Redalyc.Problems of Neogene Biostratigraphic Correlation In
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11 Sualdea Et Al.Indd
SPANISH J OURNAL OF P ALAEONTOLOGY 20 years at campus: heritage assessment update for Somosaguas fossil geosite (Pozuelo de Alarcón, Madrid) Lucía R. SUALDEA 1* , Adriana OLIVER 2, Fernando BLANCO 3, Iris MENÉNDEZ 1,4 , Manuel HERNÁNDEZ FERNÁNDEZ1,4, Laura DOMINGO 1,5 & Ana Rosa GÓMEZ CANO 6,7 1 Departamento de Geodinámica, Estratigrafía y Paleontología, Facultad de Ciencias Geológicas, Universidad Complutense de Madrid, C/ José Antonio Novais 12, 28040, Madrid; [email protected], [email protected], [email protected], [email protected]. 2 Geosfera, C/ Madres de la Plaza de Mayo, 2, 28523, Rivas-Vaciamadrid, Madrid; [email protected] 3 Museum für Naturkunde, Leibniz-Institut für Evolutions und Biodiversitätsforschung, Invalidenstraße 43, 10115, Berlin, Germany; [email protected] 4 Departamento de Geología Sedimentaria y Cambio Medioambiental, Instituto de Geociencias IGEO (CSIC, UCM), C/ Dr. Severo Ochoa, 7, 28040, Madrid 5 Earth and Planetary Sciences Department. University of California Santa Cruz, 1156 High Street, 95064, Santa Cruz, USA 6 Transmitting Science, C/ Gardenia 2, Piera, 08784, Barcelona. 7 Institut Català de Paleontologia Miquel Crusafont, Edifi ci ICP, Campus de la UAB s/n, 08193, Cerdanyola del Vallès; [email protected] * Corresponding author Sualdea, L.R., Oliver, A., Blanco, F., Menéndez, I., Hernández Fernández, M., Domingo, L. & Gómez Cano, A.R. 2019. 20 years at campus: heritage assessment update for Somosaguas fossil geosite (Pozuelo de Alarcón, Madrid). [20 años en el campus: actualización de la valoración -
Issn: 2250-0588 Fossil Mammals
IJREISS Volume 2, Issue 8 (August 2012) ISSN: 2250-0588 FOSSIL MAMMALS (RHINOCEROTIDS, GIRAFFIDS, BOVIDS) FROM THE MIOCENE ROCKS OF DHOK BUN AMEER KHATOON, DISTRICT CHAKWAL, PUNJAB, PAKISTAN 1Khizar Samiullah* 1Muhammad Akhtar, 2Muhammad A. Khan and 3Abdul Ghaffar 1Zoology department, Quaid-e-Azam campus, Punjab University, Lahore, Punjab, Pakistan 2Zoology Department, GC University, Faisalabad, Punjab, Pakistan 3Department of Meteorology, COMSATS Institute of Information Technology (CIIT), Islamabad ABSTRACT Fossil site Dhok Bun Ameer Khatoon (32o 47' 26.4" N, 72° 55' 35.7" E) yielded a significant amount of mammalian assemblage including two families of even-toed fossil mammal (Giraffidae, and Bovidae) and one family of odd-toed (Rhinocerotidae) of the Late Miocene (Samiullah, 2011). This newly discovered site has well exposed Chinji and Nagri formation and has dated approximately 14.2-9.5 Ma. This age agrees with the divergence of different mammalian genera. Sedimentological evidence of the site supports that this is deposited in locustrine or fluvial environment, as Chinji formation is composed primarily of mud-stone while the Nagri formation is sand dominated. Palaeoenvironmental data indicates that Miocene climate of Pakistan was probably be monsoonal as there is now a days. Mostly the genera recovered from this site resemble with the overlying younger Dhok Pathan formation of the Siwaliks while the size variation in dentition is taxonomically important for vertebrate evolutionary point of view and this is the main reason to conduct this study at this specific site to add additional information in the field of Palaeontology. A detailed study of fossils mammals found in Miocene rocks exposed at Dhok Bun Ameer Khatoon was carried out. -
Suidae, Mammalia) from the Late Middle Miocene of Gratkorn (Austria, Styria
Palaeobio Palaeoenv (2014) 94:595–617 DOI 10.1007/s12549-014-0152-1 ORIGINAL PAPER Taxonomic study of the pigs (Suidae, Mammalia) from the late Middle Miocene of Gratkorn (Austria, Styria) Jan van der Made & Jérôme Prieto & Manuela Aiglstorfer & Madelaine Böhme & Martin Gross Received: 21 November 2013 /Revised: 26 January 2014 /Accepted: 4 February 2014 /Published online: 23 April 2014 # Senckenberg Gesellschaft für Naturforschung and Springer-Verlag Berlin Heidelberg 2014 Abstract The locality of Gratkorn of early late Sarmatian age European Tetraconodontinae. The morphometric changes that (Styria, Austria, Middle Miocene) has yielded an abundant occurred in a series of fossil samples covering the known and diverse fauna, including invertebrates, micro-vertebrates temporal ranges of the species Pa. steinheimensis are docu- and large mammals, as well as plants. As part of the taxonom- mented. It is concluded that Parachleuastochoerus includes ical study of the mammals, two species of suids, are described three species, namely Pa. steinheimensis, Pa. huenermanni here and assigned to Listriodon splendens Vo n M ey er, 1 84 6 and Pa. crusafonti. Evolutionary changes are recognised and Parachleuastochoerus steinheimensis (Fraas, 1870). As among the Pa. steinheimensis fossil samples. In addition, it the generic affinities of the latter species were subject to is proposed that the subspecies Pa. steinheimensis olujici was debate, we present a detailed study of the evolution of the present in Croatia long before the genus dispersed further into Europe. This article is an additional contribution to the special issue "The Sarmatian vertebrate locality Gratkorn, Styrian Basin". Keywords Listriodontinae . Tetraconodontinae . Middle J. van der Made (*) Miocene . -
The Pig Conohyus Simorrensis from the Upper Aragonian of Alhambra, Madrid, and a Review of the Distribution Ofeuropeanconohyus J
t EstudiosGeoI.. 59: ~12 (2001) ~ THE PIG CONOHYUS SIMORRENSIS FROM THE UPPER ARAGONIAN OF ALHAMBRA, MADRID, AND A REVIEW OF THE DISTRIBUTION OFEUROPEANCONOHYUS J. van der Made* and J. Morales* ABSTRACT The suid remainsfrom Alhambra (Madrid, late Aragonian, Middle Miocene; MN6. wne F) are describedand assignedto Conohyuss;morrens;s. Conohyus is well known in Spain from late MN5. or zone E. MN7+8. or zone G, and MN9. The material from Alhambra fills the gap in the lberian record. The Iberian record showsthat Cononhyus becamelarger. with relatively larger posteriormolars and with reducedpremolars. This evolution occurredin a large ateathat extendsfrom westemEurope to Anatolia. We pre- senaan overview of the Europeanand Anatolian localities with Conohyus. Key words: Conohyus.T etraconodont;nae . Suidae. Aragon;an, M ;ocene,b;ogeography. RESUMEN Los restos de suido de Alhambra (Madrid. AragonienseTardío, Mioceno Medio, MN6, lona F) son descritosy asignadosa Conohyussimorrt'nsis. Este génerose conoce bien en Españade la unidadMNS": o lona E. y MN7+8, o zonaG, y en MN9. El material de Alhambra llena un hiato en el registro ibérico. La evolución de ConohyUSocurrió en una vasta área que se extiende de Europa occidental hasta Anatolia. Presentamosun sumariode yacimientoseuropeos y turcoscon Conohyus. Palabrasclave: Conohyus.T etraconodontina~. Suidae. Aragoniense. Mioceno. biogeografla. Introduction Aves Aves indet. The locality of Alhambrawas discoveredin 1991 Mammalia by the geologistJavier Gonzálezwhen a new street Soricinae indet. was constructed near to the banks of the Manzanares Galerix sp. river in the La Latina quarter in the center of Madrid Pseudaelurus quadr;dentatus The locality was excavated during two campagns.the Hemicyoninae indet. -
The Neogene of Portugal
Ciencias da Terra (tJNLl Numeroespecial IT THE NEOGENE OF PORTUGAL M. Telles ANTUNES & Joao PAIS Centro de Estratigrafia e Paleobiologia (I.N.I.C.). Faculdade de Ciencias e Tecnologia. Quinta da Torre. P-2825 Monte de Caparica FOREWORD and Gustave Dollfus gave important contribu tions. After years of research dedicated to the After a long eclipse, there was a remark Mediterranean Neogene (Project NQ 25, IUGS able resumption of Neogene studies due to UNESCO), there has been a considerable de Portuguese geologists or foreign geologists at velopment in activities concerning the Atlantic the service of Portugal. G. Zbyszewski de Neogene. serves a special reference for his work. Within this framework, the hinge-like Finally, we have tried to develop and co situation of . Portugal is quite interesting, ordinate efforts to reach the knowledge that, in considering the fact that the neogene units here spite of the amount of data already obtained, is are well represented and complete. This is far from being complete. This justifies the fol particularly true for the Tagus basin, that has a low-up of researches that are frequently done very rich record. At the beginning of the XIX with the collaboration of colleagues from other century, research has been conducted by the countries, mainly France. Part of this data is remarkable mineralogist (and future politician) presented in the following compilation of texts. Jose Bonifacio de Andrada e Silva (1763- 1838). Towards the 30's and 40's, the contributions due to Baron Von Eschwege, THE NEOGENE Alexandre Vandelli, Daniel Sharpe and a few others followed. -
Multiproxy Reconstruction of the Palaeoclimate and Palaeoenvironment of the Middle Miocene Somosaguas Site (Madrid, Spain) Using Herbivore Dental Enamel
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by EPrints Complutense Multiproxy reconstruction of the palaeoclimate and palaeoenvironment of the Middle Miocene Somosaguas site (Madrid, Spain) using herbivore dental enamel .d Laura Domingo a.* Jaime Cuevas-Gonzalez b, Stephen T. Grimes C, Manuel Hernandez Fernandez a , , Nieves L6pez-Martineza • Dept Paleont%gia, Facultad cc Geol6gicas, Universidad Complutense de Madrid, 28040 Madrid, Spain b Dept Ciencias de la Tierra y del Media Ambiente, Labomtorio de Petr%gia Ap/icada, Universidad de Alicanre, 03690 Alicante, Spain C School of Earth, Ocean and Environmental Sciences, University of Plymouth, Drake Circus, PL4 BM Plymouth, Devon, United Kingdom d Unidad de Investigaci6n de Paleonto[ogia, Instituto de Geologia Economica, Consejo Superior de Investigaciones Cientfjicas, 28040 Madrid, Spain ABSTRACT Profound palaeoc1imatic changes took place during the Middle Miocene. The Miocene Climatic Optimum (�20 to 14-13. 5 Ma) was followed by a sudden (�200 ka) decrease in temperature and an increase in aridity around the world as a consequence of the reestablishment of the ice cap in Antarctica. Somosaguas palaeontological site (Madrid Basin, Spain) has provided a rich record of mammal remains coincident with this giobal event (Middle Miocene Biozone E, 14.1-13.8 Ma). It contains four fossiliferous levels (Tl, T3-1, T3-2 Keywords: and T3-3, with Tl being the oldest) that span an estimated time of �105-125 ka. Scanning Electron Somosaguas Microscope (SEM) and Rare Earth Element (REE) analyses performed on herbivore tooth enamel Large mammalian herbivores Oxygen and carbon isotopes (Gomphotherium angustidens, Anchitherium d A. -
Lartet, 1851) (Suidae, Mammalia) from the Middle Miocene of Carpetana (Madrid, Spain
SPANISH JOURNAL OF PALAEONTOLOGY Conohyus simorrensis (Lartet, 1851) (Suidae, Mammalia) from the Middle Miocene of Carpetana (Madrid, Spain) Martin PICKFORD Département Histoire de la Terre, and UMR 7207 (CR2P) du CNRS, 8 rue Buffon, 75005, Paris, France; [email protected] Pickford, M. 2013. Conohyus simorrensis (Lartet, 1851) (Suidae, Mammalia) from the Middle Miocene of Carpetana (Madrid, Spain). [Conohyus simorrensis (Lartet, 1851) (Suidae, Mammalia) del Mioceno Medio de Carpetana (Madrid, España)]. Spanish Journal of Palaeontology, 28 (1), 91-102. Manuscript received 26 February 2013 © Sociedad Española de Paleontología ISSN 2255-0550 Manuscript accepted 2 April 2013 ABSTRACT RESUMEN Fossil suid remains excavated from Middle Miocene deposits Los restos fósiles de suidos del Mioceno medio extraídos at Carpetana, Madrid, comprise mandibles and isolated teeth del yacimiento de Carpetana, Madrid, incluyen mandíbulas of the tetraconodont suid, Conohyus simorrensis (Lartet, y dientes aislados del suido tetraconodóntido, Conohyus 1851). The Carpetana mandible is the most complete specimen simorrensis (Lartet, 1851). La mandíbula de Carpetana es el known for the genus and throws a great deal of light on the espécimen más completo conocido y proporciona una valiosa morphology of the anterior dentition. Heavy wear on all the información sobre la morfología de la dentición anterior. teeth, including deciduous ones in the sample, indicates a diet Un intenso desgaste en todos los dientes, incluso en los de of abrasive or durable food items such as nuts. leche, indica una dieta a base de comida abrasiva y dura, como nueces. Keywords: Tetraconodontinae, taxonomy, palaeoecology, revision, dento-gnathic. Palabras clave: Tetraconodontinae, taxonomía, paleoecología, revisión, dento-maxilar. https://doi.org/10.7203/sjp.28.1.17834 92 PICKFORD 1. -
Basal Middle Miocene Listriodontinae (Suidae, Artiodactyla) from Madrid, Spain
SPANISH JOURNAL OF PALAEONTOLOGY Basal middle Miocene Listriodontinae (Suidae, Artiodactyla) from Madrid, Spain Martin PICKFORD1* & Jorge MORALES2 1 Sorbonne Universités - CR2P, MNHN, CNRS, UPMC - Paris VI, 8, rue Buffon, 75005, Paris, France; [email protected] 2 Departamento de Paleobiología, Museo Nacional de Ciencias Naturales-CSIC, c/ José Gutiérrez Abascal 2, 28006, Madrid, Spain; [email protected] * Corresponding author Pickford, M. & Morales, J. 2016. Basal middle Miocene Listriodontinae (Suidae, Artiodactyla) from Madrid, Spain. [Listriodontinae (Suidae, Artiodactyla) de la base del Mioceno medio de Madrid, España]. Spanish Journal of Palaeontology, 31 (2), 369-406. Manuscript received 18 January 2016 © Sociedad Española de Paleontología ISSN 2255-0550 Manuscript accepted 14 September 2016 ABSTRACT RESUMEN Excavations in basal middle Miocene deposits in the Madrid Las excavaciones en los depósitos del Mioceno medio basal Basin (Old Mahou Brewery, Los Nogales, La Hidroeléctrica, en la Cuenca de Madrid (Antigua Fábrica de Mahou, Los Guadarrama I, Barajas) have yielded interesting assemblages Nogales, La Hidroeléctrica, Guadarrama I, Barajas) han of fossils, among which the listriodont suid Listriodon aportado una interesante asociación de fósiles, entre los que la retamaensis Pickford & Morales, 2003, is well represented. especie Listriodon retamaensis Pickford & Morales, 2003 está Much of the material is juvenile, and several of the permanent muy bien representada. Buena parte del material corresponde teeth are unworn, permitting detailed observations to be made a individuos juveniles y algunos de los dientes permanentes of the fi ne structures of the crowns, which was not possible están intactos, lo que permite hacer observaciones de detalle with the original hypodigm of the species from Retama de las estructuras de la corona. -
An Unusual Diatomyid Rodent from an Infrequently Sampled Late Miocene Interval in the Siwaliks of Pakistan
Palaeontologia Electronica http://palaeo-electronica.org AN UNUSUAL DIATOMYID RODENT FROM AN INFREQUENTLY SAMPLED LATE MIOCENE INTERVAL IN THE SIWALIKS OF PAKISTAN Lawrence J. Flynn and Michèle E. Morgan ABSTRACT The Siwalik deposits of Pakistan yield numerous superposed assemblages that record the small mammal fauna throughout the middle and late Miocene on the Indian subcontinent. A few stratigraphic intervals are poorly represented by microfaunas. Between older, rich Chinji Formation assemblages and fossiliferous levels high in the Nagri Formation, few fossil localities yield abundant rodents between about 11.3 and 10.4 Ma. Locality Y797, predating the first local appearance of hipparionine equids, is notable for presence of a new large diatomyid rodent, Willmus maximus gen. et sp. nov., recorded nowhere else. Willmus has affinity with Diatomys from China and Thai- land and with predecessors such as Fallomus from the pre-Siwalik formations of Bugti and the Zinda Pir Dome, Pakistan. Willmus is derived in its large size, absence of accessory cusps, and extreme bilophodonty, and is by far the latest and rarest member of its group. Faunal similarity indices between Y797 and well-sampled older Chinji and younger Nagri rodent faunas are very high at the species level. Large mammal faunas are also similar. Fauna and lithology suggest nothing unusual about this locality and offer no compelling evidence for a unique microhabitat. Willmus is a derived end mem- ber in a distinct rodent group of low taxonomic diversity. This unusual family reappears in the Siwalik record at Y797 after a long absence from the fossil record. It is perhaps the derived features of Willmus that contributed to the survival of this group. -
Life Finds a Way
Life finds a way Eder Amayuelas, Peru Bilbao-Lasa, Oscar Bonilla, Miren del Val, Jon Errandonea-Martin, Idoia Garate-Olave, Andrea García-Sagastibelza, Beñat Intxauspe-Zubiaurre, Naroa Martinez-Braceras, Leire Perales-Gogenola, Mauro Ponsoda-Carreres, Haizea Portillo, Humberto Serrano, Roi Silva-Casal, Aitziber Suárez-Bilbao, Oier Suarez-Hernando (Editores) © De los textos y las figuras, los autores © Del diseño de la portada y el logo del XVI EJIP, Oier Suarez Hernando y Humberto Serrano © De la fotografía de la portada, Naroa Martinez Braceras Maquetación: Jon Errandonea Martin y Roi Silva Casal Depósito Legal: xxxxxxxxxxxx Cómo citar el libro: Amayuelas, E., Bilbao-Lasa, P., Bonilla, O., del Val, M., Errandonea-Martin, J., Garate-Olave, I., García-Sagastibelza, A., Intxauspe-Zubiaurre, B., Martinez-Braceras, N., Perales-Gogenola, L., Ponsoda-Carreres, M., Portillo, H., Serrano, H., Silva-Casal, R., Suárez- Bilbao, A., Suarez-Hernando, O., 2018. Life finds a way, Gasteiz, 328 pp. Cómo citar un abstract: Intxauspe-Zubiaurre B., Flores, J-A., Payros A., Dinarès-Turell, J., Martínez-Braceras, N., 2018. Variability in the calcareous nannofossil assemblages in the Barinatxe section (Bay of Biscay, western Pyrenees) during an early Eocene climatic perturbation (~54.2 ma), p. 21– 24. In: Amayuelas, E., Bilbao-Lasa, P., Bonilla, O., del Val, M., Errandonea- Martin, J., Garate-Olave, I., García-Sagastibelza, A., Intxauspe-Zubiaurre, B., Martinez-Braceras, N., Perales-Gogenola, L., Ponsoda-Carreres, M., Portillo, H., Serrano, H., Silva-Casal, -
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A contribution to the evolutionary biology of Conohyus olujici n. sp. (Mammalia, Suidae, Tetraconodontinae) from the early Miocene of Lučane, Croatia Raymond L. BERNOR Shundong BI College of Medicine, Department of Anatomy, Laboratory of Evolutionary Biology, Howard University, 520 W St. N.W., Washington D.C. 20059 (USA) [email protected] [email protected] Jakov RADOVČIĆ Croatian Natural History Museum, Department of Geology and Paleontology, Demetrova 1, HR 10000 Zagreb (Croatia) [email protected] Bernor R. L., Bi S. & Radovčić J. 2004. — A contribution to the evolutionary biology of Conohyus olujici n. sp. (Mammalia, Suidae, Tetraconodontinae) from the early Miocene of Lučane, Croatia. Geodiversitas 26 (3) : 509-534. ABSTRACT We describe here the topotypic series of Conohyus olujici n. sp. from the Croatian locality of Lučane. This sample was originally collected by local lignite miners in the 1930’s, who conveyed the sample to the parish’s Franciscan monk Dr. Josip Olujić. The Lučane Conohyus sample includes seven lower jaws and jaw fragments; no upper cheek teeth have yet been recovered. Our use of bivariate statistics, log10 ratio diagrams and a cladistic analysis all reveal that C. olujici n. sp. is the most primitive member of the Conohyus clade. The analyses reveal that: of the sample considered, only two species are referable to Parachleuastochoerus, P. sp. and P. crusafonti; Parachleuastochoerus is the sister-taxon to Conohyus; Conohyus is a clade, KEY WORDS and C. olujici n. sp. is the sister-taxon of the C. steinheimensis-C. simorrensis Mammalia, and C. sindiensis clades. Conohyus olujici n. sp. would appear to have occurred Suidae, Tetraconodontinae, at a time when the genus enjoyed a relatively continuous geographic range Conohyus, that extended from southern Europe to South Asia. -
Redalyc.Trace Element Analyses Indicative of Paleodiets in Middle
Geologica Acta: an international earth science journal ISSN: 1695-6133 [email protected] Universitat de Barcelona España DOMINGO, L.; LÓPEZ-MARTÍNEZ, N.; GRIMES, S.T. Trace element analyses indicative of paleodiets in Middle Miocene mammals from the Somosaguas site (Madrid, Spain) Geologica Acta: an international earth science journal, vol. 10, núm. 3, septiembre, 2012, pp. 239-247 Universitat de Barcelona Barcelona, España Available in: http://www.redalyc.org/articulo.oa?id=50524523003 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 Geologica Acta, Vol.10, Nº 3, September 2012, 239-247 DOI: 10.1344/105.000001746 Available online at www.geologica-acta.com Trace element analyses indicative of paleodiets in Middle Miocene mammals from the Somosaguas site (Madrid, Spain) 1, 2, 3 2, 3, † 4 L. DOMINGO N. LÓPEZ-MARTÍNEZ S.T. GRIMES 1 Earth and Planetary Sciences Department, University of California Santa Cruz, CA 95064 (USA). E-mail: [email protected]; Fax: +34 913944849 2 Departamento de Paleontología, Facultad CC. Geológicas, Universidad Complutense de Madrid-Instituto de Geología Económica (CSIC) 28040 Madrid, Spain 3 Unidad de Investigación de Paleontología, Instituto de Geología Económica (CSIC) 28040 Madrid, Spain 4 School of Geography, Earth and Environmental Sciences, University of Plymouth Drake Circus, Plymouth, Devon, PL4 8AA, United Kingdom. E-mail: [email protected]; Fax: +44 (0)1752 584776 † Deceased, December 2010 ABS TRACT Trace element analysis of fossil bone and enamel constitutes a useful tool to characterize the paleoecological behavior of mammals.