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 />
samples from south <strong>of</strong> Brahmini Coalfield. Also<br />
visited Geological Survey <strong>of</strong> India, Kolkata to<br />
discuss the palynological reports and future plan<br />
for sampling.<br />
A. Tripathi<br />
Carried out studies on the plant megafossils<br />
<strong>of</strong> the Gangapur Formation, Pranhita-Godavari<br />
Graben. Association <strong>of</strong> cycadophytes, conifers and<br />
pteridophytes within the plant assemblage indicate<br />
gymnosperm dominant vegetation during the time<br />
<strong>of</strong> deposition. Studied equisetalean stem<br />
impressions <strong>of</strong> variable morphology. Plant<br />
megafossil impressions <strong>of</strong> pteridphytes and<br />
conifers from the Kota Formation were also<br />
studied. They are invariably small in size. Also<br />
studied conifer strobilus and stem impressions<br />
from the Lameta Formation, Nand-Dongargaon<br />
sub-basin. Robust nature <strong>of</strong> conifers facilitated<br />
their preservation. Undertook field work in the<br />
Wardha-Pranhita-Godavari and collected a number<br />
<strong>of</strong> plant fossils from Kota, Gangapur and Lameta<br />
formations. A number <strong>of</strong> associated animal fossils<br />
were also noticed.<br />
A. Rajanikanth<br />
Investigated megafossils from Eddala-Gattu<br />
locality <strong>of</strong> Raghavapuram. The recorded genera are<br />
Cladophlebis indica, Sphenopteris sp., Baiera sp.,<br />
Taeniopteris spatulata, Ptilophyllum cutchense, P.<br />
acutifolium, P. sahnii and Elatocladus<br />
jabalpurensis. In general, cycadophytes and<br />
conifers dominate the assemblage, whereas<br />
pteridophytes are comparatively less. The<br />
palae<strong>of</strong>loral assemblage is contemporaneous to<br />
Vemavaram and Gollapalle floral assemblages <strong>of</strong><br />
East Coast and Sehora floral assemblage <strong>of</strong><br />
Jabalpur Formation (MP). The floral assemblage<br />
is assigned Early Cretaceous age.<br />
N. Prakash<br />
Component 2: Morphotaxonomy, floristics, evolution, biostratigraphy and palaeoenvironmental<br />
studies <strong>of</strong> Triassic-Cretaceous <strong>of</strong> South Rewa-Satpura basins<br />
Study <strong>of</strong> detached fertile organs has been<br />
completed. Two new taxa Townrowea and<br />
Douglasea have been identified. Their<br />
morphographic and cutinized structure are quite<br />
different from each other. These forms appear to<br />
be similar to the conifers <strong>of</strong> northern and southern<br />
hemispheres, but because <strong>of</strong> their detachment from<br />
the main organ and having no fertile unit<br />
definitively attached, they could be attributed to<br />
any <strong>of</strong> the known genera, viz. Voltzia,<br />
Voltziostrobus and Voltziopsis. Townrowea has<br />
been isolated in attached condition as well, but<br />
fertile units have shed <strong>of</strong>f due to fully mature<br />
fructification.<br />
S.C. Srivastava & N. Prakash<br />
Recovered diverse and abundant leaf<br />
impressions from Chui Hill, Jabalpur Formation,<br />
Satpura Basin. Excellently preserved leaves in<br />
reddish-pink clay show dominance <strong>of</strong> conifers<br />
(Elatocladus sp., E. jabalpurensis, Brachyphyllum<br />
jabalpurensis sp. nov., Pagiophyllum chawadensis,<br />
Araucarites minutus, Satpuria sehoraensis)<br />
followed by bennettitales (Anomozamites sp.,<br />
Ptilophyllum cutchense, P. acutifolium) and<br />
pteridophytes. Cycadales is represented by<br />
Taeniopteris spatulata. The floral assemblage is<br />
compared with floral assemblages <strong>of</strong> Satpura and<br />
South Rewa basins and found to be younger than<br />
Chaugan and older than Bansa floral assemblages<br />
and belongs to Early Cretaceous age.<br />
N. Prakash<br />
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