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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 ASEP 0360114 Druh ASEP J - Článek v odborném periodiku Zařazení RIV J - Článek v odborném periodiku Poddruh J Článek ve WOS Název Report on the 4th International Meeting of the IUGS Lower Creatceous Ammonite Working Group, the "Kilian Group" (Dijon, France, 30th August 2010) Tvůrce(i) 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)Celkový počet autorů 23 Zdroj.dok. Cretaceous Research. - : Elsevier - ISSN 0195-6671
Roč. 6, č. 32 (2011), s. 786-793Poč.str. 33 s. Forma vydání www - www Jazyk dok. eng - angličtina Země vyd. GB - Velká Británie Klíč. slova Kilian Group ; ammonites ; Lower Cretaceous ; standard zonation ; Aptian ; Albian Vědní obor RIV DB - Geologie a mineralogie CEZ AV0Z30860518 - UGN-S (2005-2011) UT WOS 000295114600012 DOI 10.1016/j.cretres.2011.05.007 Anotace The 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. Pracoviště Ústav geoniky Kontakt Lucie Gurková, lucie.gurkova@ugn.cas.cz, Tel.: 596 979 354 Rok sběru 2012 Elektronická adresa http://www.sciencedirect.com/science/article/pii/S0195667111000553
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