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Radial growth, present status and future prospects of west Himalayan fir (Abies pindrow Royle) growing in the moist temperate forest of Himalayan mountains of Pakistan

Author

Listed:
  • Zahid Rauf

    (Pakistan Forest Institute, Peshawar, Pakistan)

  • Adam Khan

    (Department of Botany, University of Lakki Marwat, Lakki Marwat, Pakistan)

  • Samina Siddiqui

    (National Centre of Excellence in Geology, University of Peshawar, Peshawar, Pakistan)

  • Sidra Saleem

    (Department of Botany, Abdul Wali Khan University Mardan, Mardan, Pakistan)

  • Tahir Iqbal

    (Pakistan Forest Institute, Peshawar, Pakistan)

  • Safdar Ali Shah

    (Pakistan Forest Institute, Peshawar, Pakistan)

  • Nowsherwan Zarif

    (Pakistan Forest Institute, Peshawar, Pakistan)

  • Wahiba Iqbal

    (Pakistan Forest Institute, Peshawar, Pakistan)

Abstract

Forests play a significant role for maintaining the biodiversity. In order to manage sustainable forests, tree species history, distribution, and their future prospects are vital. Using standardized quantitative approaches, the age, radial growth, and size class distribution of Abies pindrow (Himalayan fir) were determined from three different altitudinal sites (i.e. high, middle, and lower). The results indicate that Himalayan fir growing in the high-altitude site (Ayubia, 2 917 m a.s.l.) of moist temperate forests of the Himalayan mountains showed lower radial growth (0.13 cm) than in the middle (Bara Gali, 2 617 m a.s.l.; radial growth = 0.13 cm) and lower (Kuldana, 2 455 m a.s.l.; radial growth = 0.22 cm) altitude sites. Correlation analysis demonstrated that age showed a significant positive correlation (P < 0.001) with diameter at breast height. The tree-ring width chronology (totally 80 core samples) of Himalayan fir was developed from moist temperate forests of Himalayan mountains of Pakistan. At Ayubia site it possesses a long time-span (1703-2020 C.E.), followed by Bara Gali (1862-2020 C.E.) and Kuldana (1864-2020 C.E.). Further, the tree-ring width (TRW) chronology of Ayubia showed a significant positive correlation (P < 0.05) with May and June temperature, and a significant negative correlation (P < 0.05) with June and October precipitation, indicating that summer temperatures are the key factor for the radial growth of Himalayan fir. For the Kuldana site, the response of TRW chronology to temperature and precipitation was the same, however, it was significant only for June temperature at Bara Gali. The size class distribution of the high-altitude region (Ayubia) showed a higher number of individuals than the lower altitude region, indicating the lowest disturbance conditions. The absence of individuals in the early size classes and the gap in middle and mature size classes indicate a lower regeneration potential and anthropogenic impact. The pointer year analysis indicated that the Bara Gali forest is more sensitive to abnormal climate events than the other sites. Based on the present study, we suggest that proper attention and conservation strategy should be provided to Himalayan fir growing in the moist temperate forests of Pakistan.

Suggested Citation

  • Zahid Rauf & Adam Khan & Samina Siddiqui & Sidra Saleem & Tahir Iqbal & Safdar Ali Shah & Nowsherwan Zarif & Wahiba Iqbal, 2022. "Radial growth, present status and future prospects of west Himalayan fir (Abies pindrow Royle) growing in the moist temperate forest of Himalayan mountains of Pakistan," Journal of Forest Science, Czech Academy of Agricultural Sciences, vol. 68(9), pages 344-356.
  • Handle: RePEc:caa:jnljfs:v:68:y:2022:i:9:id:3-2022-jfs
    DOI: 10.17221/3/2022-JFS
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    References listed on IDEAS

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    1. J. Remeš & L. Bílek & J. Novák & Z. Vacek & S. Vacek & T. Putalová & L. Koubek, 2015. "Diameter increment of beech in relation to social position of trees, climate characteristics and thinning intensity," Journal of Forest Science, Czech Academy of Agricultural Sciences, vol. 61(10), pages 456-464.
    2. Kerstin S. Treydte & Gerhard H. Schleser & Gerhard Helle & David C. Frank & Matthias Winiger & Gerald H. Haug & Jan Esper, 2006. "The twentieth century was the wettest period in northern Pakistan over the past millennium," Nature, Nature, vol. 440(7088), pages 1179-1182, April.
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