TJ163, Charymdara-Zydadara-Gundara watersheds: Kungurian, Tajikistan

List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Rhodophyceae - Gymnocodiaceae
Permocalculus sp. Elliott 1955
Chlorophyceae - Dasycladales - Dasycladaceae
Pseudovermiporella sp. Elliot 1958
Atractyliopsis tezakensis
Mizzia cornuta
Gyroporella sp. Gümbel 1872
Gyroporella microporosa
ssp. afghanica
Mizzia yabei (Karpinsky 1908)
original and current combination Stolleyella yabei
Clavaporella sp. Kochansky and Herak 1960
Chlorophyceae - Dasycladales
Connexia sp. Kochansky Devide 1970
Chlorophyceae - Dasycladales - Seletonellaceae
Epimastopora japonica
unclassified
Polytaxis sp.
Pachyphloiidae
Pachyphloia sp. Lange 1925
Verbeekinidae
Brevaxina dyhrenfurthi (Dutkevich 1939)
ssp. otai
Staffellidae
Nankinella sp. Lee 1933
Schwagerinidae
? Leeina sp. Galloway 1933
Darvasites sp.
Boultoniidae
? Boultonia sp. Lee 1927
Schubertellidae
Neofusulinella sp. Deprat 1912
Neofusulinella cf. pseudogiraudi (Sheng 1963)
Endothyridae
Endothyra sp.
Biseriamminidae
Globivalvulina sp. Schubert 1921
Palaeotextulariidae
Climacammina sp. Brady 1873
Deckerella sp.
Tubothalamea - Miliolida - Hemigordiopsidae
? Agathammina sp. Neumayr 1887
unclassified
Palaeonubecularia sp. Reitlinger 1950
Conodonta - Ozarkodinida - Sweetognathidae
Sweetognathus modulatus
Sweetognathus sp.
unclassified
Tubiphytes obscurus Maslov 1956
recombined as Shamovella obscura
see common names

Geography
Country:Tajikistan
Coordinates: 38.8° North, 70.9° East (view map)
Paleocoordinates:28.0° North, 67.6° East
Basis of coordinate:stated in text
Geographic resolution:outcrop
Time
Period:Permian Epoch:Cisuralian
Stage:Kungurian 10 m.y. bin:Permian 2
Key time interval:Kungurian
Age range of interval:283.50000 - 273.01000 m.y. ago
Stratigraphy
Formation:Safetdara
Stratigraphic resolution:bed
Lithology and environment
Primary lithology:shelly/skeletal lithified "limestone"
Environment:open shallow subtidal
Geology comments: Our microfacies analysis of samples from the Safetdara Formation reveals that they contain mainly photozoan assemblages. Therefore, they are typical shoal deposits of warm, shallow (5–10 m deep) and agitated but clear marine waters.
Taphonomy
Modes of preservation:body
Size of fossils:macrofossils
Collection methods and comments
Reason for describing collection:taxonomic analysis
Collection method comments: Repository: Palaeontological Museum of the Department of Earth Sciences "A. Desio", University of Milan, Italy
Metadata
Database number:182688
Authorizer:M. Clapham Enterer:M. Clapham
Modifier:M. Clapham Research group:micropaleontology
Created:2016-11-22 13:34:18 Last modified:2016-11-22 13:38:12
Access level:the public Released:2016-11-22 13:34:18
Creative Commons license:CC BY
Reference information

Primary reference:

60899. L. Angiolini, M. Campagna, L. Borlenghi, T. Grunt, D. Vachard, G. Vezzoli, I. Vuolo, J. Worthington, A. Nicora and A. Zanchi. 2016. Brachiopods from the Cisuralian–Guadalupian of Darvaz, Tajikistan and implications for Permian stratigraphic correlations. Palaeoworld 25:539-568 [M. Clapham/M. Clapham]