DOCSLIB.ORG

Multiscalar Porosity Structure of a Miocene Reefal Carbonate Complex

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Multiscalar Porosity Structure of a Miocene Reefal Carbonate Complex Research Collection Doctoral Thesis Multiscalar porosity structure of a miocene reefal carbonate complex Author(s): Jaeggi, David Publication Date: 2006 Permanent Link: https://doi.org/10.3929/ethz-a-005209372 Rights / License: In Copyright - Non-Commercial Use Permitted This page was generated automatically upon download from the ETH Zurich Research Collection. For more information please consult the Terms of use. ETH Library Diss. ETH Nr. 16519 Multiscalar porosity structure of a Miocene reefal carbonate complex A dissertation submitted to the SWISS FEDERAL INSTITUTE OF TECHNOLOGY (ETH) ZÜRICH For the degree of DOCTOR OF NATURAL SCIENCE presented by DAVID JAEGGI Dipl. Geologe Swiss Federal Institute of Technology (ETH) Zürich born September 2nd 1974 Mümliswil-Ramiswil (Solothurn) Accepted on the recommendation of Prof. Dr. Simon Löw, examiner Dr. Martin Herfort, co-examiner Prof. Dr. Flavio Anselmetti, co-examiner Dr. Philippe Pézard, co-examiner 2006 Acknowledgments 1 A) Acknowledgments This work has been conducted at the chair of Engineering Geology ETH Zurich in the framework of a European Union project called ALIANCE (Advanced logging investigations of aquifers in coastal environments) led by Dr. Philippe Pézard (University of Montpellier). I thank my supervisor Professor Simon Löw for his support and for giving me the opportunity to work with an excellent equipment and professional infrastructure within such an interesting geological environment. With Dr. Nathalie Van Meir I learnt to do borehole logging and to perform pumping tests under extreme climatic and geological conditions. The collaboration with Nathalie was extremely fruitful and on Mallorca she taught me lots of useful things about the Spanish mentality and language. Furthermore, I want to thank my co-examiner Dr. Martin Herfort who was not only of indispensable help in the field but as well extensively supported me during data analysis and the final stages of my thesis when I had to bring all this to paper. Besides the scientific support for my doctorate thesis he could motivate me additionally for a new hobby – speleology in active karstic systems. Furthermore, I would like to thank our collaborators within the Project namely Dr. Philippe Pézard, who supported me as co-examiner, Dr. Gerard Lods and all people I know from University of Montpellier for providing me with excellent logging data and for advising me during my doctorate thesis in the field and per email. Professor Modesto Montoto and his right hand Felix Mateos I thank for their introduction into digital image analysis and their enthusiasm for my work. This work would never have been possible, if there were not the Gobiern Balear, which supported our project on Mallorca with manpower and finally with a 28 ton state of the art drilling machine. Among numerous people from the Gobiern Balear to whom I had contact, I want to emphasize the two hydrogeologists Concha Gonzalez and Alfredo Baron, the man who knows every well on Mallorca, Ramon and the driller with the sunglasses Juan Antonio. All those people were always very helpful in the field and found time despite their full agenda. For a Swiss geologist Miocene reefal carbonates are exotic geology, which is not present in our country. However, with Professor Luis Pomar I had support from a man who has been working almost 30 years on the platform of Llucmajor and who knows almost everything about it. I could enjoy his excursions and courses, which built together an excellent introduction for the geology at our test site near Campos. At ETH Zurich I got further support in determining facies from thin sections and rock samples by Dr. Heinz Furrer, whose course about paleoecology of reefs was ideal for better understanding the geology of my study area. Professor Flavio Anselmetti helped me determining porosity and pore types of these carbonate rocks. With his experience in carbonate rocks he could give me many useful hints about how to solve specific technical and scientific problems. Furthermore, he agreed to be a co-examiner of my thesis. Thin sections built an important part of my work. I thank Frowin Pirovino for the preparation of dozens of thin sections and the photographer Urs Gerber for scanning them all. He furthermore introduced me into professional photography, which I directly applied on the semi-industrial core photography (imaging 500 m of cored material). Furthermore, I would like to thank Gabriele Peschke from the institute of building materials for the ESEM-images, which she made with both interest and high precision. Professor Renee Heilbronner from University of Basel provided me with software for digital image analysis and helped me 2 Acknowledgments solving specific problems. Furthermore, she regularly gives a course about digital image analysis in geoscience, which I can warmly recommend. Dr. Hansruedi Maurer and Dr. Sven Friedl acquired and processed the geophysical data of our project. Their geoelectrical and seismic tomograms were of eminent importance for the interpretation for the evolution of the pore space. Especially Hansruedi Maurer I thank for the critical review of the geophysical part of my work. Marcel Mettler from the workshop of the geological institute provided me with many useful devices, like for example the extensively used cell for standard falling head permeability tests. Furthermore, I like to thank all the people of the Engineering Geology group at ETH Hönggerberg, who supported or entertained me during the last four years! Important contributions I got from Dr. Frank Lemy, who gave me an introduction into Matlab and who helped me in establishing certain scripts. From Dr. Keith Evans I got support in the very beginning – he taught me how to use the logging equipment and how to outwit inadequate technique with simple tricks in the field. And finally this work would not have been possible without the warm support and encouraging words of my family and Mirjam, who with a big understanding accepted my physical and sometimes as well mental absence. Acknowledgments 3 Table of contents 5 B) Table of contents A) ACKNOWLEDGMENTS ............................................................................................................................ 1 B) TABLE OF CONTENTS.............................................................................................................................. 5 C) LIST OF FIGURES ...................................................................................................................................... 9 D) LIST OF TABLES ...................................................................................................................................... 17 E) ABSTRACT – ZUSAMMENFASSUNG................................................................................................... 19 1. INTRODUCTION....................................................................................................................................... 25 1.1. OBJECTIVE AND SCIENTIFIC APPROACH .................................................................................................. 25 1.2. GEOLOGICAL AND HYDROGEOLOGICAL OUTLINE ................................................................................... 27 1.3. CONTENTS OF THE THESIS....................................................................................................................... 28 2. ROCK-MATRIX-SCALE POROSITY STRUCTURE OF A MIOCENE REEFAL CARBONATE, MALLORCA (SPAIN) ............................................................................................................................... 31 2.1. INTRODUCTION....................................................................................................................................... 32 2.2. GEOLOGICAL OUTLINE OF THE STUDY AREA........................................................................................... 34 2.2.1. Regional overview and previous work............................................................................................ 34 2.2.2. Pore types encountered at the test site............................................................................................ 35 2.2.3. Lithofacies types and diagenesis at the test site.............................................................................. 37 2.3. METHODS ............................................................................................................................................... 41 2.3.1. Sampling strategy ........................................................................................................................... 41 2.3.2. Measurements on 1 inch mini-cores ............................................................................................... 42 2.3.3. Digital image analysis on thin sections (Scan, ESEM)................................................................... 42 2.3.3.1. Segmentation of TSS and ESEM-images ........................................................................................ 44 2.3.3.2. The integrated approach of TOP.................................................................................................... 45 2.3.3.3. Anisotropy and heterogeneity......................................................................................................... 46 2.3.3.4. Pore shape factor............................................................................................................................ 48 2.3.3.5. Pore size distribution.....................................................................................................................
Load more

Recommended publications
  • The Genus Phlyctenodes Milne Edwards, 1862 (Crustacea: Decapoda: Xanthidae) in the Eocene of Europe
    350 RevistaBusulini Mexicana et al. de Ciencias Geológicas, v. 23, núm. 3, 2006, p. 350-360 The genus Phlyctenodes Milne Edwards, 1862 (Crustacea: Decapoda: Xanthidae) in the Eocene of Europe Alessandra Busulini1,*, Giuliano Tessier2, and Claudio Beschin3 1 c/o Museo di Storia Naturale, S. Croce 1730, I - 30125, Venezia, Italia. 2 via Barbarigo 10, I – 30126, Lido di Venezia, Italia. 3 Associazione Amici del Museo Zannato, Piazza Marconi 15, I - 36075, Montecchio Maggiore (Vicenza), Italia. * [email protected] ABSTRACT A systematic review of the crab genus Phlyctenodes Milne Edwards, 1862 is carried out. Based on carapace features, this taxon is placed in the subfamily Actaeinae, family Xanthidae MacLeay, 1838. Species attributed to this genus are known from Eocene reef environments in Europe. Preservation of crustacean remains in this kind of environment is very rare, and it could explain scarcity of specimens of this genus. For the fi rst time, pictures of types of this genus described during the XIX century and the fi rst decades of the XX century are presented. A study of recently collected specimens from the Eocene of Veneto (Italy) allows to clarify relationships between Phlyctenodes krenneri Lörenthey, 1898 and P. dalpiazi Fabiani, 1911. Presence of P. tuberculosus Milne Edwards, 1862 among the new material is documented. The other known species of this genus, P. hantkeni Lörenthey, 1898 is placed in Pseudophlyctenodes new genus on the basis of differences in morphological features. Key words: Crustacea, Decapoda, Phlyctenodes, systematic review, Eocene, Italy. RESUMEN Se presenta una revisión sistemática del género de cangrejo Phlyctenodes Milne Edwards, 1862. Con base en las características del caparazón, este taxon es ubicado en la subfamilia Actaeinae, familia Xanthidae MacLeay, 1838.
    [Show full text]
  • Földtani Közlöny 134/2,237-255
    Földtani Közlöny 134/2,237-255. (2004) Budapest History of reef-dwelling Decapod Crustaceans from the Palaeocene to the Miocene with comments about Mesozoic occurrences A zátonylakó tízlábú rákok története a faleocéntől a miocénig — a mezozoos előfordulások rövid áttekintésével Pál Mihály MÜLLER1 (1 ábra, 1 táblázat) Keywords: Crustacea, Decapoda, Palaeocene, Miocene, reef environment, adaptation, fossilization, collection, evaluation bias Tárgyszavak: tízlábú rákok, paleocén, miocén, zátony környezet, adaptáció, fosszilizáció,gyűjtés, hibák a kiértékelésben Összefoglalás A bentosz egyik, ökológiai szempontból igen nagy jelentőségű és nagy diverzitású csoportjáról, a tízlábú rákokról az őslénytani ismeretanyag nagyon szegényes, s ez különösen érvényes a zátonyokon élő együttesekre. A zátonyokon élt tízlábú rákok története tehát nehezen követhető az adatok tér- és időbeli hiányossága miatt. A kainozoikumból viszonylag több adat van, mint a mezozoikumból, ezért a paleocéntől a miocén végéig részletesebben tárgyaljuk a faunában észlelt változásokat. Az adatok zöme Európából származik. A fosszilizálódás és a gyűjtés torzító hatása elsősorban a nagy méretű fajok megmaradásának, illetve megtalálásának kedvez. Zátonykörnyezetben a fosszilizálódás viszonylag kevéssé szelektál, viszont a gyűjtési módszer, ha felületes (ami, különösen régebben, általános volt), nagyon erősen kedvezhet a nagyobb példányok és fajok megtalálásának. Ezért gazdag, kis fajokat is tartalmazó faunákat általában az egyetemi városok, kutatóközpontok közelében hamarabb várhatunk,
    [Show full text]
  • A Catalogue of the Type and Figured Fossil Decapod Crustaceans in the Collections of the Geological Survey of Austria in Vienna
    JAHRBUCH DER GEOLOGISCHEN BUNDESANSTALT Jb. Geol. B.-A. ISSN 0016–7800 Band 156 Heft 1–4 S. 127–177 Wien, Dezember 2016 A catalogue of the type and figured fossil decapod crustaceans in the collections of the Geological Survey of Austria in Vienna MATÚš HYžNÝ1, 2 & IRENE ZORN3 17 Plates Österreichische Karte 1:50.000 BMN / UTM 41 Deutsch Wagram / NM 33-12-20 Wien 48 Vöcklabruck / NM 33-10-29 Vöcklabruck 71 Ybbsitz / NL 33-02-04 Gaming 107 Mattersburg / NL 33-03-08 Mattersburg 207 Arnfels / NL 33-05-11 Leibnitz Crustacea Decapoda Triassic Jurassic Neogene Paleogene Palaeontological Collection Contents Abstract ............................................................................................... 127 Zusammenfassung ....................................................................................... 127 Introduction............................................................................................. 128 List of the type and figured material .......................................................................... 128 Acknowledgements....................................................................................... 139 References ............................................................................................. 140 Index of genus and species names........................................................................... 142 Plates ................................................................................................. 144 Abstract The present catalogue lists and figures the type and figured
    [Show full text]
  • Anomura, Galatheoidea) from the Upper Miocene in the Maroni-Psematismenos Basin of Cyprus
    A new shallow-marine munidopsid (Anomura, Galatheoidea) from the Upper Miocene in the Maroni-Psematismenos Basin of Cyprus R.H.B. Fraaije Fraaije, R.H.B. A new shallow-marine munidopsid (Anomura, Galatheoidea) from the Upper Miocene in the Maroni-Psematismenos Basin of Cyprus. In: Fraaije, R.H.B., Hyžný, M., Jagt, J.W.M., Krobicki, M. & Van Bakel, B.W.M. (eds.), Proceedings of the 5th Symposium on Mesozoic and Cenozoic Decapod Crustaceans, Krakow, Poland, 2013: A tribute to Pál Mihály Müller. Scripta Geologica, 147: 233-239, 1 fig., 1 pl., Leiden, October 2014. René H.B. Fraaije, Oertijdmuseum De Groene Poort, Bosscheweg 80, 5283 WB Boxtel, the Netherlands ([email protected]). Key words – Decapoda, new genus, new species, Mediterranean, Cenozoic. Several well-preserved remains of a new munidopsid anomuran, Palmunidopsis muelleri n. gen., n. sp., are described from a Late Miocene (Tortonian-Messinian) reef-associated decapod crustacean faunule of southern Cyprus. This is the first record of a Late Miocene representative of the family. The occurrence in very shallow-water, reefal limestones of the Koronia Member (Pakhna Formation) in southern Cyprus is atypical in comparison to the ecology of extant munidopsids. Contents Introduction ............................................................................................................................................................ 233 Systematic palaeontology .............................................................................................................................
    [Show full text]
  • Daira Speciosa Reuss, 1871 (Crustacea, Decapoda, Xanthidae
    BolI. Soco Hist. Nat. Balears, 33 (1989-1990): 81-85 Palma de Mallorca. DAIRA SPECIOSA REUSS, 1871 (CRUSTACEA, DECA­ PODA, XANTHIDAE) EN EL MIOCENO DE LA ISLA DE MALLORCA (BALEARES) LL. GARCIA SOCIAS,1 PALABRAS CLAVE: Crustacea, Decapoda, Mioceno, Mediterráneo occidental. KEY WORDS: Crustacea, Decapoda, Miocene, Western Mediterranean. RESUMEN. Se comunica el hallazgo de restos del cangrejo fósil Daira speciosa Reuss 1871, en depósitos arrecifales del Mioceno superior del Sur de la Isla de Mallorca (Baleares, Mediterrá­ neo Occidental). Se completa la nota con algunos datos sobre la paleofauna carcínica de las Baleares. SUMMARY. DAlRA SPECIOSA REUSS 1871, IN THE MIO CENE OF MAJORCA ISLAND (BALEARICS) (CRUSTACEA, DECAPODA, XANTHIDAE). Remains of the fossil crab Daira speciosa Reuss 1871 have been discovered in reef deposits on the Upper Miocene of Majorca Island (Balearics, Wes­ tern Mediterranean). Other data of the carcinic palaeofauna of the Balearic Island are given. RESUM. DAlRA SPECIOSA REUSS 1871 (CRUSTACEA, DECAPODA, XANTHIDAE), AL MIOCE DE L'I­ LLA DE MALLORCA (BALEARS). Es comunica la troballa de restes del cranc fossil Daira speciosa Reuss 1871, als diposits d'esculls del Mioce superior, al Sud de l'Illa de Mallorca. Es donen també algunes dades sobre la resta de la paleofauna carcínica de les Balears. INTRODUCCIÓN Las referencias de Crustáceos decápodos fósiles en las Islas Baleares son muy escasas, limitándose hasta el momento a cuatro especies: Cyphoplax im­ pressa (Haime, 1855) del Mioceno de Mallorca y, por otra parte, Eriphia ve- 1 Museu Balear de Ciencies Naturals, Apartat de Correus nO 55, 07100 Sóller, Illes Balears. 82 LL. GARCIA SOCIAS rrucosa (Forskal, 1775), Xantho poressa (Olivi, 1792) y Ocypoda cursor (Lin­ né, 1758) del Cuaternario de la misma isla (HAIME, 1855; CUERDA, 1975; VÍA 1966; SOLÉ & VÍA, en prensa).
    [Show full text]
  • Decapod Crustaceans from the Retznei Quarry, Styrian Basin, Austria
    Bulletin of the Mizunami Fossil Museum, no. 40 (2014), p. 29–50, 4 pls., 1 table. ©2014,MizunamiFossilMuseum Middle Miocene “Badenian” (Langhian) decapod crustaceans from the Retznei quarry, Styrian Basin, Austria Joe S. H. Collins The Natural History Museum, Cromwell Road, London SW7 5BD and 8, Shaws Cottages, Perry Rise, London, SE23 2QN, England Abstract Thirty-four species (of which two are represented in the present collection by plaster casts) of anomuran and brachyuran decapods have been found in the Middle Miocene Langhian “Badenian” in the Retznei quarry, Stryrian Basin, Austria. Of these, twenty-nine are determined, some tentatively, to species level. Six new species are described: Pisidia ? subnodosa sp. nov., Pagurus retznensis sp. nov., Dromia evae sp. nov., Portunus muelleri sp. nov., Glabropilumnus nitidus sp. nov. and Eomaldivia friebei sp. nov. Previously described species are Callianassa”sp.aff.“Callianassa” sismondae A. Milne-Edwards, “Callianassa” almerai Müller, Galathea weinfuerteri Bachmeyer, Petrolisthes haydni Müller, Pisidia viai Müller, Dardanus hungaricus L!renthey in L!renthey and Beurlen, ‘Anapagurus’ miocenicus Müller, Calappa praelata L!renthey in L!renthey and Beurlen (plaster cast), Kerepesia viai Müller, Kromtitis koberi (Bachmayer and Tollman), Charybdis fragilis (Müller), Charybdis mathiasi Müller, Lobocarcinus sp. aff. sismondai (von Meyer), Carpilius antiquus Glaessner, Daira speciosa (Reuss), Hyastenus sp., Liocarcinus sp. aff. rakosensis L!renthey in L!renthey and Beurlen (plaster cast), Pilumnus sp. aff. mediterraneus (L!renthey), Pilumnus sp., Panopeus wroni Müller, Chlorodiella juglans Müller, Chlorodiella loczyi Müller, Chlorodiella mediterranea (L!renthey in L!renthey and Beurlen), Chlorodiella tetenyensis Müller, Xantho moldavicus (Yanakevich), Pilodius vulgaris (Glaessner), Haydnella steiningeri Müller and Majidae gen.
    [Show full text]
  • The Medobory Hills (Ukraine): Middle Miocene Reef Systems in the Paratethys, Their Biological Diversity and Lithofacies
    BIULETYN PAŃSTWOWEGO INSTYTUTU GEOLOGICZNEGO 449: 147–174, 2012 R. THE MEDOBORY HILLS (UKRAINE): MIDDLE MIOCENE REEF SYSTEMS IN THE PARATETHYS, THEIR BIOLOGICAL DIVERSITY AND LITHOFACIES MIODOBORY – ŚRODKOWOMIOCEŃSKI SYSTEM RAFOWY, JEGO ZRÓŻNICOWANIE BIOLOGICZNE I LITOFACJE MARCIN GÓRKA1, BARBARA STUDENCKA2, MAREK JASIONOWSKI3, URSZULA HARA3, ANNA WYSOCKA1, ANDRIY POBEREZHSKYY4 Abstract. The unique Middle Miocene reef belt formed within the Paratethyan realm constitutes at present the Medobory Hills in western Ukraine and northernmost Moldova. Not only is the size of this structure (almost 300 km long) quite unusual, but also the develop- ment of peculiar facies and their spatial distribution. Two distinct reef generations appear in Medobory (Late Badenian and Early Sarma- tian), both separated by a sharp erosional boundary. Two Upper Badenian calcareous lithofacies dominate – organodetrital and biohermal (with coralline-algae as main framework builders accompanied by a rich invertebrate assemblage). The Lower Sarmatian strata, although megascopically very similar to Upper Badenian ones, differ drastically when studied closely. The main reef components here are serpulids and microbialites, usually with ubiquitous, but taxonomically highly impoverished fauna. Differences in lithofacies and biotic communities between both reef systems unveil open-marine environment during formation of Upper Badenian reefs and a drastic change of conditions at the Badenian/Sarmatian boundary (including emersion and intense weathering). The Early Sarmatian basin was established soon after and highly restricted conditions prevailed in it (e.g. with mesohaline waters and intense evaporation occurring simultaneously); its deposits are the last record of Middle Miocene sedimentation within the Medobory area. Key words: coralline algae-vermetid reefs, serpulid-microbialite reefs, lithofacies, biodiversity, Badenian/Sarmatian boundary, Ukraine, Moldova.
    [Show full text]
  • A New Coral-Associated Decapod
    [Palaeontology, Vol. 53, Part 6, 2010, pp. 1315–1348] A NEW CORAL-ASSOCIATED DECAPOD ASSEMBLAGE FROM THE UPPER MIOCENE (MESSINIAN) UPPER CORALLINE LIMESTONE OF MALTA (CENTRAL MEDITERRANEAN) by MICHAEL GATT* and ANTONIO DE ANGELI à *‘Cidaris’, 18 Hal-Bajjada Street, Rabat RBT2030, Malta; e-mail [email protected] Piazzetta Nostro Tetto, 9, 36100 Vicenza, Italy àMuseo Civico G. Zannato, Piazza Marconi, 15, 36075 Montecchio Maggiore, Vicenza, Italy; e-mail [email protected] Typescript received 13 May 2009; accepted in revised form 10 November 2009 Abstract: A rich coral-associated decapod assemblage is D’Oliveira, 1888, are also recorded for the first time from recorded from the ‘Depiru Beds’ of the upper part of the Malta. Other Neogene coral-associated decapod assemblages Upper Coralline Limestone (Messinian, Upper Miocene), are investigated and correlated with the new assemblage from from the island of Malta. Nineteen species within 17 genera Malta. The migration of taxa between the Mediterranean have been discovered, where 14 genera are new for Malta. region and the Paratethys, particularly during the Lower Four new species are described, namely Micippa annamariae Badenian (Langhian), is evidenced by the strong affinity of sp. nov., Pilumnus scaber sp. nov., Panopeus muelleri sp. nov. the Maltese decapod assemblage with that of the Middle and Herbstia melitense sp. nov. Herbstia melitense sp. nov. Miocene Badenian assemblages from Hungary, Poland and constitutes the first record of the genus from the fossil Ukraine. Upper Miocene, Messinian assemblages from Spain, record in the Mediterranean region. This discovery more Algeria and Morocco are also similar to that from Malta.
    [Show full text]
  • Series Palaeontologica
    gedogica hungadca FASCICULI INSTITUTI GEOLOGICI HUNGÁRIÁÉ AD ILLUSTRANDAM NOTIONEM GEOLOGICAM ET PALAEONTOLOGICAM SERIES PALAEONTOLOGICA FASCICULUS 42 Vlllth RCMNS k CONGRESS INSTITUTUM GEOLOGICUM HUNGARICUM Tffrm ~M BUDAPESTINI, 1984 GEOLOGICA HUNGARICA FASCICULI INSTITUTI GEOLOGICI HUNGÁRIÁÉ AD ILLUSTRANDAM NOTIONEM GEOLOGICAM ET PALAEONTOLOGICAM SERIES PALAEONTOLOGICA FASCICULUS 42 DR. MÜLLER PÁL: A BÁDENI EMELET TÍZLÁBŰ RÁKJAI DR. PÁL MÜLLER: DECAPOD CRUSTACEA OF THE BADENIAN c* *- \ IX- JOHN S. GARTH , Allan Hancock Foundation University of Southern California Los Angstes, California 90007 MAR 1 - 1985 INSTITUTUM GEOLOGICUM HUNGARICUM BUDAPESTINI, NOVEMBER 1984 Lektor: DB. DUDICH ENDRE Szakszerkesztő: PIROS CHRISTA Az angol szöveg a szerző munkája Nyelvi lektor: DB. MIKLÓS MÜLLER Technikai szerkesztő: CSABAY LÁSZLÓKÉ GARAMSZEGI KÁROLYNÉ HU ISSN 03 67 4150 A kézirat lezárva 1984. január 15-én Megjelent a Műszaki Könyvkiadó gondozásában Budapest, 1984 Felelős kiadó: DR. HÁMOR GÉZA Műszaki vezető: Kőrizs Károly Műszaki szerkesztő: Metzker Sándor A könyv formátuma: A4 Terjedelem: 40 A5 ív Példányszám: 880 Ábrák száma: 12 +fény képtáblák Betűcsalád és -méret: Extended, gm/gm Papír minősége: 80 g ofszet és 120 g műnyomó Azonossági szám: 01486 84.2339 Egyetemi Nyomda, Budapest, 1984 Felelős vezető: Sümeghi Zoltán igazgató TARTALOM - CONTENTS Bevezetés 5 A bádeni emelet és a Középső Paratethys 6 A bádeni emelet rákjaival foglalkozó irodalom áttekintése 7 A bádeni emelet rákjainak gyűjteményi lelőhelyei 8 Munkamódszerek, preparálás 9 A fontosabb
    [Show full text]
  • The Genus Phlyctenodes Milne Edwards, 1862 (Crustacea: Decapoda: Xanthidae) in the Eocene of Europe Revista Mexicana De Ciencias Geológicas, Vol
    Revista Mexicana de Ciencias Geológicas ISSN: 1026-8774 [email protected] Universidad Nacional Autónoma de México México Busulini, Alessandra; Tessier, Giuliano; Beschin, Claudio The genus Phlyctenodes Milne Edwards, 1862 (Crustacea: Decapoda: Xanthidae) in the Eocene of Europe Revista Mexicana de Ciencias Geológicas, vol. 23, núm. 3, 2006, pp. 350-360 Universidad Nacional Autónoma de México Querétaro, México Available in: http://www.redalyc.org/articulo.oa?id=57223311 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 350 RevistaBusulini Mexicana et al. de Ciencias Geológicas, v. 23, núm. 3, 2006, p. 350-360 The genus Phlyctenodes Milne Edwards, 1862 (Crustacea: Decapoda: Xanthidae) in the Eocene of Europe Alessandra Busulini1,*, Giuliano Tessier2, and Claudio Beschin3 1 c/o Museo di Storia Naturale, S. Croce 1730, I - 30125, Venezia, Italia. 2 via Barbarigo 10, I – 30126, Lido di Venezia, Italia. 3 Associazione Amici del Museo Zannato, Piazza Marconi 15, I - 36075, Montecchio Maggiore (Vicenza), Italia. * [email protected] ABSTRACT A systematic review of the crab genus Phlyctenodes Milne Edwards, 1862 is carried out. Based on carapace features, this taxon is placed in the subfamily Actaeinae, family Xanthidae MacLeay, 1838. Species attributed to this genus are known from Eocene reef environments in Europe. Preservation of crustacean remains in this kind of environment is very rare, and it could explain scarcity of specimens of this genus. For the fi rst time, pictures of types of this genus described during the XIX century and the fi rst decades of the XX century are presented.
    [Show full text]
  • Compendium of Marine Species from New Caledonia
    fnstitut de recherche pour le developpement CENTRE DE NOUMEA DOCUMENTS SCIENTIFIQUES et TECHNIQUES Publication editee par: Centre IRD de Noumea Instltut de recherche BP A5, 98848 Noumea CEDEX pour le d'veloppement Nouvelle-Caledonie Telephone: (687) 26 10 00 Fax: (687) 26 43 26 L'IRD propose des programmes regroupes en 5 departements pluridisciplinaires: I DME Departement milieux et environnement 11 DRV Departement ressources vivantes III DSS Departement societes et sante IV DEV Departement expertise et valorisation V DSF Departement du soutien et de la formation des communautes scientifiques du Sud Modele de reference bibliographique it cette revue: Adjeroud M. et al., 2000. Premiers resultats concernant le benthos et les poissons au cours des missions TYPATOLL. Doe. Sei. Teeh.1I 3,125 p. ISSN 1297-9635 Numero 117 - Octobre 2006 ©IRD2006 Distribue pour le Pacifique par le Centre de Noumea. Premiere de couverture : Recifcorallien (Cote Quest, NC) © IRD/C.Oeoffray Vignettes: voir les planches photographiques Quatrieme de couverture . Platygyra sinensis © IRD/C GeoITray Matt~riel de plongee L'Aldric, moyen sous-marine naviguant de I'IRD © IRD/C.Geoffray © IRD/l.-M. Bore Recoltes et photographies Trailement des reeoHes sous-marines en en laboratoire seaphandre autonome © IRD/l.-L. Menou © IRDIL. Mallio CONCEPTIONIMAQUETIElMISE EN PAGE JEAN PIERRE MERMOUD MAQUETIE DE COUVERTURE CATHY GEOFFRAY/ MINA VILAYLECK I'LANCHES PHOTOGRAPHIQUES CATHY GEOFFRAY/JEAN-LoUIS MENOU/GEORGES BARGIBANT TRAlTEMENT DES PHOTOGRAPHIES NOEL GALAUD La traduction en anglais des textes d'introduction, des Ascidies et des Echinoderrnes a ete assuree par EMMA ROCHELLE-NEwALL, la preface par MINA VILAYLECK. Ce document a ete produit par le Service ISC, imprime par le Service de Reprographie du Centre IRD de Noumea et relie avec l'aimable autorisation de la CPS, finance par le Ministere de la Recherche et de la Technologie.
    [Show full text]
  • Daira Speciosa Reuss, 1871 (Crustacea, Deca- Poda
    Boll. Soco Hist. Nat. Balears, 33 (1989-1990): 81-85 Palma de Mallorca. DAIRA SPECIOSA REUSS, 1871 (CRUSTACEA, DECA­ PODA, XANTHIDAE) EN EL MIOCENO DE LA ISLA DE MALLORCA (BALEARES) LL. GARCIA SOCIAS,1 PALABRAS CLAVE: Crustacea, Decapoda, Mioceno, Mediterráneo occidental. KEY WORDS: Crustacea, Decapoda, Miocene, Western Mediterranean. RESUMEN. Se comunica el hallazgo de restos del cangrejo fósil Daira speciosa Reuss 1871, en depósitos arrecifales del Mioceno superior del Sur de la Isla de Mallorca (Baleares, Mediterrá­ neo Occidental). Se completa la nota con algunos datos sobre la paleofauna carcínica de las Baleares. SUMMARY. DAlRA SPECIOSA REUSS 1871, IN THE MIO CENE OF MAJORCA ISLAND (BALEARICS) (CRUSTACEA, DECAPODA, XANTHIDAE). Remains of the fossil crab Daira speciosa Reuss 1871 have been discovered in reef deposits on the Upper Miocene of Majorca Island (Balearics, Wes­ tern Mediterranean). Other data of the carcinic palaeofauna of the Balearic Island are given. RESUM. DAlRA SPECIOSA REUSS 1871 (CRUSTACEA, DECAPODA, XANTHIDAE), AL MIOCE DE L'I­ LLA DE MALLORCA (BALEARS). Es comunica la troballa de restes del cranc fossil Daira speciosa Reuss 1871, als diposits d'esculls del Mioce superior, al Sud de l'Illa de Mallorca. Es donen també algunes dades sobre la resta de la paleofauna carcínica de les Balears. INTRODUCCIÓN Las referencias de Crustáceos decápodos fósiles en las Islas Baleares son muy escasas, limitándose hasta el momento a cuatro especies: Cyphoplax im­ pressa (Haime, 1855) del Mioceno de Mallorca y, por otra parte, Eriphia ve- 1 Museu Balear de Ciencies Naturals, Apartat de Correus nO 55, 07100 Sóller, Illes Balears. 82 LL. GARCIA SOCIAS rrucosa (Forskal, 1775), Xantho poressa (Olivi, 1792) y Ocypoda cursor (Lin­ né, 1758) del Cuaternario de la misma isla (HAIME, 1855; CUERDA, 1975; VÍA 1966; SOLÉ & VÍA, en prensa).
    [Show full text]