Organisational Structure - Birbal Sahni Institute of Palaeobotany
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 />
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