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Organisational Structure - Birbal Sahni Institute of Palaeobotany

Organisational Structure - Birbal Sahni Institute of Palaeobotany

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<strong>Birbal</strong> <strong>Sahni</strong> <strong>Institute</strong> <strong>of</strong> <strong>Palaeobotany</strong><br />

Rock samples (30) from Laptal Chojan La section<br />

<strong>of</strong> Spiti Shale Formation, Malla Johar area have been<br />

worked out for their spore-pollen. The characteristic<br />

taxa, viz. Callialasporites spp, Murospora florida,<br />

Cicatricatisporites australiensis, Aequitriradites<br />

spinulosus, Appendicisporites sp,, etc. evidence the<br />

Oxfordian to Berriasian age correlation for the<br />

formation. The palynozones identified have been<br />

compared with the known Ammonite zones to<br />

develop an integrated biostratigraphy <strong>of</strong> Spiti Shale<br />

unit in the Tethyan Mesozoic sequence.<br />

Vijaya<br />

Component 2: Permian plant fossils from North-Eastern Himalayas<br />

Observation, description, morphotaxonomy and<br />

photodocumentation <strong>of</strong> Permian plant fossils from<br />

Tindharia, Pankhabari, Kalijhore nala sections <strong>of</strong><br />

Darjeeling and Rohtak Khola section <strong>of</strong> South Sikkim<br />

district have been carried out in detail. The<br />

assemblages are represented by following species:<br />

Gangamopteris cyclopterioides, G. major, G.<br />

clarkeana, Gangamopteris sp., Glossopteris<br />

communis, Gl. indica, Gl. stenoneura, Gl. varia, Gl.<br />

vulgaris, Noeggerathiopsis hislopii, equisetalian axes<br />

and vertically and horizontally preserved Vertebraria<br />

axes. The compilation <strong>of</strong> floristic data and<br />

stratigraphical significance <strong>of</strong> the flora are under<br />

progress. Carbonaceous shale samples from different<br />

sections <strong>of</strong> Tindharia, Baman Pukharia, Pankhabari<br />

and Rohtak nala were chemically processed.<br />

Although the samples are devoid <strong>of</strong> megaspores,<br />

seeds and cuticles, but presence <strong>of</strong> Botryococcus-algal<br />

colony in almost all the samples are significant. The<br />

palaeoecological significance <strong>of</strong> the algae is being<br />

studied.<br />

R. Tewari & A.K. Srivastava<br />

Chemically processed coal and carbonaceous<br />

shale samples from Kalijhora, Rakti Khola and<br />

Bamon Pokhari areas <strong>of</strong> Darjeeling district (WB) for<br />

palynological analysis. Carbonaceous shale samples<br />

from Kalijhora nala section have yielded<br />

palyn<strong>of</strong>ossils, represented by Scheuringipollenites<br />

maximus, Alisporites sp., Distriatites sp.,<br />

Faunipollenites varius, Striatopodocarpites and<br />

Micr<strong>of</strong>oveolatispora. A number <strong>of</strong> Botryococcus<br />

algal colonies have also been found.<br />

A.K. Srivastava & A.P. Bhattacharyya<br />

Project 4: Floristics, biostratigraphy and palaeoenvironment <strong>of</strong><br />

Gondwana sediments<br />

Component 1: Morphotaxonomy, floristics, evolution, biostratigraphy and palaeo-environmental<br />

studies <strong>of</strong> Son-Mahanadi, Damodar, Panagarh and Birbhum basins<br />

Completed identification <strong>of</strong> 350 impression and<br />

compression specimens from eight localities <strong>of</strong><br />

Mand–Raigarh coalfield, Chattisgarh, viz. Kantasar<br />

nala section near Dokripari village, Mand river<br />

section near Ambetikra temple, Kasaia nala section<br />

near Kasaia village, Gersaghat section near Gersa<br />

village, Saria nala section, and Barod, Jindal and<br />

Mand open cast projects. The plant fossils indicate<br />

Early to Late Permian age (Karharbari, Barakar and<br />

Kamthi formations) for the various beds. Photography<br />

<strong>of</strong> important taxa is also completed. Singh again<br />

visited the coalfield area and collected above 250<br />

megafossil specimens belonging to Glossopteris flora<br />

from Barakar and Kamthi formations exposed in<br />

different nala sections and collieries.<br />

S. Chandra & K.J. Singh<br />

Traced the marker spore-pollen species from the<br />

coal-bearing and Kamthi sediments <strong>of</strong> Talcher<br />

coalfield (Orissa). The Permo-Triassic palyn<strong>of</strong>loral<br />

transition has been recorded in the subsurface<br />

material. The change <strong>of</strong> palyn<strong>of</strong>lora is gradual. The<br />

variation in the pattern <strong>of</strong> change over the distribution<br />

<strong>of</strong> nonstriate and taeniate bisaccate pollen is more<br />

6

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