|
|
|
题名
|
作者
|
年代
|
出处
|
被引量
|
| 1 | A preliminary study of chronology for a newly-discovered ancient city and five archaeological sites in Lop Nor, China显示文摘In the past century, it has long been debated in the archeological, historical, geographical, and many other related communities where the capital of the Luolan and Shanshan states was in the Lop Nor region. This paper presents three AMS radiocarbon ages from a newly-discovered ancient city at about 6.3 km to the northwest of the Xiaohe Graveyard, and fifteen new radiocarbon ages from the Loulan (LA), LE, Qieerqiduke, Milan, and Tuyin sites in Lop Nor. The new investigation shows that the age of newly-discovered ancient city is at ca. 440–500 AD, belonging to the Northern Wei Dynasty (386–534 AD). This is about 100–300 years younger than Loulan (ca. 100–230 AD), LE (ca. 230–300 AD), Qieerqiduke (ca. 200 AD), and Tuyin (ca. 100 AD). A wooden beam from Milan fortress is dated to ca. 370 AD, while the age on north wall at west gate of the fortress is younger, around 770 AD, suggesting that its construction time might be at the Tang Dynasty. According to 14C ages, cultural relic style, and the geographical location, the newly-discovered ancient city is probably attributed to 'Zhubin City', as documented in the historical literature. Temporally, we name the city 'ancient Zhubin River City'. However, the characteristics and functions of this ancient city are largely unknown and need more detailed archaeological excavation and investigation in the future. Given its location near the ancient postal relay of Alagan on the crossroad, there is no doubt that the newly-discovered city was at an important geographical position on the Silk Road, no matter whether it was called 'Zhubin City', or 'Lielo City', or the capital of Loulan state–'Yuni City'. Our findings provide new evidence for the temporal and spatial distribution of ancient relic sites and the development of civilization in western China, thus contributing to our understanding of the relationship between human activities and environmental change in the Lop Nor region. | LU HouYuan XIA XunCheng LIU JiaQi QIN XiaoGuang WANG FuBao YIDILISI Abuduresule ZHOU Li Ping MU GuiJin JIAO YingXin LI JingZhi | 2010 | Chinese Science Bulletin2010，55，1： | 8 |
| 2 | Estimation of the rational water area for controlling wind erosion in the dried-up basin of the Ebinur Lake and its effect detection显示文摘埃比纳·莱克区域被描述为“一个格林迷宫”在“ Xinjiang MapRecords:河的记录“然而,在 1910 出版了在这个区域的生态学和环境严重由于人的活动的影响被堕落了在期间最近 40 年。渴起来,有 107.4 km^2 的一个区域的湖盆在它的西北的部分形成,是没有植被,盖住 byunconsolidated 淤泥沉积物,并且在北方 Xinjiang 成为了灰尘天气的主要灰尘来源之一,并且有 4.8x10 ~ 6t 的年度数量的灰尘被大风从有 164 天的 Alataw 山脉差距从这个区域吹一年里的发生的大风。为在弄干起来的湖盆在湖区域和有效地控制的风侵蚀改进生态学的埃比纳·莱克的合理的水区域和流入在在弄干起来的湖盆分析在沉积物的小粒的作文之间的当前的生态的问题和关系以后用水平衡方程被估计并且灰尘天气,和最近的年里的生态的效果被监视。为在弄干起来的湖盆在湖区域和有效地控制的风侵蚀改进生态学的 theEbinur 湖的水区域应该至少是 800 km^2,这被考虑,并且湖应该在 7.92x10 ~ 上的再装的表面流量和地下水的年度体积 8 m^3。 | BAO Anming MU Guijin ZHANG Yi FENG Xianwei CHANG Cun YIN Xiaojun | 2006 | Chinese Science Bulletin2006，51，A01： | 4 |
| 3 | Wind erosion at the dry-up bottom of Aiby Lake-A case study on the source of air dust显示文摘 | Mu Guijin Yan Shun Jilili Abuduwanli | 2002 | Science in China (Series D: Earth Sciences)2002，45，1： | 1 |
| 4 | Human activity during the late Pleistocene in the Lop Nur region, northwest China: Evidence from a buried stone artifact显示文摘The Lop Nur region, in the east part of Tarim Basin, was an important transportation junction between west and east,north and south Eurasia. However, previous studies on prehistoric human activity have concentrated mostly on the Bronze Age,whereas that during the Stone Age remains largely unresearched. Here, we present a new direct evidence of human activity in the late Pleistocene, recorded on a grinding stone buried in a lacustrine sediment section of the Lop Nur region. The grain size distribution of the sediment section indicates that the site was probably in the center of a lake with weak hydrodynamic environment. Therefore, the stone artifact can only be carried to here by people instead of river and it was never move as soon as left here. Results of radiocarbon dating, the evident stratigraphic relations between the stone artifact and the sedimentary formation, indicate that the human activity could extend to approximately 13 ka BP. Furthermore, the results of starch-grain and use-wear analyses suggest that ancient humans gathered seeds of Triticeae, roots, and tubers and used the grinding stone to simply process selected plant as plant foodstuffs during this period. It implies that the environmental conditions in the river delta of the Lop Nur were inhabitable during the late Pleistocene. | Kangkang LI Xiaoguang QIN Xiaoyan YANG Bing XU Lei ZHANG Guijin MU Dong WEI Chunxue WANG Yong WU Xiaohong TIAN Yongchong LIN Wen LI Jiaqi LIU Yinxin JIAO | 2018 | Science China Earth Sciences2018，61，11： | 1 |
| 5 | Characterizing variations in soil particle size distribution in oasis farmlands—A case study of the Cele Oasis显示文摘 | Dongwei Gui Jiaqiang Lei Fanjiang Zeng Guijin Mu Juntao Zhu Hui Wang Qiang Zhang | 2009 | Mathematical and Computer Modelling2009，，11： | 1 |
| 6 | Wind erosion of dry-out lake bottom of Aiby Lake,a case study on the source of air dust显示文摘 | Mu Guijin Yan Shun Jilil Abuduwani He Qing | 2002 | Chinese Science D2002，，： | 1 |
| 7 | Eolovy factor in the modern solenakopleniya in Western Junggar Basin 显示文摘 | Jilili Abuduwali Mu Guijin Mu Guydzhin | 2006 | Soil2006，，4： | 1 |
| 8 | Eolian factor in the process of modern salt accumulation in western Dzungaria, China显示文摘 | Abuduwaili Jilili Guijin Mu | 2006 | Eurasian Soil Science2006，，4： | 1 |
| 9 | Wind erosion at the dry-up bottom of Aiby Lake显示文摘 | Guijin Mu Shun Yan Abuduwanli Jilil Qing He Xuncheng Xai | 2002 | Science in China Series D: Earth Sciences2002，，1： | 1 |
| 10 | Effects of different management intensities on soil quality of farmland during oasis development in southern Tarim Basin, Xinjiang, China显示文摘 | Gui Dongwei Lei Jiaqiang Mu Guijin | 2009 | International Journal of Sustainable Development and World Ecology2009，16，： | 1 |
| 11 | Wind erosion at the dry - up bottom of Aiby Lake - a case study on the source of air dust 显示文摘 | Mu Guijin Yan Shun Jihl Abuduwaili He Qing Xia Xuncheng | 2002 | Sei in China ( Ser D)2002，，： | 1 |
| 12 | Natural and human-induced changes of Western Jungaria landscape (Ebi-Nur Lake region) 显示文摘 | Jilili Abuduvali Mu Guijin | 2004 | Izv Ross Akad Nauk Ser Geogr2004，，5： | 1 |
| 13 | Aeolian activity in the southern Gurbantunggut Desert of China during the last 900 years显示文摘The mineral dust emitted from Central Asia has a significant influence on the global climate system.However,the history and mechanisms of aeolian activity in Central Asia remain unclear,due to the lack of well-dated records of aeolian activity and the intense wind erosion in some of the dust source areas(e.g.,deserts).Here,we present the records of aeolian activity from a sedimentary sequence in the southern Gurbantunggut Desert of China using grain size analysis and optically stimulated luminescence(OSL)dating,based on field sampling in 2019.Specifically,we used eight OSL dates to construct chronological frameworks and applied the end-member(EM)analysis for the grain size data to extract the information of aeolian activity in the southern Gurbantunggut Desert during the last 900 a.The results show that the grain size dataset can be subdivided into three EMs(EM1,EM2,and EM3).The primary modal sizes of these EMs(EM1,EM2,and EM3)are 126.00,178.00,and 283.00μm,respectively.EM1 represents a mixture of the suspension components and saltation dust,while EM2 and EM3 show saltation dust transported over a shorter distance via strengthened near-surface winds,which can be used to trace aeolian activity.Combined with the OSL chronology,our results demonstrate that during the last 900 a,more intensive and frequent aeolian activity occurred during 450-100 a BP(Before Present)(i.e.,the Little Ice Age(LIA)),which was reflected by a higher proportion of the coarse-grained components(EM2+EM3).Aeolian activity decreased during 900-450 a BP(i.e.,the Medieval Warm Period(MWP))and 100 a BP-present(i.e.,the Current Warm Period(CWP)).Intensified aeolian activity was associated with the strengthening of the Siberian High and cooling events at high northern latitudes.We propose that the Siberian High,under the influence of temperature changes at high northern latitudes,controlled the frequency and intensity of aeolian activity in Central Asia.Cooling at high northern latitudes would have significantly enhanced the Siberian High,causing its position to shift southward.Subsequently,the incursion of cold air masses from high northern latitudes resulted in stronger wind regimes and increased dust emissions from the southern Gurbantunggut Desert.It is possible that aeolian activity may be weakened in Central Asia under future global warming scenarios,but the impact of human activities on this region must also be considered. | LI Wen MU Guijin YE Changsheng XU Lishuai LI Gen | 2023 | Journal of Arid Land2023，15，6： | 0 |
| 14 | Preliminary studies on the large-scale geomorphic patterns of the complex longitudinal sand ridge zone in the Taklimakan Desert显示文摘Through analysis of satellite images from Google Earth, this article expounds the characteristics of large-scale geomorphic patterns of the complex longitudinal sand ridge zone in the Taklimakan Desert, and reduces the large-scale geomorphic patterns to six types: parallel pattern, '日'character-shaped and '乡' character-shaped pattern, comb-shaped pattern, fork-shaped pattern, toe-shaped pattern and miscellaneous pattern. And according to the large-scale geomorphic pattern type (or composition of pattern types) as well as some other factors, the article divides the complex longitudinal sand ridge zone into 55 subzones. Lastly, aiming at the genetic problems of the large-scale geomorphic patterns, the article suggests three connective types of the sand ridges in the complex longitudinal sand ridge zone, i.e., connecting or intersecting after natural elongation, connecting in a narrow place and connecting with the aid of intermediary. | YUE Jian LEI JiaQiang MU GuiJin | 2008 | Chinese Science Bulletin2008，53，S2： | 0 |
您所在的机构暂未开通此部分的功能，请联系管理员