Calliderma Atagensis, Un Estel·Làrid De L'eocè De La Tossa De Montbui

Total Page:16

File Type:pdf, Size:1020Kb

Calliderma Atagensis, Un Estel·Làrid De L'eocè De La Tossa De Montbui Miscellanea Aqualatensia, 18 (2019), p. 198-207 Calliderma atagensis, un estel·làrid de l’eocè de la Tossa de Montbui Josep Llansana i Marcè Centre d’Estudis Comarcals d’Igualada (CECI) Calliderma atagensis, una estrella de Calliderma atagensis, a starfisch from mar del eoceno de la Tossa de Montbui the eocene in Tossa de Montbui RESUMEN ABSTRACT El descubrimiento excepcional de una es- The exceptional discovery of a Callider- trella de mar fósil Calliderma atagensis ma atagensis starfish, complete with all completa con todas sus piezas, nos permi- its pieces, allows us to undertake a detai- te hacer un estudio muy detallado de su led study of its morphology as well as the morfología, así como el ensamblaje de las assembly of the 580 pieces that compose 580 piezas que la componen. Asimismo, it. Furthermore, it will enable us to carry servirá para hacer una revisión de su ubi- out a revision of its location within the cación dentro de la familia Goniasteridae. Goniasteridae family. PALABRAS CLAVE: Paleontología, descubri- KEYWORDS: Paleontology, discovery, star- miento, estrella de mar, Eoceno superior fish, Upper Eocene INTRODUCCIÓ Ara fa anys, en una excursió pels voltants de la Tossa de Montbui, vaig tenir la sort de trobar una estrella de mar fòssil completa. L’estel·làrid es tro- bava en una marga, totalment desarticulat amb els ossicles solts, però agru- pats, cosa que en va permetre poder agafar-la amb tot l’espai que ocupava. La troballa és excepcional, ja que rarament es troben exemplars complets, ja que els ossicles dels estel·làrids estan units per membranes musculars, que es destrueixen ràpidament en morir l’animal. Per això, el més corrent és trobar peces marginals aïllades i disperses. 201 MISCELLANEA_18.indd 201 18/6/19 17:33 Josep Llansana i Marcè SITUACIÓ GEOGRÀFICA I GEOLÒGICA El jaciment on fou trobat l’asteroïdeu es situa al vessant nord de la Tos- sa de Montbui i a tres quilòmetres al sud-oest del cap del municipi dins de la comarca de l’Anoia. (Fig.1) Geològicament, s’ubica a la Depressió Central Catalana, que juntament amb el Pirineu i les Serralades Costaneres conformen les tres principals uni- tats geològiques de Catalunya. A la part inferior de l’era Terciària, fa entre 60 i 35 milions d’anys, la Depressió Central era una conca de sedimentació, a voltes continental i a voltes marina i que anava més enllà dels límits de Cata- lunya amb l’Aragó fins a l’Empordà. Fa uns 40 milions d’anys, era ocupada Figura 1. 202 MISCELLANEA_18.indd 202 18/6/19 17:33 Calliderma atagensis, un estel·làrid de l’eocè de la Tossa de Montbui per un mar que formava part d’un gran oceà anomenat Tethys (el qual s’este- nia des de l’actual mar Carib fins a Indonèsia, passant pel sud d’Europa, Orient mitjà, Pakistan i l’Índia). Era el període Eocè, pis Bartonià. Abad (2001) hi va aixecar una sèrie estratigràfica, amb la següent suc- cessió de baix a dalt: (Fig.2) La base de la sèrie no ha pogut ser observada, ni tampoc el sostre per estar amagades per enderrocs de pendent actuals. En la primera de les intercalacions, situada a 4 m de la base, es troben (mostra 1) discociclines i valves soltes de: Chlamys biarritzensis (D’Archiac, 1848) En la segona intercalació, a 8 m de la base i separada de l’anterior per 1 m de lutites grises, es troba una abundant fauna formada per briozous ra- mosos trencats i altres conulàrids i per abundants mol·luscs. En Pterio- morpha (mostra 2), es dona el següent contingut: Figura 2. Columna estratigráfica del jaciment del Peu Nord de la Tossa de Montbui 203 MISCELLANEA_18.indd 203 18/6/19 17:33 Josep Llansana i Marcè Septifer eurydices vapincanus (Boussac, 1911) Vulsella linguiformis (Leymerie, 1831) Lentipecten corneus (Sowerby, 1818 ) Chlamys biarritzensis (D’Archiac, 1848) Spondylus buchi (Philippi, 1846) Dimya crearoi (Oppenheim, 1901) Hyotissa martinsi (D’Archiac, 1850 ) Cubitostrea plicata (Solander in Brander, 1766 ) Tots ells, excepte Spondilus buchi Philippi, 1846 i Dimya crearoi Op- penheim, 1901, presenten les valves soltes. Cap d’ells es troba en posició de vida i no ocupen en l’estrat una posició preferent. En les lutites grises immediates al contacte amb el banc anterior (mos- tra 3) es troben exemplars dispersos de: Dimya crearoi (Oppenheim, 1901) Els exemplars d’aquesta espècie presenten les dues valves juntes i re- colzades sobre la valva inferior. El tercer banc, situat a 11,7 m de la base, està separat de l’anterior banc calcari per 2,7 m de lutites grises. La fauna és rara i es restringeix a exem- plars aïllats de foraminífers (discociclines i operculines) i rares Dimya crea roi Oppenheim, 1901 (mostra 4). SISTEMÀTICA Classe ASTEROIDEA (de Blainville, 1830) Subclasse NEOASTEROIDEA (Gale, 1987) Superordre VALVATACEA (Perrier, 1884) Ordre VALVATIDA (Perrier, 1884) Família GONIASTERIDAE (Forbes, 1841) Gènere OPHRYASTER (Spencer, 1913) Calliderma atagensis (Valette, 1925) 1925 Calliderma atagensis (Valette: Notes sur p.76) 1941 Calliderma atagensis (Valette: Bataller Equinodermos fósiles, p. 60) 1997 Calliderma atagensis (Valette: Breton & Vizcaino Astérides l. fig. 5) 204 MISCELLANEA_18.indd 204 18/6/19 17:33 Calliderma atagensis, un estel·làrid de l’eocè de la Tossa de Montbui GENERALITATS SOBRE ELS ASTEROÏDEUS Els asteroïdeus o estel·làrids formen un grup entre els invertebrats equinoderms (caracteritzat per tenir una simetria anatòmica de cinc). Dins dels equinoderms hi ha altres grups com els equinoïdeus (eriçons de mar), els holoturoïdeus (cogombres de mar), les ofïures i els crinoïdeus, entre al- tres. Els equinoderms es caracteritzen per tenir un aparell especial anomenat sistema ambulacral, format per un complicat sistema de canals relacionats amb diferents parts modificades del seu esquelet i que formen els ambula- cres. Els ambulacres es prolonguen en uns tentacles especials erèctils ano- menats peus ambulacrals, els quals surten a l’exterior, amb funcions com ara la locomoció de l’animal, la de tentacles, la d’òrgans sensitius i, fins i tot, la respiració. L’aigua de mar penetra per l’anomenada placa madrepòrica. Tam- bé tenen un sistema digestiu amb boca i anus. El sistema nerviós és difús. L’esquelet dels equinoderms és d’origen dèrmic i està format per plaques o ossicles, formats per un sol cristall de calcita. Aquestes peces tendeixen a formar files a partir de la boca. Tots els equinoderms són marins. Els asteroïdeus es caracteritzen pels seus cinc braços entorn d’un disc central; com indica el seu nom tenen forma d’estrella. Cada braç està for- mat per dues files de plaques, a les quals se n’afegeixen altres de laterals i dorsals. A la cara ventral del seu cos s’obre la boca en posició inferior, amb cinc plaques radials i des d’ells surten cadascun dels cinc solcs ambula- crals, veritables solcs oberts. Entre cada una de les plaques bucals hi ha una placa interradial. La placa madrepòrica ocupa una posició interradial i en posició dorsal. L’anus hi pot arribar a faltar. El braç conté cecs intestinals, les gònades i els canals ambulacrals radials. Els asteroïdeus són sensibles a la llum mitjançant els receptors que tenen situats als peus ambulacrals. Els individus són mascles o femelles i la reproducció és sexual. També pot ser asexuada i a partir d’un braç formar la resta de l’organisme, com en cas d’accident que es trenqui un braç... L’esquelet és intern i està format per un entramat d’ossicles que s’es- tén per tot el cos. Els ossicles tenen formes molt variades i estan units per parts toves. Un cop morts, les parts toves es descomponen i els ossicles es disgreguen i dispersen. Els asteroïdeus actuals es mouen lliurement en el fons marí (en gene- ral dur i rocós) de tots els oceans, mitjançant els peus ambulacrals, des de la zona intermareal fins a 6.000 metres de profunditat. En el registre fòssil hi ha formes que vivien enterrades a la sorra o el fang, amb els braços aixecats cap amunt, modus de vida que van anar abandonant. S’alimenten d’altres organismes. Hi ha més de 1.800 espècies repartides en set ordres. 205 MISCELLANEA_18.indd 205 18/6/19 17:33 Josep Llansana i Marcè Els asteroïdeus, malgrat que hi ha jaciments on són molt abundants, rarament fossilitzen i, en general, solament s’hi troben els ossicles solts. La manca de sedimentació fina n’impedeix la fossilització. És molt difícil tro- bar alguna part de l’animal tal com estava en el moment de morir. Es conei- xen fòssils des de l’ordovicià (Paleozoic inferior). MATERIAL Es tracta de 580 peces (Fig. 3) que corresponen a 170 ossicles margi- nals (superior-marginals i inferior-marginals), 184 plaques dorsals (hexa- gonals), 200 plaques ambulacrals i adambulacrals, 25 peces bucals i una placa madrepòrica. És un esquelet complet d’estel·làrid. Figura 3. 206 MISCELLANEA_18.indd 206 18/6/19 17:33 Calliderma atagensis, un estel·làrid de l’eocè de la Tossa de Montbui DESCRIPCIÓ Disc central ample, braços curts que passen suaument sense cap brusquedat a amples arcs interradials. La boca està situada a la cara oral en posició central, cinc solcs d’ossicles ambulacrals i adambulacrals re- corren la línia mitjana de cada braç. Els solcs acullen els tubulars, que els serveixen per caminar. La placa madrepòrica està a la cara aboral. Les pla- ques aborals es disposen com a tessel·les d’un mosaic, essent-ne el con- torn hexagonal. Les plaques de la boca de contorn triangular es disposen de forma pentagonal. Els ossicles marginals tenen la forma d’un quadri- làter allargat, cara superior bombada, coberta d’impressions punctifor- mes, fines, espesses, d’igual mida i arriben fins al fons de l’artell.
Recommended publications
  • 9 Paleontological Conference Th
    Polish Academy of Sciences Institute of Paleobiology 9th Paleontological Conference Warszawa, 10–11 October 2008 Abstracts Warszawa Praha Bratislava Edited by Andrzej Pisera, Maria Aleksandra Bitner and Adam T. Halamski Honorary Committee Prof. Oldrich Fatka, Charles University of Prague, Prague Prof. Josef Michalík, Slovak Academy of Sciences, Bratislava Assoc. Prof. Jerzy Nawrocki, Polish Geological Institute, Warszawa Prof. Tadeusz Peryt, Polish Geological Institute, Warszawa Prof. Grzegorz Racki, Institute of Paleobiology, Warszawa Prof. Jerzy Trammer, University of Warsaw, Warszawa Prof. Alfred Uchman, Jagiellonian University, Kraków Martyna Wojciechowska, National Geographic Polska, Warszawa Organizing Committee Dr Maria Aleksandra Bitner (Secretary), Błażej Błażejewski, MSc, Prof. Andrzej Gaździcki, Dr Adam T. Halamski, Assoc. Prof. Anna Kozłowska, Assoc. Prof. Andrzej Pisera Sponsors Institute of Paleobiology, Warszawa Polish Geological Institute, Warszawa National Geographic Polska, Warszawa Precoptic Co., Warszawa Cover picture: Quenstedtoceras henrici Douvillé, 1912 Cover designed by Aleksandra Hołda−Michalska Copyright © Instytut Paleobiologii PAN Nakład 150 egz. Typesetting and Layout: Aleksandra Szmielew Warszawska Drukarnia Naukowa PAN ABSTRACTS Paleotemperature and paleodiet reconstruction on the base of oxygen and carbon isotopes from mammoth tusk dentine and horse teeth enamel during Late Paleolith and Mesolith MARTINA ÁBELOVÁ State Geological Institute of Dionýz Štúr, Mlynská dolina 1, SK−817 04 Bratislava 11, Slovak Republic; [email protected] The use of stable isotopes has proven to be one of the most effective methods in re− constructing paleoenvironments and paleodiet through the upper Pleistocene period (e.g. Fricke et al. 1998; Genoni et al. 1998; Bocherens 2003). This study demonstrates how isotopic data can be employed alongside other forms of evidence to inform on past at great time depths, making it especially relevant to the Palaeolithic where there is a wealth of material potentially available for study.
    [Show full text]
  • Paleogene Asteroids (Echinodermata) Palaeobiological
    bulletin de l'institut royal des sciences naturelles de belgique sciences de la terre, 75: 183-200, 2005 bulletin van het koninklijk belgisch instituut voor natuurwetenschappen aardwetenschappen. 75: 183-200, 2005 New latest Cretaceous and earliest Paleogene asteroids (Echinodermata) from The Netherlands and Denmark and their palaeobiological significance by Daniel B. BLAKE & John W.M. JAGT famille alors Blake, D.B & Jagt, 2005. — New latest Cretaceous and qu'aujourd'hui elle est limitée aux mers profondes. Elle earliest Paleogene asteroids (Echinodermata) from The Netherlands appartient aux Neobenthopectininae, ce qui démontre la présence au and Denmark and their palaeobiological significance. Bulletin de Mésozoïque de benthopectinidés dérivés. l'Institut royal des Sciences naturelles de Belgique, Sciences de la Mots-clefs: Terre 75: 183-200, 5 pis; Bruxelles-Brussel, March 31, 2005 - ISSN Asteroidea, Crétacé, Paléogène, Pays-Bas, Danemark, 0374-6291. taxionomie. Abstract Introduction Three new starfish (Skiaster vikingr n. gen., n. sp., Betelgeusia exposita Although the Asteroidea includes many heavily skeleto- n. sp., and Aldebarania taberna n. sp.), and the first fossil occurrence of nized species, specimens are rare among marine inverte- Cheirasterl sp., are recorded from Maastrichtian (Late Cretaceous) and brate fossils, and as a resuit Danian (Early Paleogene) rocks of The Netherlands and Denmark. overall history of the class Skiaster vikingr, a member of the goniasterid subfamily Pseudarchas- and its phylogeny are poorly understood. The Cretaceous terinae, adds to the known diversity and apparent significance of that and Paleogene chalks of northwest and central Europe subfamily. Betelgeusia exposita is the second Cretaceous species of the have one more Radiasteridae to be described; together, the two species suggest that provided of the extensive ancient asteroid this now infrequently encountered deep-water family was of greater faunas, and one that has been studied by générations of significance in the past.
    [Show full text]
  • Geological Survey of Austria ©Geol
    ©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at und www.zobodat.at Berichte der Geologischen Bundesanstalt, 120 Berichte der Geologischen Bundesanstalt, Benjamin Sames (Ed.) th 10 International Symposium on the Cretaceous: ABSTRACTS Berichte der Geologischen Bundesanstalt, 120 www.geologie.ac.at Geological Survey of Austria ©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at und www.zobodat.at Berichte der Geologischen Bundesanstalt (ISSN 1017-8880) Band 120 10th International Symposium on the Cretaceous Vienna, August 21–26, 2017 — ABSTRACTS BENJAMIN SAMES (Ed.) ©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at und www.zobodat.at Berichte der Geologischen Bundesanstalt, 120 ISSN 1017-8880 Wien, im Juli 2017 10th International Symposium on the Cretaceous Vienna, August 21–26, 2017 – ABSTRACTS Benjamin Sames, Editor Dr. Benjamin Sames, Universität Wien, Department for Geodynamics and Sedimentology, Center for Earth Sciences, Althanstraße 14, 1090 Vienna, Austria. Recommended citation / Zitiervorschlag Volume / Gesamtwerk Sames, B. (Ed.) (2017): 10th International Symposium on the Cretaceous – Abstracts, 21–26 August 2017, Vienna. – Berichte der Geologischen Bundesanstalt, 120, 351 pp., Vienna. Abstract (example / Beispiel) Granier, B., Gèze, R., Azar, D. & Maksoud, S. (2017): Regional stages: What is the use of them – A case study in Lebanon. – In: Sames, B. (Ed.): 10th International Symposium on the Cretaceous – Abstracts, 21–26 August 2017, Vienna. – Berichte der Geologischen Bundesanstalt, 120, 102, Vienna. Cover design: Monika Brüggemann-Ledolter (Geologische Bundesanstalt). Cover picture: Postalm section, upper Campanian red pelagic limestone-marl cycles (CORBs) of the Nierental Formation, Gosau Group, Northern Calcareous Alps (Photograph: M. Wagreich). 10th ISC Logo: Benjamin Sames The 10th ISC Logo is composed of selected elements of the Viennese skyline with, from left to right, the Stephansdom (St.
    [Show full text]
  • Notes, Outline and Divergence Times of Basidiomycota
    Fungal Diversity (2019) 99:105–367 https://doi.org/10.1007/s13225-019-00435-4 (0123456789().,-volV)(0123456789().,- volV) Notes, outline and divergence times of Basidiomycota 1,2,3 1,4 3 5 5 Mao-Qiang He • Rui-Lin Zhao • Kevin D. Hyde • Dominik Begerow • Martin Kemler • 6 7 8,9 10 11 Andrey Yurkov • Eric H. C. McKenzie • Olivier Raspe´ • Makoto Kakishima • Santiago Sa´nchez-Ramı´rez • 12 13 14 15 16 Else C. Vellinga • Roy Halling • Viktor Papp • Ivan V. Zmitrovich • Bart Buyck • 8,9 3 17 18 1 Damien Ertz • Nalin N. Wijayawardene • Bao-Kai Cui • Nathan Schoutteten • Xin-Zhan Liu • 19 1 1,3 1 1 1 Tai-Hui Li • Yi-Jian Yao • Xin-Yu Zhu • An-Qi Liu • Guo-Jie Li • Ming-Zhe Zhang • 1 1 20 21,22 23 Zhi-Lin Ling • Bin Cao • Vladimı´r Antonı´n • Teun Boekhout • Bianca Denise Barbosa da Silva • 18 24 25 26 27 Eske De Crop • Cony Decock • Ba´lint Dima • Arun Kumar Dutta • Jack W. Fell • 28 29 30 31 Jo´ zsef Geml • Masoomeh Ghobad-Nejhad • Admir J. Giachini • Tatiana B. Gibertoni • 32 33,34 17 35 Sergio P. Gorjo´ n • Danny Haelewaters • Shuang-Hui He • Brendan P. Hodkinson • 36 37 38 39 40,41 Egon Horak • Tamotsu Hoshino • Alfredo Justo • Young Woon Lim • Nelson Menolli Jr. • 42 43,44 45 46 47 Armin Mesˇic´ • Jean-Marc Moncalvo • Gregory M. Mueller • La´szlo´ G. Nagy • R. Henrik Nilsson • 48 48 49 2 Machiel Noordeloos • Jorinde Nuytinck • Takamichi Orihara • Cheewangkoon Ratchadawan • 50,51 52 53 Mario Rajchenberg • Alexandre G.
    [Show full text]
  • An Overview of Late Cretaceous and Early Palaeogene Echinoderm Faunas from Liege-Limburg (Belgium, the Netherlands)
    BULLETIN DE L'INSTITUT ROYAL DES SCIENCES NATURELLES DE BELGIQUE SCIENCES DE LA TERRE, 69-SUPP. A: 103-118, 1999 BULLETIN VAN HIT KONINKLIJK BELGISCH INSTITUUT VOOR NATUURWETENSCHAPPEN AARDWETENSCHAPPEN. 69-SUPP. A: 103-1 IX. 19» An overview of Late Cretaceous and Early Palaeogene echinoderm faunas from Liege-Limburg (Belgium, The Netherlands) by John W. M. JAGT Abstract My3eHHHM KOJUieKIJKHM, H B OC06eHHOCTH C034aHHbIM RO 1975 roaa, He XBaraeT, B nacTHOCTH, noapoôHoft HHthopMauHH o With the exception of echinoids, echinoderm faunas from the type area CTpaTHrpatnHHecKOM npoHcxo»c;reHHH. HoBaa KOJLieKima He of the Maastrichtian Stage still are more or less terra incognita. TOJibKO SHaHHTeiiBHO \TJiy6jiHeT Hanm 3H3HH5I O tbavHax Material collected recently in the area by a group of professional and HraoK05KHX LIo3ÄHero Mena (KaMnaHCKo-MacipHXTCKHH apycbi) amateur palaeontologists comprises numerous new records, which H Parmero riarteoreHa (TJaTCKMH apyc) B aaHHOH oônactn, HO H have the added advantaue of being well documented stratigraphically. Museum collections, and those pre-dating 1975 in particular, generally no3BOjmeT nojp3ecTH HTOTH no cTpyKTvpe pa3Hoo6pa3H« H suffer from a lack of detail where slratigraphic provenance is con• BbiMHpaHH», npejiiiiecTBOBaBuieH rpamme K/T H BKpecT rparame cerned. Not only do these new collections considerably increase our K/T. Kpancoe o6o3peiöie dpavH HTJIOKOJKHX npe^cTaBaeHO B knowledge of Late Cretaceous (Campanian-Maastrichtian) and Early aaHHOM OMepKe, ocoôoe BHHMaHHe yaeaeHO MopcKHM e*aM H Palaeogene (Danian) echinoderm faunas in the area, they also allow acTepoH/raM. conclusions on diversification and extinction patterns prior to and across the KT boundary to be drawn. In the present paper a brief overview is given of these echinoderm faunas, with emphasis on KjiioReBbie cioBa: rio3aHHH Mea, PaHrodi IlajieoreH, echinoids and asteroids.
    [Show full text]
  • New Latest Cretaceous and Earliest Paleogene Asteroids (Echinodermata) from the Netherlands and Denmark and Their Palaeobiological Significance
    BULLETIN DE L’INSTITUT ROYAL DES SCIENCES NATURELLES DE BELGIQUE SCIENCES DE LA TERRE, 75: 183-200, 2005 BULLETIN VAN HET KONINKLIJK BELGISCH INSTITUUT VOOR NATUURWETENSCHAPPEN AARDWETENSCHAPPEN, 75: 183-200, 2005 New latest Cretaceous and earliest Paleogene asteroids (Echinodermata) from The Netherlands and Denmark and their palaeobiological significance by Daniel B. BLAKE & John W.M. JAGT B l a k e , D.B & J a g t , 2005. — New latest Cretaceous and famille alors qu’aujourd'hui elle est limitée aux mers profondes. Elle earliest Paleogene asteroids (Echinodermata) from The Netherlands appartient aux Neobenthopectininae, ce qui démontre la présence au and Denmark and their palaeobiological significance.Bulletin de Mésozoïque de benthopectinidés dérivés. l ’Institut royal des Sciences naturelles de Belgique, Sciences de la Terre 75: 183-200, 5 pis; Bruxelles-Brussel, March 31, 2005 - ISSN Mots-clefs: Asteroidea, Crétacé, Paléogène, Pays-Bas, Danemark, 0374-6291. taxionomie. A bstract Introduction Three new starfish (Skiaster vikingr n. gen., n. sp., Betelgeusia exposita Although the Asteroidea includes many heavily skeleto­ n. sp., and Aldebarania taberna n. sp.), and the first fossil occurrence of nized species, specimens are rare among marine inverte­ Cheiraster? sp., are recorded from Maastrichtian (Late Cretaceous) and Danian (Early Paleogene) rocks of The Netherlands and Denmark. brate fossils, and as a result overall history of the class Skiaster vikingr, a member of the goniasterid subfamily Pseudarchas- and its phylogeny are poorly understood. The Cretaceous terinae, adds to the known diversity and apparent significance of that and Paleogene chalks of northwest and central Europe subfamily.Betelgeusia exposita is the second Cretaceous species of the Radiasteridae to be described; together, the two species suggest that have provided one of the more extensive ancient asteroid this now infrequently encountered deep-water family was of greater faunas, and one that has been studied by generations of significance in the past.
    [Show full text]
  • Starfishes from the Caribbean F and the Gulf of Mexico
    MAUREEN E. DOWN Starfishes from the Caribbean f and the Gulf of Mexico SMITHSONIAN CONTRIBUTIONS TO ZOOLOGY NUMBER 126 SERIAL PUBLICATIONS OF THE SMITHSONIAN INSTITUTION The emphasis upon publications as a means of diffusing knowledge was expressed by the first Secretary of the Smithsonian Institution. In his formal plan for the Insti- tution, Joseph Henry articulated a program that included the following statement: "It is proposed to publish a series of reports, giving an account of the new discoveries in science, and of the changes made from year to year in all branches of knowledge." This keynote of basic research has been adhered to over the years in the issuance of thousands of titles in serial publications under the Smithsonian imprint, com- mencing with Smithsonian Contributions to Knowledge in 1848 and continuing with the following active series: Smithsonian Annals of Flight Smithsonian Contributions to Anthropology Smithsonian Contributions to Astrophysics Smithsonian Contributions to Botany Smithsonian Contributions to the Earth Sciences Smithsonian Contributions to Paleobiology Smithsonian Contributions to Zoology Smithsonian Studies in History and Technology In these series, the Institution publishes original articles and monographs dealing with the research and collections of its several museums and offices and of professional colleagues at other institutions of learning. These papers report newly acquired facts, synoptic interpretations of data, or original theory in specialized fields. These pub- lications are distributed by mailing lists to libraries, laboratories, and other interested institutions and specialists throughout the world. Individual copies may be obtained from the Smithsonian Institution Press as long as stocks are available. S. DILLON RIPLEY Secretary Smithsonian Institution SMITHSONIAN CONTRIBUTIONS TO ZOOLOGY NUMBER 126 Maureen E.
    [Show full text]
  • Mitteilungen Aus Dem Mineralogisch-Geologischen Institut in Hamburg 1911(1912)
    Mitteilungen aus dem Mineralogisch-Geologischen Institut in Hamburg 1911(1912) - 1918(1920) 1912 (1) Auch erschienen im Jahrbuch der Hamburgischen Wissenschaftlichen Anstalten / Wissenschaftliche Anstalten des Staates Hamburg von 29.1911, Beih. 4 Digital: http://www.biodiversitylibrary.org/item/94918#page/11/mode/1up Gürich, G. (1912). Gryposuchus Jessei, ein neues schmalschnauziges Krokodil aus den jüngeren Ablagerungen des oberen Amazonas-Gebietes. 1, S. 59-71 Horn, E. (1912). Die geologischen Verhältnisse des Elbtunnels nebst einem Beitrag zur Geschichte des unteren Elbtales. 1, S. 35-58 Koch, E., Gripp, K. & Franke, A. (1912). Die staatlichen Tiefbohrungen XIV, XV, XVI, XVII in den Vierlanden bei Hamburg. 1, S. 1-33 1913 (2) Auch erschienen im Jahrbuch der Hamburgischen Wissenschaftlichen Anstalten / Wissenschaftliche Anstalten des Staates Hamburg von 30.1912, Beih. 6 Digital: http://www.biodiversitylibrary.org/item/92000#page/153/mode/1up Beyle, M. (1913). Über einige Ablagerungen fossiler Pflanzen der Hamburger Gegend: erster Teil. 2, S. 83-99 Gripp, K. (1913). Über den Gipsberg in Segeberg und die in ihm vorhandene Höhle. 2, S. 35-51 Gürich, G. (1913). Zur Altersbestimmung des Otawi-Kalkes. 2, S. 19-33 Horn, E. (1913). Die Meteoritensammlung des Mineralogisch-Geologischen Instituts zu Hamburg. 2, S. 1-18 Koch, E. (1913). Der Untergrund der rechtselbischen Marsch oberhalb Hamburgs. 2, S. 53-81 1914 (3) Auch erschienen im Jahrbuch der Hamburgischen Wissenschaftlichen Anstalten / Wissenschaftliche Anstalten des Staates Hamburg von 31.1913, Beih. 5 Digital: http://www.biodiversitylibrary.org/item/92005#page/9/mode/1up Gripp, K. (1914). Über eine untermiozäne Molluskenfauna von Itzehoe. 3, S. 1-40 1918 (4) Auch erschienen im Jahrbuch der Hamburgischen Wissenschaftlichen Anstalten / Wissenschaftliche Anstalten des Staates Hamburg von 35.1917, Beih.
    [Show full text]
  • Late Cretaceous-Early Palaeogene Echinoderms and the K/T Boundary in the Southeast Netherlands and Northeast Belgium — Part 1: Introduction and Stratigraphy
    pp 03-60 (Jagt-1) 15-01-2007 10:19 Pagina 1 Late Cretaceous-Early Palaeogene echinoderms and the K/T boundary in the southeast Netherlands and northeast Belgium — Part 1: Introduction and stratigraphy John W.M. Jagt Jagt, J.W.M. Late Cretaceous-Early Palaeogene echinoderms and the K/T boundary in the southeast Netherlands and northeast Belgium — Part 1: Introduction and stratigraphy. — Scripta Geol., 116: 1- 57, 3 figs., Leiden, May 1999. John W.M. Jagt, Natuurhistorisch Museum Maastricht, Postbus 882, NL-6200 AW Maastricht, The Netherlands; E-mail: [email protected] Key words: Echinodermata, Late Cretaceous, Early Palaeogene, localities, stratigraphy. In a series of papers describing Late Cretaceous and Early Palaeogene echinoderm faunas (exclusive of holothurians) of the Maastrichtian type area, the present contribution comprises a detailed account of the litho- and chronostratigraphy and biozonations of these deposits, and of localities from which the echinoderm material to be described stems. In subsequent papers reference will be made to this introductory part. Contents Introduction ............................................................................................................................. 1 Geographic and stratigraphic setting .................................................................................. 1 Acknowledgements .............................................................................................................. 40 References .............................................................................................................................
    [Show full text]
  • The Geology of Norfolk
    THE GEOLOGY OF NORFOLK A collection of papers assembled by the PARAMOUDRA CLUB to mark its tenth anniversary. Edited by G. P. LARWOOD and B. M. FUNNELL CONTENTS Introduction -------- Page 269 Strata of Norfolk .. 270 The Sub-Cretaceous Rocks of Norfolk, by R. G. Thurrell -------- 271 The Lower Cretaceous Deposits of Norfolk, by G. P. Larwuod .. 280 The Upper Cretaceous of Norfolk, by N. B. Peake and J. M. Hancock .. 293 The Palaeogene and Early Pleistocene of Norfolk, by B. M. Funnell 340 The Glacial and Interglacial Deposits of Norfolk, by R. G. West ------- ,, 365 TRANSACTIONS OF THE NORFOLK AND NORWICH NATURALISTS’ SOCIETY, VOLUME 19 PART 6 Edited by E. A . ELLIS Grateful acknowledgment is made to the Royal Society for a generous grant towards the cost of this publication. Norwich Printed by the Soman-Wherry Press Ltd., Norwich Published September, 1961 THE GEOLOGY OF NORFOLK INTRODUCTION The present collection of papers incorporates the results of import- ant recent investigations, and provides a comprehensive, up-to-date account of the pre-Holocene geology of Norfolk. It has been assembled by the Paramoudra Club to mark its tenth anniversary, and is published in co-operation with the Norfolk and Norwich Naturalists’ Society. The Paramoudra Club was founded in 1950, as an association of student geologists, to promote interest in the geology of the county of Norfolk, and now includes in its membership many professional and amateur geologists from Norfolk and elsewhere. The members of the Paramoudra Club take this opportunity to thank those authors whose contributions have made this publication possible.
    [Show full text]
  • Seesterne) 113-141 62: 113 – 141 29 Dec 2016
    ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Geologica Saxonica - Journal of Central European Geology Jahr/Year: 2016 Band/Volume: 62 Autor(en)/Author(s): Niebuhr Birgit, Seibertz Ekbert Artikel/Article: Asteroiden (Seesterne) 113-141 62: 113 – 141 29 Dec 2016 © Senckenberg Gesellschaft für Naturforschung, 2016. 13. Asteroiden (Seesterne) 13. Asteroids (starfishes) Birgit Niebuhr 1 und Ekbert Seibertz 2 1 Senckenberg Naturhistorische Sammlungen Dresden, Museum für Mineralogie und Geologie, Sektion Paläozoologie, Königsbrücker Landstraße 159, 01109 Dresden, Deutschland; [email protected] — 2 Institut für Geoökologie der TU Braunschweig, Abt. Geochemie, Arb.-Ber. Sedimentgeologie und Stratigraphie, Langer Kamp 19c, 38106 Braunschweig, Deutschland; [email protected] Revision accepted 18 July 2016. Published online at www.senckenberg.de/geologica-saxonica on 29 December 2016. Kurzfassung In der Oberkreide der Elbtal-Gruppe in Sachsen treten zwölf Seestern-Arten aus den folgenden zehn Gattungen auf: Lophidiaster, Hadranderaster, Manfredaster, Geinitzaster, Metopaster, Chomataster, Crateraster, Comptoniaster, Calliderma und Nymphaster. Sie repräsentieren die Familien Astropectinidae, Stauranderasteridae, Goniasteridae und eine möglicherweise neue Familie. Manfredaster praebulbiferus aus dem Obercenomani- um von Dresden-Plauen und Calliderma lindneri aus dem basalen Mittelturonium von Schmilka werden als neue Arten beschrieben. Comptoniaster
    [Show full text]
  • Systematics and Palaeoecology of Middle Toarcian Asteroidea (Echinodermata) from the “Seuil Du Poitou”, Western France Syst
    Geobios 37 (2004) 807–825 www.elsevier.com/locate/geobio Original article Systematics and palaeoecology of middle Toarcian Asteroidea (Echinodermata) from the “Seuil du Poitou”, Western France Systématique et paléoécologie des Asteroidea (Echinodermata) du Seuil du Poitou (ouest de la France) Loïc Villier a,d,*, Manfred Kutscher b, Christopher L. Mah c a Institute für Paläontologie, Museum für Naturkunde, Humboldt-Universität zu Berlin, Invalidenstrasse 43, 10115 Berlin, Germany b Dorfstrasse 10, 18546 Sassnitz, Germany c Department of Geology, University of Illinois, 245 NHB, 1301 W. Green Street, Urbana, IL 61801, USA d Centre de Sédimentologie-Paléontologie, Université de Provence, place Victor Hugo, 13331 Marseille cedex 3, France Received 13 December 2002; accepted 26 May 2003 Available online 30 September 2004 Abstract Complete, articulated starfish fossils are rare. However, more frequently encountered dissociated skeletal elements (ossicles) permit reli- able taxonomic identification, making them a valuable data source for diversity estimates. Nearly 300 asteroid ossicles, collected from the middle Toarcian marls in western France can be assigned to five species. Four species and two genera are described: Comptoniaster vrinensis nov. sp. (Goniasteridae), Poncetaster crateri nov. gen. nov. sp. (Stauranderasteridae), Galbaster recurrans nov. gen. nov. sp. (Goniasteridae) and Pentasteria? liasica nov. sp. (Astropectinidae). The known diversity of Early Jurassic asteroids is increased from 12 to 16 species. These taxa illustrate the diversification of crown-group asteroids early in the Jurassic, following the Permo-Triassic crisis. They also reflect bias of the fossil record, and imply the existence of numerous ghost lineages in the evolutionary trees of extant groups. Variation in asteroid diversity across the “Seuil du Poitou” was driven by ecological constraints.
    [Show full text]