Also known as Locality 5 of Webster et al. 2003.
Where: Kerman, Iran (30.6° N, 57.0° E: paleocoordinates 40.9° S, 68.3° E)
• coordinate stated in text
• local area-level geographic resolution
When: Siphonodella crenulata - Gnathodus typicus conodont zone, Bahram Formation, Hastarian to Hastarian (360.7 - 345.3 Ma)
• Fig. 2. Originally dated as Fammenian; Webster et al. (2003) note that this is actually Mississippian: "Conodonts from Locality 5, southeast of Hutk (upper horizon), yielded Protognathus praedelicatus Lane, Sandberg, and Ziegler 1980; Gnathodus typicus Cooper, 1939; Polygnathus communis communis (Branson and Mehl, 1934); and Clydagnathus cavusformis Rhodes, Austin, and Druce, 1969. This fauna suggests the horizon can be no older than S. isosticha-Upper crenulata Biozone because G. typicus first occurs within this biozone (Lane et al., 1980) and no younger than Scaliognathus anchoralis-latus Biozone. All three taxa are known to occur in this latter biozone." and "Conodonts from the crinoid-bearing beds represent two faunas and indicate an age of Upper Siphonodella crenulata Biozone to Gnathodus typicus Biozone."
• bed-level stratigraphic resolution
Environment/lithology: lithified, argillaceous limestone
Size class: macrofossils
Primary reference: R. D. Hoare and B. Aghababula. 2001. Large Devonian and Mississippian rostroconchs (Mollusca) from Iran. Journal of Paleontology 75(5):1047-1051 [P. Wagner/P. Wagner]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 57115: authorized by Pete Wagner, entered by Pete Wagner on 02.12.2005
Creative Commons license: CC BY (attribution)