ENSIKLOPEDIA
Gansu Corridor
| Hexi Corridor | |
|---|---|
| Gansu Corridor | |
Zhangye National Geopark in the Hexi Corridor Scenery of the Hexi Corridor at Jiayuguan | |
| Length | 1,000–1,200 km (620–750 mi) |
| Width | 40–100 km (25–62 mi) |
| Geography | |
| Population centers | Dunhuang, Yumen City, Jiayuguan City, Jiuquan, Zhangye, Jinchang, Wuwei, and Lanzhou |
| Borders on | Gobi Desert (north) Wushao Mountains (east) Qilian Mountains (south) Dunhuang (west) |
| Coordinates | 38°42′N 100°47′E / 38.700°N 100.783°E / 38.700; 100.783 |
The Hexi Corridor,[a] also known as the Gansu Corridor, is an important historical region located in the modern western Gansu province of China. It refers to a narrow stretch of traversable and relatively arable plain west of the Yellow River's Ordos Loop (hence the name Hexi, meaning 'west of the river'), flanked between the much more elevated and inhospitable terrains of the Mongolian and Tibetan Plateaus. The Hexi Corridor enabled cultural and agricultural exchange between China and Eurasia for several milennia, in both prehistory and as part of the Northern Silk Road after the Han Dynasty.[1]
As part of the Northern Silk Road, running northwest from the western section of the Ordos Loop between Yinchuan and Lanzhou, the Hexi Corridor was the most important trade route in Northwest China. It linked China proper to the historic Western Regions for traders and military incursions into Central Asia. It is a string of oases along the northern edges of the Qilian Mountains and Altyn-Tagh, with the high and desolate Tibetan Plateau further to the south. To the north are the Longshou, Heli and Mazong Mountains separating it from the arid Badain Jaran Desert, Gobi Desert and the cold steppes of the Mongolian Plateau. At the western end, the route splits into three, going either north of the Tianshan Mountains or south on either side of the Tarim Basin. At the eastern end, the mountains around Lanzhou grants access to the Longxi Basin, which leads east through Mount Long along the Wei River valley into the populous Guanzhong Plain, and then into the Central Plain.
Geography
The Hexi Corridor encompasses much of northwestern Gansu province, and is located on the west side of the Yellow River as it runs north around the Ordos Loop (hence the name Hexi, meaning 'west of the river'). The corridor stretches roughly 1,100 kilometres (680 mi) from the Wushao Mountains in the east to Yumen Pass in the west, 100–200 kilometres (60–100 mi) from north to south, ranges from 40–100 kilometres (20–60 mi) in width, and covers an area of approximately 276,000 square kilometres (107,000 mi2) or around 60% of the area of Gansu Province. Its population was 4.82 million people in 2011, representing around 19% of the province's total population. As of 2024, the corridor contains 20 administrative divisions and five prefecture-level cities, which are, from east to west: Wuwei, Jinchang, Zhangye, Jiuquan, and Jiayuguan.[2][3][4]
The elevation of the Hexi Corridor descends from around 1,500 metres (4,900 ft) above sea level in the southeast to 1,000 metres (3,300 ft) in the northwest.[4] It is bordered by the Qilian Mountains in the south and southeast, the Kumtag Desert to the west, the Mazong, Helan, and Longshou Mountains to the north, the Badain Jaran Desert to the northeast, and the Tengger Desert to the southeast.[5][6] The Qilian Mountains run south of the Hexi Corridor for 600 kilometres (370 mi) and contain several peaks exceeding 4,500 metres (14,800 ft) above sea level, while the mountains to the north generally range from 1,500–2,500 metres (4,900–8,200 ft) in height.[7] The location of the Hexi Corridor between these landforms as a relatively arable and low-lying valley makes it the most convenient route between China and Central Asia.[8]
The three largest rivers in the Hexi Corridor are the Shiyang, Heihe, and Shule rivers.[9] Like most rivers in the region, much of their discharge is derived from the melting of glaciers and snow in the Qilian Mountains; they form extensive alluvial fans and inland drainage basins as they flow through the Hexi Corridor, beyond which lie deserts and large sand-dune fields.[10][11] Arid landscapes such as deserts comprise roughly 70% of the Hexi Corridor, while fertile land and vegetation are largely confined to oases along the major rivers, which have sustained both nomadic groups and settled societies for thousands of years.[12][13][14]
Geology
The Hexi Corridor is a Cenozoic foreland basin formed over millions of years by the uplift, crustal shortening, and northward advance of the Tibetan Plateau, a landform of which the Hexi Corridor forms the northeastern margin. The region is seismically active, having experienced five earthquakes of magnitude 7 or greater since 180 AD, and is dominated by northwest-trending reverse faults. It is internally divided by three uplifts into four depressions filled with thick fluvial and lacustrine sediment deposited during the Quaternary era.[15][7][16]

The area of the present-day Hexi Corridor was successively part of various foreland and strike-slip basins throughout the Paleozoic and early to mid-Mesozoic.[18] During the Cretaceous, the region encompassing the Hexi Corridor and Qilian Mountains was lifted above its surroundings and tectonic activity waned, causing the region to be dominated by erosional activity until the early Oligocene.[19][20]
During the Oligocene, crustal shortening as a result of the India–Eurasia collision and the growth of the Tibetan Plateau caused the down-faulting and subsidence of the Hexi Corridor.[20] As a result, the region likely became the northern margin of a wide basin extending northward from the Kunlun Mountains, interrupted by a low rise roughly 400 kilometres (250 mi) to the south of the Hexi Corridor in the present-day southern Qilian Mountains.[21][22] Sedimentation in the Hexi Corridor during this time was dominated by fine and highly eroded material derived from this low rise and transported by long meandering streams, with deposition likely occurring in shallow terminal lakes within the basin.[23][24]
During the Miocene (around 13 million years ago), the northeastward propagation of the Altyn Tagh Fault reached its maximum extent at the Hexi Corridor; subsequent crustal shortening around this new terminus led to the formation of the Qilian Mountains, separating the Qaidam Basin to the south from the Hexi Corridor.[25][26] During the Pliocene and Pleistocene, crustal shortening spread into the Hexi Corridor itself and formed multiple uplifts. Since the mid-Miocene, deposition in the Hexi Corridor has been dominated by coarse weakly-eroded material owing to the close proximity of the Qilian Mountains and short sediment transport distances.[27]
Sedimentation rates in the Hexi Corridor increased significantly during the early Pleistocene.[28] 1.7 million years ago, the terminal lakes in the Hexi Corridor began to contract as the deltas of rivers prograded into the basin. By 1.1 million years ago, the lakes and former river deltas had disappeared with the formation rivers such as the Heihe and Shiyang, which cut through the former systems by running parallel down the length of the corridor rather than perpendicularly across it.[24] Continued tectonic activity steepened the Qilian Mountains and caused the alluvial fans of many rivers to shift toward the basin's center, converting them into tributaries of the new longitudinal channels.[29][30]
Climate

The dominant climate types in the Hexi Corridor are temperate semi-arid (Köppen: BSk) and temperate arid (Köppen: BWk).[31] The region experiences an average annual temperature of 4–10 °C (39–50 °F) and an average annual precipitation of less than 200 mm (7.9 in) which generally decreases from southwest to northeast.[32][33] The climate in the Hexi Corridor is heavily influenced by its location at the intersection of a humid zone in the east dominated by the East Asian monsoon and an arid zone in the west dominated by the westerlies,[34] and has varied over thousands to millions of years as a result of Milankovitch cycles.[35]
Climate fluctuations in the Hexi Corridor have historically played a dominant role in shaping human settlement and interaction in the region. Between the Last Glacial Maximum and the late Holocene, the northern boundary of the East Asian Monsoon migrated at least 300 km (190 mi) northwest of its current location near Zhangye.[34] Further intensification during the middle Holocene led to high lake levels and abundant vegetation, and it was during this time when human settlement first expanded into the Hexi Corridor.[36] From 4000–2000 BP, the East Asian monsoon retreated and the climate became cold and arid, leading to a period of cultural and agricultural decline in the region.[37][38] Since 2000 BP, the influence of climate variability in the Hexi Corridor has increased; for instance, the abundance of early Han dynasty sites may be attributed to relatively warm and humid conditions at the time, while the Little Ice Age during the Ming to Qing dynasties likely contributed to the decline of the region's sites and the Silk Road.[39][40]
History
Prehistory
The Hexi Corridor has been the site of cultural exchanges across Eurasia since prehistory.[41] It was first settled around 4800 BP in Neolithic times by millet farmers from the Yangshao Culture in the western Loess Plateau,[42][43][44] who enabled the spread of millet to Central Asia and the rest of Eurasia and Africa.[45] These farmers also used pottery production techniques from Northern China.[43] Several cultures developed in the Hexi corridor during this time, such as the Majiayao, Banshan, and Machang.[46]
The oldest known bronze object discovered in China, dating to 5000–4500 BP, was unearthed at the Majiayao site.[47] The introduction of copper-smelting technology around 4200 BP marked the beginning of the Bronze Age in the Hexi Corridor,[48][49] and bronze production reached its peak between 4000 and 3500 BP.[50] Bronze artifacts from the Hexi Corridor dating to this period account for approximately 70 percent of all bronze objects found in China prior to the Shang dynasty.[51] During this time, domesticated livestock were introduced to the region,[52] so local cultures such as the Shajing, Qijia, Xichengyi, Siba, and Shanma developed agricultural economies based on smelting copper, cultivating millet, and herding animals such as sheep, pigs, cattle, and horses.[53][54]
Wheat and barley from the Fertile Crescent arrived in the Hexi Corridor via Central Asia around 4000 BP,[55][56][57] and from there spread into China proper.[58] By around 3700–3500 BP, most likely due increasing aridity caused by the retreat of the East Asian Monsoon,[59][60] the more drought-resistant wheat and barley had replaced millet as the main staple crop in the Hexi Corridor.[61][56][62] Cultures after this time period (such as the Shajing culture) saw a decrease in site numbers and bronze artifacts,[63][64][65] and became dominated by nomadic production rather than agriculture.[66][67]
Han dynasty

The nomadic Yuezhi resided in the Hexi Corridor in the 3rd century BCE.[68] The Great Wall of China was constructed into parts of the Hexi Corridor following the Qin-Xiongnu Wars,[69] and the defeated Xiongnu formed a confederacy under leader Modu Chanyu.[70][71] In 176 BCE, the Xiongnu defeated the Yuezhi, most of whom fled from the region while the remaining population moved south into the Qilian Mountains to live with the Qiang.[72][73] The Xiongnu were subsequently in complete control of the Hexi Corridor.[74][75]
During the Han-Xiongnu Wars, Han dynasty general Huo Qubing expelled the Xiongnu from the Hexi Corridor at the Battle of Hexi [zh] (121 BCE).[76][77] The province of Liangzhou was created with its capital at Guzang (modern Wuwei City), within which the commanderies of Wuwei, Zhangye, Jiuquan and Dunhuang (the Four Commanderies of Hexi) were established.[77][78][79] This gave the Han dynasty control over major trade routes to Central Asia and is regarded by most scholars as the beginning of the Silk Road.[80][81][82] Agricultural garrison towns were established in the Hexi Corridor to secure the route and the Great Wall was extended to Yumen Pass 80 kilometres (50 mi) west of Dunhuang.[83][84][85] Additionally, the Han dynasty's acquisition of the Hexi Corridor allowed them to conquer the Tarim Basin and establish the Protectorate of the Western Regions in 60 BCE,[86][87] and proved instrumental in defeating the Xiongnu as it prevented contact between them and the Qiang.[88][89]

Following the collapse of the interregnum Xin dynasty in 23 CE, the Hexi Corridor was settled by large numbers of Qiang people and came under the control of warlord Dou Rong [zh], who submitted to the reinstated Eastern Han dynasty in 29 CE.[90][91][92] In the 2nd century CE, millions of Han settlers withdrew from the Hexi Corridor when the Qiang began to raid the region.[93][94][95] The Yuezhi, Xiongnu, and Qiang instigated the Liangzhou Rebellion in 184, which largely isolated the Hexi Corridor from central control and contributed to the fall of the Han dynasty.[96][97][98] By the end of the Han dynasty, the Hexi Corridor was occupied by warlords Han Sui, Ma Teng and Ma Chao.[99][100] In 214, warlord Cao Cao conquered the region and incorporated it into his state of Cao Wei.[101]
Six Dynasties and Sixteen Kingdoms

Cao Cao's son Cao Pi of Wei deposed the Han dynasty in 220, marking the start of the Three Kingdoms era.[102][103] In 230, rival Three Kingdoms state Shu Han attacked the Hexi Corridor as part of Zhuge Liang's Northern Expeditions.[104] In 266, Cao Wei became the Jin dynasty, which inherited the Hexi Corridor.[105][106] In 270, the Xianbei, related to the Xiongnu, began a rebellion in the region which lasted until 279.[107] Starting in the late 3rd century, groups such as the Kushans (descended from the Yuezhi) and Sogdians established a widespread presence in the Hexi Corridor as merchants along the Silk Road.[108][109] These groups contributed significantly to the spread of belief systems such as Buddhism into the Hexi Corridor.[110][111][112]

The state of Former Liang was founded in the Hexi Corridor in the early 4th century, and became the longest-lasting and most politically stable of the Sixteen Kingdoms.[113][114] In 376, Former Liang was conquered by Former Qin; various parts of the Hexi Corridor then came under the control of Later Liang in 386, Southern and Northern Liang in 397, and Western Liang in 400, before reunifying under Northern Liang in 421.[115][116] During this period, the Hexi Corridor was spared from much of the turmoil of the Central China Plains, which caused increased migration to the region and led to it becoming a centre of culture in China.[117][118][119] Buddhist culture and activity flourished in the region; the first of the Mogao Caves were constructed during this time,[120] and the extensive creation of Buddhist artworks and translation of texts at this time directly contributed to the adoption of the religion in the rest of China.[121][122]
In 439, Northern Wei conquered Northern Liang and ended the Sixteen Kingdoms era, though the final Northern Liang stronghold at Dunhuang remained until 442.[123][124] A garrison was then established at Dunhuang to defend against the Rouran and significant numbers of civilians were moved from the Hexi Corridor to the Wei capital at Pingcheng, promoting the readoption of classical Chinese culture and spread of Buddhism in the Central Plains.[119][125][126] In the 470s, the Northern Wei government considered abandoning the Hexi Corridor due to repeated raids by the Rouran. They later defeated the Rouran in 492, although the region remained largely desolate into the early 6th century.[127][128] After the fall of Northern Wei, the Hexi Corridor came into the control of Western Wei in 535, which became Northern Zhou in 557.[129][130]
Medieval history

In 581, Northern Zhou became the Sui dynasty,[131] which later reunited China Proper for the first time in three centuries.[132][133] In 609, Emperor Yang of Sui toured the region and personally commanded an expedition against the Tuyuhun to protect its trade routes.[134][135] Warlord Li Gui seized control of the Hexi Corridor in 617 and proclaimed himself ruler of Liang, which was conquered by the newly-founded Tang dynasty in 619.[136][137] In 627, Buddhist monk Xuanzang passed through the Hexi Corridor on his way to India.[138][139]
Between 630 and 657, the Tang dynasty conquered territories from several Central Asian states to secure the Hexi Corridor and consolidate control over the Silk Road.[140][141] The renewed stability encouraged trade and cultural exchange; religions such as Zoroastrianism, Nestorian Christianity, and Islam spread through the region into central China, and cities in the Hexi Corridor became increasingly cosmopolitan.[142] This expansion also brought the Tang into conflict with the Tibetan Empire, which began encroaching on the Hexi Corridor around 670.[143][144] In 711, the Hexi Corridor was organised under a military governor (jiedushi) as one of nine frontier commands of the Tang dynasty,[145] which by 742 possessed a quarter of all horses in the empire and represented its third-largest military force.[146]

Tang forces were withdrawn from the Hexi Corridor following the outbreak of the An Lushan Rebellion in 755 and the Tibetan Empire gradually occupied the region, culminating in their capture of Dunhuang in 786 and the rest of the Hexi Corridor in the 790s.[148][149] Following this, residents of the region adopted various Tibetan customs such as the use of Tibetan names and the Tibetan script, which continued even after the Tang dynasty reasserted control.[150] Tibetan influence in the Hexi Corridor during this period led to the spread of Tibetan Buddhist culture to the rest of Eurasia, where it remained a dominant culture into the early 20th century.[151][152]
The Tibetan Empire collapsed in 842;[153] the Hexi Corridor was then seized by warlord Zhang Yichao in 848, who established the Tang-loyal Guiyi Circuit in 851.[154][155] The Guiyi Circuit reunified the Hexi Corridor and reached its greatest extent in the 860s.[156] Its power and territory then steadily declined under pressure from two Uyghur states: the Qocho Kingdom in the Tarim Basin to the west and the Ganzhou Uyghur Kingdom to the east,[157] which was founded after the Guiyi Circuit lost control of its eastern provinces in the 880s.[158]
By the early 10th century, the Guiyi Circuit was confined to the area surrounding Dunhuang, and was almost completely isolated from the rest of China by the Ganzhou Uyghurs' seizure of goods along the Silk Road.[159][160] In 911, the Guiyi Circuit became a vassal of the Ganzhou Uyghurs and reopened the Silk Road in 925.[161][162] After this, Dunhuang once again became a centre of culture in the region;[163] some of the largest temples at the Mogao Caves were constructed during this time, and Buddhist texts produced at Dunhuang were freely distributed to the Ganzhou and Qocho kingdoms. This revival was partly driven and financed by the diplomatic relations that the three states maintained with one another and with the dominant dynasties of the Central Plains.[164][165]
Western Xia dynasty and Mongol rule

The timeline of the Hexi Corridor's conquest by the Tangut-led Western Xia dynasty remains somewhat unclear, with Western Xia likely beginning its invasion in 1028 and completing the conquest in 1036.[166] However, a state (possibly the Guiyi Circuit or a Uyghur kingdom) in the vicinity of Dunhuang may have remained independent until at least 1052, though it is known that Western Xia controlled the entire region by the 1070s.[167][168] After the conquest of the Hexi Corridor, large numbers of civilians were mobilized for a campaign against the Song dynasty and the region's trade routes were increasingly bypassed by merchants, leading to a decline in the region's prosperity.[169][170]
In 1205, the Mongol Empire under Genghis Khan plundered the Hexi Corridor in the first of their attacks on Western Xia; this was followed in 1209 by a full-scale invasion launched through the corridor which led to Western Xia's submission as a vassal in 1210.[171] Genghis Khan invaded once again in 1225, conquering the entire Hexi Corridor in 1226 and the rest of Western Xia in 1227, the year of his death.[172]
Sometime between 1271 and 1275 (shortly after the establishment of the Mongol Yuan dynasty), Marco Polo travelled through the Hexi Corridor on his way to Xanadu, and recorded sights such as the giant reclining Buddha statue at Zhangye and the region's yaks.[173]
Ming and Qing dynasties

In 1370, the newly-established Ming dynasty seized the eastern section of the Hexi Corridor from the Mongols and captured most of the remaining territory in 1372.[175][176] Later that same year, they constructed Jiayu Pass 15 kilometres (9 mi) east of Dunhuang,[174] which left the city under the control of the Northern Yuan dynasty and led to it largely being abandoned.[177][178] By this point, the Hexi Corridor had largely lost its importance as a major trade route.[179]
Like the Han dynasty over a millennium prior, the Ming dynasty established garrison towns along the frontier shortly after their conquest of the region.[180][181] In 1524, Jiayu Pass was closed and Dunhuang was occupied by the Turfan Khanate.[182] The Ming dynasty rebuilt the Great Wall through the Hexi Corridor from 1539–1541 and added an extension in 1573.[174]
In 1644 during the Ming-Qing transition, the Hexi Corridor was briefly seized by the short-lived Shun dynasty until forces of the Qing dynasty under general Ajige defeated them in 1645.[183] In 1648, Muslim rebels led by Milayin [zh] occupied most of Gansu and retreated west to the Hexi Corridor in June of that year, where the rebels held out against Qing generals Meng Qiaofang [zh] and Zhang Yong [zh] in the cities of Ganzhou (Zhangye) and Suzhou (Jiuquan) until 1649.[184][185] After the Qing victory, 5,000 rebels were executed and Muslims in the Hexi Corridor were resettled away from major cities.[179][185] Between 1674 and 1676, the Hexi Corridor was isolated from the rest of the Qing dynasty during the Revolt of the Three Feudatories, in which Zhang Yong and his lieutenants played a major role in its suppression.[186][187]

Thousands of soldiers and farmers were settled in the Hexi Corridor to cultivate the land in the 1720s as part of a defensive system designed to isolate the Dzungar Khanate from Kokonor (Qinghai),[188] where a Dzungar uprising had been quelled.[189] By the 1750s, yields of millet and wheat, the region's two main crops, had become so high that the Qing dynasty frequently redistributed its harvest across the empire to stabilize grain prices and alleviate famines.[190]
Most of the Hexi Corridor fell to Muslim rebels in 1865 during the Dungan Revolt, which triggered further revolts in Xinjiang.[191] In 1873, General Zuo Zongtang laid siege to Jiuquan with 15,000 soldiers, and attacked its walls with siege guns and explosives. More than 7,000 Muslims were executed after the city's capture, and the remaining Muslims in the Hexi Corridor were resettled to southeastern Gansu to prevent future collaboration with Muslims in Xinjiang.[192][193]
In 1907, archaeologist Aurel Stein explored the Hexi Corridor, where he rediscovered treasures such as the Mogao Caves and a collection of ancient Sogdian letters in Dunhuang.[194][195]
Modern era

The Hexi Corridor, along with the rest of Gansu, was seized by Hui Muslim warlords in 1911 following the collapse of the Qing dynasty and the onset of the Warlord Era. These warlords established the Ma clique, which declared its allegiance to the Kuomintang government in 1927.[196] In August 1949, Gansu was captured by the People's Liberation Army during the final stages of the Chinese Civil War.[197]
The Lanzhou–Xinjiang railway, which runs through the Hexi Corridor, began construction in 1952 and opened in 1963.[198] In 1987, the Mogao Caves were listed as a UNESCO World Heritage Site.[199] The Lanzhou–Xinjiang high-speed railway, also passing through the Hexi Corridor, began construction in 2009 and opened in 2014.[200] In 2025, the Chinese government announced a plan to construct a 1,000 km (620 mi) "national heritage route" along the Hexi Corridor, which is expected to be completed in ten years.[201][202]
See also
References
Notes
- ↑ Chinese: 河西走廊; pinyin: Héxī Zǒuláng; Wade–Giles: Ho2-hsi1 Tsou3-lang2; Dungan: Хәщи зулон; Xiao'erjing: حْسِ ظِوْلاْ; Mandarin pronunciation: [xɤ̌ɕí tsòʊlɑ̌ŋ] /həˈʃiː/
Citations
- ↑ Yang et al. 2020.
- ↑ Liu et al. 2015, pp. 251–252.
- ↑ Nie, Wang & Huang 2023, pp. 3–4.
- 1 2 Zhou et al. 2025, p. 255.
- ↑ Zhang et al. 2016, pp. 70–71.
- ↑ Yang et al. 2020, p. 613.
- 1 2 Li & Yang 1998, p. 347.
- ↑ Li et al. 2023, p. 2, Section 2.1: Study Area.
- ↑ Chen 1996, p. 247.
- ↑ Li & Yang 1998, p. 299.
- ↑ Zhu 2022.
- ↑ Tang et al. 2023, Section 2.1. Study area and period.
- ↑ Wang, Yan & Li 2026, p. 4.
- ↑ Zhu et al. 2022, p. 5, Section 3: Results.
- ↑ Li et al. 1999, pp. 299–300.
- ↑ Zhuang et al. 2011.
- ↑ Zhuang et al. 2011, pp. 117–119.
- ↑ Bovet et al. 2009, p. 294.
- ↑ Bovet et al. 2009, pp. 320–321.
- 1 2 Li & Yang 1998, p. 351.
- ↑ Bovet et al. 2009, pp. 320–323.
- ↑ Wang et al. 2016, p. 2253.
- ↑ Bovet et al. 2009, pp. 320–322.
- 1 2 Pan et al. 2016, pp. 258–260.
- ↑ Wang et al. 2016, pp. 2252–2254.
- ↑ Zhuang et al. 2011, pp. 145–146.
- ↑ Bovet et al. 2009, pp. 321–322.
- ↑ Métivier et al. 1998, pp. 833–836.
- ↑ Li et al. 1999, pp. 303–307.
- ↑ Pan et al. 2016, pp. 260–261.
- ↑ Qiu et al. 2022, p. 2, Study Region.
- ↑ Ma et al. 2024, p. 3, Methods.
- ↑ Yu et al. 2017, p. 2, Materials and Methods.
- 1 2 Li et al. 2023, pp. 1–2.
- ↑ Chen et al. 2024.
- ↑ Li et al. 2023, pp. 4, 7, Section 3: Result; Section 4: Discussion.
- ↑ Yang et al. 2020, p. 616.
- ↑ Li et al. 2023, p. 8.
- ↑ Yang et al. 2020, pp. 617–618.
- ↑ Liu & Shu 2025.
- ↑ Dong et al. 2017.
- ↑ Dong, Liang & Zhang 2024, p. 4: "Millet farmers settled in the northeast Tibetan Plateau and the Hexi Corridor during 5500–4300 BP, with broomcorn and foxtail millet being the primary crops in these two regions, respectively".
- 1 2 Dong et al. 2017, p. 627: "The data indicate that millet farmers had settled in the Hexi Corridor by 4800 BP, with the production of painted pottery that originated from north China".
- ↑ Li et al. 2023, pp. 4–5.
- ↑ Stevens et al. 2016, pp. 1544–1545.
- ↑ Dong et al. 2017, p. 622: "The Neolithic of the Hexi Corridor consists of three types of the Majiayao culture: the Majiayao (5000–4600 BP), Banshan (4600–4300 BP), and Machang (4300–4000 BP)".
- ↑ Chen et al. 2020, p. 954: "In this context, the Hexi Corridor is again at the heart of the discussion [...] It is within this region that archaeologists discovered the oldest bronze object so far in China (c.5000–4500 bp at the Majiayao site)".
- ↑ Zhou et al. 2012, p. 42: "After 4200 cal BP, the Qijia and Siba Cultures, which had copper smelting technology, prevailed in this region. Prosperous Bronze Age agriculture in the Hexi Corridor appears to have terminated suddenly around 3500-3400 cal BP".
- ↑ Dong et al. 2017, p. 625, Material evidence in the context of prehistoric transcontinental exchange.
- ↑ Zhang et al. 2017, pp. 93–94, Section 2.1 Study area.
- ↑ Zhang et al. 2017, p. 94: To date, archaeologists have unearthed more than 300 bronze artifacts and copper smelting artifacts from Qijia, Xichengyi and Siba culture archaeological sites. In total, these artifacts account for around 70% of the number of unearthed bronze artifacts in China before Shang Dynasty.
- ↑ Ren et al. 2022, p. 6: "The dispersal of domestic cattle and caprines along the Chinese Oasis route, including through the Hexi Corridor, probably occurred later than that of the more northern grassland route. Specifically, domestic cattle and sheep/goats may not have been introduced to the Hexi Corridor until ∼4000 BP".
- ↑ Yang et al. 2020, p. 615, Section 3.3 Subsistence strategy data.
- ↑ Zhou et al. 2012, pp. 46–47: "The prosperity of Bronze Age agricultural societies in the Hexi Corridor persisted from ca. 4200 to 3500 cal BP, and was characterised by agro-pastoralist societies that kept livestock including pig, sheep, cattle and horse, while also producing bronze objects of alloyed copper, arsenic and tin".
- ↑ Dong et al. 2017, p. 623: "Charred seeds of wheat, barley, foxtail, and broomcorn millet are all identified from Huoshiliang and other Bronze sites in the central Hexi Corridor. This implies that wheat had been introduced to the Hexi Corridor region by at least the early fourth millennium BP".
- 1 2 Li et al. 2023, p. 1: "Archaeobotanical and stable isotope evidence suggests that wheat and barley were introduced into the Hexi Corridor and northeastern Qinghai-Tibet Plateau in 4000 BP, rapidly replacing millets as primary staple crops after 3700 BP".
- ↑ Stevens et al. 2016, pp. 1542–1544.
- ↑ Li et al. 2007.
- ↑ Zhou et al. 2012, p. 42: "But the increasing climate aridity between ca. 4000 and 3500 cal BP, which was induced by a weakening of the Asian monsoon, is the underlying cause for the shrinking of arable land and vegetation degradation in Hexi Corridor, and this is the likely cause for the decrease of the agricultural activities and collapse of the Bronze Age societies in Hexi Corridor".
- ↑ Li et al. 2023, pp. 4–5, Section 3. Result.
- ↑ Yang et al. 2020, p. 615: "During~2800–2000 BC, people in the Hexi Corridor adopted a sedentary lifestyle, cultivating millet and raising pigs, sheep/goats, cattle, and dogs. Moreover, they began to cultivate wheat and barley beginning ~2000 BC. By ~2000–1000 BC, the strategy had shifted to semi-sedentary agro-pastoral production, based on the utilization of sheep/goats, pigs, cattle, dogs, and horses. During ~1000–200 BC, wheat and naked barley replaced millet as the major crops".
- ↑ Dong, Liang & Zhang 2024, p. 7: "However, wheat and barley were adopted as important staple in the Hexi Corridor and the northeast Tibetan Plateau during 4000–3600 BP, respectively. This may be due to their adaptability to different altitude environments of these two regions, especially, barley is tolerant to low cumulative temperatures and precipitation, making it well-suited for successful growth in colder climates".
- ↑ Zhang et al. 2017, pp. 93–94: The number of bronze artifacts and sites with smelting relics reached a maximum during Xichengyi (4000–3700 BP), Qijia (4000–3500 BP) and Siba (3700–3400 BP) Bronze Age cultures period, but diminished substantially during Shanma (3000–2400 BP) and Shajing (2800–2400 BP) cultures..
- ↑ Zhou et al. 2012, p. 42: "The subsequent Shajing cultures show evidence of cultural retrogression and site numbers are low until the rise of nomadic tribes after 3000 cal BP".
- ↑ Yang et al. 2020, p. 616: "The agricultural culture was entirely replaced by a pastoral culture, and the numbers of archaeological sites of the subsequent Shajing and Shanma Cultures are significantly smaller than that of the Siba Culture. During the subsequent millennium, Human settlement in the Hexi Corridor remained low, especially during 1350–950 BC".
- ↑ Li et al. 2023, p. 5.
- ↑ Li et al. 2023, Abstract: "In contrast, the Shajing Culture flourished along the lower Shiyang River with the retreat of the Zhuye Lake, the Xiongnu Empire established the city of Xiutu along the Hongshui River, which experienced downcutting linked to the arid environment, and a nomadic culture emerged against the backdrop of drought in the Shiyang River Basin".
- ↑ Reden 2020, p. 76: "Prior to their migration into Bactria, the history of the Yuezhi is only tenuously known from Chinese historical sources, which place their earliest known home in the Gansu corridor".
- ↑ Beckwith 2009, p. 71.
- ↑ Yü 1986, pp. 385–386.
- ↑ Di Cosmo 2002, pp. 190–192.
- ↑ Beckwith 2009, pp. 84–85.
- ↑ Harmatta 1996, p. 172.
- ↑ Kim 2017, p. 1: "At its height, the Xiongnu Empire stretched from the forests of Manchuria in the east to the territory of the Kangju (southern Kazakhstan and northern Uzbekistan) in the west, from the Baikal region (southern Siberia) in the north to the Ordos and Gansu regions of northern China in the south".
- ↑ Declercq 2025, pp. 24-25: "The Yuezhi having been disposed of, the Hexi Corridor — from 176 BCE and for as long as the Han heqin policy lasted (134 BCE) — was undisputedly under Xiongnu control".
- ↑ Sneath & Kaplonski 2010, p. 58.
- 1 2 Yü 1986, p. 391.
- ↑ Harmatta 1996, p. 220.
- ↑ Declercq 2025, pp. 28–29.
- ↑ Benjamin 2018, pp. 102–104.
- ↑ Reden 2020, pp. 73–77, 122.
- ↑ Benjamin 2018, pp. 103–104.
- ↑ Benjamin 2018, p. 100.
- ↑ Declercq 2025, p. 29.
- ↑ Loewe 1986, p. 165.
- ↑ Declercq 2025, p. 4.
- ↑ Yü 1986, p. 434.
- ↑ Yü 1986, pp. 422–425.
- ↑ Di Cosmo 2002, p. 229.
- ↑ Reden 2020, p. 118.
- ↑ Bielenstein 1986, p. 276: "The other powerful man was Tou Jung, another northwesterner. He had from A.D. 24 onward become warlord of the Kansu corridor, and recognized Kuang-wu-ti in 29".
- ↑ Declercq 2025, pp. 31–34.
- ↑ Declercq 2025, p. 48: "Qiang bands pillaged Wuwei, Zhangye and Jiuquan, sometimes even Dunhuang, in 120, 141, 160, 162, 163 ("Liangzhou was almost lost!"), 166, 167, etc".
- ↑ Yü 1986, pp. 425–430.
- ↑ Bielenstein 1986, p. 170.
- ↑ Yü 1986, p. 434.
- ↑ Declercq 2025, pp. 39, 53.
- ↑ Dien & Knapp 2019, pp. 27–28.
- ↑ de Crespigny 2007, pp. 310, 638–639, 650.
- ↑ de Crespigny 2010, p. 258.
- ↑ Dien & Knapp 2019, p. 37.
- ↑ Benjamin 2018, p. 241.
- ↑ Dien & Knapp 2019, p. 40.
- ↑ Killigrew 1999, p. 69.
- ↑ Dien & Knapp 2019, p. 79.
- ↑ Declercq 2025, p. 59.
- ↑ Declercq 2025, p. 61.
- ↑ Reden 2020, pp. 127–133.
- ↑ McLaughlin 2016, p. 102.
- ↑ Reden 2020, pp. 136–137.
- ↑ Beckwith 2009, p. 85, 115.
- ↑ Hansen 2012, p. 4.
- ↑ Dien & Knapp 2019, p. 133.
- ↑ Declercq 2025, p. 65.
- ↑ Dien & Knapp 2019, p. 136, 140,.
- ↑ Declercq 2025, chapters 5, 7, 8, 12, 13.
- ↑ Liu 2022, p. 20.
- ↑ Rong & Galambos 2013, p. 57.
- 1 2 Tse 2018, p. 112.
- ↑ Hansen 2012, p. 172.
- ↑ Liu 2022, pp. 26–28.
- ↑ Soper 1958, pp. 134–143.
- ↑ Soper 1958, p. 143.
- ↑ Rong & Galambos 2013, pp. 26–27.
- ↑ Dien & Knapp 2019, p. 165.
- ↑ Soper 1958, p. 141.
- ↑ Soper 1958, p. 156.
- ↑ Rong & Galambos 2013, pp. 28–29.
- ↑ Rong & Galambos 2013, pp. 29–31.
- ↑ Dien & Knapp 2019, pp. 210–211, 224.
- ↑ Rong & Galambos 2013, p. 31.
- ↑ Twitchett 1979, p. 48: "In the last quarter of the sixth century, China had been politically fragmented for nearly three hundred years - the longest period of disunion in Chinese history. The Sui dynasty brought this period to an end".
- ↑ Liu 2022, p. 27: "When Yang Jian, Emperor Wen set up the Sui Dynasty, he reunited China and ended the separation between south and north for over 3 centuries".
- ↑ Twitchett 1979, p. 122.
- ↑ Xiong 2006, p. 206.
- ↑ Rong & Galambos 2013, p. 32: "In 617 Li Gui 李軌 gathered an army in Wuwei and proclaimed himself King of Liang, bringing Hexi under his control. After the Tang dynasty was established in Chang'an, in 619 the court relied on the powerful Sogdian An 安 clan to destroy Li Gui's rule from the inside. With this, Hexi was annexed to the Tang domain".
- ↑ Xiong 2006, p. 260: "Seventh month [of 617]: Officer Li Gui rebelled in Wuwei, and declared himself prince of Liang".
- ↑ Rong & Galambos 2013, p. 32: "Hence when Xuanzang 玄奘 was starting on his pilgrimage to the West in 627, he left the empire in secret between Guazhou and Dunhuang.".
- ↑ Hansen 2012, pp. 85–86.
- ↑ Rong & Galambos 2013, pp. 32–33.
- ↑ Twitchett 1979, pp. 221–228.
- ↑ Rong & Galambos 2013, pp. 64–67.
- ↑ Twitchett 1979, pp. 285–286.
- ↑ Beckwith 2009, pp. 129–130.
- ↑ Twitchett 1979, pp. 366–367.
- ↑ Rong & Galambos 2013, p. 36.
- ↑ Hansen 2012, p. 190.
- ↑ Rong & Galambos 2013, pp. 37–38.
- ↑ Hansen 2012, p. 185.
- ↑ Hansen 2012, pp. 185–186.
- ↑ Rong & Galambos 2013, pp. 39–40.
- ↑ Tuttle & Schaeffer 2013, pp. 137–138.
- ↑ Tuttle & Schaeffer 2013, p. 130.
- ↑ Rong & Galambos 2013, p. 40.
- ↑ Hansen 2012, pp. 187–188.
- ↑ Rong & Galambos 2013, pp. 42–44.
- ↑ Liu 2022, p. 46.
- ↑ Russell-Smith 2005, pp. 57–58.
- ↑ Rong & Galambos 2013, pp. 43–44.
- ↑ Russell-Smith 2005, p. 63.
- ↑ Rong & Galambos 2013, p. 44.
- ↑ Liu 2022, p. 48.
- ↑ Rong & Galambos 2013, p. 46.
- ↑ Elverskog 2024, pp. 12–14.
- ↑ Russell-Smith 2005, pp. 63–67.
- ↑ Twitchett 1994, p. 179.
- ↑ Rong & Galambos 2013, p. 47.
- ↑ Russell-Smith 2005, p. 73.
- ↑ Rong & Galambos 2013, p. 76.
- ↑ Twitchett 1994, pp. 179–180.
- ↑ Twitchett 1994, pp. 207–208.
- ↑ Twitchett 1994, pp. 210–213, 365.
- ↑ Man 2009, pp. 77–102.
- 1 2 3 Jeans 1992, pp. 142–143.
- ↑ Mote, Twitchett & Fairbank 2007, pp. 100–103.
- ↑ Jeans 1992, p. 74.
- ↑ Rong & Galambos 2013, p. 48.
- ↑ Liu 2022, p. 70.
- 1 2 Liu 2022, p. 72.
- ↑ Mote, Twitchett & Fairbank 2007, p. 248.
- ↑ Jeans 1992, p. 76.
- ↑ Rong & Galambos 2013, p. 81.
- ↑ Wakeman 1985, p. 688.
- ↑ Wakeman 1985, pp. 798–802, 821–827.
- 1 2 Lipman 1997, pp. 54–55.
- ↑ Dzengšeo & Di Cosmo 2006, pp. 15, 24.
- ↑ Wakeman 1985, pp. 1109–1112.
- ↑ Liu 2022, pp. 72–73.
- ↑ Perdue 2005, pp. 313, 329.
- ↑ Perdue 2005, pp. 362–370.
- ↑ Fairbank 1989, pp. 220–221.
- ↑ Fairbank 1989, pp. 234–235.
- ↑ Lipman 1997, p. 128.
- ↑ Hansen 2012, pp. 116–117, 167–175.
- ↑ Rong & Galambos 2013, Lecture 3: "The Discovery of the Dunhuang Cave Library and Its Early Dispersal".
- ↑ Lipman 1997, 5 / Strategies of Integration: Muslims in New China.
- ↑ Croddy 2022, pp. 148–149.
- ↑ "Double-tracking of China's Lanzhou-Xinjiang Railway completed". www.ourchinastory.com. Archived from the original on 30 October 2025. Retrieved 2025-10-30.
- ↑ Centre, UNESCO World Heritage. "Mogao Caves". UNESCO World Heritage Centre. Archived from the original on 30 October 2025. Retrieved 2025-10-30.
- ↑ "Lanxin (Lanzhou−Xinjiang) High-Speed Rail Line". Railway Technology. Archived from the original on 27 August 2025. Retrieved 2025-10-30.
- ↑ 郑成琼. "China to build national heritage route on ancient Silk Road". english.scio.gov.cn. Archived from the original on 30 October 2025. Retrieved 2025-10-30.
- ↑ "China to build national heritage route on ancient Silk Road". regional.chinadaily.com.cn. Archived from the original on 30 October 2025. Retrieved 2025-10-30.
Sources
- Li, Youli; Yang, Jingchun; Tan, Lihua; Duan, Fengjun (July 1999). "Impact of tectonics on alluvial landforms in the Hexi Corridor, Northwest China". Geomorphology. 28 (3–4): 299–308. Bibcode:1999Geomo..28..299L. doi:10.1016/S0169-555X(98)00114-7.
- Zhuang, G.; Hourigan, J. K.; Ritts, B. D.; Kent-Corson, M. L. (2011-02-01). "Cenozoic multiple-phase tectonic evolution of the northern Tibetan Plateau: Constraints from sedimentary records from Qaidam basin, Hexi Corridor, and Subei basin, northwest China". American Journal of Science. 311 (2): 116–152. Bibcode:2011AmJS..311..116Z. doi:10.2475/02.2011.02. ISSN 0002-9599.
- Wang, Weitao; Zhang, Peizhen; Pang, Jianzhang; Garzione, Carmala; Zhang, Huiping; Liu, Caicai; Zheng, Dewen; Zheng, Wenjun; Yu, Jingxing (22 April 2016). "The Cenozoic growth of the Qilian Shan in the northeastern Tibetan Plateau: A sedimentary archive from the Jiuxi Basin". Journal of Geophysical Research: Solid Earth. 121 (4): 2235–2257. Bibcode:2016JGRB..121.2235W. doi:10.1002/2015JB012689. ISSN 2169-9313.
- Bovet, P. M.; Ritts, B. D.; Gehrels, G.; Abbink, A. O.; Darby, B.; Hourigan, J. (2009-04-01). "Evidence of Miocene crustal shortening in the North Qilian Shan from Cenozoic stratigraphy of the western Hexi Corridor, Gansu Province, China". American Journal of Science. 309 (4): 290–329. Bibcode:2009AmJS..309..290B. doi:10.2475/00.4009.02. ISSN 0002-9599.
- Métivier, François; Gaudemer, Yves; Tapponnier, Paul; Meyer, Bertrand (1998). "Northeastward growth of the Tibet plateau deduced from balanced reconstruction of two depositional areas: The Qaidam and Hexi Corridor basins, China". Tectonics. 17 (6): 823–842. Bibcode:1998Tecto..17..823M. doi:10.1029/98tc02764. ISSN 0278-7407.
- Pan, Baotian; Chen, Dianbao; Hu, Xiaofei; Cao, Xilin; Chen, Jinjun; Mao, Junwei (4 September 2016). "Drainage evolution of the Heihe River in western Hexi Corridor, China, derived from sedimentary and magnetostratigraphic results". Quaternary Science Reviews. 150: 250–263. Bibcode:2016QSRv..150..250P. doi:10.1016/j.quascirev.2016.08.036. ISSN 0277-3791.
- Liu, Hailong; Shi, Peiji; Tong, Huali; Zhu, Guofeng; Liu, Haimeng; Zhang, Xuebin; Wei, Wei; Wang, Xinmin (2015). "Characteristics and driving forces of spatial expansion of oasis cities and towns in Hexi Corridor, Gansu Province, China". Chinese Geographical Science. 25 (2): 250–262. Bibcode:2015ChGpS..25..250L. doi:10.1007/s11769-014-0687-0. ISSN 1002-0063.
- Zhang, Zhengcai; Dong, Zhibao; Li, Jiyan; Qian, Guangqiang; Jiang, Chanwen (2016). "Implications of surface properties for dust emission from gravel deserts (gobis) in the Hexi Corridor". Geoderma. 268: 69–77. Bibcode:2016Geode.268...69Z. doi:10.1016/j.geoderma.2016.01.011.
- Nie, Xiaoying; Wang, Chao; Huang, Wanzhuang (2023-11-08). "Evolution and spatial reconstruction of rural settlements based on composite features of agglomeration effect and ecological effects in the Hexi Corridor, Northwest China". PLOS ONE. 18 (11) e0294037. Bibcode:2023PLoSO..1894037N. doi:10.1371/journal.pone.0294037. ISSN 1932-6203. PMC 10631663. PMID 37939090.
- Li, Youli; Yang, Jingchun (1998). "Tectonic geomorphology in the Hexi Corridor, north-west China". Basin Research. 10 (3): 345–352. Bibcode:1998BasR...10..345L. doi:10.1046/j.1365-2117.1998.00070.x. ISSN 1365-2117.
- Zhou, Xuqiang; Wang, Xufeng; Ren, Zhiguo; Zhang, Yang; Tan, Junlei; Nawaz, Zain (2025). "Human activities rather than climate change dominate the growth of carbon fluxes in the Hexi Corridor oasis area, China". Journal of Geographical Sciences. 35 (2): 252–272. Bibcode:2025JGSci..35..252Z. doi:10.1007/s11442-025-2321-8. ISSN 1009-637X.
- Schettler, Georg; Romer, Rolf L.; Qiang, Mingrui; Plessen, Birgit; Dulski, Peter (2009). "Size-dependent geochemical signatures of Holocene loess deposits from the Hexi Corridor (China)". Journal of Asian Earth Sciences. 35 (2): 103–136. Bibcode:2009JAESc..35..103S. doi:10.1016/j.jseaes.2009.01.003.
- Chen, Changyu (1996). "Water resource in Qilian Mountainous region and its influence on eco-environment of Hexi Corridor". Chinese Geographical Science. 6 (3): 247–258. Bibcode:1996ChGpS...6..247C. doi:10.1007/s11769-996-0027-0. ISSN 1002-0063.
- Zhu, Bingqi (2022). "The recent evolution of dune landforms and its environmental indications in the mid-latitude desert area (Hexi Corridor)". Journal of Geographical Sciences. 32 (4): 617–644. Bibcode:2022JGSci..32..617Z. doi:10.1007/s11442-022-1964-y. ISSN 1009-637X.
- Yang, Liu; Shi, Zhilin; Zhang, Shanjia; Lee, Harry F. (5 June 2020). "Climate Change, Geopolitics, and Human Settlements in the Hexi Corridor over the Last 5,000 Years". Acta Geologica Sinica - English Edition. 94 (3): 612–623. Bibcode:2020AcGlS..94..612Y. doi:10.1111/1755-6724.14529. ISSN 1000-9515.
- Zhu, Bing-Qi; Zhang, Jia-Xing; Sun, Chun (2021-08-17). "Physiochemical Characteristics, Provenance, and Dynamics of Sand Dunes in the Arid Hexi Corridor". Frontiers in Earth Science. 9 728202: 726. Bibcode:2021FrEaS...9..726Z. doi:10.3389/feart.2021.728202. ISSN 2296-6463.
- Zhang, Zhengcai; Pan, Kaijia; Zhang, Caixia; Liang, Aiming (2020-07-01). "Geochemical characteristics and the provenance of aeolian material in the Hexi Corridor Desert, China". CATENA. 190 104483. Bibcode:2020Caten.19004483Z. doi:10.1016/j.catena.2020.104483. ISSN 0341-8162.
- Palumbo, Luigi; Hetzel, Ralf; Tao, Mingxin; Li, Xiaobin; Guo, Jianming (2009). "Deciphering the rate of mountain growth during topographic presteady state: An example from the NE margin of the Tibetan Plateau". Tectonics. 28 (4) 2009TC002455. Bibcode:2009Tecto..28.4017P. doi:10.1029/2009TC002455. ISSN 1944-9194.
- Dong, Guanghui; Liang, Huan; Zhang, Zhixiong (2024-09-01). "Human–environment interaction along the eastern Silk Road during the Neolithic and Bronze Age". Palaeogeography, Palaeoclimatology, Palaeoecology. 649 112340. Bibcode:2024PPP...64912340D. doi:10.1016/j.palaeo.2024.112340. ISSN 0031-0182.
- Dong, Guanghui; Yang, Yishi; Liu, Xinyi; Li, Haiming; Cui, Yifu; Wang, Hui; Chen, Guoke; Dodson, John; Chen, Fahu (17 October 2017). "Prehistoric trans-continental cultural exchange in the Hexi Corridor, northwest China". The Holocene. 28 (4): 621–628. doi:10.1177/0959683617735585. ISSN 0959-6836.
- Li, Yu; Gao, Mingjun; Zhang, Zhansen; Duan, Junjie; Xue, Yaxin (2023-04-01). "Phased human-nature interactions for the past 10 000 years in the Hexi Corridor, China". Environmental Research Letters. 18 (4): 044035. Bibcode:2023ERL....18d4035L. doi:10.1088/1748-9326/acc87b. ISSN 1748-9326.
- Stevens, C. J.; Murphy, C.; Roberts, R.; Lucas, L.; Silva, F.; Fuller, D. Q. (2016). "Between China and South Asia: A Middle Asian corridor of crop dispersal and agricultural innovation in the Bronze Age". The Holocene. 26 (10): 1541–1555. Bibcode:2016Holoc..26.1541S. doi:10.1177/0959683616650268. ISSN 0959-6836. PMC 5125436. PMID 27942165.
- Li, Haiming; James, Nathaniel; Chen, Junwei; Zhang, Shanjia; Du, Linyao; Yang, Yishi; Chen, Guoke; Ma, Minmin; Jia, Xin (6 February 2023). "Agricultural Economic Transformations and Their Impacting Factors around 4000 BP in the Hexi Corridor, Northwest China". Land. 12 (2): 425. Bibcode:2023Land...12..425L. doi:10.3390/land12020425. ISSN 2073-445X.
- Li, Xiaoqiang; Dodson, John; Zhou, Xinying; Zhang, Hongbin; Masutomoto, Ryo (5 January 2007). "Early cultivated wheat and broadening of agriculture in Neolithic China". The Holocene. 17 (5): 555–560. Bibcode:2007Holoc..17..555L. doi:10.1177/0959683607078978. ISSN 0959-6836.
- Zhou, Xinying; Li, Xiaoqiang; Dodson, John; Zhao, Keliang; Pia, Atahan; Sun, Nan; Yang, Qing (2012-03-16). "Land degradation during the Bronze Age in Hexi Corridor (Gansu, China)". Quaternary International. Holocene Vegetation Dynamics and Human Impact: Agricultural Activities and Rice Cultivation in East Asia II. 254: 42–48. Bibcode:2012QuInt.254...42X. doi:10.1016/j.quaint.2011.06.046. ISSN 1040-6182.
- Chen, G.; Cui, Y.; Liu, R.; Wang, H.; Yang, Y.; Pollard, A. M.; Li, Y. (4 April 2020). "Lead isotopic analyses of copper ores in the Early Bronze Age central Hexi Corridor, north-west China". Archaeometry. 62 (5): 952–964. Bibcode:2020Archa..62..952C. doi:10.1111/arcm.12566. hdl:21.11116/0000-0006-0FF7-4. ISSN 0003-813X.
- Ren, Lele; Yang, Yishi; Qiu, Menghan; Brunson, Katherine; Chen, Guoke; Dong, Guanghui (2022-08-01). "Direct dating of the earliest domesticated cattle and caprines in northwestern China reveals the history of pastoralism in the Gansu-Qinghai region". Journal of Archaeological Science. 144 105627. Bibcode:2022JArSc.144j5627R. doi:10.1016/j.jas.2022.105627. ISSN 0305-4403.
- Li, Yu; Zhang, Zhansen; Zhou, Xueru; Gao, Mingjun; Li, Haiye; Xue, Yaxin; Duan, Junjie (2023-05-01). "Paleo-environmental changes and human activities in Shiyang River Basin since the Late Glacial". Chinese Science Bulletin (in Chinese). doi:10.1360/tb-2022-0965. ISSN 0023-074X.
- Xie, Yaowen; Bie, Qiang; Lu, Hui; He, Lei (29 November 2018). "Spatio-Temporal Changes of Oases in the Hexi Corridor over the Past 30 Years". Sustainability. 10 (12): 4489. Bibcode:2018Sust...10.4489X. doi:10.3390/su10124489. ISSN 2071-1050.
- Barnes, Ian (2007). Mapping History: World History. London: Cartographica. ISBN 978-1-84573-323-0.
- Yap, Joseph P. (2019), The Western Regions Xiongnu and Han: From the Shiji, Hanshu and Hou Hanshu. ISBN 978-1-79282-915-4
- Liu, Xinru (1 September 2001). "Migration and Settlement of the Yuezhi-Kushan: Interaction and Interdependence of Nomadic and Sedentary Societies". Journal of World History. 12 (2): 261–292. doi:10.1353/jwh.2001.0034. ISSN 1527-8050.
- Beckwith, Christopher I. (2009). Empires of the Silk Road: A History of Central Eurasia from the Bronze Age to the Present. Princeton University Press. ISBN 978-1-4008-2994-1.
- Tang, Xia; Yang, Linshan; Qu, Hao; Feng, Qi (2023-12-01). "The evolution of artificial oasis over two millennia in Hexi corridor, China". Heliyon. 9 (12) e22690. Bibcode:2023Heliy...922690T. doi:10.1016/j.heliyon.2023.e22690. ISSN 2405-8440. PMC 10724675. PMID 38107282.
- Di Cosmo, Nicola (1999). "The Northern Frontier in Pre-Imperial China". In Michael Loewe and Edward Shaughnessy (eds.). The Cambridge History of Ancient China. Cambridge University Press.
- Harmatta, János, ed. (1996). History of civilizations of Central Asia. 2: The development of sedentary and nomadic civilizations: 700 B.C. to A.D. 250 / ed.: János Harmatta (2. impr ed.). Paris: UNESCO Publ. ISBN 978-92-3-102846-5.
- Kim, Hyun Jin (2017-03-29), "The Xiongnu", Oxford Research Encyclopedia of Asian History, doi:10.1093/acrefore/9780190277727.013.50, ISBN 978-0-19-027772-7, retrieved 2025-01-01
- Reden, Sitta von (2020). Handbook of ancient Afro-Eurasian economies. De Gruyter Oldenbourg reference. Berlin: De Gruyter Oldenbourg. ISBN 978-3-11-060451-1.
- Di Cosmo, Nicola; Wyatt, Don J, eds. (2005-08-16). Political Frontiers, Ethnic Boundaries and Human Geographies in Chinese History. Routledge. doi:10.4324/9780203987957. ISBN 978-1-135-79095-0.
- Loewe, Michael (1986), Twitchett, Denis; Loewe, Michael (eds.), "The Former Han dynasty", The Cambridge History of China: Volume 1: The Ch'in and Han Empires, 221 BC–AD 220, The Cambridge History of China, vol. 1, Cambridge: Cambridge University Press, pp. 103–222, doi:10.1017/chol9780521243278.004, ISBN 978-0-521-24327-8, retrieved 2025-06-21
{{citation}}: CS1 maint: work parameter with ISBN (link) - Bielenstein, Hans (1986), Twitchett, Denis; Loewe, Michael (eds.), "Wang Mang, the restoration of the Han dynasty, and Later Han", The Cambridge History of China: Volume 1: The Ch'in and Han Empires, 221 BC–AD 220, The Cambridge History of China, vol. 1, Cambridge: Cambridge University Press, pp. 223–290, doi:10.1017/chol9780521243278.005, ISBN 978-0-521-24327-8, retrieved 2025-06-20
{{citation}}: CS1 maint: work parameter with ISBN (link) - Yü, Ying-Shih (1986-12-26), "Han foreign relations", The Cambridge History of China, Cambridge University Press, pp. 377–462, doi:10.1017/chol9780521243278.008, ISBN 978-1-139-05473-7
{{citation}}: CS1 maint: work parameter with ISBN (link) - Sneath, David; Kaplonski, Christopher (2010-01-01), "Sima Qian (1993) 'The Account of the Xiongnu'", The History of Mongolia (3 Vols.), BRILL, pp. 43–67, doi:10.1163/9789004216358_004, ISBN 978-90-04-21635-8
{{citation}}: CS1 maint: work parameter with ISBN (link) - Di Cosmo, Nicola (2009). "Han Frontiers: Toward an Integrated View". Journal of the American Oriental Society. 129 (2): 199–214. ISSN 0003-0279. JSTOR 40593813.
- Zhang, Shanjia; Yang, Yishi; Storozum, Michael J.; Li, Haiming; Cui, Yifu; Dong, Guanghui (2017). "Copper smelting and sediment pollution in Bronze Age China: A case study in the Hexi corridor, Northwest China". CATENA. 156: 92–101. Bibcode:2017Caten.156...92Z. doi:10.1016/j.catena.2017.04.001. ISSN 0341-8162.
- Benjamin, Craig (2018-04-20). Empires of Ancient Eurasia. Cambridge University Press. doi:10.1017/9781316335567. ISBN 978-1-316-33556-7.
- Strathern, Paul (1994). The silk and spice routes. Exploration by land. New York: New Discovery Books : UNESCO. ISBN 978-0-02-788375-6.
{{cite book}}: CS1 maint: publisher location (link) - Di Cosmo, Nicola (2002-02-25). Ancient China and its Enemies. Cambridge University Press. doi:10.1017/cbo9780511511967. ISBN 978-0-521-77064-4.
- Hansen, Valerie (2021-05-26), "The Classical Silk Road: Trade and Connectivity across Central Asia, 100 BCE–1200 CE", Oxford Research Encyclopedia of Asian History, Oxford University Press, doi:10.1093/acrefore/9780190277727.013.576, ISBN 978-0-19-027772-7, retrieved 2025-05-13
- Christian, David (2000). "Silk Roads or Steppe Roads? The Silk Roads in World History". Journal of World History. 11 (1): 1–26. doi:10.1353/jwh.2000.0004. ISSN 1527-8050.
- Declercq, Dominik, ed. (2025-01-27). A Prince of Martial Splendour in the Sixteen Kingdoms: Li Hao (351-417), Ruler of Western Liang. BRILL. doi:10.1163/9789004727380. ISBN 978-90-04-72738-0.
- Lewis, Mark Edward (2009-07-01). The Early Chinese Empires: Qin and Han. Harvard University Press. doi:10.2307/j.ctv1kmj82j. ISBN 978-0-674-04014-4. JSTOR j.ctv1kmj82j.
- Dien, Albert E.; Knapp, Keith N., eds. (2019). The Cambridge History of China: Volume 2: The Six Dynasties, 220–589. Vol. 2. Cambridge: Cambridge University Press. doi:10.1017/9781139107334. ISBN 978-1-107-02077-1.
- de Crespigny, Rafe (2010-08-18). Imperial Warlord. BRILL. doi:10.1163/ej.9789004185227.i-554. ISBN 978-90-04-18522-7.
- de Crespigny, Rafe (2007-01-01). A Biographical Dictionary of Later Han to the Three Kingdoms (23-220 AD). BRILL. doi:10.1163/ej.9789004156050.i-1311. ISBN 978-90-04-15605-0.
- Dien, Albert E. (2007). Six Dynasties Civilization. Early Chinese civilization series. New Haven: Yale University Press. ISBN 978-0-300-07404-8.
- Killigrew, John (1999). "Zhuge Liang and the Northern Campaign of 228–234". Early Medieval China. 1999 (1): 55–91. doi:10.1179/152991099788199472. ISSN 1529-9104.
- McLaughlin, Raoul (2016). The Roman Empire and the silk routes: the ancient world economy and the empires of Parthia, Central Asia and Han China. Barnsley, South Yorkshire: Pen & Sword History. ISBN 978-1-4738-3374-6.
- Hansen, Valerie (2012). The Silk Road: a new history. Oxford; New York: Oxford University Press. ISBN 978-0-19-515931-8.
- Tse, Wicky W. K. (2018). "Fabricating Legitimacy in a Peripheral Regime: Imperial Loyalism and Regionalism in the Northwestern Borderlands Under the Rule of the Former Liang (301-376)". Early Medieval China. 24 (1): 108–130. doi:10.1353/emc.2018.a943122. ISSN 1946-7842.
- Rong, Xinjiang; Galambos, Imre (2013). Eighteen lectures on Dunhuang. Brill's humanities in China library. Leiden; Boston: Brill. ISBN 978-90-04-25042-0.
- Soper, Alexander C. (1958). "Northern Liang and Northern Wei in Kansu". Artibus Asiae. 21 (2): 131–164. doi:10.2307/3248871. ISSN 0004-3648. JSTOR 3248871.
- Twitchett, Denis (1979). The Cambridge history of China. Vol 3: Sui and T'ang China, 589-906, Part I. Cambridge: Cambridge University Press. ISBN 978-0-521-21446-9.
- Xiong, Victor Cunrui (2006). Emperor Yang of the Sui Dynasty: His Life, Times, and Legacy. SUNY Series in Chinese Philosophy and Culture. Ithaca: State University of New York Press. ISBN 978-0-7914-6587-5.
- Liu, Jinbao (2022). The general theory of Dunhuang studies. Qizhen humanities and social sciences library. Singapore: Springer Singapore. ISBN 978-981-16-9072-3.
- Tuttle, Gray; Schaeffer, Kurtis R. (2013). The Tibetan history reader. New York: Columbia university press. ISBN 978-0-231-14468-1.
- Chang, H. K.; Humes, Bruce (2023). Mapping civilizations across Eurasia. Singapore: Palgrave Macmillan. ISBN 978-981-99-7640-9.
- Russell-Smith, Lilla (2005). Uygur Patronage in Dunhuang: Regional Art Centres on the Northern Silk Road in the Tenth and Eleventh Centuries. Brill's Inner Asian Library. Leiden Boston: BRILL. ISBN 978-90-474-1569-5.
- Twitchett, Denis (1994), Franke, Herbert (ed.), The Cambridge history of China. 6: Alien regimes and border states, 907 - 1368 / ed. by Herbert Franke (Repr ed.), Cambridge: Cambridge Univ. Press, ISBN 978-0-521-24331-5
- Elverskog, Johan (2024). A History of Uyghur Buddhism. New York, NY: Columbia University Press. ISBN 978-0-231-56069-6.
- Man, John (2009). Xanadu: Marco Polo and Europe's discovery of the East. London: Bantam. ISBN 978-0-593-06176-3.
- Mote, Frederick W.; Twitchett, Denis Crispin; Fairbank, John King, eds. (2007). The Ming dynasty, 1368 - 1644; Part 1. The Cambridge history of China / general eds.: Denis Twitchett and John K. Fairbank (Reprinted ed.). Cambridge: Cambridge Univ. Press. ISBN 978-0-521-24332-2.
- Jeans, Roger B. (1992). "The Great Wall of China: From History to Myth. By Arthur Waldron. [Cambridge: Cambridge University Press, 1990. 296 pp. $39.50. ISBN 0 521 36518 X.]". The China Quarterly. 132: 1186–1187. doi:10.1017/s0305741000045719. ISSN 0305-7410.
- Wakeman, Frederic Evans (1985). The Great enterprise: the Manchu reconstruction of imperial order in seventeenth-century China. Berkeley; Los Angeles; London: University of California press. ISBN 978-0-520-04804-1.
- Dzengšeo; Di Cosmo, Nicola (2006). The diary of a Manchu soldier in seventeenth-century China: " my service in the army ". Routledge studies in the early history of Asia. London New York: Routledge. ISBN 978-0-7007-1611-1.
- Perdue, Peter C. (2005). China Marches West: The Qing Conquest of Central Eurasia. Cambridge (Mass.): Harvard University Press. ISBN 978-0-674-01684-2.
- Fairbank, John King, ed. (1989), The Cambridge history of China. 11: Late Ch'ing 1800 - 1911: Pt. 2 / ed. by John K. Fairbank (Authorized Taiwan ed., 2. print ed.), Taipei, Taiwan: Caves Books, ISBN 978-0-521-22029-3
- Lipman, Jonathan Neaman (1997). Familiar strangers: a history of Muslims in Northwest China. Studies on ethnic groups in China. Seattle: University of Washington Press. ISBN 978-0-295-97644-0.
- Croddy, Eric (2022). China's Provinces and Populations: A Chronological and Geographical Survey (1st ed.). Cham: Springer. ISBN 978-3-031-09165-0.
- Qiu, Menghan; Li, Haoran; Lu, Minxia; Yang, Yishi; Zhang, Shanjia; Li, Ruo; Chen, Guoke; Ren, Lele (2022-06-13). "Diversification in Feeding Pattern of Livestock in Early Bronze Age Northwestern China". Frontiers in Ecology and Evolution. 10 908131. Bibcode:2022FrEEv..1008131Q. doi:10.3389/fevo.2022.908131. ISSN 2296-701X.
- Yu, Xinyang; Zhao, Gengxing; Zhao, Weijun; Yan, Tingting; Yuan, Xiujie (2017-05-19). "Analysis of Precipitation and Drought Data in Hexi Corridor, Northwest China". Hydrology. 4 (2): 29. Bibcode:2017Hydro...4...29Y. doi:10.3390/hydrology4020029. ISSN 2306-5338.
- Ma, Yali; Niu, Zuirong; Sun, Dongyuan; Wang, Xingfan (2024-09-12). "Spatiotemporal evolution of dry and wet and quantitative analysis of the influence of meteorological factors based on MI and the FAO P–M model". Scientific Reports. 14 (1): 21343. Bibcode:2024NatSR..1421343M. doi:10.1038/s41598-024-72183-8. ISSN 2045-2322. PMC 11393096. PMID 39266590.
- Wang, Qian; Yan, Zhengang; Li, Wei (2026-03-03). "Synergistic Optimization of Land Use and Ecosystem Services in Arid Regions: Scenario Simulation of the Hexi Corridor Based on the PLUS Model". Land. 15 (3): 414. Bibcode:2026Land...15..414W. doi:10.3390/land15030414. ISSN 2073-445X.
- Zhu, Hanshou; Zhai, Jun; Hou, Peng; Gao, Haifeng; He, Yingli; Jin, Diandian; Xu, Ningning (2022-09-27). "Divergent trends of ecosystem status and services in the Hexi Corridor". Frontiers in Environmental Science. 10 1008441. Bibcode:2022FrEnS..1008441Z. doi:10.3389/fenvs.2022.1008441. ISSN 2296-665X.
- Li, Yanzhen; Zhang, Rui; Long, Hao; Cheng, Peng; Kemp, David B.; Zhang, Ze; Huang, Chunju; Hou, Mengyang; Li, Yue; Jia, Shizhen; Wang, Zhixiang; Tan, Liangcheng (2023). "Climate changes in the Hexi Corridor, western China over the past 13.3 ka". Palaeogeography, Palaeoclimatology, Palaeoecology. 622 111605. Bibcode:2023PPP...62211605L. doi:10.1016/j.palaeo.2023.111605.
- Chen, Dianbao; Yang, Jiaming; Nie, Junsheng; Wang, Fei; Mo, Qinhong; Pan, Baotian (2024-06-15). "Orbital forcing of aridity/humidity fluctuations in the Hexi Corridor and Alxa Plateau, NW China, during the last 1.8 million years". Palaeogeography, Palaeoclimatology, Palaeoecology. 644 112204. Bibcode:2024PPP...64412204C. doi:10.1016/j.palaeo.2024.112204. ISSN 0031-0182.
- Liu, Yang; Shu, Bo (2025-10-02). "Evolution of Hexi Corridor architectural spaces under climate change". npj Heritage Science. 13 (1): 487. doi:10.1038/s40494-025-02053-7. ISSN 3059-3220.