Neues Jahrbuch Für Mineralogie, Geologie and Paläontologie

Total Page:16

File Type:pdf, Size:1020Kb

Neues Jahrbuch Für Mineralogie, Geologie and Paläontologie XXVI Sachverzeichniss. Sachverzeichniss. Die Abhandlungen und Briefe sind cursiv gedruckt. Aarmassiv, Gliederung d. mesoz. Sedi- Alpen mente am Nordrande 94. Aarmassiv 94. Abietineenholz, Braunkohle, Häring in Bau u. Grenze gegen Appennin 491. Tirol 386. Berner, nördl. Kette 488. Absorptionsbüschel, Lage inzweiaxigen schweizer, Tektonik 98. pleochroit. Kryst. 3. südl., Graptolithenschiefer 490. Acanthonautilus bispinosus, Kohlen- transsylvan. Bumäniens 106. kalk, Ireland 177. Turiner Hügel 491. Acetylentetrabromid zur Trennung von venetianische, Gliederung der Kreide Mineralgemengen 389. 331. Achtalj, Gouv. Tiflis, Schlammvulcane westl., Tektonik 56, 100, 101. 1892-96 437. Altenberg bei Aachen, faseriger Zink- Adamellit, Birkrem und Lister, Norw. vitriol 76. • 450, 454. Aluminit aus Pyrit entst. 206. Adamellogruppe , Contactmineralien Aluminium, Metall 405. (Dipyr) 223. Amalgam, Chalanches, Kryst. 13. Adare, Gap, Südpolargeb., Gesteine 476. Amberg,Weisserz = Spatheisen, Anal. 8. Aegäische Inseln, Geol. 121. Amerika, Nord- Aetna, alte Beschreibung 431. Jura und Kreide, atlant. Küste 529. Africa, Süd-, Apophyllit 33. New Red 524. - - Aktinolith Magnetit Schiefer , Birch Ammoniten Lake, Minnesota 280. Barremien, Querola, Spanien 568. Alaska, Goldfelder 478. obere Kreide, Algier 372. Albit, Radauthal 223. Vertheilung im russ. Jura 177. Alemtejo, Portugal Ammonites Tschefkini , Schumarowo Cambr. Diabastuff 321. 569. Carbon 325. Ammonoidea und Bactritidae d. brit. Algen, palaeozoische 590. Museums 566. Algier Amphibolandesit, 81. Ammoniten der oberen Kreide 372. Amphibolgabbro, Kiew, Wolhynien 463. Zeolithe, Cap Djinet 226. Amphibolite, Oaxaca 76. Algonkian, Schweden 320. Analcim Alit im Portlandcement 485. Montecatini 224. Allanit, grosse Kryst., Mineville, N. Y. Montecatini, opt. Anom. 32. 212 Ostsibirien 32. Allauch, Massif d\ Geol. 304, 305, 307. Radauthal 223. Alluvium d. Garonne b. Toulouse 303. Schottland 214. Alnöit, Manheim, N. Y. 264. Wiersberg, Anal. 11. Sachverzeichniss. XXVII Ancistrocrania 142. Arseniknickelglanz, Stehen, Anal. 9. Ancodus, amerikanische Arten 547. Artbegriff, Zoologie und Palaeonto- Anden, Chile, Geol. n. Petr. 282. logie 234. Andesit Artefacten im Geschiebelehm, Engl.432. chilen. Anden 283. Arten, physiologische und descriptive Oaxaca, Mexico 81. 233. Santorin mit Drusenmineralien 227. Artes. Brunnen Sierra Nevada 513. Dakota 297. Westerwald 249. Westerloo bei Brüssel, Teit. 531. Andesitgang, Glasdrumman Port, Irel. Arundel-Formation, Maryland 140. 455. Arzberg Andorit = Sundtit und Webnerit 19. Manganspath, Anal. 9. Anisbenztolhydroxylamin, Kryst. 193. Spatheisen, Anal. 8. Anistolhydroxamsäure, Kryst. 203. Asbest, Vorkommen imVal Malenco 211. Anomalien, opt., Analcim 33. Asien, Central-, Orographie 503. Anorthit, Buck Creek, N. Car. 230. Aspasia-Schichten Pontalto, U.-Lias , Anorthosit, Kiew und Wolhynien 465. 327. Anser anatoides, Piioc, Eoussillon 545. As Tavastmorr, Erosionsterrassen und Antarktisches Gebiet, Gesteine 476. Strandlinien 156. Anthophyllit , Jenks Corundum Mine, Asteroiden, tert., Parma etc. 179. Macon Co., N. Car. 230. Augit Anthracit Castle Mountain, Ma. 279. Columbien mit Smaragd 212. Kaukasus, Kryst. 44. Wallis, Stauungsmetamorphose 226. Biotit nach A., Mte Guglielma 6k Antimonglanz, Bunguran, Indien 428. Augitporphyrit Antrim, Grafsch., Liparit u. Bauxit 455. chilen. Anden 282. Apatit, Fluor-, Tokowoja 34. südl. Dalekarlien 445. Aphrodit = Meerschaum 419. Aures-Massif, südl. Constantine, Oligo- Aplit mit Granat, Cap Adare, Süd- cän und Tektonik 334. polargeb. 476. Australien Apophyllit Association for the advancement of Fl-Gehalt 420. Science, Adresse of the President Kimberley 213. LlVERSIDGE 45. Koppiesfontein, Südafrika 33. Gesteine 283. Minnesota, im Diabasmandelst. 228. AxenwinJcel, opt., Aenderung mit Appennin Temp. bei Lithiophilit 154. nördl., geol. Bau 105. Axinit, Lage der Absorptionsbüschel 3. Bau u. Grenze gegen Alpen 491, 492. Azul-Hügel, Buenos Aires 129. Aragonit Bactritidae u. Ammonoidea d. brit. Romagna, mit Schwefel 391. Museums 566. Sicilien 416. Baden (zw. Kandern u. Lörrach), Geol. Val Malenco 211. 303. Archaeopteryx Siemensi, Osteol. 363. Bagneres de Bigorres, Alter der Schie- Archaicum fer 311. Eintheilung 514. Balkan, östl., Geol. 118. laurentin. Kalke 321. Balkanhalbinsel, geolog. Reisen 121. Charkow 111. Banatit, Farsund, Norw. 450, 454. Grottau, Nord-Böhmen 294. Barrettiamultiliratau. sparcilirata 180. Rainy Lake, Goldregion, N.-Amerika Baryt, siehe Schwerspath. 287. chlorid, Cl . Baryum Ba 2 2H2 0, Kry- Schweden 320. stallwasser 1. Schweden u. Finland, Präcambrium Basalt 514. Cap Adare, Südpolargeb. 477. westl. Ontario, klast. Gest. 129. Castle Mountain, Ma. 276. Argentinien Franz-Josephsland 124. Geol. 343. Hernikerland, Born 96. Devon 225. Kangaroo-Insel, mit Gold 283. Arsenfahlerz. Lörzenbach, Anal. 10. Oaxaca, Mex. 82. XXVIII Sachverz 3ichniss. Basalt Böden, verschied. Farben, wahrsch. Slieve Gallion, Londonderry 457. Ursprung 51. Westerwald 249. rothe und grüne 51. Basanit, Hernikerland, Born 97. gelbe 54. Basawluk-Typus d. Syenits 476. Böhm.-bayr. Wald, Graphit 394, 399. Basilicata, südl., Geol. 312. Böhmen Bastide bei Camps, Turon und Senon Damourit, Tabor 427. 141. Delvauxit, Beraun 427. Batolites = Bihippurites 178. Monazit, Anal. 427. Batum, Wolframit 41. Phenakit, Horni Novosedlo 427. Bauxit Siluroidenreste d. Braunkohlenform. Grafsch. Antrira 455. 367. Frankreich, Entstehung 414. Bohrlöcher, Temperatur 51. Verwendung 413. Bojit, Passau 396. Bayr.-böhm. Wald, Graphit 394, 399. Bolivia,Silber-Zinnerzlagerstätten481. Beauxit, siehe Bauxit. Bordeaux, Tertiär, Bohrloch 334. Beggingen, Ctn. Schaffhausen, U. Lias Bosporus, Geolog. Beise 63. 326. Bos primigenius, Ostorf b. Schwerin 168. Belgien, Tertiär (Artes. Brunnen bei Bournonit, Pulacayo, Boliv., Anal. 19. Westerloo) 531. Bozen, Steinmark = Speckstein, Anal. Belit im Portlandcement 485. 11. Bell River , N.-Amerika , recente He- Brachiopoden, Convergenzerscheinun- bung 536. gen 231. Ben More, Mull, Min. in den tert. Brasilien Eruptivgest. 226. Amazonasgebiet, Palaeozoicum 509. Berner Alpen, nördl. Ketten 488. Diamantvorkommen 202. Bernstein 222. Silur 257. nördl. Polen 109. Braunkohlen Romagna, mit Schwefel 391. Grottau, Nordböhmen 294, 367. Rumänien 422. Sardinien, SW. (Gonnesa) 290. Bertrandit mit Hamlinit, Oxford Co., Braunkohlenform. Bilin, Siluridenreste Me. 35. 367. Bieler See, glac. Stauchungserschei- Brefven, Diabas-Granit-Gang, Schwe- nungen (Taschen) 216. den 260. Biella, Piemont, Korund 21. Briancon, Westphalien 100. Bihippurites = Batolites 178. Bröken Hill, Austr., Granat 212. Biotit nach Augit, Mte Guglielmo 61. Bronteus senescens, Chemung-Gruppe, Biotit-Cyanit-Cordierit-Gestein, Hima- N. York 369. laya 263. Brown's Park beds, Uintageb., Plio- 335. Biss-Tscheka , Ural, Bleiglanz mit cän Zwillingslam. 14. Brüx, Whewellit 421, 422. Bittersalz mit Schwefel, Romagna 391. Brunnenbohrungen, Schweden 238. Bitumen mit Schwefel, Romagna 391. Bryozoen, Classification 571. Bixbyit, Utah, 24. Buenos Aires, Geologie 129, 508. Blei, , Roeblingit, N. Jers. Bunguran, Natuna-Archipel Indien, ged. mit , 405. Min. u. Gest. 427. Bleiglanz Buntkupfererz, Tirol, grosse Kryst. 16. mit ged. Silber. Colorado 405. Cadmiumcarbonat, Herstellung 209. mit Zwillingslamellen, Biss-Tscheka, Caernarvonshire, Seen 443. Ural 14. Calabrien, nördl., Geol. 312. Bleiglanzlagerstätten , S W.-Sardinien Calamarien, untercarb., tekton. Ver- 289. ändertingen der Form, Südalpen Blendelagerstätten, SW.-Sardinien289. 259. Südalpen 490. Block Island, Geol. 128. 529. Calamites transitionis , Blödit, Punjab Salt Range 41. Calchiste de Tournay 132. Bockenrod, Odenw., Manganspath 27. Calciumcarbonat, Löslichkeit 209. Bodenuntersuchungen , Deutsch - Ost- Calciumchloroaluminat,wasserhaltiges, afrika u. Kamerun 264. Compressionszwillinge 2. Sachverzeichniss. XXIX Callovien, ob., Dives und Villers-sur- Centrai-Asien, Orographie 503. Mer 328. Cephalopoden d. brit. Mus. III. Bac- Cambrium tritidae und Ammonoidea 566. Alto Alemtejo, Port. 321. Ceratopygenkalktauna. Verbreitung in Buenos Aires 509. Europa 517. östl. Nordamerika, Paradoxides beds Cervus 515. australis, Plioc, Roussillon 545. Schweden 320. ramosus, Plioc, Roussillon 544. Sibirien 516. ruscinensis, Plioc, Roussillon 544. Tennessee 512. Cetaceen, Fahrns des Landes 362. Camps, Bastide bei, Turon und Senon Chabasit 141. Buck Creek, N. Car. 229. Cannelkohle, Peterswald b. Ostrau 295. Ost-Sibirien 33. Cannstatt, Pleistocänbildungen 158. Chalanches, Isere, Amalgam 13. Cap Adare, Südpolargebiet, Gesteine Chalcedon, Mähren 408. 476. Chalcostibit (Wolfsbergit) = Guejaiit Capreolus australis, Plioc, Eoussillon 17. 545. Huanchaca, Boliv., 17. Capstadt, Turmalinfels 264. Charentes, Portlandien 134. | Caracal brevirostris. Plioc, Roussillon ! Charkow, Gouvernement, HydrogeoL 540. 111. Carbon i Chemung-Gruppe, N. York, Crustaceen Calamiten 259, 490. 369. Gliederung 132. Chenango-Thal , N. Amer. , Fluvio- Pflanzen in Concretionen, Schottland glacialbildungen 159* Gannister beds 385. Chicago Area, Glacialbildungen 53. Alemtejo, Port 324. Chile Gross-Britannien, Eintheilung und Anden, Geol. und Petr. 282. Yore dale Series etc. 522. Erzlagerstätten abhängig vom , südl. Harzrand, Culm 133. Eruptivgestein 87, 282. Kansas, Coal measures 324. Chilesalpeter, Westafrika 416. New River, Pottsville Series, West- Chilhowee-Schichten, Tennessee 512. Virginien, Pflanzen 577. China Nord -Wales, Kohlenkalk 523. Nordwest-, geologischer Bau 501. Bjäsan, Wolgastufe 315, 317. Zinnober 205. Rossitz, ,
Recommended publications
  • Neogene and Quaternary Mammal Faunas of Thessaly*
    NEOGENE AND QUATERNARY MAMMAL FAUNAS OF THESSALY* by A. ATHANASSIOU ** I. INTRODUCTION The Province of Thessaly is situated in Central Greece. It is a mainly plain geographical area (the most extensive low relief area in the Greek peninsula), delimited in the North by Olympus Mountain, in the West by Pfndos mountain range, in the East by the Aegean Sea and in the South by Orthrys mountain range. Alluvial deposits that form extensive plains cover most of the eastern and central part of the region. A hill range made of tertiary gravel beds and directed NW-SE, divides these plains into two regions: the plain of Larissa in the East and the plain of Trfkala-Kardftsa in the West. Two smaller basins, those of Volos and Almyros, extend in SE Thessaly. The westernmost part of the province is mountainous, formed by alpine and molassic formations of Mesozoic and Neogene age respectively. In the southwestern part the long peninsula of P61ion Mountain forms the wide and rather closed Pagassetic Gulf. 11. GEOLOGY The Thessalian mountain ranges are placed in the Pelagonic and Pfndos geotectonic zones, which have a NW-SE direction. The Pelagonic is a very wide zone that covers a very extensive area of Northern and Central Greece. It is usually divided to several minor zones, either metamorphic or not. Most of those zones are of Triassic-lurassic age and they are covered by a transgression series that begins in Late Cretaceous (Cenomanian). The stratigraphic columns of the Pelagonic zone consist of Late Palaeozoic and Mesozoic metamorphic, semimetamorphic or sedimentary rocks, as gneiss, amphibolites, slates and limestones.
    [Show full text]
  • New Data on the Equus Stenonis Cocchi, 1867 from the Late Pliocene Locality of Sésklo (Thessaly, Greece)
    New data on the Equus stenonis Cocchi, 1867 from the late Pliocene locality of Sésklo (Thessaly, Greece) Athanassios ATHANASSIOU University of Athens, Department of Historical Geology and Palaeontology, Panepistimiopolis, 157 84 Athens (Greece) [email protected] Athanassiou A. 2001. — New data on the Equus stenonis Cocchi, 1867 from the late Pliocene locality of Sésklo (Thessaly, Greece). Geodiversitas 23 (3): 439-469. ABSTRACT The equid material from the late Pliocene locality of Sésklo (Thessaly, Greece) is described and compared in this article. It belongs to a large and KEY WORDS fairly stout Equus stenonis form, which shares many morphological characters Mammalia, with the species samples from Saint-Vallier, La Puebla de Valverde and Perissodactyla, Equidae, Olivola, as well as with already known Equus stenonis samples from other Equus stenonis, Greek localities (Dafneró, Vólax). Its main features are the big skull and late Pliocene, limbs, the short protocones and the very simple enamel plication in the teeth. Villafranchian, Thessaly, Large sized and relatively robust stenonid horses are common elements of the Greece. late Pliocene faunas of Greece. RÉSUMÉ Nouvelles données sur l ’Equus stenonis Cocchi, 1867 de la localité pliocène de Sésklo (Thessalie, Grèce). Dans l’article présent, l’équidé de la localité pliocène de Sésklo (Thessalie, Grèce) est décrit et comparé. Il appartient à une forme d’Equus stenonis large MOTS CLÉS et assez robuste, qui a des caractères morphologiques communs avec les Mammalia, échantillons de Saint-Vallier, La Puebla de Valverde et Olivola, ainsi qu’avec Perissodactyla, Equidae, des échantillons déjà connus d’autres localités grecques (Dafneró et Vólax).
    [Show full text]
  • Preliminary Note on the Late Pliocene Fauna from Vatera (Lesvos, Greece)
    ANNALES GÉOLOGIQUES DES PAYS HELLÉNIQUES PUBLIÉES SOUS LA DIRECTION DE DÉPARTEMENT DE GÉOLOGIE DE L' UNIVERSITÉD' ATHÈNES DE Vos, J., VANDER MADE,J., ATHANASSIOU,A., LYRAS,G., SONDAAR,P.Y., & M.D. DERMITZAKIS PRELIMINARY NOTE ON THE LATE PLIOCENE FAUNA FROM VATERA (LESVOS, GREECE) DE VOS, J., VAN DER MADE,J., AOANALIOY,A., AYPAL,r., SONDAAR,P.Y., & M.A. AEPMITZAKHL IIPOKATAPTIKH ITEPITPAQH THE ANQIIAEIOKAINIKHE ITANIAAZ TQN BATEPQN (N. AECBOE) ATHENES DÉPARTEMENT DE GÉOLOGIE Panepistimiopolis, Athènes (157 84) 2002 AY&TWJIOY&ilTOY «Teohoytilcih XeovixOv TOY Ehhqviilhv Xcoph», 39, Fasc. A., 2002 Extrait des «Annales Géologiques des Pays Helléniques», 39, Fasc. A., 2002 PRELIMINARY NOTE ON THE LATE PLIOCENE FAUNA FROM VATERA (LESVOS, GREECE)* by J. DE VOS**, J. VAN DER MADE***, A. ATHANASSIOU****, G. LYRAS****, P.Y. SONDAAR***** & M.D. DERMITZAKIS**** I. INTRODUCTION There are six fossil vertebrate yielding sites near Vateri (Lesvos, Greece), these are the F, E, H, DS, T and U-sites. The material is kept in the Natural History Collection in the Museum of Vrissa, near Polychnitos on Lesvos Island. It is the aim of this paper to present the preliminary faunal list and describe or discuss some of the characteristic faunal elements. In future publications, each taxon will be more completely described and discussed. Measurements and their abbreviations Measurements are taken as indicated by VAN DER MADE & HUSSAIN (1994). In the figures and text measurements are indicated by their abbreviations. DAP Antero-posterior diameter DAPb Basal DAP DT Transverse diameter DTa DT of the anterior lobe of a tooth DTb Basal DT DTP DT of the posterior lobe of a tooth, or the proximal part of a bone Dist.
    [Show full text]
  • New Data on the Early Villafranchian Fauna from Vialette (Haute-Loire, France) Based on the Collection of the Crozatier Museum (Le Puy-En-Velay, Haute-Loire, France)
    ARTICLE IN PRESS Quaternary International 179 (2008) 64–71 New data on the Early Villafranchian fauna from Vialette (Haute-Loire, France) based on the collection of the Crozatier Museum (Le Puy-en-Velay, Haute-Loire, France) Fre´de´ric Lacombata,Ã, Laura Abbazzib, Marco P. Ferrettib, Bienvenido Martı´nez-Navarroc, Pierre-Elie Moulle´d, Maria-Rita Palomboe, Lorenzo Rookb, Alan Turnerf, Andrea M.-F. Vallig aForschungsstation fu¨r Quata¨rpala¨ontologie Senckenberg, Weimar, Am Jakobskirchhof 4, D-99423 Weimar, Germany bDipartimento di Scienze della Terra, Universita` di Firenze, Via G. La Pira 4, 50121 Firenze, Italy cICREA, A`rea de Prehisto`ria, Universitat Rovira i Virgili-IPHES, Plac-a Imperial Tarraco 1, 43005 Tarragona, Spain dMuse´e de Pre´histoire Re´gionale de Menton, Rue Lore´dan Larchey, 06500 Menton, France eDipartimento di Scienze della Terra, Universita` degli Studi di Roma ‘‘La Sapienza’’, CNR, Ple. Aldo Moro, 500185 Roma, Italy fSchool of Biological and Earth Sciences, Liverpool John Moore University, Liverpool L3 3AF, UK g78 rue du pont Guinguet, 03000 Moulins, France Available online 7 September 2007 Abstract Vialette (3.14 Ma), like Sene` ze, Chilhac, Sainzelles, Ceyssaguet or Soleilhac, is one of the historical sites located in Haute-Loire (France). The lacustrine sediments of Vialette are the result of a dammed lake formed by a basalt flow above Oligocene layers, and show a geological setting typical for this area, where many localities are connected with maar structures that have allowed intra-crateric lacustrine deposits to accumulate. Based on previous studies and this work, a faunal list of 17 species of large mammals has been established.
    [Show full text]
  • Télécharger L'article Complet Au Format
    Le gisement de vertébrés pliocenes de Çalta, Ankara, Turquie. 10. Bovidae Geneviève BOUVRAIN Laboratoire de Paléontologie des vertébrés, URA 1761 du CNRS, université Pierre-et-Marie-Curie, 4 place Jussieu, F-75252 Paris cedex 05 (France) Bouvrain G. 1998. — Bovidae, in Sen S. (éd.), Le gisement de vertébrés pliocènes de Çalta, Ankara, Turquie. 10, Geodiversitas 20 (3) : 467-485. RÉSUMÉ Cinq genres de Bovidae sont présents parmi les mammifères du gisement pliocène de Çalta (Turquie). Gazella emilii n.sp. montre des affinités avec certaines gazelles d'Asie centrale ; elle est très spécialisée par la longueur de ses métapodes. Tcbaltacerus longicornis n.g. n.sp. possède des caractères de caprins : orbites proéminentes, basioccipital coutt et large, métapodes trapus. Un troisième bovidé, malheureusement connu par seulement quelques pièces, pourrait être voisin de Koufotragus bailloudi. Enfin quelques fossiles MOTS CLES prouvent la présence d'une antilope proche de Gazellospira et d'un Pliocène, Hippotragini. À l'exception de Tcbaltacerus qui peut correspondre à un Turquie, milieu escarpé, les autres bovidés indiquent, par l'allongement remarquable mammifères, Bovidae. de leurs métapodes, un milieu ouvert. ABSTRACT Pliocene vertebrate locality of Calta, Ankara, Turkey. 10. Bovidae. The Pliocene mammal locality of Calta (Turkey) has yielded five bovid genera. Gazella emilii n.sp. shows close affinities with some gazelles from Central Asia, but the Turkish species has very specialized lengthened metapods. Tchaltacerus longicornis n.g. n.sp. shows caprine characters: wide projection of the dm of the orbits, wide basioccipital, short metapods. The third bovid, unfortunatly known by very few pieces, could be more or less closely related KEYWORDS to Koufotragus bailloudi.
    [Show full text]
  • Eastern Georgia and Western Azerbaijan, South Caucasus)
    Synopsis of the terrestrial vertebrate faunas from the Middle Kura Basin (Eastern Georgia and Western Azerbaijan, South Caucasus) MAIA BUKHSIANIDZE and KAKHABER KOIAVA Bukhsianidze, M. and Koiava, K. 2018. Synopsis of the terrestrial vertebrate faunas from the Middle Kura Basin (Eastern Georgia and Western Azerbaijan, South Caucasus). Acta Palaeontologica Polonica 63 (3): 441–461. This paper summarizes knowledge on the Neogene–Quaternary terrestrial fossil record from the Middle Kura Basin accumulated over a century and aims to its integration into the current research. This fossil evidence is essential in understanding the evolution of the Eurasian biome, since this territory is located at the border of Eastern Mediterranean and Central Asian regions. The general biostratigraphic framework suggests existence of two major intervals of the terrestrial fossil record in the area, spanning ca. 10–7 Ma and ca. 3–1 Ma, and points to an important hiatus between the late Miocene and late Pliocene. General aspects of the paleogeographic history and fossil record suggest that the biogeographic role of the Middle Kura Basin has been changing over geological time from a refugium (Khersonian) to a full-fledged part of the Greco-Iranian province (Meotian–Pontian). The dynamic environmental changes during the Quaternary do not depict this territory as a refugium in its general sense. The greatest value of this fossil record is the potential to understand a detailed history of terrestrial life during demise of late Miocene Hominoidea in Eurasia and early Homo dispersal out of Africa. Late Miocene record of the Middle Kura Basin captures the latest stage of the Eastern Paratethys regression, and among other fossils counts the latest and the easternmost occurence of dryopithecine, Udabnopithecus garedziensis, while the almost uninterrupted fossil record of the late Pliocene–Early Pleistocene covers the time interval of the early human occupation of Caucasus and Eurasia.
    [Show full text]
  • Virtual Museum” Context: the Permanent Challenge of Reconciliation of Diverging Scientific, Technical, Operational and Financial Objectives
    38 FOTOGRAMA DEL AUDIOVISUAL "ALEJANDRÍA, EL SUEÑO DE ALEJANDRO MAGNO" EL RANCHITO IMAGEN DIGITAL. MADRID. ESPAÑA, MESA PONENTES_1/ TABLE OF LECTURES_1 REINVENTANDO LA DIFUSIÓN. PROYECTOD DE DIFUSIÓN/ RETHINKING HERITAGE PRESENTATION. INNOVATIONS PROJECTS III Congreso Internacional de Arqueología e Informática Gráfica, Patrimonio e Innovación Sevilla 21-24 de Junio de 2011 39 The Persepolis3D project, the methodology of the virtual reconstruction of Persepolis Kourosh Afhami and Wolfgang Gambke persepolis3D.com, DemanaVision Object Oriented Virtual Visualization of Architecture and Archaeology, Germany Resumen It is imperative for museums to help their visitors in understanding the relationship between the exhibited archaeological findings and their original architectural/constructive and artistic contexts. Only in the interrelationship between the exhibited items and their structures of origin do the exhibits unfold their full expression and may be understood by the non-expert visitor. The virtual visualization of the ancient palaces of Persepolis, the Persepolis3D project, was created for this aim as well as providing a comprehensive image of the ancient palace complex for both professionals and interested laymen alike. Palabras Clave : PERSEPOLIS3D, PERSIAN ARCHITECTURE, VIRTUAL VISUALIZATION Abstract The first systematic and scholarly excavation of Persepolis was conducted by Ernst Herzfeld and Friedrich Krefter which led to the onsite reconstruction of the so- called 'Harem' in 1931. About forty years later, the Harem reconstruction became the basis for Krefter's drawings published in Persepolis-Rekonstruktionen in 1971. Our goal with this virtual reconstruction project is to continue and expand on Krefter's work using modern tools and technology not only to show the different perspectives drawn by Krefter, but also to show Persepolis from every angle and point of view both in pictures and animation with its original materials, lighting, and mood.
    [Show full text]
  • Reconstructing Life History Traits from Bone Histology in Extant and Fossil Ruminants
    Departament de Biologia Animal Biologia Vegetal i Ecologia Reconstructing life history traits from bone histology in extant and fossil ruminants Memòria presentada per Miren Nekane Marín Moratalla per a optar al títol de Doctor en Biologia, programa de doctorat en Biodiversitat del Departament de Biologia Animal Biologia Vegetal i Ecologia de la Universitat Autònoma de Barcelona, dirigida per: ‐ Dra. Meike Köhler, ICREA a l’Institut Català de Paleontologia Miquel Crusafont i professora associada al Departament d’Ecologia de la Universitat de Barcelona. ‐ Dr. Xavier Jordana, Institut Català de Paleontologia Miquel Crusafont. Dra. Meike Köhler Dr. Xavier Jordana Miren Nekane Marín Moratalla TESI DOCTORAL 2014 ABSTRACT The study of life histories is of special importance because it provides valuable insights into ecological conditions, biodiversity, demography, vulnerability and many other aspects of a species’ biology. Bone histology is a widely used tool to reconstruct vertebrate life histories, either by analysing primary bone tissue or by counting the number of growth marks (skeletochronology). However, it has long been considered that endotherms, unlike ectotherms, display a continuous or noncyclical bone growth, disabling bone histology for life history inferences in mammals. The general purpose of the research presented in this PhD Thesis is to challenge this statement, contributing to the foundations of mammalian bone histology as a tool for inferences on life history strategies. The specific aims are: i) to analyse the reliability of the skeletochronology in mammalian bone, ii) to explore the association of bone tissue features with environment, physiology, ontogeny and life history, and finally iii) to reconstruct life history traits in fossil and living mammals to get insights on life history evolution and conservation biology.
    [Show full text]
  • Archiv Für Naturgeschichte
    © Biodiversity Heritage Library, http://www.biodiversitylibrary.org/; www.zobodat.at Bericht über die wissenschaftlichen Leistungen in der Naturgeschichte der Säugethiere während des Jahres 1892. II. Systematik, Biologie und geographische Verbreitung. Von Paul Matsehie. I. Verzeichniss der Publikationen. [Die Namen der Aiitoren, welche über ausgestorbene Thiere geschrieben haben, sind gesperrt, diejenigen der Autoren, welche über recente Thiere ge- schrieben haben, fett gedruckt worden. Alle Arbeiten, bei welchen eine Jahres- zahl nicht angegeben worden ist, sind im Jahre 1892 erschienen. Diejenigen Arbeiten, deren Titel nur gegeben sind, waren mir nicht zugänglich und werden im nächsten Jahresberichte, soweit es möglich sein wird, im systematischen Theile ausgezogen werden ] Abbott, W. J. L. On the occurrence of Walrus in the Thames Valley. — P. Geol. Assoc. XII, p. 357. Adams, Lionel, E. Observations on Mole. — The Zoologist XVI, p. 421—422. Beobachtungen über Talpa in der Gefangenschaft. Allen, H. (1). On the Molars of the Pteropine Bats. — Proc. Ac. Nat. Sc. Philad. p. 172—173. Versuch bei den Molaren der Pteropodidue die Homologien der Höcker durchzuführen als Proso-Meta-Para- und Hypocone. Die Stenodermata sind in der Zahnbildung den Flughunden ähnlich. Molaren bei Cephalotes und Earpyia ; s. auch diesen Bericht I, p. 82. Allen (2), On the Foramen Magnum of the Common Porpoise, and on a Human Lower Jaw of unusual size. — Proc. Ac. Nat. Sc. Philad. p. 289. Das Foramen magnum von Tursiops tursio wird unten nicht vom Basioccipitale begrenzt, sondern von den Exoccipitalia; s. a. diesen Bericht 1, p. 83. © Biodiversity Heritage Library, http://www.biodiversitylibrary.org/; www.zobodat.at 202 Paul Matschie: Bericht über die wissenscliaftl.
    [Show full text]
  • A New Early Pleistocene Mammalian Fauna from Burdur Basin, SW Turkey
    Russian J. Theriol. 13(2): 5563 © RUSSIAN JOURNAL OF THERIOLOGY, 2014 A new Early Pleistocene mammalian fauna from Burdur Basin, SW Turkey Fatma Arzu Demirel, Serdar Mayda ABSTRACT. A new Early Pleistocene mammalian locality, referred to as Yassigüme from Burdur Basin of SW Anatolia is reported here for the first time. Here, we describe remains of an equid and bovids, most frequent elements of the fauna, as Equus sp., Gazellospira torticornis, and Leptobos cf. etruscus, all being the first records in Turkey. The coexistence of medium-sized bovine L. etruscus with spiral-horned antelope G. torticornis, and Equus sp. suggests Late Villafranchian age (~1.5 Ma) for Yassigüme. These records fill the gap in the paleobiogeographic range of these taxa in SE Mediterranean during Pleistocene. KEY WORDS: Leptobos, Gazellospira, Villafranchian, Early Pleistocene, Burdur Basin, Turkey. F. Arzu Demirel [[email protected]], Mehmet Akif Ersoy University, Faculty of Arts and Sciences, Deparment of Anthropology, Burdur, Turkey; S. Mayda [[email protected]], Ege University Natural History Museum, Izmir, Turkey. Íîâàÿ òåðèîôàóíà ðàííåãî ïëåéñòîöåíà èç áàññåéíà Áóðäóð, þãî-çàïàäíàÿ Òóðöèÿ Ô.À. Äåìèðåëü, Ñ. Ìàéäà ÐÅÇÞÌÅ. Îïèñûâàåòñÿ íîâàÿ ôàóíà ìëåêîïèòàþùèõ ðàííåãî ïëåéñòîöåíà ßññèãþìå (Yassigüme) èç áàññåéíà Áóðäóð, þãî-çàïàäíàÿ Òóðöèè. Ïðåîáëàäàþùèå â ìåñòîíàõîæäåíèè îñòàòêè áûêîâ è ëîøàäåé îïðåäåëåíû êàê Equus sp., Gazellospira torticornis è Leptobos cf. etruscus. Âñå ýòè ôîðìû âïåðâûå îáíàðóæåíû â Òóðöèè. Ñîâìåñòíîå ïðèñóòñòâèå ñðåäíåðàçìåðíîãî áûêà L. etruscus ñî ñïèðàëüíîðîãîé àíòèëîïîé G. torticornis è ëîøàäüþ Equus sp. óêàçûâàåò íà ïîçäíåâèëëàôðàíêñêèé âîçðàñò (~1,5 ìëí. ëåò) ôàóíû ßññèãþìå. Íîâûå íàõîäêè çàïîëíÿþò ïðîáåë â ïàëåîãåîãðàôè÷åñêîì ðàñïðîñòðàíåíèè ýòèõ òàêñîíîâ â ïëåéñòîöåíå þãî-âîñòî÷íîãî Ñðåäèçåìíîìîðüÿ.
    [Show full text]
  • Late Neogene and Early Quaternary Paleoenvironmental and Paleoclimatic Conditions in Southwestern Europe: Isotopic Analyses on Mammalian Taxa
    Late Neogene and Early Quaternary Paleoenvironmental and Paleoclimatic Conditions in Southwestern Europe: Isotopic Analyses on Mammalian Taxa Laura Domingo1*, Paul L. Koch1, Manuel Herna´ndez Ferna´ndez2,3, David L. Fox4, M. Soledad Domingo5, Marı´a Teresa Alberdi6 1 Earth and Planetary Sciences Department. University of California Santa Cruz, Santa Cruz, California, United States of America, 2 Departamento de Paleontologı´a, Universidad Complutense de Madrid, Madrid, Spain, 3 Departamento de Cambio Medioambiental, Instituto de Geociencias (UCM, CSIC), Madrid, Spain, 4 Department of Earth Sciences. University of Minnesota, Minneapolis, Minnesota, United States of America, 5 Museum of Paleontology, University of Michigan, Ann Arbor, Michigan, United States of America, 6 Departamento de Paleobiologı´a, Museo Nacional de Ciencias Naturales-CSIC, Madrid, Spain Abstract Climatic and environmental shifts have had profound impacts on faunal and floral assemblages globally since the end of the Miocene. We explore the regional expression of these fluctuations in southwestern Europe by constructing long-term records (from ,11.1 to 0.8 Ma, late Miocene–middle Pleistocene) of carbon and oxygen isotope variations in tooth enamel of different large herbivorous mammals from Spain. Isotopic differences among taxa illuminate differences in ecological niches. The d13C values (relative to VPDB, mean 210.361.1%; range 213.0 to 27.4%) are consistent with consumption of C3 vegetation; C4 plants did not contribute significantly to the diets of the selected taxa. When averaged by time interval to examine secular trends, d13C values increase at ,9.5 Ma (MN9–MN10), probably related to the Middle Vallesian Crisis when there was a replacement of vegetation adapted to more humid conditions by vegetation adapted to drier and more seasonal conditions, and resulting in the disappearance of forested mammalian fauna.
    [Show full text]
  • Gazellospira Torticornis (Aymard, 1854) from the Late Pliocene Locality of Sésklo (Thessaly, Greece) ⅲ
    GAZELLOSPIRA TORTICORNIS (AYMARD, 1854) FROM THE LATE PLIOCENE LOCALITY OF SÉSKLO (THESSALY, GREECE) Ⅲ Athanassios ATHANASSIOU1 ABSTRACT The locality of Sésklo (E. Thessaly, Greece) has yielded an interesting fossil fauna of Late Pliocene age (MNQ17). The Bovids are the most frequent elements, comprising mainly the genera Gazella and Gazellospira. The sample of Gazellospira torticornis is described in this study. Its morphology and dimensions are typical, showing no considerable differences in comparison to the Western European samples. Key words: Pliocene, Artiodactyla, Bovidae, Gazellospira, Thessaly, Greece. RESUMÉ GAZELLOSPIRA TORTICORNIS (AYMARD, 1854) DE LA LOCALITÉ PLIOCÈNE SUPÉRIEUR DE SÉSKLO (THESSALIE, GRÈCE) La localité de Sésklo a livré une faune intéressante d’âge Pliocène supérieur (MNQ17). Les Bovidés sont les éléments les plus fréquents. Il s’agit principalement de Gazella et de Gazellospira. L’échantillon de Gazellospira torticornis est décrit dans l’article présent. Comparé avec les échantillons d’Europe occidentale, aucune différence morphologique ou dimensionnelle n’est décelable. Mots-clés : Pliocène, Artiodactyles, Bovidé, Gazellospira, Thessalie, Grèce. INTRODUCTION The fossil fauna of Sésklo is already described in other papers (Symeonidis & Tataris, 1983; Symeonidis, 1992; Athanassiou, 1996; Kostopoulos & Athanassiou, The locality of Sésklo (Magnesia, Thessaly, Greece; 1997, 2005; Athanassiou, 2001, 2002a, 2002b). The fig. 1) is situated about 10 km west of the town of Vólos faunal list, given by Athanassiou (1996) (and, the capital of the Magnesia district. It is located in a ba- concerning the Artiodactyla, revised by Kostopoulos sin filled with Neogene fluvio-lacustrine clay sedi- & Athanassiou, 1997, 2005, and Athanassiou, ments. The basement of the basin is formed of 2002a, 2002b), includes Carnivora [Nyctereutes metamorphic rocks (peridotites, serpentinites and megamastoides (Pomel, 1843), Vulpes cf.
    [Show full text]