Current Science

Open Access Open Access  Restricted Access Subscription Access

Treeline Migration and Settlement Recorded by Himalayan Pencil Cedar Tree-Rings in the Highest Alpine Zone of Western Himalaya, India


Affiliations
1 Birbal Sahni Institute of Palaeosciences, 53 University Road, Lucknow 226 007, India
2 Wadia Institute of Himalayan Geology, 33 GMS Road, Dehradun 248 001, India
 

Himalayan pencil cedar (Juniperus polycarpos) is an evergreen tree distributed from Afghanistan, Baluchistan, Kagan valley, Kashmir, Lahaul-Spiti to upper reaches of western Tibet1. Naturally, the lower and upper limit of a tree species over a specific region varies due to the ecological settings of the area. Recently it has been noted that due to global/ regional climatic changes there is marked change in distribution and composition of vegetation at its upper limit. Various studies from different parts of the globe indicate migration and shifting of treeline towards the higher altitudes2-15. Treeline migration/shifting have also been recorded from the Indian Himalaya by studying treeline dynamics over Uttarakhand- Himachal Pradesh16,17 and Sikkim18. Himalayan pencil cedar is known to grow generally at high altitudes with the highest treeline recorded from the forest of Juniperus tibetica at southeast Tibet (~4900 masl)19 and Juniperus sp. in Hunza-Karakorum (~3900 masl)20. Demarcation of the upper limit of treeline in complex mountainous terrains remains a challenging task.
User
Notifications
Font Size

  • Sahni, K. C., Gymnosperms of India and Adjacent Countries, Shiva Offset Press Dehradun, 1990.

  • Walther, G. R. et al., Nature, 2002, 416, 389–395.

  • Grace, J., Berninger, F. and Nagy, L., Ann. Bot., 2002, 90, 537–544.

  • Holtmeier, F. K., Mountain Timberlines: Ecology, Patchiness and Dynamics, Kluwer, Dordrecht, The Netherlands, 2003.

  • Holtmeier, F. K. and Broil, G., Glob. Ecol. Biogeogr., 2005, 14, 395–410.

  • Holtmeier, F. K. and Broil, G., Landsc. Online, 2007, 1, 1–33.

  • Malanson, G. P. et al., Phys. Geogr., 2007, 28, 378–396.

  • Beckage, B. et al., Proc. Natl. Acad. Sci., 2008, 105, 4197–4202.

  • Harsch, M., Hulme, P. E., McGlone, M. S. and Duncan, R. P., Ecol. Lett., 2009, 12, 1040–1049.

  • Hofgaard, A., Dalen, L. and Hytteborn, H., J. Veget. Sci., 2009, 20, 1133– 1144.

  • Kullman, L., Ambio, 2010, 39, 159–169.

  • Liang, E., Wang, Y., Eckstein, D. and Luo, T., New Phytol., 2011, 190, 760– 769.

  • Körner C., Alpine Treelines: Functional Ecology of the Global High Elevation Tree Limits, Springer, Basel, 2012.

  • Shrestha, K. B., Hofgaard, A. and Vandvik, V., J. Plant. Ecol., 2015, 8, 347– 358.

  • Liang, E. et al., Proc. Natl. Acad. Sci. USA, 2016, 113, 4380–4385; doi: 10.1073/pnas.1520582113.

  • Dubey, B., Yadav, R. R., Singh, J. and Chaturvedi, R., Curr. Sci., 2003, 85, 1135–1136.

  • Yadava, A. K. et al., Quat. Int., 2017, 444, 44–52.

  • Telwala, Y., Brook, B. W., Manish, K. and Pandit, M. K., PLoS One, 2013, 8, 1–8.

  • Miehe, G., Miehe, S., Vogel, J., Co, S. and Duo, L., Mt. Res. Dev., 2007, 27, 169–173.

  • Esper, J., Holocene, 2000, 10, 253– 260.

  • Stokes, M. A. and Smiley, T. L., An Introduction to Tree-Ring Dating, University of Chicago, Press, Chicago, 1968.

  • Fritts, H. C., Tree-Rings and Climate, Academic Press, London, 1976, p. 567.

  • Holmes, R. L., Tree-Ring Bull., 1983, 43, 69–78.

  • Rinn, F., TSAP-Win time series analysis and presentation for dendrochronology and related applications, version 0.53 for Microsoft Windows. Rinn Tech, Heidelberg, Germany, 1996, p. 110.

  • Cook, E. R., Ph D thesis, University of Arizona, Tucson, AZ, 1985, p. 171.

  • Cook, E. R. and Peters, K., Holocene, 1997, 7, 361–370.

  • Wigley, T. M. L., Briffa, K. R. and Jones, P. D., J. Clim. Appl. Meteorol., 1984, 23, 201–213.

  • Biondi, F. and Waikul, K., Comput. Geosci., 2004, 30, 303–311.


Abstract Views: 546

PDF Views: 168




  • Treeline Migration and Settlement Recorded by Himalayan Pencil Cedar Tree-Rings in the Highest Alpine Zone of Western Himalaya, India

Abstract Views: 546  |  PDF Views: 168

Authors

Krishna G. Misra
Birbal Sahni Institute of Palaeosciences, 53 University Road, Lucknow 226 007, India
Vikram Singh
Birbal Sahni Institute of Palaeosciences, 53 University Road, Lucknow 226 007, India
Akhilesh K. Yadava
Birbal Sahni Institute of Palaeosciences, 53 University Road, Lucknow 226 007, India
Sandhya Misra
Birbal Sahni Institute of Palaeosciences, 53 University Road, Lucknow 226 007, India
Ram R. Yadav
Wadia Institute of Himalayan Geology, 33 GMS Road, Dehradun 248 001, India

Abstract


Himalayan pencil cedar (Juniperus polycarpos) is an evergreen tree distributed from Afghanistan, Baluchistan, Kagan valley, Kashmir, Lahaul-Spiti to upper reaches of western Tibet1. Naturally, the lower and upper limit of a tree species over a specific region varies due to the ecological settings of the area. Recently it has been noted that due to global/ regional climatic changes there is marked change in distribution and composition of vegetation at its upper limit. Various studies from different parts of the globe indicate migration and shifting of treeline towards the higher altitudes2-15. Treeline migration/shifting have also been recorded from the Indian Himalaya by studying treeline dynamics over Uttarakhand- Himachal Pradesh16,17 and Sikkim18. Himalayan pencil cedar is known to grow generally at high altitudes with the highest treeline recorded from the forest of Juniperus tibetica at southeast Tibet (~4900 masl)19 and Juniperus sp. in Hunza-Karakorum (~3900 masl)20. Demarcation of the upper limit of treeline in complex mountainous terrains remains a challenging task.

References





DOI: https://doi.org/10.18520/cs%2Fv118%2Fi2%2F192-195