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广西南宁市大学东路100号
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博士研究生导师, 硕士研究生导师
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• 1992年毕业于南京大学，古生物学及地层学专业，获学士学位。• 1995年毕业于中国科学院南海海洋研究所，海洋地质专业，获硕士学位。• 2000年毕业于中国科学院广州地球化学研究所，地球化学专业，获博士学位。• 2002-2004年，同济大学海洋科学，博士后。• 1995-2013年于中国科学院南海海洋研究所工作，先后任助理研究员（1996年）、副研究员（2000 年）、研究员（2001 年）、博士研究生导师（2003 年）和二级研究员（2011 年）。• 2014年到广西大学工作，任“八桂****”****、“****”****。创建广西大学珊瑚礁研究中心、广西大学海洋学院、广西南海珊瑚礁研究重点实验室。
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• 中国第四纪科学研究会，常务理事。 • 中国第四纪科学研究会珊瑚礁专业委员会，主任（2009-2016）。 • 2011计划“中国南海研究协同创新中心”，特约研究员。• 《中国科学：地球科学》、《Science China: Earth Sciences》、《海洋学报》、《Acta Oceanologia Sinica》、《第四纪研究》、《海洋地质与第四纪地质》、《热带地理》、《海洋地质前沿》编委。
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多年专注于南海珊瑚礁地质、生态与环境研究，多次考察南沙群岛、西沙群岛、中沙群岛、海南岛、雷州半岛、涠洲岛和南海西岸的珊瑚礁.在历史时期珊瑚礁白化与恢复、珊瑚礁记录的全新世气候（温度、风暴、ElNino）事件与高分辨率气候过程、珊瑚礁记录的全新世海平面波动历史等方面取得研究进展。
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• 国家重大科学研究计划项目（973 项目）：南海珊瑚礁对多尺度热带海洋环境变化的响应、记录与适应对策研究，（2013-2017 年，经费2600 万元），首席科学家。 • 国家自然科学基金重点项目：珊瑚礁千米深钻记录的西沙碳酸盐台地形成演化和环境变迁史（2015-2018年，经费300万元），负责人。 • 国家****科学基金项目：第四纪地质学（2011-2014 年，经费200 万元），负责人。•国家自然科学基金重点项目: 全新世南海珊瑚礁白化的频率与恢复周期（2009-2012年 经费165万元），负责人。• 973计划项目课题: 热带海洋珊瑚礁台地与碳循环（2007-2011年, 经费: 368万元），负责人。• 国家海洋公益性行业科研专项项目：海南热带海洋生态资源可持续利用模式的研究（2007-2010年，经费248 万元），负责人。• 中国科学院知识创新工程重要方向性项目: 南海珊瑚礁记录之4000年来年代际温度过程与生态响应（2007-2009年, 经费180万元），负责人。• 国家科技支撑计划课题: 南沙海区珊瑚礁生态与工程地质环境调查技术及应用研究（2006-2008年, 经费300万元），负责人。• 国家自然科学基金重点项目: 全新世特征时期年际-年代际气候变化的南海珊瑚记录（2003-2006年, 经费120万元），负责人。• 科技部重大基础研究前期专项: 南海珊瑚礁记录的全新世冷、暖气候事件及其生态影响(2003-2005年，经费100万元) ，负责人。
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人才称号：• 2016年，国家“****”科技创新领军人才、教育部科技委学部委员• 2015年，教育部“****”****、政府特殊津贴获得者• 2014年，广西“珊瑚礁资源与环境”八桂****• 2013年, 入选国家百千****才工程、科技部中青年科技创新领军人才• 2012年, 国家重大科学研究项目(或973项目)首席科学家• 2010年, 国家****科学基金获得者代表性论文：(1)余克服．珊瑚礁科学概论．北京: 科学出版社, 2018: 1-578.(2)Huang Rongyong, Yu Kefu, Wang Yinghui, et al. (2018). Method to design a live coral cover sensitive index for multispectral satellite images. Optics Express, 26(10): 374-397. https://doi.org/10.1364/OE.26.00A374(3)Jiang Wei, Yu Kefu, Song Yingxian, et al. (2018). Annual REE signal of East Asian winter monsoon in surface seawater in the northern South China Sea: Evidence from a century-long Porites coral record. Paleoceanography and Paleoclimatology, 33: 168-178. https://doi.org/ 10.1002/2017PA003267(4)Jiang Wei, Yu Kefu, Song Yinxian, Zhao Jian-xin, et al. (2018). Coral geochemical record of submarine groundwater discharge back to 1870 in the northern South China Sea. Palaeogeography Palaeoclimatology Palaeoecology, 507: 30-38. https://doi.org/10.1016/j.palaeo.2018.05.045. (5)Pan ChangGui Yu Kefu, Wang YingHui, et al. (2018). Species-specific profiles and risk assessment of perfluoroalkyl substances in coral reef fishes from the South China Sea. Chemosphere, 2018, 191:450-457(6)Wang Rui, Yu Kefu, Brian Jones, et al. (2018). Evolution and development of Miocene “island dolostones” on Xisha Islands, China South Sea. Marine Geology, 406: 142-158, https: //doi.org/ 10.1016/ j.margeo. 2018. 09. 006.(7)Xu Shendong, Yu Kefu, Wang Yinghui, et al. (2018). Oil spill recorded by skeletal δ13C of Porites corals in Weizhou Island, Beibu Gulf, Northern South China Sea. Estuarine, Coastal and Shelf Science, 207: 338-344. https://doi.org/10.1016/j.ecss.2018.04.031(8)Xu Shendong., Yu Kefu, Tao, Shichen., et al. (2018).Evidence for the thermal bleaching of Porites corals from 4.0 ka B.P. in the Northern South China Sea. Journal of Geophysical Research: Biogeosciences,123: 79-94. https://doi.org/10.1002/2017JG004091(9)Yan Hongqiang, Yu Kefu, Shi Qi, et al. (2018). Air-sea CO2 fluxes and spatial distribution of seawater pCO2 in Yongle Atoll, northern-central South China Sea. Continental Shelf Research, 165: 71-77, https://doi.org/10.1016/j.csr.2018.06.008(10)Zhang Yu, Yu Kefu, Qian Handong. (2018). LA-ICP-MS Analysis of Clinopyroxenes in Basaltic Pyroclastic Rocks from the Xisha Islands, Northwestern South China Sea. Minerals, 8(12): 575; doi:10.3390/min**(11)Liang Jiayuan, Yu Kefu, Wang Yinghui, et al. (2017). Distinct bacterial communities associated with massive and branching scleractinian corals and potential linkages to coral susceptibility to thermal or cold Stress. Frontiers in Microbiology, 8 Psii 979(12)Jiang Wei, Yu Kefu, Song Yinxian, et al. (2017). Coral trace metal of natural and anthropogenic influences in the northern South China Sea. Science of the Total Environment, 607-608:195-203(13)Guo Jing, Yu Kefu, Wang Yinghui, et al. (2017). Nutrients distribution in coral reefs degraded area-Sanya,South China Sea. Journal of Coastal Research, 33(5):1148-1160(14)Wang Guanghua, Yu Kefu, Wang Yinghui, et al. (2017). Pelagibacterium lentulum sp. nov., a marine bacterium from the culture broth of Picochlorum sp. 122. International Journal of Systematic and Evolutionary Microbiology, 67(9): 3182-3185(15)Huang Rongyong, Yu Kefu, Wang Yinghui, et al. (2017). Bathymetry of the Coral Reefs of Weizhou Island Based on Multispectral Satellite Images. Remote Sensing, 9, 750(16)Xu Lijia, Yu Kefu, Li Shu, et al. (2017). Interseasonal and interspecies diversities of Symbiodinium density and effective photochemical efficiency in five dominant reef coral species from Luhuitou fringing reef, northern South China Sea. Coral Reefs, 36:477-487(17)Zhao Meixia, Yu Kefu, Shi Qi, et al. (2017). Comparison of coral diversity between big and small atolls: a case study of Yongle atoll and Lingyang reef, Xisha Islands, central of South China Sea. Biodiversity and Conservation, 26:1143-1159(18)Pei Jiying, Yu Kefu, Wang Yinghui. (2016). Thermal bursting ionization for ambient mass Spectrometry. RSC Advances, 6, 2496–2499(19)Yan Hongqiang, Yu Kefu, Shi Qi, et al. (2016). Seasonal variations of seawater pCO2 and sea-air CO2 fluxes in a fringing coral reef, northern South China Sea. Journal of Geophysical Research: Oceans. 121(1): 998-1008. DOI: 10.1002/2015JC011484(20)Zhao Meixia, Yu Kefu, Shi Qi, et al. (2016). The coral communities of Yongle atoll: status, threats and conservation significance for coral reefs in South China Sea. Marine and Freshwater Research, 67: 1888-1896(21)Yang Hongqiang, Yu Kefu, Zhao Meixia, et al. (2015). Impact on the coral reefs at Yongle Atoll, Xisha Islands, South China Sea from a strong typhoon direct sweep: Wutip, September 2013. Journal of Asian Earth Sciences, 114(3): 457–466(22)Zhao Meixia, Yu Kefu, Zhang Qiaoming, et al. (2014). Age structure of massive Porites lutea corals at Luhuitou fringing reef (northern South China Sea) indicates recovery following severe anthropogenic disturbance. Coral Reefs, 33(1): 39-44(23)Song Yinxian, Yu Kefu, Zhao Jianxin, et al. (2014). Past 140-year environmental record in the northern South China Sea: evidence from coral skeletal trace metal variations. Environmental Pollution, 185: 97-106.(24)Meng Qingshan, Yu Kefu, Wang Ren, et al. (2014).Characteristics of Rocky Basin Structure of Yongshu Reef in the Southern South China Sea. Marine Georesources & Geotechnology, 32: 307-315.(25)Zhang, Huiling, Yu, Kefu, Zhao, Jianxin, Feng Yuexin, Lin Yushi, Zhou Wei, Liu Guohui, (2013). East Asian Summer Monsoon variations in the past 12.5 ka: High-resolution δ18O record from a precisely dated aragonite stalagmite in central China. Journal of Asian Earth Sciences 73, 162-175. (26)Zhao Meixia, Yu Kefu, Shi Qi et al. (2013). Coral communities of the remote atoll reefs in the Nansha Islands, southern South China Sea. Environ Monit Assess, 185: 7381-7392(27)Chen Tianran, Yu Kefu, Chen Tegu. (2013). Sr/Ca–sea surface temperature calibration in the coral Porites lutea from subtropical northern South China Sea. Palaeogeography, Palaeoclimatology, Palaeoecology 392, 98-104.(28)Song Yinxian, Yu Kefu., Ayoko Godwin A, et al. (2013). Vibrational spectroscopic characterization of growth bands in Porites coral from South China Sea. Spectrochimica Acta Part A: Molecular and Biomolecular Spectroscopy 112, 95-100.(29)Zhao Meixia, Yu Kefu, Zhang Qiaoming, et al. (2012). Long-term decline of a fringing coral reef in the northern South China Sea. Journal of Coastal research, DOI: 10.2112/JCOASTRES-D-10-00172.1.(30)Yu kefu, et al. (2012). Recent massive coral mortality events in the South China Sea: was global warming and ENSO variability respon sible? Chemical Geology, 320-321: 54-65.(31)Yu Kefu, et al. (2012). High-precision U-series ages of storm-transported coral blocks on Heron Reef (southern Great Barrier Reef) and storm activity during the last century. Palaeogeography Palaeoclimatology Palaeoecology, 337-338: 23-36(32)Yu Kefu. (2012). Coral reefs in the South China Sea: their responses to and records on past environmental changes. Science China-Earth Sciences, 55(8): 1217-1229 [余克服，2012. 南海珊瑚礁及其对全新世环境变化的记录与响应. 中国科学-地球科学 42(8): 1160-1172.](33)Yu Kefu, et al. (2010). Holocene marine 14C reservoir age variability: evidence from 230Th-dated corals in the South China Sea. Paleoceanography, PA3205, doi:10.1029/2009PA001831. (34)Yu Kefu, et al. (2010). U-series dates of Great Barrier Reef corals suggest at least +0.7m sea level ~7000 years ago. The Holocene 20, 161-168. (35)Yu Kefu, et al. (2010). Timing and duration of growth hiatuses in mid-Holocene massive Porites corals from the northern South China Sea. Journal of Quaternary Science 25(8), 1284-1292. (36)Yu Kefu, et al. (2009). Microatoll record for large century-scale sea-level fluctuations in the mid-Holocene. Quaternary Research 71, 354-360.(37)Yu Kefu, et al. (2009). Reconstruction of storm/tsunami records over the last 4000 years using transported coral blocks and lagoon sediments in the southern South China Sea. Quaternary International 195, 128-137.(38)Yu Kefu, et al (2009). Coral reefs (of the South China Sea). In: Wang PX and Li QY (eds), The South China Sea – Paleoceanography and sedimentology, Springer, Dordrecht, The Netherlands, 186-209.(39)Yu Kefu, et al. (2009). Beach sediment from northern South China Sea suggest high and osicillating sea level during the late Holocene. Earth Science Frontiers 16, 138-145.(40)Yu Kefu, et al. (2007). High-precision analysis on annual variations of heavy metals, lead isotopes and rare earth elements in mangrove tree rings by inductively coupled plasma mass spectrometry. Nuclear Instruments & Methods in Physics Research Section B-Beam Interactions with Materials and Atoms 255, 399-408.(41)Yu Kefu, et al. (2006). U-series dating of dead Porites corals in the South China sea: Evidence for episodic coral mortality over the past two centuries. Quaternary Geochronology 1, 129-141.(42)Yu Kefu, et al. (2006). High-precision TIMS U-series and AMS C-14 dating of a coral reef lagoon sediment core from southern South China Sea. Quaternary Science Reviews 25, 2420-2430.(43)Yu Kefu, et al. (2005). Mid-late Holocene monsoon climate retrieved from seasonal Sr/Ca and δ18O records of Porites lutea corals at Leizhou Peninsula, northern coast of the South China Sea, Global and Planetary Change, 47(2-4): 301-316.(44)Yu Kefu, et al. (2005). δ18O, Sr/Ca and Mg/Ca records of Porites lutea corals from Leizhou Peninsula, northern South China Sea and their applicability as paleothermometers, Palaeogeography Palaeoclimatology Palaeoecology, 218(1-2): 57-73.(45)Yu Kefu, et al. (2005). Recent progress and further potenyial: High-resolution Holocene climate reconstruction with coral reefs in the South China Sea. PAGES News, 2005, 13(2): 20-22.(46)Yu Kefu, et al. (2004). High-frequency winter cooling and coral mortality during the Holocene climatic optimum. Earth and Planetary Science Letters, 2004, 224(1-2): 143-155. (47)Yu Kefu, et al. (2004). Alpha-cellulose δ13C variation in mangrove tree rings correlates well with annual sea level trend between 1982 and 1999. Geophysical Research Letters, 31: L11203, doi:10.1029/2004GL019450. (48)Yu Kefu, et al. (2004). Storm cycles in the last millennium recorded in Yongshu Reef, southern South China Sea. Palaeogeography Palaeoclimatology Palaeoecology, 210(1): 89-100. (49)Yu Kefu, et al. (2002). High-frequency climatic oscillations recorded in a Holocene coral reef at Leizhou Peninsula, South China Sea. Science in China, Series D, 45(12): 1057-1067. (50)Yu Kefu, et al. (2002). High-resolution climate recorded in the δ13C of Porites lutea from Nansha Islands of China. Progress in Natural Science, 2002, 12(4): 284-288. (51)Yu Kefu, et al. (2001). The high-resolution climate recorded in the δ18O of Porites lutea from the Nansha Islands of China. Chinese Sciences Bulletin, 2001, 46(24): 2097-2102 (52)余克服，张光学，汪稔. (2014) 南海珊瑚礁: 从全球变化到油气勘探—第三届地球系统科学大会专题评述．地球科学进展. 2014, 29(11): 1287-1293.(53)余克服．年轻沉积物形成年龄的测定．见: 丁仲礼(主编)．固体地球科学研究方法．北京: 科学出版社, 2013: 566-579.(54)廖芝衡, 余克服, 王英辉. (2016).大型海藻在珊瑚礁退化中的作用. 生态学报, 36(21), doi: 10.5846/stxb9.(55)覃祯俊，余克服，王英辉. (2016) 珊瑚礁生态修复的理论与实践. 热带地理, 2016, 36(1): 80-86. (56)王丽荣, 余克服, 赵焕庭, 等. (2014). 南海珊瑚礁经济价值评估. 热带地理, 34(1): 44-49.(57)施祺, 余克服, 陈天然, 等. (2012). 南海南部美济礁200 余年滨珊瑚骨骼钙化率变化及其与大气CO2和海水温度的响应关系. 中国科学-地球科学 42(1): 71-82.(58)严宏强, 余克服, 施祺, 等. (2011). 南海珊瑚礁夏季是大气CO2的源. 科学通报, 55(6): 414-422(59)李淑, 余克服, 陈天然, 等. (2011). 珊瑚共生虫黄藻密度结合卫星遥感分析2007年南沙群岛珊瑚热白化. 科学通报，56(10): 756-764 .(60)黄玲英, 余克服. (2010). 珊瑚疾病的主要类型、生态危害及其与环境的关系. 生态学报, 30(5): 1328-1340.(61)余克服，陈特固. (2009). 南海北部晚全新世高海平面及其波动的海滩沉积证据. 地学前缘, 2009, 16(6): 138-145.(62)陈天然，余克服，施祺，等. (2009). 大亚湾石珊瑚群落近25年的变化及其对2008年极端低温事件的响应. 科学通报, 54(6): 812-820.(63)严宏强, 余克服, 谭烨辉. (2009). 珊瑚礁区碳循环研究进展. 生态学报, 29(11): 6207-6215. (64)张江勇, 余克服. (2008). 珊瑚骨骼生长研究进展. 地质论评, 54(3): 362-372(65)李 淑, 余克服, 施祺, 等. (2007). 南海北部珊瑚共生虫黄藻密度的种间与空间差异及其对珊瑚礁白化的影响. 科学通报, 52(22): 2655-2662(66)李 淑, 余克服. (2007). 珊瑚礁白化研究进展. 生态学报, 27(5): 2059-2069(67)赵美霞,余克服, 张乔民. (2006). 珊瑚礁区的生物多样性及其生态功能. 生态学报, 26(1): 186-194(68)陈天然, 余克服, 林志芬, 等. (2006). 珊瑚礁对赤潮的响应与记录研究进展. 岩石矿物学杂志, 25(6): 523-529(69)余克服. (2005). 雷州半岛珊瑚礁的生态特征与资源可持续利用. 生态学报, 2005, 25(4): 669-675.(70)韦刚健，余克服，赵建新. (2004). 雷州半岛中晚全新世造礁珊瑚Sr/Ca比值的表层海水温度记录，科学通报, 49(17)：1770-1775(71)赵建新, 余克服. (2001). 南海雷州半岛造礁珊瑚的质谱铀系年代及全新世高海面. 科学通报, 46(20): 1734-1738
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