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Byline: Muhammad Zia Ul Rehman, Farhat Masood AND Tahira Malik


The type section of Chhidru Formation (Chhidru Gorge) was selected for present study. A very diverse palynoflora was recovered. Present paper deals with only few bisaccate pollen viz Protohaploxipinus goraiensis, Protohaploxypinus varius, Protohaploxypinus limpidus, Protohaploxypinus amplus, Protohaploxypinus microcorpus, Striatopodocarpites raniganjensis, Striatopodocarpites cancellatus, Stroiatopodocarpites rarus, Striatopodocarpites pantii, Striatoabieites elongatus, Striatoabieites multistriatus, Striatoabieites striatus, Lunatisporites novialensis, Lunatisporites pellucidus, Guttulapollenites hannonicus and Hamiapollenites bullaeformis. These palynomorphs were thoroughly explained and their affinities were also carefully worked out and were tentatively linked with gymnosperms.

Keywords: Bisaccate pollen, Chhidru formation, salt range, palynomorphs

Running Title: Bisaccate Pollen From Chhidru Formation


The Chhidru Formation, Western Salt Range, Pakistan represents not only the termination of late Permian period, but also the end of Paleozoic era. This part of the salt range owes its existence because of the Himalayan collision [1]. Chhidru Formation is present in both Trans Indus and Cis Indus regions[2]. Salt Range is full of evidence reflecting part of geological and biological events and represents one of the best section to study such events. Lot of work has been done all over the world on the rocks of Permian age [3, 4, 5, 6, 7, 8, 9, 10]. Recently, based on the Palynological evidence, the Gondwana Carboniferous- Permian of Nilawahan Group of the Salt Range, Pakistan have been correlated with middle to upper part of Al Khalata Formation of Oman and Unayzah B Member of Saudia Arabia [11]. The Present study deals with the palynogical survey including identification and description of Palynomorphs from the Chhidru Formation, present at top most of the Zaluch Group (Late Permian).


Rock samples from Chhidru Formation, Chhidru gorge, (32o 32' 36" N, 71o 46' 25"E), Western Salt Range Pakistan were collected and processed according to the standard processing techniques [12, 13]. Different grades of HCl and HF (20 %50% each) were used for the removal of carbonate and silicates after physical disaggregation (compact samples only). Pyrites and organic matter was loosened using 20% HNO3. Ultimately, palynomorphs were oxidized by 2% KOH and separated on density gradient basis by employing heavy liquid separation [14]. All the spores/pollen were photographed and their dimensions were measured. Canada Balsam was used as the mounting medium. Coordinates of each slide were noted and slides were cataloged in the micro Palaeontology laboratory, Department of Botany, university of the Punjab, Lahore, Pakistan.


The pollen recovered during present work were described in alphabetic order and their affinities were suggested according to Looy et al.., [15] which showed that these palynomorphs represent gymnosperms.


Type Species: Guttulapollenites hannonicus Goubin, 1965 G. hannonicus Goubin, 1965

This taxon occurs in abundance in the upper Permian of Madagascar [16]. Balme [10] also isolated such pollen from Amb, Wargal and Chhidru Formations of the Permian age and early Triassic strata (Mianwali Formation) Salt Range, Pakistan. Guttulapollenites hannonicus has been reported by Hart [17]from the upper Permian South Africa

Genus: HAMIAPOLLENITES Wilson emend. Tschudy and Kosanke, 1966

Type species: Hamiapollenites saccatus Wilson, 1962 H. bullaeformis (Samoilovich) Jansonius ,1962 Balme [10] recovered Hamiapollenites insolitus from the Amb Formation (Salt Range). The present sporomorph however differs significantly from Hamiapollenites insulatus in having much broader and rounded corpus and small less distally inclined sacci. This is the first record of this genus from the Chhidru Formation Genus LUNATISPORITES (Leschik) Klaus, 1963

Type Species: Lunatisporites acutus Leschik, 1956 L. novialensis (Leschik) Foster, 1974

Although Lunatisporites novialensis was quiet abundant to common in the Chhidru Formation, very few complete specimens were available for detailed morphographic comparison. Even in moderately preserved specimens the taenae were partly or totally corroded and could only be identified by their faint outline detectable only undr oil immersion objective.

L. pellucidus (Goubin) Balme,1970

Pollen of this type had always been a characteristic component of early and middle Triassic sediments in most Gondwanaland countries [10, 18, 19, 20]. Perhaps it is the first report of this taxon from Permian of Pakistan

Genus: PROTOHAPLOXYPINUS Samoilovich, 1953

Type species: Protohaploxypinus latissimus (Lubur) Samoilovich, 1953

P. amplus Balme and Hennelly, 1955

Early Permian (Artinskian) sediments of Australia are also rich in Protohaploxypinus amplus [21].

P. goraiensis PAltonie and Lele(1961)

One of the main synthetic features of Protohaploxypinus goraiensis as mentioned by PAltonie and Lele [22] is the narrow cappula and poorly defined corpus [10]. Hart [17] while recombining the species restructured it to forms with 7-8 taenae. The Chhidru sporomorph seems more close to the Hart's interpretation than that of PAltonie and Lele [22].

P. limpidus Balme and Hennelly, 1955

Specimens of Protohaploxypinus limpidus are slightly smaller in size than those originally described by Balme and Hennelly [23]. This taxon has abundantly been reported from the early to late Permian sediments of Africa, Australia. Russia, India and Madagascar [10].

P. microcorpus Schaarschmidt, 1954

Although Protohaploxypinus microcorpus was common to rare in the Chhidru Formation, (Salt Range), it has rarely been reported, from the late Permian (Dzulfian) sediments of Europe.

P. varius (Bharadwaj) Balme,1970

The morphographic and systematic status of Protohaploxypinus varius have been thoroughly discussed by Balme [10]. Faunipollenites was erected by Bharadwaj [24] to include taeniate haploxylonoid pollen with a poorly defined corpus and intraretiuclate cappa, but this was rejected by Hart [17]. Balme [10] accepted Hart's view and stressed on undertaking more detailed critical morphographic comparison between Faunipollenites varius and all the previously reported sporomorphs of this type. Nevertheless Balme [10] treated Faunipollenites varius as the synonym of Protohaploxypinus varius.

Genus STRIATOABIEITES Zorichova and Sedova ex Sedova emend. Hart, 1964

Type species: Striatoabieites brickii Sedova, 1956

S. elongatus (Luber and Valtz) Hart, 1964

It morphology of sacci in the present sporomorph is not clear due to bad preservation.

S. multistriatus Balme and Hennely, 1955

Balme and Hennelly [23] originally assigned to Striatoabieites multistriatus, a rather wide range of forms and two of them should be assigned to Vittatina rather than to Striatoabieites.

S. striatus (Luber and Valtz) Hart, 1964

It is distinguished from Striatoabieites multisriatus by its less number of taenae on cappa and strongly distally inclined sacci. Genus STRIATOPODOCARPITES Samoilovich emend. Hart, 1964.

Type species: Striatopodocarpites tojmensis Sedova, 1956

S. cancellatus Balme and Hennelly, 1955

Despite the fact that Striatopodocarpites cancellatus is widespread it has been rarely observed in the Permian sediments of the Gondwanaland countries [10]. In the presently studied Chhidruan assemblages, it constituted the most conspicuous elements among the bisaccate population. Hill and Woods [25]and Virkki [26] recorded similar forms form the Pali beds, Rewa and they are also known from the Raniganj Coal measures [24]. In Africa Striatopodocarpites cancellatus occurs in lower Permian strata in Tanzania [27] and also in the early Karroo deposits in the Orange Free State [28]. Balme and Playford [29] reported S. cancellatus in upper Permian sediments from the Aery Formation, Prince Charles Mt. East Antartica.

S. pantii (Jansonius) Balme, 1970

Jansonius [30] described pollen of similar morphology from lower Triassic of Canada identifying it as Striatites Samoilovitch var. Pantii. But these specimens tend to be interrupted by wedge shaped or oblique taenae. These pollen had not been properly identified until thoroughly examined by Playford [19] and Balme [10].

S. raniganjensis (Bharadwaj) Hart, 1964

Striatopodocarpites octostriatus from the lower Permian of Tanganyika is a similar form but in the Chhidruan specimen the taenae are not as widly spaced as in Hart's [16] specimen.

S. rarus (Bharadwaj and Salujha) Balme, 1970

Pollen identical to Striatopodocarpites rarus have been reported from in the Permian of Iraq [31]. The presently isolated Chhidruan specimen is however distinct in having circular corpus, which is more thick and dark brown in color making detection or identification of taenae rather difficult even under oil immersion objective.


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Publication:Science International
Article Type:Report
Geographic Code:9PAKI
Date:Apr 30, 2015

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