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Latest progress in graptolitic phylogeny studies——Cladistic analysis of Ashgillian Dicellograptus 被引量:1
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作者 冯洪真 《Science China Earth Sciences》 SCIE EI CAS 1998年第5期537-544,共8页
The graptolites studied here were collected from the Ashgillian Wufeng Formation in Wuning County, Jiangxi Province, which included 9 species of Dicellograptus, 2 species of Tangyagraptus and 1 species of Dicranograpt... The graptolites studied here were collected from the Ashgillian Wufeng Formation in Wuning County, Jiangxi Province, which included 9 species of Dicellograptus, 2 species of Tangyagraptus and 1 species of Dicranograptus . The polarity and states of 8 selected characters are analyzed based on the morphological features and stratigraphic sequences of the 12 species and a parsimonious cladogram is reconstructed by using the monothetic method proposed by Camin and Sokal. A phyloneny tree of evolutionary significance formed by adding a time_axis to the cladogram indicates that the Ashgillian Dicellograptus in the investigated area includes two independent evolutionary lineages starting to diverge as early as in the Caradocian and, within the main lineage composed of the dicellograptids with square or subsquare basal portion, two clades represented respectively by Dicellograptus complexus and D. turgidus mark the highest stage of the Ashgillian dicellograptid evolution. 展开更多
关键词 CLADISTICS GRAPTOLITES the ashgillian age.
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川西南阿什及尔期地层中的Ce异常及其古海洋学意义 被引量:10
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作者 冯洪真 E.Wallis +1 位作者 刘家润 姚素平 《火山地质与矿产》 2001年第2期126-134,共9页
川西南阿什及尔期地层中的全岩REE分配模式显示 ,含有浮游笔石和小型无铰纲腕足类的黑色页岩具有较低的Ce异常值 (0 .6 2~ 0 .74) ,而含有底栖三叶虫、有铰纲腕足类和藻类的非黑色页岩则具有较高的Ce异常值 (0 .92~ 1.30 )。Ce与其他... 川西南阿什及尔期地层中的全岩REE分配模式显示 ,含有浮游笔石和小型无铰纲腕足类的黑色页岩具有较低的Ce异常值 (0 .6 2~ 0 .74) ,而含有底栖三叶虫、有铰纲腕足类和藻类的非黑色页岩则具有较高的Ce异常值 (0 .92~ 1.30 )。Ce与其他元素的相关分析进一步揭示 ,Ce与Fe的相关性最好 (r =0 .85 ) ,与P的相关性次之 (r =0 .6 1) ,与Al的相关性较差 (r =0 .2 9) ,而与Mn和Ca几乎不相关 (r =0 .14,r =- 0 .0 2 )。实际观察可能表明 ,研究区底层水体在氧化和碱性条件下 ,Ce氧化为Ce4 + 并进入Fe的氢氧化物和磷酸盐的晶格中 ,或者被吸附到它们的表面 ,造成Ce在氧化水体中呈现负异常而在同期氧化沉积物中呈现正异常或负异常不明显 ;相反 ,在还原和酸性条件下 ,Ce在水体中以 +3价状态富集 ,引起Ce在同期缺氧沉积物中呈现明显负异常。作为古海水氧化还原指示的全岩Ce异常 ,通常限定于解释远洋细粒沉积物的沉积环境。我们的研究结果说明 ,移去化石骨骼 (通常是磷酸盐化石骨骼 )的浅海细粒沉积物同样可以用于全岩REE分析 。 展开更多
关键词 阿什及尔期 四川 古海水 REE分析 铈异常 古海洋学 稀土元素
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Morphometrics of Heliolites(Tabulata) from the Late Ordovician, Yushan, Jiangxi, South China
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作者 DAI Mingjian LIU Lu +2 位作者 LEE Dong-Jin PENG Yunbiao MIAO Aisheng 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 2015年第1期38-54,共17页
The Upper Ordovician Xiazhen Formation in the Jiangshan-Changshan-Yushan (JCY) triangle area on the Zhejiang-Jiangxi provincial border, South China, is composed of a mixed carbonate-siliciclastic sequence representi... The Upper Ordovician Xiazhen Formation in the Jiangshan-Changshan-Yushan (JCY) triangle area on the Zhejiang-Jiangxi provincial border, South China, is composed of a mixed carbonate-siliciclastic sequence representing various shallow-water platform environments. Highly diversified and abundant heliolitid coral faunas are recognized in the formation and occur over time and space in certain stratigraphic horizons and various lithofacies. Heliolites has been studied using multivariate morphometric analysis applied to differentiate species and evaluate intraspecific and interspecific variations. Ten morphological characters quantified by examination and measurement from transverse and longitudinal thin sections and statistically tested allowed selection of effective characters to discriminate species. Results of frequency histograms, correlation analysis and principle component analysis indicated that certain characters would be suitable for cluster analysis, which were performed on principle component score matrices obtained from the raw data set coordinated with coralla by all those characters. Five major clusters at a relative distance of five on the resulting dendrogram of Heliolites are regarded as morphospecies thus making valid taxa: Heliolites tashanensis Lin and Chow, 1977; Heliolites caracolica (Lin and Chow, 1977); Heliolites columella (Lin and Chow, 1977); Heliolites waicunensis Lin and Chow, 1977; and H. sinensis irregularis Lin and Chow, 1977. The discrimination of these morphospecies by the cluster analysis is verified by discriminant analyses and descriptive statistics. 展开更多
关键词 TAXONOMY tabulate corals MORPHOMETRICS ashgillian Zhejiang-Jiangxi provinces
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The Central Guizhou and Yi-chang uplifts, Upper Yangtze region,between Ordovician and Silurian 被引量:22
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作者 CHEN Xu RONG Jiayu +4 位作者 ZHOU Zhiyi ZHANG Yuandong ZHAN Renbin LIU Jianbo FAN Junxuan 《Chinese Science Bulletin》 SCIE EI CAS 2001年第18期1580-1584,共5页
The Central Guizhou and Yichang Uplifts are present in central Guizhou to western Hubei. Biostrati-graphic evidences from more than 20 sections in 14 counties of this region provide the data about the duration of thes... The Central Guizhou and Yichang Uplifts are present in central Guizhou to western Hubei. Biostrati-graphic evidences from more than 20 sections in 14 counties of this region provide the data about the duration of these uplifts. Although this duration differs from locality to locality, it is mainly from Ashgillian to Rhuddanian. The uplifts result from a horizontally driven movement to the South China Paleoplate from an uncertain block in southeast. Global sea-level drop during the end of the Ordovician made the uplifts obvious, particularly the Central Guizhou Uplift.It might have emerged above sea level in the short interval between the Ordovician and Silurian. 展开更多
关键词 Central GUIZHOU UPLIFT Yichang UPLIFT ashgillian Rhuddanian.
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浙赣边区晚奥陶世地层之新见 被引量:13
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作者 詹仁斌 傅力浦 《地层学杂志》 CSCD 北大核心 1994年第4期267-274,共8页
浙赣两省交界的三山地区(江山、常山、玉山)晚奥陶世Ashgill中期的海相沉积主要包括3种岩相:碳酸盐岩相的三衢山组、碎屑岩相的长坞组以及碳酸盐岩和碎屑岩交互相的下镇组;这3种类型的地层在研究区内的横向分布存在一定规... 浙赣两省交界的三山地区(江山、常山、玉山)晚奥陶世Ashgill中期的海相沉积主要包括3种岩相:碳酸盐岩相的三衢山组、碎屑岩相的长坞组以及碳酸盐岩和碎屑岩交互相的下镇组;这3种类型的地层在研究区内的横向分布存在一定规律,即从西南至东北大致为下镇组、三衢山组和长坞组。经详细的生物地层和岩石地层研究,建议取消“大桥灰岩”一名,用“下镇组”代替;整合于三衢山组之上的“文昌组”不宜归为Ashgill晚期,仍属Ashgill中期的沉积。通过系统的生态地层分析,对研究区内各种岩相地层之间的对比也提出了新的意见。 展开更多
关键词 晚奥陶世 地层 下镇组 浙赣边区
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