人才详细信息
简介
个人简介：
张清海，中国科学院青藏高原研究所研究员。主要从事早新生代有孔虫生物地层、古环境和沉积盆地研究。在“Earth and Planetary Science Letters”、“Global and
Planetary Change”、“Geological Society of America Bulletin”、“Gondwana Research”、“International Journal of Earth Sciences”、“The Journal of Geology”等主流学术期刊上发表论文20余篇。（共同）主持二次科考任务七专题八、国家自然科学基金面上项目、中科院人才计划项目、德国自然科学基金（DFG）等项目，参与中科院先导A专项和德国DFG优先项目（TiP）。2013年获不来梅大学优秀博士论文。2020年获中国科学院杰出科技成就奖（主要完成者）。
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 – 2021/12，中国科学院青藏高原研究所，副研究员/项目研究员
2022/01 – 今，中国科学院青藏高原研究所，研究员
研究方向
古生物地层，古环境，沉积盆地演化，大地构造
职务
社会任职
承担项目
1. 第二次青藏高原综合科学考察研究任务七专题八：青藏高原不同地块的隆升过程与动力学机制（2022-2024），共同主持
2. 中国科学院人才择优项目：早古近纪大有孔虫在东特提斯洋的演化规律（2021-2023），主持
3. 国家自然科学基金基础科学中心项目课题一子课题六：印度与欧亚大陆碰撞详细过程及环境影响（2020-2024），主持
4. 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
5. 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
6. 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
获奖及荣誉
中国科学院杰出科技成就奖（主要完成者），中国科学院，2020
优秀博士论文，德国不来梅大学，2013
代表论著
1. Zhang, Q. *, Ding, L., Chen, X. *, Brennecka, G.A., Sun, Y., Ma, X., Gao, B., Zhang, Q., Willems, H. (2023). The large decline in carbonate δ238U from a PETM section at Tingri (South Tibet) was driven by local sea-level changes, not global oceanic anoxia. Earth and Planetary Science Letters 612, 118164.
2. Wang, T. *, He, S., Zhang, Q. *, Ding, L. *, Farnsworth, A., Cai, F., Wang, C., Xie, J., Li, G., Sheng, J., Yue, Y. (2023). Ice sheet expansion in the Cretaceous greenhouse world. Fundamental Research. Accepted.
3. Gao, B.-T., Zhang, Q. *, Ding, L., Zhang, H.-J., Fang, P.-Y. (2023). Age of the latest marine sedimentation in the western Kunlun area constrained by planktic foraminifera. Palaeoworld, doi:10.1016/j.palwor.2022.10.002.
4. 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.
5. 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.
6. Zhang, Q.* (2019). The Paleocene/Eocene boundary and the Tethyan shallow benthic zonation. Acta Palaeontologica Sinica, 58, 372-387.
7. 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.
8. 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.
9. 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.
10.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.
其他主要论文：
1. Cai, F., Ding, L., Wang, H., Laskowski, A.K., Zhang, L., Zhang, B., Mohammadi, A., Li, J., Song, P., Li, Z., Zhang, Q. (2021). Configuration and Timing of Collision Between Arabia and Eurasia in the Zagros Collision Zone, Fars, Southern Iran. Tectonics 40, e2021TC006762.
2. 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.
3. 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.
4. 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.
5. 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.
6. 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.
7. 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.
8. 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.
9. 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.
10.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.
11. 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.
12. 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.
13. 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.
14. 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.
15. 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.
