This article aims to study the geomorpometric features of alluvial fans since they act as a small-scale geomorphic unit response to tectonics and climate changes around the Chaka-Qinghai Lake area in the northeastern ...This article aims to study the geomorpometric features of alluvial fans since they act as a small-scale geomorphic unit response to tectonics and climate changes around the Chaka-Qinghai Lake area in the northeastern Tibetan Plateau. We quantitatively extracted geomorphic parameters, such as the surface area and slope of alluvial fans adjacent to the Qinghai Nan Shan and Ela Shan. Alluvial fans in the Chaka Lake partition area, south of the Qinghai Nan Shan, are featured by a small area and short length, but the largest slope. Geomorphic parameters of the alluvial fans in Ela Shan area are in- termediate in size, and the alluvial fans in the Qinghai Lake partition area north of Qinghai Nan Shan have the gentlest slope. Together with the regional faulting activity analysis, we suggest that the alluvial fans with the high slopes in the south of Qinghai Nan Shan are mainly controlled by the reverse faulting along the Qinghai Nan Shan faults, and the strike-slip movement of the Eia Shan fault zone plays a weak role. In contrast, due to the lack of active faults, the alluvial fans near the Qinghai Lake area north of the Qinghai Nan Shan only respond to regional erosion, transportation, and deposition proc- esses, thereby forming relatively gentle geomorphic units.展开更多
Halite precipitation with water and air temperature was observed in detail,and homogenization temperature of fluid inclusions in halite formed in ancient and modem Chaka Salt Lake was studied.Halite precipitates mainl...Halite precipitation with water and air temperature was observed in detail,and homogenization temperature of fluid inclusions in halite formed in ancient and modem Chaka Salt Lake was studied.Halite precipitates mainly in August every year and largely precipitates between 13 and 15pm at one day when water temperatures reach 20℃but can seldom reach 30℃.Homogenization temperatures of fluid inclusions in halite formed in Chaka Salt Lake range from 14℃to 38℃with an average of 23.7℃.The number of inclusions appears an obvious peak value at homogenization temperatures between 18～25℃,which probably represent the water temperature in which halite mainly precipitates when water temperatures reach 20℃.Therefore,homogenization temperatures of fluid inclusions in halite formed in Chaka Salt Lake can well reflect the water temperature.展开更多
【目的】茶卡盐湖(Chaka Salt Lake,CSL)是青藏高原有名的天然结晶盐湖,具有独特的石盐盐湖矿床,盛产青盐。盐湖卤水环境中存在丰富的嗜盐菌资源和潜在的新种,细菌和古菌的群落结构特征和物种多样性尚不明确。【方法】采用Illumina高通...【目的】茶卡盐湖(Chaka Salt Lake,CSL)是青藏高原有名的天然结晶盐湖,具有独特的石盐盐湖矿床,盛产青盐。盐湖卤水环境中存在丰富的嗜盐菌资源和潜在的新种,细菌和古菌的群落结构特征和物种多样性尚不明确。【方法】采用Illumina高通量测序平台对茶卡盐湖水样和底泥混合物中的细菌和古菌群落进行16S r RNA基因(V3-V5区)高通量测序,检测4个样本的群落结构差异和微生物多样性。【结果】获得细菌和古菌总有效序列分别为117 192和110 571条。结果分析表明细菌和古菌的物种注释(Operational taxonomic unit,OTU)数目分别为421和317,获得分类地位明确的细菌种类为14门28纲170属,古菌为5门4纲34属。细菌的优势类群是厚壁菌门(Firmicutes),所占比例为68.37%,其次为变形菌门Proteobacteria(20.49%);优势种属依次为芽孢杆菌属Bacillus(41.94%)、海洋芽孢杆菌属Oceanobacillus(8.03%)、假单胞菌属Pseudomonas(7.67%)、盐厌氧菌属Halanaerobium(7.42%)和乳球菌属Lactococcus(7.38%);古菌的优势类群以广古菌门(Euryarchaeota)盐杆菌纲(Halobacteria)为主,优势菌是Halonotius(17.21%)和盐红菌属Halorubrum(16.23%)。【结论】揭示了茶卡盐湖中细菌和古菌的群落结构及物种多样性,为嗜盐菌的开发及后续微生物资源的挖掘提供了理论依据。展开更多
基金supported by the Fund of the Insti-tute of Geology,CEA(No.IGCEA1115)the National Natural Science Foundation of China(Nos.41203012,41272196)
文摘This article aims to study the geomorpometric features of alluvial fans since they act as a small-scale geomorphic unit response to tectonics and climate changes around the Chaka-Qinghai Lake area in the northeastern Tibetan Plateau. We quantitatively extracted geomorphic parameters, such as the surface area and slope of alluvial fans adjacent to the Qinghai Nan Shan and Ela Shan. Alluvial fans in the Chaka Lake partition area, south of the Qinghai Nan Shan, are featured by a small area and short length, but the largest slope. Geomorphic parameters of the alluvial fans in Ela Shan area are in- termediate in size, and the alluvial fans in the Qinghai Lake partition area north of Qinghai Nan Shan have the gentlest slope. Together with the regional faulting activity analysis, we suggest that the alluvial fans with the high slopes in the south of Qinghai Nan Shan are mainly controlled by the reverse faulting along the Qinghai Nan Shan faults, and the strike-slip movement of the Eia Shan fault zone plays a weak role. In contrast, due to the lack of active faults, the alluvial fans near the Qinghai Lake area north of the Qinghai Nan Shan only respond to regional erosion, transportation, and deposition proc- esses, thereby forming relatively gentle geomorphic units.
基金National Natural Science Foundation of China （Grant No.40373016）.
文摘Halite precipitation with water and air temperature was observed in detail,and homogenization temperature of fluid inclusions in halite formed in ancient and modem Chaka Salt Lake was studied.Halite precipitates mainly in August every year and largely precipitates between 13 and 15pm at one day when water temperatures reach 20℃but can seldom reach 30℃.Homogenization temperatures of fluid inclusions in halite formed in Chaka Salt Lake range from 14℃to 38℃with an average of 23.7℃.The number of inclusions appears an obvious peak value at homogenization temperatures between 18～25℃,which probably represent the water temperature in which halite mainly precipitates when water temperatures reach 20℃.Therefore,homogenization temperatures of fluid inclusions in halite formed in Chaka Salt Lake can well reflect the water temperature.
文摘【目的】茶卡盐湖(Chaka Salt Lake,CSL)是青藏高原有名的天然结晶盐湖,具有独特的石盐盐湖矿床,盛产青盐。盐湖卤水环境中存在丰富的嗜盐菌资源和潜在的新种,细菌和古菌的群落结构特征和物种多样性尚不明确。【方法】采用Illumina高通量测序平台对茶卡盐湖水样和底泥混合物中的细菌和古菌群落进行16S r RNA基因(V3-V5区)高通量测序,检测4个样本的群落结构差异和微生物多样性。【结果】获得细菌和古菌总有效序列分别为117 192和110 571条。结果分析表明细菌和古菌的物种注释(Operational taxonomic unit,OTU)数目分别为421和317,获得分类地位明确的细菌种类为14门28纲170属,古菌为5门4纲34属。细菌的优势类群是厚壁菌门(Firmicutes),所占比例为68.37%,其次为变形菌门Proteobacteria(20.49%);优势种属依次为芽孢杆菌属Bacillus(41.94%)、海洋芽孢杆菌属Oceanobacillus(8.03%)、假单胞菌属Pseudomonas(7.67%)、盐厌氧菌属Halanaerobium(7.42%)和乳球菌属Lactococcus(7.38%);古菌的优势类群以广古菌门(Euryarchaeota)盐杆菌纲(Halobacteria)为主,优势菌是Halonotius(17.21%)和盐红菌属Halorubrum(16.23%)。【结论】揭示了茶卡盐湖中细菌和古菌的群落结构及物种多样性,为嗜盐菌的开发及后续微生物资源的挖掘提供了理论依据。
