The granitioids in question are located in the geosynclinal fold belt of the Northern Tianshan Mountains.The magmas are intruded into a Carboniferous marine volcanic-sedimentary rock series. forming a contempo-raneous...The granitioids in question are located in the geosynclinal fold belt of the Northern Tianshan Mountains.The magmas are intruded into a Carboniferous marine volcanic-sedimentary rock series. forming a contempo-raneous. intermediate-basic to acid. composite intrusion. With a whole-rock Rb-Sr isochron age of 315.7 Ma. itis considered to be of middle Heicynian age. The granitoids have a SiO_2 content of 48-78%, a calc-alkali indexof 60 and silica-alkali indices ρ=2.2-2.4 and σ=1.5-2. From basic to acid compositions, the total REE con-tent increases from 38 to 143 ppm. δEu ranges from 0.47 to 0.86 and the Eu anomalies are negative. Thenormalized curves of REE of various rock types are very similar. These coupled with the characteristics of traceelement geochemistry show that the intrusion is an island arc-continental margin, calc-alkaline one. Theδ^(18)O values range from 5.8 to 8.9‰ and the ^(87)Sr/^(86)Sr initial ratio is 0.705. The materials of the intrusion arecomposed of a mixture of the magmas at the top of the upper mantle and in the lower crust, This indicates thatthe rocks might be consanguineous. differentiated and evolved products and possess the characteristics of Ⅰtype granites.展开更多
本研究旨在探究饲料中添加不同浓度桑叶水提物(MLWE)对鳜(Siniperca chuatsi)生长性能、脂质代谢、抗氧化性能、肝脏和肠道组织形态的影响。选择经过驯化后的鳜(42.35±0.07) g 540尾,随机分成4组,每组3个重复,每个重复45尾鱼,在基...本研究旨在探究饲料中添加不同浓度桑叶水提物(MLWE)对鳜(Siniperca chuatsi)生长性能、脂质代谢、抗氧化性能、肝脏和肠道组织形态的影响。选择经过驯化后的鳜(42.35±0.07) g 540尾,随机分成4组,每组3个重复,每个重复45尾鱼,在基础配合饲料中分别添加0%(对照组)、0.1%、0.2%和0.5%的MLWE,实验周期为72 d。结果显示:1)与对照组相比,饲料中添加0.1%~0.5%的MLWE不影响鳜的增重率、特定生长率、饲料系数、成活率、脏体指数、肝体指数、肠体指数和肥满度(P>0.05);2)与对照组相比,饲料中添加0.1%的MLWE能够显著降低鳜血清中总胆固醇(T-CHO)和低密度脂蛋白胆固醇(LDL-C)的含量(P<0.05),添加0.2%的MLWE能够显著降低鳜血清中T-CHO、LDL-C和高密度脂蛋白胆固醇(HDL-C)的含量(P<0.05),添加0.5%的MLWE能够显著降低鳜血清中LDL-C和HDL-C的含量(P<0.05);3)与对照组相比,在饲料中添加0.1%和0.2%的MLWE能够显著提高鳜血清超氧化物歧化酶(T-SOD)的活性(P<0.05),添加0.5%的MLWE能够显著提高鳜还原性谷胱甘肽(GSH)的含量以及过氧化氢酶(CAT)和T-SOD的活性(P<0.05);4)与对照组相比,饲料中添加MLWE后,鳜肠道褶皱增多,绒毛数量增加,当MLWE添加浓度为0.5%时,绒毛高度显著高于对照组(P<0.05)。此外,饲料中添加0.1%~0.5%的MLWE都能够改善肝细胞空泡化现象。综上所述,在鳜配合饲料中添加0.1%~0.5%的MLWE不影响鳜的生长性能,但添加适量的MLWE能够提高鳜血清抗氧化能力,改善鳜脂质代谢、肝脏和肠道健康,鳜配合饲料中MLWE的最适添加量为0.5%。展开更多
We made multi-proxy analysis of 14C, grain size, microfossils, plant seeds, and geochemical elements on samples from a profile in the central West Lake of Lop Nur. The grain size suggests relatively stable sedimentary...We made multi-proxy analysis of 14C, grain size, microfossils, plant seeds, and geochemical elements on samples from a profile in the central West Lake of Lop Nur. The grain size suggests relatively stable sedimentary environment around the Medieval Warm Period (MWP) with weak storm effect, which is followed by frequent strong storm events. Abundant microfossils and plant seeds in this stage indicate a warm and humid fresh to brackish lake environment. C, N, and stable elements are high in content in the sediments while Rb/Sr, Ba/Sr, and Ti/Sr are in a steady low level. In addition, plenty of red willows lived here prior to about 700 a B.P., indicating a favorable environmental condition. The results indicate that the environment in Lop Nur and its west bank turned to be favorable at about 2200 a B.P., where the Loulan Culture began to thrive. Then the climate and environment came to be in the good condition in the Tang and Song Dynasties, when the storm effect became weaker, rainfall increased and the salty lake water turned to be brackish to fresh lake water. Hence, limnic biomass increased with higher species diversity.展开更多
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 pape...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.展开更多
文摘The granitioids in question are located in the geosynclinal fold belt of the Northern Tianshan Mountains.The magmas are intruded into a Carboniferous marine volcanic-sedimentary rock series. forming a contempo-raneous. intermediate-basic to acid. composite intrusion. With a whole-rock Rb-Sr isochron age of 315.7 Ma. itis considered to be of middle Heicynian age. The granitoids have a SiO_2 content of 48-78%, a calc-alkali indexof 60 and silica-alkali indices ρ=2.2-2.4 and σ=1.5-2. From basic to acid compositions, the total REE con-tent increases from 38 to 143 ppm. δEu ranges from 0.47 to 0.86 and the Eu anomalies are negative. Thenormalized curves of REE of various rock types are very similar. These coupled with the characteristics of traceelement geochemistry show that the intrusion is an island arc-continental margin, calc-alkaline one. Theδ^(18)O values range from 5.8 to 8.9‰ and the ^(87)Sr/^(86)Sr initial ratio is 0.705. The materials of the intrusion arecomposed of a mixture of the magmas at the top of the upper mantle and in the lower crust, This indicates thatthe rocks might be consanguineous. differentiated and evolved products and possess the characteristics of Ⅰtype granites.
文摘本研究旨在探究饲料中添加不同浓度桑叶水提物(MLWE)对鳜(Siniperca chuatsi)生长性能、脂质代谢、抗氧化性能、肝脏和肠道组织形态的影响。选择经过驯化后的鳜(42.35±0.07) g 540尾,随机分成4组,每组3个重复,每个重复45尾鱼,在基础配合饲料中分别添加0%(对照组)、0.1%、0.2%和0.5%的MLWE,实验周期为72 d。结果显示:1)与对照组相比,饲料中添加0.1%~0.5%的MLWE不影响鳜的增重率、特定生长率、饲料系数、成活率、脏体指数、肝体指数、肠体指数和肥满度(P>0.05);2)与对照组相比,饲料中添加0.1%的MLWE能够显著降低鳜血清中总胆固醇(T-CHO)和低密度脂蛋白胆固醇(LDL-C)的含量(P<0.05),添加0.2%的MLWE能够显著降低鳜血清中T-CHO、LDL-C和高密度脂蛋白胆固醇(HDL-C)的含量(P<0.05),添加0.5%的MLWE能够显著降低鳜血清中LDL-C和HDL-C的含量(P<0.05);3)与对照组相比,在饲料中添加0.1%和0.2%的MLWE能够显著提高鳜血清超氧化物歧化酶(T-SOD)的活性(P<0.05),添加0.5%的MLWE能够显著提高鳜还原性谷胱甘肽(GSH)的含量以及过氧化氢酶(CAT)和T-SOD的活性(P<0.05);4)与对照组相比,饲料中添加MLWE后,鳜肠道褶皱增多,绒毛数量增加,当MLWE添加浓度为0.5%时,绒毛高度显著高于对照组(P<0.05)。此外,饲料中添加0.1%~0.5%的MLWE都能够改善肝细胞空泡化现象。综上所述,在鳜配合饲料中添加0.1%~0.5%的MLWE不影响鳜的生长性能,但添加适量的MLWE能够提高鳜血清抗氧化能力,改善鳜脂质代谢、肝脏和肠道健康,鳜配合饲料中MLWE的最适添加量为0.5%。
基金Supported by the National Natural Science Foundation of China (Grant No. 40701190)the University Doctoral Foundation (Grant No. 20070284067)the Opening Test Foundation of Institute of Earth Environment, CAS and the Test Foun-dation of Modern Analyses Center of Nanjing University
文摘We made multi-proxy analysis of 14C, grain size, microfossils, plant seeds, and geochemical elements on samples from a profile in the central West Lake of Lop Nur. The grain size suggests relatively stable sedimentary environment around the Medieval Warm Period (MWP) with weak storm effect, which is followed by frequent strong storm events. Abundant microfossils and plant seeds in this stage indicate a warm and humid fresh to brackish lake environment. C, N, and stable elements are high in content in the sediments while Rb/Sr, Ba/Sr, and Ti/Sr are in a steady low level. In addition, plenty of red willows lived here prior to about 700 a B.P., indicating a favorable environmental condition. The results indicate that the environment in Lop Nur and its west bank turned to be favorable at about 2200 a B.P., where the Loulan Culture began to thrive. Then the climate and environment came to be in the good condition in the Tang and Song Dynasties, when the storm effect became weaker, rainfall increased and the salty lake water turned to be brackish to fresh lake water. Hence, limnic biomass increased with higher species diversity.
基金supported by the National Natural Science Founda-tion of China (Grant No 40771216)Hundred Talent Program of the Chinese Academy of Sciences and Project of Water Resources in Northwest of China,Chinese Academy of Engineering
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.
