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- Syed M. Shah
- N. Saini
- S. Ashraf
- Chhaya Sharma
- R. Sinha
- D. N. Yadav
- M. M. Sarin
- S. K. Singla
- N. L. Selokar
- M. Saini
- P. Palta
- R. S. Manik
- Anjali Trivedi
- M. F. Quamar
- H. Agrawal
- A. K. Raja
- A. A. Sahare
- D. Priya
- Ankur Sharma
- A. Kumaresan
- M. K. Singh
- S. Chand
- K. Patel
- S. S. Lathwal
- T. K. Mohanty
- S. Chand
- R. Verma
- G. Tripathi
- R. Meena
- Ajay Aswal
Journals
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Chauhan, M. S.
- Bioinformatics in Stem Cell Characterization
Abstract Views :526 |
PDF Views:444
Authors
Affiliations
1 Animal Biotechnology Center National Dairy Research Institute, Karnal-132001, IN
1 Animal Biotechnology Center National Dairy Research Institute, Karnal-132001, IN
Source
Indian Journal of Bioinformatics and Biotechnology, Vol 1, No 1 (2012), Pagination: 17-18Abstract
Speaking in realistic sense a stem cell is endowed with potentials only, which are options rather than specific gene-expression patterns, thereby making its identification vague. Their characterization thus necessitates an overall genomic and proteomic analysis, coupled with mathematical modeling providing for the need for a wide range of bioinformatics tools to efficiently and effectively process large amounts of data being generated. A large number of computational tools and bioinformatic methods are thus required to deal with the experimental riches of this complex and multivariate data and the subsequent transition from data collection to information or knowledge in order to arrive at a universal definition of stemness.Keywords
Bioinformatics, Stem Cell Characterization, StemnessReferences
- Flower D, Macdonald I, Ramakrishan K, Davies M and Doytchinova I (2010) Immunomee research. 6, 2-16.
- Choo K, Tan T and Ranganathan S(2009) BMC Bioinformatics 10, S2.
- Zipori D(2004) Nature Reviews Genetics 5, 873-78.
- Robert JS (2004) Model systems in stem cell biology, BioEssays 26, 1005–1012.
- Kapetanovic I, Rosenfeld S and Izmirlian G (2004) New York Academy of Sciences. 1020,10-21.
- Vegetation and climatic variability in southeastern Madhya Pradesh, India since Mid-Holocene, based on pollen records
Abstract Views :222 |
PDF Views:106
Authors
Affiliations
1 Birbal Sahni Institute of Palaeobotany, Lucknow 226 007, IN
1 Birbal Sahni Institute of Palaeobotany, Lucknow 226 007, IN
Source
Current Science, Vol 109, No 5 (2015), Pagination: 956-965Abstract
Pollen analysis of 1.75 m deep sediment core from Tula-Jalda (Amarkantak) in Anuppur district, Madhya Pradesh unravels that around 4500–3600 cal years BP, this region supported open mixed tropical deciduous forests comprising chiefly Madhuca indica followed by Terminalia, Mitragyna parvifolia, Haldina cordifolia, Emblica officinalis and Acacia, under a warm and relatively less humid climate. The retrieval of Cerealia and other cultural plants, viz. Artemisia, Cheno/Am and Caryophyllaceae signifies that the region was under cereal-based agricultural practice. The open mixed deciduous forests got enriched and dense around 3600–2761 cal years BP with the expansion of trees that already existed coupled with invasion of Symplocos, Diospyros, Lannea coromandelica and Radermachera with the inception of a warm and moderately humid climate in response to increased monsoon precipitation. Around 2761–2200 cal years BP, much expansion of the forests took place owing toinitiation of a warm and more humid climate, attributed to intensification of the southwest (SW) monsoon. The modern Sal (Shorea robusta) forests were established around 2200 cal years BP, as clearly deciphered by the steady presence of S. robusta along with close allies such as M. indica, Terminalia, H. cordifolia, E. officinalis, etc. This change in the vegetation scenario implies that a warm and relatively more humid climate prevailed with timely arrival of the more active SW monsoon.Keywords
Climate, pollen analysis, sediment core, vegetation.References
- Vishnu-Mittre, Studies of the vegetation history from the swamps in the Nilgiris. 1. The Nilgiri peat deposits. In Proceedings of 50th Indian Science Congress, Calcutta, 15–17 January 1963, vol. 3, pp.394–395.
- Vishnu-Mittre and Gupta, H. P., A living fossil plant community in south Indian hill. Curr. Sci., 1968, 37, 671–672.
- Vishnu-Mittre and Gupta, H. P., The origin of Shola forest in the Nilgiris, south Indian hill. Palaeobotanist, 1971, 19(1), 110–114.
- Gupta, H. P. and Bera, S. K., Silent valley, a correlation between pollen spectra and vegetation. Palaeobotanist, 1996, 43(2), 139–144.
- Anupama, K., Prasad, S. and Reddy, C. S., Vegetation, land cover and land use changes of the last 200 years in the Eastern Ghats (southern India) inferred from pollen analysis of sediments from a rain-fed tank and remote sensing. Quaternary Int., 2014, 325, 93–104.
- Vasanthy, G., Pollen analysis of late Quaternary sediments: evolution of upland savanna in Sandynallah (Nilgiris, South India). Rev.of Palaeobot. Palynol., 1988, 55, 175–192.
- Van Campo, E., Duplessy, J. C. and Rossignol-Strick, M., Climatic conditions deduced from a 150 kyr oxygen isotope-pollen record from Arabian Sea. Nature, 1982, 296(2852), 56–59.
- Gupta, H. P. and Khandelwal, A., Mangrove development at Nalabana island, Chilka Lake: a palynological interpretation. Geophytology,1992, 22, 235–238.
- Farooqui, A. and Achyuthan, H., Evidence of Middle to Late Holocene vegetation in Adyar Estuary, Chennai. J. Geol. Soc.India, 2006, 68, 230–238.
- Singh, G., Joshi, R. D., Chopra, S. K. and Singh, A. B., Late Quaternary history of vegetation and climate of the Rajasthan Desert,India. Philos. Trans. R. Soc. London, Ser. B, 1974, 267(889), 467–501.
- Chauhan, M. S., Origin and history of tropical deciduous Sal (Shorea robusta Gaertn.) forests in Madhya Pradesh, India. Palaeobotanist,1995, 43, 89–101.
- Chauhan, M. S., Pollen evidence of Late-Quaternary vegetation and climatic changes in northeastern Madhya Pradesh. Palaeobotanist,2000, 49(3), 491–500.
- Chauhan, M. S., Holocene vegetation and climatic changes in southeastern Madhya Pradesh, India. Curr. Sci., 2002, 83, 1444–1445.
- Chauhan, M. S., Late-Holocene vegetation and climatic changes in Eastern Madhya Pradesh. Gondwana Geol. Mag., 2004, 19(2), 165–175.
- Chauhan, M. S., Pollen record of vegetation and climatic changes in northeastern Madhya Pradesh during last 1600 years. Trop.Ecol., 2005, 46(2), 263–269.
- Chauhan, M. S. and Quamar, M. F., Vegetation and climate change in southeastern Madhya Pradesh during Late Holocene, based on pollen evidence. J. Geol. Soc. India, 2010, 76, 143–150.
- Chauhan, M. S., Sharma, A., Phartiyal, B. and Kumar, K., Holocene vegetation and climatic variations in central India: a study based on multiproxy evidences. J. Asian Earth Sci., 2013, 77, 45–58.
- Yadav, D. N., Chauhan, M. S. and Sarin, M. M., Geochemical and pollen records from northeastern Madhya Pradesh: an appraisal of Late-Quaternary vegetation and climate change. J. Geol. Soc.India, 2006, 68(1), 95–102.
- Shaw, J., Sutcliffe, J., Lloyd-Smith, L., Schwenninger, J., Chauhan, M. S., Mishra, O. P. and Harwey, S., Ancient irrigation and Buddhist history in Central India: optically stimulated luminescence dates and pollen sequences from Sanchi dams. Asian Perspectives, 2007, 46(1), 166–201.
- Chauhan, M. S. and Quamar, M. F., Pollen records of vegetation and inferred climate change in southwestern Madhya Pradesh during the last ca. 3800 years. J. Geol. Soc. India, 2012, 80, 470–480.
- Chauhan, M. S. and Quamar, M. F., Mid-Holocene vegetation visà-vis climate change in southwestern Madhya Pradesh, India. Curr. Sci., 2012, 103(12), 1455–1461.
- District Ground Water Information Booklet, Anuppur district, Madhya Pradesh, Ministry of Water Resources, Central Ground Water Board, North-Central Region, Bhopal, 2007, pp. 1–16.
- Champion, H. G. and Seth, S. K., The Revised Survey of Forest Types of India, Delhi, 1968.
- Erdtman, G., An Introduction to Pollen Analysis, Chronica Botanica, Mass., USA, 1943.
- Nayar, T.S., Pollen Flora of Maharashtra State, India. Today & Tomorrow’s Printer and Publisher, Delhi, 1990.
- Chauhan, M. S. and Bera, S. K., Pollen morphology of some important plants of tropical deciduous Sal (Shorea robusta) forests, district Sidhi, Madhya Pradesh. Geophytology, 1990, 20(1), 30–36.
- Atluri, J. B., Venkataraman, S. P. and Subba Reddi, C., Explosive pollen release, windpollination and mixed mating in the tropical tree Shorea robusta Gaertn. F. (Dipterocarpaceae). Curr. Sci., 2004, 86, 1416–1419.
- Chauhan, M. S., Modern pollen/vegetation relationship in the tropical deciduous Sal (Shorea robusta) forests in District Sidhi, Madhya Pradesh. J. Palynol., 1994, 30, 165–175.
- Chauhan, M. S., Pollen deposition pattern in the tropical deciduous Sal (Shorea robusta) forests in northeastern Madhya Pradesh. Geophytology, 2007, 37, 119–125.
- Vincens, A., Semmanda, I., Roux, M. and Jolly, D., Study of the modern pollen rain in Western Uganda with a numerical approach. Rev. Palaeobot. Palynol., 1997, 96, 145–168.
- Benarde, M. A., Global Warming, John Wiley, New York, 1996.
- Chauhan, M. S., Pokharia, A. K. and Singh, I. B., Pollen record of Holocene vegetation, climate change and human habitation from Lahuradewa Lake, Sant Kabir Nagar District, Uttar Pradesh, India. Man Environment, 2009, 34(1), 88–100.
- Trivedi, A., Chauhan, M. S., Sharma, A., Nautiyal, C. M. and Tiwari, D. P., Record of vegetation and climate during Late Pleistocene–Holocene in Central Ganga Plain, based on multiproxy data from Jalesar Lake, Uttar Pradesh, India. Quaternary Int.,2013, 306, 97–106.
- Meher-Homji, V. M., Climate changes: projects and prospects. Curr. Sci., 2000, 78, 777–779.
- Studies on Holocene Climatic Changes From Priyadarshini Lake Sediments, East Antarctica: The Palynological Evidence
Abstract Views :191 |
PDF Views:2
Authors
Affiliations
1 Department of Geology, University of Lucknow, Birbal Sahni Institute of Palaeobotany, Lucknow - 226 007, IN
2 Birbal Sahni Institute of Palaeobotany, Lucknow - 226 007, IN
3 Indian Institute of Technology, Kanpur - 208 016, IN
1 Department of Geology, University of Lucknow, Birbal Sahni Institute of Palaeobotany, Lucknow - 226 007, IN
2 Birbal Sahni Institute of Palaeobotany, Lucknow - 226 007, IN
3 Indian Institute of Technology, Kanpur - 208 016, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 69, No 1 (2007), Pagination: 92-96Abstract
Pollen analysis of a sediment core from Priyadarshini Lake (Core S3), East Antarctica, has revealed the climatic oscillations in the region since Holocene. Three pollen zones have been identified on the basis of recovered pollen taxa and varying frequencies. Between 10,000 and 9,000 yr BP, cold and dry climate prevailed in the region as reflected by the dominance of grasses, Acritarch and very low frequencies of Cosmarium - a fresh water alga. The lake was probably shallow and smaller in dimension during this period. Between 9,000 to 2,400 yr BP, relative increase in grasses is witnessed though in fluctuating frequencies. Cosmarium also exhibits a distinct increasing trend, whereas Acritarch declines considerably. This overall change in the assemblage reflects the onset of warm and moist climate and the lake had a wider expansion during this phase on account of amelioration in climate than witnessed before. Between 2,400 and 1,000 yr BP, relatively reduced frequencies of grasses, coupled with total disappearance of Cosmarium, demonstrate that the climate changed once again to cold and dry. However, 1,000 yr BP onwards, marked increase in grasses coupled with exceedingly high values of Cosmarium implies that the climate ultimately turned warm and moist.Keywords
Palynology, Holocene, Climate Changes, Priyadarshini Lake, Antarctica.- Geochemical and Pollen Proxy Records from Northeastern Madhya Pradesh: An Appraisal of Late-Quaternary Vegetation and Climate Change
Abstract Views :173 |
PDF Views:2
Authors
Affiliations
1 Bhabha Atomic Research Centre, Trombay, Mumbai - 400 085, IN
2 Birbal Sahni Institute of Palaeobotany, 53 University Road, Lucknow - 226 007, IN
3 Earth Science Division, Physical Research Laboratory, Ahemdabad - 380 009, IN
1 Bhabha Atomic Research Centre, Trombay, Mumbai - 400 085, IN
2 Birbal Sahni Institute of Palaeobotany, 53 University Road, Lucknow - 226 007, IN
3 Earth Science Division, Physical Research Laboratory, Ahemdabad - 380 009, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 68, No 1 (2006), Pagination: 95-102Abstract
A 15 m deep sedimentary core from Jagmotha swamp in northeastern Madhya Pradesh has been analyzed for reconstruction of Late-Quaternary vegetation and climate change based on distribution of major/Trace elements, organic carbon, nitrogen and pollen grains contained in the sediments. The combined geochemical and palynological results indicate a cool and dry climate between 6000 to 5000 yrs BP representing a tree savannah type vegetation followed by warm and moist climate between 5000 to 3000 yrs BP. Such a drastic change in climate promoted tropical mixed deciduous forests in the region. Subsequently, between 3000 to 1200 yrs BP, the climatic condition got further improved with enhanced precipitation in the region marked by the advent of sal tree in the forest floristics. Since then, the climate has been inferred conducive for development of modern sal forests in the region.Keywords
Palaeoclimate, Palaeovegetation, Late-Quaternary Period, Major/Trace Element Geochemistry, Organic Carbon and Nitrogen, C/N Ratio, Pollen Frequency.- Buffalo Cloning:what we Have Achieved so Far
Abstract Views :288 |
PDF Views:110
Authors
Affiliations
1 Animal Biotechnology Centre, National Dairy Research Institute, Karnal 132 001, IN
2 Animal Physiology and Reproduction Division, Central Institute for Research on Buffaloes, Hisar 125 001, IN
1 Animal Biotechnology Centre, National Dairy Research Institute, Karnal 132 001, IN
2 Animal Physiology and Reproduction Division, Central Institute for Research on Buffaloes, Hisar 125 001, IN
Source
Current Science, Vol 109, No 4 (2015), Pagination: 670-671Abstract
No Abstract.- Holocene Vegetation and Climate Fluctuations in Northwest Himalaya, Based on Pollen Evidence from Surinsar Lake, Jammu Region, India
Abstract Views :214 |
PDF Views:0
Authors
Affiliations
1 Department of Geology, Lucknow University, Lucknow - 226 007, IN
2 Birbal Sahni Institute of Palaeobotany, Lucknow - 226 007, IN
1 Department of Geology, Lucknow University, Lucknow - 226 007, IN
2 Birbal Sahni Institute of Palaeobotany, Lucknow - 226 007, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 74, No 3 (2009), Pagination: 402-412Abstract
Pollen analysis of a 33.21 m deep sediment core from Surinsar lake in Jammu region has revealed that between 9,500 and 7,700 yr BP (Pollen zone SL-I), the mixed oak-broad-leaved/chirpine forest occurred in the region under a warm and humid climate. The record of aquatic plants viz. Potamogeton, Typha and freshwater alga Botryococcus in appreciable numbers denotes the existence of the lake since the Early Holocene. Subsequently, mixed chirpine/oakbroad- leaved forests appeared in the area around 7,700 to 6,125 yr BP (Pollen zone SL-II) with the dominance of chirpine (Pinus cf. roxburghii) by the onset of cool and dry climate, attributed to decrease in monsoon rainfall. The expansion of oak and its broad-leaved associates between 6,125 and 4,330 yr BP (Pollen zone SL-III) suggests that the climate turned moderately humid and warm, presumably due to enhanced monsoonal effect. The region has witnessed a brief spell of pluvial environment between 4,330 and 4,000 yr BP (Pollen zone SL-IV) as evidenced by the presence of sandy layer at 15.4-14 m depths. The period of 4,000 to 2,100 yr BP (Pollen zone SL-V) is marked by the prevalence of cool and dry climate as depicted by a sharp decline in oak (Quercus cf. incana) and other broad-leaved taxa and a concurrent increase in chirpine. From 2,100 to 800 yr BP (Pollen zone SL-VI) no palaeofloristic inferences could be drawn due to paucity of pollen, however, the presence of sandy deposit at the corresponding level in lithocolumn implies a pluvial episode by this time. Since 800 yr BP to Present (Pollen zone SL-VII) the slight advance in the oak reflects the ameliorating trend of climate, despite the existing cool and dry climate.Keywords
Pollen Analysis, Palaeovegetation, Palaeoclimate, Holocene, Surinsar Lake, Jammu.References
- BHATTACHARYYA, A. (1989) Vegetation and climate during the last 30,000 years in Ladakh. Palaeogeo. Palaeoclimat. Palaeoeco., v.73, pp.25-38.
- CHAMPION, H.G. and SETH, S.K. (1968) A Revised Survey of Forest Types of India. New Delhi, 397p.
- CHAUHAN, M.S. and SHARMA, C. (1993) Modern pollen deposition in subtropical zone of Kumaon Himalaya. Geophytology, v.23, No.1, pp.147-153.
- DODIA, R. (1988) Climate of Kashmir during the last 700,000 years: The Baltal pollen profile. Proc. natn. Sci. Acad., v.54A, No.3, pp.481-489.
- ERDTMAN, G. (1943) An Introduction to Pollen Analysis. Waltham Mass., USA, 239p.
- GUPTA, H. P. (1991) Changing pattern of vegetation in the intermontane basin of Kashmir since 4 Ma: A palynological approach. Palaeobotanist, v.40, pp.354-373.
- GUPTA, H.P. and SHARMA, C. (1989) Vegetational history and palaeoenvironment of Hirpur Loc. I, Lower Karewa. Palaeobotanist, v.37, No.2, pp.155-158.
- GUPTA, H.P., SHARMA, C., DODIA, R., MANDAVIA, C. and VORA, A.B. (1984) A palynological interpretation of climate changes in Kashmir (India) during the past three million years. Proceedings of Palaeoenvironment of East Asia from Mid-Tertiary II, Hong Kong, pp.553-568.
- GUPTA, H. P., SHARMA, C., DODIA, R., MANDAVIA, C. and VORA, A. B. (1988) Palynostratigraphy and palaeoenvironment of Kashmir, Hirpur Loc. III. Climate and Geology of Kashmir (Publ.), pp.75-90.
- PURI, G.S. (1947) The occurrence of tropical fig (Ficus cunia Buch- Ham.) in the Karewa beds at Liddarmarg, Pir Panjal Range, Kashmir with remarks on the sub-tropical forests of the Kashmir Valley during the Pleistocene. Jour. Indian Bot. Soc., v.26, No.3, pp.131-135.
- PURI, G.S. (1948) The flora of the Karewa series of Kashmir and its phytogeographical affinities with chapter on the method used in identification. Indian Forester, v.74, no.3, pp.105-122.
- SEKHAR, B. (2000) Interpretation of past climatic changes around Tsokar Lake, Ladakh for the last 33 ka on the basis of chemical data. Palaeobotanist, v.49, pp.519-527.
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- SHARMA, C. and GUPTA, H.P. (1984) Past and present distribution of Larix griffithiana Hort. ex. Carr. in the Indian subcontinent as evidence by palynology. Zfa. Z. Archaeol. Berlin, v.18, pp.239-246.
- SHARMA, C., GUPTA, H. P., DODIA, R. and MANDAVIA, C. (1985) Palynostratigraphy and palaeoenvironment, Dubjan, Lower Karewa, Kashmir. Climate and Geology of Kashmir, pp.69-73.
- SHARMA, C., TRIVEDI, A. and MALIK, M.A. (2001) Modern pollen/ spore rain in Surinsar and Mansar lakes, Jammu. Geophytology, v.31, Nos.1&2, pp.9-17.
- SINGH, G. (1964) A preliminary survey of the Postglacial vegetational history of the Kashmir Valley. Palaeobotanist, v.12, No.1, pp.73-108.
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- VISHNU-MITTRE and SHARMA, B. D. (1966) Studies of Post glacial vegetational history from the Kashmir Valley-1, Haigam Lake. Palaeobotanist, v.15, No.12, pp.185-212.
- VISHNU-MITTRE and ROBERT, R.D. (1973) Pollen analysis and palaeobotany of impressions bearing sediments in the Lower Karewa. Palaeobotanist, v.20, No.3, pp.344-355.
- Vegetation and Climate Change in Southeastern Madhya Pradesh during Late Holocene, Based on Pollen Evidence
Abstract Views :198 |
PDF Views:0
Authors
Affiliations
1 Birbal Sahni Institute of Palaeobotany, Lucknow – 226 007, IN
1 Birbal Sahni Institute of Palaeobotany, Lucknow – 226 007, IN
Source
Journal of Geological Society of India (Online archive from Vol 1 to Vol 78), Vol 76, No 2 (2010), Pagination: 143-150Abstract
Pollen analysis of 2 m deep sediment core from Kiktiha swamp, Shahdol district has revealed that between 1600 and 700 yr BP, tropical deciduous Sal forests comprising Shorea robusta (Sal), Madhuca indica, Terminalia, Lagerstroemia, Aegle marmelos flourished in the region under a warm and moist climate. Between 700 and 300 yr BP the deciduous Sal forests were succeeded by mixed deciduous forests, which turned sparse and less diversified, reflecting a relatively less moist climate attributed to the weak SW monsoon. The unfavourable climate also adversely affected the agricultural practice as evidenced from the diminution of Cerealia and other culture taxa. Since 300 yr BP onwards the modern deciduous Sal forests were re-established with the timely arrival of active SW monsoon. The increase in Cerealia and culture taxa indicates agricultural prosperity.Keywords
Pollen Analysis, Late Holocene, Vegetation, Climate, Southeastern Madhya Pradesh.- Milk-Derived Epithelial Cells Area a Potential Source of Donor Genome for the Production of Buffalo (Bubalus bubalis) Cloned Embryos
Abstract Views :302 |
PDF Views:79
Authors
N. L. Selokar
1,
M. Saini
1,
H. Agrawal
1,
A. K. Raja
1,
A. A. Sahare
1,
D. Priya
1,
P. Palta
1,
M. S. Chauhan
1,
R. S. Manik
1,
S. K. Singla
1
Affiliations
1 Animal Biotechnology Centre, National Dairy Research Institute, Karnal 132 001, IN
1 Animal Biotechnology Centre, National Dairy Research Institute, Karnal 132 001, IN
Source
Current Science, Vol 110, No 8 (2016), Pagination: 1411-1413Abstract
In most somatic cell nuclear transfer (SCNT) experiments, traditional skinderived fibroblast cells are commonly used as the donor genome. In addition, alternative sources of donor genome include those derived from hair follicles, colostrum/milk, blood and semen. Milk is easily obtained from live animals with out any biopsies and can be a safe mode of somatic cell source for those animals with high risk of bacterial infection. Therefore, milk-derived somatic cells may be an important source donor genome for the production of cloned embryos and for endangered species conservation programmes as part of genome resource banking. Recently, Golla et al.- Spermatogonial Stem-Cell Transplantation: An Alternative Approach For Transgenesis in Farm Animals
Abstract Views :270 |
PDF Views:90
Authors
Affiliations
1 Theriogenology Laboratory, Veterinary Gynaecology and Obstetrics, Southern Regional Station of ICAR National Dairy Research Institute, Bengaluru 560 030, IN
2 ICAR-National Dairy Research Institute, Karnal 132 001, IN
1 Theriogenology Laboratory, Veterinary Gynaecology and Obstetrics, Southern Regional Station of ICAR National Dairy Research Institute, Bengaluru 560 030, IN
2 ICAR-National Dairy Research Institute, Karnal 132 001, IN
Source
Current Science, Vol 120, No 2 (2021), Pagination: 260-261Abstract
Genetic modification of spermatogonial stem cells followed by their transplantation to homologous recipients has shown immense potential to complement the current methods being used for generating transgenic farm animals. Using this technique, the time duration required to generate transgenic founder animals can be reduced at least by half, which would significantly reduce the generation interval. However, significant efforts need to be made to improve the efficiency of transgenic offspring production for its successful implementation in large-scale production of therapeutic proteins for human use.
References
- Mehta, P. et al., Agric. Rev., 2017, 38, 129–136.
- Sharma, A. et al., Cell. Reprogram., 2019, 21, 1–10.
- Sharma, A. et al., Theriogenology, 2020, 142, 441–449.
- Honaramooz, A. and Yanfei, Y., Vet. Med. Int., 2011, 2011, 657860.
- Zeng, W. et al., Biol. Reprod., 2013, 88(1), 27-1.
- Izadyar, F. et al., Reproduction, 2003, 126, 765–774.
- Herrid, M. et al., Reprod. Fertil. Dev., 2019, 31(3), 538.
- Honaramooz, A. et al., Biol. Reprod., 2003, 69, 1260–1264.
- Buffalo calves from the semen of cloned bulls
Abstract Views :230 |
PDF Views:87
Authors
M. K. Singh
1,
N. L. Selokar
1,
S. Chand
1,
K. Patel
1,
S. S. Lathwal
1,
T. K. Mohanty
1,
M. S. Chauhan
1
Affiliations
1 Embryo Biotechnology Lab, Animal Biotechnology Centre, ICAR-National Dairy Research Institute, Karnal 132 001, India
1 Embryo Biotechnology Lab, Animal Biotechnology Centre, ICAR-National Dairy Research Institute, Karnal 132 001, India
Source
Current Science, Vol 123, No 3 (2022), Pagination: 253-253Abstract
No Abstract.- Ganga: India’s First Cloned Cow that belongs to Indigenous Gir Breed
Abstract Views :84 |
PDF Views:64
Authors
N. L. Selokar
1,
M. K. Singh
1,
S. S. Lathwal
1,
S. Chand
1,
R. Verma
1,
K. Patel
1,
G. Tripathi
1,
R. Meena
1,
M. S. Chauhan
1,
Ajay Aswal
2
Affiliations
1 ICAR-National Dairy Research Institute, Karnal 132 001, IN
2 Uttarakhand Livestock Development Board, Dehradun 248 001, IN
1 ICAR-National Dairy Research Institute, Karnal 132 001, IN
2 Uttarakhand Livestock Development Board, Dehradun 248 001, IN
Source
Current Science, Vol 125, No 1 (2023), Pagination: 10-10Abstract
No Abstract.Keywords
No Keywords.References
- Basic Animal Husbandry Statistics, Department of Animal Husbandry, Dairying and Fisheries (DADF) of India, 2022; http://dahd.nic.in
- Selokar et al., 2018; https://doi.org/10.1089/cell.2017.0051.
- National Dairy Plan, Department of Animal Husbandry, Dairying and Fisheries (DADF) of India; http://dahd.nic.in