Biostratigraphy, paleoecology, and paleoenvironmental reconstruction of the Asmari formation in Zagros basin, southwest Iran
详细信息 查看全文
- 作者：Umid Kakemem ; Mohammad Hossein Adabi ; Abbas Sadeghi…
- 关键词：Asmari Formation ; Biostratigraphy ; Paleoecology ; Paleoenvironment ; Oligocene ; early Miocene
- 刊名：Arabian Journal of Geosciences
- 出版年：2016
- 出版时间：February 2016
- 年：2016
- 卷：9
- 期：2
- 全文大小：17,356 KB
- 参考文献：Abreu VS, Haddad GA (1998) Glacioeustatic variations: the mechanism linking stable isotope events and sequence stratigraphy from the early Oligocene to middle Miocene. SEPM Spec Publ 60:245–260
Adabi MH, Kakemem U, Sadeghi A (2015) Sedimentary facies, depositional environment, and sequence stratigraphy of Oligocene–Miocene shallow water carbonate from the Rig Mountain, Zagros basin (SW Iran). Carbonates Evaporites. doi:10.1007/s13146-015-0242-9
Adams CG, Bourgeois E (1967) Asmari Biostratigraphy. Geological and Exploration Div, Iranian Oil Offshore Company Report 1074: unpublished
Alavi M (2004) Regional stratigraphy of the Zagros fold-thrust belt of Iran and its proforland evolution. Am J Sci 304:1–20. doi:10.2475/ajs.304.1.1 CrossRef
Alavi M (2007) Structures of the Zagros fold-thrust belt in Iran. Am J Sci 307:1064–1095. doi:10.2475/09.2007.02 CrossRef
Altenbach AV, Lutze GF, Schiebel R, Schonfeld J (2003) Impact of interrelated and interdependent ecological controls on benthic foraminifera: an example from the Gulf of Guinea. Palaeogeogr Palaeoclimatol Palaeoecol 197(213):238
Amirshahkarami M, Vaziri-moghaddam H, Taheri A (2007) Sedimentary facies and sequence stratigraphy of the Asmari formation at Chaman-Bolbol, Zagros basin, Iran. J Asian Earth Sci 29:947–959. doi:10.1016/j.jseaes.2006.06.008 CrossRef
Barattolo F, Bassi D, Romano R (2007) Upper Eocene larger foraminiferal-coralline algal facies from the Knokova mountain(southern continental Greece). Facies 53:361–375CrossRef
Beavington-Penney SJ, Racey A (2004) Ecology of extant nummulitids and other larger benthic foraminifera: applications in palaeoenvironmental analysis. Earth Sci Rev 67:219–265. doi:10.1016/j.earscirev.2004.02.005 CrossRef
Berberian M, King GCP (1981) Towards a paleogeography and tectonic evolution of Iran. Can J Earth Sci 18:210–265. doi:10.1139/e81-163 CrossRef
BouDagher-Fadel MK (2008) Evolution and Geological Significance of Larger Benthic Foraminifera. Developments in Palaeontology and Stratigraphy, 21, Elsevier, p 540
BouDagher-Fadel MK (2013) Biostratigraphic and geological significance of planktonic foraminifera, 2nd edn. OVPR UCL, London, p 307. doi:10.14324/99.1 CrossRef
BouDagher-Fadel MK, Price GD (2014) The phylogenetic and palaeogeographic evolution of the nummulitoid larger benthic foraminifera. Micropaleontology 60(6):483–508
BouDagher-Fadel MK, Wilson M (2000) A revision of some larger foraminifera of the Miocene of Southeast Kalimantan. Micropaleontology 46:153–165. doi:10.2113/46.2.153 CrossRef
Brandano M, Frezza V, Tomassetti L, Pedley M (2009) Facies analysis and paleoenvironmental interpretation of the Late Oligocene Attard Member (Lower Coralline Limestone Formation), Malta. Sedimentology 56:1138–1158. doi:10.1016/j.palaeo.2008.12.018 CrossRef
Brandano M, Morsilli M, Vannucci G, Parente M, Bosellini F, Vicens G (2010) Rhodolith-rich lithofacies of the Porto Badisco Calcarenites (upper Chattian, Salento, southern Italy). J Geosci 129(1):119–131. doi:10.3301/1JG.2009.10
Brasier MD (1975) An outline history of seagrass communities. Palaeontology 18:681–702
Burchette TP, Wright VP (1992) Carbonate ramp depositional systems. Sediment Geol 79:3–57. doi:10.1016/0037-0738(92)90003-A CrossRef
Cahuzac B, Poignant A (1997) Essai de biozonation del 'Oligo-Miocene dans les loassinseuropeens al'aids des grands foraminifers netitique. Bull Soc Geol Fr 168:155–169
Chaproniere GCH (1975) Palaeoecology of Oligo-Miocene larger foraminiferida, Australia. Alcheringa 1:37–58CrossRef
Cosovic V, Drobne K, Moro A (2004) Paleoenvironmental model for Eocene foraminiferal limestones of the Adriatic carbonate platform (Istrian Peninsula). Facies 50:61–75. doi:10.1007/s10347-004-0006-9 CrossRef
Daneshian J, Ramezani-Dana L (2007) Early Miocene benthic foraminifera and biostratigraphy of the Qom Formation, Deh-Namak, Central Iran. J Asian Earth Sci 29:844–858CrossRef
Dickson J (1965) Carbonate identification and genesis as revealed by staining. J Sediment Petrol 205:491–505. doi:10.1038/205587a0
Dunham RJ (1962) Classification of carbonate rocks according to depositional texture. In: Classification of Carbonate Rocks. Journal of American Assocition Petroleum Geology, p 121
Ehrenberg SN, Pickard NAH, Laursen GV, Monibi S, Mossadegh ZK, Svånå TA, Aqrawi AAM, McArthur JM, Thirlwall MF (2007) Strontium isotope stratigraphy of the Asmari Formation (Oligocene - Lower Miocene), SW iran. J Pet Geol 30(2):107–128. doi:10.1111/j.1747-5457.2007.00107.x CrossRef
Embry AF, Klovan JE (1971) A late Devonian reef tract on northeastern banks island, NWT. Bull Can Petrol Geol 19:730–781
Flügel E (2010) Microfacies of carbonate rocks. Analysis, interpretation and application. Springer, p 976
Geel T (2000) Recognition of stratigraphic sequences in carbonate platform and slope deposits: empirical models based on microfacies analysis of paleogene deposits in southeastern Spain. Palaeogeogr Palaeoclimatol Palaeoecol 155:211–238. doi:10.1016/S0031-0182(99)00117-0 CrossRef
Gischler A, Lomando AJ (2005) Offshore sedimentary facies of a modern carbonate ramp, Kuwait, northwestern Arabian-Persian Gulf. Facies 50:443–462. doi:10.1007/s10347-005-0075-4 CrossRef
Gradstein FM, Ogg JG, Schmitz MD, Ogg GM (2012) The geologic time scale 2012. Elsevier 1–144. doi:10.1016/B978-0-444-59425-9.00004-4
Hallock P (1981) Production of carbonate sediments by selected large benthic foraminifera on two Pacific coral reefs. J Sediment Petrol 51:467–474
Hallock P, Glenn EC (1986) Larger foraminifera, a tool for paleoenvironmental analysis of Cenozoic carbonate facies. Palaios 1:55–64. doi:10.2307/3514459 CrossRef
Heydari E (2008) Tectonics versus eustatic control on supersequences of the Zagros Mountains of Iran. Tectonophysics 451:56–70. doi:10.1016/j.tecto.2007.11.046 CrossRef
Hohenegger J (2000) Coenoclines of larger foraminifera. Micropaleontology 46(1):127–151
Hohenegger J (2004) Depth coenoclines and environmental considerations of Western Pacific larger foraminifera. Journal of Foraminifera Research 34:9–33. doi:10.2113/0340009 CrossRef
Hohenegger J, Yordanova E, Hatta A (2000) Remarks on western Pacific nummulitidae (foraminiferida). J Foraminifer Res 30:3–28CrossRef
Hottinger L (1997) Shallow benthonic foraminiferal assemblages as signals for depth of their deposition and their limitations. Bull Geol Soc Den Fr 168:491–505
James GA, Wynd JG (1965) Stratigraphic nomenclature of Iranian oil consortium agreement area. Am Assoc Pet Geol Bull 49:2182–2245
James NP, Collins LB, Bone Y, Hallock P (1999) Subtropical carbonates in a temperate realm, modern sediment on the southwest Australian shelf. J Sediment Res 69:1297–1321CrossRef
Khadivi S (2010) Tectonic evolution and growth of the Zagros Mountain Belt (Fars, Iran): constraints from magnetostratigraphy, sedimentology and low- temperature thermochronometry, Earth sciences. Université Pierre et Marie Curie, Paris, p 225
Kumar A, Saraswati PK (1997) Response of larger foraminifera to mixed carbonate-silliciclastic environments: an example from the Oligocene-Miocene sequence of Kutch, India. Palaeogeogr Palaeoclimatol Palaeoecol 136:53–65CrossRef
Langer M, Hottinger L (2000) Biogeography of selected larger foraminifera. Micropaleontology 46:57–86
Laursen GV, Mobini S, Allan TL, Pickard NAH, Hosseiney A, Vincent B, Hamon Y, Van-Buchem FSP, Moallemi A, Druillion G (2009) The Asmari formation revisited: changed stratigraphic allocation and new biozonation: first International Petroleum Conference and Exhibition, Shiraz, Iran. Palaeogeogr Palaeoclimatol Palaeoecol 272:17–36CrossRef
Leckie RM, Olsen HC (2003) Foraminifera as proxies of sea-level change on silliciclastic margins. In: Olsen HC, Leckie RM (Eds) Micropaleontologic proxies for sea-level change and stratigraphic discontinuities. SEPM Special Publication 75: 5–19
Miller KG, Wright JD, Browning JV (2005) Visions of ice sheets in a greenhouse world. Mar Geol 217:215–231. doi:10.1016/j.margeo.2005.02.007 CrossRef
Mossadegh ZK, Haig DW, Allan T, Adabi MH, Sadeghi A (2009) Salinity changes during late Oligocene to early Miocene Asmari formation deposition, Zagros mountains, Iran. Palaeogeogr Palaeoclimatol Palaeoecol 272:17–36. doi:10.1016/j.palaeo.2008.10.021 CrossRef
Motiei H (1993) Stratigraphy of Zagros. Geological Survey of Iran Publication (in Persian). p 536
Murray JW (2006) Ecology and applications of Benthic foraminifera. Cambridge University Press, Cambridge, p 426. doi:10.1017/S0016756808004676 CrossRef
Mutti M, Piller WE, Betzler C (Eds.) (2011) Carbonate Systems During the Oligocene-Miocene Climatic Transition. Special Publication 42 of the International Associations of the Sedimentologists, p 312
Payros A, Pujalte V, Tosquella J, Orue-Etxebarria X (2010) The Eocene storm-dominated foralgal ramp of the western Pyrenees (Urbasa–Andia formation): an analogue of future shallow-marine carbonate systems? Sediment Geol 228(3):184–204. doi:10.1016/j.sedgeo.2010.04.010 CrossRef
Pecheux MJF (1995) Ecomorphology of a recent large foraminifer, Operculina ammonoides. Geobios 28:529–566. doi:10.1016/S0016-6995(95)80209-6 CrossRef
Pomar L (2001) Types of carbonate platforms: a genetic approach. Basin Res 13:313–334. doi:10.1046/j.0950-091x.2001.00152.x CrossRef
Rahaghy A (1980) Tertiary faunal assemblage of Qom-Kashan, Sabzewar and Jahrom area. National Iranian Oil Company, Geological Laboratories, Publication 8
Rasser MW, Scheibner C, Mutti M (2005) A paleoenvironmental standard section for Early Ilerdian tropical carbonate factories (Corbieres, France; Pyrenees, Spain). Facies 51:217–232CrossRef
Read JF (1985) Carbonate platform facies models. Bull Am Assoc Pet Geol 69:1–21
Renema W (2002) Larger foraminifera and their distribution patterns on the Spermonde shelf, South Sulawesi. Scr Geol 124:1–263. doi:10.1016/S0016-6995(95)80209-6
Renema W (2006) Large benthic foraminifera from the deep photic zone of a mixed siliciclastic-carbonate. Mar Micropaleontol 58:73–82. doi:10.1016/j.marmicro.2005.10.004 CrossRef
Romero J, Caus E, Rossel J (2002) A model for the palaeoenvironmental distribution of larger foraminifera based on Late Middle Eocene deposits on the margin of the south Pyrenean basin (SE Spain). Palaeogeogr Palaeoclimatol Palaeoecol 179:43–56. doi:10.1016/S0031-0182(01)00406-0 CrossRef
Sadeghi R, Vaziri-Moghaddam H, Taheri A (2011) Microfacies and sedimentary environment of the Oligocene sequence (Asmari formation) in Fars sub-basin, Zagros mountains, southwest Iran. Facies 57:431–446. doi:10.1007/s10347-010-0245-x CrossRef
Samankassou E (2002) Cool-water carbonates in paleoequatorial shallow-water environment: the paradox of the Auering cyclic sediments (Upper Pennsylvanian, Carnic Alps, Austria-Italy) and its implications. Geology 30:655–658. doi:10.1130/0091-7613(2002)030<0655:CWCIAP>2.0.CO;2 CrossRef
Schlager W (2005) Carbonate sedimentology and sequence stratigraphy, vol 8. SEPM, USA, p 200CrossRef
Scholle PA, Scholle Dana SU (2006) A color guide to the petrography of carbonate rock: grain, texture, porosity, diagenesis. Bull Am Assoc Pet Geol 69:549
Sepehr M, Cosgrove JW (2004) Structural framework of the Zagros Fold-Thrust Belt, Iran. Mar Pet Geol 21:829–843. doi:10.1016/j.marpetgeo.2003.07.006 CrossRef
Seyrafian A, Vaziri-Moghaddam H, Torabi H (1996) Biostratigraphy of the Asmari formation. Burujen area, Iran. Journal of Science 7:31–47
Sharland PR, Archer R, Casey DM, Davis RB, Hall SH, Heward AP, Horbury AD, Simmons MD (2001) Arabian plate sequence stratigraphy. Geo-Arabia 2:1–371
Sharland PR, Casey DM, Davies RB, Simmons MD, Sutcliffe OE (2004) Arabian plate sequence straigraphy—revisions to SP2. Geo-Arabia 9:199–214
Shinn E (1983) Tidal flat environment. In: Scholle PA, Bebout DG, Moore C (eds) Carbonate depositional environments. Bulletin American Association Petroleum Geologists 33:171–210
Stocklin J (1968) Structural history and tectonics of Iran: a review. Bull Am Assoc Pet Geol 52:1229–1258
Thomas AN (1950) The Asmari limestone of southwest Iran. In: 18th International Geological Congress, London, pt. 6:35–55
Tucker ME, Wright VP (1990) Carbonate sedimentology. Blackwell Scientific Publications, p 482
Van Buchem FSP, Allan TL, Laursen GV, Lotfpour M, Moallemi A, Monibi M, Motiei H, Pickard NAH, Tahmasbi AR, Vedrenne V, Vincent B (2010) Regional stratigraphic architecture and reservoir types of the Oligo-Miocene deposits in the Dezful embayment (Asmari and Pabdeh formations) SW Iran. Geol Soc Lond, Spec Publ 329:219–263. doi:10.1144/SP329.10 CrossRef
Vaziri-Moghaddam H, Kimiagari M, Taheri A (2006) Depositional environment and sequence stratigraphy of the Oligo-Miocene Asmari Formation in SW Iran, Lali Area. Facies 52:41–51. doi:10.1007/s10347-005-0018-0 CrossRef
Wilson JL (1975) Carbonate Facies in Geological History. Springer, p 471
Wilson MEJ, Evans MEJ (2002) Sedimentology and diagenesis of tertiary carbonates on the Mangkalihat Peninsula, Borneo: implications for subsurface reservoir quality. Mar Pet Geol 19:873–900. doi:10.1016/S0264-8172(02)00085-5 CrossRef
Wilson MEJ, Vecsei A (2005) The apparent paradox of abundant foramol facies in low latitudes: their environmental significance and effect on platform development. Earth Sci 69:133–168. doi:10.1016/j.earscirev.2004.08.003
Wynd J (1965) Biofacies of Iranian Oil Consortium Agreement Area, IOOC Report 1082: unpublished
Zachos JC, Pagani M, Sloan L, Tomas E, Billups K (2001) Trends rhythms and aberrations in global climate 65Ma to present. Science 292:686–693. doi:10.1126/science.1059412 CrossRef - 作者单位：Umid Kakemem (1)
Mohammad Hossein Adabi (2)
Abbas Sadeghi (2)
Mohammad Hasan Kazemzadeh (3)
1. Special Drilling Services Devision, National Iranian Drilling Compay, Ahwaz, Iran
2. Department of Geology, Faculty of Earth Sciences, Shahid Beheshti University, Tehran, Iran
3. Tehran Energy Consultants Company, Tehran, Iran - 刊物类别：Earth and Environmental Science
- 出版者：Springer Berlin Heidelberg
- ISSN：1866-7538
文摘
The present work is focused on the biostratigraphic analysis, paleoecological interpretations, and paleoenvironmental reconstruction of sediments of the Asmari Formation. The Asmari Formation, which is mainly composed of carbonates, has been studied in the Rig anticline in the Izeh zone, Zagros Basin, Iran. The Asmari Formation at the study area is Rupelian to Burdigalian in age, based on the occurrence of 21 foraminiferal species belonging to 21 genera which led to identification of five assemblage zones including (1) Nummulites vascus-Nummulites fichteli, (2) Lepidocyclina-Operculina-Ditrupa, (3) Archaias asmaricus-Archaias hensoni-Miogypsinoides complanatus, (4) Miogypsina sp.-Elphidium sp. 14-Peneroplis farsenensis, and (5) Borelis melo group-Meandropsina iranica. Detailed petrographic analysis led to the recognition of 13 facies that are belonging to four depositional environments including tidal flat, lagoon, shoal, and open marine environments. These carbonate facies were deposited in shallow marine carbonate platform as a homoclinal ramp type. The lower part of the Asmari Formation deposited in an open marine environment with normal water salinity, while the middle and upper parts of the Asmari Formation were deposited in a shallower water with alternating intermittent normal and higher water salinity. Occurrence of larger benthic foraminifera such as Nummulites, Operculina, Heterostegina, Amphistegina, Archaias, Peneroplis and Borelis, coral and red algae reflect mesophotic to oligophotic conditions in subtropical to tropical environments with a high nutrient stability in a mesotrophic to oligotrophic conditions existed during deposition of the Asmari Formation.