Permophiles Issue #68 January 2020
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First Report of Swimming Trace Fossils of Fish from the Upper Permian and Lower Triassic of the Dolomites (Italy)
Annales Societatis Geologorum Poloniae (2018), vol. 88: ...–... doi: https://doi.org/10.14241/asgp.2018.013 FIRST REPORT OF SWIMMING TRACE FOSSILS OF FISH FROM THE UPPER PERMIAN AND LOWER TRIASSIC OF THE DOLOMITES (ITALY) Ausonio RONCHI1, Giuseppe SANTI1, Lorenzo MARCHETTI 2, Massimo BERNARDI 3 & Piero GIANOLLA4 1 Dipartimento di Scienze della Terra e dell’Ambiente, University of Pavia, Italy; e-mails: [email protected]; [email protected] 2 Urweltmuseum GEOSKOP/Burg Lichtenberg (Pfalz), Thallichtenberg, Germany; e-mail: [email protected] 3 MUSE – Museo delle Scienze, Trento, Italy; e-mail: [email protected] 4 Dipartimento di Fisica e Scienze della Terra, University of Ferrara, Italy; e-mail: [email protected] Ronchi, A., Santi, G., Marchetti, L, Bernardi, M. & Gianolla, R., 2018. First report of swimming trace fossils of fish from the Upper Permian and Lower Triassic of the Dolomites (Italy). Annales Societatis Geologorum Poloniae, 88: xxx-xxx Abstract: In the Upper Permian continental to marginal-marine succession of the Southern Alps (Dolomites, north Italy), the ichnological record consists of diverse vertebrate footprints and non-diverse invertebrate trace fossils, mainly occurring in the “Bletterbach ichnoassociation” of the Val Gardena Sandstone Formation. After the Perm- ian-Triassic Boundary event, vertebrate ichnoassociations are scarce until the Middle Triassic (Anisian), whereas the uppermost Permian–Lower Triassic Werfen Formation preserves a rich invertebrate trace-fossil record. To date, fish body and trace fossils (Undichna) are very rare in the pre- and post-extinction deposits of the Dolomites; only Undichna gosiutensis Gibert, 2001 was identified in the “Voltago Conglomerate” (Middle Anisian), whereas some unidentified fossil fish casts were found in the Permian Val Gardena Sandstone and some fish remains in the overlying Werfen Formation. -
Analysis of Accumulation Models of Middle Permian in Northwest Sichuan Basin
EARTH SCIENCES RESEARCH JOURNAL GEOLOGY Earth Sci. Res. J. Vol. 24, No. 4 (December, 2020): 419-428 Analysis of accumulation models of middle Permian in Northwest Sichuan Basin Bin Li1,2,*, Qiqi Li3, Wenhua Mei2, Qingong Zhuo4, Xuesong Lu4 1State Key Laboratory of Shale Oil and Gas Enrichment Mechanisms and Effective Development, Wuxi, 214126 2School of Geoscience and Technology, Southwest Petroleum University, Chengdu, 610500 3School of Earth Resources, China University of Geosciences, Wuhan, 430074; 4PetroChina Research Institute of Petroleum Exploration and Development, Beijing 100083, China *Corresponding author: [email protected] ABSTRACT Keywords: Northwest of Sichuan Basin; Great progress has been made in middle Permian exploration in Northwest Sichuan in recent years, but there are still Structure Evolution of Foreland Basin; Middle many questions in understanding the hydrocarbon accumulation conditions. Due to the abundance of source rocks and Permian; Paleozoic; Accumulation conditions; the multi-term tectonic movements in this area, the hydrocarbon accumulation model is relatively complex, which has Accumulation Model. become the main problem to be solved urgently in oil and gas exploration. Based on the different tectonic backgrounds of the middle Permian in northwest Sichuan Basin, the thrust nappe belt, the hidden front belt, and the depression belt are taken as the research units to comb and compare the geologic conditions of the middle Permian reservoir. The evaluation of source rocks and the comparison of hydrocarbon sources suggest that the middle Permian hydrocarbon mainly comes from the bottom of the lower Cambrian and middle Permian, and the foreland orogeny promoted the thermal evolution of Paleozoic source rocks in northwest Sichuan to high maturity and over maturity stage. -
GUIDEBOOK the Mid-Triassic Muschelkalk in Southern Poland: Shallow-Marine Carbonate Sedimentation in a Tectonically Active Basin
31st IAS Meeting of Sedimentology Kraków 2015 GUIDEBOOK The Mid-Triassic Muschelkalk in southern Poland: shallow-marine carbonate sedimentation in a tectonically active basin Guide to field trip B5 • 26–27 June 2015 Joachim Szulc, Michał Matysik, Hans Hagdorn 31st IAS Meeting of Sedimentology INTERNATIONAL ASSOCIATION Kraków, Poland • June 2015 OF SEDIMENTOLOGISTS 225 Guide to field trip B5 (26–27 June 2015) The Mid-Triassic Muschelkalk in southern Poland: shallow-marine carbonate sedimentation in a tectonically active basin Joachim Szulc1, Michał Matysik2, Hans Hagdorn3 1Institute of Geological Sciences, Jagiellonian University, Kraków, Poland ([email protected]) 2Natural History Museum of Denmark, University of Copenhagen, Denmark ([email protected]) 3Muschelkalk Musem, Ingelfingen, Germany (encrinus@hagdorn-ingelfingen) Route (Fig. 1): From Kraków we take motorway (Żyglin quarry, stop B5.3). From Żyglin we drive by A4 west to Chrzanów; we leave it for road 781 to Płaza road 908 to Tarnowskie Góry then to NW by road 11 to (Kans-Pol quarry, stop B5.1). From Płaza we return to Tworog. From Tworog west by road 907 to Toszek and A4, continue west to Mysłowice and leave for road A1 then west by road 94 to Strzelce Opolskie. From Strzelce to Siewierz (GZD quarry, stop B5.2). From Siewierz Opolskie we take road 409 to Kalinów and then turn we drive A1 south to Podskale cross where we leave south onto a local road to Góra Sw. Anny (accomoda- for S1 westbound to Pyrzowice and then by road 78 to tion). From Góra św. Anny we drive north by a local road Niezdara. -
Invertebrate Ichnofossils from the Adamantina Formation (Bauru Basin, Late Cretaceous), Brazil
Rev. bras. paleontol. 9(2):211-220, Maio/Agosto 2006 © 2006 by the Sociedade Brasileira de Paleontologia INVERTEBRATE ICHNOFOSSILS FROM THE ADAMANTINA FORMATION (BAURU BASIN, LATE CRETACEOUS), BRAZIL ANTONIO CARLOS SEQUEIRA FERNANDES Departamento de Geologia e Paleontologia, Museu Nacional, UFRJ, Quinta da Boa Vista, São Cristóvão, 20940-040, Rio de Janeiro, RJ, Brazil. [email protected] ISMAR DE SOUZA CARVALHO Departamento de Geologia, Instituto de Geociências, UFRJ, 21949-900, Cidade Universitária, Rio de Janeiro, RJ, Brazil. [email protected] ABSTRACT – The Bauru Group is a sequence at least 300 m in thickness, of Cretaceous age (Turonian- Maastrichtian), located in southeastern Brazil (Bauru Basin), and consists of three formations, namely Adamantina, Uberaba and Marília. Throughout the Upper Cretaceous, there was an alternation between severely hot dry and rainy seasons, and a diverse fauna and flora was established in the basin. The ichnofossils studied were found in the Adamantina Formation outcrops and were identified as Arenicolites isp., ?Macanopsis isp., Palaeophycus heberti and Taenidium barretti, which reveal the burrowing behavior of the endobenthic invertebrates. There are also other biogenic structures such as plant root traces, coprolites and vertebrate fossil egg nests. The Adamantina Formation (Turonian-Santonian) is a sequence of fine sandstones, mudstones, siltstones and muddy sandstones, whose sediments are interpreted as deposited in exposed channel-bars and floodplains associated areas of braided fluvial environments. Key words: Bauru Basin, ichnofossils, late Cretaceous, continental palaeoenvironments, Adamantina Formation. RESUMO – O Grupo Bauru é uma seqüência de pelo menos 300 m de espessura, de idade cretácica (Turoniano- Maastrichtiano), localizada no Sudeste do Brasil (bacia Bauru), e consiste das formações Adamantina, Uberaba e Marília. -
ABSTRACTS BOOK Proof 03
1st – 15th December ! 1st International Meeting of Early-stage Researchers in Paleontology / XIV Encuentro de Jóvenes Investigadores en Paleontología st (1December IMERP 1-stXIV-15th EJIP), 2018 BOOK OF ABSTRACTS Palaeontology in the virtual era 4 1st – 15th December ! Ist Palaeontological Virtual Congress. Book of abstracts. Palaeontology in a virtual era. From an original idea of Vicente D. Crespo. Published by Vicente D. Crespo, Esther Manzanares, Rafael Marquina-Blasco, Maite Suñer, José Luis Herráiz, Arturo Gamonal, Fernando Antonio M. Arnal, Humberto G. Ferrón, Francesc Gascó and Carlos Martínez-Pérez. Layout: Maite Suñer. Conference logo: Hugo Salais. ISBN: 978-84-09-07386-3 5 1st – 15th December ! Palaeontology in the virtual era BOOK OF ABSTRACTS 6 4 PRESENTATION The 1st Palaeontological Virtual Congress (1st PVC) is just the natural consequence of the evolution of our surrounding world, with the emergence of new technologies that allow a wide range of communication possibilities. Within this context, the 1st PVC represents the frst attempt in palaeontology to take advantage of these new possibilites being the frst international palaeontology congress developed in a virtual environment. This online congress is pioneer in palaeontology, offering an exclusively virtual-developed environment to researchers all around the globe. The simplicity of this new format, giving international projection to the palaeontological research carried out by groups with limited economic resources (expensive registration fees, travel, accomodation and maintenance expenses), is one of our main achievements. This new format combines the benefts of traditional meetings (i.e., providing a forum for discussion, including guest lectures, feld trips or the production of an abstract book) with the advantages of the online platforms, which allow to reach a high number of researchers along the world, promoting the participation of palaeontologists from developing countries. -
Using Volcaniclastic Rocks to Constrain Sedimentation Ages
Using volcaniclastic rocks to constrain sedimentation ages: To what extent are volcanism and sedimentation synchronous? Camille Rossignol, Erwan Hallot, Sylvie Bourquin, Marc Poujol, Marc Jolivet, Pierre Pellenard, Céline Ducassou, Thierry Nalpas, Gloria Heilbronn, Jianxin Yu, et al. To cite this version: Camille Rossignol, Erwan Hallot, Sylvie Bourquin, Marc Poujol, Marc Jolivet, et al.. Using vol- caniclastic rocks to constrain sedimentation ages: To what extent are volcanism and sedimentation synchronous?. Sedimentary Geology, Elsevier, 2019, 381, pp.46-64. 10.1016/j.sedgeo.2018.12.010. insu-01968102 HAL Id: insu-01968102 https://hal-insu.archives-ouvertes.fr/insu-01968102 Submitted on 2 Jan 2019 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Accepted Manuscript Using volcaniclastic rocks to constrain sedimentation ages: To what extent are volcanism and sedimentation synchronous? Camille Rossignol, Erwan Hallot, Sylvie Bourquin, Marc Poujol, Marc Jolivet, Pierre Pellenard, Céline Ducassou, Thierry Nalpas, Gloria Heilbronn, Jianxin Yu, Marie-Pierre -
Organic Geochemistry and Element Distribution in Coals Formed in Eocene Lagoon Facies from the Eastern Black Sea Region, NE Turkey
Turkish Journal of Earth Sciences Turkish J Earth Sci (2016) 25: 467-489 http://journals.tubitak.gov.tr/earth/ © TÜBİTAK Research Article doi:10.3906/yer-1512-12 Organic geochemistry and element distribution in coals formed in Eocene lagoon facies from the Eastern Black Sea Region, NE Turkey Çiğdem SAYDAM EKER*, İbrahim AKPINAR, Ferkan SİPAHİ Department of Geology, Faculty of Engineering, Gümüşhane University, Gümüşhane, Turkey Received: 17.12.2015 Accepted/Published Online: 28.06.2016 Final Version: 24.10.2016 Abstract: The amount and type, the inorganic element content, and the maturity of organic materials of Eocene coals, shaly coals, and coaly shales exposed in the Gümüşhane and Bayburt districts of the Eastern Black Sea Region of Turkey were investigated. The depositional environments and hydrocarbon potentials were also interpreted. The total organic carbon concentrations in the studied samples ranged from 0.50% to 63.08%. The samples from Özyurt, Kayadibi, and Tarhanas contained types II and III kerogen, and those from Sökmen and Manas contained type III kerogen. The samples contained Co, Cs, Ga, Hf, Th, U, Y, Mo, Be, Cd, Sb, and La, with average values similar to those of standard brown coals. The samples showed average contents of Co, Ga, Nb, Rb, V, Y, Cu, Pb, Zn, As, Be, and Se, similar to those of other Turkish coals. The sediment source of Eocene samples in the five areas was characterized by rocks with intermediate or mafic geochemical characteristics. The terrigenous/aquatic ratio of coal and shaly coal samples of the areas in question is >1. The sterane distribution was 29C > C28 > C27 and C29 > C27 > C28 for the Özyurt and Tarhanas areas, respectively. -
This Article Appeared in a Journal Published by Elsevier. the Attached
(This is a sample cover image for this issue. The actual cover is not yet available at this time.) This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution and sharing with colleagues. Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites are prohibited. In most cases authors are permitted to post their version of the article (e.g. in Word or Tex form) to their personal website or institutional repository. Authors requiring further information regarding Elsevier’s archiving and manuscript policies are encouraged to visit: http://www.elsevier.com/copyright Author's personal copy Chemical Geology 322–323 (2012) 121–144 Contents lists available at SciVerse ScienceDirect Chemical Geology journal homepage: www.elsevier.com/locate/chemgeo The end‐Permian mass extinction: A rapid volcanic CO2 and CH4‐climatic catastrophe Uwe Brand a,⁎, Renato Posenato b, Rosemarie Came c, Hagit Affek d, Lucia Angiolini e, Karem Azmy f, Enzo Farabegoli g a Department of Earth Sciences, Brock University, St. Catharines, Ontario, Canada, L2S 3A1 b Dipartimento di Scienze della Terra, Università di Ferrara, Polo Scientifico-tecnologico, Via Saragat 1, 44100 Ferrara Italy c Department of Earth Sciences, The University of New Hampshire, Durham, NH 03824 USA d Department of Geology and Geophysics, Yale University, New Haven, CT 06520–8109 USA e Dipartimento di Scienze della Terra, Via Mangiagalli 34, Università di Milano, 20133 Milan Italy f Department of Earth Sciences, Memorial University, St. -
New Radiometric 40Ar–39Ar Dates and Faunistic Analyses Refine
www.nature.com/scientificreports OPEN New radiometric 40Ar–39Ar dates and faunistic analyses refne evolutionary dynamics of Neogene vertebrate assemblages in southern South America Francisco J. Prevosti1,2*, Cristo O. Romano2,3, Analía M. Forasiepi2,3, Sidney Hemming4, Ricardo Bonini2,5, Adriana M. Candela2,6, Esperanza Cerdeño2,3, M. Carolina Madozzo Jaén2,7,8, Pablo E. Ortiz2,7, François Pujos2,3, Luciano Rasia2,6, Gabriela I. Schmidt2,9, Matias Taglioretti10,11,12, Ross D. E. MacPhee13 & Ulyses F. J. Pardiñas2,14,15 The vertebrate fossil record of the Pampean Region of Argentina occupies an important place in South American vertebrate paleontology. An abundance of localities has long been the main basis for constructing the chronostratigraphical/geochronological scale for the late Neogene–Quaternary of South America, as well as for understanding major patterns of vertebrate evolution, including the Great American Biotic Interchange. However, few independently-derived dates are available for constraining this record. In this contribution, we present new 40Ar/39Ar dates on escorias (likely the product of meteoric impacts) from the Argentinean Atlantic coast and statistically-based biochronological analyses that help to calibrate Late Miocene–Pliocene Pampean faunal successions. For the type areas of the Montehermosan and Chapadmalalan Ages/Stages, our results delimit their age ranges to 4.7–3.7 Ma and ca. 3.74–3.04 Ma, respectively. Additionally, from Buenos Aires Province, dates of 5.17 Ma and 4.33 Ma were recovered for “Huayquerian” and Montehermosan faunas. This information helps to better calibrate important frst appearances of allochthonous taxa in South America, including one of the oldest records for procyonids (7.24–5.95 Ma), cricetids (6.95– 5.46 Ma), and tayassuids (> 3.74 Ma, oldest high-confdence record). -
AUSTRIAN JOURNAL of EARTH SCIENCES Volume 98 2005
AUSTRIAN JOURNAL of EARTH SCIENCES [MITTEILUNGEN der ÖSTERREICHISCHEN GEOLOGISCHEN GESELLSCHAFT] an INTERNATIONAL JOURNAL of the AUSTRIAN GEOLOGICAL SOCIETY volume 98 2005 Gerd RANTITSCH & Barbara RUSSEGGER: Organic maturation within the Central Northern Calcareous Alps (Eastern Alps)________________________________ www.univie.ac.at/ajes EDITING: Grasemann Bernhard, Wagreich Michael PUBLISCHER: Österreichische Geologische Gesellschaft Rasumofskygasse 23, A-1031 Wien TYPESETTER: Irnberger Norbert, www.irnberger.net Copy-Shop Urban, Bahnstraße 26a, 2130 Mistelbach PRINTER: Holzhausen Druck & Medien GmbH Holzhausenplatz 1, 1140 Wien ISSN 0251-7493 Austrian Journal of Earth Sciences Volume 98 Vienna 2005 Organic maturation within the Central Northern Calca- reous Alps (Eastern Alps) Gerd RANTITSCH1) & Barbara RUSSEGGER2) KEYWORDS very low-grade metamorphism Northern Calcareous Alps 1) Department of Applied Geosciences and Geophysics, Montanuniversität Leoben, vitrinite reflectance Austria, A-8700 Leoben, Austria, Email: [email protected] thermal modeling Jurassic orogeny 2) Library of the University of Graz, A-8010 Graz, Austria Eastern Alps Abstract Organic maturation within the central Northern Calcareous Alps (Eastern Alps) has been investigated using vitrinite reflectance data from Upper Permian to Upper Cretaceous strata of the Stauffen-Höllengebirge Nappe, Dachstein Nappe, Tennengebirge Block and Lammer Unit. Within the Lammer Unit a metamorphic break is observed between the Strubberg Formation and the tectonically overlying -
15 Al 17 De Abril De 2013 Museo Paleontológico Egidio Feruglio Trelew, Chubut, Patagonia Argentina
AMEGHINIANA 50 (4) Suplemento 2013–RESÚMENES 15 al 17 de Abril de 2013 Museo Paleontológico Egidio Feruglio Trelew, Chubut, Patagonia Argentina LIBRO DE RESUMENES R34 AMEGHINIANA 50 (4) Suplemento 2013–RESÚMENES COMITÉ ORGANIZADOR Presidente Rubén Cúneo Tesorero Alejandro Andreini - Ignacio Escapa Secretaria M. Alejandra Pagani Vocales Diego Pol, Mariel Ferrari, José Luis Carballido, Cecilia Apaldetti, Juliana Sterli, Carlos Asaro COMITÉ CIENTÍFICO Susana Damborenea, Zulma Brandoni de Gasparini, Mirta Quattrocchio, Roberto Scasso INSTITUCIONES ORGANIZADORAS R35 AMEGHINIANA 50 (4) Suplemento 2013–RESÚMENES NEW CarBon Isotope Records of THE EarLY JUrassic Toarcian Oceanic Anoxic Event from THE NEUQUén Basin, Argentina A.H. Al-Suwaidi1, F. Baudin2, S.E. Damborenea3, S.P. Hesselbo2, H.C. Jenkyns2, M.O. Manceñido3 and A.C. Riccardi3 1Petroleum Geoscience Department, Petroleum Institute, PO Box 2533, Abu Dhabi, UAE. [email protected] 2Department of Earth Sciences, University of Oxford, Parks Road, Oxford, OX1 3PR, UK. 3UPMC - Université de Paris 06 & CNRS, UMR 7193, ISTeP, F-75252, Paris Cx 05, France. 4Departamento Paleontología Invertebrados, Museo de Ciencias Naturales La Plata, Argentina, Paseo del Bosque S /N, 1900 La Plata, Argentina. The Neuquén Basin is located in Argentina, between 32°S and 41°S latitude. The basin is a back-arc with a multiphase tectonic history domi- nated by rifting related to the break up of Gondwana and extension of the South American Plate. New biostratigraphy and organic-carbon 13 isotope data (δ Corg) from -
Permian-Triassic-Boundary and Lower Triassic in the Dolomites, Southern Alps (Italy)
Journal of Alpine Geology, 54: 379-404, Wien 2012 Permian-Triassic-Boundary and Lower Triassic in the Dolomites, Southern Alps (Italy) By RAINER BRANDNER, MICHA HORACEK & LORENZ KEIM† With 21 figures Field Trip Guide 29th IAS Meeting of Sedimentology Schladming/Austria Addresses of the authors: RAINER BRANDNER Universität Innsbruck Institut für Geologie & Paläontologie Innrain 52 6020 Innsbruck Austria E-mail: [email protected] MICHA HORACEK BLT Wieselburg Lehr-und Forschungszentrum Francisco Josephinum Rottenhauser Straße 1 3250 Wieselburg Austria E-mail address: [email protected] Journal of Alpine Geology 54 S. 379-404 Wien 2012 379 BRANDNER, HORACEK & KEIM: Permian-Triassic boundary and Lower Triassic in the Dolomites, Southern Alps (Italy) LORENZ KEIM Amt für Geologie & Baustoffprüfung/ Ufficio Geologia e prove materiali Autonome Provinz Bozen - Südtirol/Provincia Autonoma di Bolzano-Alto Adige Eggentalerstr. 48/ Via Val d’Ega 48 I-39053 Kardaun/Cardano Italy Lorenz Keim died during a cross country ski tour in a snow avalanche at the Stallersattel (South Tirol, Italy) on February 4, 2012. He just turned 43, was married and had three little boys. In the last years he worked at the Geological Survey as field geologist, as coordinator of geological maps and was involved in reconnaissance studies for the Brenner Base Tunnel on the South Tyrolean side. As excellent geologist he leaves a big hole in the Tyrolean geology. He is painfully missed. Content Abstract........................................................................................................................................................................380