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| 1 | Unique recovery stage of reef communities after F/F event in a huge coral reef of Carboniferous, Southern Guizhou,China显示文摘A huge coral reef occurring in the Triticites belt of the Maping Formation, in Bianping Village, about 4 km west of Houchang Town from Ziyun County, Southern Guizhou, China is described. The coral reef has been well studied and some significant characteristics were dis-covered: the composition of reef-building community is very monotonous; there are only one or two builders in each reef-building stage; the dwellers are also poor in variety; the reef-building process is very simple; the reef has been separately built by various reef-building mechanisms, and there have been few parts built by two coexisting building mechanisms; the process of reef building is often discontinuous and lacks transition. All these characteristics are considered to be unique to the recovery stage of reef communities after F/F event and are representative of a process that reef communities must undergo post the catastrophe. | GONG Enpu YANG Hongying GUAN Changqing SUN Baoliang YAO Yuzeng | 2004 | Science China Earth Sciences2004，47，5： | 14 |
| 2 | Paleoecology of Late Carboniferous Phylloid Algae in Southern Guizhou,SW China显示文摘叶状的水藻是重要礁石建筑者在晚含碳。叶状的水藻在的苍白的生态学的 Thispaper 焦点在在 Ziyun 县的暴露得好的礁石上晚含碳,贵州省。仔细成长包装了的叶状的水藻经由可夹紧之用物或类似的结构被纳入底层。他们在象浅水区那样的环境正在成长,透光层并且在有中等精力水流的波浪酌的限界深度下面。他们有许多词法形式,例如单身者杯状,塑造卷心菜、聚类杯状。thalli 具有某些固执和紧张。在叶状的水藻统治的区域,另外的海洋的有机体是相对少见的。显然,叶状的水藻比发生 otherco 有机体是更强壮的竞争者生活空间。 | GONG Enpu ZHANG Yonglil GUAN Changqing Elias SAMANKASSOU SUN Baoliang | 2007 | Acta Geologica Sinica(English Edition)2007，81，4： | 9 |
| 3 | Palynomorph assemblages and paleoclimate records from the Zhuanchengzi Bed of the Yixian Formation, western Liaoning Province, China显示文摘We collected, processed, identified, and analyzed the spores and pollen samples from the Zhuanchengzi Bed of the Yixian Formation in the Yingwoshan area of western Liaoning. As a result, we confirm a palynomorph assemblage of Cicatricosisporites-Protoconiferus. The pollen was primarily from gymnosperms, dominated especially by conifer pollen. Pteridophyte spores were less common and some questionable angiosperm pollen occurred occasionally. The age of the palynomorph assemblage is dated as the late Valanginian or Hauterivian-Barremian stage, the Early Cretaceous. The study applies the concept of Palynological Vegetation based on palynological spectra and the paleoecological characteristics of palynological taxa for the first time. Palynological vegetation type, climatic zone type, and humidity type are divided quantitatively for the Zhuanchengzi Bed in the Yixian Formation of western Liaoning. We then obtained the evolutionary trends. The results showed that the overall climate was warm and humid during the deposition period of the Zhuanchengzi Bed in the Yixian Formation. Palynological vegetation types are various and include coniferous forest, deciduous broadleaf forest, evergreen broad-leaved forest, grass, and shrubs. The local temperature changed from warm to much warmer and from a semi-humid to humid climate. Palynological vegetation types are always dominated by coniferous forest. The coexistence of deciduous broad-leaved forest, evergreen broad-leaved forest, shrubs, grass, and some xerophytic plants indicates vertical zonation and seasonal climate change The vertical vegetation types and the warm humid climate may imply a large geomorphological contrast in the Yixian Formation of western Liaoning. | CUI Ying GONG EnPu WANG TieHui GUAN ChangQing ZHANG YongLi LIANG JunHong | 2015 | Science China Earth Sciences2015，58，9： | 5 |
| 4 | The Carboniferous reefs in China | Gong Enpu,Zhang Yongli,Guan Changqing,Chen Xiaohong Department of Geology,Northeastern University,Shenyang 110819,China | 2012 | Journal of Palaeogeography2012，1，1： | 4 |
| 5 | Mineralization Patterns and Conditions of Lateritic Gibbsite Bauxite in Guinea显示文摘After the exploration and research of Lateritic-Gibbsite bauxite for years in Guinea, based on factors such as paleoclimate, paleogeography and parent rocks, the laterization and bauxite mineralization process of lateritic gibbsite bauxite in Guinea were analyzed. The mineralization conditions and topography were favorable for the formation of bauxite deposits on the West Africa craton of NW Africa, especially in Guinea. Through chemical and phase analysis for mineralogy and petrology of different mining area in BOKE-SANGAREDI of Guinea, the mineralization characters of different minerals were analyzed. Due to the paleoclimate and paleogeographical conditions, the parent rocks were leached of certain major elements, such as Si, K, Na, Ca and Mg. However, some elements, such as Al, Fe, and Ti, became relatively concentrated. Based on composition analyses of the bauxite and surrounding rocks, the laterization and bauxite mineralization processes are evaluated in the Boke-Sangaredi area of Guinea. | Rongliang Zhang Enpu Gong Guoku Wang Weiya Peng | 2018 | Advances in Geoscience2018，2，1： | 2 |
| 6 | Paleoecology of Pennsylvanian phylloid algae buildups in South Guizhou, China 显示文摘 | Gong Enpu Elias Samankassou Guan Changqing | 2007 | Facies2007，53，： | 1 |
| 7 | Paleoecology of Pennsylvanian phylloid algal buildups in south Guizhou,China显示文摘 | Gong Enpu Elias Samankassou Guan Changqing | 2007 | Facies2007，53，： | 1 |
| 8 | Distribution of the Carboniferous coral limestone belt in the eastern part of North China and its geological significance显示文摘Alarge number of coral fossils such as Arachnastraea, Chaetetes and Multithecopora havebeen found in the marine strata of the upper part of the Carboniferous Benxi Formation in theeastern part of North China. The coral fossils are so abundant that they form coral limestonesin some outcrops. These limestones almost made up a rock belt, in which coral reefs areformed in some sections. The occurrence of the belt provides important information for un-derstanding of the history of the Middle and Late Carboniferous in the eastern part of NorthChina. | GONG Enpu and GUAN GuangyueDepartment of Geology, Northeast University, Shenyang 110006, China | 1997 | Chinese Science Bulletin1997，42，14： | 1 |
| 9 | Paleoecology of Pennsylvanian phylloid algal buildups in south Guizhou,China显示文摘 | Gong Enpu Elias Samankassou Guan Changqing | 2007 | Facies2007，53，： | 1 |
| 10 | Paleoenvironmental changes recorded on Upper Carboniferous reef in Guangxi,China显示文摘Based on detailed measurement in the field and a comprehensive analysis of carbonate microfacies,the Pennsylvanian reefal microfacies characteristic and sedimentary environment from Longjiangdong,Guangxi,China are analyzed. The twelve carbonate microfacies have been recognized including micritic / microsparitic limestone,peloidal / aggregate-grain grainstone,bioclastic wackestone / packstone,laminated mudstone,boundstone,bioclastic wackestone / packstone with single shell,coral framestone / bafflestone,bioclastic packstones /grainstones with abundant benthic foraminifera or crinoids,wackestone / mudstone with calcispheres,bioclastic packstone / grainstone,unname reef-building organism framestone and brachiopod grainstone. In addition,four facies have been identified including open platform facies,restricted platform facies,coral reefal facies and shoal facies. According to analysis of microfacies combination and facies evolution,three stages and three reef units during the reef formation process have been noted. The evolution of each stage indicates a repeating fluctuation of the sea-level,but the water energy is still relatively low overall,which represents frequent changes of paleoclimate in the early Late Carboniferous. | GONG Enpu CHEN Xiaohong ZHANG Yongli GUAN Changqing CHANG Honglun HONG Guang | 2014 | Global Geology2014，17，4： | 0 |
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