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Report on the 4th International Meeting of the IUGS Lower Creatceous Ammonite Working Group, the "Kilian Group" (Dijon, France, 30th August 2010)

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    SYSNO ASEP0360114
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleReport on the 4th International Meeting of the IUGS Lower Creatceous Ammonite Working Group, the "Kilian Group" (Dijon, France, 30th August 2010)
    Author(s) Reboulet, S. (FR)
    Rawson, P. F. (GB)
    Moreno-Bedmar, J. A. (MX)
    Aquirre-Urreta, M. B. (AR)
    Barragán, R. (MX)
    Bogomolov, Y. (RU)
    Company, M. (ES)
    Gonzáles-Arreola, C. (MX)
    Stoyanova, V. (BG)
    Lukeneder, A. (AT)
    Matrion, B. (FR)
    Mitta, V. (RU)
    Randrianaly, H. (MG)
    Vašíček, Zdeněk (UGN-S) RID
    Baraboshkin, E. J. (RU)
    Bert, D. (FR)
    Bersac, S. (FR)
    Bogdanova, T. M. (RU)
    Bulot, L. G. (FR)
    Latil, J. L. (FR)
    Mikhailova, I. A. (RU)
    Ropolo, P. (FR)
    Szives, O. (HU)
    Number of authors23
    Source TitleCretaceous Research. - : Elsevier - ISSN 0195-6671
    Roč. 6, č. 32 (2011), s. 786-793
    Number of pages33 s.
    Publication formwww - www
    Languageeng - English
    CountryGB - United Kingdom
    KeywordsKilian Group ; ammonites ; Lower Cretaceous ; standard zonation ; Aptian ; Albian
    Subject RIVDB - Geology ; Mineralogy
    CEZAV0Z30860518 - UGN-S (2005-2011)
    UT WOS000295114600012
    DOI10.1016/j.cretres.2011.05.007
    AnnotationThe 4th Kilian Group meeting (Dijon, France, 30th August 2010) focused on the Aptian and Albian Stages. For the Aptian, a two-fold division of the stage was adopted for the Mediterranean area with a boundary between the Dufrenoyia furcata and Epicheloniceras martini Zones. The main changes to the zonal scheme concern the Lower Aptian with: the introduction of a Deshayesites luppovi Subzone in the upper part of the Deshayesites oglanlensis Zone; the replacement of Deshayesites weissi by Deshayesites forbesi as new index-species of the second interval zone; the introduction of a Roloboceras hambrovi Subzone in the upper part of the D. forbesi Zone; and the subdivision of the Dufrenoyia furcata Zone into the D. furcata and Dufrenoyia dufrenoyi Subzones. For the Albian, the upper part of the Douvilleiceras mammillatum Zone (Lower Albian) is now characterized by a Lyelliceras pseudolyelli Subzone. The main amendments concern the Upper Albian. The base of this substage is defined by the base of the Dipoloceras cristatum Zone.
    WorkplaceInstitute of Geonics
    ContactLucie Gurková, lucie.gurkova@ugn.cas.cz, Tel.: 596 979 354
    Year of Publishing2012
    Electronic addresshttp://www.sciencedirect.com/science/article/pii/S0195667111000553
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