In North Xinjiang there is an alkali granite belt extending in the NW-SE direction along the southern band of the Ulungur River and running parallel to the suture zone,i.e.,Aermantai-Zhaheba Ophiolitic Melange Zone ,b...In North Xinjiang there is an alkali granite belt extending in the NW-SE direction along the southern band of the Ulungur River and running parallel to the suture zone,i.e.,Aermantai-Zhaheba Ophiolitic Melange Zone ,between the Junggar Plate and the Altay Orogenic Belt.Whole -rock Rb-Sr isochron ages of the Ulungur alkali granites are within the range of 292-309Ma, showing that they were genetically connected with the latest episode of Hercynian magmatism subsequent to the syncollision S-type and post-collision uplifting I-type granitoids in the Altay region .The alkali granites are miner-alogically characterized by the occurrence of aegirine and arfvedsonite and chemically by high silicon and alkali,low calcium and magnesium and abundant high-field elements, being typical A-type granites .The alkali granites were formed in the final stage of the Hercynian calc-alkaline magmatic cycle in a very short period of time .They are in line with the post-orogenic A-type(PA-type)granites, implying that the tectonic regime was changed from compression to extension.展开更多
More than 200 upper and lower jaws of ochotonid were found in the Late Oligocene of thenorthern part of the Junggar Basin,Xinjiang Uygur Autonomous Region,in the summer of1982.Sinolagomys.a unique Paleogene lagomorph ...More than 200 upper and lower jaws of ochotonid were found in the Late Oligocene of thenorthern part of the Junggar Basin,Xinjiang Uygur Autonomous Region,in the summer of1982.Sinolagomys.a unique Paleogene lagomorph with rootless(?) cheek teeth,was erected byBohlin(1937)based on the collections from Shargaltien and Taben-buluk,Gansu province.Upto now,it has been recorded from Middle Oligocene to the Lower Miocene of Gansu,Ninxia,Nei Mongol,and Xinjiang of China,and the Mongolian People’s Republic.展开更多
根据线粒体12S r RNA基因和S7核糖体蛋白基因内含子1序列,构建额尔齐斯河中11种鲤科鱼类的系统发育树。结果表明:12S基因AT含量与GC含量相当,而S7基因AT含量明显高于GC含量。12S基因保守区分散在整个序列中,而S7基因保守区均集中在前30...根据线粒体12S r RNA基因和S7核糖体蛋白基因内含子1序列,构建额尔齐斯河中11种鲤科鱼类的系统发育树。结果表明:12S基因AT含量与GC含量相当,而S7基因AT含量明显高于GC含量。12S基因保守区分散在整个序列中,而S7基因保守区均集中在前300bp内。12S r RNA和S7基因系统发育树中有三枝聚在一起,即贝加尔雅罗鱼Leuciscus baicalensis与高体雅罗鱼Leuciscus idus,尖鳍鮈Gobio gobio与麦穗鱼Pseudorasbora parva,金鲫Carassius carassius、银鲫Carassius auratus和鲤Cyprinus carpio。12S基因的聚类树中,丁鱥Tinca tinca与雅罗鱼亚科鱼类聚类,表明两者关系密切;而S7基因的聚类树中丁鱥以较高的支持率与尖鳍鮈、麦穗鱼聚在一起,与鮈亚科关系紧密;分子证据支持将丁鱥列入雅罗鱼系。12S基因构建的三种系统发育树拓扑结构有一定差异,而S7基因构建的三种系统发育树基本一致,支持率也高于前者,表明S7构建鲤科系统发育树的优势高于12S。展开更多
文摘In North Xinjiang there is an alkali granite belt extending in the NW-SE direction along the southern band of the Ulungur River and running parallel to the suture zone,i.e.,Aermantai-Zhaheba Ophiolitic Melange Zone ,between the Junggar Plate and the Altay Orogenic Belt.Whole -rock Rb-Sr isochron ages of the Ulungur alkali granites are within the range of 292-309Ma, showing that they were genetically connected with the latest episode of Hercynian magmatism subsequent to the syncollision S-type and post-collision uplifting I-type granitoids in the Altay region .The alkali granites are miner-alogically characterized by the occurrence of aegirine and arfvedsonite and chemically by high silicon and alkali,low calcium and magnesium and abundant high-field elements, being typical A-type granites .The alkali granites were formed in the final stage of the Hercynian calc-alkaline magmatic cycle in a very short period of time .They are in line with the post-orogenic A-type(PA-type)granites, implying that the tectonic regime was changed from compression to extension.
文摘More than 200 upper and lower jaws of ochotonid were found in the Late Oligocene of thenorthern part of the Junggar Basin,Xinjiang Uygur Autonomous Region,in the summer of1982.Sinolagomys.a unique Paleogene lagomorph with rootless(?) cheek teeth,was erected byBohlin(1937)based on the collections from Shargaltien and Taben-buluk,Gansu province.Upto now,it has been recorded from Middle Oligocene to the Lower Miocene of Gansu,Ninxia,Nei Mongol,and Xinjiang of China,and the Mongolian People’s Republic.
