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| 1 | New material of microfossils from the Ediacaran Doushantuo Formation in the Zhangcunping area, Yichang, Hubei Province and its zircon SHRIMP U-Pb age显示文摘The Zhangcunping area is located at the north limb of the Huangling anticline in Yichang, Hubei Prov-ince. Here, the sedimentary succession of the Ediacaran Doushantuo Formation is similar with that in the Weng'an area, Guizhou Province. A large number of new microfossils (mainly acanthoacritarchs) from the Doushantuo Formation in this area are reported in this paper. The fossil assemblage shows similarity as the phosphatized biota of the Doushantuo Formation at Weng'an, Guizhou Province and the silicified biota of the Doushantuo Formation at the Yangtze Gorges, which suggests that the Zhangcunping area is a key for correlation of the Doushantuo Formation between the Weng'an area, Guizhou Province and the Yangtze Gorges. Besides, a new zircon SHRIMP U-Pb age (614.0±7.6 Ma) is first obtained from a horizon underneath the exposed surface in the middle of the Doushantuo Forma-tion in the Zhangcunping area. This age not only provides a new datum for subdivision of the Ediacaran Doushantuo Formation, but also indicates that the age of the exposed surface in the middle of the Doushantuo Formation in the Yangtze Platform should be posterior to 614.0±7.6 Ma. Due to the horizon of the Weng'an biota situated above the exposed surface, the age of the Weng'an biota should be pos-terior to 614.0±7.6 Ma as well. | LIU PengJu YIN ChongYu GAO LinZhi TANG Feng CHEN ShouMing | 2009 | Chinese Science Bulletin2009，54，6： | 19 |
| 2 | Acanthomorph Biostratigraphic Succession of the Ediacaran Doushantuo Formation in the East Yangtze Gorges,South China显示文摘大 acanthomorphic acritarchs 在华南在几个地区在 Ediacaran Doushantuo 形成的燧石被发现了,包括湖北省的东方 Yangtze 峡,贵州省的 Weng'an 区域,并且在其它地方。然而,他们为 biostratigraphic 分和 Ediacaran 继任的关联的潜力被外形控制, taphonomic 偏爱,和分类问题限制。在 Yangtze 峡, Doushantuo 形成通常被细分进四个 lithologic 成员。在 Weng'an 区域,然而, Doushantuo 形成包括就 mid-Doushantuo erosional 表面分开的更低、上面的部分。在在 Zhangcunping 节的 Yangtze 峡, Doushantuo 继任在 Weng'an 类似于那。到目前为止,在 Yangtze 之间的关联塞满并且 Weng'an 区域,并且在其它地方是争论的一个问题。解决争论,我们在 Yangtze 峡区域选择了八节并且全身地取样了 Doushantuo 形成的燧石小瘤,特别地集中于上面的 Doushantuo 形成。我们的数据证实在第二和第三个成员独立出现的二个不同集合,它被一次否定 13C 旅行(EN2 ) 分开。更低的集合被 Tianzhushania 和大 acanthomorphic acritarchs 的一间多样的套房描绘。上面的集合与更低的集合被区分开来,由(1 ) Tianzhushania 的缺席;(2 ) 出现丰富, 100150 m,光滑墙的球形的微化石;(3 ) 包括种类在这个成员从第二个成员和新形式延长的高度多样的 acanthomorphic acritarchs 的出现;(4 ) 原生生物的未命名的新形式的出现;并且(5 ) 管状的微化石 Sinocyclocylicus guizhouensis 的出现。因为统治 Tianzhushania 的集合不是在澳大利亚的现在,看起来仅仅上面的 acanthomorph 集合是在场的,因此,更低的 Doushantuo acanthomorph 集合在澳大利亚失踪。 | YIN Chongyu LIU Pengju Stanley M. AWRAMIK CHEN Shouming TANG Feng GAO Linzhi WANG Ziqiang Leigh A. RIEDMAN | 2011 | Acta Geologica Sinica(English Edition)2011，85，2： | 6 |
| 3 | Hematological Changes in White Spot Syndrome Virus-Infected Shrimp,Fenneropenaeus chinensis(Osbeck)显示文摘The pathological changes of hemocytes in the haemolymph and hepatopancreas were examined in experimentally and naturally WSSV(white spot syndrome virus) infected Fenneropenaeus chinensis. The results showed that the pathological manifesta-tions of hemocytes were similar among moribund shrimps infected via injection,feeding and by nature. Firstly,the total hemocyte counts(THCs) in WSSV-infected shrimp were significantly lower than those in healthy shrimp. Secondly,necrotic,broken and dis-integrated cells were often observed,and a typical hematolysis was present in the haemolymph smear of WSSV-infected shrimp. Thirdly,necrosis and typical apoptosis of hemocytes were detected with TEM in the peripheral haemolymph of WSSV-infected shrimp. Hyalinocytes and semi-granulocytes with masses of WSSVs in their nuclei often appeared,whereas no granular hemocytes with WSSV were found in the hepatopancreas of moribund infected shrimps. All our results supported that hemocytes were the main target cells of WSSV,and hyalinocytes and semigranular hemocytes seemed to be more favorable for WSSV infection in F. chinensis. | FENG Shouming ZHAN Wenbin XING Jing LI Jun YANG Kai WANG Jing | 2008 | Journal of Ocean University of China2008，7，3： | 1 |
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