Biodiversity and community structure of Late Pleistocene foraminifera from Kish Island, Persian Gulf (Iran)
Tóm tắt
The raised coral reef sequences at Kish Island provide a rare window into the depositional setting and paleoenvironment of a high-latitude, shallow-water coral reef that developed under turbid conditions in the Persian Gulf during Marine Isotope Stage 7 (~200 to 250 ka). Six sedimentary facies and eight foraminiferal assemblages can be identified throughout the sequence. A ninth assemblage can be defined for the modern subtidal realm. At the base of the sequence is a marl rich in hyaline foraminifera (Elphidium, Ammonia, Asterorotalia, Bulimina, Nonion, and Quinqueloculina) and ostracods, which was deposited in about 30–40 m water depth in a turbid deltaic setting. Shallowing resulted in the marl becoming sandy, and changing to a mollusc-rich facies with rare foraminifera (mostly smaller miliolid taxa) that formed the substrate for coral recruitment. The coral marl layer contains many large corals embedded in situ in an aggregate and coralline algae-rich marl. Two abundance peaks in the foraminifera occur at the base and mid-way through this layer, which also correspond to a change from Murrayinella-dominated to Placopsilina-dominated assemblages, indicating deepening and more open-marine conditions, but elevated turbidity. Towards the top of the layer, abundance of foraminifera decreases and miliolid foraminifera become dominant. The top-most layer is dominated by coral and mollusc fragments and has an Amphistegina-rich reef-related assemblage. Of the Late Pleistocene foraminiferal assemblages, the Murrayinella-, Pararotalia-, and Placopsilina-dominated assemblages are no longer present in the modern gulf for unknown reasons. Of the other five assemblages, only the Amphistegina assemblage is found within proximity to the modern Kish Island. The Elphidium and Asterorotalia-Bulimina assemblages are from deeper areas of the gulf. The Ammonia and Quinqueloculina assemblages occur in lagoonal sediments on the Arabian side of the gulf. Like the modern Persian Gulf, the diversity of foraminifera was low (~80 common species) during the Pleistocene and does not correlate with foraminiferal abundance.
Tài liệu tham khảo
Al-Ghadban AN, Abdali F (1998) Sedimentation rate and bioturbation in the Arabian Gulf. Environ Int 24:23–31
Al-Rifaiy IA, Cherif OH (1988) The fossil coral reefs of Al-Aqaba, Jordan. Facies 18:219–230
Badawi A, Schmiedl G, Hemleben C (2005) Impact of late quaternary environmental changes on deep-sea benthic foraminiferal faunas of the Red Sea. Mar Micropaleont 58:13–30
Bicchi E, Debenay JP, Pagés J (2002) Relationship between benthic foraminiferal assemblages and environmental factors in atoll lagoons of the Central Tuamotu Archipelago (French Polynesia). Coral Reefs 21:275–290
Brewer PG, Dyrssen D (1985) Chemical oceanography of the Persian Gulf. Prog Oceanogr 14:41–55
Cherif OH, Al-Ghadban AN, Al-Rifaiy IA (1997) Distribution of foraminifera in the Arabian Gulf. Micropaleontology 43:253–280
Chivas AR, Garcia A, van der Kaars S, Couapel MJJ, Holt S, Reeves JM, Wheeler DJ, Switzer AD, Murray-Wallace CV, Banerjee D, Price DM, Wang SX, Pearson G, Edgar NT, Beaufort L, De Deckker P, Lawson E, Cecil CB (2001) Sea-level and environmental changes since the last interglacial in the Gulf of Carpentaria, Australia: an overview. Quat Int 83:19–46
Coles SL, Fadlallah YH (1991) Reef coral survival and mortality at low temperatures in the Arabian Gulf: new species-specific lower temperature limits. Coral Reefs 9:231–237
Crame JA (1980) Succession and diversity in the Pleistocene coral reefs of the Kenya coast. Palaeontology 23:1–37
Crame JA (1981) Ecological stratification in the Pleistocene coral reefs of the Kenya coast. Palaeontology 24:609–646
Debenay J-P (2000) Foraminifers of paralic tropical environments. Micropaleontol 46(suppl 1):153–160
Dullo WC (1990) Facies, fossil record and age of Pleistocene reefs along the Red Sea (Saudi Arabia). Facies 22:1–46
Ellis BF, Messina A (1940) et seq. Catalogue of foraminifera. American Museum of Natural History, New York (1940 and suppl)
Ghazban F (2007) Petroleum geology of the Persian Gulf. Tehran University and National Iranian Oil Company, Tehran, p 707
Gischler E, Lomando AJ (2005) Offshore sedimentary facies of a modern carbonate ramp, Kuwait, northwestern Arabian-Persian Gulf. Facies 50:443–462
Haake FW (1975) Miliolinen (Foram.) in Oberflächensedimenten des Persischen Golfes. Meteor Forsch Ergeb Reihe C 21:15–51
Haig DW (1997) Foraminifera from Exmouth Gulf, Western Australia. J R Soc Western Aust 80:263–280
Hallock P (2000) Larger Foraminifers as indicators of coral reef vitality. In: Martin R (ed) Environmental micropaleontology. Topics Geobiol 15:121–150
Hallock P, Lidz BH, Cockey-Burkhard EM, Donnelly KB (2003) Foraminifera as bioindicators in coral reef assessment and monitoring: the FORAM index. Environ Monit Assess 81:221–238
Hammer O, Harper DAT, Ryan PD (2001) PAST: palaeontological statistics software package for education and data analysis. Palaeontologia Electronica 4(1):1–9
Haunold TG, Baal C, Piller WE (1998) Larger foraminifera. In: Piller WE, Haunold TG (eds) The northern Bay of Safaga (Red Sea, Egypt), an actuopalaeontological approach. V. Foraminifera. Abh Senck Naturforsch Gesellsch 548:155–180
Hohenegger J (1994) Distribution of living larger Foraminifera NW of Sesoko-Jima, Okinawa, Japan. Mar Ecol 15:291–334
Hohenegger J, Yordanova E, Nakano Y, Tatzreiter F (1999) Habitats of larger foraminifera on the upper slope of Sesoko Island, Okinawa, Japan. Mar Micropaleont 36:109–168
Hottinger L, Halicz E, Reiss Z (1993) Recent Foraminiferida from the Gulf of Aqaba. Red Sea. Slov Akad Znan Umetnosti, Ljubljana, p 179
Houbolt JJHC (1957) Surface sediments of the Persian Gulf near the Qatar Peninsula. Thesis, State Univ Utrecht, p 113
Javaux EJ, Scott DB (2003) Illustration of modern benthic foraminifera from Bermuda and remarks on distribution in other subtropical/tropical areas. Palaeont Electron 6(4):1–29
Kim J-M, Kucera M (2000) Benthic foraminifer record of environmental changes in the Yellow Sea (Hwanghae) during the last 15, 000 year. Q Sci Rev 19:1067–1085
Lambeck K (1996) Shoreline reconstructions for the Persian Gulf since the last glacial maximum. Earth Planet Sci Lett 142:43–57
Langer M, Hottinger L (2000) Biogeography of selected “larger” foraminifera. Micropaleontology 46(Suppl 1):105–127
Langer M, Lipps JH (2003) Foraminiferal distribution and diversity, Madang reef and lagoon, Papua New Guinea. Coral Reefs 22:143–154
Lobegeier MK (2002) Benthic foraminifera of the family Calcarinidae from Green Island Reef, Great Barrier Reef Province. J Foram Res 32:201–216
Loeblich AR, Tappan H (1987) Foraminiferal genera and their classification. Van Nostrand Reinhold, New York, p 970
Loeblich AR, Tappan H (1994) Foraminifera of the Sahul Shelf. Cushman Found Foram Res Spec Pub 31:1–661
Lomando AJ (1999) Structural influence on facies trends of carbonate inner ramp systems, examples from the Kuwaiti-Saudi Arabian coast of the Arabian Gulf and northern Yucatan, Mexico. GeoArabia 4:339–360
Lutze GF (1974) Benthische Foraminiferen in Oberflächen-Sedimenten des Persischen Golfes. Teil: Arten. Meteor Forsch Ergeb Reihe C 7:1–66
Lutze G, Wolf R (1975) Persian Gulf foraminifera, depth distribution and sea level change. Marit Sedim, Spec Publ 1:425–429
Lutze G, Grabert B, Seibold E (1971) Lebendbeobachtungen an Gross-Foraminiferen (Heterostegina) aus dem Persichen Gulf. Teil Arten. Meteor Forsch Ergeb Reihe C 6:21–40
Meandro Consultant Engineers (2006) Report on the engineering geology and earthquake risk assessment of Kish Island. Unpubl Rep Kish Island Authority (in Farsi)
Melguen M (1973) Corresponding analysis for recognition of facies in homogeneous sediments off an Iranian river mouth. In: Purser BH (ed) The Persian Gulf. Holocene carbonate sedimentation and diagenesis in a shallow epicontinental sea. Springer, Berlin Heidelberg New York, pp 99–114
Melis R, Violanti D (2006) Foraminiferal biodiversity and Holocene evolution of the Phetchaburi coastal area (Thailand Gulf). Mar Micropaleont 61:94–115
Mossadegh ZK, Haig DW, Allan T, Adabi MH, Sadeghi A (2009) Salinity changes during Late Oligocene to Early Miocene Asmari Limestone deposition, Zagros Mountains, Iran. Palaeogeogr Palaeoclimat Palaeoecol 272:17–36
Motiei H, (1993) Stratigraphy of Zagros. Treatise on the geology of Iran no. 1, Ministry mines metals. Geol Surv Iran, Tehran, p 199 (in Farsi)
Murray JW (1965) The Foraminiferida of the Persian Gulf. 2. The Abu Dhabi Region. Palaeogeogr Palaeoclimatol Palaeoecol 1:307–332
Murray JW (1966a) The Foraminiferida of the Persian Gulf. 4. Khor Al Bazam. Palaeogeogr Palaeoclimatol Palaeoecol 2:153–169
Murray JW (1966b) The Foraminiferida of the Persian Gulf. 3. The Halat Al Bahrani Region. Palaeogeogr Palaeoclimatol Palaeoecol 2:59–68
Murray JW (1966c) The Foraminiferida of the Persian Gulf. 5. The shelf off the trucial coast. Palaeogeogr Palaeoclimatol Palaeoecol 2:267–278
Murray JW (2006) Ecology and applications of benthic foraminifera. Cambridge University Press, Cambridge, p 426
Nigam R, Saraswat R, Kurtarka SR (2006) Laboratory experiment to study the effect of salinity variations on benthic foraminiferal species—Pararotalia nipponica (Asano). J Geol Soc India 67:41–46
Nomura R, Takayanagi Y (2000) The suprageneric classification of the foraminiferal genus Murrayinella and a new species from Japan. Paleont Res 4:171–181
Orpin AR, Haig DW, Woolfe KJ (1999) Sedimentary and foraminiferal facies in Exmouth Gulf, in arid tropical northwestern Australia. Austral J Earth Sci 46:607–621
Pandolfi JM (1996) Limited membership in Pleistocene reef coral assemblages from the Huon Peninsula, Papua New Guinea: constancy during global change. Paleobiology 22:152–176
Pandolfi JM (1999) Response of Pleistocene coral reefs to environmental change over long temporal scales. Am Zool 39:113–130
Parker JH (2009) Taxonomy of foraminifera from Ningaloo Reef, Western Australia. Mem Assoc Austral Palaeont 36:1–812
Parker JH, Gischler E (2011) Modern foraminiferal distribution and diversity in two atolls from the Maldives, Indian Ocean. Mar Mircopaleont 78:30–49
Pillai CSG (1977) The structure, formation and species diversity of south Indian reefs. Proc 3rd Int Coral Reef Symp 2:47–53
Pirazzoli PA, Reyss JL, Dontugne M, Haghipour A, Hilgers A, Kasper HU, Nazari H, Preusser F, Radtke U (2004) Quaternary coral-reef terraces from Kish and Qeshm Islands, Persian Gulf: new radiometric ages and tectonics implications. Quat Int 120:15–27
Playford PE (2004) Geology and hydrology of Rottnest Island, Western Australia. In: Vacher HL, Quinn T (eds) Geology and hydrology of carbonate islands. Develop Sediment 54:783–810
Purkis SJ, Renegar DA, Riegl BM (2011) The most temperature-adapted corals have an Achilles’ Heel. Mar Poll Bull 62:246–250
Purser BH (1973) Sedimentation around bathymetric highs in the southern Persian Gulf. In: Purser BH (ed) The Persian Gulf. Holocene carbonate sedimentation and diagenesis in a shallow epicontinental sea. Springer, Berlin Heidelberg New York, pp 157–178
Reiss Z, Hottinger L (1984) The Gulf of Aqaba—ecological micropaleontology. Ecol Stud, 50. Springer, Berlin Heidelberg New York, p 354 (Ecol Stud, 50)
Renema W (2006) Habitat variables determining the occurrence of large benthic foraminifera in the Berau area (East Kalimantan, Indonesia). Coral Reefs 25:351–359
Renema W, Troelstra SR (2001) Larger foraminifera distribution on a mesotrophic carbonate shelf in SW Sulawesi (Indonesia). Palaeogeogr Palaeoclimatol Palaeoecol 175:125–146
Renema W, Hoeksema BW, van Hinte JE (2001) Larger benthic foraminifera and their distribution patterns on the Spermonde shelf, South Sulawesi. Zool Verh (Leiden) 334:115–150
Saidova KM (2010) Benthic foraminifer communities of the Persian Gulf. Oceanology 50:61–66
Sanders D, Baron-Szabo RC (2005) Scleractinian assemblages under sediment input: their characteristics and relation to the nutrient input concept. Palaeogeogr Palaeoclimatol Palaeoecol 216:139–181
Sarnthein M (1972) Sediments and history of the postglacial transgression in the Persian Gulf and northwest Gulf of Oman. Mar Geol 12:245–366
Sarnthein M, Walger E (1973) Classification of modern marl sediments in the Persian Gulf by factor analysis. In: Purser BH (ed) The Persian Gulf. Holocene carbonate sedimentation and diagenesis in a shallow epicontinental sea. Springer, Berlin Heidelberg New York, pp 81–89
Seibold E, Diester L, Fütterer D, Lange H, Müller P, Werner F (1973) Holocene sediments and sedimentary processes in the Iranian part of the Persian Gulf. In: Purser BH (ed) The Persian Gulf. Holocene carbonate sedimentation and diagenesis in a shallow epicontinental sea. Springer, Berlin Heidelberg New York, pp 57–80
Sheppard C, Al-Husiani M, Al-Jamali F, Al-Yamani F, Baldwin R, Bishop J, Benzoni F, Dutrieux E, Dulvy NK, Durvasula SRV, Jones DA, Loughland R, Medio D, Nithyanandan M, Pilling GM, Polikarpov I, Price ARG, Purkis S, Riegl B, Saburova M, Samimi Namin K, Taylor O, Wilson S, Zainal K (2010) The Gulf: a young sea in decline. Mar Poll Bull 60:13–38
Shinn EA (1969) Submarine lithification of Holocene carbonate sediments in the Persian Gulf. Sedimentology 12:109–144
Stainforth RM (1952) Ecology of arenaceous foraminifera. Micropaleontol 6:1–42
Stoffers P, Ross DA (1979) Late Pleistocene and Holocene sedimentation in the Persian Gulf–Gulf of Oman. Sediment Geol 23:181–208
Strasser A, Strohmenger C (1997) Early diagenesis in Pleistocene coral reefs, southern Sinai, Egypt: response to tectonics, sea-level and climate. Sedimentology 44:537–558
Szarek R, Kuhnt W, Kawamura H, Kitizato H (2006) Distribution of Recent benthic foraminifera on the Sunda Shelf (South China Sea). Mar Micropaleont 61:171–195
Uchupi E, Swift SA, Ross DA (1999) Late quaternary stratigraphy, paleoclimate and neotectonism of the Persian Arabian/Gulf region. Mar Geol 160:1–23
Uthicke S, Nobes K (2008) Benthic foraminifera as indicators for terrestrial runoff: a foram index for the GBR. Estuar Coast Shelf Sci 78:763–773
Uthicke S, Thompson A, Schaffelke B (2010) Effectiveness of benthic foraminiferal and coral assemblages as water quality indicators on inshore reefs of the Great Barrier Reef, Australia. Coral Reefs 29:209–225
Wagner E, van der Togt C (1973) Holocene sediment types and their distribution in the southern Persian Gulf. In: Purser BH (ed) The Persian Gulf. Holocene carbonate sedimentation and diagenesis in a shallow epicontinental sea. Springer, Berlin Heidelberg New York, pp 123–156
Walkden G, Williams A (1998) Carbonate ramps and the Pleistocene–Recent depositional systems of the Arabian Gulf. In: Wright VP, Burchette TP (eds) Carbonate ramps. Geol Soc Spec Publ 149:43–53
Walker SE, Parsons-Hubbard K, Richardson-White S, Brett C, Powell E (2011) Alpha and beta diversity of encrusting foraminifera that recruit to long-term experiments along a carbonate platform to shelf gradient: paleoecological and paleoenvironmental implications. Palaeogeogr Palaeoclimatol Palaeoecol. doi:10.1016/j.palaeo.2011.04.028
Waller HO (1960) Foraminiferal biofacies off the south China coast. J Paleont 34:1164–1182
Woodroffe SA, Horton BP, Larcombe P (2005) Contemporary intertidal foraminifera distributions of Cleveland Bay, Central Great Barrier Reef shelf, Australia: implications for sea-level reconstructions. J Foram Res 35:259–270
Zheng S (1990) Foraminiferal fauna trends and assemblages of the Bohai Sea, Huanghai Sea and East China Sea. Bull Mar Sci 47:192–212