Early Permian megaspores from Goutham Khani
Open Cast Mine, Kothagudem Area, Godavari Graben,
Telangana, India
ARUN JOSHI
*
AND RAJNI TEWARI
Birbal Sahni Institute of Palaeobotany, 53 University Road, Lucknow 226 007, India.
*
Corresponding author: arunjoshi119@gmail.com
(Received 13 October, 2015; revised version accepted 28 November, 2015)
ABSTRACT
Joshi A & Tewari R 2015. Early Permian megaspores from Goutham Khani Open Cast Mine, Kothagudem Area, Godavari
Graben, Telangana, India. The Palaeobotanist 64(2): 139–150.
Early Permian megaspores are reported for the irst time from the Barakar Formation of Index Seam, Goutham Khani Open
Cast Mine, Kothagudem Area, Godavari Graben, Telangana, India. The megaspore assemblage includes three genera and ten
species, namely Biharisporites spinosus, Biharisporites sp. A (in Tewari et al., 2009), Biharisporites sp., Jhariatriletes iliformis,
Jhariatriletes sp., Singhisporites indica, S. nautiyalii, S. radialis, S. surangei and Singhisporites sp. Besides adding to the existing
knowledge of megaspores from the Godavari Graben, the comparison of megaspores from the Goutham Khani Open Cast Mine with
those of the other Indian Lower Gondwana basins, namely Damodar, Satpura, Wardha, South Rewa and other areas of the Godavari
Graben reveals that majority of these differ in the presence of dense ornamentations on their exosporia. The previous records of
megaspores from the late Permian of the Godavari Graben show dense spinate exosporia. Presence of such dense diverse spines on
megaspores of this study indicates their early appearance during the Barakar Formation. An analysis of the developmental pattern
of the exosporium architecture of Lower Gondwana megaspores in general, indicates that during the early Permian Talchir and
Karharbari formations, the megaspores had simple outer layer with usually smooth, granulate, verrucate and sometimes baculate/
connate ornamentations whereas, dense spinate exosporia were more common during Barakar and Raniganj formations indicating
fresh water aquatic conditions. As such, the spinate megaspores of Kothagudem region also point towards terrestrial aquatic conditions.
Key–words—Megaspores, Barakar Formation, Palaeoenvironment, Kothagudem Area, Godavari Graben.
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© Birbal Sahni Institute of Palaeobotany, India
The Palaeobotanist 64(2015): 139–150
0031–0174/2015