Wang Yi-Lin, Yang Qun, Ablett J M
Department of Physics and Electronic Science, Chuxiong Normal University, Chuxiong 675000, China.
Guang Pu Xue Yu Guang Pu Fen Xi. 2008 May;28(5):1194-8.
The metal elements mapping of Shuangbai dinosaur fossil, was obtained by synchrotron x-ray fluorescence (SXRF). Eight elements, Ca, Mn, Fe, Cu, Zn, As, Y and Sr were determined. Elements As and Y were detected for the first time in the dinosaur fossil. The data indicated that metal elements are asymmetrical on fossil section. This is different from common minerals. Mapping metals showed that metal element As is few. The dinosaur most likely belongs to natural death. This is different from Zigong dinosaurs which were found dead from poisoning. This method has been used to find that metals Fe and Mn are accrete, and the same is ture for Sr and Y. This study indicated that colloid granule Fe and Mn, as well as Sr and Y had opposite electric charges in lithification process of fossils. By this analysis, compound forms can be ascertained. Synchrotron light source x-ray fluorescence is a complementary method that shows mapping of metal elements at the dinosaur fossil, and is rapid, exact and intuitionist. This study shows that dinosaur fossil mineral imaging has a potential in reconstructing the paleoenvironment and ancient geology.
通过同步辐射X射线荧光(SXRF)获得了双柏恐龙化石的金属元素图谱。测定了钙、锰、铁、铜、锌、砷、钇和锶8种元素。砷和钇元素首次在恐龙化石中被检测到。数据表明,金属元素在化石切片上呈不对称分布。这与普通矿物不同。金属元素图谱显示砷元素含量很少。这只恐龙很可能属于自然死亡。这与自贡发现的因中毒死亡的恐龙不同。该方法已用于发现铁和锰元素是共生的,锶和钇元素也是如此。该研究表明,在化石成岩过程中,胶体颗粒铁和锰以及锶和钇带有相反电荷。通过这种分析,可以确定化合物形式。同步辐射光源X射线荧光是一种补充方法,可显示恐龙化石上金属元素的图谱,且快速、准确、直观。该研究表明,恐龙化石矿物成像在重建古环境和古代地质方面具有潜力。