R
Ravuru Sudhakar
Researcher at Acharya N. G. Ranga Agricultural University
Publications - 4
Citations - 81
Ravuru Sudhakar is an academic researcher from Acharya N. G. Ranga Agricultural University. The author has contributed to research in topics: Germplasm & Population. The author has an hindex of 3, co-authored 3 publications receiving 59 citations.
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Identification of QTLs and possible candidate genes conferring sheath blight resistance in rice (Oryza sativa L.)
Shailesh Yadav,G. Anuradha,Ravi Ranjan Kumar,Lakshminaryana Reddy Vemireddy,Ravuru Sudhakar,Krishnaveni Donempudi,Durgarani Venkata,Farzana Jabeen,Yamini Kalinati Narasimhan,Balram Marathi,Balram Marathi,E. A. Siddiq +11 more
TL;DR: In order to map the quantitative trait loci (QTLs) governing the sheath blight resistance, two mapping populations (F2 and BC1F2) were developed from the cross BPT-5204/ARC10531 which expressed moderate level of resistance to the disease.
Journal ArticleDOI
Assessment of resistance to Fusarium wilt disease in sesame (Sesamum indicum L.) germplasm
Badri Jyothi,Nisar Ahmed Ansari,Yepuri Vijay,Ganta Anuradha,Ananta Sarkar,Ravuru Sudhakar,E. A. Siddiq +6 more
TL;DR: The accessions identified in the present study may be considered in crop improvement programmes involved in developing wilt resistant varieties, however further efforts need to be concentrated on identifying highly resistant genotypes with the inclusion of vast germplasm in screening procedures.
Journal ArticleDOI
Bulked Segregant Analysis to Detect Main Effect of QTL Associated withSheath Blight Resistance in BPT-5204/ARC10531 Rice (Oryza sativa L)
Shailesh Yadav,G. Anuradha,Ravi Ranjan Kumar,Lakshminarayana R. Vemireddy,Ravuru Sudhakar,Balram M,E. A. Siddiq +6 more
TL;DR: The results obtained from the DNA pooling of phenotypic extremes could be a useful strategy to detect the genetic loci with major effects of the complex trait such as disease resistance in rice.
Baratang island mud volcanoes, india: a potential candidate for martian
TL;DR: The most common landforms on the Mars surface are pitted cones, mounds and lobate flows which are mostly deciphered as having formed through a variety of overlapping processes like periglacial, glacial, volcanic, and/or impact processes as discussed by the authors .