研究兴趣
海洋地质；
古海洋学；
古气候变化；
第四纪地质学；
元素和同位素地球化学；
古气候数值模拟。
科研项目
国家自然科学基金面上项目-“：晚中新世大洋碳位移事件的成因机制及其古环境效应”,2018-1-2021.12;
国家杰出青年科学基金-“古海洋学””晚新近纪南海和太平洋碳酸盐补偿深度变化及其古气候意义”，2016.1-2020.12；
国家自然科学基金重大计划“南海深部计划”重点项目-“晚第三纪重大冰盖生长期南海深部洋流变迁”，2012.1-2015.12
国家自然科学基金面上项目-“蒙特利碳位移”末期太平洋中深层水团重组”,2010-1-2012.12；
国家自然科学基金面上项目-“氧同位素5期以来热带西非季风气候的高分辨率海洋记录”,2008.1-2010.12；
国家自然科学基金面上项目-“北极冰盖形成期南沙表层海水对地球轨道周期变化的响应”,2005.1-2007.12；
国家自然科学青年基金项目-“地球轨道驱动的半岁差周期及其在南沙海区的响应”，2004.1-2004.12；
教育部新世纪优秀人才支持计划项目-“中中新世太平洋中、深层水团变化与全球变冷”,2009-1-2011.12；
全国百篇优秀博士论文作者专项基金-“70,000年以来千年尺度上的东亚季风演化–来自南沙的气候记录”，2006.1-2010.12；
上海市青年科技启明星项目-“氧同位素5期东亚季风与印度尼西亚穿越流的对比研究”，2006.9-2008.9；
上海市青年科技启明星跟踪项目-“末次冰期旋回中西非气候变化的海陆响应”，2010.3-2012.3；
第十一届霍英东高等院校青年教师基金-“晚更新世热带西大西洋千年尺度的季风气候”,2008.1-2010.12;
上海市曙光人才项目-“千年尺度上热带季风系统与高纬过程的相位”，2012.1-2015.1。
上海市人才发展资金项目-“新近纪轨道尺度上开放太平洋和边缘海上层海水结构变化的异同点极其气候意义”,2014/01-2016/12.
上海市优秀学术带头人项目-“新近纪南海碳酸盐补偿深度变化及其古气候意义”, 2016/05-2019/04.
研究成果
论文：
Ma, X.L.*, Tian, J.*, Ma, W.T., Li, K., and Yu, J.M., 2018. Changes of deep Pacific overturning circulation and carbonate chemistry during middle Miocene East Antarctic ice sheet expansion. Earth and Planetary Science Letters, 484:253–263.
Tian, J.*, Ma, X.L., Zhou, J.H., and Wang, W.J., 2017. Subsidence of the northern South China Sea and formation of the Bashi Strait in the latest Miocene: paleoceanographic evidences from 9-Myr high resolution benthic foraminiferal d18O and d13C records. Palaeogeography, Palaeoclimatology, Palaeoecology, 466: 382–391, PALAEO8076.
Huang, Enqing, Tian, J., Qiao, P.J., Wan, S., Xie, X., and Yang, W.G., 2015. Early interglacial carbonate-dilution events in the South China Sea: Implication for strengthened typhoon activities over subtropical East Asia. Quaternary Science Reviews,125:61-77.
Huang, Enqing, Tian, J., and Liu, JingJing, 2015. Dynamics of the Australian–Indonesian monsoon across Termination II: Implications of molecular-biomarker reconstructions from the Timor Sea. Palaeogeogr. Palaeoclimatol. Palaeoecol., 423:32–43.
Tian, J.*, Wentao Ma, Mitchell Lyle, Julia Shackford, 2014. Synchronous mid-Miocene upper and deep oceanic d13C changes in the east equatorial Pacific linked to ocean cooling and ice sheet expansion. Earth and Planetary Science Letters, 406:72-80.
Ma,W.T., Chai, F., Xiu, P., Xue, H.J., and Tian, J., 2014. Simulation of export production and biological pump structure in the South China Sea. Geo-Marine Letters, DOI 10.1007/s00367-014-0384-0.
Ma, W.T., and Tian, J., 2014. Modeling the contribution of dissolved organic carbon to carbon sequestration during the last glacial maximum. Geo-Mar Lett, 34:471-482.
Ma, W.T., Fei Chai, Peng Xiu, Huijie Xue, and Jun Tian, 2013.Modeling the long-term variability of phytoplankton functional groups and primary productivity in the South China Sea. Journal of Oceanography, 69:527-544.
Tian, J.*, 2013. Coherent variations of the obliquity components in global ice volume and ocean carbon reservoir over the past 5 Ma. Science China Earth Sciences, 56(12):2160-2172.
Tian, J.*, M. Yang, M. W. Lyle, R. Wilkens, and J. K. Shackford, 2013. Obliquity and long eccentricity pacing of the Middle Miocene climate transition, Geochem. Geophys. Geosyst., 14, 1740–1755, doi:10.1002/ggge.20108.
Huang Enqing* and Tian Jun*, 2012. Sea-level rises at Heinrich stadials of early Marine Isotope Stage 3: Evidence of terrigenous n-alkane input in the southern South China Sea. Global and Planetary Change, 94-95:1-12.
Tian, J.*, X. Xie, W. Ma, H. Jin, and P. Wang, 2011. X-ray fluorescence core scanning records of chemical weathering and monsoon evolution over the past 5 Myr in the southern South China Sea, Paleoceanography, 26, PA4202, doi:10.1029/2010PA002045.
Ma Wentao, Tian Jun, Li Qianyu and Wang Pinxian, 2011. Simulation of long eccentricity (400‐kyr) cycle in ocean carbon reservoir during Miocene Climate Optimum: Weathering and nutrient response to orbital change. Geophys. Res. Lett., 38, L10701, doi:10.1029/2011GL047680.
Huang Enqing*, Tian Jun*, Steinke S., 2011. Millennial-scale dynamics of the winter cold tongue in the southern South China Sea over the past 26 ka and the East Asian winter monsoon. Quat. Res., 75:196–204.
Tian C.C., and Tian Jun*, 2010. Warming magnitude of Indonesian Throughflow during the penultimate deglaciation (Termination II) and its relationship with climate change in high-latitude regions. Chinese Science Bulletin, 55 (32): 3709-3717.
Tian J.*, Enqing Huang, Dorothy K.Pak, 2010. East Asian winter monsoon variability over the last glacial cycle: Insights from a latitudinal sea-surface temperature gradient across the South China Sea. Palaeogeogr. Palaeoclimatol. Palaeoecol., 292:319–324
Wang P., Tian J., Lourens L. (2010): Obscuring of long eccentricity cyclicity in Pleistocene oceanic carbon isotope records. Earth and Planetary Science Letters, 290:319-330.
Ma W.*, Tian J.*, and Li Q., 2010. Astronomically modulated late Pliocene equatorial Pacific climate transition and Northern Hemisphere ice sheet expansion. Chinese Science Bulletin, 55(2):212-220.
Tian J.*, Amelia Shevenell , Pinxian Wang, Quanhong Zhao, Qianyu Li, Xinrong Cheng, 2009. Reorganization of Pacific Deep Waters linked to middle Miocene Antarctic cryosphere expansion: A perspective from the South China. Palaeogeogr. Palaeoclimatol. Palaeoecol. 284:375-382.
Tian J.*, Quanhong Zhao, Pinxian Wang, Qianyu Li, Xinrong Cheng, 2008. Astronomically modulated Neogene sediment records from the South China Sea, Paleoceanography, 23, PA3210, doi:10.1029/2007PA001552.
Huang E.*, Tian J.*, 2008. Melt-Water-Pulse (MWP) events and abrupt climate change of the last deglaciation. Chinese Science Bulletin. 53(18), 2867-2878.
Tian J.*, Dorothy K. Pak., P.X. Wang, David Lea, Xinrong Cheng, Quanhong, Zhao (2006): Late Pliocene Monsoon Linkage in the Tropical South China Sea, Earth and Planetary Science Letters, 252, 72-81.
Tian J.*, P. Wang, R. Chen, and X. Cheng, 2005. Quaternary upper ocean thermal gradient variations in the South China Sea: Implications for east Asian monsoon climate. Paleoceanography, 20, PA4007, doi:10.1029/2004PA001115.
Tian J.*, Wang Pinxian, Cheng Xinrong, Wang Rujian, Sun Xiangjun, 2005. Forcing mechanism of the Pleistocene east Asian monsoon variations in a phase perspective. Science in China (D), 48(10), 1708-1717.
Wehausen R., Tian J., Hans-Jürgen Brumsack et al., 2005. Geochemistry of Pliocene sediments from ODP Site 1143 (southern South China Sea). Proc. ODP, Sci. Results 184: College Station, TX. (Ocean Drillin Program).
Tian J.*, Wang Pinxian, Cheng Xinrong, 2004. Responses of foraminiferal isotopic variations at ODP Site 1143 in the southern South China Sea to orbital forcing. Science in China (D) 47(10), 943-953.
Tian J.*, Wang Pinxian, Cheng Xinrong, 2004. Pleistocene Precession forcing of the upper ocean structure variations in the southern South China Sea. Progress in Natural Science 14(11), 1004-1009.
Tian J.*, Wang Pinxian, Cheng Xinrong, 2004. Time-frequency variations of the Plio-Pleistocene foraminiferal isotopes: A case study from the southern South China Sea. Earth Sciences-Journal of China University of Geosciences 15(3), 283-289.
Wang P., Tian, J., Xinrong Cheng, Chuanlian Liu, and Jian Xu, 2004. Major Pleistocene stages in a carbon perspective: The South China Sea record and its global comparison. Paleoceanography 19, doi:10.1029/2003PA000991, PA4005 1-16.
Tian J.*, Wang P.X., Cheng X.R., 2004. Development of the East Asian monsoon and Northern Hemisphere glaciation: oxygen isotope records from the South China Sea. Quaternary Science Reviews, 23:2007-2016.
Wang P., Tian J., Cheng X., Liu C., Xu J., 2003. Carbon reservoir changes preceded major ice-sheets expansion at the mid-Brunhes event. Geology, 31: 239-242.
Wang P., Tian J., Cheng X., Liu C., Xu J., 2003. Exploring cyclic changes of the ocean carbon reservoir. Chinese Science Bulletin 48(23): 2536-2548.
Tian J.*, Wang P.X., Cheng X.R., Li Q.Y., 2002. Astronomically tuned Plio-Pleistocene benthic d18O records from South China Sea and Atlantic-Pacific comparison. Earth and Planetary Science Letters 203: 1015-1029.
Wang P., Tian J., Cheng X., 2001. Transition of Quaternary glacial cyclicity in deep-sea records at Nansha, South China Sea. Science in China (Ser. D) 44, 926-933.
田军，拓守廷, 2015. 新十年科学大洋钻探——照亮地球的过去、现在和未来. 自然杂志, 37(4), 239-250.
马文涛,田军,李前裕, 2011. 晚更新世以来冰盖与大洋碳储库相互作用的箱式模型模拟. 地球科学-中国地质大学学报, 36(4):621-634.
田军，2011.跨越时空变化的季风系统-第2届PAGES全球季风研讨会回顾与展望.海洋地质与第四纪地质，31(1):61-65.
田翠翠，田军, 2010. 倒数第2 个冰消期印度尼西亚穿越流的增温幅度及其与高纬气候变化的关系.科学通报, 55(30)：2944-2952.
田军，2009， 新生代的气候节律：赤道太平洋IODP320、321航次。地球科学进展，24(12):11-15.
马文涛，田军，李前裕，2009，晚上新世赤道太平洋气候转型和北极冰盖扩张的轨道驱动。科学通报，54(22): 3537-3545.
黄恩清，田军，2008，末次冰消期冰融水事件与气候突变. 科学通报, 53(12): 1437-1447.
黄恩清，田军，2007，早上新世非洲季风与地中海表层生产力变化的岁差节律。地球科学－中国地质大学学报, 32(3):313-321.
田军，汪品先，2006，深海记录中的热带过程及其周期性。地球科学-中国地质大学学报，31(6):747-753.
田军，汪品先，成鑫荣，王汝建，孙湘君，2005. 从相位差探讨更新世东亚季风的驱动机制。中国科学D辑－地球科学, 35 (2): 158~166.
田军，汪品先，成鑫荣，李前裕，2005. 南海ODP1143站上新世至更新世天文年代标尺的建立.地球科学－中国地质大学学报，30(1)：31-39.
田军，汪品先，成鑫荣，李前裕，2005. 南海ODP1148站中中新世（12~18.3 Ma）天文调谐的年代标尺。地球科学－中国地质大学学报，30(5)：513-518.
田军，汪品先，成鑫荣，2004. 南海ODP1143站底栖有孔虫Cibicidoides与Uvigerina稳定氧碳同位素值的均衡试验, 地球科学－中国地质大学学报, 29(1):1-6.
田军,汪品先,成鑫荣, 2004, 南沙ODP1143站有孔虫同位素变化对地球轨道驱动的响应, 中国科学D辑, 34(5): 452-460.
田军, 汪品先, 成鑫荣, 2004，更新世南海南部上层海水结构变化的岁差驱动, 自然科学进展, 14(6): 683-688. pdf
汪品先，田军，成鑫荣，2001，第四纪冰期旋回转型在南沙深海的记录，中国科学-D辑，31(10):793-799.
专著：
Wang Pinxian, Li Qianyu (Eds), 2009, The South China Sea,参与编写, Springer, ISBN：978-1-4020-9744-7.
田军，2007，南海ODP1143站有孔虫稳定同位素揭示的上新世至更新世气候变化，bat365在线平台出版社, ISBN：978-7-5608-3402-3.
教学情况
主讲课(课程网站211.152.43.30:8889)：
《地球科学概论》(本科生)
《地球表层系统与演变》(硕士与博士研究生)
教学成果：
参编教材：《地球表层系统与演变》，科学出版社，2018
2018年度上海市重点课程建设项目：《地球科学概论》，负责人
指导研究生
在读研究生：
硕士：李金澜、李方舟、凤羽、杨莹、孔乐
博士：刘晶晶、杜金龙、冯华、庄燕培
已毕业研究生：
硕士：黄恩清、杨玫、刘晶晶、周建宏、陈云如
博士：马文涛、马小林