The Tethyan Seaway during the early to middle Miocene - New data and a review

被引:3
作者
Piller, Werner E. [1 ]
Harzhauser, Mathias [1 ,2 ]
Kranner, Matthias [2 ,3 ]
Mandic, Oleg [2 ]
Mohtat, Tayebeh [4 ]
Daneshian, Jahanbakhsh [5 ]
机构
[1] Karl Franzens Univ Graz, Inst Erdwissenschaften, NAWI Graz Geoctr, Heinrichstr 26, A-8010 Graz, Austria
[2] Nat Hist Museum Vienna, Geol Paleontol Dept, Burgring 7, A-1014 Vienna, Austria
[3] Bavarian Environm Agcy, Geol Dept, Hans Hogn Str 12, D-95030 Hof, Germany
[4] Geol Survey Iran, Azadi Sq,Meraj St, Tehran, Iran
[5] Kharazmi Univ, Dept Geol, Fac Sci, 43,Mofatteh Ave, Tehran 1571914911, Iran
关键词
Qom Formation; Asmari Formation; Gachsaran Formation; Iranian Gateway; Mesopotamian Gateway; EURASIA COLLISION ZONE; QOM FORMATION; CENTRAL IRAN; FORAMINIFERAL BIOSTRATIGRAPHY; GACHSARAN FORMATION; FACIES ANALYSIS; ZAGROS BASIN; DEPOSITIONAL-ENVIRONMENTS; SEQUENCE STRATIGRAPHY; BENTHIC FORAMINIFERA;
D O I
10.1016/j.gr.2024.08.004
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The Tethyan Seaway was the connection between the Eastern and Western Tethys which became restricted and finally closed during the Early and Middle Miocene. The growing Zagros Mountains split the seaway into two entities, the Iranian Gateway in the northeast and the Mesopotamian Gateway in the southwest. The reconstruction of the seaway is based on sedimentological and paleontological data of the Qom, Asmari and Gachsaran formations predominantly on biostratigraphy. This paper presents an evaluation and new data on the occurrence of the Qom Formation in the Zanjan area (Sheikh Jaber section) of Iran. The Qom Formation there is dominated by marls and sandstones and subordinated limestones. Unusual for the Qom Formation is the high share of volcanic rocks (basalts, tuffs, tuffitic marls, lapilli, coarse volcanoclastic components in all types of lithologies) which indicate that the Qom Formation in the Zanjan area belongs either to the Sanandaj-Sirjan Basin or the Urumieh-Dokhtar Basin. Planktonic foraminifers and mollusks, in particular, pteropods, indicate a late Burdigalian to Langhian age for the studied section. The mollusk fauna exhibits a pure Mediterranean character and no overlap with the Indo-Pacific fauna occurs. Both the fauna and the overlying continental deposits of the Upper Red Formation preclude a marine connection along the Iranian Gateway in the Langhian between the Proto-Mediterranean and Indian Ocean, the mollusk fauna also obviates a connection between the Proto-Mediterranean/Indian Ocean and the Eastern Paratethys. The sediments in the Mesopotamian Gateway are represented by the Asmari Formation, which is similar in facies and stratigraphy to the Qom Formation, and the Gachsaran Formation dominated by evaporites and shallow marine sediments. This gateway may have not been completely blocked in the Langhian, but the very shallow water connection was paleoceanographically ineffective and not passable for biota such as mollusks. (c) 2024 The Authors. Published by Elsevier B.V. on behalf of International Association for Gondwana Research. This is an open access article under the CC BY license (http://creativecommons.org/licenses/by/ 4.0/).
引用
收藏
页码:57 / 74
页数:18
相关论文
共 104 条
  • [1] Abich H., 1878, Geologische Forschungen in den Kaukasischen Landern. I. Theil. Eine Bergkalkfauna aus der Araxesenge bei Djoulfa in Armenien
  • [2] ADAMS C G, 1970, Bulletin of the British Museum (Natural History) Geology, V19, P87
  • [3] Adams C.G., 1983, Utrecht Micropaleontological Bulletins, P273
  • [4] Adams T., 2023, Geol. Explorat. Divis. Rep., V1074, P1
  • [5] Biometric study of late Oligocene larger benthic Foraminifera (Lepidocyclinidae and Nummulitidae) from the Qom Formation, Central Iran (Tajar-Kuh section)
    Akbar-Baskalayeh, Narges
    Less, Gyorgy
    Ghasemi-Nejad, Ebrahim
    Yazdi-Moghadam, Mohsen
    Pignatti, Johannes
    [J]. JOURNAL OF PALEONTOLOGY, 2020, 94 (04) : 593 - 615
  • [6] Microfacies models and sequence stratigraphic architecture of the Oligocene-Miocene Qom Formation, south of Qom City, Iran
    Amirshahkarami, Mahnaz
    Karavan, Mahnaz
    [J]. GEOSCIENCE FRONTIERS, 2015, 6 (04) : 593 - 604
  • [7] Tectono-sedimentary framework of the Gachsaran Formation in the Zagros foreland basin
    Bahroudi, A
    Koyi, HA
    [J]. MARINE AND PETROLEUM GEOLOGY, 2004, 21 (10) : 1295 - 1310
  • [8] Barrier E., 2018, Atlas of 20 maps
  • [9] PALAEOBIOGEOGRAPHY AND EVOLUTIONARY PATTERNS OF THE LARGER FORAMINIFER BORELIS DE MONTFORT (BORELIDAE)
    Bassi, Davide
    Braga, Juan C.
    Di Domenico, Giovanni
    Pignatti, Johannes
    Abramovich, Sigal
    Hallock, Pamela
    Koenen, Janine
    Kovacs, Zoltan
    Langer, Martin R.
    Pavia, Giulio
    Iryu, Yasufumi
    [J]. PAPERS IN PALAEONTOLOGY, 2021, 7 (01) : 377 - 403
  • [10] Behforouzi E, 2011, REV MEX CIENC GEOL, V28, P555