Abstract
In the Eocene of Pakistan, India and Burma, two genera—Miscellanea and Pellatispira—have shown a remarkably stable and limited vertical range in the several areas in which representatives of these genera are found. Miscellanea, which is represented byM. miscella (d’Archiac and Haime),M. stampi (Davies), andM. meandrina (Carter), is confined to the Ranikot (Palæocene age) in all the areas examined so far, while Pellatispira, which is represented byP. cf. orbitoidea (Provale),P. cf. inflata Umbgrove,P. cf. madaraszi Von Hantken,P. cf. glabra Umbgrove, is found only in the very high Eocene (Upper Eocene) beds. Because of their very restricted vertical range these two genera are of considerable stratigraphic value.
Similar content being viewed by others
Bibliography
Carter, H. J. “Further Observations on the structure of Foraminifera,”Ann. Mag. Nat. Hist., 1861, Ser. 3,8.
Cotter, G. de P. “Pegu-Eocene Succession in Minbu,”Rec. Geol. Surv. Ind., 1912,41, 235.
— “Nummulites as Zone Fossils,” —, 1914,44, 53.
- “Age of the so-called Danian Fauna from Tibet,”ibid., 1926,59.
Davies, A. M.Tertiary Faunas, 1934, 1935, Vols. 1 and 2.
Davies, L. M. “Ranikot Beds of Thal,”Q. J. G. S., 1927,83.
- “Fossil Fauna of the Samana Range,”Pal. Ind., N.S., 1930.15 (1 and 6).
- “The Eocene of the Punjab Salt Range,”ibid., N.S., 1937.24 (1), Part 2.
Douville, H. “Le Crètacè et l’Eocène du Tibet Central,”ibid., N.S., 1916,5 (3).
Ellis and MassinaCatalogue of Foraminifera.
Evans, P. “Tertiary Succession in Assam,”Trans. Min. Geol. Inst. India, 1932,27 (3).
Furon RaymondGeologie de L’Inde Orientale Francaise, Pub. Bureau d’Etudes Geol. et Min. Coloniales, 1941, No. 17.
Glaessner, M. F. “Problems of Stratigraphic Correlation in the Indo-Pacific region,”Proc. Roy. Soc. Vic., N.S. 1943,55, Part 1.
Hoffmeister, J. E. “Geology of Eua, Tonga,”Bernice P. Bishop Mus. Bull. Honolulu, Hawaii, 1932, No. 96.
Narayana Rao, S. R. “Tertiary Sequence near Surat and Broach,”Jour. Mys. Uni., Sec. B, 1941,2 (2).
Nuttall, W. L. F. “The Laki Series of Sind and Baluchistan,”Q.J.G.S., 1925,81 (3).
- “The Larger Foraminifera of U. Ranikot, Sind,”Geol. Mag. 1926,63.
- “The Stratigraphy of the U. Ranikot of Sind,”Rec. Geol. Surv. Ind., 1931,65 (2).
— and Brighton, A. G. “Larger Foraminifera from the Tertiary of Somaliland,”Geol. Mag., 1931,68, 60.
Pfender, J.Bull. Soc. Geol. Fr., Ser. 5, 1936,6, p. 308.
Rama Rao, L. “On the Occurrence of an Eocene bed in the Pondicherry Cretaceous area, S. India,”Current Science, 1939,8, No. 4.
- “OnNummulites cf. thalicus Davies from the Eocene bed in the Pondicherry area, S. India,”ibid., 1940,9.
- “Recent Advances in our knowledge of the Upper Cretaceous and Lower Eocene beds of India with special reference to the Cretaceous-Eocene boundary,”Presidential Address, Geol. Sec., 27th Ind. Sci. Congress, 1940.
Shimer, H. W. and Shrock, R. R.Index Fossils of North America, 1947.
Umbgrove, J. H. F. “Het genus Pellatispira in het Indo-Pacifische gebied,”Weten. Med., 1928, No. 10.
— “Feestbudel Prof. K. Martin,”Leidische geol. Med., 1931,5, p. 53.
Vaughan, T. W. “American Palæocene and Eocene larger Foraminifera,”Geol. Soc. Amr. Mem., 1945,9, p. 23.
Vredenburg, E. “Note on the Stratigraphy of the Ranikot Series,”Pal. Ind., N.S. 1909,3, (1).
Author information
Authors and Affiliations
Additional information
Communicated by Prof. L. Rama Rao
Paper read at the 37th Indian Science Congress (Geology Section), Poona, January 1950. Published with the kind permission of The Burmah Oil Co. (India Concessions) Ltd.
Rights and permissions
About this article
Cite this article
Nagappa, Y. The stratigraphical value of Miscellanea and Pellatispira in India, Pakistan and Burma. Proc. Indian Acad. Sci. 33, 41–48 (1951). https://doi.org/10.1007/BF03049974
Received:
Issue Date:
DOI: https://doi.org/10.1007/BF03049974