1 Geography Location At 16：30 on August 3rd, 2014, Ludian County, Zhaotong City, Yunnan Province （27.1°N, 103.3°E） was hit by Ms 6.5 earthquake, with the maximum intensity is 9 and epicenter depth is aro...1 Geography Location At 16：30 on August 3rd, 2014, Ludian County, Zhaotong City, Yunnan Province （27.1°N, 103.3°E） was hit by Ms 6.5 earthquake, with the maximum intensity is 9 and epicenter depth is around 12 km （Figs. 1 and 2）.展开更多
DEAR EDITOR, The sun bear, Helarctos malayanus （Raffles, 1821）, is a forest- dependent bear species distributed in tropical Southeast Asia. The species was previously reported from scattered localities in southweste...DEAR EDITOR, The sun bear, Helarctos malayanus （Raffles, 1821）, is a forest- dependent bear species distributed in tropical Southeast Asia. The species was previously reported from scattered localities in southwestern China, which is at the northeastern edge of its global range. Due to the scarcity of reliable recent records, some authorities cast doubt on the continued existence of sun bear in China. Here we present the rediscovery of this species in Yingjiang County, western Yunnan Province, China, near the international border with Myanmar＇s Kachin State.展开更多
On the investigation of the biodiverisities of plant resources of Nujiang River Valley in Nujiang Autonomous Prefacure, Yunnan Province, China, a new species of Ehretia has been described and illustrated as Ehretia re...On the investigation of the biodiverisities of plant resources of Nujiang River Valley in Nujiang Autonomous Prefacure, Yunnan Province, China, a new species of Ehretia has been described and illustrated as Ehretia retroserrata in the arid valley of Nujiang according to the new living state of erect shrub and the characteristics of serrate leave margin, retrose, apiculate, endocarp divided at maturity into 4 1-seeded pyrene and serrate leaves margins by comparison with other species of the genus Ehretia.展开更多
Geotectonically, the Shuikou ultrabasic-basic rock mass is located on the western margin of the Yangtze Platform. As revealed by field geological surveys, the Shuikou rock mass intrudes into the quartz sandstones of t...Geotectonically, the Shuikou ultrabasic-basic rock mass is located on the western margin of the Yangtze Platform. As revealed by field geological surveys, the Shuikou rock mass intrudes into the quartz sandstones of the Sinian Chengjiang Formation (Zac). It is dominated by pyroxenites and can be roughly divided into four lithofacies zones, namely gabbros at the outermost periphery and fine-, medium-, and coarse-grained pyroxenites from margin to center. With the transition from pyroxenites to gabbros, the Shuikou rock mass features gradual enrichment in silica and alkali overall, an increase in ΣREE and (La/Yb)<sub>N</sub> ratio, and a decrease in δEu values and Eu/Sm ratio, indicating that the Shuikou rock mass was formed from the continuous differentiation and crystallization of consanguineous magma and that low-degree partial melting occurred meanwhile. According to the U-Pb baddeleyite geochronology, the crystallization age of the Shuikou rock mass is 210.7 ± 3 Ma (MSWD = 1.01). Based on this, as well as the analysis of geochemical characteristics, the Shuikou rock mass occurred in a continental intraplate tensional environment, this is closely related to the activities of the Emeishan mantle plume during the same period.展开更多
Through studies on the element geochemistry, alteration of country rocks, ore-forming fluids and isotopegeochemistry of the Arno tin deposit in the metamorphic rocks of the Upper Proterozoic Ximeng Group, theauthors c...Through studies on the element geochemistry, alteration of country rocks, ore-forming fluids and isotopegeochemistry of the Arno tin deposit in the metamorphic rocks of the Upper Proterozoic Ximeng Group, theauthors consider that the concentration of the B-F-Li-Rb-Cs-Sn association is related to acidic magmatism inthe study area. The Fe-Mg-Li tourmaline in the ore is the replaced product of the country rocks byhypothermal fluid. The δ^(18)O values of mineral separates are +2.01- +13.16‰ and their δ^(34)S values, +2.6-+7.2‰. The ore-forming materials were derived from hydrothermal fluid of granitic magma. For themineralization, the temperature is 450°-350℃, the pressure, 450-1000×10~5 Pa, and the age, Himalayan(21.5 Ma). According to the geochemical characteristics, a minerogenic model is established: the deposit is ahypothermal cassiterite-quartz vein type tin deposit controlled by the hidden Himalayan granites.展开更多
[Objectives]This study was conducted to clarify the pathogens causing suspected sugarcane leaf scald symptoms in sugarcane plants found in the Xinping sugarcane area of Yunnan in 2019.[Methods]The XAF1/XAR1 specific p...[Objectives]This study was conducted to clarify the pathogens causing suspected sugarcane leaf scald symptoms in sugarcane plants found in the Xinping sugarcane area of Yunnan in 2019.[Methods]The XAF1/XAR1 specific primers of Xanthomonas albilineans were used to detect 8 suspected samples from Xinping County,Yunnan Province.[Results]The specific band 600 bp in size was detected.The sequencing results showed that the sequences detected were all 608 bp,and were 100%identical.The BLAST search results showed that the obtained sequence was 100%identical to the nucleotide sequence of X.albilineans GPE PC73 strain(GenBank accession number:FP565176)from France,and they were located in the same branch of the phylogenetic tree.According to the field symptom diagnosis and molecular identification results,the sugarcane disease in Xinping,Yunnan was confirmed to be the quarantine disease sugarcane leaf scald caused by X.allbilineasn.[Conclusions]The pathogens were identified by molecular biological identification methods,providing a scientific basis for the prevention and control of leaf scald disease in the future.展开更多
A new species of </span><i><span style="font-family:Verdana;">Gentiana</span></i><span style="font-family:Verdana;"> (</span><i><span style="...A new species of </span><i><span style="font-family:Verdana;">Gentiana</span></i><span style="font-family:Verdana;"> (</span><i><span style="font-family:Verdana;">Gentianaceae</span></i><span style="font-family:Verdana;">), </span><i><span style="font-family:Verdana;">Gentiana</span></i> <i><span style="font-family:Verdana;">ciliolata</span></i> <span style="font-family:Verdana;">is</span><span style="font-family:Verdana;"> described and illustrated;it has a spectacular characteristics of calyx lobe ciliolate, distributed in Yunnan and Sichuan Provinces on the two sides of Jinsha River, and then two subspecies have been further re-classified as </span><i><span style="font-family:Verdana;">Gentiana</span></i> <i><span style="font-family:Verdana;">ciliolata</span></i> <span style="font-family:Verdana;">subsp</span><i><span style="font-family:Verdana;">.</span></i> <i><span style="font-family:Verdana;">ciliolata</span></i> <span style="font-family:Verdana;">and </span><i><span style="font-family:Verdana;">Gentiana</span></i> <i><span style="font-family:Verdana;">ciliolata</span></i> <span style="font-family:Verdana;">subsp.</span> <i><span style="font-family:Verdana;">longiloba</span></i> <span style="font-family:Verdana;">respectively</span><i><span style="font-family:Verdana;">.</span></i> <span style="font-family:Verdana;">The subsp.</span> <i><span style="font-family:Verdana;">ciliolata</span></i><span style="font-family:Verdana;"> idistributes</span> <span style="font-family:Verdana;">on the right side of Jinsha River in Yiliang County, Yunnan Province and the subsp</span><i><span style="font-family:Verdana;">.</span></i> <i><span style="font-family:Verdana;">longiloba</span></i><span style="font-family:Verdana;"> distributes itself </span><span style="font-family:Verdana;">on the southwest and west part of Sichuan Province, such as Leibo County, Wenchuan County and Mabian Yi Autonomous Prefacture, in the grassland under forests and moist rock slopes at an altitude of 1300 - 3200 m.展开更多
云南省施甸县地形地貌复杂,构造活动强烈,地质环境条件脆弱,加上人类活动的不断扩大,导致滑坡、泥石流和崩塌等地质灾害频发.为了对施甸县地质灾害风险进行综合评估,以RS和GIS技术为支撑,选取7个孕灾稳定性因子、9个致灾危险性因子和5...云南省施甸县地形地貌复杂,构造活动强烈,地质环境条件脆弱,加上人类活动的不断扩大,导致滑坡、泥石流和崩塌等地质灾害频发.为了对施甸县地质灾害风险进行综合评估,以RS和GIS技术为支撑,选取7个孕灾稳定性因子、9个致灾危险性因子和5个脆弱性因子,分别从孕灾环境稳定性、致灾因子危险性、承灾体脆弱性3方面出发,采用信息量模型+逻辑回归模型(I+LR)和确定性系数模型+逻辑回归模型(CF+LR)2种组合模型对施甸县孕灾环境稳定性进行评价;采用层次分析法(analytic hierarchy process,AHP)和最小二乘法(ordinary least squares,OLS)2种模型对施甸县致灾因子危险性进行评价;采用层次分析法(AHP)对施甸县承灾体脆弱性进行评价,并对施甸县地质灾害风险进行综合评估.结果表明:施甸县综合风险较高区多集中在县域中部地区,其中甸阳镇、仁和镇和由旺镇最为明显,施甸县约10%的区域属于孕灾环境动荡区,约5%的区域属于致灾因子极高危险区,约12%的区域属于承灾环境危险区.对比分析了多种综合模型的评价精度与适用性,发现信息量模型与确定性系数模型评价结果相差较小,均适用于孕灾环境稳定性评价,最小二乘法评价模型ROC曲线AUC值为0.756,略高于层次分析法.展开更多
文摘1 Geography Location At 16：30 on August 3rd, 2014, Ludian County, Zhaotong City, Yunnan Province （27.1°N, 103.3°E） was hit by Ms 6.5 earthquake, with the maximum intensity is 9 and epicenter depth is around 12 km （Figs. 1 and 2）.
基金the Yingjiang County Propaganda Departmentthe Forestry Bureau
文摘DEAR EDITOR, The sun bear, Helarctos malayanus （Raffles, 1821）, is a forest- dependent bear species distributed in tropical Southeast Asia. The species was previously reported from scattered localities in southwestern China, which is at the northeastern edge of its global range. Due to the scarcity of reliable recent records, some authorities cast doubt on the continued existence of sun bear in China. Here we present the rediscovery of this species in Yingjiang County, western Yunnan Province, China, near the international border with Myanmar＇s Kachin State.
文摘On the investigation of the biodiverisities of plant resources of Nujiang River Valley in Nujiang Autonomous Prefacure, Yunnan Province, China, a new species of Ehretia has been described and illustrated as Ehretia retroserrata in the arid valley of Nujiang according to the new living state of erect shrub and the characteristics of serrate leave margin, retrose, apiculate, endocarp divided at maturity into 4 1-seeded pyrene and serrate leaves margins by comparison with other species of the genus Ehretia.
文摘Geotectonically, the Shuikou ultrabasic-basic rock mass is located on the western margin of the Yangtze Platform. As revealed by field geological surveys, the Shuikou rock mass intrudes into the quartz sandstones of the Sinian Chengjiang Formation (Zac). It is dominated by pyroxenites and can be roughly divided into four lithofacies zones, namely gabbros at the outermost periphery and fine-, medium-, and coarse-grained pyroxenites from margin to center. With the transition from pyroxenites to gabbros, the Shuikou rock mass features gradual enrichment in silica and alkali overall, an increase in ΣREE and (La/Yb)<sub>N</sub> ratio, and a decrease in δEu values and Eu/Sm ratio, indicating that the Shuikou rock mass was formed from the continuous differentiation and crystallization of consanguineous magma and that low-degree partial melting occurred meanwhile. According to the U-Pb baddeleyite geochronology, the crystallization age of the Shuikou rock mass is 210.7 ± 3 Ma (MSWD = 1.01). Based on this, as well as the analysis of geochemical characteristics, the Shuikou rock mass occurred in a continental intraplate tensional environment, this is closely related to the activities of the Emeishan mantle plume during the same period.
文摘Through studies on the element geochemistry, alteration of country rocks, ore-forming fluids and isotopegeochemistry of the Arno tin deposit in the metamorphic rocks of the Upper Proterozoic Ximeng Group, theauthors consider that the concentration of the B-F-Li-Rb-Cs-Sn association is related to acidic magmatism inthe study area. The Fe-Mg-Li tourmaline in the ore is the replaced product of the country rocks byhypothermal fluid. The δ^(18)O values of mineral separates are +2.01- +13.16‰ and their δ^(34)S values, +2.6-+7.2‰. The ore-forming materials were derived from hydrothermal fluid of granitic magma. For themineralization, the temperature is 450°-350℃, the pressure, 450-1000×10~5 Pa, and the age, Himalayan(21.5 Ma). According to the geochemical characteristics, a minerogenic model is established: the deposit is ahypothermal cassiterite-quartz vein type tin deposit controlled by the hidden Himalayan granites.
基金Special Fund for Construction of Sugar Crop Research System(CARS-170303)Yunling Industrial Technology Leading Talent Training Project:Sugarcane Pest Control(2018LJRC56)Special Fund for the Construction of Modern Agricultural Industry Technology System in Yunnan Province.
文摘[Objectives]This study was conducted to clarify the pathogens causing suspected sugarcane leaf scald symptoms in sugarcane plants found in the Xinping sugarcane area of Yunnan in 2019.[Methods]The XAF1/XAR1 specific primers of Xanthomonas albilineans were used to detect 8 suspected samples from Xinping County,Yunnan Province.[Results]The specific band 600 bp in size was detected.The sequencing results showed that the sequences detected were all 608 bp,and were 100%identical.The BLAST search results showed that the obtained sequence was 100%identical to the nucleotide sequence of X.albilineans GPE PC73 strain(GenBank accession number:FP565176)from France,and they were located in the same branch of the phylogenetic tree.According to the field symptom diagnosis and molecular identification results,the sugarcane disease in Xinping,Yunnan was confirmed to be the quarantine disease sugarcane leaf scald caused by X.allbilineasn.[Conclusions]The pathogens were identified by molecular biological identification methods,providing a scientific basis for the prevention and control of leaf scald disease in the future.
文摘A new species of </span><i><span style="font-family:Verdana;">Gentiana</span></i><span style="font-family:Verdana;"> (</span><i><span style="font-family:Verdana;">Gentianaceae</span></i><span style="font-family:Verdana;">), </span><i><span style="font-family:Verdana;">Gentiana</span></i> <i><span style="font-family:Verdana;">ciliolata</span></i> <span style="font-family:Verdana;">is</span><span style="font-family:Verdana;"> described and illustrated;it has a spectacular characteristics of calyx lobe ciliolate, distributed in Yunnan and Sichuan Provinces on the two sides of Jinsha River, and then two subspecies have been further re-classified as </span><i><span style="font-family:Verdana;">Gentiana</span></i> <i><span style="font-family:Verdana;">ciliolata</span></i> <span style="font-family:Verdana;">subsp</span><i><span style="font-family:Verdana;">.</span></i> <i><span style="font-family:Verdana;">ciliolata</span></i> <span style="font-family:Verdana;">and </span><i><span style="font-family:Verdana;">Gentiana</span></i> <i><span style="font-family:Verdana;">ciliolata</span></i> <span style="font-family:Verdana;">subsp.</span> <i><span style="font-family:Verdana;">longiloba</span></i> <span style="font-family:Verdana;">respectively</span><i><span style="font-family:Verdana;">.</span></i> <span style="font-family:Verdana;">The subsp.</span> <i><span style="font-family:Verdana;">ciliolata</span></i><span style="font-family:Verdana;"> idistributes</span> <span style="font-family:Verdana;">on the right side of Jinsha River in Yiliang County, Yunnan Province and the subsp</span><i><span style="font-family:Verdana;">.</span></i> <i><span style="font-family:Verdana;">longiloba</span></i><span style="font-family:Verdana;"> distributes itself </span><span style="font-family:Verdana;">on the southwest and west part of Sichuan Province, such as Leibo County, Wenchuan County and Mabian Yi Autonomous Prefacture, in the grassland under forests and moist rock slopes at an altitude of 1300 - 3200 m.
文摘云南省施甸县地形地貌复杂,构造活动强烈,地质环境条件脆弱,加上人类活动的不断扩大,导致滑坡、泥石流和崩塌等地质灾害频发.为了对施甸县地质灾害风险进行综合评估,以RS和GIS技术为支撑,选取7个孕灾稳定性因子、9个致灾危险性因子和5个脆弱性因子,分别从孕灾环境稳定性、致灾因子危险性、承灾体脆弱性3方面出发,采用信息量模型+逻辑回归模型(I+LR)和确定性系数模型+逻辑回归模型(CF+LR)2种组合模型对施甸县孕灾环境稳定性进行评价;采用层次分析法(analytic hierarchy process,AHP)和最小二乘法(ordinary least squares,OLS)2种模型对施甸县致灾因子危险性进行评价;采用层次分析法(AHP)对施甸县承灾体脆弱性进行评价,并对施甸县地质灾害风险进行综合评估.结果表明:施甸县综合风险较高区多集中在县域中部地区,其中甸阳镇、仁和镇和由旺镇最为明显,施甸县约10%的区域属于孕灾环境动荡区,约5%的区域属于致灾因子极高危险区,约12%的区域属于承灾环境危险区.对比分析了多种综合模型的评价精度与适用性,发现信息量模型与确定性系数模型评价结果相差较小,均适用于孕灾环境稳定性评价,最小二乘法评价模型ROC曲线AUC值为0.756,略高于层次分析法.
