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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 />

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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