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Dendrochronological potential of Ephedra equisetina from Zaravshan Mountains (Tajikistan) in climate change studies

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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Samples from Mongolian Ephedra (Ephedra equisetina Bunge) was collected in the Zaravshan Mountains (the Fann Mountains), Tajikistan. The wood of Ephedra is ring-porous with well-defined growth rings. Annual ring widths were measured, individual series were first cross-dated and then averaged as a standard chronology. Correlations were calculated between the standard ring-width chronology and monthly climate data recorded in the weather station Iskanderkul. Dendroclimatological analysis showed that July temperature is the growth limiting factor of this species. Our study has shown high dendrochronological potential of Ephedra.
Wydawca
Rocznik
Strony
48--52
Opis fizyczny
Bibliogr. 25 poz., wykr.
Twórcy
autor
  • Faculty of Earth Science, University of Silesia, Bedzinska Str. 60, 41-200 Sosnowiec
  • Faculty of Earth Science, University of Silesia, Bedzinska Str. 60, 41-200 Sosnowiec
autor
  • Faculty of Earth Science, University of Silesia, Bedzinska Str. 60, 41-200 Sosnowiec
Bibliografia
  • 1. Au R., Tardif J.C. (2007) Allometric relationships and dendroecology of the dwarf shrub Dryas integrifolia near Churchill, subarctic Manitoba. Canadian Journal of Botany 85, 585–597.
  • 2. Bär A., Bräuning A., Löffler J. (2007) Ringwidth chronologies of the alpine dwarf shrub Empetrum hermaphroditum from the Norwegian mountains. IAWA Journal 28, 325–338.
  • 3. Biondi F., Waikul K. (2004) DendroClim2002: A C ++ program for statistical calibration of climate signals in tree-ring chronologies. Computers and Geosciences 30, 303–311.
  • 4. Carlquist S. (1992) Wood, bark, and pith anatomy of old world species of Ephedra and summary for the genus, ALISO 13(2), 255-295.
  • 5. Chen F., Yuan Y., Wei W., Wang L., Yu S., Zhang R., Fan Z., Shang H., Zhang T., Li Y. (2012) Tree ring density-based summer temperature reconstruction for Zajsan Lake area, East Kazakhstan, Int. J. Climatol. 32, 1089–1097.
  • 6. Cook E. R, Holmes R (1999) Users manual for Program ARSTAN. Laboratory of Tree-Ring Research, University of Arizona, Tucson
  • 7. Cook E.R., Kairiukstis L.A. (eds.) (1990) Methods of dendrochronology: applications in the environmental sciences. Dordrecht: Kluwer Academic Publishers.
  • 8. Liguo F., Yong-fu Y., Riedl H. (1999) Ephedraceae. (In:) Zheng-yi W., Raven P.H. (eds.). Flora of China, Volume 4. Beijing: Science Press; St. Louis: Missouri Botanical Garden.
  • 9. Holmes RL. (1983) Computer-assisted quality control in tree-ring dating and measurement. Tree-Ring Bulletin 43, 69–78.
  • 10. Makhmadaliev B., Kayumov A., Novikov V., Mustaeva N., Rajabov I. (2008) The Second National Communication of the Republic of Tajikistan under the United Nations Framework Convention on Climate Change, Dushanbe
  • 11. Liang E.Y., Eckstein D. (2009) Dendrochronological potential of the alpine shrub Rhododendron nivale on the south-eastern Tibetan Plateau. Annals of Botany 104, 665–670.
  • 12. Liang E.Y., Lu X., Ren P., Li X., Zhu L., Eckstein D. (2012) Annual increments of juniper dwarf shrubs above the tree line on the central Tibetan Plateau: a useful climatic proxy, Annals of Botany 109: 721–728.
  • 13. Liang E.Y., Shao X.M., Qin N.S. (2008) Treering based summer temperature reconstruction for the source region of the Yangtze River on the Tibetan Plateau. Global and Planetary Change 61, 313–320.
  • 14. Lydolph P.E. (ed.) (1977) Climates of the Soviet Union, World Survey of Climatology Volume 7, Amsterdam-Oxford – New York, 1-441.
  • 15. Owczarek, P. (2009) Dendrogeomorphological potential of Salicaceae from SW Spitsbergen, Svalbard. (In:) Kaczka, R., Malik, I., Owczarek, P., Gartner, H., Helle, G. & Heinrich, I. (eds.): TRACE –Tree Rings in Archaeology, Climatology and Ecology, Vol. 7. GFZ Potsdam. – Sci. Tech. Rep. STR 09/03, 181–186.
  • 16. Owczarek P., Latocha A., Wistuba M., Malik I., (2013) Reconstruction of modern debris flow activity in the arctic environment with the use of dwarf shrubs (south-western Spitsbergen) – a new dendrochronological approach, Zeitschrift für Geomorphologie Vol. 57 (2013), Suppl. 3, 075-095.
  • 17. Rinn F. (2010) TSAP – reference manual. Frank Rinn, Heidelberg.
  • 18. Sass-Klaassen U., Couralet C., Sahle Y., Sterck F.J. (2008) Juniper from Ethiopia contains a large-scale precipitation signal. International Journal of Plant Sciences 169, 1057–1065.
  • 19. Schmidt N.M., Baittinger C., Forchhammer M.C. (2006) Reconstructing century-long snow regimes using estimates of high arctic Salix arctica radial growth. Arctic, Antarctic, and Alpine Research 38: 257–262.
  • 20. Earl J.C. (ed.) (2013) The Gymnosperm Database, http://www.conifers.org/ep/Ephedraceae.php.
  • 21. Williams M. W., Konovalov V. G. (2008) Central Asia temperature and precipitation data, 1879–2003. Boulder, Colorado: USA National Snow and Ice Data Center.
  • 22. Woodcock H., Bradley R.S. (1994) Salix arctica (Pall.): its potential for dendroclimatological studies in the high arctic. Dendrochronologia 12: 11–22.
  • 23. Xiao S.C., Xiao H.L., Kobayashi O., Liu P.X. (2007) Dendroclimatological investigations of sea buckthorn (Hippophae rhamnoides) and reconstruction of the equilibrium line altitude of the July First Glacier in the Western Qilian mountains, northwestern China. Tree-Ring Research 63: 15–26.
  • 24. Zalatan R., Gajewski K. (2006) Dendrochronological potential of Salix alaxensis from the Kuujjua river area, Western Canadian arctic. Tree-Ring Research 62, 75–82.
  • 25. Zheng Y.H., Liang E.Y., Shao X.M., Zhu H.F. (2008) Radial growth characteristic of Qilian Juniper and it’s response to climatic change at different environments. Journal of Beijing Forestry University 30, 7–12.
Uwagi
Opracowanie ze środków MNiSW w ramach umowy 812/P-DUN/2016 na działalność upowszechniającą naukę.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-d9c4e8ca-700b-4eea-8392-ea360b7e568a
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