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Relationships between loess and the Silk Road reflected by environmental change and its implications for human societies in the area of ancient Panjikent, central Asia

Published online by Cambridge University Press:  05 October 2017

Piotr Owczarek*
Affiliation:
Institute of Geography and Regional Development, Faculty of Earth Sciences and Environmental Management, University of Wroclaw, Pl. Uniwersytecki 1, 50-137 Wroclaw, Poland
Magdalena Opała-Owczarek
Affiliation:
Department of Climatology, Faculty of Earth Sciences, University of Silesia in Katowice, ul. Będzińska 60, 41-200 Sosnowiec, Poland
Oimahmad Rahmonov
Affiliation:
Department of Physical Geography, Faculty of Earth Sciences, University of Silesia in Katowice, ul. Będzińska 60, 41-200 Sosnowiec, Poland
Abdurauf Razzokov
Affiliation:
Academy of Sciences of Tajikistan, Historical and Archaeological Reserve of Sarazm, Penjikent Archaeological Base, 102 Rudaki Street, Penjikent, Tajikistan
Zdzisław Jary
Affiliation:
Institute of Geography and Regional Development, Faculty of Earth Sciences and Environmental Management, University of Wroclaw, Pl. Uniwersytecki 1, 50-137 Wroclaw, Poland
Tadeusz Niedźwiedź
Affiliation:
Department of Climatology, Faculty of Earth Sciences, University of Silesia in Katowice, ul. Będzińska 60, 41-200 Sosnowiec, Poland
*
*Corresponding author at: Institute of Geography and Regional Development, Faculty of Earth Sciences and Environmental Management, University of Wroclaw, Pl. Uniwersytecki 1, 50-137 Wroclaw, Poland. E-mail address: piotr.owczarek@uwr.edu.pl (P. Owczarek).

Abstract

Rich ancient societies of central Asia developed on the basis of trade between East and West; their existence was dependent on natural resources that favoured agriculture. The branches of the Silk Road in central Asia clearly coincide with loess areas, where many settlements were erected based on the presence of fertile loess soil and water. The aim of the study was to analyse the environmental factors that led to the growth and decline of one of the most important Silk Road “loess towns,” ancient Panjikent, as an example of human and climatic impacts on landscape changes. The town, established in the fifth century, quickly became one of the most important cities of Sogdiana. Local loess material was used for the production of the sun-dried bricks. Rapid population growth led to deforestation and consequently increased the intensity of erosion rates and reductions in cultivation area. A period of drought near the end of the first millennium AD influenced the final abandonment of the ancient town and its relocation to the lower terrace of the Zarafshan River. A decline in natural and agricultural resources and subsequently climatic forces caused a decline in the number of cities in semiarid regions of central Asia.

Type
Research Article
Copyright
Copyright © University of Washington. Published by Cambridge University Press, 2017 

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References

REFERENCES

Baumer, C., 2014. The History of Central Asia: The Age of the Silk Roads. Tauris, London.Google Scholar
Beckwith, C.I., 2011. Empires of the Silk Road: A History of Central Eurasia from the Bronze Age to the Present. Princeton University Press, Princeton, NJ.Google Scholar
Belenitskii, A.M., Marshak, B.I., Raspopova, V.I., 1979. Social structure of the population of ancient Panjikant. [In Russian.]. In: Gafurov, B., Girs, G.F., Davidovich E.A. (Eds.), Commodity-Money Relations in Near and Middle East in Medieval Time. Institute of Oriental Studies, Academy of Sciences of the USSR, Nauka, Moscow, pp. 1926.Google Scholar
Belenitskii, A.M., Marshak, B.I., Raspopova, V.I., 1981. The Sogdian city at the beginning of the Middle Ages: results and methods of the study of ancient Panjikent. [In Russian.] Soviet Archaeology 2: 94110.Google Scholar
Bloom, J.M., Blair, S.S., 2009. The Grove Encyclopedia of Islamic Art & Architecture. Oxford University Press, Oxford.Google Scholar
Bogolyubov, M., Smirnova, O., 1963. Economic Documents [In Russian.] In: Sogdian Documents from Mount Mōḡ 3. Oriental Literature Publishing House, Moscow.Google Scholar
Bronger, A., 2003. Correlation of loess–paleosol sequences in East and Central Asia with SE Central Europe: towards a continental Quaternary pedostratigraphy and paleoclimatic history. Quaternary International 106–107: 1131.Google Scholar
Bronger, A., Winter, R., Derevjanko, O., Aldag, S., 1995. Loess–palaeosol sequences in Tadjikistan as a palaeoclimatic record of the Quaternary in Central Asia. Quaternary Proceedings 4: 6981.Google Scholar
Bronger, A., Winter, R., Heinkele, T., 1998. Pleistocene climatic history of East and Central Asia based on paleopedological indicators of loess–paleosol sequences. Catena 34: 117.Google Scholar
Büntgen, U., Tegel, W., Nicolussi, K., McCormick, M., Frank, D., Trouet, V., Kaplan, J.O., 2011. 2500 Years of European climate variability and human susceptibility. Science 331: 578582.CrossRefGoogle ScholarPubMed
Chen, F.H., Chen, J.H., Holmes, J., Boomer, I., Austin, P., Gates, J.B., Wang, N.L., Brooks, S.J., Zhang, J.W., 2010. Moisture changes over the last millennium in arid central Asia: a review, synthesis and comparison with monsoon region. Quaternary Science Reviews 29: 10551068.Google Scholar
Chen, F.H., Shi, Q., Wang, J.M., 1999. Environmental changes documented by sedimentation of Lake Yiema in arid China since the late glaciation. Journal of Paleolimnology 22: 159169.Google Scholar
Dani, A.H., Masson, V.M. (Eds.), 1992. History of Civilizations of Central Asia. Vol. 1, The Dawn of Civilization: Earliest Times to 700 B.C. UNESCO, Paris.Google Scholar
deMenocal, P.B., 2001. Cultural responses to climate change during the Late Holocene. Science 292: 667673.Google Scholar
Derbyshire, E., 2001. Geological hazards in loess terrain, with particular reference to the loess regions of China. Earth-Science Reviews 54: 231260.Google Scholar
Ding, Z.L., Ranov, V., Yang, S.L., Finaev, A., Han, J.M., Wang, G.A., 2002. The loess record in southern Tajikistan and correlation with Chinese loess. Earth and Planetary Science Letters 200: 387400.Google Scholar
Dodonov, A.E., 1987. Stratigraphy and paleogeography of loess in Middle Asia. Annales Universitatis Mariae Curie-Skłodowska, Section B 41: 114.Google Scholar
Dodonov, A.E., 1991. Loess of Central Asia. GeoJournal 24: 185194.CrossRefGoogle Scholar
Dodonov, A.E., 2002. Quaternary of Middle Asia: Stratigraphy, Correlation, Paleogeography. [In Russian.] GEOS. Moscow.Google Scholar
Dodonov, A.E., 2007. Loess records: Central Asia. In: Elias, S.A. (Ed.), The Encyclopedia of Quaternary Sciences. Elsevier, Amsterdam, pp. 14181429.Google Scholar
Dodonov, A.E., Zhou, L., 2008. Loess deposition in Asia: its initiation and development before and during the Quaternary. Episodes 31: 222225.CrossRefGoogle Scholar
Esper, J., Schweingruber, F.H., Winiger, M., 2002. 1300 years of climate history for Western Central Asia inferred from tree-rings. Holocene 12: 267277.Google Scholar
Fan, K., 2010. Climatic change and dynastic cycles in Chinese history: a review essay. Climatic Change 101: 565573.CrossRefGoogle Scholar
Fedorovich, B.A., 1972. Recent and ancient, cold and warm loesses and their relationship with glaciations and deserts. Acta Geologica Academiae Scientiarum Hungaricae 16: 371381.Google Scholar
Fowell, S., Hansen, B., Peck, J., Khosbayar, P., Ganbold, E., 2003. Mid to late Holocene paleoclimate evolution of the Lake Telmen Basin, north central Mongolia, based on palynological data. Quaternary Research 59: 353363.Google Scholar
Ghafurov, B., 2011. Tajiks: Pre-ancient, Ancient and Medieval History. Ministry of Culture of the Republic of Tajikistan, Irfon, Dushanbe, Tajikistan.Google Scholar
Giosan, L., Fuller, D.K., Nicoll, K., Flad, R.K., Clift, P.D. (Eds.), 2013. Climates, Landscapes, and Civilizations. Geophysical Monograph Series 198. American Geophysical Union, Washington, DC.Google Scholar
Goudie, A.S., Middleton, N.J., 2006. Desert Dust in the Global System. Springer, Berlin.Google Scholar
Goudie, A.S., Rendell, H.M., Bull, P.A., 1984. The loess of Tajik SSR. In: K. Miller (Ed.), International Karakoram Project. Cambridge University Press, Cambridge, pp. 399412.Google Scholar
Grenet, F., de la Vaissière, E., 2002. The last days of Panjikent. Silk Road Art and Archaeology. 8: 155196.Google Scholar
Harmatta, J., Puri, B.N., Etemadi, G.F. (Eds.), 1994. History of Civilizations of Central Asia Vol. 2, The Development of Sedentary and Nomadic Civilizations: 700 B.C. to A.D. 250. UNESCO, Paris.Google Scholar
Haug, G.H., Günther, D., Peterson, L.C., Sigman, D.M., Hughen, K.A., Aeschlimann, B., 2003. Climate and the collapse of Maya civilization. Science 299: 17311735.Google Scholar
He, X., Zhou, J., Zhang, X., Tang, K., 2006. Soil erosion response to climatic change and human activity during the Quaternary on the Loess Plateau, China. Regional Environmental Change 6: 6270.Google Scholar
Hodell, D.A., Curtis, J.H., Brenner, M., 1995. Possible role of climate in the collapse of Classic Maya civilization. Nature 375: 391394.Google Scholar
Kottek, M., Grieser, J., Beck, C., Rudolf, B., Rubel, F., 2006. World map of the Köppen-Geiger climate classification updated. Meteorologische Zeitschrift 15: 259263.Google Scholar
Latorre, C., Wilmshurst, J.M., von Gunten, L., 2016. Climate change and cultural evolution. Past Global Change Magazine 24: 5384.Google Scholar
Li, X., Sun, N., Dodson, J., Zhou, X., 2012. Human activity and its impact on the landscape at the Xishanping site in the western Loess Plateau during 4800–4300 cal yr BP based on the fossil charcoal record. Journal of Archaeological Science 39: 31413147.Google Scholar
Litvinsky, B.A., Zhang, G., Samghabadi, R.S. (Eds.), 1996. History of Civilizations of Central Asia Vol. 3, The Crossroads of Civilizations: A.D. 250 to 750. UNESCO, Paris.Google Scholar
Livshits, V., 1962. Legal documents and letters. [In Russian.] In: Sogdian Documents from Mount Mōḡ 2. Oriental Literature Publishing House, Moscow.Google Scholar
Lukk, A.A., Yunga, S.L., Shevchenko, V.I., Hamburger, M.W., 1995. Earthquake focal mechanisms, deformation state, and seismotectonics of the Pamir-Tien Shan region, central Asia. Journal of Geophysical Research 100: 2032120343.Google Scholar
Lydolph, P.E., 1977. World Survey of Climatology Vol. 7, Climates of the Soviet Union. Elsevier, Amsterdam.Google Scholar
Markovsky, A.P., 1959. Geology of the USSR Vol. 24, Tajik SSR: Part I—Geological Description. [In Russian.]. Ministry of Geology and Soil Protection USSR, Moscow.Google Scholar
Marshak, B.I., 2003. The archaeology of Sogdiana. Silk Road 1: 28.Google Scholar
Marshak, B.I., 2016. Panjikant. Encyclopædia Iranica. http://www.iranicaonline.org/articles/panjikant (accessed September 2016).Google Scholar
Mestdagh, H., Haesaerts, P., Dodonov, A., Hus, J., 1999. Pedosedimentary and climatic reconstruction of the last interglacial and early glacial loess–paleosol sequence in south Tadzhikistan. Catena 35: 197218.Google Scholar
Mirzobaev, X., Zubarev, A.M., Ismailov, M.M., Musaelyan, A.A., Romanov, O.O., 1968. The prediction of loess subsidence. [In Russian.]. In: Narzikulov, I.K., Stanjukovich, K.B. (Eds.), Atlas of Tajik SSR. Tajik SSR Academy of Sciences, Dushanbe, Tajikistan.Google Scholar
Nugteren, G., Vandenberghe, J., Van Huissteden, J., An, Z., 2004. A Quaternary climate record based on grain size analysis from the Luochuan section on the central Loess Plateau, China. Global and Planetary Change 41: 167183.Google Scholar
Obruchev, V.A., 1911. The question of the origin of loess—in defense of the aeolian hypothesis. [In Russian.] Izvestiya Tomskaya Tekhnologiya Institute 33: 138.Google Scholar
Obruchev, V.A., 1945. Loess types and their origin. American Journal of Science 243: 256262.CrossRefGoogle Scholar
Obruchev, V.A., 1986. Loess and Its Significance. Loess Letter Supplement 11 (translated from Novyi Mir 1952). Leicester University, Leicester, UK.Google Scholar
Opała, M., Niedźwiedź, T., Rahmonov, O., Owczarek, P., Małarzewski, Ł., 2017. Towards improving the Central Asian dendrochronological network—new data from Tajikistan, Pamir-Alay. Dendrochronologia 41: 1023.Google Scholar
Opała-Owczarek, M., Niedźwiedź, T., Owczarek, P., Rahmonov, O., 2017. Tree-ring based reconstruction of winter precipitation in the semi-arid Pamir-Alay Mts. (central Asia) over the last millennium. In: International Symposium on Eolian Dynamics, Paleosols and Environmental Change in Drylands, La Oliva, Spain. INQUA, SACCOM, LOESS Focus Group, p. 55.Google Scholar
Owczarek, P., Opała-Owczarek, M., Rahmonov, O., Mendecki, M., 2017. 100 Years of earthquakes in the Pamir region as recorded in juniper wood: a case study of Tajikistan. Journal of Asian Earth Sciences 138: 173185.Google Scholar
Pages 2k Consortium. 2013. Continental-scale temperature variability during the past two millennia. Nature Geosciences 6: 339346.Google Scholar
Peel, M.C., Finlayson, B.L., McMahon, T.A., 2007. Updated world map of the Köppen-Geiger climate classification. Hydrology and Earth System Sciences 11: 16331644.Google Scholar
Pei, Q., Zhang, D.D., 2014. Long-term relationship between climate change and nomadic migration in historical China. Ecology and Society 19: 68. http://dx.doi.org/10.5751/ES-06528-190268.Google Scholar
Raspopova, V.I., 1980. Metalwork of Early Medieval Sogdia. [In Russian.] Nauka, Leningrad.Google Scholar
Różycki, S.Z., 1991. Loess and Loess-Like Deposits. Ossolineum, Wrocław, Poland.Google Scholar
Schurr, B., Ratschbacher, L., Sippl, C., Gloaguen, R., Yuan, X., Mechie, J., 2014. Seismotectonics of the Pamir. Tectonics 33: 15011518.Google Scholar
Semenov, G.L., 1996. Sogdian Fortifications in the 5th–8th Centuries. [In Russian.] Institute of Archeology, St. Petersburg.Google Scholar
Shackleton, N.J., An, Z.S, Dodonov, A.E., Gavin, J., Kukla, G., Ranov, V.A., Zhou, L.P., 1995. Accumulation rate of loess in Tadjikistan and China: relationship with global ice volume cycles. Quaternary Proceedings 4: 16.Google Scholar
Sheppard, P., Tarasov, P., Graumlich, L., Heussner, K., Wagner, M., Osterle, H., Thompson, L., 2004. Annual precipitation since 515 BC reconstructed from living and fossil juniper growth of northeast Qinghai Province, China. Climate Dynamics 23: 869881.Google Scholar
Sidle, R.C., Taylor, D., Lu, X.X., Adger, W.N., Lowe, D.J., de Lange, W.P., Newnham, R.M., Dodson, J.R., 2004. Interactions of natural hazards and society in Austral-Asia: evidence in past and recent records. Quaternary International 118: 181203.Google Scholar
Su, Y., Liu, L., Fang, Q., Ma, Y.N., 2016. The relationship between climate change and wars waged between nomadic and farming groups from the Western Han Dynasty to the Tang Dynasty period. Climate of the Past 12: 137150.Google Scholar
Tan, L., Cai, Y., An, Z., Yi, L., Zhang, H., Qin, S., 2011. Climate patterns in north central China during the last 1800 yr and their possible driving force. Climate of the Past 7: 685692.Google Scholar
Vandenberghe, J., 2013. Grain size of fine-grained windblown sediment: a powerful proxy for process identification. Earth-Science Reviews 121: 1830.Google Scholar
Vandenberghe, J., Renssen, H., Van Huissteden, J., Nugteren, G., Konert, M., Lu, H., Dodonov, A., Buylaert, J.-P., 2006. Penetration of Atlantic westerly winds into Central and East Asia. Quaternary Science Reviews 25: 23802389.CrossRefGoogle Scholar
Vinnichenko, G.P., Tadzhibekov, M., 2010. The relief evolution of Pamir and Hissar-Alay in the Phanerozoic. [In Russian.] Doklady Akademii Nauk Respubliki Tadzhikistan 53: 879883.Google Scholar
Vlasov, N.G., Dyakov, Y.A., Cherev, E.S., 1991. Geological Map of the Tajik SSR and Adjacent Territories, 1:500,000. Vsesojuznoi Geological Institute, Leningrad.Google Scholar
Wang, L., Shao, M., Wang, Q., Gale, W.J., 2006. Historical changes in the environment of the Chinese Loess Plateau. Environmental Science & Policy 9: 675684.Google Scholar
Weiss, H., Bradley, R.S., 2001. What drives societal collapse? Science 291: 609610.Google Scholar
Williams, M.W., Konovalov, V.G., 2008. Central Asia Temperature and Precipitation Data, 1879-2003. USA National Snow and Ice Data Center, Boulder, CO. http://dx.doi.org/10.7265/N5NK3BZ8.Google Scholar
Yang, B., Qin, C., Wang, J., He, M., Melvin, T.M., Osborn, T.J., Briffa, K.R., 2014. A 3,500-year tree-ring record of annual precipitation on the northeastern Tibetan Plateau. Proceedings of the National Academy of Sciences of the United States of America 111: 29032908.Google Scholar
Yang, B., Shi, Y.F., 2001. Comparison of Guliya ice core accumulation with other proxy precipitation data of China during the last two millennia. Marine Geology and Quaternary Geology 21: 6166.Google Scholar
Yang, B., Wang, J., Bräuning, A., Dong, Z., Esper, J., 2009. Late Holocene climatic and environmental changes in arid central Asia. Quaternary International 194: 6878.Google Scholar
Yin, J., Su, Y., Fang, X., 2016. Climate change and social vicissitudes in China over the past two millennia. Quaternary Research 86: 133143.Google Scholar