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This chapter introduces, by literature reviews, the issue of the links and processes behind climate change, environmental change, and socio-culture change in the past at the ancient Silk Road region. Analyses of the changes of the socio-environment system in this area enhance our understanding on the regular patterns of coupled natural and social evolution, and is thus of important theoretical and practical significance. We argue that the cross-cutting theme has been to reach beyond simple explanations of environmental or human determinism, but social resilience under environmental impacts. Studies indicate both that climate conditions significantly influence human socio-cultural systems and that the socio-culture systems are certainly resilient to climate impacts. This chapter also summarizes the scope of all chapters in this book by illustrating the specific topics, research areas, focused periods and their inner relationships. The conclusion further summarizes the recent research states on past socio-environmental dynamics and the findings achieved in this book, as well as some outlooks.

This study reconstructed the possible existence of saline lakes in the Guanzhong Basin during the past 2000 years. Using Chinese historical literature as well as stone inscriptions, a total of five historical saline lake bodies which had existed in this region were documented: Lakes Yanchize, Xiluchi, Dongluchi, Zhuyanze and Xiaoyanchi. Lakes Zhuyanze, Yanchize, Xiluchi, Dongluchi, and Xiaoyanchi desiccated respectively at some point during 1076–1701 AD, 1584–1735 AD, 1666–1791 AD, 1666–1791 AD, and 1712–1906 AD. The lakes in the west of this region possibly desiccated relatively early, and the lakes in the east desiccated relatively late. Most of the lakes desiccated during a cold climate period. It seems that the dry period of the 15th–17th centuries overlapped with the periods that some of the lakes desiccated. All the five lakes desiccated during periods of increased soil erosion. The main causes of the degradation and desiccation of Lakes Yanchize, Xiluchi and Dongluchi were flood irrigation and silt sedimentation. The degradation and desiccation of Lake Yanchize and Lakes Dongluchi and Xiluchi corresponded to periods of population explosion when land was heavily cultivated in Fuping and Pucheng Counties. The existence of historical saline lakes indicates that the remains of the Sanmen Paleo-Lake existed in the Guanzhong Basin during the past 2000 years.

The Chinese empire experienced a large expansion to the arid regions in the west during the Han Dynasty (206 BCE–220 CE). The Hexi Corridor, the Yanqi Basin, the southeastern part of the Junggar Basin and the Tarim Basin became part of the empire. The expansion of the Han Dynasty was accompanied by the significant intensification of irrigation farming along rivers draining the Qilian, Tianshan and Kunlun Mountains. Sedimentological and geochemical analyses and dating of lake sediments and shorelines revealed that four large lakes in the region experienced falling levels, or were almost or completely desiccating. The level of Zhuyeze Lake was falling rapidly ca. 2100 years before present (a BP), and the accumulation of lake sediments was replaced by an alluvial fan setting in large parts of the basin. Lake Eastern Juyan desiccated ca. 1700 a BP. Lake Bosten experienced low levels and increasing salinities at ca. 2200 a BP. Lake sediments in the Lop Nur region were mostly replaced by aeolian sands during a period of near-desiccation at 1800 a BP. In contrast, records from fifteen lakes farther in the west, north or south of the Han Dynasty realm indicate relatively wet climate conditions ca. 2000 years ago. Thus, dramatic landscape changes including the near and complete desiccation of large lakes in the arid western part of today’s China probably resulted from the withdrawal of water from tributaries during the Han Dynasty. These changes likely represent the earliest man-made environmental disasters comparable to the recent Aral-Sea crisis.

Extensive survey of paleocourses of the Ili delta discovered archaeological findings that, chronologically attributed and systematized, allowed the historical reconstruction of the human occupation of the delta. Until recently the colonization was believed to have begun only during medieval times. We argue it began much earlier at the start of the Bronze Age of Kazakhstan (second half of the III millennium BC) under the impulse of new economical activities based on stockbreeding and bronze metallurgy. The basic method of research consisted in surveys, collection of surface finds and documentation of hydrogeological and climatic data. The correlation between the two types of information gives an idea of the factors that influenced the distribution of habitats, mostly represented by winter camps. Their number and concentration change by epoch, pointing to changes in both cultural proclivities and environmental factors. The understanding of the whole historical process requires background knowledge of the hydrological history of the Ili delta, a complex system involving active distributaries and intermittent or inactive paleo-courses, and showing the anticlockwise rotation of 5 successive deltas. Generally speaking, arid climate phases stabilize the delta, pluvial phases favor changes in various directions. Human colonization concerned the two Holocene deltas preceding the modern one: relict terraces of the Uzunaral delta (8–4 ka BP) and terraces of mild active distributaries of the Bakanas delta (4000–250 BP), subject during the last 4000 years to complex geomorphological and hydrological changes that, when reconstructed and correlated with the distribution of finds, explain the location of habitats and allow the mutual chronological attribution of geological and cultural deposits.

Paleo-climatic, environmental, archaeological studies and historical accounts concerning the behavior of the Aral Sea during the last 2000 years point to a number of water level regressions similar or deeper than the modern one. This article is focused on the causes of such regressions, which are variously attributed to climatic change, diversion of river courses and anthropogenic water withdrawal. The first factor has been researched by several geo-specialists and its potential impact has been preliminarily evaluated. The second factor has been considered only in the case of the Amu Darya river. The third factor—water withdrawal for irrigation purposes—has been hypothesized, though never deserved specific analysis. The article provides a quantitative evaluation of the total hectares covered by the medieval urban systems of the Syr Darya and Amu Darya river basins, and of the coefficient of water use per hectare of walled towns during the X-XII centuries AD. Estimates of annual volumes of anthropogenic water withdrawal allow the investigation of the complex interaction of the three factors above in determining the hydrological conditions of the Aral Sea. On the basis of the calculation of possible scenarios of water mass balance, the occurrence of transmission losses by medieval diversions of the Syr Darya course has been suspected as the main cause of lake regressions, which is supported by geological considerations, archaeological data and historical accounts.

As response to climate change becomes an ever present issue, considerations of human-environment interactions in the past have moved beyond deterministic notions of climatically driven cycles of social expansion and collapse to more complex examinations of anthropogenic effects upon environments, as well as the transformative effects environmental change has upon human societies. The entanglement between these processes may be explored through a number of theoretical frameworks, including Niche Construction Theory (NCT) and other notions of human resilience. The Valley of Kashmir in the northernmost region of South Asia presents an opportunity for examining a number of these processes. This paper aims to synthesise past archaeological and Holocene palaeoclimate data, as well as review past interpretations of human responses to climate factors in Kashmir. Arguments are raised for new theoretical and methodological approaches to understanding human-environment interactions in the valley, based on recent studies from Kashmir and adjacent regions. These approaches aim to address gaps in understanding arising from poorly resolved environmental records or uncritical integration of archaeological and palaeoclimate data. Some early conclusions may be drawn as to ways in which differentiated land use patterns across the valley and adjacent mountain zones would have allowed for long term patterns of adjustment and reorganisation as a response to climate pressures. New preliminary data that has the potential for exploring some of these processes in the valley is also presented.

Earthquakes are among the most horrible events of nature due to unexpected occurrence, for which no spiritual means are available for protection. The only way of preserving life and property is to prepare for the inevitable: applying earthquake-resistant construction methods. Zones of damaging earthquakes along the Silk Road are reviewed for seismic hazard and to understand the ways local civilizations coped with it during the past two thousand years. China and its wide sphere of cultural influence certainly had earthquake-resistant architectural practice, as the high number of ancient buildings, especially high pagodas, prove. A brief review of anti-seismic design and construction methods (applied both for wooden and masonry buildings) is given, in the context of earthquake-prone zones of Northern China. Muslim architects in Western China and Central Asia used brick and mortar to construct earthquake-resistant structural systems. Ancient Greek architects in Anatolia and the Aegean applied steel clamps embedded in lead casing to hold together columns and masonry walls during frequent earthquakes. Romans invented concrete and built all sizes of buildings as a single, non-flexible unit. Masonry, surrounding and decorating the concrete core of the wall, did not bear load. Concrete resisted minor shaking, yielding only to forces higher than fracture limits. Roman building traditions survived the Dark Ages, and 12th century Crusader castles erected in earthquake-prone Syria survive until today in reasonably good condition. Usage of earthquake-resistant technology depends on the perception of earthquake risks and on available financial resources. Earthquake-resistant construction practice is significantly more expensive than regular construction. Frequent earthquakes maintain safe construction practices, like the timber-laced masonry tradition in the Eastern Mediterranean throughout 500 years of political and technological development.

This article analyzes the effect of climate extremes on the historical processes that took place (AD 536, 581, 601, 626 and 679) in the Eastern Turk Empire (AD 534–745) in Inner Asia. Climate extremes are sharp, strong and sometimes protracted periods of cooling and drought caused by volcanic eruptions that in this case resulted in a negative effect on the economy of a nomadic society and were often accompanied by famine and illness. In fact, many of these natural catastrophes coincided with the Black Death pandemics among the Eastern Turks and the Chinese living in the north of China. The Turk Empire can be split into several chronological periods during which significant events that led to changes in the course of history of the nomadic state took place: AD 534–545—the rise of the Turk Empire; AD 581–583—the division of the Turk Empire into the Western and the Eastern Empires; AD 601–603—the rise of Qimin Qaghan; AD 627–630—the Eastern Turks are conquered by China; AD 679–687—the second rise of the Eastern Turk Empire. The research shows that there is clearly-discernable interplay between important historical events and climate extremes in the history of the Turk Empire. This interplay has led us to the conclusion that the climatic factor did have an impact on the historical processes that took place in the eastern part of Inner Asia, especially on the territories with a nomadic economy.

One of the richest societies along the Silk Road developed in Sogdiana, located in present-day Tajikistan, Uzbekistan, and Kyrgyzstan. This urban civilisation reached its greatest prosperity during the golden age of the Silk Road (sixth to ninth century ). Rapid political and economic changes, accelerated by climatic variations, were observed during last millennium in this region. The newly developed tree-ring-based reconstruction of precipitation for the past millennium revealed a series of dry and wet stages. During the Medieval Climate Anomaly (MCA), two dry periods occurred (900–1000 and 1200–1250), interrupted by a phase of wetter conditions. Distinct dry periods occurred around 1510–1650, 1750–1850, and 1920–1970, respectively. The juniper tree-ring record of moisture changes revealed that major dry and pluvial episodes were consistent with those indicated by hydroclimatic proxy data from adjacent areas. These climate fluctuations have had long- and short term consequences for human history in the territory of former Sogdiana.

Naryn River provides large amounts of water resource for Central Asian countries. Thus, the severity and frequency of drought variation relate to runoff has important influences on social and economic development of this region. In this study, the new tree-ring width chronologies of juniper trees from the low-elevation site of the western Tien Shan are used to reconstruct drought variation for northwestern Kyrgyzstan and place the short instrumental period (1950–2013) of Standardised Precipitation-Evapotranspiration Index (SPEI) in a long-term context. The SPEI reconstruction successfully reflects the dry and wet periods over the past 451 years, and captures a recent wetting trend that generally agrees with the drought reconstructions for the spruce-dominated area. However, some differences between the tree-ring records from spruce-dominated and juniper-dominated areas reflect regional climate differences. The comparison between drought events in the SPEI reconstruction and historical event of Central Asia reveals drought variations have had profound influences on some historical archives over the past several centuries. This study provides the first long-term SPEI reconstruction and drought evaluation from the low-altitude area of Central Asia, contributing to climate change issues in Central Asia.