Also known as Locality 5 of Webster et al. 2003.

Where: Kerman, Iran (30.6° N, 57.0° E: paleocoordinates 40.4° S, 68.7° E)

• coordinate stated in text

• local area-level geographic resolution

When: Siphonodella crenulata - Gnathodus typicus conodont zone, Hutk Formation, Hastarian to Hastarian (358.9 - 346.7 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." This is now Hutk formation, not Bahram.

• 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)