|
|
|
题名
|
作者
|
年代
|
出处
|
被引量
|
| 1 | Octoradiate Spiral Organisms in the Ediacaran of South China显示文摘摘要:华南的 Ediacaran Doushantuo 形成的页岩包含新扁圆形 macrofossil, Eoandromeda octobrachiata,用可能是在外部膜以内的 housed 的八只螺线手臂描绘了。尽管八放射的结构的存在必要相似到 cnidarian octocorals 以及到栉水母,与这些现存的组一起的直接相同是不大可能的。相反,我们从 Doushantuo 形成把注意带到最新报导的胚胎的 helicospiral 形态学,建议 Ediacaran 胚胎的 metazoans 的长寻求的成年人最后被发现了。 | TANG Feng YIN Chongyu Stefan BENGTSON LIU Pengju WANG Ziqiang GAO Linzhi | 2008 | Acta Geologica Sinica(English Edition)2008，82，1： | 29 |
| 2 | A new discovery of macroscopic fossils from the Ediacaran Doushantuo Formation in the Yangtze Gorges area显示文摘Two new horizons with macroscopic fossils are reported in the Doushantuo Formation, Ediacaran System, from the Yangtze Gorges area. The fossils were discovered in the lower and middle black shales of the Doushantuo Formation in the new section at Sandouping Town, Zigui County, Hubei Province. The new macroscopic assemblages in- clude Chuaria and Tawuia, and occur below the well- known ”Miaohe Biota”. These fossils indicate that after the Nantuo ice age, macroscopic multicellular organisms gradually increased in abundance and diversity. Simple, discoidal carbonaceous compres- sions such as chuarids are present in the initial macrofossil assemblage of the Doushantuo Stage. This assemblage was eventually replaceded by the more diverse Miaohe macrofossils, including unam- biguously branching forms, in the uppermost Dou- shantuo Formation. The new discovery of carbona- ceous compression macrofossils from the Doushan- tuo Formation in the Yangtze Gorges area provides new evidence for the correlation of late Neoprotero- zoic successions in southern China. | TANG Feng YIN Chongyu Bengtson Stefan LIU Yongqing WANG Ziqiang LIU Pengju GAO Linzhi | 2006 | Chinese Science Bulletin2006，51，12： | 23 |
| 3 | 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 |
| 4 | Discovery of phosphatized gastrula fossils from the Dou-shantuo Formation,Weng'an,Guizhou Province,China显示文摘Globular fossils from Doushantuo phosphorites at the Weng’an area are for the first time identified as a gas-trulation stage of phosphatized embryos. They are got from the fossiliferous remains after acetic acid maceration. The fossils are found together with formerly reported animal resting eggs and embryos of the earlier cleavage stage. The oblate-shaped fossils with the same size as those reported embryos and invaginate at the middle part into the embryos, show the characteristics of the late blastula to the early gas-trula stage of the embryo development. This discovery convinces the existence of animal embryos at Doushantuo age and offers new facts for the studying of the affinity of related fossils, which are still controversial at present. | Yin Chongyu Yue Zhao Gao Linzhi | 2001 | Chinese Science Bulletin2001，46，20： | 16 |
| 5 | Detrital Zircon Dating of Meso-and Neoproterozoic Rocks in North China and Its Implications显示文摘从中央的新日期 -- 并且 Neoproterozoic 阶层贡献分会在 2009 年 11 月 24 日在中国的地层学上在前寒武纪的系统,和国家委员会上同意的中国的最近定义的前寒武纪的地层学的 timescale。首先, Changcheng 系统的年龄范围包括 Changzhougou, Chuanlinggou, Tuanshanzi 和 Dahongyu 形成被抑制了到 1.81.6 Ga。第二,包括 Gaoyuzhuang, Yangzhuang, Wumishan, Hongshuizhuang 和 Tieling 形成的 Jixian 系统被抑制了到 1.61.4 Ga。第三,一当还未命名(未定义) 系统(1.41.0 Ga ) 仅仅在 Jixian 节在 Xiamaling 形成被开发, Tianjing。第四, Qingbaikou 系统,包括 Luotuoling 和 Jing'eryu 形成被抑制了到 1.00.78 Ga。第五,在 780635 妈之间的 Nanhuan 系统范围,和 Sinian 系统在 635542 妈以内。然而,根据一系列虾, U-Pb 标明日期从在在华南站台的 Jiangnan Orogen 带晚前寒武纪,抑制阶层将作为在 Qingbaikou 系统的上面的部分被重新定义。帮助全球地球动力学,表示晚前寒武纪的节与是有用的统一,精确、高精确按年代先后的标明日期;这这里在诺思中国块和 Jiaoliao 朝鲜语块被定义。然而,在诺思中国的 Neoproterozoic Qingbaikou 学习将是在整个中央的影响 -- 并且在在在华南的扬采·布洛克和卡赛西亚·布洛克之间的 Jiangnan Orogenic 带的 Neoproterozoic。 | GAO Linzhi LIU Pengju YIN Chongyu ZHANG Chuanheng DING Xiaozhong LIU Yanxue SONG Biao | 2011 | Acta Geologica Sinica(English Edition)2011，85，2： | 9 |
| 6 | Microtubular metazoan fossils with multi-branches in Weng'an Biota显示文摘Microtubular metazoan fossils with multi- branches are found at least 4 times from the Sinian (Ediacarian) Doushantuo Formation at Weng’an, Guizhou, China. Their living mode should be the benthonic colony with higher ability of asexual re- production. The inner of the tube with cross-walls and chamber shows that these fossils are basal or stem- group cnidarians, similar to extinct tabulates. The multi-branching microtubular fossils are real meta- zoan found from Weng’an biota, which is very im- portant for studying the origin and evolvement of metazoan. | LIU Pengju YIN Chongyu TANG Feng | 2006 | Chinese Science Bulletin2006，51，5： | 8 |
| 7 | Qingbaikouan and Crygenian in South China:Constraints by SHRIMP Zircon U-Pb dating显示文摘The Qingbaikouan System is the lowest unit of the Neoproterozoic Erathem in Chinese stratigraphic succession,and it now provides a precise geochronological framework and geological time scale for mapping and stratal correlation in China.However,a sensitive high-resolution ion microprobe(SHRIMP)U-Pb zircon age date(1368±12 Ma)obtained from a bentonite in the Qingbaikouan Xiamaling Formation indicates that it belongs to the Mesoproterozoic Erathem instead.This change is a milestone in understanding the Precambrian Stratigraphic Time Scale in China,and it has had great influence on Precambrian correlations in Asia.Otherwise,a large amount of geochronological work has been done in the'Jiangnan Orogen Belt'of South China,and new isotopic data have redefined the traditional recognition of metamorphosed Mesoproterozoic strata from the Sibao orogeny to the Neoproterozoic Erathem.Based on SHRIMP zircon U-Pb age data,the authors regard the Sibao orogeny(equal to the Wuling orogeny)as a movement at ca 820 Ma,meaning that the Sibao orogeny was not equivalent to the Grenvillian orogeny.Finally,we report here the first SHRIMP U-Pb age of the boundary between the top of the Qingbaikouan Gongdong Formation(786.8±5.6 Ma)and the bottom of the Chang’an(diamictite)Formation(778.4±5.2 Ma),which is the age of the lowest diamictite of the Nanhuan System in China. | GAO Linzhi DING Xiaozhong YIN Chongyu ZHANG Chuanheng Frank R. ETTENSOHN | 2013 | Acta Geologica Sinica(English Edition)2013，87，6： | 8 |
| 8 | 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 |
| 9 | A New Diverse Macrofossil Lagersttte from the Uppermost Ediacaran of Southwestern China显示文摘A new macrofossil Lagersttte was discovered from the uppermost Ediacaran Jiucheng Member at Jinning and Jiangchuan of the eastern Yunnan,yielding numerous diverse well-preserved thallophyte macrofossils.These include the previously-known representatives of vendobionts, Vendotaenia and Tyrasotaenia,and the biggish multicellular benthos such as Chuaria-like and Tawuia- like fossils,as well as Longfengshaniaceaens with diverse holdfast structures.There are still some other problematic macrofossils with peculiar configurations as well as uncertain relatives.The distinct dominance of the giant,unbranching thallophytes occasionally with hoidfast structures distinguishes this assemblage from the other Ediacaran macrofossil Lagerstttes in the Doushantuo Formation at Miaohe,Wenghni and Lantian,and the contemporary assemblage in the Shibantan Member of Dengying Formation,Yangtze Gorges area.This paper outlines the characteristics of some of the multicellular macrofossils from the Jiucheng Member at Jiangchuan.They include some macrofossils with different types of holdfast structure,larger Chuaria-like and Tawuia-like morphology and questionable affinities as well.The discovery of greater diverse macrofossil assemblages from the Jiucheng Member of eastern Yunnan has further indicated that an important diversification and evolutionary radiation of metaphytes took place in the latest Ediacaran time.This radiation of large- scale,benthic metaphyte along with phytoplankton was likely important contributors to the early Cambrian explosion of metazoans. | TANG Feng YIN Chongyu LIU Pengju GAO Linzhi ZHANG Wenyan | 2008 | Acta Geologica Sinica(English Edition)2008，82，6： | 6 |
| 10 | The Early Evolution of the Acanthomorphic Acritarchs in China and Their Biostratigraphical Implication显示文摘On the basis of a study of the acanthomorphic acritarchs discovered in the Late Proterozoicto Early Cambrian Meishucunian Stage in different regions of China, especially in southernShaanxi and the Yangtze Platform, coupled with a study of the assemblages, morphological cor-relation, microstructure, and evolutional relations of the acanthorphic acritarchs, as well as awide correlation with those found in different regions of the world, the authors discuss the earlyevolutionary stages of the acanthomorphs, features of their assemblages in various stages, theirbiostratigraphical significance, and their evolutionary trend in China. | Yin Chongyu and Gao Linzhi Institute of Geology, Chinese Academy of Geological Sciences, Beijing | 1996 | Acta Geologica Sinica(English Edition)1996，70，2： | 5 |
| 11 | Discovery of the budding phosphatized globular fossils from the Neoproterozoic Doushantuo Formation at Weng'an, Guizhou Province, China显示文摘phosphatized 的生物亲密关系上有许多争论从在 Weng' 的 Neoproterozoic Doushantuo 磷钙土的球状的石块一,贵州省。这里,我们第一次报导一些这些球状的石块的开始发育的结构,它以前作为 metazoans 的休息的卵劈开胚胎被解释了。开始发育的结构类似于生活水藻的孢子和接合子的发芽试管,建议从 Doushantuo 磷钙土的一些球状的石块忍受与水藻的亲密关系。现在的新信息显示了 phosphatized 的各种各样的生物亲密关系从 Doushantuo 磷钙土的球状的石块。 | LIU Pengju YIN Chongyu TANG Feng | 2006 | Progress in Natural Science:Materials International2006，16，10： | 4 |
| 12 | New Data of Phosphatized Acritarchs from the Ediacaran Doushantuo Formation at Weng'an,Guizhou Province,Southwest China显示文摘Abundant phosphatized acritarchs are preserved in the late Precambrian (Ediacaran) Doushantuo Formation at Weng’an, Guizhou Province, southwest China. Most of them are large with various spinous ornaments and multilayered outer walls. The general characters of these fossils are quite similar to those found from the homochronous deposits of the Yangtze Gorges, southern China. Therefore the Doushantuo Formation in the Weng’an area can be correlated directly with the Doushantuo Formation of the Yangtze Gorges. Four species in four genera, including two new genera, two new species and one uncertain species are systematically described for the first time from the studied locality. The taxa are Bacatisphaera baokangensis Zhou, Brasier et Xue, 2001, Taeniosphaera doushantuoensis gen. et sp. nov., Rugospinasphaera speciosa gen. et sp. nov. and Meghystichosphaeridium sp. The new data enriches the famous Weng’an biota, especially the marine microplankton flora in the Ediacaran Doushantuo Formation. | LIU Pengju YIN Chongyu | 2005 | Acta Geologica Sinica(English Edition)2005，79，5： | 3 |
| 13 | The microfossils in phosphate deposit in Doushantuo stage, Sinian System, Weng' an, Guizhou Province显示文摘The aim of this study is to discuss the microfossils in phosphate deposit in the Doushantuo stage, Sinian System, weng’an, Guizhou Province. Based on the detailed observation in morphology and microstructures, it is considered that those acritarchs with interior spicules probably belong to sponge animals. However, some explanations for a part of soft-tissue are stili contrioversial. The reliable conciusion stili needs more evidence to study. The scientific significance of this study and the key questions for further studies are suggested here. | Chongyu Yin Linzhi Gao | 2000 | Chinese Science Bulletin2000，45，3： | 3 |
| 14 | Microfossils from the Upper Sinian (Late Neoproterozoic)Doushantuo Formation in Changyang, Western Hubei, China显示文摘 | Yin Chongyu | 1999 | Continental Dynamics1999，4，2： | 1 |
| 15 | Fossilized metazoan embryos——the historical testimony of the Cambrian explosion显示文摘IN zoology, the developmental stage of individual from zygote to hatching was called embryo. The modem embryology is a branch of study on the organism’ s embryos. The palaeoembryology is a new field in palaeontology, and it has not been considered an important field before, because the invertebrate’s eggs or embryos are minute size and without mineralized envelope. Until now, fossilized eggs of invertebrates in Cambrian have been rarely reported and most of them are small globular structures without recognizable features. Other reported fossilized embryos found from Middle Cambrian are spherical with a | YIN Chongyu | 1999 | Chinese Science Bulletin1999，44，9： | 1 |
| 16 | Optical experimental solution for the multiway number partitioning problem and its application to computing power scheduling显示文摘Quantum computing is an emerging technology that is expected to realize an exponential increase in computing power. Recently,its theoretical foundation and application scenarios have been extensively researched and explored. In this work, we propose efficient quantum algorithms suitable for solving computing power scheduling problems in the cloud-rendering domain, which can be viewed mathematically as a generalized form of a typical NP-complete problem, i.e., a multiway number partitioning problem.In our algorithm, the matching pattern between tasks and computing resources with the shortest completion time or optimal load balancing is encoded into the ground state of the Hamiltonian;it is then solved using the optical coherent Ising machine, a practical quantum computing device with at least 100 qubits. The experimental results show that the proposed quantum scheme can achieve significant acceleration and save 97% of the time required to solve combinatorial optimization problems compared with classical algorithms. This demonstrates the computational advantages of optical quantum devices in solving combinatorial optimization problems. Our algorithmic and experimental work will advance the utilization of quantum computers to solve specific NP problems and will broaden the range of possible applications. | Jingwei Wen Zhenming Wang Zhiguo Huang Dunbo Cai Bingjie Jia Chongyu Cao Yin Ma Hai Wei Kai Wen Ling Qian | 2023 | Science China(Physics,Mechanics & Astronomy)2023，66，9： | 0 |
| 17 | Storm Deposits of the Sinian Zhangqu Formation in Northern Anhui——An Upward Shallowing Carbonate Sequence显示文摘This paper studies. for the first time, the storm deposits of a carbonate sequence in the Sinian ZhangquFormation in northern Anhui. In the formation. a great number of calcareous trider sponge spicules were dis-covered in a distal storm turbidity sequence, which have provided further evidence for the correlation of theSinian Systems in North and South China from a view point of palaeontology. | Qiao Xiufu Xing Yusheng Gao Linzhi Yin Chongyu Yue Zhao Liu Guizhi Institute of Geology, Chinese Academy of Geological Sciences, Beijing Jia Zhongpeng Gao Linzhi | 1990 | Acta Geologica Sinica(English Edition)1990，64，2： | 0 |
| 18 | Microfossils from the Chert in the Lower Cambrian Shuijingtuo Formation at Miaohe, Zigui, Hubei Province显示文摘This paper reports for the first time on the microfossils discovered in the black cherts of the basal part of the Lower Cambrian Shuijingtuo Formation at Miaohe village, Zigui County, Hubei Province, all of which were observed in thin sections. Nine genera, 9 species and 3 indeterminate species (including a new species) are described. According to these microfossils, the conclusion is made that the microfossil zone may be equivalent to the small shelly fossil assemblage zones 2—3 of the Meishucun stage. They have provided another important line of evidence for the correlation of the Sinian-Cambrian boundary strata with those of the adjacent areas. | Yin Chongyu, Yue Zhao, Gao Linzhi Institute of Geology, CAGS, Beijing and Ding Qixiu Hubei Geological Institute, Hubei Bureau of Geology, Wuhan | 1993 | Acta Geologica Sinica(English Edition)1993，67，2： | 0 |
您所在的机构暂未开通此部分的功能，请联系管理员