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Invertebrate fauna of the Albian-Lower Cenomanian deposits in the Fars and Isfahan provinces (Firuzabad and Fasakhod sections), Zagros Basin, Central Iran
被引:0
|作者:
Sedghi, Babak
[1
]
Bahrami, Ali
[1
]
Yazdi, Mehdi
[1
]
Vega, Francisco J.
[2
]
机构:
[1] Univ Isfahan, Fac Sci, Dept Geol, Esfahan 81746-73441, Iran
[2] Univ Nacl Autonoma Mexico, Inst Geol, Ciudad Univ, Coyoacan 04510, Mexico
来源:
关键词:
Cretaceous;
Albian-Cenomanian;
Kazhdumi Formation;
fossil content;
Iran;
SANANDAJ-SIRJAN ZONE;
KAZHDUMI FORMATION;
BELT;
BIOSTRATIGRAPHY;
GEOCHEMISTRY;
STRATIGRAPHY;
TECTONICS;
EVOLUTION;
GEOLOGY;
MAKRAN;
D O I:
10.18268/BSGM2023v75n3a220623
中图分类号:
P5 [地质学];
学科分类号:
0709 ;
081803 ;
摘要:
The Albian-Cenomanian deposits of the Kazhdumi Formation at Zagros Basin (Firuzabad section and Central Iran (Fasakhod section), represents a carbonate sedimentary succession and contain rich and diverse invertebrate macro fauna. Detailed studies on about 200 specimens of invertebrate macro fauna revealed from two strati-graphic intervals led to recognition of 5 species of gastropods; (Liopeplum? sp., Columbellina sp., Cryptaulax? sp., Turritella? sp., Pleurotomaria sp.), 3 species of ammonites; (Knemiceras duberter-ti, Sphenodiscus sp., Knemiceras persicum), 10 species of bivalves assemblages; (Ceratostreon flabellatum, Cardium? sp., Exogyra (Costagyra) olisiponensis, Neithea (Neithea) quinquecostata, Trigonia sp., Bu-chia? sp., Cardium? sp., Pseudogyra sp., Ontaria? sp., Nucula? sp., Pleuromia? sp., 1 species of echinoids; Dorocidaris taou-zensis with a prolific horizon of Notopocorystes xizangensis of raninoid crabs. The absence of large gastropods and bivalves fauna and abundance of suspension-feeders indicated instability of the substrate, shallow marine paleoenvironment.and a medium energy condition.
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