巩恩普
地质古生物学
个性化签名
- 姓名:巩恩普
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学术头衔:
博士生导师
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学科领域:
古生物学
- 研究兴趣:地质古生物学
巩恩普,男,1958年生。博士,教授,博士生导师。1982年和1985年分别从中南大学(原中南工业大学)获学士和硕士学位,1995年从东北大学获博士学位。从事专业:古生物学、地层学、沉积学。研究方向为生物礁地质学、辽西中生代地层古生物学。获国务院政府特殊津贴,入选辽宁省百千万人才工程百人层次计划,教育部地矿学科教学指导委员会委员,中国冶金地质学会理事兼副秘书长。多年来在地质古生物学研究领域取得多项重大成果,并发表在重要学术刊物上,为我国古生物学研究作出应有贡献。本人在完成教学任务的同时一直从事科学研究工作。作为项目负责人主持:国家自然科学基金项目“黔南桂西北石炭纪生物礁群落重建与礁体生长动力学研究”;教育部高等学校骨干教师资助计划项目“中国石炭纪典型生物礁生长动力学研究”;辽宁省自然科学基金项目“辽东石炭纪沉积盆地演化及生物造礁作用”;辽宁省“十五”科技攻关项目“辽宁北票地区鸟化石形成地质环境研究”;原冶金部“八五”攻关课题“扬子地台北缘震旦纪含锰岩系岩相古地理及优质锰矿成矿机理与找矿方向研究”;教育部博士学科点基金项目“辽西中生代反鸟起源及辐射演化序列研究”等多项国家和省部级项目。
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【期刊论文】Growth Dynamics of the Middle Devonian Jukoupu Bioherm, Xinshao, Hunan
巩恩普, Gong Enpu
ACTA GEOLOGICA SINICA, 1994, 7 (1): 95-105,-0001,():
-1年11月30日
The growth process, palacoccological fcatures and the function of organisms in reef-building of the Jukoupu bioherm in Hunan are discussed in detall. The bioherm is divided into 10 microfacies. Organisms are very abundant in the reef. Thirty-two genera belonging to 7 phyta have been recognized. They make up 5 communities composed mainly fo stromatopoies, corals and algae, each of which has its own salient ecological features. An analysis of all communities shows that the organic functions are very comples. The same organisms may possess diverse may involve five stages; (1) biostrome stage, (2) stabilization stage, (30 frame-type reef-building stage, (4) binding and covering-type-reef-building stage, and (5) baffle-type reef-building stage
Hunan Province,, Middle Devonian,, Reef., Community structure,, community succession,, growth process of bioherm
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巩恩普, GONG Enpu, HOU Lianhai and WANG Lixia
ACTA GEOLOGICA SINICA, 2004, 78 (1): 1-7,-0001,():
-1年11月30日
A large number of enantionithine birds are discovered from the Early Cretaceous Jiufutang Formation in western Liaoning, China. They are all small-sized birds with a few small tecth. The enantirnithine bird from the Jiufutang Formation in the Shangheshou area, Chaoyang, Liaoning Province reported in this paper is the largest individual known in all enantiornithine birds of the Early Cretaceous, Hower, its teeth posses a feature of pseudoheterodont. Some different development stages of the new teeth substiute the earlier stages and the stages of development are preserved in this speciment. T
Early Cretaceous,, enantionithine,, dental development,, Aberratiodontus wui
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巩恩普, GONG Enpu& FAN Jiasong
SCIENCE IN CHINA (Series D) 2000, 43 (4): 347-355,-0001,():
-1年11月30日
A typical reef occurs in the eastern part of south Qinling Mountains in Sanlixia, Xunyang, Shaanxi Province. The reef, extending in north-south direction, was built up by various kinds of calcareous tubes including Girvanella, tubular cyanobacteria and problem microbials. The bioclastic bank, built up by algal clasts, foraminiferous, and fusulinids, formed the reef basement, on which dasyclads baffle bioclasts formed the original bafflestone at a small scale on the reef base ment, and then a mass of bindstone was made up by all kinds of calcareous tubes and algae. On lateral part the reef is cryptalgal mudstone. The reef that occurred in the geosynclinal area is so familiar with one of the platforms in many respects, such as in reef structure, morphology and building mold. This indicates that building organisms have amazing adaptability and identity for building capacity in the two kinds of geotectonic background mentioned above.
Permian,, Qinling Mountains,, reef,, tubular cyanobacteria,, building mode.,
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巩恩普, GONG Enpu and GUAN Guangyue
Chinese Science Bulletin Vol. 42 No.14 July 1997,-0001,():
-1年11月30日
Alarge number of coral fossils such as Arachnastraea, Chaetetes and Mulithecopora have been found in the marine strata of the upper part of the Carboniferous Benxi Formation in the eastern part of North China. The coral fossils are so abundant that they form coral limestones in some outcrops. These limestiones almost made up a rock belt, in which coral reefs are formed in some sections [1]. The occurrrence of the belt provides improtant information for understanding of the history of the Middle and Late Carboniferous in the eastern part of North China.
eastern part of North China,, Benxi Formation., Coral limestone helt.,
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