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1994-95 - Birbal Sahni Institute of Palaeobotany

1994-95 - Birbal Sahni Institute of Palaeobotany

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BSIP<br />

To palynologically differentiate Langpar (Early Palaeocene),<br />

Langpar-Lakadong (Middle Palaeocene), Lakadong­<br />

Umalatodoh-Prang (Early-Middle Eocene), Prang-Kopili (Lale<br />

Eocene) and Kopili-Barail (Early Oligocene) sediments<br />

To correlate the Therriaghm<br />

and Caro Hills<br />

assemblages with Ihose <strong>of</strong> Jaintia<br />

The Late Cretaceous and Tertiary palynological assemblages recovered from<br />

Then'iaghat and other localities were divided into several phytogeoprovinces and cenozones.<br />

The Senonian palyn<strong>of</strong>lora <strong>of</strong>lndia were clubbed with Brazil and West African palyn<strong>of</strong>loras<br />

as Constanlinisporis phytoprovince characterized by the presence <strong>of</strong> Constanlinisporis,<br />

Victorisporis and Andreisporis. The Danian to Middle Eocene palyn<strong>of</strong>loras <strong>of</strong> India were<br />

placed under pantropical Proxaperlites operculalus zone and this was further subdivided<br />

into Acroslichumsporiles meghalayensis subzone, Dandoliaspora dilma subzone,<br />

Kielmeyerapolleniles syncolporatus subzone, Lakiapollis ovatus subzone, Tricolporopililes<br />

robustus subzone and Pellicieroipollis langenheimii subzone. The Oligocene and Miocene<br />

palyn<strong>of</strong>loras were placed under pantropical Slrialriletes susannae zone and were divided<br />

into Trisyncolpites ramanujamii subzone and Hibisceaepolleniles robuslispinosus subzone.<br />

A comparison <strong>of</strong> Borneo, Caribbean and Atlantic Tertiary palynological assemblages with<br />

India reveals that the transatlantic palynological assemblages show closer similarity.<br />

R.K. Kar<br />

Important palynotaxa recovered from Bapung, Mukshay, Thangskai and Waliyncott<br />

<strong>of</strong> Meghalaya are: Cyathidites minor, Dandotiaspora dilma, D. telonala, D. plicala,<br />

Lycopodiumsporites speciosus, L. umstwensis, Polypodiisporiles repandus, Neocouperipollis<br />

kulchensis, N. wodehousei, Malanomadhiasulciles maximus, M. kutchensis,<br />

Spinizonocolpites echinatus, Proxapertiles microreliculatus, P assamicus, Lakiapollis ovalUS,<br />

Relilribrevicolporites matanomadhensis, Triangulorites bellus, Trilatiporiles kutchensis,<br />

etc. The assemblage indicates a Late Palaeocene age for the sediments.<br />

Manisha Nanda & R.K. Kar<br />

Spores and pollen recovered from Bhalu KUlUg, Meghalaya were photographed.<br />

The assemblage is dominated by the various species <strong>of</strong> Lycopodiumsporites, Dandotiaspora,<br />

Malanomadhiasulciles, Proxaperlites, Neocouperipollis, Spinizonocolpites, Tripilaoriles,<br />

Trianguloriles and Kielmeyerapollenites. The assemblage indicates a Late Palaeocene age.<br />

R.K. Kar & M. Chakraborty<br />

(Part-time Ph.D. work)<br />

Programme 6,3<br />

Objeclive<br />

Palynostratigraphy <strong>of</strong> Thra Formation (Palaeocene), Garo<br />

Hills, Meghalaya<br />

To establish significance <strong>of</strong> the palyn<strong>of</strong>lora in biostratigraphic<br />

zonation, correlation and dating<br />

To study palyn<strong>of</strong>loras<br />

recovered from selected sections in or-<br />

108

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