyster-dominated biostromes and belong to a new ichnospecies, Palaxius chosmalalensis n. isp., which was previously described as P. decemlunulatus (Paréjas) from the Upper Cretaceous of Egypt. As a consequence of the description of the new ichnospecies, we propose to incor- porate quantitative criteria regarding the angle with which the canals are oriented, as well as its position with respect to the center of symmetry of the coprolite. Keywords: pellets, Callianassidae, ichnology, Cretaceous. RESUMEN Palaxius chosmalalensis n. isp., un nuevo microcoprolito de crustáceos del Cretácico Inferior de la Cuenca Neuquina, Argen- tina. Los microcoprolitos de crustáceos son constituyentes abundantes en el Jurásico Superior - Cretácico Inferior de la Cuenca Neuquina. -
Maquetación 1
ISSN 2469-0228 www.peapaleontologica.org.ar JURASSIC ORGANIC-WALLED MARINE MICROPLANKTON FROM THE NEUQUÉN BASIN. DISTRIBUTION, BIOSTRATIGRAPHY AND PALEOBIOGEOGRAPHY. A REVIEW MARCELO A. MARTÍNEZ 1,2 DANIELA E. OLIVERA 1,2 1Instituto Geológico del Sur-CONICET/Departamento de Geología (UNS), San Juan 670, B8000ICN Bahía Blanca, Buenos Aires, Argentina. ²Universidad Nacional del Sur, Departamento de Geología, San Juan 670, B8000ICN Bahía Blanca, Buenos Aires, Argentina. Recibido: 29 de abril de 2016 - Aceptado: 25 de noviembre de 2016 Para citar este artículo: Marcelo A. Martínez and Daniela E. Olivera (2016). Jurassic organic-walled marine microplankton from the Neuquén Basin. Distribution, biostratigraphy and paleobiogeography. A review. En: M. Martínez y D. Olivera (Eds.), Pali nología del Meso-Cenozoico de Argentina - Volumen en homenaje a Mirta Elena Quattrocchio. Pub licación Electrónica de la Asociación Paleontológica Argentina 16 (2): 106–128. Link a este artículo: http://dx.doi.org/ 10.5710/PEAPA.25.11.2016.115 DESPLAZARSE HACIA ABAJO PARA ACCEDER AL ARTÍCULO Asociación Paleontológica Argentina Maipú 645 1º piso, C1006ACG, Buenos Aires República Argentina Tel/Fax (54-11) 4326-7563 Web: www.apaleontologica.org.ar Otros artículos en Publicación Electrónica de la APA 16(2): Borromei et al. Deschamps & Tomassini Prieto POSTGLACIAL VEGETATION AND LATE CENOZOIC VERTEBRATES FROM ANÁLISIS E INTERPRETACIÓN DE REGIS- CLIMATE CHANGES INFERRED THE SOUTHERN PAMPEAN REGION: TROS PALINOLÓGICOS DE SUCESIONES FROM A PEAT POLLEN RECORD SYSTEMATIC AND ALUVIALES DE LA REGIÓN PAMPEANA: IN THE RÍO PIPO VALLEY, BIO-CHRONOSTRATIGRAPHIC UPDATE REVISIÓN E IMPLICANCIAS PARA LA SOUTHERN TIERRA DEL FUEGO RECONSTRUCCIÓN DE LA VEGETACIÓN Y EL CLIMA DURANTE EL PLEISTOCENO TARDIO – HOLOCENO Año 2016 - 16(2): 106–128 VOLUMEN TEMÁTICO ISSN 2469-0228 JURAssiC oRGANiC-WAlleD MARiNe MiCRoPlANKToN fRoM The NeUQUÉN BAsiN. -
Bivalvia, Late Jurassic) from South America
Author's personal copy Pala¨ontol Z DOI 10.1007/s12542-016-0310-z RESEARCH PAPER Huncalotis, an enigmatic new pectinoid genus (Bivalvia, Late Jurassic) from South America 1 2 Susana E. Damborenea • He´ctor A. Leanza Received: 29 September 2015 / Accepted: 16 March 2016 Ó Pala¨ontologische Gesellschaft 2016 Abstract The extensive outcrops of the Late Jurassic– orientated at right angles to the shell margins. A few speci- Early Cretaceous Vaca Muerta Formation black shales and mens were found on the outside of large calcareous con- marls in the Neuque´n Basin have yielded very few bivalves, cretions within black shales; these are often articulated, and these are not well known. The material described here complete shells, which preserve the original convexity of the was collected in central Neuque´n, from late Tithonian cal- valves. In some cases these articulated shells seem to be careous levels within the black shales, between beds with associated with large ammonite shells, suggesting an epi- Substeueroceras sp. and with Argentiniceras noduliferum byssate (possibly also pseudoplanktonic) lifestyle. (Steuer). The material is referred to the new genus Huncalotis and to the new species H. millaini. The strongly Keywords Late Tithonian Á Neuque´n Basin Á Vaca inequivalve shells, the ligamental area with a triangular Muerta Formation Á Argentina Á Peru Á Bivalvia Á slightly prosocline resilifer, the right valve with ctenolium Pectinoidea Á Pectinidae and a very deep byssal notch, and the lack of radial orna- mentation make the shell of this new genus strikingly similar Kurzfassung Die reichlich zutage tretenden Schwarz- to the Triassic pectinid Pleuronectites. -
Abelisaurus Comahuensis 321 Acanthodiscus Sp. 60, 64
Index Page numbers in italic denote figure. Page numbers in bold denote tables. Abelisaurus comahuensis 321 structure 45-50 Acanthodiscus sp. 60, 64 Andean Fold and Thrust Belt 37-53 Acantholissonia gerthi 61 tectonic evolution 50-53 aeolian facies tectonic framework 39 Huitrin Formation 145, 151-152, 157 Andes, Neuqu6n 2, 3, 5, 6 Troncoso Member 163-164, 167, 168 morphostructural units 38 aeolian systems, flooded 168, 169, 170, 172, stratigraphy 40 174-182 tectonic evolution, 15-32, 37-39, 51 Aeolosaurus 318 interaction with Neuqu6n Basin 29-30 Aetostreon 200, 305 Andes, topography 37 Afropollis 76 Andesaurus delgadoi 318, 320 Agrio Fold and Thrust Belt 3, 16, 18, 29, 30 andesite 21, 23, 26, 42, 44 development 41 anoxia see dysoxia-anoxia stratigraphy 39-40, 40, 42 Aphrodina 199 structure 39, 42-44, 47 Aphrodina quintucoensis 302 uplift Late Cretaceous 43-44 Aptea notialis 75 Agrio Formation Araucariacites australis 74, 75, 76 ammonite biostratigraphy 58, 61, 63, 65, 66, Araucarioxylon 95,273-276 67 arc morphostructural units 38 bedding cycles 232, 234-247 Arenicolites 193, 196 calcareous nannofossil biostratigraphy 68, 71, Argentiniceras noduliferum 62 72 biozone 58, 61 highstand systems tract 154 Asteriacites 90, 91,270 lithofacies 295,296, 297, 298-302 Asterosoma 86 92 marine facies 142-143, 144, 153 Auca Mahuida volcano 25, 30 organic facies 251-263 Aucasaurus garridoi 321 palaeoecology 310, 311,312 Auquilco evaporites 42 palaeoenvironment 309- 310, 311, Avil6 Member 141,253, 298 312-313 ammonites 66 palynomorph biostratigraphy 74, -
NEUQUÉN BASIN, ARGENTINA Latin American Journal of Sedimentology and Basin Analysis, Vol
Latin American Journal of Sedimentology and Basin Analysis ISSN: 1669-7316 [email protected] Asociación Argentina de Sedimentología Argentina TUNIK, Maisa A.; PAZOS, Pablo J.; IMPICCINI, Agnes; LAZO, Darío; AGUIRRE- URRETA, María Beatriz DOLOMITIZED TIDAL CYCLES IN THE AGUA DE LA MULA MEMBER OF THE AGRIO FORMATION (LOWER CRETACEOUS), NEUQUÉN BASIN, ARGENTINA Latin American Journal of Sedimentology and Basin Analysis, vol. 16, núm. 1, enero-julio, 2009, pp. 29-43 Asociación Argentina de Sedimentología Buenos Aires, Argentina Available in: http://www.redalyc.org/articulo.oa?id=381740363004 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative LATIN AMERICAN JOURNAL OF SEDIMENTOLOGY AND BASIN ANALYSIS | VOL. 16 (1) 2009, 29-43 © Asociación Argentina de Sedimentología - ISSN 1669 7316 DOLOMITIZED TIDAL CYCLES IN THE AGUA DE LA MULA MEMBER OF THE AGRIO FORMATION (LOWER CRETACEOUS), NEUQUÉN BASIN, ARGENTINA Maisa A. TUNIK 1, Pablo J. PAZOS 2, Agnes IMPICCINI 3, Darío LAZO 4 and María Beatriz AGUIRRE-URRETA 4 1Laboratorio de Tectónica Andina, Universidad de Buenos Aires. CONICET. Actualmente en: CIMAR - Universidad Nacional del Comahue. Av. Buenos Aires 1400, Neuquén. Argentina. E-mail: [email protected] 2Universidad de Buenos Aires. Ciudad Universitaria, Pabellón 2, 1428 Buenos Aires. Argentina. 3Universidad Nacional del Comahue, Av. Buenos Aires 1400, Neuquén, Argentina. 4Laboratorio de Bioestratigrafía de Alta Resolución. Universidad de Buenos Aires. Ciudad Universitaria, Pabellón 2, 1428 Buenos Aires. Argentina. Abstract: The Agrio Formation (Valanginian to early Barremian) is a siliciclastic and carbonate unit of the Neuquén Basin in west central Argentina. -
Valanginian Knowles Limestone, East Texas: Biostratigraphy and Potential Hydrocarbon Reservoir 81
A Publication of the Gulf Coast Association of Geological Societies www.gcags.org V K L, E T: B P H R Robert W. Scott Precision Stratigraphy Associates, 149 W. Ridge Rd., Cleveland, Oklahoma 74020–5037, U.S.A. ABSTRACT The Lower Cretaceous Knowles Limestone is the uppermost unit of the Cotton Valley Group in the northeastern Texas Gulf Coast. It is the oldest Cretaceous carbonate shelf deposit that is a prospective reservoir. This shallow shelf-to-ramp shoal- ing-up complex is an arcuate lenticular lithosome that trends from East Texas across northwestern Louisiana. It is up to 330 m (1080 ft) thick and thins both landward and basinward. Landward lagoonal inner ramp facies are mollusk wackestone and peloidal packstone. The thickest buildup facies are coral-chlorophyte-calcimicrobial boundstone and bioclast grainstone, and the basinward facies is pelagic oncolite wackestone. The base of the Knowles is apparently conformable with the Bossier/Hico dark gray shale. The top contact in East Texas is disconformable with the overlying Travis Peak/Hosston formations. Porosity resulted from successive diagenetic stages including early marine fringing cements, dissolution of aragonitic bioclasts, micrite encrustation, later mosaic cement, and local fine crystalline dolomitization. The age of the Knowles Limestone is early Valanginian based on a calpionellid-calcareous dinoflagellate-calcareous nan- nofossil assemblage in the lower part and a coral-stromatoporoid assemblage in its upper part. The intra-Valanginian hiatus represented by the Knowles/Travis Peak unconformity correlates with the Valanginian “Weissert” oceanic anoxic event. Possi- bly organic-rich source rocks were deposited downdip during that oceanic low-oxygen event. -
(Bivalvia) in the Transition Between the Vaca Muerta and Mulichinco Formations, Early Valanginian, Neuquén Basin, Argentina
AMEGHINIANA - 2012 - Tomo 49 (1): 96 – 117 ISSN 0002-7014 THE GENUS STEINMANELLA CRICKMAY (BIVALVIA) IN THE TRANSITION BETWEEN THE VACA MUERTA AND MULICHINCO FORMATIONS, EARLY VALANGINIAN, NEUQUÉN BASIN, ARGENTINA LETICIA LUCI and DARÍO GUSTAVO LAZO Instituto de Estudios Andinos “Don Pablo Groeber”, Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Ciudad Universitaria, Pabellón II, C1428EGA Buenos Aires, Argentina – Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET). [email protected]; [email protected] Abstract. The genus Steinmanella Crickmay is recorded in several Lower Cretaceous marine units of the Neuquén Basin. It is particularly abundant at the transition between the Vaca Muerta and Mulichinco formations. This paper presents a taxonomic revision of this fauna, discusses the stratigraphic range of each species, and describes and interprets the associated lithofacies based on detailed field sections, newly collected specimens and revision of previous fossil collections. Four sections were measured in northern Neuquén comprising the upper beds of the Vaca Muerta Formation and the lower ones of the Mulichinco Formation. The Steinmanella fauna was dated accurately on the basis of a precise ammonoid zonation. The species were found in the Neocomites wichmanni and Lissonia riveroi zones of early Valanginian age. Specimens were collected in situ from dark grey shales, alternating siltstones, wackestones and mudstones, and rudstones. Three species were identified: Steinmanella curacoensis (Weaver), S. quintucoensis (Weaver), and S. subquadrata sp. nov. Steinmanella curacoensis has an oval outline, poor demarcation of carinae, flank and corselet ribs partially intercalated at the median part of the valve, and oval escutcheon. -
RESEARCH Triassic to Neogene Evolution of the South-Central Andean Arc Determined by Detrital Zircon U-Pb and Hf Analysis Of
RESEARCH Triassic to Neogene evolution of the south-central Andean arc determined by detrital zircon U-Pb and Hf analysis of Neuquén Basin strata, central Argentina (34°S–40°S) Elizabeth A. Balgord* DEPARTMENT OF GEOSCIENCES, UNIVERSITY OF ARIZONA, 1040 4TH STREET, TUCSON, ARIZONA 85721, USA ABSTRACT The Andes Mountains provide an ideal natural laboratory to analyze the relationship between the tectonic evolution of a subduction margin, basin morphology, and volcanic activity. Magmatic output rates in Cordilleran-style orogenic systems vary through time and are character- ized by high-flux magmatic events alternating with periods of low or no activity. The Neuquén Basin (34°S–40°S) of south-central Argentina is in a retroarc position and provides a geological record of sedimentation in variable tectonic settings. Strata ranging in age from Middle Jurassic to Neogene were sampled and analyzed to determine their detrital zircon U-Pb age spectra and Hf isotopic composition. When all detrital zircon data are combined, results indicate that significant pulses in magmatic activity occurred from 190 to 145 Ma, and at 129 Ma, 110 Ma, 67 Ma, 52 Ma, 16 Ma, and 7 Ma. The εHf values were highly evolved when the arc initiated at 190 Ma and transitioned into intermediate and juvenile values between ca. 160 and 150 Ma. There was a large shift toward more juvenile Hf isotopic values at 16 Ma that is consistent with renewed extension in the backarc during the Neogene. Overall geochemical trends in the Neuquén Basin section of the Andean arc are different from those observed in the central (21°S–26°S) and southern Andean arc (41°S–46°S), suggesting a segmented margin with vari- able tectonic settings and arc processes controlling magmatic output and chemistry along strike. -
An Early Cretaceous Astropectinid (Echinodermata, Asteroidea)
Andean Geology 41 (1): 210-223. January, 2014 Andean Geology doi: 10.5027/andgeoV41n1-a0810.5027/andgeoV40n2-a?? formerly Revista Geológica de Chile www.andeangeology.cl An Early Cretaceous astropectinid (Echinodermata, Asteroidea) from Patagonia (Argentina): A new species and the oldest record of the family for the Southern Hemisphere Diana E. Fernández1, Damián E. Pérez2, Leticia Luci1, Martín A. Carrizo2 1 Instituto de Estudios Andinos Don Pablo Groeber (IDEAN-CONICET), Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Intendente Güiraldes 2160, Pabellón 2, Ciudad Universitaria, Ciudad Autónoma de Buenos Aires, Argentina. [email protected]; [email protected] 2 Museo de Ciencias Naturales Bernardino Rivadavia, Ángel Gallardo 470, Ciudad Autónoma de Buenos Aires, Argentina. [email protected]; [email protected] ABSTRACT. 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, infero- marginals (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). -
Taphonomy of Decapod-Bearing Concretions and Their Associated
Volumen 77 (3): REVISTA DE LA DESARROLLOS RECIENTES EN ICNOLOGÍA ARGENTINA ASOCIACIÓN GEOLÓGICA ARGENTINA www.geologica.org.ar Septiembre 2020 Taphonomy of decapod-bearing concretions and their associated trace fossils from the Agrio Formation (Lower Cretaceous, Neuquén Basin), with paleobiological implications for axiid shrimps A. Mariel ANDRADA1, Graciela S. BRESSAN1,2 and Darío G. LAZO1,2 1Instituto de Estudios Andinos “Don Pablo Groeber”, Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires. 2CONICET E-mails: [email protected], [email protected], [email protected] Editor: Diana E. Fernández Recibido: 7 de julio de 2020 Aceptado: 14 de septiembre de 2020 ABSTRACT A total of 22 concretions containing 37 decapod crustacean specimens belonging to the family Axiidae, from the Hauterivian (Lower Cretaceous) of the Agrio Formation in the Neuquén Basin, were studied. The decapods were assigned to Protaxius sp., which likely had a fossorial life habit. In this work we attempt to determine, through taphonomic analysis, if the specimens fossilized within their burrows or outside them in order to interpret paleobiological aspects of the studied taxon. Several taphonomic criteria of the specimens and concretions, known from the literature, were applied and their utility discussed, including anatomical disposition, completeness of specimens, orientation and alignment, dispersion of exoskeletal elements in the concretion, preservation of both chelae, sedimentary fabric of the concretion, position within the concretion, and shape of the concretions. The relative importance of these criteria was discussed especially in those concretions with conflicting evidence pointing to either fossilization within or outside burrow systems. -
MESOZOIC TECTONIC INVERSION in the NEUQUÉN BASIN of WEST-CENTRAL ARGENTINA a Dissertation by GABRIEL ORLANDO GRIMALDI CASTRO Su
MESOZOIC TECTONIC INVERSION IN THE NEUQUÉN BASIN OF WEST-CENTRAL ARGENTINA A Dissertation by GABRIEL ORLANDO GRIMALDI CASTRO Submitted to the Office of Graduate Studies of Texas A&M University in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY December 2005 Major Subject: Geology MESOZOIC TECTONIC INVERSION IN THE NEUQUÉN BASIN OF WEST-CENTRAL ARGENTINA A Dissertation by GABRIEL ORLANDO GRIMALDI CASTRO Submitted to the Office of Graduate Studies of Texas A&M University in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY Approved by: Chair of Committee, Steven L. Dorobek Committee Members, Philip D. Rabinowitz Niall C. Slowey Brian J. Willis David V. Wiltschko Head of Department, Richard L. Carlson December 2005 Major Subject: Geology iii ABSTRACT Mesozoic Tectonic Inversion in the Neuquén Basin of West-Central Argentina. (December 2005) Gabriel Orlando Grimaldi Castro, B.S., Universidad Nacional de Córdoba, Argentina; M.S., Texas A&M University Chair of Advisory Committee: Dr. Steven L. Dorobek Mesozoic tectonic inversion in the Neuquén Basin of west-central Argentina produced two main fault systems: (1) deep faults that affected basement and syn-rift strata where preexisting faults were selectively reactivated during inversion based on their length and (2) shallow faults that affected post-rift and syn-inversion strata. Normal faults formed at high angle to the reactivated half-graben bounding fault as a result of hangingwall expansion and internal deformation as it accommodated to the shape of the curved footwall during oblique inversion. Contraction during inversion was initially accommodated by folding and internal deformation of syn-rift sedimentary wedges, followed by displacement along half-graben bounding faults. -
U-Pb Geochronology and Paleogeography of the Valanginian– Hauterivian Neuquén Basin: Implications for Gondwana-Scale
Research Paper GEOSPHERE U-Pb geochronology and paleogeography of the Valanginian– Hauterivian Neuquén Basin: Implications for Gondwana-scale GEOSPHERE, v. 17, no. 1 source areas https://doi.org/10.1130/GES02284.1 E. Schwarz1,*, E.S. Finzel2,*, G.D. Veiga1, C.W. Rapela1, C. Echevarria3,*, and L.A. Spalletti1 1Centro de Investigaciones Geológicas (Universidad Nacional de La Plata–Consejo Nacional de Investigaciones Científicas y Técnicas [CONICET]), Diagonal 113 #256 B1904DPK, La Plata, Argentina 13 figures; 2 tables; 1 set of supplemental files 2Earth and Environmental Science Department, University of Iowa, 115 Trowbridge Hall, Iowa City, Iowa 52242, USA 3Pampa Energía S.A. Gerencia Tight, Dirección de E&P, J.J. Lastra 6000, 8300 Neuquén, Argentina CORRESPONDENCE: [email protected] ABSTRACT starting in the mid-continent region of south- Early Cretaceous was the Neuquén Basin, which CITATION: Schwarz, E., Finzel, E.S., Veiga, G.D., western Gondwana and by effective sorting, was during that time was a backarc basin separated Rapela, C.W., Echevarria, C., and Spalletti, L.A., Sedimentary basins located at the margins bringing fine-grained or finer caliber sand to the from the proto–Pacific Ocean (i.e., to the west) by 2021, U-Pb geochronology and paleogeography of the of continents act as the final base level for con- Neuquén Basin shoreline. This delivery system was a discontinuous volcanic arc (Howell et al., 2005). Valanginian–Hauterivian Neuquén Basin: Implications for Gondwana-scale source areas: Geosphere, v. 17, tinental-scale catchments that are sometimes probably active (though not necessarily continu- This marine basin was bounded by the Sierra no.