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Beiranvand, Bijan, Ghasemi-Nejad, Ebrahim, Kamali, Mohammad Reza. (1392). Palynomorphs’ response to sea-level fluctuations: a case study from Late Cretaceous – Paleocene, Gurpi Formation, SW Iran. , 3(1), 11-24. doi: 10.22059/jgeope.2013.31928
Bijan Beiranvand; Ebrahim Ghasemi-Nejad; Mohammad Reza Kamali. "Palynomorphs’ response to sea-level fluctuations: a case study from Late Cretaceous – Paleocene, Gurpi Formation, SW Iran". , 3, 1, 1392, 11-24. doi: 10.22059/jgeope.2013.31928
Beiranvand, Bijan, Ghasemi-Nejad, Ebrahim, Kamali, Mohammad Reza. (1392). 'Palynomorphs’ response to sea-level fluctuations: a case study from Late Cretaceous – Paleocene, Gurpi Formation, SW Iran', , 3(1), pp. 11-24. doi: 10.22059/jgeope.2013.31928
Beiranvand, Bijan, Ghasemi-Nejad, Ebrahim, Kamali, Mohammad Reza. Palynomorphs’ response to sea-level fluctuations: a case study from Late Cretaceous – Paleocene, Gurpi Formation, SW Iran. , 1392; 3(1): 11-24. doi: 10.22059/jgeope.2013.31928

Palynomorphs’ response to sea-level fluctuations: a case study from Late Cretaceous – Paleocene, Gurpi Formation, SW Iran

Geopersia
مقاله 2، دوره 3، شماره 1، شهریور 2013، صفحه 11-24    اصل مقاله (1.34 M)
نوع مقاله: Research Paper
شناسه دیجیتال (DOI): 10.22059/jgeope.2013.31928
نویسندگان
Bijan Beiranvand* 1؛ Ebrahim Ghasemi-Nejad2؛ Mohammad Reza Kamali1
1Exploration & Production Division, Research Institute of Petroleum Industry, Tehran, Islamic Republic of Iran
2Department of Geology, University College of Sciences, University of Tehran, Tehran, Iran
چکیده
Statistical studies on Palynology contents of Late Cretaceous to Paleocene age Gurpi Formation in a surface section in Zagros Basin,
SW Iran indicate changes in abundance, species diversity, ratio of Spiniferites to Cyclonephelium (S/C), palynological marine index
(PMI) values and organic facies. These palynological variations clearly reflect fluctuations in relative sea-level and depositional
environment and can be used for recognition and differentiation of systems tracts and key horizons such as flooding surfaces and
sequence boundaries. Dramatic increase in PMI, dinoflagellate species diversity and S/C ratio associated with sedimentary facies
parameters indicate a marine transgressive systems tract while, a reduced species diversity, lower S/C ratio and PMI value along with
increase in abundance of phytoclasts and degraded land-plant materials are characteristics of marine regression. The variation trends of
the palynological parameters when consecutive indicate a complete cycle of relative sea-level change. Abundance of Spiniferites,
Achomosphaera, Areoligera, and Cleistosphaeridium species and presence of peridiniacean dinoflagellate cysts show a warm Tethyan,
upper bathyal to middle shelf environment of deposition for the Gurpi Formation. The nine depositional sequences identified here can
be correlated to the global third-order sea-level cycles. The main regional sequence surfaces like K180 (maximum flooding surface) in
the Late Cretaceous sequences (68Ma) in northeast of Arabian Plate are recognizable here.
کلیدواژه‌ها
Palynomorph؛ Sea-level fluctuation؛ Gurpi Formation؛ SW Iran
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