[Objective] The aim was to investigate the genetic diversity and analyze the genetic differentiation of germplasm resources of Gentiana officinalis H.Smith from Qinghai.[Method] The cpDNA of chloroplast psbA-trnH gene...[Objective] The aim was to investigate the genetic diversity and analyze the genetic differentiation of germplasm resources of Gentiana officinalis H.Smith from Qinghai.[Method] The cpDNA of chloroplast psbA-trnH gene was sequenced to analyze the genetic diversity of six populations of G.officinalis.[Result] A total of 10 distinct haplotypes were detected in the studied populations,and seven variable sites were found by comparing their sequences.G.officinalis with high-level genetic diversity（h=0.771）.Genetic diversity was largely varied within populations,ranging from 0.563 to 0.857 for haplotype diversity,and from 0.002 43 to 0.005 83 for nucleotide diversity,respectively.Genetic differentiation among populations（Gst） of G.officinalis was 0.196 0;gene flow（Nm） was 2.05;80.40% of the genetic variability occurred within population.[Conclusion] The cultivated G.officinalis in Qinghai showed rich genetic diversity,which is beneficial for the production of high-quality herb medicine.展开更多
The features of physical geography in the transitional region between Qinling Mountains and Huanghuai Plain possess transitional characters evidently in two directions: one is from the western mountain to the eastern ...The features of physical geography in the transitional region between Qinling Mountains and Huanghuai Plain possess transitional characters evidently in two directions: one is from the western mountain to the eastern plain and the other is from southern subtropical zone to northern temperate zone. Torrential rain, especially strong torrential rain is frequent in the transitional region, and there are many torrential rain centers. A majority of torrential rain is distributed among 100-200 m asl. The winter temperature at 100-400 m asl is higher than that in Huanghuai Plain whose altitude is lower than that of the transitional region, and the highest temperature in January appears at 350-400 m asl.The thickness of warm slope belt in the transitional region varies from 100 m to 250 m asl. The formation of torrential rain and warm slope belt is the result of joint action of atmospheric circulation and local terrain. Frequent torrential rains and warm slope belt had tremendous influences on the soil properties, plant distribution and local climate in the transitional region.展开更多
基金Supported by Science Foundation for the Excellent Youth and Middle-aged Scholars in Qinghai University(2009-QY-19)~~
文摘[Objective] The aim was to investigate the genetic diversity and analyze the genetic differentiation of germplasm resources of Gentiana officinalis H.Smith from Qinghai.[Method] The cpDNA of chloroplast psbA-trnH gene was sequenced to analyze the genetic diversity of six populations of G.officinalis.[Result] A total of 10 distinct haplotypes were detected in the studied populations,and seven variable sites were found by comparing their sequences.G.officinalis with high-level genetic diversity（h=0.771）.Genetic diversity was largely varied within populations,ranging from 0.563 to 0.857 for haplotype diversity,and from 0.002 43 to 0.005 83 for nucleotide diversity,respectively.Genetic differentiation among populations（Gst） of G.officinalis was 0.196 0;gene flow（Nm） was 2.05;80.40% of the genetic variability occurred within population.[Conclusion] The cultivated G.officinalis in Qinghai showed rich genetic diversity,which is beneficial for the production of high-quality herb medicine.
文摘The features of physical geography in the transitional region between Qinling Mountains and Huanghuai Plain possess transitional characters evidently in two directions: one is from the western mountain to the eastern plain and the other is from southern subtropical zone to northern temperate zone. Torrential rain, especially strong torrential rain is frequent in the transitional region, and there are many torrential rain centers. A majority of torrential rain is distributed among 100-200 m asl. The winter temperature at 100-400 m asl is higher than that in Huanghuai Plain whose altitude is lower than that of the transitional region, and the highest temperature in January appears at 350-400 m asl.The thickness of warm slope belt in the transitional region varies from 100 m to 250 m asl. The formation of torrential rain and warm slope belt is the result of joint action of atmospheric circulation and local terrain. Frequent torrential rains and warm slope belt had tremendous influences on the soil properties, plant distribution and local climate in the transitional region.
