Extending the stratigraphic range of Nummulites bormidiensis Tellini in the Neo-Tethys (Zagros basin, SE Iran) through biometry and calcareous nannofossil biostratigraphy

被引:2
|
作者
Hadi, Mehdi [1 ]
Forouzande, Seyyed Khalil [1 ]
Consorti, Lorenzo [2 ]
Parandavar, Mohammad [3 ]
Vahidinia, Mohammad [1 ]
机构
[1] Ferdowsi Univ Mashhad, Fac Sci, Dept Geol, Mashhad, Iran
[2] Inst Marine Sci ISMAR, CNR, Area Sci Pk Basovizza, Trieste, Italy
[3] NIOC, Paleontol & Geochem Res Off, Explorat Directorate Oil, Tehran, Iran
关键词
Asmari Formation; nannofossil; Nummulites; Rupelian; Zagros Basin; Iran; LARGER FORAMINIFERA; MIOCENE DEPOSITS; DEZFUL EMBAYMENT; SHALLOW-MARINE; THRACE BASIN; OLIGOCENE; EOCENE; EVOLUTION; OLIGOMIOCENE; BIOZONATION;
D O I
10.47894/mpal.69.4.06
中图分类号
Q91 [古生物学];
学科分类号
0709 ; 070903 ;
摘要
Abiometrical study on four reticulate Nummulites populations from the lower part of Asmari Formation of the Vazag sec-tion (Zagros zone) is carried out. The biostratigraphy obtained by studing the succession points to the Early Oligocene (Rupelian), indi-cating shallow benthic zones SBZ21 and SBZ22A by the occurrence of Operculina cf. complanata, Eulepidina formosoides, Nephrolepidina sp. The age assignment is calibrated with calcareous nannofossils biostratigraphy indicating the NP22-NP23 (=CNO2-CNO3) Zones. We have observed a stratigraphic trend related to Nummulites bormidiensis Tellini 1888 that results to be char-acterized by two populations composed of transitional Nummulites fichteli/bormidiensis with values of mean inner proloculus that ex-ceeds by very little the boundary commonly established at 300 & mu;m. Such a populations, indicated as Nummulites ex interc. bormidiensis et fichteli, span through the lower Rupelian where classically just N. fichteli is reported so far. The stratigraphic distribution of Nummulites bormidiensisis and related transitional forms is here stretched to the Rupelian (SBZ21 and SBZ22A), encompassing older ages than previously recorded throughout the Neo-Tethys Ocean.
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页码:509 / 526
页数:18
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