1994-95 - Birbal Sahni Institute of Palaeobotany
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 />
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