西北大学地质学系

教师名称


2005年毕业于中国科学院地球环境研究所,2009-2010年在美国佐治亚大学海洋系做访问学者,2012-2014年以玛丽居里学者身份在英国布里斯托尔大学化学系从事研究。

website:http://geology.nwu.edu.cn/en/wp-content/pws/zhengyanhong/

  主持国家级科研项目:


1、国家自然科学基金面上项目,41372033、东北全新世泥炭微生物类脂物记录:季风变化及其对甲烷生物地球化学过程的影响、2014/01-2017/12。

2、国家自然科学基金面上项目,41072024、青藏高原东北部泥炭微生物群落时空分布及其对季风气候变化的响应、2011/01-2013/12。

3、国家自然科学基金青年基金项目,40602004、青藏高原东北部泥炭类脂分子单体碳氢同位素高分辨率的生物与气候研究、2007/01-2009/12。

主持国际科研项目:

1、欧盟玛丽居里行动计划,2012-2014与2015-2016。

代表性论文:

Zheng, Y,Pancost, R, Liu, X, Wang, Z, Naafs, D, Xie, X, Liu, Z, Yu, X & Yang, H. Atmospheric connections with the North Atlantic enhanced the deglacial warming in Northeast China.Geology, 2017, in press.

B.D.A. Naafs, G.N. Inglis, Y. Zheng, M.J. Amesbury, H. Biester, R. Bindler, J. Blewett, M.A. Burrows, D. del Castillo Torres, F.M. Chambers, A.D. Cohen, R.P. Evershed, S.J. Feakins, M. Gałka, A. Gallego-Sala, L. Gandois, D.M. Gray, P.G.  Hatcher, E.N. Honorio Coronado, P.D.M. Hughes, A. Huguet, M. Könönen, F. Laggoun-Défarge, O. Lähteenoja, M. Lamentowicz, R. Marchant, E. McClymont, X. Pontevedra-Pombal, C. Ponton, A. Pourmand, A.M. Rizzuti, L. Rochefort,  J. Schellekens, F. De Vleeschouwer, R.D. Pancost. Introducing global peat-specific temperature and pH calibrations based on brGDGT bacterial lipids. Geochimica et Cosmochimica Acta, 2017, 208: 285-301.

Slowakiewicz, M., Whitaker, F., Thomas, L., Tucker, M.,Zheng, Y., Gedl, P., Pancost, R.D. Biogeochemistry of intertidal microbial mats from Qatar: New insights from organic matter characterisation.Organic Geochemistry, 2016, 102: 14-29.

Zheng, Y.,Li, Q., Wang, Z., Naafs, B., Yu, X., Pancost, R.D.Peatland GDGT records of Holocene climatic and biogeochemical responses to the Asian Monsoon.Organic Geochemistry, 2015, 87: 86-95.

Zheng, Y., Singarayer, J.S., Cheng, P., Yu, X., Liu, Z., Valdes, P.J., Pancost, R.D., Holocene variations in peatland methane cycling associated with the Asian summer monsoon  system. Nature Communications, 2014, 5:4631 doi: 10.1038/ ncomms5631.

Li, Y. X., Zhang, Y. X.,Zheng, Y. H.Erinaceus europaeusfossils (Erinaceidae, Insectivora) from the Middle Pleistocene cave site of Shanyangzhai, Hebei Province, China.Quaternary International, 2013, 286: 75-80.

Zheng, Y. H., Zhou, W. J., Meyers, P. A. Proxy value ofn-alkan-2-ones in the Hongyuan peat sequence to reconstruct Holocene climate changes on the Eastern margin of the Tibetan Plateau. Chemical Geology, 2011, 288, 97-104.

Seki, O., Meyers, P. A., Yamamoto, S., Kawamura, K., Nakatsuka, T., Zhou, W. J.,Zheng, Y. H. Plant-wax hydrogen isotopic evidence for postglacial variations in delivery precipitation in the monsoon domain of China.Geology, 2011, 39, 875-878.

Zheng, Y. H., Liu, X. M., Zhou, W, J., Zhang, C. L.n-Alkan-2-one distributions in a northeastern China peat core spanning the last 16kyr.Organic Geochemistry, 2011, 42:25-30.

Zheng, Y. H., Zhou, W. J., Liu, Z., Liu, X. M. The n-alkanol paleoclimate records in two peat deposits: a comparative study of the northeastern margin of the Tibetan Plateau and Northeast  China. Environmental Earth Sciences, 2011, 63: 135-143.

Yamamoto, S, Kawamura, K., Seki, O., Meyers, P. A.,Zheng, Y. H., Zhou, W. J. Environmental influences over the last 16ka on compound-specific δ13C variations of leaf wasn-alkanes in the Hani peat deposit from Northeast China.Chemical Geology, 2010, 277: 261-268.

Yamamoto, S., Kawamura, K., Seki, O., Meyers, P. A.,Zheng, Y. H., Zhou, W. J. Paleoenvironmental significance of compound-specific δ13C variations inn-alkanes in the Hongyuan peat sequence from southwest China over the last 13ka.Organic Geochemistry, 2010, 41: 491-497.

Zheng, Y. H., Zhou, W. J., Liu, Z., Chen, Q. M., Yu, X. F., Liu, X. M. Compositions of aliphaticdes-A-triterpenoids in the Hani peat deposit, Northeast China and its biological significance. Chinese Science Bulletin, 2010, 55: 2275-2281.

Zhou, W.,Zheng, Y. H., Meyers, P. A., Jull, A. J. T., Xie, S. C. Postglacial climate-change record in biomarker lipid compositions of the Hani peat sequence, northeastern China.Earth and Planetary Science Letters, 2010, 294: 37-46.

Yu, X. F., Zhou, W. J., Liu, X. Q., Xian, F., Liu, Z.,Zheng, Y. H., An, Z. S. Peat records of human impacts on the atmosphere in Northwest China during the late Neolithic and Bronze Ages. Palaeogeography, Palaeoclimatology, Palaeoecology, 2010, 286(1-2):17-22.

Seki, O., Meyers, P. A., Kawamura, K.,Zheng, Y. H., Zhou, W. J. Hydrogen isotopic ratios of plant-waxn-alkanes in a peat bog deposited in northeast china during the last 16kyr. Organic Geochemistry, 2009, 40: 671-677.

Zheng, Y. H., Zhou, W. J., Xie, S. C., Yu, X. F. A comparative study ofn-alkane biomarker and pollen records: an example from southern China.Chinese Science Bulletin, 2009, 54(6):1065-1072.

Zheng, Y. H., Xie, S. C., Liu, X. M., Zhou, W. J.n-alkanol ratios as proxies of  paleovegetation and paleoclimate in a peat-lacustrine core in southern China since the last deglaciation. Frontiers Earth Sciences in China, 2009, 3(4): 445-451.

Zheng, Y. H., Zhou, W. J., Xie, S. C,, Meyers, P. A. Lipid Biomarkers in the Zoigê-Hongyuan Peat Deposit: Indicators of Holocene Climate Changes in West China.Organic Geochemistry, 2007, 38:1927-1940.

Zhou, W. J., Xie, S. C., Meyers, P. A.,Zheng, Y. H.Reconstruction of late glacial and Holocene climate evolution in southern China from geolipids and pollen in the Dingnan peat sequence.  Organic Geochemistry, 2005, 36: 1272-1284.

编辑

郑艳红

所属部门:古生物教研室
职称:教授
研究方向:第四纪气候与全球变化;有机生物地球化学;地微生物
电子邮件:zhengnwu@163.com

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