南海常见硬骨鱼类COⅠ条码序列   总被引：8，自引：1，他引：7       下载免费PDF全文

王中铎  郭昱嵩  陈荣玲  何晓莹  刘楚吾  刘筠 《海洋与湖沼》2009,40(5):608-614

运用一对特异性引物扩增并测定了南海硬骨鱼类40个物种89个样本的线粒体DNA的细胞色素c氧化酶Ⅰ(COⅠ)约660bp的部分序列,即COⅠ条码序列。综合比较了《中国鱼类系统检索》、《海洋鱼类志》、FishBase鱼类形态学分类库、ITIS综合分类学信息系统和生物条码系统(The Barcode of Life Data System,BOLD)的相应形态学与DNA序列资料,在揭示完善我国鱼类检索系统必要性基础上,探讨了COⅠ条码序列在硬骨鱼类辅助物种鉴别和适用性,并对运用该条码序列库完善我国鱼类检索系统的可能途径进行了初步摸索。结果表明,COⅠ条码序列获取便捷,广泛适用硬骨鱼类物种鉴别,并可用于低级分类阶元的系统进化分析。本研究结果可为分子生物学辅助分类、市场监督、资源有序利用和保护提供参考。  相似文献   

Determination of Fe2+/Fe3+ Ratios of Magnetite using Different Methods: A Case Study from the Qimantag Metallogenic Belt          下载免费PDF全文

YI Liwen  LI Qiuping  LU Anhuai  GU Xiangping  CHI Guoxiang 《《地质学报》英文版》2022,96(6):2135-2147

Determination of Fe2+/Fe3+ ratios from metallogenic belts to explore controlling physical and chemical conditions of rock formation is of great significance. In order to explore magnetite Fe2+/Fe3+ ratios of the Qimantag metallogenic belt, part of the Eastern Kunlun orogenic belt in the northeastern margin of the Qinghai–Tibetan plateau, western Central Orogenic Belt of China, and overcome the limitation of the traditional electronic probe, five different measurement methods are proposed and their respective advantages and disadvantages evaluated, with the composition data of the magnetite obtained using electron probe microanalysis (EPMA). The direct oxygen measurement method has a significant impact on the determination results of FeO and Fe2O3, but the accuracy and uniformity of the results are low. The valence method (Flank method) based on the spectral intensity ratio of Lα to Lβ for iron is also unreliable for FeO and Fe2O3 measurements because it is difficult to establish a relationship between Lβ/Lα, the spectral intensity ratio, and the Fe2+/Fe3+ content ratio. In comparison, the charge difference method, the surplus-oxygen method and the M?ssbauer spectrum method are still the most favorable. M?ssbauer spectroscopy, with its isomer movement particularly sensitive to the oxidation state of iron, yields results closer to 0.5, which is relatively reliable. Earlier magnetite deposits are located in intrusions or contact zones and formed by magmatic fluids with high Fe2+/Fe3+ ratios, whereas later magnetite deposits are farther away from intrusions and have low Fe2+/Fe3+ ratios. The transformation mechanism of hematite and magnetite in the Qimantage metallogenic belt is also studied. No large volume changes, such as pore filling and shrinkage fracture, were detected in the metallogenic belt, and the transformation mechanism is more similar to a reoxidation and reduction mechanism.  相似文献