Also known as Coral interval B
Where: Iran (32.1° N, 50.8° E: paleocoordinates 29.5° N, 49.1° E)
• coordinate stated in text
• outcrop-level geographic resolution
When: Bakhtiari Formation, Miocene (23.0 - 5.3 Ma)
• The precise dating of the Bakhtiari succession (within the Miocene) requires further highresolution taxonomic and biostratigraphic studies of the foraminifera and nannofossil species.
Environment/lithology: shallow subtidal; wackestone and packstone
Size classes: macrofossils, mesofossils
Primary reference: A. H. Rahiminejad, M. Yazdi, and A. R. Ashouri. 2010. Miocene scleractinian corals from a mixed siliciclastic–carbonate system: Bakhtiari succession, Zagros Basin (central-western Iran). Alcheringa: An Australasian Journal of Palaeontology 35(4):571-592 [W. Kiessling/M. Krause/M. Krause]more details
Purpose of describing collection: paleoecologic analysis
PaleoDB collection 151424: authorized by Wolfgang Kiessling, entered by Mihaela Krause on 01.10.2013
Creative Commons license: CC BY (attribution)
Taxonomic list
unclassified | |
Mollusca indet. Linnaeus 1758 | |
Echinoidea | |
Echinoidea indet. Leske 1778 sea urchin | |
Anthozoa | |
Porites cf. maigensis Kühn 1925 stony coral
Porites cf. mancietensis Chevalier 1961 stony coral | |
Foraminifera | |
Amphistegina sp. d'Orbigny 1826 | |
Globothalamea | |
Miogypsina sp. Sacco 1893 | |
Tubothalamea | |