Late Devonian (Famennian) to Carboniferous (Mississippian-Pennsylvanian) conodonts from the Anarak section, Central Iran

Abstract

A relatively complete conodont record from Famennian to the Mississippian/Pennsylvanian boundary was investigated in the Anarak section, Central Iran. The studied interval belongs to the Bahram, Shishtu, Ghaleh and Absheni formations. The Famennian part of the section (Bahram Formation) ranges from the Palmatolepis triangularis Zone into the Bispathodus ultimus Zone. Not all conodont zones could be defined due to the lack of indicative species. Furthermore, it seems likely that a hiatus occurs around the Devonian/Carboniferous (D/C) boundary (most probably from the Siphonodella praesulcata to the ?Siphonodella sulcata–early Siphonodella crenulata conodont zones) based on the lack of stratigraphically important conodonts as well as on sedimentological criteria. The lack of representative siphonodellids and protognathodids at the base of the Mississippian prevents detailed stratigraphic position of the D/C boundary. Lower Carboniferous (Mississippian) rocks are characterized by red nodular limestone which is unique in comparison with other studied sections of the same age in Central Iran. Within the studied section, we could define the Mississippian/Pennsylvanian boundary. The mid-Carboniferous boundary was defined by the occurrence of Declinognathus noduliferus s.l. Conodont biofacies changes (Mississippian genera Gnathodus and Lochriea have been replaced by Pennsylvanian genera Declinognathus and Idiognathodus) are recognized in this section as well.

Famennian conodont assemblage in the Compte section (Upper Devonian, Central Pyrenees) and its comparison with Eurasian sequences

“…inclinatus. Slightly similar to the Compte record are the conodont faunas from Anarak section (Sattari et al, 2021), which are composed of: Ic. alt.…”

Extreme lower jaw elongation in a placoderm reflects high disparity and modularity in early vertebrate evolution

“…cf. strigosa , dating the fossils to the middle to late Famennian ( trachytera conodont zone) [ 19 , 20 ]. The other Moroccan materials come from the localities of Rich bel Ras and Madene El Mrakib in the Maider basin, in ( figure 1 b ) and date back to the middle to late Famennian Platyclymenia annulata ammonoid zone [ 21 ].…”

Middle - Late Devonian boundary conodonts from Anarak and Sar-Ashk sections, Central Iran

“…Bahrami et al (2019) examined the Anarak section and attributed it to the Late Givetian to Early Famennian Sattari et al (2021). investigated the upper part of the section and attributed it to the Famennian -Bashkirian time interval.…”