Report on the 5th International Meeting of the IUGS Lower Cretaceous Ammonite Working Group, the Kilian Group (Ankara, Turkey, 31st August 2013) - Archive ouverte HAL Accéder directement au contenu
Article Dans Une Revue Cretaceous Research Année : 2014

Report on the 5th International Meeting of the IUGS Lower Cretaceous Ammonite Working Group, the Kilian Group (Ankara, Turkey, 31st August 2013)

Ottilia Szives
  • Fonction : Auteur
Beatriz Aguirre-Urreta
  • Fonction : Auteur
Ricardo Barragan
  • Fonction : Auteur
Miguel Company
  • Fonction : Auteur
Vyara Idakieva
  • Fonction : Auteur
Mann Ivanov
  • Fonction : Auteur
Mikheil V. Kakabadze
  • Fonction : Auteur
Josep A. Moreno-Bedmar
  • Fonction : Auteur
Jose Sandoval
  • Fonction : Auteur
Evgenij J. Baraboshkin
  • Fonction : Auteur
Meral K. Caglar
  • Fonction : Auteur
Istvan Fozy
  • Fonction : Auteur
Celestina Gonzalez-Arreola
  • Fonction : Auteur
Samer Kenjo
  • Fonction : Auteur
Alexander Lukeneder
  • Fonction : Auteur
Seyed N. Raisossadat
  • Fonction : Auteur
Peter F. Rawson
  • Fonction : Auteur
Jose M. Tavera
  • Fonction : Auteur

Résumé

The 5th meeting of the IUGS Lower Cretaceous Ammonite Working Group (the Kilian Group) held in Ankara, Turkey, 31st August 2013, discussed the Mediterranean ammonite zonation, and its calibration with different ammonite zonal schemes of the Boreal, Austral and Central Atlantic realms. Concerning the standard zonation, that corresponds to the zonal scheme of the West Mediterranean province, some changes have been made on two stages. For the Valanginian, the Busnardoites campylotoxus Zone was abandoned; the upper part of the lower Valanginian is now characterised by the Neocomites neocomiensiformis and Karakaschiceras inostranzewi zones. For the upper Barremian, the former Imerites giraudi Zone is here subdivided into two zones, a lower I. giraudi Zone and an upper Martellites sarasini Zone. The I. giraudi Zone is now subdivided into the I. giraudi and Heteroceras emerici subzones, previously considered as horizons. The current M. sarasini and Pseudocrioceras waagenoides subzones correspond to the lower and upper parts of the M. sarasini Zone, respectively. The Anglesites puzosianum Horizon is kept. The Berriasian, Hauterivian, Aptian and Albian zonal schemes have been discussed but no change was made. The upper Hauterivian zonal scheme of the Georgian (Caucasus) region (East Mediterranean province) has been compared with the standard zonation. Discussions and some attempts at correlations are presented here between the standard zonation and the zonal schemes of different
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Dates et versions

hal-02351049 , version 1 (06-11-2019)

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Stephane Reboulet, Ottilia Szives, Beatriz Aguirre-Urreta, Ricardo Barragan, Miguel Company, et al.. Report on the 5th International Meeting of the IUGS Lower Cretaceous Ammonite Working Group, the Kilian Group (Ankara, Turkey, 31st August 2013). Cretaceous Research, 2014, 50, pp.126--137. ⟨10.1016/j.cretres.2014.04.001⟩. ⟨hal-02351049⟩
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