Detailed Information on Publication Record
2017
New unornamented siphonodellids (Conodonta) of the lower Tournaisian from the Rhenish Massif and Moravian Karst (Germany and Czech Republic)
KAISER, Sandra, Tomáš KUMPAN and Vojtěch CÍGLERBasic information
Original name
New unornamented siphonodellids (Conodonta) of the lower Tournaisian from the Rhenish Massif and Moravian Karst (Germany and Czech Republic)
Authors
KAISER, Sandra (276 Germany), Tomáš KUMPAN (203 Czech Republic, guarantor, belonging to the institution) and Vojtěch CÍGLER (203 Czech Republic, belonging to the institution)
Edition
Neues Jahrbuch für Geologie und Paläontologie, Abhandlungen, STUTTGART, 2017, 0077-7749
Other information
Language
English
Type of outcome
Článek v odborném periodiku
Field of Study
10500 1.5. Earth and related environmental sciences
Country of publisher
Germany
Confidentiality degree
není předmětem státního či obchodního tajemství
References:
Impact factor
Impact factor: 0.760
RIV identification code
RIV/00216224:14310/17:00095012
Organization unit
Faculty of Science
UT WoS
000423279000001
Keywords in English
biostratigraphy;carboniferous;conodont biofacies;siphonodella belkai;mississippian
Tags
International impact, Reviewed
Změněno: 9/4/2018 16:33, Ing. Nicole Zrilić
Abstract
V originále
Conodonts of lower Tournaisian successions in the Remscheid-Altena Anticline of the Rhenish Massif (Germany) and from the Moravian Karst of the Bohemian Massif (Czech Republic) have been re-studied based on previous high-resolution conodont stratigraphy. New lower Tournaisian siphonodellids without ornamentation on the oral platform side were recorded here in carbonate pe- lagic and turbiditic settings. Siphonodella belkai, which was previously unknown in western Europe, is the most abundant species among the unornamented siphonodellids. Two morphotypes of Si. belkaias well asSi. kalvodai sp. nov. are defined herein. The new faunas occur in the jii, sandbergi, andquadruplicata conodont zones. Siphonodella kalvodai sp. nov. has its FAD in the jii Zone, and Si. belkai first occurs in the basal jii Zone in both regions. The basal jii Zone can therefore be correlated with the basal belkai Zone established in neritic and pelagic settings of the East European Platform and Uralian Mountains. The new faunas enable a more precise correlation between lower Tournaisian biozones established previously in Central, South and Western Europe, North America, China, and East European and Uralian regions. Distributional restrictions of unornamented siphonodellids indicate a subordinate ecological significance but points out their palaeogeographic provincialism, tied to the northern Palaeotethys or palaeoequatorial realm.
Links
| GA16-11563S, research and development project |
|