|
|
|
题名
|
作者
|
年代
|
出处
|
被引量
|
| 1 | Mesoproterozoic age for Xiamaling Formation in North China Plate indicated by zircon SHRIMP dating显示文摘Zircon grains of magmatic origin from tuffite layers in the Xiamaling Formation at Zhaojiashan Village, Xuanhua area, Hebei Province, were used for zircon dating with a Sensitive High-Resolution Ion Microprobe (SHRIMP II), which gives a weighted mean 207Pb/206Pb age of 1366±9 Ma. It shows a very similar age (1368±12 Ma) as the zircon dating from the Xiamaling Formation in Western Hill, Beijing. This age proposes that the Xiamaling Formation in the North China plate should be of Mesoproterozoic, instead of Neoproterozoic based on K-Ar, Ar-Ar dating. The new zircon age also indicates the devel- opment of macrofossils algae from the Mesoproterozoic age. | GAO LinZhi ZHANG ChuanHeng SHI XiaoYing SONG Biao WANG ZiQiang LIU YaoMing | 2008 | Chinese Science Bulletin2008，53，17： | 68 |
| 2 | Seismic Sequence in Carbonate Rocks By Vibrational Liquefaction显示文摘On the basis of the records of strong seismic events taking place in soft carbonate sediments, a new seismic sequence system of vibrational liquefaction is established, which consists of a series of units, such as escaped structure of micrite veins and liquefied deformation formed in the period of seismic liquefaction, land subsidence structure after liquefaction, tsunamic hummocky and turbidite produced by seismic events, This sequence is a generalization and summation of field observation in vast areas, which shows the whole process of a strong seismic event and provides an unified theoretical explanation. The pattern of the seismic sequence by vibrational liquefaction provides one of correlation standards for geologists in the field to discriminate events in carbonate sequences. Based on the pattern of seismic sequence, the authors first advance a new conception of the Palaeo-Tanlu (Tancheng-Lujiang) Zone and discuss primarily its geological significations. | Qiao Xiufu, Song Tianrui, Gao Linzhi, Peng Yang, Li Haibing, Gao Mai, Song Biao and Zhang QiaodaInstitute of Geology, Chinese Academy of Geological Sciences, Beijing | 1994 | Acta Geologica Sinica(English Edition)1994，68，3： | 39 |
| 3 | Zircon U-Pb dating for the earliest Neoproterozoic mafic magmatism in the southern margin of the North China Block显示文摘Huge diabase occurs within the Pro- terozoic strata in the southern margin of the North China Block, geographically in the northern parts of Anhui and Jiangsu provinces, where no strata younger than Neoproterozoic have been found. Zir- cons from the diabase show three different structures from cathodoluminesecence imaging, but they are all of magmatic origin. SHRIMP U-Pb dating yields a range of 206Pb/238U ages from 2600 to 124 Ma, but two geological events can clearly be identified from both concordant and discordant ages. One gives two weighted mean 207Pb/206Pb ages of 976 ± 24 and 1038 ± 26 Ma which are interpreted as timing of dia- base crystallization, and the other has a weighted mean 207Pb/206Pb age of 2523 ± 52 Ma that repre- sents formation time of inherited zircon from the old crust. The dating results indicate that the mafic magmatic event occurred in a transition period from the latest Mesoproterozoic to the earliest Neopro- terozoic, consistent with global subduction of Grenvill ocean crust to result in the assembly of superconti- nent Rodinia. Therefore, the North China Block needs to be taken into account when reconstructing the position of China continents within the framework of Rodinia supercontinent. | LIU Yongqing GAO Linzhi LIU Yanxue SONG Biao WANG Zongxiu | 2006 | Chinese Science Bulletin2006，51，19： | 36 |
| 4 | SHRIMP U-Pb zircon age of tuff from the Kunyang Group in central Yunnan:Evidence for Grenvillian orogeny in South China显示文摘Whether or not Grenvillian orogeny occurred in South China still remains highly controversial because high-quality,discriminating data are lacking,and therefore,the key to resolve this matter is to find datable volcanic and/or sedimentary rocks related to Grenvillian orogeny. Such rocks are apparently present in the Fuliangpeng Member from the lower-middle part of Kunyang Group in central Yunnan; here the unit is more than 100 m thick and consists of andesitic ignimbrite,tuffite,terrigeous clastic rocks and carbonates. These volcanic rocks,developed south of the Sibao fold-thrust belts,represent the earliest calc-alkaline volcanic activity in late Precambrian time from central Yunnan and are coeval with both a change in sedimentary facies from detritus to carbonates and the beginning of seismite development elsewhere. Two samples for SHRIMP analysis were collected from this volcanic unit. Sample G3-29-2,from the bottom of Fuliangpeng Member,is an ignimbrite,and about 100 zircon crys-tals recovered from it have euhedral shapes and display relatively simple sector zonation under cathodoluminescent (CL) imaging,suggesting a magmatogenic origin. Twenty-five of the zircons were analyzed and a weighed-mean U-Pb age of 1032±9 Ma was obtained. Sample G3-29-3 from uppermost part of Fuliangpeng Member is a tuffite,and many rounded,evidently detrital zircons were recovered. Nine of these zircons were analyzed,and the oldest single-grain U-Pb zircon age is 1938±26 Ma,im-plying that Paleoproterozoic basement developed in Cathaysia. The dating result,combined with the geotectonic research on the Fuliangpeng Member,leads us to conclude that late Mesoproterozoic orogenic volcanic activity occurred in the western part of South China,and that the related collision of Yangtze and Cathaysian cratons was an integral part of the assembly of Rodinia. | ZHANG ChuanHeng GAO LinZhi WU ZhenJie SHI XiaoYing YAN QuanRen LI DaJian | 2007 | Chinese Science Bulletin2007，52，11： | 35 |
| 5 | A New SHRIMP Age of the Xiamaling Formation in the North China Plate and Its Geological Significance显示文摘建立 hypostratotype 近来前寒武纪是关于中央的研究的主要目的 -- 并且在诺思中国的 Neoproterozoic。chronostratigraphic 位置是在这研究的钥匙。然而,许多关键地平线没与高质量的同位素的年龄被校准。用有敏感高分辨率的离子 Microprobe (虾 II ) 的报导新 U-Pb 年龄,锆石 U-Pb 年龄在诺思中国板中在 Xiamaling 形成灰床被获得,产出 1368+-12 妈的加权的吝啬的 ^(206 )Pb/^(238 ) U 年龄。现在是从在北方中国板中的 Xiamaling 形成的第一虾 U-Pb 年龄,并且代表 Xiamaling 形成的中间的部分的扔的时间。锆石年龄起一个重要作用到在中央期间理解北方中国板的地质的进化 -- 并且 Neoproterozoic。 | GAO Linzhi ZHANG Chuanheng SHI Xiaoying ZHOU Hongrui WANG Ziqiang SONG-Biao | 2007 | Acta Geologica Sinica(English Edition)2007，81，6： | 35 |
| 6 | Reclassification of the Meso- and Neoproterozoic Chronostratigraphy of North China by SHRIMP Zircon Ages显示文摘High-quality zircon U-Pb ages acquired from Meso- and Neoproterozoic strata in North China in recent years has provided a high-resolution chronostratigraphic framework for dating. A basis of this high-level chronostratigraphic system provides the foundation for a global Precambrian study and stratigraphic correlation and so recent geological studies have focused attention on systemic SHRIMP zircon dating. A chronology of Meso- and Neoproterozoic strata and the time of origin of the overlying Changcheng System is given on the basis of new SHRIMP zircon dating from the Qianxi Complex and diabase of the Chuanlinggou Formation. A new tectonostratigraphy for a Neoproterozoic chronostratigraphic framework in the southeastern margin of the North China continent is underpinned by the new SHRIMP zircon dating of a Neoproterozoic mafic magma diabase in the Jiao-Liao-Xu-Huai Sub-Province. | GAO Linzhi ZHANG Chuanheng LIU Pengju TANG Feng SONG Biao DING Xiaozhong | 2009 | Acta Geologica Sinica(English Edition)2009，83，6： | 36 |
| 7 | 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 |
| 8 | Earthquake events in Neoproterozoic and Early Paleozoic and its relationship with supercontinental Rodinia in North China显示文摘Carbonate liquefied veins in limestone and liquefied mud veins in mudstone are the result by earthquake, which is liquefied in sediments and a strong earthquake event remains clearly records in strata. 24 strata units with earthquake events (molar tooth), which are subdivided into 11 seismic periods, have been distinguished from Mid-Proterozoic to Early Paleozoic strata in the Sino-Korean platform. The distributions of them represent paleo-seismic tectonic zones in different periods, which is tallied with convergent continental block before Proterozoic supercontinental Rodinia and the evidence of the breakup or splitting developed in the inner Sino-Korean Platform in 700 Ma. | Xiufu Qiao Linzhi Gao | 2000 | Chinese Science Bulletin2000，45，10： | 26 |
| 9 | 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 |
| 10 | Mesoproterozoic Earthquake Events and Breakup of the Sino-Korean Plate显示文摘在 Mesoproterozoic 时间,中国朝鲜语的 Plateexperienced 的北部分集中的构造扩展和决裂的一个时期。1。沉积地震记录的许多在 theMesoproterozoic Changcheng 系统(1800-1400 妈) 并且在 Jixian 系统(1400-1000 妈) 的 Mesoproterozoic Wumishan 形成在 Chuanlinggou, Tuanshanzi 和 Gaoyuzhuang 形成被保存。这些地震记录被各种各样的 liquefiedsand 静脉,碳酸盐 micros 同等和更粗糙的圆材描绘静脉,石灰石堤,液化角砾岩和液化褶皱层理的各种各样的形式。这变丑是总是联系的 withsynsedimentary 差错和火的活动。2。为软碳酸盐沉积的三个液化模型被认出,包括在把压成薄片的碳酸盐岩石中的液化,液化沿着巨大的碳酸盐堤的床 inthin 的碳酸盐和大规模液化。3。基于地震和暴烈的活动的记录,中国朝鲜语的板经历了至少 twiceintraplate 决裂。一个人在 1800-1400 妈之间发生了,并且其它发生在大约 1200 妈。Thelast 决裂导致了 Yan 辽河 aulacogen,更深的材料活力描绘的一个构造地区,活断层,主要火的活动和经常的地震的形成。 | QIAO Xiufu GAO Linzhi PENG Yang | 2007 | Acta Geologica Sinica(English Edition)2007，81，3： | 19 |
| 11 | 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 |
| 12 | 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 |
| 13 | Earthquake-induced soft-sediment deformation structures in the Mesoproterozoic Wumishan Formation,North China,and their geologic implications显示文摘Soft-sediment structures are key to defining seismites. Two soft-sediment deformation horizons, bounded by undeformed carbonate strata, have been found in the Wumishan Formation in the Jumahe region, 175 km southwest of Beijing. One is in the lowest part of Wumishan Formation; and the other is in the uppermost part of Litho-member I. The soft-sediment structures in these two horizons fall into three categories: mould-and-sag structures, hydraulic shatterings and liquefaction dikes. The mould-and-sag structures are divided into two types: one developed in tidal-flat sediments, accompa-nied by many liquefaction-related structures and characterized by autochthonous post-earthquake sediments in sags, and the other type developed in deep-water environments, is not associated with liquefaction structures, and is overlain immediately by seismogenic tsunamites. The hydraulic shat-terings are composed of pockets of fluidization conglomerate, sand intrusions, and syndepositional faults. The liquefaction dikes fall into two categories: hydraulic-fracturing dikes and lateral-spreading dikes. The former are steep, planar, and pinch out upwards. The latter are snake-like and characterized by no diapir-related drag structures in surrounding rocks. Examination of the attitudes and strati-graphic positions of these structures suggests that these soft-sediment structures are seismogenic, and consequently, are seismites. Most seismites in the Wumishan Formation are developed near the former western, margin fault of Yanliao rift. This occurrence suggests that they could be related to movements on this fault. Other geological implications are discussed. | ZHANG ChuanHeng WU ZhengJie GAO LinZhi WANG Wei TIAN YanLin MA Chao | 2007 | Science China Earth Sciences2007，50，3： | 15 |
| 14 | Revised Chronostratigraphic Framework of the Metamorphic Strata in the Jiangnan Orogenic Belt,South China and its Tectonic Implications显示文摘In a re-study of regional geology by the China Geological Survey(CGS),the key problem is in the stratigraphical division and correlation.According to the new isotopic dating of the Meso-and Neoproterozoic in China,there have been great changes in the strata correlation and tectonic explanation.The authors obtained four zircon sensitive high resolution ion micro-probe(SHRIMP) U-Pb datings from the bentonite of the Lengjiaxi Group(822±10 Ma,823±12 Ma and 834±11 Ma) and Banxi Group(802.6±7.6 Ma) in north Hunan Province,which is considered to be the middle part of the Jiangnan Orogenic Belt.On the basis of the zircon dating mentioned above,the end of the Wuling orogen is first limited in the period from 822 Ma to 802 Ma in one continued outcrop(Lucheng section) in Linxiang city,Hunan Province.Combining a series of new zircon U-Pb datings in the Yangtze and Cathaysia blocks,several Neoproterozoic volcanic events and distribution of the metamorphic rocks in the Jiangnan Orogenic Belt have been distinguished.In the context of the global geodynamics,it is useful to set up a practical and high precision chronological framework and basic and unified late Precambrian section in South China. | GAO Linzhi DING Xiaozhong ZHANG Chuanheng CHENJun LIU Yaorong ZHANG Hang LIU Xanxue PANG Weihua | 2012 | Acta Geologica Sinica(English Edition)2012，86，2： | 14 |
| 15 | Neoproterozoic Molar-tooth Structure and Constraint of Depositional Facies and Environment in the North China Platform in Jiangsu, Anhui and Liaoning, Eastern China显示文摘Molar tooth structure (MTS) represented by complex ptygmatical shapes is widely distributed in the Proterozoic of the world. MTS filled by fine, equant sparry calcite (or dolomite) displays an abrupt contact with hosting rocks, which are mainly composed of carbonaceous micrites and fine-grained carbonates with local silts and storm-dominated deposits with graded, cross or wave beddings, numerous erosional surfaces and truncated and fills or guttered bases. Occurrence of MTS suggests a result of the constraint of sedimentary facies, and the storm-base in ramp settings is the maximum depth for the formation of MTS. Vertical succession of MTS-bearing carbonates shows a deposition stacked by high-frequency shallow subtidal and peritidal cycles. An individual cyclic MTS-bearing sequence is characterized by thinning, shallowing and dynamic decreasing-upward, and peritidal caps of purple red iron and organic carbonaceous sediments with more complicated shapes of MTS are common on the top of individual MTS-bearing sequences. | LIU Yongqing GAO Linzhi LIU Yanxue | 2005 | Acta Geologica Sinica(English Edition)2005，79，4： | 11 |
| 16 | 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 |
| 17 | Provenance of the Paleoproterozoic Hutuo Group basal conglomerates and Neoarchean crustal growth in the Wutai Mountains,North China Craton:Evidence from granite and quartzite pebble zircon U-Pb ages and Hf isotopes显示文摘Zircon U-Pb ages(SHRIMP and LA-ICPMS) and Lu-Hf isotope data(LA-ICPMS) are presented for two granite and two quartzite pebbles from the basal conglomerates of the Sijizhuang Formation in the Hutuo Group from the Wutai Mountains area in the North China Craton.These two granite pebbles give zircon 207 Pb/206 Pb ages of 2513±8 Ma and 2527±8 Ma respectively,which are consistent with the emplacement ages of the Wangjiahui grey granite and Guangmingsi or Shifo granite in the Wutai Mountains.Detrital zircons from those two quartzite pebbles are mostly 2550-2490 Ma old with lesser number of 2800-2550 Ma grains,which is similar to the ages of detrital zircons from quartzites in the Gaofan Subgroup of the Neoarchean Wutai Group.Thus,the pebbles in the Hutuo Group basal conglomerates were derived locally from Wutai Mountains Neoarchean sources.Zircons from the Sijizhuang Formation conglomerate granite and quartzite pebbles mostly have positive ε Hf(t) values,a minority with ε Hf(t) values like model depleted mantle(DM) of the same age,but with most showing DM model ages 200-100 Ma.This indicates that most of the source materials were derived from the mantle within the previous 200 million years,whereas some are derived from 2550-2510 Ma juvenile crustal additions.This additional evidence suggests that in the North China Craton there was important initial polycyclic crustal formation and cratonization in the late Neoarchaean,prior to superimposed Palaeoproterozoic orogenic cycles. | DU LiLin YANG ChongHui WANG Wei REN LiuDong WAN YuSheng SONG HuiXia GAO LinZhi GENG YuanSheng HOU KeJun | 2012 | Science China Earth Sciences2012，55，11： | 8 |
| 18 | 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 |
| 19 | 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 |
| 20 | 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 |
您所在的机构暂未开通此部分的功能，请联系管理员