Printer Friendly

EARLY TRIASSIC AZONATE TRILETE SPORES FROM MIANWALI FORMATION, WESTERN SALT RANGE, PAKISTAN.

Byline: Tahira malik, Farhat masood and M. Zia ul rehman

ABSTRACT

Mianwali Formation represents the Early Triassic strata of the Salt Range, Pakistan that is underlained by Chhidru Formation (Late Permian) and overlained by Tredian Formation (Middle Triassic). The Mianwali Formation has three members in ascending order viz., Katwai, Mittiwali and Narmia member. It is predominantly composed of black shales along with the dolomite, limestone, sandstone and sandy shales. A diverse palynoassemblage was recovered from some sandstones of Mianwali Formation at the Nammal Gorge Section. The detailed palynoflora recovered from Mianwali Formation cannot be covered in a single paper, therefore the present paper deals exclusively with the azonate trilete spores viz; Calamospora mutabilis, Pachytriletes densus, Granulatisporites minutes, Cyclogranisporites aeureus and Punctatisporites gratensis.

INTRODUCTION

Mianwali Formation represents the lower most Triassic strata of the Salt Range, Pakistan. Lithologically it represents varied composition having coarse and fine grained sandstones, limestone, dolomite and compact, splintery and fissile shales [1,2]. Mianwali Formation overlies the Chhidru Formation of late Permian age, though a paraconformity is indicated on palaeontological and palynological grounds [3]. It is overlained by Tredian Formation of Late Triassic age in the Salt Range and by Chak Jabbi Limestone in the Kalachitta Range [4]. Mianwali Formation has been divided into three members in ascending order i.e., Katwai, Mittiwali and Narmia members, respectively [5]. Rock samples for the present investigation were collected from Nammal Gorge Section (Long 71 47' 50 Lat 32 39' 27) located 25 km east of Mianwali city on Musakhel Mianwali road.

Here the Mianwali Formation is approximately 107 m thick (The section was measured accurately in accordance with the internationally recommended procedures [6]) All the members are well exposed. Limited Published literature is available on palynology of the Early Triassic Sediments Salt Range, Pakistan. The most significant and outstanding work was done by Balme[7]. Some later contributions include Masood et al.[8] and Masood [9].

MATERIALS AND METHODS

Rock samples were processed in accordance with the scheme as suggested by[10,11]. Bulk maceration was employed by overnight treatment of samples (50 g) by analar grades of 50 % HCl, HF and HNO3 followed by neutralizations of acids through several decantations with distilled water. This was followed by 1% KOH treatment and subsequent neutralization. Strew mount permanent slides were prepared in Canada Balsam. Photographs were made under oil immersion X60, X40 objectives on Kodak 100 ASA panchromatic film.

Relative frequencies of various species were expressed as follows:- Abundant above 25% , Dominant above 15% but less than 25%, Frequent above 10% but less than 15%, Rare above 5% but less than 10% and Very rare less than 5% . Furthermore sample code was employed in the following manner:-

NGK Nammal Gorge Katwai, NGM Nammal Gorge Mittiwali and NGN Nammal Gorge Narmia. While the numbers 1, 2, 3 etc. represent the sample numbers oblique slide no.

The dimensions are based on specimens preserved in polar view, the values given on right side represent the maximum diameter, the values on the left side represent the minimum diameter while the values in the parenthesis represent the average diameter.

RESULTS AND DISCUSSION

Most samples contained identifiable and well prererved spores. Spores varied in color from dark yellow to reddish brown in color, polar and off polar compressions were the most common type of preservation. Palynomorphs are infact sporopollenin bearing acid resistant microfossils [12] which are well preserved in a number of depositional environments like sandstone, shales, mudstones [13]etc.

Pl.1 Fig. 1

Occurrence: Nammal Gorge: Mittiwali member abundant to common,

Dimensions: (45 Specimens) Equatorial diameter 28(32) 45m.

Description: Miospore, trilete, amb originally circular to sub circular, distorted due to compressional folds, imparting typical oval or arcuate appearance to the spore, lete distinct, labra sharply developed, raised straight to sinuous, arms of leasurae never extending 1/4 spore radius, a large biconvex compressional fold, intersect rest of the folds at right angle, exine infragranulate 1 m thick.

Remarks: The spore apparently confirm more closely to the spores description by Potonie and Kremp [14] than that of Smith and Butterworth [15]

Collection: NGM-94/6, NGM-106/3

Possible affinities: Pteridophytic (Calamitales).

Calamospora mutabilis (Loose) Schopf, Wilson and Bentall.

Pachytriletes densus Bose and Kar, 1966

Pl. 1 Fig 2,3

Occurrence: Nammal Gorge: Mittiwali member common to frequent

Dimensions: (54 Specimens) Equatorial diameter 36(41) 62m.

Description: Miospore, trilete, amb triangular, lete distinct, raised, arms of lete extending up to angles, labra distinct, massive, raised, exine up to 2 m thick, infra punctate, exhibiting occasional folding along the margin of the contact area, exoexinal layer generally present

Remarks: Pachytriletes densus was confined to Mittiwali member of the Mianiwali Formation.

Collection: NGM-94/8, NGM-92/1

Possible affinities: Pteridophytic (Filicinean).

Granulatisporites minutus Utting, 1994

Pl.1 Fig.4

Occurrence: Nammal Gorge: Mittiwali member common to rare, Narmia member very rare.

Dimensions: (14 Specimens) Equatorial diameter 21(25) 32m.

Description: Miospore, trilete, amb triangular, angles rounded, sides straight to partially concave, trilete distinct, flat, arms of lete extending up to angles, labra poorly developed, commissure smooth, contact area masked by dark exinal band within the vaccinity of Y'' marking, exine infra granulate, grana less than 1m in diameter appearing flat or rounded, visible only upon careful L-O analysis.

Remarks: Granulate nature of exine is not discernible in the microphotograph provided; however it is only detectable under oil immersion objective upon careful L O analysis.

Collection: NGM-31/13

Possible affinities: Pteridophytic (Filicinean).

Cyclogranisporites aureus (Loose) Potonie and Kremp, 1955

Pl.1 Fig. 5

Occurrence: Nammal Gorge: Katwai member very rare, Mittiwali member common, Narmia member abundant. Dimensions: (31 Specimens) Equatorial diameter 23(31) 42m.

Description: Miospore, trilete, amb circular to sub circular but never sub triangular,,lete distinct, slightly raised, arms of lete never extending more than half or 3/4 radius, labra distinct raised, sinuous, masking lete completely, exine 1.5m thick, intragranulate, grana conical to rounded.

Remarks: This taxon is same as described and illustrated by Bharadwaj [16]

Collection: NGM-94/1, NGN-113/2, NGM-39/9, 46/3-S1

Possible affinities: Pteridophytic ( Filicinean).

Cyclogranisporites minutus Bharadwaj, 1957

Pl. 1 Fig. 6.

Occurance: Nammal Gorge: Katwai member very rare, Mittiwali member rare, Narmia member very rare. Dimensions: (19 Specimens) Equatorial diameter 29(35) 40 m.

Description: Miospore, trilete, amb characteristically circular, lete distinct, arms of lete approximately half radius, labra absent, commissure smooth, contact area indistinct, exine up to 1.5 m, intragranulate, grana dense, rounded to conical in outline, exine may exhibit some secondary foldings often in specimens preserved in polar view.

Remarks: Despite rough and rugose exine of the proximal hemisphere and clearly defined lete which are strong taxonomic armors to warrant institutions of a new species, I however preferred maintaining it as Cyclogranisporites minutus as such minor variations in exinal ornamentation are sometimes induced by differential compression during fossilization.

Collection: NGM-44/1, 46/7-S1, 90/2, 34/5

Possible affinities: Pteridophytic (Filicinean).

Punctatisporites gratensis Balme and Henelly, 1956

Pl.1 Fig. 6

Occurrence: Except Katwai member, this taxon was common to frequent in all the members of the Mianwali Formation.

Dimension: (41 Specimens) Equatorial diameter 29(36) 52m.

Description: Miospore, trilete, amb circular to subcircular, lete distinct, arms of lete never extending 3/4 spore radius, labra well developed, raised, translucent uniform up to 4 m broad, 2 m high, contact area indistinct in few specimens may be masked by dark uniform exinal folds parallel to lete, exine up to 1 m thick, infra punctate to intra punctate, punctae more pronounced and dominant around Y'' marking and equator, compressional folds common usually confined to the distal hemisphere.

Remarks: It compares well with an identical taxon described by Maheshwari and Bose [17] from the Kibama River (Lukuga coalfield area). It also compares closely with Punctatisporites obesur [14] except for the low ridges and verrucae on the distal surface of the former.

Collection: NGM-40/6, 34/7,106/3, NGN-113/2

Possible affinities: Pteridophytic (Filicinean).

Early Triassic period was constituted by many plant groups , ferns being the most important and the most dominating group as shown by the well preserved and highly preserved azonate trilete spores. These azonate triletes were with varied morphologies, with distinct lete, and with

smooth, infrapunctate, infra or intraranulte exine showing great variations even with in a single plant group.

REFERENCES

[1]Waagen, W., (1879). Salt Range fossils. I Productus Limestone fossils. Pisces- cephalopodia., Geol. Surv. India, Palaeont. Indica, Ser., 13,1, pt. 1, 1-72.

[2]Waagen, W., (1895). Salt Range Fossils; fossils from the Creatite formation; Pisces- Ammonoidea., India Geol. Surv. Mem., Palaeont. Indica, Ser., 13(2): 1-324.

[3]Kummel, B. (1970). Stratigraphy and Paleontology of the Permian-Triassic Boundary Beds, Salt Range and Trans-Indus Ranges, West Pakistan: in Stratigraphic Boundary Problems: Permian and Triassic of West Pakistan. Univ. Kansas, Geol. Deptt. Sp. Pub., 4: 1-110.

[4]Fatimi, A, N. (1972). Stratigraphy of the Jurassic and Lower Cretaceous rocks and Jurassic ammonites from Northern areas of west Pakistan. Bull. British Mus. (Nat.His) Geology, London ., 20(7).

[5]Kummel, B. (1966). The Lower Triassic Formations of the Salt Range and Trans-Indus ranges, West Pakistan. Mus. Comp. Zoology, Bull., 134(19): 361-429.

[6]Masood, K.R., Qureshi, K.A., Iqbal, J. and Hussain, Z. (1992). Auriculate Miospores from Early Jurassic sediments (Datta Formation), Western Salt Range, Pakistan. Pak. J. Geol., 1(1): 52-58.

[7]Balme, B.E. (1970). Palynology of Permian and Triassic strata in the Salt Range and surghar Range, West Pakistan. Stratigraphic boundary problems: Permian and Triassic of West Pakistan. Special Pub., 4: 306-453.

[8]Masood, K.R., Qureshi, K.A., Sabri, S.N. and Hussain, Z. (1991). Middle Triassic Flora and Climatic changes in the Western Salt Range, Pakistan, based on Palynological data. Acta Scientia, 1(2): 79-84.

[9]Masoodi, K.R. (1992). Middle Triassic (Anisian) Megaspore from Western Salt Range, Pakistan. Pak. J. Geol., 1(1): 66-71.

[10]Phipps, D. and Playford., (1984). Laboratory Techniques for Extraction of Palynomorphs from Sediments. Pub Dept. Geol. Univ. Queensland., 11(1): 1-33.

[11]Dohar, L.I. (1980). Palynomorph preparation procedure currently used in Palaeotol and stratigraphy laboratories. U. S. Geol. Surv. U.S.G.S Pub. 830: 1-29.

[12]Traverse, A. (1988). Palaeopalynology, Unwin HymanLondon, Sydney, Wellinton. 559p.

[13]Masood, K.R., Khalid, A. N., Qureshi, K.A., Hussain, Z.( 1995). Further observations on Fossil Fungi (VA Mycorrhizae) from the Permian of Salt Range, Pakistan. Pak. J. Geol., 3(2): 7-10.

[14]Potonie, R. and Kremp, G.O.W. (1955). Die Sporae disperse des Ruhukarbons, ihre Morphographie und Stratigraphie mit Ausblicken auf Arten anderer Gebiete und Zeitabschnitte, Teil I. Palaeontographica., Abt. B, Bd., 98: 136.

[15]Smith, A.H.V. and Butterworth, M.A. (1967). Miospores in the coal seams of the Carboniferous of Great Britain. Special Papers in Palaeotol, no. 1. the Palaeontological Assoc., 324 p.

[16]Bharadwaj, D.C. (1957a). The Palynological investigations of the Saar coals (part 1-Morphography of Sporae dispersae). Palaeontogra., Abt. B, Bd., 101: 73-125.

[17]Maheshwari, H.K. and Bose, M.N. (1969). Palaeozoic Sporae dispersae from Congo, the Kibama River (Lukuga coalfield area). Musee Royal De L'afrique centrale-Tervuren, Belgique Annales, Serie 1N-8o Sciences geologiques-no 63: 3-61.
COPYRIGHT 2015 Asianet-Pakistan
No portion of this article can be reproduced without the express written permission from the copyright holder.
Copyright 2015 Gale, Cengage Learning. All rights reserved.

Article Details
Printer friendly Cite/link Email Feedback
Publication:Science International
Article Type:Report
Date:Aug 31, 2015
Words:1847
Previous Article:USE OF OPTIMAL HOMOTOPY ASYMPTOTIC METHOD FOR FRACTIONAL ORDER NONLINEAR FREDHOLM INTEGRO-DIFFERENTIAL EQUATIONS.
Next Article:TRAINING EVALUATION PRACTICES AMONG CALL CENTERS BASED ON TWO CULTURE-FREE CHARACTERISTICS: OWNERSHIP AND FIRM SIZE.
Topics:

Terms of use | Privacy policy | Copyright © 2019 Farlex, Inc. | Feedback | For webmasters