Distribution Mapping of Rare, endangered and threatened (RET) Plants in the Chitteri Hills, Eastern Ghats, South India

Author(s):  
D. Natarajan ◽  
R. Srinivasan
1968 ◽  
Vol 5 (3) ◽  
pp. 591-600 ◽  
Author(s):  
U. Aswathanarayana

There are three Precambrian provinces in southern India — the Dharwars (metavolcanics, metasediments, charnockites and granites), the Eastern Ghats (metasediments, charnockites and granites), and the Cuddapahs (essentially flat-lying continental sediments disturbed at the margins) — with chronostratigraphic histories dovetailing into one another. The Dharwars bear the impress of three episodes (about 3000 m.y., 2600–2300 m.y., and about 2000 m.y.) of folding, metamorphism, and emplacement of granites, the second being the most important. The pelitic sediments deposited in the Eastern Ghats geosyncline during the post-Dharwar times (upper limit, 2600 m.y.) were later folded and metamorphosed about 1600 m.y. ago into garnet-sillimanite-graphite gneisses (khondalites). Important deposits of mica pegmatites developed during this episode. Charnockites and granites associated with the Eastern Ghats were emplaced 1520–1300 m.y. ago. The Eastern Ghats rocks were subsequently cross-folded and metamorphosed about 500 m.y. ago. The sedimentation in the Cuddapah Basin was initiated sometime after the Eastern Ghats orogeny (1600 m.y. ago) but before 1160 m.y. ago. The Cuddapahs were subjected to regional metamorphism about 500 m.y. ago.


2019 ◽  
Vol 42 (1) ◽  
pp. 99-103
Author(s):  
Neerja Pande ◽  
◽  
Priyanshu Srivastava ◽  
A.K. Asthana ◽  
◽  
...  

A recent exploration and study on bryophytes of Eastern Ghats’ area of Andhra Pradesh has revealed the occurrence of two pleurocarpous mosses viz., Thuidium assimile (Mitt.) A. Jaeger and Anomodon minor subsp. integerrimus (Mitt.) Iwatsuki as new addition to the moss flora of South India. A detailed morpho-taxonomical account and illustration of these taxa are provided.


2011 ◽  
Vol 4 (9) ◽  
pp. 698-705 ◽  
Author(s):  
Chinnaperumal Kamaraj ◽  
Abdul Abdul Rahuman ◽  
Asokan Bagavan ◽  
Gandhi Elango ◽  
Abdul Abduz Zahir ◽  
...  

2018 ◽  
Vol 2 (6) ◽  
pp. 495-498
Author(s):  
Ramar M ◽  
Mahendran M ◽  
Kamalakannan S ◽  
Jayakumar E ◽  
Anbalagan V ◽  
...  

1965 ◽  
Vol 60 (5) ◽  
pp. 1046-1051 ◽  
Author(s):  
J. S. R. Krishna Rao ◽  
V. Malleswara Rao
Keyword(s):  

Zootaxa ◽  
2020 ◽  
Vol 4768 (3) ◽  
pp. 374-382
Author(s):  
SANKARAPPAN ANBALAGAN ◽  
KALIMUTHU REKHA ◽  
SURULIYANDI VIJAYAN ◽  
CHELLAPANDIAN BALACHANDRAN ◽  
SUNDARAM DINAKARAN ◽  
...  

A new black fly species, Simulium (Nevermannia) karavalliense sp. nov. is described from Southern Eastern Ghats of South India. This new species is placed in the Simulium ruficorne species-group of the subgenus Nevermannia. S. (N.) karavalliense sp. nov. is characterized by female with a long sensory vesicle, male upper eye with 14 vertical columns and 16 horizontal rows of large facets, pupal gill with 8 filaments and larval hypostoma with 6 hypostomal bristles lying parallel to lateral margin. Taxonomic keys are provided to distinguish this new species from related species in India.  


2015 ◽  
Vol 38 (3) ◽  
pp. 244-248
Author(s):  
A. Asthana ◽  
Ichha Omar ◽  
Priyanshu Srivastava

Lejeunea minutiloba A. Evans has been identified in Eastern Ghats region of Tamil Nadu which is a new record for South India. It was earlier reported from Brazil, Bermuda, Cuba, North America, Puerto Rico (Mona Island), ST. Thomas, West Indies and from Eastern Himalaya in India. The taxon is characterized by highly reduced obsolete lobules, small marginal cells of leaf lobe, non connate bracts and bracteole and occurrence of clavate as well as ovoid - oblong perianth exhibiting an interesting transitional morphoform with an affinity with L. cladogyna A. Evans.


2013 ◽  
Vol 134 (1) ◽  
pp. 26-32 ◽  
Author(s):  
Naveen Kumar Kaushik ◽  
Asokan Bagavan ◽  
Abdul Abdul Rahuman ◽  
Dinesh Mohanakrishnan ◽  
Chinnaperumal Kamaraj ◽  
...  

2009 ◽  
Vol 73 (1) ◽  
pp. 149-164 ◽  
Author(s):  
H. E. Belkin ◽  
R. Macdonald ◽  
E. S. Grew

Electron microprobe data are presented for chevkinite-group minerals from granulite-facies rocks and associated pegmatites of the Napier Complex and Mawson Station charnockite in East Antarctica and from the Eastern Ghats, South India. Their compositions conform to the general formula for this group, viz. A4BC2D2Si4O22 where, in the analysed specimens A = (rare-earth elements (REE), Ca, Y, Th), B = Fe2+, Mg, C = (Al, Mg, Ti, Fe2+, Fe3+, Zr) and D = Ti and plot within the perrierite field of the total Fe (as FeO) (wt.%) vs. CaO (wt.%) discriminator diagram of Macdonald and Belkin (2002). In contrast to most chevkinite-group minerals, the A site shows unusual enrichment in the MREE and HREE relative to the LREE and Ca. In one sample from the Napier Complex, Y is the dominant cation among the total REE + Y in the A site, the first reported case of Y-dominance in the chevkinite group. The minerals include the most Al-rich yet reported in the chevkinite group (≤9.15 wt.% Al2O3), sufficient to fill the C site in two samples. Conversely, the amount of Ti in these samples does not fill the D site, and, thus, some of the Al could be making up the deficiency at D, a situation not previously reported in the chevkinite group. Fe abundances are low, requiring Mg to occupy up to 45% of the B site. The chevkinite-group minerals analysed originated from three distinct parageneses: (1) pegmatites containing hornblende and orthopyroxene or garnet; (2) orthopyroxene-bearing gneiss and granulite; (3) highly aluminous paragneisses in which the associated minerals are relatively magnesian or aluminous. Chevkinite-group minerals from the first two parageneses have relatively high FeO content and low MgO and Al2O3 contents; their compositions plot in the field for mafic and intermediate igneous rocks. In contrast, chevkinite-group minerals from the third paragenesis are notably more aluminous and have greater Mg/Fe ratios.


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