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Foraminiferal biostratigraphy and paleoecology of the late Santonian-early Paleocene in the eastern Tethys, Northern Iran

Author Affiliations

  • 1Department of Geological Sciences, University of Florida, Gainesville, FL USA

Int. Res. J. Earth Sci., Volume 6, Issue (8), Pages 1-10, August,25 (2018)

Abstract

The late Santonian-early Paleocene sequences were investigated at the Galanderud section, to recognize the biostratigraphy scheme paleoenvironmental changes in eastern Tethys. This section mainly consists of green and gray marl, marly limestone, and limestones. A high-resolution study based upon benthic and planktic foraminiferal assemblages has been used. The planktic foraminifera were diverse and abundance, where 56 planktic species belonging to 27 genera have been recognized. In this study, first and last appearances of the planktic foraminifera have been used as major bio events to identified different biozonation. Planktic foraminiferal zonation from bottom to top of the section consists of fifteen zones include: i. Dicarinella asymetrica, ii. Globotruncanita elevata, iii. Globotruncana ventricosa, iv. Radotruncana calcarata, v. Globotruncanella havanensis, vi. Globotruncana aegyptiaca, vii. Gansserina gansseri, viii. Racemiguembelina fructicos, ix. Pseudoguembelina hariaensis, x. Pseudoguembelina palpebra, xi. Plummerita hantkeninoides, xii. Guembelitria cretacea, xiii. Parvularugoglobigerina eugubina, xiv. Parasubbotina pseudobulloides, xv. Subbotina triloclinoides. Also, three distinct zones have been defined based on benthic foraminifera morphotypes and Cibicidoides spp. First zone (Dicarinella asymetrica to Gansserina gansseri biozones) is dominated by Infauna morphotype and less abundance of Cibicidoides spp. indicating high food availability and lower oxygen condition. The second zone, with the increase of epifauna morphotype and Cibicidoides spp. show decreasing in organic matter. Finally, high abundance of epifauna species and Cibicidoides spp. indicate a collapse of food availability after the extinction of primary producers that may cause by asteroid impact after Cretaceous- Paleogene boundary mass extinction.

References

  1. Alavi M. (1996)., Tectonostratigraphic synthesis and structural style of the Alborz mountain system in northern Iran., Journal of Geodynamics, 21(1), 1-33.
  2. Asgharian Rostami M., Darvishzad B. and Ghasemi Nejad E. (2009)., Planktonic Foraminifera Response to Sudden Global Warming in Late Maastrichtian, a Case Study from Ziyarat-Kola, Central Alborz, Iran., Journal of Sciences, Islamic Republic of Iran, 20, 233-242.
  3. Asgharianrostami M., Leckie R.M. and Font E. (2013)., High stress environment across the Cretaceous/Paleogene boundary at the Galanderud section (northern Alborz, Iran)., Geological Society of America Annual Meeting, Denver, Colorado, USA.
  4. Asgharianrostami M., Vahidinia M., Ghasemi-Nejad E. and Sadeghi A. (2013)., Biostratigraphy and mass extinction pattern across the Cretaceous/Paleogene boundary, Northern Alborz, Iran., Open Journal of Geology, 3, 33-38.
  5. Asgharianrostami M., Leckie R.M., Font E., Frontalini F. and Koeberl C. (2014)., Turnover and paleoenvironmental changes across the Cretaceous/Paleogene boundary at the Galanderud section (Northern Alborz, Iran) based on benthic foraminifera., EGU General Assembly, Vienna, Austria.
  6. Asgharian Rostami M., Leckie R.M., Font E., Frontalin F., Finkelstein D. and Koeberl C. (2018)., The Cretaceous-Paleogene transition at Galanderud (northern Alborz, Iran): A multidisciplinary approach., Palaeogeography, Palaeoclimatology, Palaeoecology, 493, 82-101.
  7. Corliss B.H. and Chen C. (1988)., Morphotype patterns of Norwegian Sea deep-sea benthic foraminifera and ecological implications., Geology, 16(8), 716-719.
  8. Frontalini F., Rostami M.A. and Coccioni R. (2016)., Paleobathymetric assessments of the upper Albian-lower Danian Gubbio section (Italy)., Geological Society of America Special Papers, 524, 105-113.
  9. Keller G. (1988)., Extinction, survivorship and evolution of planktic foraminifera across the Cretaceous/Tertiary boundary at El Kef, Tunisia., Marine Micropaleontology, 13(3), 239-263.
  10. Keller G. (1988)., Biotic turnover in benthic foraminifera across the Cretaceous/Tertiary boundary at El Kef, Tunisia., Palaeogeography, Palaeoclimatology, Palaeoecology, 66(3-4), 153-171.
  11. Arenillas I., Arz J.A. and Molina E. (2004)., A new high-resolution planktic foraminiferal zonation and subzonation for the lower Danian., Lethaia, 37, 79-95.
  12. Berggren W.A. and Pearson P.N. (2005)., A revised tropical to subtropical Paleogene planktonic foraminiferal zonation., The Journal of Foraminiferal Research, 35(4), 279-298.
  13. Li L. and Keller G. (1998)., Maastrichtian climate, productivity and faunal turnovers in planktic foraminifera in South Atlantic DSDP Sites 525A and 21., Marine Micropaleontology, 33, 55-86.
  14. Berggren W.A., Kent D.V., Swisher C.C. and Aubry M.P. (1995)., A revised Cenozoic geochronology and chronostratigraphy., in Berggren, W. A., Kent, D. V., Swisher, C. C., III, Aubry, M.-P. and Hardenbol, J., (Editors), Geochronology, Time Scales and Global Stratigraphic Correlation. SEPM (Society for Sedimentary Geology) Special Publication, 54, 129-212.
  15. Robaszynski F. (1984)., Atlas of late Cretaceous globotruncanids., Rev. Micropaleont., 26, 145-305.
  16. Caron M. (1985)., Cretaceous planktonic foraminifera., Plankton stratigraphy, 17-86.
  17. Nederbragt A.J. (1989)., Maastrichtian Heterohelicidae (planktonic Foraminifera) from the north west Atlantic., Journal of Micropalaeontology, 8, 183-206.
  18. Nederbragt A.J. (1991)., Late Cretaceous biostratigraphy and development of Heterohelicidae (planktic foraminifera)., Micropaleontology, 329-372.
  19. Bolli H.M., Beckmann J.P. and Saunders J.B. (1994)., Benthic Foraminiferal Biostratigraphy of the South Caribbean Region., Cambridge University Press, 408.
  20. Olsson R.K., Hemleben C., Berggren W.A. and Huber B.T. (1999)., Atlas of Paleocene Planktonic Foraminifera., Smithsonian Contributions to Paleobiology, 85, 255.
  21. Premoli Silva I. and Verga D. (2004)., Practical Manual of Cretaceous Planktonic Foraminifera., course 3, in Verga, D., and Rettori, R. (Editors), International School on Planktonic Foraminifera: Universities of Perugia and Milano, Tipografiadi di Pontefelcino, Perugia, Italy, 283.
  22. Canudo J.I., Keller G. and Molina E. (1991)., Cretaceous/Tertiary boundary extinction pattern and faunal turnover at Agost and Caravaca, SE Spain., Marine Micropaleontology, 17(3-4), 319-341.
  23. Postuma J.A. (1971)., Manual of Planktonic Foraminifera., Elsevier, Amsterdam, London, 397.
  24. Premoli S.I. and Sliter W.V. (1995)., Cretaceous planktonic foraminiferal biostratigraphy & evolutionary trends from the Bottaccione section, Gubbio, Italy., Paleontographia Italica, 82, 89.
  25. Premoli Silva I. and Sliter W.V. (1981)., Cretaceous planktonic foraminifers from the Nauru Basin, Leg 61, Site 462, western equatorial Pacific., Initial Rep. Deep Sea Drill. Proj, 61, 423-437.
  26. Robaszynski F. and Caron M. (1995)., Foraminiferes planctoniques du Cretace; commentaire de la zonation Europe-Mediterranee., Bulletin de la Société géologique de France, 166(6), 681-692.
  27. Petrizzo M.R. (2003)., Late cretaceous planktonic foraminiferal bioevents in thetethys and in the southern ocean record: an overview., The journal of foraminiferal research, 33(4), 330-337.
  28. Pardo A. Ortiz N. and Keller G. (1996)., Latest Maastrichtian and Cretaceous-Tertiary Boundary Foraminiferal Turmover and Environmental Changes at Agost, Spain., Cretaceous. Tertiary Mass Extinction: Biotic and Environmental Changes. by Norman MacLeod and Gerta Keller, W.W Norton Company, New York-London, 139-139-171.
  29. Keller G. (2003)., Guembelitria-dominated late Maastrichtian planktic foraminiferal assemblages mimic early Danian in central Egypt., Marine Micropaleontology, 47(1-2), 71-99.
  30. Abramovich S. and Keller G. (2002)., High stress late Maastrichtian paleoenvironment: inference from planktonic foraminifera in Tunisia., Palaeogeography, Palaeoclimatology, Palaeoecology, 178(3-4), 145-164.
  31. Smit J., Silver L.T.and Schultz P.H. (1982)., Extinction and evolution of planktonic foraminifera after a major impact at the Cretaceous/Tertiary boundary., In Geological implications of impacts of large asteroids and comets on the Earth, Geol. Soc. Am. Spec. Paper, 190, 329-352.
  32. Luterbacher H.P. (1964)., Biostratigrafia del limite cretaceo-terziario nell, Riv. Ital. Paleont., 70, 67-128.
  33. Leonov V.P. and Alimarina G.P. (1961)., Stratigraphy and planktonic foraminifera of the Cretaceous-Paleogene "Transition"., Beds of the central part of the North Caucasus: Collected Papers Geological Faculty, University of Moscow, to XXI International Geological Congress, 29-60.
  34. Bolli H.M. (1966)., Zonation of Cretaceous to Pliocene marine sediments based on planktonic foraminifera., Asoc. Venezolana Geologia, Mineria y Petroleo, Bol. Inf., 9, 3-32.
  35. Molina E., Arenillas I. and Arz J.A. (1996)., The Cretaceous/Tertiary boundary mass extinction in planktic foraminifera at Agost, Spain., Revue de Micropaléontologie, 39(3), 225-243.
  36. Amao A.O., Kaminski M.A., Asgharian Rostami M., Mahmudy Gharaie M.H. and Lak R., Frontalini F. (2018)., Distribution of benthic foraminifera along the Iranian coast., Marine Biodiversity, 1-14.
  37. Asgharian Rostami M., Ghasemi Nejad E., Shafiee Ardestani M. and Balmaki B. (2011)., Biostratigraphy and studying The hypothesis uses of Rugoglobigerina in appointing the paleosalinity in central Alborz, Maastrichtian., Geoscience, 20, 23-32.
  38. Asgharianrostami M., Vahidinia M. and Ghasemi Nejad E. (2012)., Paleoenvironmental reconstruction using benthic foraminiferal assemblages across the Cretaceous/Palaeogene boundary in the Alborz basin, northern Iran., Journal of American Science, 8, 53-55.
  39. Alegret L. and Thomas E. (2009)., Food supply to the seafloor in the Pacific Ocean after the Cretaceous/Paleogene boundary event., Marine Micropaleontology, 73(1), 105-116.
  40. Rodelli D., Jovane L., Özcan E., Giorgioni M., Coccioni R., Frontalini F. and Rostami M.A. (2018)., High-resolution integrated magnetobiostratigraphy of a new middle Eocene section from the Neotethys (Elazığ Basin, eastern Turkey)., GSA Bulletin, 130(1-2), 193-207.
  41. Jorissen F.J., de Stigter H.C. and Widmark J.G. (1995)., A conceptual model explaining benthic foraminiferal microhabitats., Marine micropaleontology, 26(1-4), 3-15.
  42. Bernhard J.M. (1996)., Microaerophilic and facultative anaerobic benthic foraminifera: a review of experimental and ultrastructural evidence., Revue de Paleobiologie, 15, 261-275.
  43. Kaiho K. (1999)., Effect of organic carbon flux and dissolved oxygen on the benthic foraminiferal oxygen index (BFOI)., Marine Micropaleontology, 37, 67-76.
  44. Rodelli D., Jovane L., Özcan E., Giorgioni M., Coioni R., Frontalini F., Rego E.S., Brogi A., Catanzariti R., Less Gy. and Rostami M.A. (2018)., High-resolution integrated magnetobiostratigraphy of a new middle Eocene section from the Neo-Tethys (Elazığ Basin, eastern Turkey)., Geological Society of America Bulletin, 130(1-2), 193-207.
  45. Asgharian Rostami M. and Balmaki B. (2018)., Biostratigraphy and Paleoecology of Maastrichtian and Paleocene Sediments in the Northern Alborz, Iran, Using Foraminifera., International Journal of Geography and Geology, 7(3), 56-72.
  46. Font E., Adatte T., Asgharian Rostami M., Leckie M., Frontalini F. and Thibault N. (2018)., Environmental acidification triggered by Deccan volcanism at the KPg Galanderud section, Iran., European Geosciences Union General Assembly, 20.
  47. Martin E.E., Rostami M.A., MacLeod K.G., Haynes S., Poulsen C.J. and Vande Guchte A. (2017)., Deep-water formation in the North Atlantic during the latest Cretaceous., In AGU Fall Meeting Abstracts., PP14A-02.
  48. Asgharian Rostami M., Martin E., Macleod K., Poulsen C., Haynes S., Vande guchte A. and Haynes S. (2017)., Gateways and water mass mixing in the late Cretaceous North Atlantic., American Geophysical Union, Fall Meeting, PP23A-1288.
  49. Balmaki B., Asgharian Rostami M., Vahidinia M. and Mohamadi M. (2012)., Paleogeography Study of Seymare member, Gurpi Formation, based on determining systematic of Echinoids and Foraminifera at Mish-khas section, South east of Illam province., Sedimentary Facies, 3(2), 19-30.
  50. Rostami M.A., Balmaki B., Ardestani M.S. and Kohansal E. (2009)., Biostratigraphy and assigning the paleosalinity by using Echinocorys and Planktonic foraminifera at Upper Maastrichtian, in Jorband section, Central Alborz, Iran., Nature Publishing, 713, 1-7.
  51. Asgharian Rostami M., Ghasemi-Nejad E. and Shafiee ardestani M. (2011)., Palaeobathymetry of the Ziarat-kola section at the upper Maastrichtian, Central Alborz, through planktonic and benthic foraminifera., Geosciences, Geological survey of Iran, 20(78), 27-34.
  52. Raquel B., Leckie R.M., Khalifa M.E., Martin E.E. and Asgharian Rostami M. (2016)., Paleoceanographic implications of rising sea level in the Western Interior Seaway though the Cenomanian-Turonian boundary interval., Geological Society of America, Denver, Abstracts with Programs, 48(7).
  53. Asgharian Rostami M., Leckie R.M., Font E., Finkelstein D. and Koeberl C. (2014)., Foraminiferal turnover and paleoenvironmental changes across an expanded Cretaceous/Paleogene boundary section, northern Alborz, Iran., Geological Society of America, Vancouver, British Columbia, Abstracts with Programs, No. 200-2.
  54. Asgharian Rostami M., Balmaki B. and Wigand P.E. (2013)., Foraminiferal biostratigraphy and paleoecology of the Maastrichtian through Danian Sediments of the Ziarat-Kola Section, Central Alborz Mountains, Iran., Geological Society of America, Denver, Abstracts with Programs, 45(7), 330.
  55. Asgharian Rostami M., Martin E.E., Kenneth G.M. and Shannon H. (2016)., Changes in intermediate water sources during the early Maastrichtian cooling event: Evidence from Nd isotopes and foraminifera assemblages., Geological Society of America, Colorado, Abstracts with Programs, 48(7).
  56. Raquel B., Leckie R.M., Khalifa M.E., Martin E.E. and Asgharian Rostami M. (2016)., Paleoceanographic implications of rising sea level in the Western Interior Seaway though the Cenomanian-Turonian boundary interval., Geological Society of America,Colorado, Abstracts with Programs, 48(7).