Paleoclimate modeling and identification of anthropogenic effects in high Zagros Mountains

Document Type : علمی - پژوهشی

Authors

1 Faculty of Earth Sciences, University of Shahid Beheshti

2 2 Institute of Earth Sciences, Geoogical Survey of Iran, Tehran

3 Institute of applied Sciences, Geoogical Survey of Iran, Tehran, Karaj

4 University of Goettingen, Germany

5 University of Payamnoor, Yasouj

6 Faculty of Geography, University of Tehran

Abstract

Abstract: In this research we tried to investigate the respond of high part of Zagros Mountains to past climate change by studying a 300cm core was extracted from Lake Gahar. This region is as an important biome of oak forest of Iran. Then the aim of this investigation is to detect past climate condition by palynology and modeling. According to the pollen percentage diagram of Lake Gahar (Fig. 3, 4, 5), four main local pollen assemblage zones consisting of two older zones GHA(depth of 300 to 210 cm), GHB (210 to 65 cm depth) and two more new zones GHC (depth 65 to 30 cm) and GHD (depth 30 to 0 cm) were identified. For interpretation the pollen diagram we reconstructed the annual mean precipitation and temperature data over 40000 years by MCM (Macrophysical Climate Model). By calculation the Z-score index four major thermal and moisture period found in Gahar region: 1- Cold and dry period (40000-30000 Yr. B.P) 2- Warm and dry period (30000-20000Yr. B.P) 3- Cold and wet period (20000-11900 Yr. B.P) and 4- Warm and dry period (11900-now Yr. B.P). The indices and our data showed that two zones GHA and GHB beyond depth 300-60cm may have been exposed to cold and wet period around 20000-11900 Years B.P..The mentioned zones have vegetation of forest- steppe with dominant species of oak trees. It seems that the disappearing of arboreal pollen, especially Quercus at a depth of 50 and 60 cm at the boundary between the two zones GHB and GHC is associated with unfavorable conditions for plant growth during the last glacial period. There are also upland herbs pollen types such as Poaceae crealia types and polygonium, and also arboreal pollen such as Corylus, Juglans, olive and Vitis can be considered as evidence of the destruction of the region as a result of anthropogenic effects and heavy grazing and farming operations. It is approved that consecutive period of cold/wet and warm/dry period in the past climate of Gahar region by comparing the results with other lakes in the north west of Iran.

Keywords


  1. Cuffey K M, Clow G D. Temperature, accumulation, and ice sheet elevation in central Greenland through the last deglacial transition. Journal of Geophysical Research; 1997; 102: 26383-26396.
  2. Alley R B, Mayewski P A, Sowers T, Stuiver M, Taylor K C and Clark P U. Holocene climatic instability: A prominent, widespread event 8,200 years ago. Geology; 1997; 25: 483-486.
  3. Van Zeist W, Bottema, S. Palynological investigations in Iran. Palaeohistoria ; 1977 ; 19, 19-85.
  4. Van Zeist W, Wright H E. Preliminary pollen studies at Lake Zeribar, science; 1963; 140, 65-67.
  5. Wasylikowa K, Witkowski A. Diatom Monographs. The palaeoecology of Lake Zeribar and surrounding areas; Western Iran; during the last 48000 years. A.R.G. Gantner Verlag K.G. Koeltz Science books; 2008 :8 Germany, ISBN-13978-3-906166-55-1.
  6. Djamali M, Akhani H, Andrieu-Ponel V, Braconnot P, Brewer S, de Beaulieu J L, Fleitmann D, Fleury J, Gass F, Guibal F, Jackson S T, Lezine A M, Medail M, Ponel P, Roberts N and Stevens L. Indian Summer Monsoon variations could have affected the early Holocene woodland expantion in the Near East. The Holocene; 2010; 20: 5: 153: 813–820.
  7. Nabavi M H. The first overview on origin of Lake Gahar: Oshtorankuh in Lorestan Province. Iran. Iranian Geological Survey; 1986; [in Persian].
  8. Zohary M, Majnounian(translator). The geobotanical structure of Iran,Dayereh sabz publication. first pub; 2005. 87,[ in Persian].
  9. Lashanizand M, Parvaneh B. Regionalization of climate in Lorestan Province. Journal of Physical Geography.4th year; 2000; N.11. Spring. 23-45. [Persian].
  10. Hasanvand Z. Synoptic and thermodynamic analysis of heavy precipitation in Lorestan Province. Master Thesis. Climatology. Shahid Beheshti University. Tehran, Iran; 2015.143 [in Persian].
  11. Djamali M, Akhani H, Khoshravesh R, Andrieu-Ponel V, Ponel P, Brewer S. Application of global bioclimatic classification to Iran: implications for understanding the modern vegetation and biogeography, Ecol. Mediterranean; 2011; 37: 91–114.
  12. Beug H J. Atlas: Leitfaden der Pollenbestimmung fur Mitteleuropa und angrenzende Gebiete. published by verlag Dr Friedrich pfeil. ISBN 3-89937-043-0. Gottingen; 2004.p.586.
  13. a] [19a] Reille M. Pollen et Spores D’Europe et D’Afrique du Nord, Laboratoire de Botanique historique et Palynologie. Marseille. France ; 1992 ; ISBN 2-9507175-0-0.
  14. b] [19b] Reille M. Pollen et Spores D’Europe et D’Afrique du Nord. Laboratoire de Botanique historique et Palynologie,BOITE 451. 13397 Marseille cedex 20. France ;1995 ; Supplement 1.
  15. c] [19c] Reille M. Pollen et Spores D’Europe et D’Afrique du Nord. Laboratoire de Botanique historique et Palynologie. BOITE 451. 13397 Marseille cedex 20. France ; 1998 ;Supplement 2.
  16. Grimm EC. CONISS: a Fortran 77 program for stratigraphically contrained cluster analysis by the method of the incremental sum of squares. Comp Geosci;1987. 13:13–35
  17. Bryson R A. Modelling the NW India Monsoon for the Last 40000 Years. Climate Dynamics;1989; 3: 169-177.
  18. El-Moslimany A P. The Late Pleistocene climates of the Lake Zeribar region.Vegetation. Dr W. Junk Publishers. Dordrecht - Printed in the Netherlands; 1987; 72: 131-139.
  19. Rull V. A note on pollen counting in palaeoecology. I.V.I.C. Centro de Ecologia y Ciencias Ambientales. Apartado 21827 ; 1987 ; Caracas 1020-A.Venezuela .
  20. Bottema S, Woldring H. Anthropogenic indicators in the pollen diagrams of the Eastern Mediterranean. In: Bottema S, EntjesNieborg G, van Zeist W (eds) Man’s role in the shaping of the Eastern Mediterranean landscape. Balkema. Rotterdam; 1990; 231–264.
  21. Djamali M, De Beaulieu J L, Miller N, Andrieu-Ponel V, Berberian M, Gandouin E, Lahijani H, Ponel P, Salimian M, and Guiter F. A late Holocene pollen record from Lake Almalou in NW Iran: evidence for changing land-use in relation to some historical events during the last 3700 years, J Archaeol Sci ; 2009 ;36:1. 346–1.375.
  22. Djamali M, Jones M D, Migliore M, Balatti S, Fader M, Contreras D, Gondet S, Hosseini Z, Lahijani H, Naderi A, Shumilovskikh L S, Tengberg M, and Weeks L. Olive cultivation in the heart of the Persian Achaemenid Empire:new insights into agricultural practices and environmental changes reflected in a late Holocene pollen record from Lake Parishan, SW Iran. Vegetation History Archeobot; 2015; DOI 10.1007/s00334-015-0545-8.
  23. Stevens L R, Wright Jr HE, Ito E. Proposed changes in seasolality of climate during the Lateglacial and Holocene at Lake Zeribar. Iran. Holocene ;2001 ; 11 : 747-755.
  24. Moore P D, Webb JA, and Collinson M E. Pollen Analysis. Second edition. Oxford: Blackwell;1991. 633.