1995-96 - Birbal Sahni Institute of Palaeobotany
1995-96 - Birbal Sahni Institute of Palaeobotany
1995-96 - Birbal Sahni Institute of Palaeobotany
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<strong>1995</strong>-<strong>96</strong><br />
PROJECT I<br />
Research<br />
Projects and Programmes<br />
ANTIQUITY, RADIATION AND EVOLUTIONARY<br />
TERNS OF EARLY LIFE<br />
PAT<br />
Programme<br />
Ohjective<br />
I. I<br />
Palaeobiology <strong>of</strong> Vindhyan Basin<br />
To identify metaphytes and metazoan hody ji-Jssils,<br />
ichn<strong>of</strong>ossils and their relics from the Proterozoic succession<br />
and their evolution and diversification<br />
To identify organa-sedimentary stmctures found in association<br />
<strong>of</strong> metaphytes and metazoans and to decipher<br />
environmental conditions<br />
To determine the significance <strong>of</strong> metaphytes and<br />
metazoans in hiostratigraphy<br />
Macroscopic biota comprising Chuaria - Tawuia - Krishnania were studied from<br />
the argillaceous sediments <strong>of</strong> Rohtas Formation, in Bihar, Uttar Pradesh and Madhya<br />
Pradesh. The sediments represent topmost part <strong>of</strong> the Semri Group. Two distinct<br />
carbonaceous impressions were identified, both belonging to the family Bryopsidaceae<br />
(Chlorophyta). The feather-shaped fomls compare morphologically to Bryopsis and<br />
branched filamentous fonus bearing lateral spheroidal stmctures to Derhesia. This<br />
evidence supports the presence <strong>of</strong> Chlorophyta even during ± 1000 Ma years before.<br />
New collection was done from the Lower Bhander Limestone Formation exposed<br />
around Bainkuiyan, Madhya Pradesh. Another problematic trace fossil showing fine<br />
curvature was marked. Additionally a macroscopic foml Sekwia H<strong>of</strong>mann (reported<br />
from the Vendian <strong>of</strong> Canada) was recorded. The presence <strong>of</strong> Sekwia was previously not<br />
known from the Indian Precambrian. Examined tubular forms <strong>of</strong> ichn<strong>of</strong>ossils previously<br />
described from the Kaimur. The septate tubular form indicates that it may be representing<br />
resting stage <strong>of</strong> metazoan.<br />
Studied 30 samples exposed around Judwani area, Semri Group <strong>of</strong> Madhya Pradesh<br />
both in thin section and maceration. The acritarch and cyanophycean forms arc poorly<br />
preserved and highly distorted.<br />
P.K. Maithy & Rupendra Babu<br />
Programme 1.2 Palaeobiology <strong>of</strong>the Proterozoic sediments in Cuddapah,<br />
Kaladgi and Bhima basins<br />
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