Main Article Content

Abstract

Baropal wetland is situated near to the Baropal village, Pilibanga tehsil of Hanumangarh District in Rajasthan state (290 22’ 10” North, 740 05’ 48” East) and comes under the Ghaggar river floodplain. Baropal wetland is a recently and naturally originated water body, presumably recharged by the seepage water of Ghaggar river and Indira Gandhi Canal Project (IGNP). It is a real example of rapid succession and species aggregation in the barren land and has been established as a rich biodiversity amphitheatre within the semi-desert region. The vegetation cover of Baropal wetland stretch has changed into Xerophytic to Mesophytic and Hydrophytic. As, it has established enormous plant and animal communities in a short period, in the present picture, the plant communities of Baropal wetland are much productive to support enough food and habitat to a variety of organisms. Unfortunately, Baropal wetland has not received any ecological attention despite being a water body and always ignored due to the inadequacy in the number of the well-established local researchers. Its beauty has always been superimposed by the fascinating archaeological sites which are present in the same locality (Ghaggar floodplain) and by the Ghaggar and Saraswati debate.

Keywords

Baropal wetland Ecological heterogeneity Ghaggar river Indira Gandhi Canal Project (IGNP)

Article Details

How to Cite
Malhotra, G., & Madan, J. . (2020). Origin and ecological heterogeneity of Baropal wetland: A Review. Environment Conservation Journal, 21(3), 165–170. https://doi.org/10.36953/ECJ.2020.21320

References

  1. Chatterjee, A. and Ray, J. S. 2018. Geochemistry of Harappan potteries from Kalibangan and sediments in the Ghaggar River: Clues for a dying river. Geoscience Frontiers, 9(4): 1203-1211.
  2. Dwivedi, R. S. and Sreenivas, K. 2002. The vegetation and waterlogging dynamics as derived from spaceborne multispectral and multitemporal data, International Journal of Remote Sensing, 23(14): 2729-2740.
  3. Garg, D. and Soni, A. K. 2016. Seasonal Variations of Physico- Chemical Characteristics of Badopal Wetland (Water Logged Area), Hanumangarh District, North Rajasthan, India. Remarking an Analisation, 1(8): 9-13.
  4. Gogi, S. 2002. Flamingoes of Baropal Lake. The Tribune, 24 March 2002. p.21.
  5. Keddy, P. 2010. Wetlands: An overview. In Wetland Ecology: Principles and Conservation (pp. 1-41). Cambridge: Cambridge University Press.
  6. Kenoyer, J. M. 1991. The Indus valley tradition of Pakistan and western India. Journal of World Prehistory, 5(4): 331-385.
  7. Kundu, S. 2012. Assessment of surface water quality for drinking and irrigation purposes: a case study of Ghaggar River system surface waters. Bulletin of Environment, Pharmacology & Life Sciences, 1(2): 1-1.
  8. Maemoku, H., Shitaoka, Y., Nagatomo, T. and Yagi, H. 2012. Geomorphological constraints on the Ghaggar River regime during the Mature Harappan period, in Climates, Landscapes, and Civilizations, Geophys. Monogr. Ser., vol. 198, edited by L. Giosan et al., 97–106, AGU, Washington, D. C.
  9. Malhotra, G. S., Kapoor, N. and Saxena, M. M. 2019. Spider diversity and abundance in different habitats of Upper-Northern Rajasthan, ESSENCE- International Journal for Environmental Rehabilitation and Conservation, 10(1): 1-14.
  10. Mamatamayee, C. 1991. Pioneers of the Settlement at Kalibangan. Journal of Human Ecology, 2(2), 159-164.
  11. Miller, D. 1985. Ideology and the Harappan civilization. Journal of Anthropological Archaeology, 4(1): 34-71.
  12. Mirande, C. M. and Harris, J. T. 2019. Crane Conservation Strategy. International Crane Foundation, Baraboo, WI.
  13. Mishra D. C. and Mallick, K. 2008. Paleochannels and settlements of Harappan period in kalibangan, Rajasthan based on geophysical investigations, Current Science, 95(12): 1657-1658.
  14. Moharana, P. C. 2012. Types, distribution and morphology of aeolian bedforms in canal-irrigated region of arid western Rajasthan. Journal of Indian Geomorphology, 1: 1-7.
  15. Ramakrishnan, M. and Vaidyanadhan, R. 2010. Geology of India (Vol. 1 & 2). GSI Publications, 2(1).
  16. Rao, A. S. 2009. Climate and microclimate changes influencing the fauna of the hot Indian arid zone. In Faunal ecology and conservation of the Great Indian Desert (pp. 13-23). Springer, Berlin, Heidelberg.
  17. Roy, M. M., Yadava, N. D., Soni, M. L. and Tewari, J. C. 2016. Combating Waterlogging in IGNP Areas in Thar Desert (India): Case Studies on Biodrainage. In Agroforestry for the Management of Waterlogged Saline Soils and Poor-Quality Waters (pp. 109-120). Springer, New Delhi.
  18. Sankaran, A.V. 1999. Saraswati- the ancient river lost in the desert. Current science, 77(8): 1054-1060.
  19. Sharma, R. C. and Gaur, S. 2005. Changing ecology and faunal diversity of amphibians and reptiles in the Thar Desert of Rajasthan, India. Changing Faunal Ecology in the Thar Desert, Kumar Scientific Publishers, Jodhpur, 149-171.
  20. Singh, B.P., 1995. Impact of canal irrigation on the natural flora of Rajasthan. Rheedea, 5: 90-92.
  21. Sinha-Roy, S., Malhotra, G. and Mohanty, M. 1998. Geology of Rajasthan. Geological Society of India.
  22. Sivaperuman C. and Baqri Q. H. 2009. Avifaunal Diversity in the IGNP Canal Area, Rajasthan, India. In: Sivaperuman C., Baqri Q.H., Ramaswamy G., Naseema M. (eds) Faunal Ecology and Conservation of the Great Indian Desert. Springer, Berlin, Heidelberg.
  23. Su, M., Zheng, Y., Hao, Y., Chen, Q., Chen, S., Chen, Z. and Xie, H. 2018. The influence of landscape pattern on the risk of urban water-logging and flood disaster. Ecological Indicators, 92: 133-140.
  24. Thapar, B. K. 1975. Kalibangan: a Harappan metropolis beyond the Indus Valley. Expedition, 17(2): 19.
  25. Tiner, R. W. 2016. Wetland indicators: A guide to wetland formation, identification, delineation, classification, and mapping. CRC Press.
  26. Tripathi, J. K., Bock, B., Rajamani, V. and Eisenhauer, A. 2004. Is river Ghaggar, Saraswati? Geochemical constraints. Current Science, 87: 1141–1145.