Luminescence dating of a hearth from the archaeological site of Jiangxigou in the Qinghai Lake area of the northeastern Qinghai-Tibetan Plateau

Abstract As a daily utensil and artefact, the presence of ceramic at an archaeological site is direct evidence of human activity. While ceramics have been found at numerous sites on the Qinghai-Tibetan Plateau (QTP), most have been aged using conventional methods such as typology or radiocarbon dating of associated charcoal and bone. In this study, five sand-tempered grey ceramics from Talitaliha in the Qaidam Basin were dated using quartz and K-feldspar OSL. The reliability of the ceramic OSL ages was determined using six independent radiocarbon samples, three charcoal and three bone, from the same cultural layer. Six additional OSL ages were determined on sandy loess sediments at the Talitaliha site to provide upper and lower limits for the ceramic ages. The ceramic luminescence dating results are in good agreement with the 14C ages and are within the constraints of the stratigraphic OSL ages, suggesting that OSL dating of ceramics has great potential for archaeological research on the QTP. The determined age range for the Talitaliha site was between 3400–2800 cal BP; this fits well with Nuomuhong culture dates from other locations in the Qaidam Basin that range between 3400–2450 cal BP.

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Luminescence Dating of Relics in Ancient Cities Provides Absolute Dates for Understanding Human-Land Relationships in Qinghai Lake Basin, Northeastern Tibetan Plateau

Frontiers in Earth Science ◽

10.3389/feart.2021.701037 ◽

2021 ◽

Vol 9 ◽

Author(s):

Manping Sun ◽

Yongjuan Sun ◽

Haicheng Wei ◽

Guangliang Hou ◽

Ji Xianba ◽

...

Keyword(s):

Tibetan Plateau ◽

Ming Dynasty ◽

Han Dynasty ◽

Central China ◽

Qinghai Lake ◽

Lake Basin ◽

Lake Area ◽

Northeastern Tibetan Plateau ◽

Southern And Northern Dynasties ◽

Qinghai Lake Basin

The study of ancient city sites provides valuable evidence for understanding human-land relationships. Qinghai Lake Basin, on the northeastern Tibetan Plateau, was a key location for economic and cultural exchanges between East and West in ancient China and archaeological surveys have identified the remains of many ancient cities. Although there are relatively good historical records for some ancient cities, their absolute ages are still unclear due to a lack of systematic chronological dating. In this study, OSL dating of ceramic and tile remains from three ancient cities in Qinghai Lake Basin, Xihaijun (XHJGC), Beixiangyang (BXYGC), and Fuxi (FSC), was combined with documentary and paleoclimate evidence to investigate historical human-land relationships. Relics from XHJGC and BXYGC were dated to 0–220 AD, in the Han Dynasty, while tiles from FSC were dated to 120–520 AD, largely corresponding to the Wei Jin Southern and Northern Dynasties. Luminescence ages were generally consistent with dates recorded in historical documents, indicating that the OSL method can be reliably used to date buried tiles in ancient cities on the northeastern Tibetan Plateau. Comparing the dates with paleoclimatic records suggests that the warm and humid climate at c. 2 ka was an important driver of immigration to the region that led to the construction of cities in the Qinghai Lake area during the late Western Han Dynasty. During the Wei Jin Southern and Northern Dynasties (220–589 AD), communication between East and the West flourished, and human activities in the area were strong with the continuation of the war in Central China and Hexi Corridor. Fuxi was largely abandoned in the later Wei Jin Southern and Northern Dynasties, although it was still used intermittently until the Ming Dynasty. Pollen records confirm that humans were extensively engaged in agricultural production in the Qinghai Lake area during the Wei Jin Southern and Northern Dynasties.

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When did prehistoric human beings migrate to the harsh eastern Tibetan Plateau: luminescence and 14C dating results from Qinghai Lake area

Quaternary International ◽

10.1016/j.quaint.2012.08.1610 ◽

2012 ◽

Vol 279-280 ◽

pp. 477

Author(s):

Yongjuan Sun

Keyword(s):

Tibetan Plateau ◽

Qinghai Lake ◽

Lake Area ◽

Human Beings ◽

Eastern Tibetan Plateau ◽

14C Dating

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Luminescence chronology of aeolian deposits from the Qinghai Lake area in the Northeastern Qinghai-Tibetan Plateau and its palaeoenvironmental implications

Quaternary Geochronology ◽

10.1016/j.quageo.2012.01.016 ◽

2012 ◽

Vol 10 ◽

pp. 37-43 ◽

Cited By ~ 61

Author(s):

XiangJun Liu ◽

ZhongPing Lai ◽

LuPeng Yu ◽

YongJuan Sun ◽

David Madsen

Keyword(s):

Tibetan Plateau ◽

Qinghai Lake ◽

Lake Area ◽

Aeolian Deposits

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Evaluation of land use sustainability in Qinghai Lake area

CHINESE JOURNAL OF ECO-AGRICULTURE ◽

10.3724/sp.j.1011.2009.01017 ◽

2009 ◽

Vol 17 (5) ◽

pp. 1017-1022 ◽

Cited By ~ 2

Author(s):

Wen-Zheng YU ◽

Fu-Tian QU ◽

Ying-Xiang QI ◽

Guo-Feng YU ◽

Jun SHI

Keyword(s):

Land Use ◽

Qinghai Lake ◽

Lake Area

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Carbon Dynamics in the Northeastern Qinghai–Tibetan Plateau from 1990 to 2030 Using Landsat Land Use/Cover Change Data

Remote Sensing ◽

10.3390/rs12030528 ◽

2020 ◽

Vol 12 (3) ◽

pp. 528 ◽

Cited By ~ 1

Author(s):

Jingye Li ◽

Jian Gong ◽

Jean-Michel Guldmann ◽

Shicheng Li ◽

Jie Zhu

Keyword(s):

Land Use ◽

Tibetan Plateau ◽

Carbon Storage ◽

Sharp Decrease ◽

Total Carbon ◽

Qinghai Lake ◽

Lake Basin ◽

Ecosystem Carbon ◽

Trade Offs ◽

The Impact

Land use/cover change (LUCC) has an important impact on the terrestrial carbon cycle. The spatial distribution of regional carbon reserves can provide the scientific basis for the management of ecosystem carbon storage and the formulation of ecological and environmental policies. This paper proposes a method combining the CA-based FLUS model and the Integrated Valuation of Ecosystem Services and Trade-offs (InVEST) model to assess the temporal and spatial changes in ecosystem carbon storage due to land-use changes over 1990–2015 in the Qinghai Lake Basin (QLB). Furthermore, future ecosystem carbon storage is simulated and evaluated over 2020–2030 under three scenarios of natural growth (NG), cropland protection (CP), and ecological protection (EP). The long-term spatial variations in carbon storage in the QLB are discussed. The results show that: (1) Carbon storage in the QLB decreased at first (1990–2000) and increased later (2000–2010), with total carbon storage increasing by 1.60 Tg C (Teragram: a unit of mass equal to 1012 g). From 2010 to 2015, carbon storage displayed a downward trend, with a sharp decrease in wetlands and croplands as the main cause; (2) Under the NG scenario, carbon reserves decrease by 0.69 Tg C over 2020–2030. These reserves increase significantly by 6.77 Tg C and 7.54 Tg C under the CP and EP scenarios, respectively, thus promoting the benign development of the regional ecological environment. This study improves our understanding on the impact of land-use change on carbon storage for the QLB in the northeastern Qinghai–Tibetan Plateau (QTP).

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Contrasting Evolution Patterns of Endorheic and Exorheic Lakes on the Central Tibetan Plateau and Climate Cause Analysis during 1988–2017

Water ◽

10.3390/w13141962 ◽

2021 ◽

Vol 13 (14) ◽

pp. 1962

Author(s):

Zhilong Zhao ◽

Yue Zhang ◽

Zengzeng Hu ◽

Xuanhua Nie

Keyword(s):

Climate Change ◽

Tibetan Plateau ◽

Climatic Factors ◽

Global Climate ◽

Rapid Expansion ◽

Annual Precipitation ◽

The Tibetan Plateau ◽

Lake Area ◽

Climate Change Research ◽

Mean Temperature

The alpine lakes on the Tibetan Plateau (TP) are indicators of climate change. The assessment of lake dynamics on the TP is an important component of global climate change research. With a focus on lakes in the 33° N zone of the central TP, this study investigates the temporal evolution patterns of the lake areas of different types of lakes, i.e., non-glacier-fed endorheic lakes and non-glacier-fed exorheic lakes, during 1988–2017, and examines their relationship with changes in climatic factors. From 1988 to 2017, two endorheic lakes (Lake Yagenco and Lake Zhamcomaqiong) in the study area expanded significantly, i.e., by more than 50%. Over the same period, two exorheic lakes within the study area also exhibited spatio-temporal variability: Lake Gaeencuonama increased by 5.48%, and the change in Lake Zhamuco was not significant. The 2000s was a period of rapid expansion of both the closed lakes (endorheic lakes) and open lakes (exorheic lakes) in the study area. However, the endorheic lakes maintained the increase in lake area after the period of rapid expansion, while the exorheic lakes decreased after significant expansion. During 1988–2017, the annual mean temperature significantly increased at a rate of 0.04 °C/a, while the annual precipitation slightly increased at a rate of 2.23 mm/a. Furthermore, the annual precipitation significantly increased at a rate of 14.28 mm/a during 1995–2008. The results of this study demonstrate that the change in precipitation was responsible for the observed changes in the lake areas of the two exorheic lakes within the study area, while the changes in the lake areas of the two endorheic lakes were more sensitive to the annual mean temperature between 1988 and 2017. Given the importance of lakes to the TP, these are not trivial issues, and we now need accelerated research based on long-term and continuous remote sensing data.

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