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WU Ya Sheng
May 2003 at Texas A& M University as visiting scholar
Tel: 86-10-82998342 (O) Mobile Phone: 13241929326 Email: wys@mail.igcas.ac.cn, 111@geofinds.com Fax: 86-10-62010846 Mail add.: P.O. BOX 9825, Beijing 100029, China
Web:
http://www.geofinds.com/wys.htm 1994--Present Associate Professor of Institute of Geology and Geophysics, Chinese Academy of Sciences . 2005--present Member of the Council of the Paleontological Society of China. Member of the Commentator Committee of Science Times, the organ of Chinese Academy of Science Chief Editor of the international professional weekly web journal on geosciences, Earth & Life (www.geofinds.com). Educations
1999-2002 Ph.D. degree from Nanjing Institute of Geology and Paleontology, Chinese Academy of Sciences (Supervisor: JIN Yugan) 1984-1987 M.S. degree from Institute of Geology, Chinese Academy of Science (Supervisor: FAN Jiasong) 1980-1984 B.S. degree from Nanjing University
Researches & results
(1)Studied the extinction of the reef ecosystem in Ziyun, Guizhou Province, southwestern China at the end of the Permian, and found that the extinction of reef ecosystem at the end of the Permian happened in two steps: firstly, the extinction of all stenotropic organisms such as calcisponges and fusulinids in the Clarkina yini conodont zone, and secondly, the disappearance of microgastropod-dominated biota or algal mats at the beginning of the Hindeodus parvus zone. see: WU Ya Sheng, FAN Jia Song, JIANG Hong Xia & YANG Wan. Extinction pattern of reef ecosystems in latest Permian. Chinese Science Bulletin, 2007.Vol.52 No. 4 pp.512-520) Abstract in English Full-Paper PDF in English The Chinese version: 吴亚生, 范嘉松, 姜红霞, Yang Wan, 2007. 二叠纪末生物礁生态系绝灭的方式. 科学通报 , 52 (2): 207-214. Abstract in Chinese Full-paper PDF in Chinese (2) Studied the evolution of conodonts across Permian-Triassic boundary, and found that there is a lagged mass extinction in conodonts in the latest Permian. see: Wu Ya Sheng 2006. Lagged mass extinction in conodonts across the Permian-Triassic boundary. Earth & Life (http://www.geofinds.com), 1(1): 1-6. Full paper on web Full-paper PDF Wu Ya Sheng, 2005, Conodont evolution during Permian-Triassic transition in Mid-Low latitudes: a close-up view. Albertiana 33: 93-94. (=吴亚生, 2005. 二叠纪-三叠纪之交中低纬度地区牙形刺化石的演化. Albertiana 33: 93-94.）
(3) Studied the end-Permian extinction of thalamid sponges, the main reef-building organisms in Permian reefs, and found that all reef-building thalamid sponge species became extinct at the end of the Permian, and all thalamid sponge species in Middle and Upper Triassic reefs are new. see: WU Ya Sheng, FAN Jia Song, 2002, Permian-Triassic evolution of reefal thalamid sponges. Acta Paleontologica Sinica, 41(2): 163-177. (in Chinese with English abstract) (=吴亚生，范嘉松，2002，二叠纪-三叠纪礁相房室海绵演化。古生物学报。41（2）：163-177。) Abstract in Chinese Full-paper PDF (4) Studied the sedimentology of the P-T boundary sections in Xiushui, Jiangxi Province, south China, and found that there was substantial sea-level falls in the latest Permian in Xiushui, at about the same time as when the mass extinction happened! see: WU Ya Sheng, YANG Wan，JIANG Hong Xia, FN Jia Song, 2006，Petrologic evidence for sea-level drop in the latest Permian in Jiangxi Province, China, and its meanings for mass extinction. Acta Petrologica Sinica, 22(12): 3039-3046. (in Chinese with English abstract) (SCI impact factor being 1.1 in 2005) （=吴亚生，Yang Wan，姜红霞，范嘉松，2006，江西修水二叠纪－三叠纪界线地层的海平面下降的岩石学证据。 岩石学报， 22(12)：3039-3046。） Abstract pdf for Chinese pdf in images ppt pictures (rar) ppt pictures (zip) (5) Restudied the P-T boundary section at Laolongdong, Sichuan Province (now Chongqing City), southwestern China, and found that there was substantial sea-level falls in the latest Permian and the Earliest Triassic in Chongqing area! see: WU Ya Sheng, JIANG Hong Xia, LIAO Tai Ping. 2006. Sea-level drops in the Permian-Triassic boundary section at Laolongdong, Chongqing, Sichuan Province. Acta Petrologica Sinica, 22(9): 2405-2412. (in Chinese with English abstract) (SCI impact factor being 1.1 in 2005) (=吴亚生，姜红霞，廖太平，2006，重庆老龙洞二叠系－三叠系界线地层的海平面下降事件。岩石学报，22(9): 2405-2412.) Abstract Full-Paper PDF in Chinese Full-Paper PDF in images (6) Studied the temporal pattern of oceanic anoxia across the Permian-Triassic boundary and found that regardless of latitudes, the oceanic anoxia originated in deep-marine areas at the end of Permian and expanded to shallow-marine areas in the earliest Triassic. WU Ya Sheng, YANG Wan, JIANG Hong Xia, FAN Jia Song, 2007. Temporal Pattern of Oceanic Anoxia across the Permian-Triassic Boundary. Earth & Life (http://www.geofinds.com), 1(2): 15-22. (7) Studied a P-T boundary section in Guizhou Province, and found that a microbial biota adapted to anoxic condition was present in the Earliest Triassic Hindeodus parvus zone. see:wys-microbialite-sci chi D-english.pdf WU Ya Sheng, JIANG Hong Xia, YANG Wan & FAN Jia Song. 2007. Microbialite of anoxic condition from Permian-Triassic transition in Guizhou, China. Science in China, Series D, 50(1): 1-12. . (key points in this paper: (1) a microbial biota lived in parvus zone in Ziyun, Guizhou, China; (2) microbialites from PTB include six types; (3) the viewpoint that some reef ecosystems lived to Mesozoic is incorrect.) 吴亚生，姜红霞，Yang Wan，范嘉松，2007，二叠纪－三叠纪之交缺氧环境的微生物和微生物岩。中国科学，D, 37(5): 618-628。 （中国科学网站下载PDF有困难） (8) Revised the incorrectly assigned conodonts from the P-T boundary section in Meishan, Zhejiang Province (the GSSP of P-T boundary) and that in Shangsi, Sichuan Province, and made some revision on conodont zones of the P-T boundary strata. see: WU Ya Sheng, 2005, Conodonts, reef evolution and mass extinction across Permian-Triassic boundary. Geological Publishing House. (some paper copies available) PDF of content PDF of p1-p10 PDF of p11-20 PDF of p21-41 PDF of p42-90 (9) Studied the ecological selection in end-Permian extinctions of plants, reef-building organisms, foraminifers, bivalves, ammonoids, gastropods, brachiopods, ostracods and insects, and found that the extinct taxa are warm-water, stenobiontic organisms, while the sparse taxa that survived the crisis are eruytropic or eurythermal organisms that can inhabit cold water environments, and proposed that the end-Permian mass extinction was probably triggered by global climatic cooling! see: Wu Ya Sheng, 2006. Ecological selection in end-Permian mass extinction and its climatic implication. Earth & Life (http://www.geofinds.com), 1(1): 16-30. (10) Studied the floral features after the end-Permian mass extinction, and proposed that there was no climate zonation after the end-Permian mass extinction and the whole Earth was a “cooling ball”. see: Wu Ya Sheng: Cold climate after the end-Permian crisis as implied by the aftermath vegetation. Earth & Life (http://www.geofinds.com), 2006-10-1, Vol.1. , No.1: 12-15. Full text on web Full-papert PDF (11) Proposed the methods to quantitatively calculate the amplitude of pre-Cenozoic sea-level changes. see: WU Ya Sheng, FAN Jia Song, 2003, Quantitative evaluation of the sea-level drop at the end-Permian: based on reefs. Acta Geologica Sinica, 77(1): 95-102. (in English. SCI impact factor being 1.4 in 2005) Abstract in English Full-paper 吴亚生，范嘉松，金玉玕，2003，晚二叠世末的生物礁出露及其意义。地质学报，77（3）：289-296。(in Chinese with English abstract) Abstract in Chinese Full-paper PDF in Chinese
WU Ya Sheng, FAN Jia Song, 2002, Calculating eustatic amplitude of Middle Permian from reefs. Science in China, Series D, 45(3): 221-232. (in English) Abstract in English Full-paper PDF in English 吴亚生，范嘉松，2001，根据生物礁定量计算茅口期全球海平面变化幅度。中国科学，D，31（3）：233-242。(in Chinese) Abstract in Chinese Full-Paper PDF in Chinese (12) Studied the diagenesis in the main Ordovician reservoirs of the central Changqing gas fields, Ordos Basin, and recognized the main diagenetic patterns and pore system types. see: WU Ya Sheng, HE Shun Li, LU Tao, DA Shi Pan, LI Yu Gang, DAI Yong Ding. 2006. Diagenetic patterns and pore systems of the Lower Ordovician Majiagou Formation reservoirs of the central Changqing gas fields. Acta Petrologica Sinica 22(8): 2171-2181. (in Chinese with English abstract) Abstract in English Full-paper PDF scanned PDF (13) Studied the communities in the Middle Permian reef in Longlin, Guangxi Province, and described 68 new species and 44 new genera of calcisponges (thalamid sponges, inozoans, sclerosponges), hydrozoans, algae, and microproblematica. Many of them have been used by peers. Wu Ya Sheng, 1991, Organisms and communities of the Permian reef of Xiangbo, China.-calcisponges, hydrozoans, algae, microproblematica. International Academic Publisher. 192p. (Some paper copies are available. This monograph has been deposited in more than 50 libraries of famous universities including Harvard University and Southern California University. If you need a copy, please contact Wu Ya Sheng: wys@mail.igcas.ac.cn). (14) Proposed the conceptions of community-facies, fabric-facies, and diagenetic facies of reefs. see: Wu Ya Sheng, 1994. Community facies of reefs. Acta Petrologica Sinica, 10(2): 218-222. (in Chinese with English abstract) (=吴亚生, 1994, 生物礁的群落相. 岩石学报, 10/2:218-222.) Wu Ya Sheng, 1993, Diagenetic facies of reefs. Scientia Geologica Sinica, 2(3): 349-355. Wu Ya Sheng, 1992, Fabric-facies and fabric-rock-types of reefs. Science in China (Series B), 35/12: 1503-1511. 吴亚生, 1992, 生物礁的结构岩石类型和结构相。中国科学，B, 3: 304－310.
Ongoing and finished projects from NNSFC
[1] Paleoenvironmental changes and biotic evolution across Permian-Triassic boundary in reef-districts. (National Natural Scientific Foundation of China No. 40472015, as leader, 2005-2007) [2] Quantitative determination of amplitudes of global sea-level change in Late Permian Changxingian Stage. (National Natural Scientific Foundation of China No. 40172007, as leader, 2002-2004) [3] Probematic organisms in the Permian reefs in southwestern China (National Natural Scientific Foundation of China No. 49102017, as leader, 1992-1994) [4] Carbonate facies and sedimentary in South and North China. (National Natural Scientific Foundation of China No. 48970112, as key member, 1990-1993) [5] Triassic reefs in Sichuan and Guizhou Provinces, China. (National Natural Scientific Foundation of China No. 4870128, as key member, 1988-1990) [6] Permian and Triassic reefs in South China. (National Natural Scientific Foundation of China No. D84039, 1985-1987)
Some other publications
Wu Ya Sheng, Fan JS, 2000, Paleoecology of calcisponges. Acta Paleontologica Sinica, 39(4): 544-547. (＝吴亚生，范嘉松，２０００。钙质海绵之古生态。古生物学报，39(4): 544-547.)(in Chinese with English abstract) Abstract in English and Chinese Full text PDF Wu YS, Fan JS, 2004. Revision on some Permian-Triassic thalamid sponges. Act Palaeontologica Sinica, 43(4)：602-608. (=吴亚生，范嘉松，2004，对一些二叠纪－三叠纪房室海绵属种的分类厘定。古生物学报，43(4)：602-608。) Abstract in English and Chinese Full text PDF Wu YS, 1998. Development pattern of the Middle Permian reef in Tonglu, Zhejiang Province, China. Marine Oil and Gas Geology, 3(2): 11-15. (=吴亚生, 1998, 浙江桐庐冷坞中二叠世生物礁发育模式. 海相油气地质， 3(2): 11-15.) (in Chinese) Wu YS, 1997. Classification of reef rocks. Geological Review, 43(3): 281-289. (=吴亚生, 1997, 生物礁岩分类方案. 地质论评, 43(3): 281-289. ) (in Chinese with English bstract) Wu YS, Yang WQ, 1996. Evolution of thalamid sponges: computer analysis. Acta Palaeontologica Sinica 35(4): 500-508. (=吴亚生, 杨伟强, 1996, 房室海绵性状演化：微机分析. 古生物学报. 35(4): 500-508.) (in Chinese with English abstract) Wu YS, 1995. Paleontology and paleoecology of reefs. Bulletin of Institute of Geology, Chinese Academy of Science, 8: 248-262. (=吴亚生, 1995, 生物礁的古生物学与古生态学研究。中国科学院地质研究所集刊. 8: 248-262. ) (in Chinese) Wu YS, 1995. Characters and classification of thalamid sponges. Acta Palaeontologica Sinica, 34(3)381-392. (=吴亚生, 1995, 房室海绵特征与分类. 古生物学报, 34(3)381-392. ) (in Chinese with English abstract) Wu YS, 1995. Comparison of thalamid sponges in the Permian reefs of Longlin and of Tunisia. Guangxi Geology, 8(3). (=吴亚生, 1995, 重现率：广西隆林二叠纪生物礁房室海绵生物群与突尼斯二叠纪生物礁房室海绵生物群之对比。广西地质，8(3).) (in Chinese with English abstrct) Wu YS, 1994. Paleoecology of the Permian reefs in Guangxi and Guizhou Provinces. Oil and Gas Geology, 15(3):201-207. (=吴亚生, 1994, 广西贵州二叠纪生物礁的古生态. 石油与天然气地质, 15/3:201-207.) (in Chinese with English abstract) Wu Ya Sheng, 1993, Models of China reefs. Carboniferous to Jurassic--Pangea: Program and Abstracts. GSGP & CSPG. Wu YS, Liu SC, Liu GB, et al., 1992. Microfacies and fusulinid ecostratigraphy of the Middle Permian Maokou Stage in Tonglin, Anhui Province. Journal of Nanjing University (Erath Sciences, 4(1):75-81. (=吴亚生等, 1992, 安徽铜陵中二叠世茅口期微相分析与蜓生态地层研究. 南京大学学报（地球科学版）, 4(1):75-81.) (in Chinese with English abstract) Wu YS, 1992. Reef studies in China: current and the future. Oil and Gas Geology, 13(4). (=吴亚生, 1992,中国生物礁研究：现状与方向. 石油与天然气地质, 13(4). ) (in Chinese with English abstract) Wu YS, Fan JS, 1991. Conception and type of reefs. Oil and Gas Geology, 12(3). (=吴亚生，范嘉松, 1991, 生物礁分类的问题. 石油与天然气地质, 12(3).) (in Chinese with English abstract) Wu YS, 1991. Clacareous algae in the Middle Permian reef in Longlin, Guangxi Province. Acta Palaeontologica Sinica, 30(6). (=吴亚生, 1991, 广西隆林中二叠世生物礁的钙藻化石。古生物学报, 30(6). ) (in Chinese with English abstract) Wu YS, 1989. Comprehensive study on the Early Permian reef in Longlin, Guangxi Province. Geological Review, 35(1). (=吴亚生, 1989, 广西隆林早二叠世生物礁综合研究. 地质论评, 35(1).) (in Chinese with English abstract) 陈占坤，吴亚生，罗晓容，陈瑞银，2006，鄂尔多斯盆地陇东地区长8段古输导格架恢复。地质学报，80（5）：718-723。 Abstract in Chinese and English Full Text PDF 范嘉松，吴亚生. 2005. 世界二叠纪生物礁的基本特征及其古地理分布.古地理学报， 7(3): 287-304. 范嘉松，吴亚生，2004，从塔北隆起奥陶纪钙藻化石探讨奥陶纪的古环境。微体古生物学报，21(3)：251-266。 范嘉松，吴亚生，2002，川东二叠纪生物礁的再认识。石油与天然气地质，23（1）：12－18。 范嘉松，吴亚生，2002，广西、贵州和川东二叠纪三生物礁的钙藻化石及其古生态环境。微体古生物学报，19（4）：337－347。 Abstract in Chinese and English Full text PDF 范嘉松，吴亚生，2002，贵州关岭中三叠统坡段组沉积特征及其形成环境。古地理学报，4(1):67-74。 Abstract in Chinese and English Full text PDF 范嘉松，王予卯，吴亚生，2002，广西西部二叠纪生物礁中的海绵、水螅动物化石。古生物学报，41(3):334-348. 范嘉松，田树刚，吴亚生，2004，东昆仑阿尔格山二叠纪生物礁的特征及其古地理古气候意义。古地理学报，6(3): 329-338. 张发强; 王震亮; 吴亚生; 杨计海; 罗晓容; 2002. 消除影响压实趋势线地质因素的方法——以莺歌海盆地为例. 沉积学报 , 20(2): 326-332 Commentary papers on science and society problems
吴亚生，2007，现行职称评定体系的弊病。科学时报(http://www.sciencenet.cn 发布时间：2007-11-2 3:4:21： http://www.sciencenet.cn/htmlnews/200711274520125193204.html?id=193204 http://www.sciencenet.cn/sbhtmlnews/200711201736640193172.html?id=193172
吴亚生，2007，建立一种新的审稿机制-公示审稿制度。科学时报 www.sciencenet.cn 发布时间：2007-10-26 6:39:21 在科学网网址：http://www.sciencenet.cn/htmlnews/2007102675910771192637.html?id=192637
吴亚生，2005，科学研究岂可只定位于“跟踪”。科学时报 发布时间：2005-9-8 9:57:04： http://www.sciencenet.cn/html/shownews.aspx?id=136584
吴亚生，2004,，科学研究中的国家利益。科学时报，发布时间：2004-07-15：。 网址：http://www.sciencenet.cn/html/shownews.aspx?id=120127
吴亚生，2004，大题目是科技体制改革。科学时报，发布时间：2004-11-19： 网址：http://www.sciencenet.cn/html/shownews.aspx?id=125259
吴亚生，2005，从故宫门票涨价看国家财产功能异化。科学时报，发布时间：2005-01-10： 网址：http://www.sciencenet.cn/html/shownews.aspx?id=127441
吴亚生，2005，腐败生于贫穷？——从“廉政保证金”制度说起。科学时报，发布时间：2005-02-02。网址： 网址：http://www.sciencenet.cn/html/shownews.aspx?id=128444
吴亚生，2005，呼唤学者的良知回归。科学时报，发布时间：2005-02-22： 网址：http://www.sciencenet.cn/html/shownews.aspx?id=128767
吴亚生，2005，话说涨工资。科学时报：发布时间：2005-03-02 11:58:14： 网址：http://www.sciencenet.cn/html/shownews.aspx?id=129067
吴亚生，2005，应当怎样“培养”人才？。科学时报，发布时间：2005-03-16 13:57:47： 网址：http://www.sciencenet.cn/html/shownews.aspx?id=129614
吴亚生，2005，遏制招生腐败要靠严打。科学时报，发布时间：2005-04-15 13:26:24： 网址：http://www.sciencenet.cn/html/shownews.aspx?id=131117
吴亚生，2005，文化遗产保护要升至立法层次。科学时报，发布时间：2005-04-22。网址： http://www.sciencenet.cn/html/shownews.aspx?id=131360 引用：新浪网http://tech.sina.com.cn/d/2005-04-22/1405591009.shtml
吴亚生，2005，开展国际合作研究应注意平等。科学时报，发布时间：2005-04-25： 网址：http://www.sciencenet.cn/html/shownews.aspx?id=131388 引用：科学院网站http://www.cas.ac.cn/html/Dir/2005/04/26/12/77/99.htm
吴亚生，2005，弘扬“国学”要弘扬什么？ 科学时报，发布时间：2005-07-08： 网址：http://www.sciencenet.cn/html/shownews.aspx?id=134223
中国学者称2.5亿年前全球海平面下降
吴亚生：论文同行评议阻碍新观点发表
IN CHINESE： 1984年获南京大学理学学士学位，专业为古生物学与地层学；1987年获中国科学院地质与地球物理研究所理学硕士学位，研究方向为碳酸盐岩与生物礁；2002年在职获中国科学院南京地质古生物研究所理学博士学位，以及方向为古代全球环境变化与生物演化。硕士导师是中国著名生物礁专家范嘉松研究员；博士导师是国际古生物学会副主席、中国科学院院士金玉玕先生。2002年11月－2003年6月受国家教委资助在Texas A & M 大学地质系做高级访问研究，在国际著名碳氧同位素地质学专家E. Grossman教授那里做碳酸盐岩和腕足动物化石的碳氧同位素研究。 1987年留所工作至今。1994年特批晋升为中国科学院地质与地球物理研究所副研究员。1999年中国科学院实施创新工程后一直在担任创新副研究员岗位至今。从2005年起担任中国古生物学会理事。 1998年以前主要从事生物礁研究，着重于各门类造礁生物的系统古生物学研究、礁群落古生态学研究、礁体沉积学研究。近年来主要从事古代全球环境变化与生物演化研究。研究经历包括蜓（应为：虫筳）化石与二叠纪生物地层学、钙质海绵化石的古生物学和古生态学、二叠纪－三叠纪生物礁的古生物学和沉积学、碎屑岩和碳酸盐岩的成岩作用、新生代前全球海平面变化幅度的定量研究、二叠纪-三叠纪界线地层（PTB）的牙形刺生物地层学、腕足动物化石和碳酸盐岩全岩样品的碳氧同位素研究、生物礁相区PTB地层的生物与环境演化研究等。 主持过3项、参加过3项国家自然科学基金项目：《二叠纪生物礁疑难宗教生物研究》、《根据生物礁定量计算长兴期全球海平面变化幅度》、《生物礁相区的环境和生物演化》 承担和完成1项中国科学院资源与环境重大项目（K2951-B1-409）的子项目：《二叠纪乐平世生物礁群落演化》 承担和完成现代古生物学和地层学国家重点实验室开放基金项目开放基金１个：《江西修水生物礁顶二叠系-三叠系界线地层的环境和生物演化》（项目号053102） 承担和完成中国石油天然气总公司现代储层研究重点实验室开放基金１个：《贵州紫云晚二叠系生物礁顶白云岩流体运移模式》 承担和完成中国石油天然气总公司长庆油田分公司项目3个：《靖安油田西南区长6储层非均质性三维定量描述》、《长庆下古生代奥陶纪马家沟组储层成岩相》、《储层描述新技术探索研究》。 正在承担中国石油、中国石化项目2个：《苏里格气田苏6加密井区储层精细描述研究》、《塔中地区南坡奥陶系生物演化与礁滩相形成条件》。 以第一作者在核心刊物发表地质学方面的学术论文50余篇，出版英文版学术专著2部。曾获中国地质学会优秀论文奖。参加的项目获中国科学院科学进步二等奖。 主要研究成果：（1）确定了二叠纪末生物礁生态系集群灭绝发生的模式是二步式的（Wu et al., 2007）。第一步是所有狭适性生物的灭绝，发生在二叠纪末期的Clarkina yini带；第二步是广适性生物的灭绝，发生在三叠纪最初的Hindeodus parvus带。 （2）在二叠纪-三叠纪之交全球海平面变化研究中取得重要进展。国外学者(Wignall and Hallam, 1992, 1997) 提出二叠纪-三叠纪之交全球海平面只有上升，没有下降；是海平面上升造成海洋缺氧, 缺氧导致二叠纪末的生物大绝灭。 但是，本人在2001－2003年对贵州紫云生物礁顶部的2个P-T界线地层剖面的研究中，发现了海平面下降的证据（Wu & Fan, 2003）；2005年，在江西修水的P-T界线地层中也发现了海平面下降的证据（吴亚生等，2006, 岩石学报，12期）；2006年，在重庆老龙洞的P-T界线地层中再次发现海平面下降的证据（吴亚生等，2006，岩石学报，9期）。海平面下降证据在不同地区的P-T界线地层中的发现，证明外国学者抱持的P-T之交只有海平面上升的认识是不正确的。 （3）在贵州紫云的P-T界线地层中首次发现了一种适应缺氧环境的微生物化石（吴亚生等，2007，中国科学，中英文版）。 （4）在物种水平上研究了造礁生物房室海绵在二叠纪－三叠纪的演化，发现房室海绵在二叠纪末全部绝灭了，是一项填补空白的成果（吴亚生等，2002, 古生物学报）。 （5）提出了根据生物礁定量计算新生代前全球海平面变化幅度的方法。 定量计算新生代前的全球海平面变化幅度一直是地质学的难题。本人提出的根据生物礁结构相以及某些特殊的成岩相定量计算古代全球海平面变化幅度的方法（Wu & Fan, 2002；Wu & Fan, 2003）初步解决了这一难题。 （6）发现牙形刺生物群在二叠纪-三叠纪之交有一个滞后的集群绝灭事件，否定了前人的二叠纪-三叠纪之交牙形刺没有集群绝灭的看法（Wu,2005;该成果如Yin et al., 2007, Global and Planetary Change 55: 1-20） （7）全面修订了浙江煤山P-T界线金钉子剖面的牙形刺化石鉴定错误数十处（Wu, 2005,英文专著）。 （8）系统研究了广西隆林二叠纪生物礁的造礁生物和群落古生态，描述新属 68个新种44个（Wu, 1991）。有关成果已经被国外学者广泛引用。 （9）提出了生物礁结构相群落相和成岩相的研究方法（吴亚生，1992；Wu, 1992, 1993）。 代表性论著：以第一作者发表SCI期刊论文8篇国际刊物论文1篇: Wu Ya Sheng, Jiang Hong Xia, Yang Wan, Fan Jia Song, 2007, Microbialite of anoxic condition from Permian-Triassic transition in Guizhou, China. Science in China, Series D, 50(7): 1040-1051. Wu Ya Sheng, Fan Jia Song, Jiang Hong Xia, Yang Wan, 2007, Extinction pattern of reef ecosystems in latest Permian. Chinese Science Bulletin, 52(4): 512-520. 吴亚生，姜红霞，廖太平，2006，重庆老龙洞二叠系－三叠系界线地层的海平面下降事件。岩石学报，22(9): 2405-2412. 吴亚生，Yang Wan，姜红霞，范嘉松，2006，江西修水二叠纪－三叠纪界线地层的海平面下降的岩石学证据。 岩石学报， 22(12) 3039-3046。 吴亚生，何顺利，卢涛，达世攀，李跃刚，戴永定，2006，长庆中部气田奥陶纪马家沟组储层成岩模式与孔隙系统。岩石学报，2006，22（8）：2171－2181。 Wu Ya Sheng, 2005, Conodont evolution during Permian-Triassic transition in Mid-Low latitudes: a close-up view. Albertiana 33: 93-94. Wu Ya Sheng, Fan Jiasong, 2003, Quantitative evaluation of the sea-level drop at the end-Permian: based on reefs. Acta Geologica Sinica, 77(1): 95-102. Wu Ya Sheng, Fan JiaSong, 2002, Calculating eustatic amplitude of Middle Permian from reefs. Science in China, Series D, 45(3): 221-232. Wu Ya Sheng, 1992, Fabric-facies and fabric-rock-types of reefs. Science in China (Series B), 35/12: 1503-1511. 以非第一作者发表SCI期刊论文4篇: Jiang Hongxia, Wu Yasheng. 2007. Comment--The Pattern and Timing of Biotic Recovery from the End-Permian Extinction on the Great Bank of Guizhou, Guizhou Province, China (Payne et al. 2006). Palaios, 22(4): 1-4. Jiang Hongxia, Wu Ya Sheng, 2008. Filamentous cyanobacteria fossils and their significance in the Permian-Triassic boundary section at Laolongdong, Chongqing. Chinese Science Bulletin, (已经接受中文版，英文版在修改中)。 姜红霞，吴亚生，2007. 重庆二叠系-三叠系界线地层微生物岩新认识. 岩石学报，23）（5）：1189-1196. Shen Wenjie, Lin Yangting, Xu Lin, Li Jianfeng, Wu Yasheng and Sun Yongge. 2007. Pyrite framboids in the Permian–Triassic boundary section at Meishan, China: Evidence for dysoxic deposition. Palaeogeography, Palaeoclimatology, Palaeoecology, 253(3-4)：323-331. Cai, CF, Hu, GY, He, H., Li, J, Li, JF, Wu, Y. S., 2005. Geochemical characteristics and origin of natural gas and thermochemical sulfate reduction in Ordovician carbonates in the Ordos Basin, China. Journal of Petroleum Science and Engineering 48(3/4), 209-226. (SCI) （提供部分数据） (Jiang Hongxia为杨长春和我指导的博士生，已毕业，在博士期间的研究工作中表现出色；Shen Wenjie为广州所博士生，已毕业，研究工作同样十分出色)
近年的核心期刊论文： 吴亚生，姜红霞，Yang Wan，范嘉松，2007，二叠纪－三叠纪之交缺氧环境的微生物和微生物岩。中国科学，D, 37(5): 618-628. 吴亚生, 范嘉松, 姜红霞, Yang Wan, 2007. 二叠纪末生物礁生态系绝灭的方式. 科学通报 , 52 (2): 207-214. 吴亚生，范嘉松，2004，对一些二叠纪－三叠纪房室海绵属种的分类厘定。古生物学报，43(4)：602-608。 吴亚生，范嘉松，金玉玕，2003，晚二叠世末的生物礁出露及其意义。地质学报，77（3）：289-296。 吴亚生，范嘉松，2002，二叠纪-三叠纪礁相房室海绵演化。古生物学报。41（2）：163-177。 吴亚生，范嘉松，2001，根据生物礁定量计算茅口期全球海平面变化幅度。中国科学，D，31（3）：233-242。 吴亚生，范嘉松，2000，钙质海绵之古生态。古生物学报，39(4): 544-547. 吴亚生, 1994, 生物礁的群落相. 岩石学报, 10/2:218-222.) Wu Ya Sheng, 1993, Diagenetic facies of reefs. Scientia Geologica Sinica, 2(3): 349-355. 吴亚生, 1992, 生物礁的结构岩石类型和结构相。中国科学，B, 3: 304－310. 姜红霞，吴亚生，袁生虎. 2007. 重庆二叠-三叠系界线地层中发现干裂缝和侵蚀面及其意义. 高校地质学报，13(1): 53-59. 姜红霞，吴亚生. 2007. 江西修水二叠系－三叠系界线地层树枝状微生物岩状岩石成因初解. 地质论评，53(3): 233-239. 姜红霞，吴亚生，罗晓容，喻建，毛明陆，杨飏，陈瑞银. 2007. 鄂尔多斯盆地中南部三叠系长8油层组的成岩作用及其对储层物性的控制. 沉积与特提斯地质，27(1): 54-61. 陈占坤，吴亚生，罗晓容，陈瑞银，2006，鄂尔多斯盆地陇东地区长8段古输导格架恢复。 地质学报，80（5）：718-723。 范嘉松，吴亚生. 2005. 世界二叠纪生物礁的基本特征及其古地理分布.古地理学报， 7(3): 287-304. 范嘉松，吴亚生，2004，从塔北隆起奥陶纪钙藻化石探讨奥陶纪的古环境。微体古生物学报，21(3)：251-266。
英文专著： Wu Ya Sheng, 2005, Conodonts, reef evolution and mass extinction across Permian-Triassic boundary. Geological Publishing House. 90p. Wu Ya Sheng, 1991, Organisms and communities of the Permian reef of Xiangbo, China.-calcisponges, hydrozoans, algae, microproblematica. International Academic Publisher. 192p.
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