人才详细信息

姓名:张清海
性别:
学历:博士
专家类别:研究员
电话:010-84097079
传真:010-8409 7079
电子邮箱:zhang@itpcas.ac.cn
职称:研究员
通讯地址:北京市朝阳区林萃路16号院3号楼

简介

张清海,1980年生,中国科学院青藏高原研究所副研究员/项目研究员。主要从事早新生代古生物(大有孔虫)和古环境研究。在“Global and Planetary Change”“Geological Society of America Bulletin”“Gondwana Research”“International Journal of Earth Sciences”“The Journal of Geology”等期刊上发表论文20余篇。2013年获不来梅大学优秀博士论文。

教育背景 

1998.09 – 2002.06,大庆石油学院(现东北石油大学),学士 

2002.09 – 2005.06,中国石油大学(北京),硕士 

2005.09 – 2008.11,中国科学院青藏高原研究所,博士生 

2008.12 – 2013.01,德国不来梅大学,博士

工作经历 

2013.05 – 2017.01,德国不来梅大学,博士后 

2018.01 –     今,中国科学院青藏高原研究所,副研究员/项目研究员 

研究方向

古生物,古环境

职务

社会任职

 

承担项目

1.  国家自然科学基金面上项目:青藏高原及其周边地区早古近纪底栖大有孔虫的演化规律(2020–2023),主持 

2.  中国科学院人才项目:早古近纪大有孔虫分类学及基于大有孔虫的古生物地层和古环境研究(2018-2020),主持 

3. 德国自然科学基金(DFG)项目:The late Paleocene to early Eocene CIE and biotic changes in the eastern Neotethys Ocean (Tibet/China and Ladakh/India) 2013-2016),共同主持 

4.  德国自然科学基金(DFG)优先项目(1372)子课题:India-Eurasia plate convergence and environmental consequences (2009-2012),主要参与者 

获奖及荣誉

优秀博士论文,德国不来梅大学,2013

代表论著

1.  Zhang, Q.*, Ding, L., Kitajima, K., Valley, J. W., Zhang, B., Xu, X., et al. (2020). Constraining the magnitude of the carbon isotope excursion during the Paleocene-Eocene thermal maximum using larger benthic foraminifera. Global and Planetary Change, 184, 103049. 

2.  Zhang, Q.*, Willems, H., Ding, L., & Xu, X. (2019). Response of larger benthic foraminifera to the Paleocene-Eocene thermal maximum and the position of the Paleocene/Eocene boundary in the Tethyan shallow benthic zones: Evidence from south Tibet. Geological Society of America Bulletin, 131, 84-98. 

3.  Zhang, Q.* (2019). The Paleocene/Eocene boundary and the Tethyan shallow benthic zonation. Acta Palaeontologica Sinica, 58, 372-387. 

4.   Zhang, Q.*, Wendler, I., Xu, X., Willems, H., & Ding, L. (2017). Structure and magnitude of the carbon isotope excursion during the Paleocene-Eocene thermal maximum. Gondwana Research, 46, 114-123. 

5.  Zhang, Q.*, Willems, H., & Ding, L. (2013). Evolution of the Paleocene-Early Eocene larger benthic foraminifera in the Tethyan Himalaya of Tibet, China. International Journal of Earth Sciences, 102, 1427-1445. 

6.  Zhang, Q.*, Willems, H., Ding, L., Gr?fe, K.-U., & Appel, E. (2012). Initial India-Asia Continental Collision and Foreland Basin Evolution in the Tethyan Himalaya of Tibet: Evidence from Stratigraphy and Paleontology. The Journal of Geology, 120, 175-189. 

7.  Zhang, Q., Ding, L.*, Cai, F.-L., Xu, X.-X., Zhang, L.-Y., Xu, Q., & Willems, H. (2011). Early Cretaceous Gangdese retroarc foreland basin evolution in the Selin Co basin, central Tibet: evidence from sedimentology and detrital zircon geochronology. Geological Society, London, Special Publications, 353, 27-44. 

8.  Xiong, Z., Ding, L., Spicer, R. A., Farnsworth, A., Wang, X., Valdes, P. J., Su, T., Zhang, Q., et al. (2020). The early Eocene rise of the Gonjo Basin, SE Tibet: From low desert to high forest. Earth and Planetary Science Letters, 543, 116312. 

9.   Cai, F., Ding, L., Zhang, Q., Orme, D. A., Wei, H., Li, J., et al. (2020). Initiation and evolution of forearc basins in the Central Myanmar Depression. Geological Society of America Bulletin, 132, 1066-1082. 

10.   Kahsnitz, M. M., Zhang, Q., & Willems, H. (2016). Stratigraphic distribution of the larger benthic foraminifera Lockhartia in south Tibet (China). Journal of Foraminiferal Research, 46, 34-47. 

11.  Willems, H., Wendler, I., & Zhang, Q. (2015). Von der Schliessung des Tethys-Ozeans und der Entstehung des Himalaya. In G. Wefer & F. Schmieder (Eds.), Expedition Erde (pp. 51-57). Bremen. 

12.   Liebke, U., Appel, E., Ding, L., & Zhang, Q. (2013). Age constraints on the India - Asia collision derived from secondary remanences of Tethyan Himalayan sediments from the Tingri area. Journal of Asian Earth Sciences, 62, 329-340. 

13.  Ding, L., Yang, D., Cai, F., Pullen, A., Kapp, P., Gehrels, G., Zhang, L., Zhang, Q. et al. (2013). Provenance analysis of the Mesozoic Hoh-Xil-Songpan-Ganzi turbidites in northern Tibet: Implications for the tectonic evolution of the eastern Paleo-Tethys Ocean. Tectonics, 32, doi:10.1002/tect.20013. 

14.  Crouzet, C., Appel, E., El Bay, R., Ding, L., Dunkl, I., Montomoli, C., Carosi, R., Zhang, Q., Wauschkuhn, B. (2012). Kinematics of the crust around the Ama Drime Massif (southern Tibet) - Constraints from paleomagnetic results. Journal of Asian Earth Sciences, 58, 119-131. 

15.  Pullen, A., Kapp, P., Gehrels, G. E., Ding, L., & Zhang, Q. (2011). Metamorphic rocks in central Tibet: Lateral variations and implications for crustal structure. Geological Society of America Bulletin, 123, 585-600. 

16.  Ding, L., Cai, F., Zhang, Q., Zhang, L., Xu, Q., Yang, D., et al. (2009). Provenance and tectonic evolution of the foreland basin systems in the Gandese-Himalayan collisional orogen belt. Chinese Journal of Geology, 44, 1289-1311. 

17.  Cai, F., Ding, L., Zhang, Q., Xu, X., Yue, Y., Zhang, L., & Xu, Q. (2008). Provenance and tectonic evolution of the Yalu-Zangbo peripheral foreland basin. Acta petrological Sinica, 24, 430-446. 

18.  Bao, Z., Qi, Y., Jin, Z., Zhang, X., Hu, G., Zhang, Q., et al. (2007). Karst development respondence to sea-level fluctuation: a case from the Tarim area in the Early Paleozoic. Acta Geologica Sinica, 81, 205-211. 

19.  Ding, L., Yue, Y., Cai, F., Xu, X., Zhang, Q., & Lai, Q. (2006). 40Ar/39Ar geochronology, geochemical and Sr-Nd-O isotopic characteristics of the high-Mg ultrapotassic rocks in Lhasa block of Tibet: Implications in the onset time and depth of NS-striking rift system. Acta Geologica Sinica, 80, 1252-1261. 

20.  Bao, Z., Jin, Z., Sun, L., Wang, Z., Wang, Q., Zhang, Q., et al. (2006). Sea-level fluctuation of the Tarim area in the Early Paleozoic: Respondence from geochemistry and karst. Acta Geologica Sinica, 80, 366-373. 

21.  Bao, Z., Chen, J., Zhang, S., Zhao, H., Zhang, Q., & Li, Y. (2004). Sedimentary environment and development controls of the hydrocarbon source beds: Middle and Upper Proterozoic in northern North China. Science in China Series D, 47, 133-140.