| Peer-Reviewed

Biometric Analysis of Lepidocyclina (Nephrolepidina) from Baba Formation (Late Oligocene) in Bai-Hassan Well-25, Kirkuk Area, Northeast Iraq

Received: 25 September 2014     Accepted: 7 October 2014     Published: 20 October 2014
Views:       Downloads:
Abstract

The investigation is based on a subsurface sequences of bioclastic limestone in Kirkuk area, Northeastern Iraq. These sequences were deposited in a shallow open marine environment during Late Oligocene. Tests of larger foraminifera Lepidocyclina(Nephrolepidina) are abundant in the lower and upper parts of the Baba Formation. Biometric investigations of the Megalospheric forms of Nephrolepidina assemblages from, Bai-Hassan well- 25 section led to recognize three morphometrically defined species by the combination of three parameters, 1- the degree of embracement of the protoconch by the deuteroconch (Factor A), 2- the numbers of accessory auxiliary chambers on the deuteroconch (Factor B), and 3- (Factor C ) which expressed by the protoconch angle( ) formed by the two hypothetical line from the center of protoconch throught the outer attachment points of the deuteroconch walls with protoconch.

Published in Science Research (Volume 2, Issue 5)
DOI 10.11648/j.sr.20140205.16
Page(s) 111-118
Creative Commons

This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.

Copyright

Copyright © The Author(s), 2014. Published by Science Publishing Group

Keywords

Late Oligocene, Kirkuk Area, Northeast Iraq, Bai-Hassan Well-25, Biometric Analysis

References
[1] Abid, A, A.(1997). Biostratigraphy and Microfacies of the Late Oligocene-Miocene formations center and north Iraq. (Unpublished) Ph.D. Thesis, Coll. Of Sci. Baghdad Univ., 258p. (In Arabic)
[2] Adams, C. G. (1987). On the classification of the Lepidocyclinidae (Foraminifera) with re-description of the unrelated Paleocene genera Actinosiphon and Orbitosiphon. Micropaleontology, vol. 33, no.4, pp.289-317, pls. 1-4.
[3] Al-Guburi, H. M. Q; and El-Esa, R. M. (2002). The stratigraphy and depositional environment of Paleogene –Lower Neogene subsurface sequence in the area between Bai-Hassan and Al-Qayarah oil fields. 5th Iraqi Geological Congress, Baghdad.
[4] Al-Hashimi, H. A. J.; and Amer, R.M. (1985) . Tertiary Microfacies of Iraq. D.G. geol. Surv. Min. Invest. Puli., Baghdad, 56pp, 17figs., 159pls. (S.O.M.).
[5] Cole, W. S., (1938): Stratigraphy and Micropaleontology of two deep wells in Florida. Florida Geol. Surv., Bull., vol. 16, pp. 1-73.
[6] De Mulder, E. F. J. (1975). Microphona and sedimentary tectonic history of the Oligo- Miocene of the Joniane Islamnd and Western Europe (Greece). Ulrecht. Micropal. Bull., vol. 13, 140.pp.
[7] Douvillé, H. . (1898). Sur I’age des couches traverse/es par le canal du Panama . Soc. Ge/ol. France, Bull.; vol.3, 26, pp. 587-600.
[8] Drooger, C. W. (1952). Study of American Miogypsinidae. Thesis Univ.Utrecht, p. 1-80.
[9] Drooger, C. W. (1993). Radial Foraminifera Morphometrics and Evolution, verhamd, Kon. Ned. Akad. Wetensch. Amesterdam, pp. 1-241.
[10] Drooger, C. W. and Freudenthal, Th. (1964). Associations of Miogypsina and Lepidocyclina at some European localities. Ecl. Geol. Helv.; vol. 57; pp. 509- 528.
[11] Drooger, C. W.; and Laagland, H.,M (1986). Larger Foraminiferal zonation of the Europian-Mediteeriane Oligocene. Proc. Kon. Ned. Akad. Wet., ser. B, vol. 189, pp. 135-148.
[12] Drooger, C. W.; and Rohling E. j. (1988). Lepidocylina migration across the Atlantic, Jou. of Paleontology , Procceedings loninklijike Nederlandse Academie van wetenschappen, (B), vol. 91: pp. 39-52.
[13] El-Eisa, M. E. S. (1992). Coral reef of Late Oligocene-early Miocene, Kirkuk and surrounding area. Iraqi. Geol. Jour. vol.(25), no. 2, Issued, pp. 17-32. (In Arabic)
[14] Freudenthal, Th. (1966). Nephrolepidina at some classical European localities. Proc. 3rd. Sess. Comm. Med. Neog. Strat., Berne 1964, pp.55-57. Brill, Leiden.
[15] Geerates, W., (1983). Biometrical analysis of early middle Oligocene Nephrolepidina praemarginata and Heterostegina sp. Associations from Villajoyosa, SE.Spain Intern. Rep. dept. stratigraphy state Univ. Utrecht. 91 pages.
[16] Hadad, N. H. (1991). Biostratigrapgic studies for the Tertiary Formations in some
[17] oilfields, in the area of N.O.C. Kirkuk Office, unpublished (In Arabic).
[18] Mohammed, Q. A. (1983). Biostratigraphy of Kirkuk Group in Kirkuk and Bai-Hassan areas, Unpublish. M.Sc. Thesis, coll. Sci. Univ. of Baghdad.
[19] Mulenkamp, J. E.; and Amato, V. (1972). Cycloclypeus and Nephrolepidina from the Oligocene of mollero (N. Italy). Id., (B); 75, pp. 34-47
[20] Muthukrishnan, S.; and Saraswati, P. K. (2001). Shape analysis of the nucleoconch of Lepidocyclina from Kutch-ataxonomic interpretation. Micropaleontology, vol. (47), no. 1, pp. 87-92, text figures, 1-33, plates 1.
[21] Saraswati, P. K. (1995)’ Biometry of early Oligocene Lepidocyclina from Kutch, India. Marine Micropal. vol. (20), pp. 303-311.
[22] Saraswati, P. K.; and Kumar, A. (2000). Morphometrics of some Lepidocyclina Foraminifera: applications in Taxonomy and Biostratigraphy. Geological data analysis: statistical methods. Hindistan publishing corporation (India) New Delhi. pp. 63-70, Figs. 6.
[23] Tan Sin Hok. (1936a).Zur Kenntnis der Miogypsiniden. De Ingenieur in Ned. Indië, Jaarg. 3, no. 3, pp. 45-61. no.5, pp. 84-98, no. 7, pp. 109-123.
[24] Vlerk, Van der I.M, (1929).Groote Foraminiferen van Noord-Oost borneo. Id., vol. (9), p. 5-44.
[25] Van Der Vlerk, I.M, (1957). Des Stratigrafische betekensis van het “genus Lepidocyclina”. Proc. Kon. Ned. Akad. Wet., (B); vol. (66), pp. 23-27.
[26] Vlerk , Van der I.M, (1959a). Modification de I’ontogénése pendant I’évolution des Lépedocyclines (Foraminifers). Soc. Géol. France, bull. (7); vol. (1), p. 669-673.
[27] Vlerk, Van der I.M, (1959b). Problems and principles of Tertiary and Quaternary stratigraphy. Geol. London, Quart. Journ:., 115, pp. 49-63.
[28] Vlerk, Van der I.M, (1963).Biometrical research on Lepidocyclina. Micropal. vol. (9), pp. 425-426.
[29] Vlerk, Van der I.M, (1974). Nomenclatural and numerical taxonomy (names and numbers). Verhandi. Naturf. Ges. Basel; vol. (84), pp. 245-255.
Cite This Article
  • APA Style

    Imad Mahmood Ghafor. (2014). Biometric Analysis of Lepidocyclina (Nephrolepidina) from Baba Formation (Late Oligocene) in Bai-Hassan Well-25, Kirkuk Area, Northeast Iraq. Science Research, 2(5), 111-118. https://doi.org/10.11648/j.sr.20140205.16

    Copy | Download

    ACS Style

    Imad Mahmood Ghafor. Biometric Analysis of Lepidocyclina (Nephrolepidina) from Baba Formation (Late Oligocene) in Bai-Hassan Well-25, Kirkuk Area, Northeast Iraq. Sci. Res. 2014, 2(5), 111-118. doi: 10.11648/j.sr.20140205.16

    Copy | Download

    AMA Style

    Imad Mahmood Ghafor. Biometric Analysis of Lepidocyclina (Nephrolepidina) from Baba Formation (Late Oligocene) in Bai-Hassan Well-25, Kirkuk Area, Northeast Iraq. Sci Res. 2014;2(5):111-118. doi: 10.11648/j.sr.20140205.16

    Copy | Download

  • @article{10.11648/j.sr.20140205.16,
      author = {Imad Mahmood Ghafor},
      title = {Biometric Analysis of Lepidocyclina (Nephrolepidina) from Baba Formation (Late Oligocene) in Bai-Hassan Well-25, Kirkuk Area, Northeast Iraq},
      journal = {Science Research},
      volume = {2},
      number = {5},
      pages = {111-118},
      doi = {10.11648/j.sr.20140205.16},
      url = {https://doi.org/10.11648/j.sr.20140205.16},
      eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.sr.20140205.16},
      abstract = {The investigation is based on a subsurface sequences of bioclastic limestone in Kirkuk area, Northeastern Iraq. These sequences were deposited in a shallow open marine environment during Late Oligocene. Tests of larger foraminifera Lepidocyclina(Nephrolepidina) are abundant in the lower and upper parts of the Baba Formation. Biometric investigations of the Megalospheric forms of Nephrolepidina assemblages from, Bai-Hassan well- 25 section led to recognize three morphometrically defined species by the combination of three parameters, 1- the degree of embracement of the protoconch by the deuteroconch (Factor A), 2- the numbers of accessory auxiliary chambers on the deuteroconch (Factor B), and 3- (Factor C ) which expressed by the protoconch angle( ) formed by the two hypothetical line from the center of protoconch throught the outer attachment points of the deuteroconch walls with protoconch.},
     year = {2014}
    }
    

    Copy | Download

  • TY  - JOUR
    T1  - Biometric Analysis of Lepidocyclina (Nephrolepidina) from Baba Formation (Late Oligocene) in Bai-Hassan Well-25, Kirkuk Area, Northeast Iraq
    AU  - Imad Mahmood Ghafor
    Y1  - 2014/10/20
    PY  - 2014
    N1  - https://doi.org/10.11648/j.sr.20140205.16
    DO  - 10.11648/j.sr.20140205.16
    T2  - Science Research
    JF  - Science Research
    JO  - Science Research
    SP  - 111
    EP  - 118
    PB  - Science Publishing Group
    SN  - 2329-0927
    UR  - https://doi.org/10.11648/j.sr.20140205.16
    AB  - The investigation is based on a subsurface sequences of bioclastic limestone in Kirkuk area, Northeastern Iraq. These sequences were deposited in a shallow open marine environment during Late Oligocene. Tests of larger foraminifera Lepidocyclina(Nephrolepidina) are abundant in the lower and upper parts of the Baba Formation. Biometric investigations of the Megalospheric forms of Nephrolepidina assemblages from, Bai-Hassan well- 25 section led to recognize three morphometrically defined species by the combination of three parameters, 1- the degree of embracement of the protoconch by the deuteroconch (Factor A), 2- the numbers of accessory auxiliary chambers on the deuteroconch (Factor B), and 3- (Factor C ) which expressed by the protoconch angle( ) formed by the two hypothetical line from the center of protoconch throught the outer attachment points of the deuteroconch walls with protoconch.
    VL  - 2
    IS  - 5
    ER  - 

    Copy | Download

Author Information
  • Department of Geology School of Science, Faculty of Science and Scientific Education, Sulaimani University—Iraqi Kurdistan Region.

  • Sections