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Ghavidel-syooki, M.. (1395). Biostratigraphy of Acritarchs and Chitinozoans in Ordovician Strata from the Fazel Abad Area, Southeastern Caspian Sea, Alborz Mountains, Northern Iran: Stratigraphic Implications. , 28(1), 37-57.
M. Ghavidel-syooki. "Biostratigraphy of Acritarchs and Chitinozoans in Ordovician Strata from the Fazel Abad Area, Southeastern Caspian Sea, Alborz Mountains, Northern Iran: Stratigraphic Implications". , 28, 1, 1395, 37-57.
Ghavidel-syooki, M.. (1395). 'Biostratigraphy of Acritarchs and Chitinozoans in Ordovician Strata from the Fazel Abad Area, Southeastern Caspian Sea, Alborz Mountains, Northern Iran: Stratigraphic Implications', , 28(1), pp. 37-57.
Ghavidel-syooki, M.. Biostratigraphy of Acritarchs and Chitinozoans in Ordovician Strata from the Fazel Abad Area, Southeastern Caspian Sea, Alborz Mountains, Northern Iran: Stratigraphic Implications. , 1395; 28(1): 37-57.

Biostratigraphy of Acritarchs and Chitinozoans in Ordovician Strata from the Fazel Abad Area, Southeastern Caspian Sea, Alborz Mountains, Northern Iran: Stratigraphic Implications

Journal of Sciences, Islamic Republic of Iran
مقاله 4، دوره 28، شماره 1، فروردین 2017، صفحه 37-57    اصل مقاله (6.09 M)
نوع مقاله: Final File
نویسنده
M. Ghavidel-syooki*
Institute of Petroleum Engineering of Tehran University, Tehran, P. O. Box, 11365-4563, Islamic Republic of Iran
چکیده
Sixty-four surface samples from the Lower Palaeozoic rock units (mainly Lalun,
Abastu and Abarsaj formations) near Kholin-Darreh village in the Fazel Abad area,
southeastern the Caspian Sea, Northern Iran, were analyzed to determine their age
relationships. The samples of Lalun Formation were barren, but those of Abastu and
Abarsaj formations contained well-preserved and abundant palynomorph entities, which
are dominated by acritarchs (23 species belonging to 15 genera) and chitinozoans (29
species distributing among 15 genera) with remains of scolecodonts, graptolite and a
few cryptospores, although not determined in detail. Based on the restricted stratigraphic
range of acritarch species, an Early Ordovician (Tremadocian) age was assigned to the
Abastu Formation; while based upon index chitinozoan and acritarch taxa, a Late
Ordovician (Katian to Hirnantian) age was assigned to the Abarsaj Formation. Likewise,
based on the presence of diagnostic chitinozoan taxa, the Abarsaj Formation can be
assigned to the Armoricochitina nigerica, Ancyrochitina merga, Tanuchitina elongata
and Spinachitina oulebsiri chitinozoan Biozones. These chitinozoan assemblages reflect
a clear palaeobiogeographic affinity with the so-called "North Gondwana Domain".
Two major hiata are present within the studied Lower Palaeozoic succession in the Fazel
Abad area. The first hiatus appeared between the Lalun Formation (Early Cambrian) and
the Abastu Formation (Tremadocian) and includes the Middle-Upper Cambrian Mila
Formation. The second hiatus occurs between the Abastu Formation (Tremadocian) and
the Abarsaj Formation (Katian-Hirnantian) and spans the interval of the Floian-
Sandbian, which corresponds to uplift related to the initial stage of rifting of the Palaeo-
Tethys Ocean.
کلیدواژه‌ها
Acritarchs؛ Chitinozoans؛ Biostratigraphy؛ Gondwana؛ southeastern Caspian Sea
آمار
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