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 GEP  Vol.5 No.8 , August 2017
Middle-Late Pleistocene Paleo-Climate and Paleo-Altimetry of the Centre of Tibetan Plateau Indicated by the Sporopollen Record of Well QZ-4
Abstract: The core sample from well QZ-4 is an important climate archive for the central Tibetan Plateau in the middle-late Pleistocene. In this work, a detailed pollen analysis of it is carried out to provide a preliminary insight into the paleo-climate and paleo-altimetry change in the central Tibetan Plateau. It can be concluded that the pollen assemblage can be obviously divided into two pollen zones, Pollen zone I (251.1 - 314 m in depth, 120.0 - 345.8 ka BP.) and Pollen zone II (200 - 251.1 m in depth, 105.4 - 120 ka BP.). The paleo-climate during pollen zone I deposition period was comparatively colder and wetter than it during the pollen zone II deposition period. After Gonghe Movement, the center of Tibetan Plateau was uplifted about 300 m (from 3500 - 3700 m to 3800 - 4000 m in elevation). The wind was changed from horizontal or downward direction to upward direction, in the study area. In the central of Tibetan Plateau, the climate change seems to be mainly driven by global climate change, and that tectonic uplift may have been a subordinate influence at the middle-late Pleistocene.
Cite this paper: He, J. , Wang, J. , Li, W. , Sun, W. (2017) Middle-Late Pleistocene Paleo-Climate and Paleo-Altimetry of the Centre of Tibetan Plateau Indicated by the Sporopollen Record of Well QZ-4. Journal of Geoscience and Environment Protection, 5, 148-165. doi: 10.4236/gep.2017.58013.
References

[1]   He, J., Wang, J., Fu, X., Zheng, C. and Chen, Y. (2012) Assessing the Conditions Favorable for the Occurrence of Gas Hydrate in the Tuonamu Area Qiangtang Basin, Qinghai–Tibetan, China. Energy Conversion and Management, 53, 11-18.

[2]   Zhang, X. and Yang, T. (2015) Environmental Impacts of Hydraulic Fracturing in Shale Gas Development in the United States. Petroleum Exploration and Development, 42, 876-883.

[3]   Hoorn, C., Straathof, J., Abels, H.A., Xu, Y., Utescher, T. and Dupont-Nivet, G. (2012) A Late Eocene Palynological Record of climate Change and Tibetan Plateau Uplift (Xining Basin, China). Palaeogeography, Palaeoclimatology, Palaeoecology, 344-345, 16-38.

[4]   Xiao, G., Guo, Z., Dupont-Nivet, G., Lu, H., Wu, N., Ge, J., Hao, Q., Peng, S., Li, F., Abels, H.A. and Zhang, K. (2012) Evidence for Northeastern Tibetan Plateau Uplift between 25 and 20Ma in the Sedimentary Archive of the Xining Basin, Northwestern China. Earth and Planetary Science Letters, 317-318, 185-195.

[5]   Li, S., Zhang, H., Shi, Y. and Zhu, Z. (2008) A High Resolution MIS 3 Environmental Change Record Derived from Lacustrine Depostit of Tianshuihai Lake, Qinghai-Tibet Plateau. Quaternary Sciences, 28, 122-131.

[6]   Yu, S., Zhu, Z., Li, S., Li, B., Zhou, H. and Sun, Y. (1997) Environmental Records of Variation of Iron Oxides in Drill Core from Tianshuihai Lake on the Southern Flanke of West Kunlun Mountains. Geochemica, 26, 88-98.

[7]   Yamamoto, K., Yamashita, F. and Adachi, M. (2005) Precise Determination of REE for Sedimentary Reference Rocks Issued by the Geological Survey of Japan. Geochemical Journal, 39, 289-297.

[8]   Dahl-Jensen, D., Albert, M.R., Aldahan, A., Azuma, N., Balslev-Clausen, D., Baumgartner, M., Berggren, A.-M., Bigler, M., Binder, T. and Blunier, T. (2013) Eemian Interglacial Reconstructed from a Greenland Folded Ice Core. Nature, 493, 489-494.
https://doi.org/10.1038/nature11789

[9]   Yi, H., Zhu, X. and Zhu, Y. (2006) Lake Level Change Recorded by Core of the Quaternary Lacustrine Sediment in the Central Tibetan Plateau and Its Climatic Implications. Earth Science Frontiers, 13, 300-307.

[10]   Li, J. (1991) The Environmental Effects of the Uplift of the Qinghai-Xizang Plateau. Quaternary Science Reviews, 10, 479-483.
https://doi.org/10.1016/0277-3791(91)90041-R

[11]   Qiao, Y., Qi, L., Liu, Z., Wang, Y., Yao, H., Yang, J. and Zhao, Z. (2014) Intensification of Aridity in the Eastern Margin of the Tibetan Plateau since 300 ka BP Inferred from Loess-Soil Sequences, Western Sichuan Province, Southwest China. Palaeogeography, Palaeoclimatology, Palaeoecology, 414, 192-199.
https://doi.org/10.1016/j.palaeo.2014.08.025

[12]   He, J., Wang, J., Sun, W., Zheng, C., Li, W., Guo, T. and Zeng, S. (2016) Geochemical Characteristics of Lake Clay Drilled in Well QZ-4: Its Implication for Geochemical Response to Climate Change in the Central Tibetan Plateau in the Middle-Late Pleistocene. Environmental Earth Sciences, 75, 1-14.
https://doi.org/10.1007/s12665-016-6119-y

[13]   Lu, H., Wu, N., Liu, K.-B., Zhu, L., Yang, X., Yao, T., Wang, L., Li, Q., Liu, X., Shen, C., Li, X., Tong, G. and Jiang, H. (2011) Modern Pollen Distributions in Qinghai-Tibetan Plateau and the Development of Transfer Functions for Reconstructing Holocene Environmental Changes. Quaternary Science Reviews, 30, 947-966.
https://doi.org/10.1016/j.quascirev.2011.01.008

[14]   Zhao, K., Li, X., Dodson, J., Atahan, P., Zhou, X. and Bertuch, F. (2012) Climatic Variations over the Last 4000 cal yr BP in the Western Margin of the Tarim Basin, Xinjiang, Reconstructed from Pollen Data. Palaeogeography, Palaeoclimatology, Palaeoecology, 321-322, 16-23.
https://doi.org/10.1016/j.palaeo.2012.01.012

[15]   Wu, F., Herrmann, M. and Fang, X. (2014) Early Pliocene Paleo-Altimetry of the Zanda Basin Indicated by a Sporopollen Record. Palaeogeography, Palaeoclimatology, Palaeoecology, 412, 261-268.
https://doi.org/10.1016/j.palaeo.2014.08.006

[16]   Xiao, X., Shen, J. and Wang, S. (2011) Spatial Variation of Modern Pollen from Surface Lake Sediments in Yunnan and Southwestern Sichuan Province, China. Review of Palaeobotany and Palynology, 165, 224-234.
https://doi.org/10.1016/j.revpalbo.2011.04.001

[17]   Li, Q., Ge, Q. and Tong, G. (2012) Modern Pollen-Vegetation Relationship Based on Discriminant Analysis across an Altitudinal Transect on Gongga Mountain, Eastern Tibetan Plateau. Chinese Science Bulletin, 57, 4600-4608.
https://doi.org/10.1007/s11434-012-5236-6

[18]   Cordova, C.E. (2007) Holocene Mediterranization of the Southern Crimean Vegetation: Paleoecological Records, Regional Climate Change and Possible Non-Climatic Influences. In: Yanko-Hombach, V., Gilbert, A.S., Panin, N. and Dolukhanov, P.M., Eds., The Black Sea Flood Question: Changes in Coastline, Climate and Human Settlement, Springer, Dordrecht, 319-344.
https://doi.org/10.1007/978-1-4020-5302-3_13

[19]   Good, R.E. and Good, N.F. (1975) Growth Characteristics of Two Populations of Pinus rigida Mill. from the Pine Barrens of New Jersey. Ecology, 56, 1215-1220.
https://doi.org/10.2307/1936162

[20]   Jaimand, K., Nejad, S., Monfared, A. and Akbarzadeh, M. (2014) Study of the Chemical Composition of Essential Oil of Teucrium chamaedrys at the Different Distillation in Mazandaran Province. Journal of Medicinal Plants and By-Products, 3, 193-198.

[21]   Li, Y., Sun, X., Zhao, X., Zhao, L., Xu, S., Gu, S., Zhang, G.F. and Yu, G. (2006) Seasonal Variations and Mechanism for Environmental Control of NEE of CO2 Concerning the Potentilla Fruticosa in Alpine Shrub Meadow of Qinghai-Tibet Plateau. Science in China Series D: Earth Sciences, 49, 174-185.
https://doi.org/10.1007/s11430-006-8174-9

[22]   Ji, S., Xingqi, L., Sumin, W. and Matsumoto, R. (2005) Palaeoclimatic Changes in the Qinghai Lake Area during the Last 18,000 Years. Quaternary International, 136, 131-140.
https://doi.org/10.1016/j.quaint.2004.11.014

[23]   Zhao, Y., Yu, Z., Chen, F., Liu, X. and Ito, E. (2008) Sensitive Response of Desert Vegetation to Moisture Change Based on a Near-Annual Resolution Pollen Record from Gahai Lake in the Qaidam Basin, Northwest China. Global and Planetary Change, 62, 107-114.
https://doi.org/10.1016/j.gloplacha.2007.12.003

[24]   Wafa’a, A., Al-Qarawi, A.A. and Alsubiee, M.S. (2010) Effect of Water Stress by Polyethylene Glycol 8000 and Sodium Chloride on Germination of Ephedra alata decne Seeds. Saudi Journal of Biological Sciences, 17, 253-257.
https://doi.org/10.1016/j.sjbs.2010.04.011

[25]   Zhang, J., Wu, B., Zhu, Y., Li, Y., Lu, Q. and Yao, B. (2013) Responses of Nitraria tangutorum to Water and Photosynthetic Physiology in Rain Enrichment Scenario. Acta Ecologica Sinica, 33, 172-177.
https://doi.org/10.1016/j.chnaes.2013.03.008

[26]   Gentry, A.H., Bullock, S., Mooney, H.A. and Medina, E. (1995) Seasonally Dry Tropical Forests. Cambridge University Press, Cambridge.

[27]   Fujii, R. and Sakai, H. (2002) Paleoclimatic Changes during the Last 2.5 myr Recorded in the Kathmandu Basin, Central Nepal Himalayas. Journal of Asian Earth Sciences, 20, 255-266.
https://doi.org/10.1016/S1367-9120(01)00048-7

[28]   Herzschuh, U. (2007) Reliability of Pollen Ratios for Environmental Reconstructions on the Tibetan Plateau. Journal of Biogeography, 34, 1265-1273.
https://doi.org/10.1111/j.1365-2699.2006.01680.x

[29]   Chuanhu, Z. and Xing, C. (2010) Climatological Significance of Pollen Factors Revealed by Pollen-Climate Response Surface Functions in Dajiuhu, Shennongjia. Journal of Meteorological Research, 24, 699-712.

[30]   Song, X.-Y., Spicer, R.A., Yang, J., Yao, Y.-F. and Li, C.-S. (2010) Pollen Evidence for an Eocene to Miocene Elevation of Central Southern Tibet Predating the Rise of the High Himalaya. Palaeogeography, Palaeoclimatology, Palaeoecology, 297, 159-168.
https://doi.org/10.1016/j.palaeo.2010.07.025

[31]   Xu, Q., Ding, L., Zhang, L., Cai, F., Lai, Q., Yang, D. and Liu-Zeng, J. (2013) Paleogene High Elevations in the Qiangtang Terrane, Central Tibetan Plateau. Earth and Planetary Science Letters, 362, 31-42.
https://doi.org/10.1016/j.epsl.2012.11.058

[32]   Sun, J., Xu, Q., Liu, W., Zhang, Z., Xue, L. and Zhao, P. (2014) Palynological Evidence for the Latest Oligocene-Early Miocene Paleoelevation Estimate in the Lunpola Basin, Central Tibet. Palaeogeography, Palaeoclimatology, Palaeoecology, 399, 21-30.
https://doi.org/10.1016/j.palaeo.2014.02.004

[33]   Xianhao, Z., Wenjing, Z. and Ji, L. (1999) The Characteristics of the Mountain Ecosystem and Environment in the Gongga Mountain Region. Joint Seminar on Ecosystem Research and Management in China, 28, 648-654.

[34]   Cheng, G. and Luo, J. (2001) Successional Features and Dynamic Simulation of Sub-Alpine Forest in the Gongga Mountain, China. Acta Ecologica Sinica, 22, 1049-1056.

[35]   Wang, X., Song, C., Wang, J., Miao, Y., Mao, R. and Song, Y. (2013) Carbon Release from Sphagnum Peat during Thawing in a Montane Area in China. Atmospheric Environment, 75, 77-82.
https://doi.org/10.1016/j.atmosenv.2013.04.056

[36]   Cai, Y., Zhang, H., Cheng, H., An, Z., Lawrence Edwards, R., Wang, X., Tan, L., Liang, F., Wang, J. and Kelly, M. (2012) The Holocene Indian Monsoon Variability over the Southern Tibetan Plateau and Its Teleconnections. Earth and Planetary Science Letters, 335, 135-144.
https://doi.org/10.1016/j.epsl.2012.04.035

[37]   Lu, H., Wu, N., Gu, Z., Guo, Z., Wang, L., Wu, H., Wang, G., Zhou, L., Han, J. and Liu, T. (2004) Distribution of Carbon Isotope Composition of Modern Soils on the Qinghai-Tibetan Plateau. Biogeochemistry, 70, 275-299.
https://doi.org/10.1023/B:BIOG.0000049343.48087.ac

[38]   Lu, C. (2014) Spatial Distributing Characteristics of Land Use in the Southern Slope of Mid-Himalaya Mountains. In: International Society for Optics and Photonics, SPIE Asia Pacific Remote Sensing, International Society for Optics and Photonics, Bellingham, 92604N-92604N-7.

[39]   Zhou, W., Yu, S.Y., Burr, G.S., Kukla, G.J., Jull, A., Xian, F., Xiao, J., Colman, S.M., Yu, H. and Liu, Z. (2010) Postglacial Changes in the Asian Summer Monsoon System: A Pollen Record from the Eastern Margin of the Tibetan Plateau. Boreas, 39, 528-539.

[40]   Zhou, S., Wang, X., Wang, J. and Xu, L. (2006) A Preliminary Study on Timing of the Oldest Pleistocene Glaciation in Qinghai-Tibetan Plateau. Quaternary International, 154, 44-51.
https://doi.org/10.1016/j.quaint.2006.02.002

[41]   Wu, Z., Zhao, X., Ye, P., Hu, D. and Zhou, C. (2007) Paleo-Elevation of the Tibetan Plateau Inferred from Carbon and Oxygen Isotopes of Lacustrine Deposits. Acta Geologica Sinica, 81, 1277-1288.

[42]   Vimeux, F.O., Cuffey, K.M. and Jouzel, J. (2002) New Insights into Southern Hemisphere Temperature Changes from Vostok Ice Cores Using Deuterium Excess Correction. Earth and Planetary Science Letters, 203, 829-843.
https://doi.org/10.1016/S0012-821X(02)00950-0

[43]   Yamamoto, Y., Kitahara, N. and Kano, M. (2012) Long Memory Effect of Past Climate Change in Vostok Ice Core Records. Thermochimica Acta, 532, 41-44.
https://doi.org/10.1016/j.tca.2011.11.033

[44]   Liu, D., Fang, X., Song, C., Dai, S., Zhang, T., Zhang, W., Miao, Y., Liu, Y. and Wang, J. (2010) Stratigraphic and Paleomagnetic Evidence of Mid-Pleistocene Rapid Deformation and Uplift of the NE Tibetan Plateau. Tectonophysics, 486, 108-119.
https://doi.org/10.1016/j.tecto.2010.01.014

[45]   Han, W., Fang, X. and Berger, A. (2012) Tibet Forcing of Mid-Pleistocene Synchronous Enhancement of East Asian Winter and Summer Monsoons Revealed by Chinese Loess Record. Quaternary Research, 78, 174-184.
https://doi.org/10.1016/j.yqres.2012.05.001

[46]   Ge, J., Dai, Y., Zhang, Z., Zhao, D., Li, Q., Zhang, Y., Yi, L., Wu, H., Oldfield, F. and Guo, Z. (2013) Major Changes in East Asian Climate in the Mid-Pliocene: Triggered by the Uplift of the Tibetan Plateau or Global Cooling? Journal of Asian Earth Sciences, 69, 48-59.
https://doi.org/10.1016/j.jseaes.2012.10.009

 
 
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