马文涛研究员

出生年月:1981年12月

学位学历:博士

研究方向:海洋生物地球化学循环

教育背景及工作经历

2022/12-现在:自然资源部第二海洋研究所研究员;

2017/12-2022.11自然资源部第二海洋研究所副研究员;

2015/06月-2017/11同济大学海洋高等研究院副研究员;

2011/04月-2015/06同济大学博士后;

2011/08月-2012/02美国缅因大学访问学者;

2007/09-2011/03同济大学, 海洋与地球科学学院, 海洋地质专业, 博士/博士学位;

2004/09-2007/06中国地质大学(武汉), 地空学院,  固体地球物理专业, 硕士/硕士学位;

2000/09-2004/06中国地质大学(武汉),  地空学院, 地球物理专业, 本科/学士学位。

科研项目及荣誉奖励

1. 重点研发计划课题, 近海碳汇可持续性与增汇潜力模拟(项目编号:2023YFC3108104), 资助额度:241万元. 起止时间:2023/12-2026/11;

2. 国家自然科学基金面上项目, 末次盛冰期热带东印度洋上升流及其碳循环效应的高分辨率数值模拟(项目编号:42276063), 资助额度:55万元. 起止时间:2023/01-2026/12;

3. 南方海洋科学与工程广东省实验室(珠海)自主科研项目课题, 南海海洋生物地球化学过程数值模拟研究(项目编号:SML2020SP008), 资助额度:90万元. 起止时间:2020/11-2023/10;

4. 中国科学院战略性先导科技专项(B类)子课题, 区域生物多样性中心形成过程的物理生态耦合模拟(项目编号:XDB42040204), 资助额度:109.75万元. 起止时间:2020/01-2024/12;

5. 国家自然科学基金面上项目, 南海微型生物碳泵时空演变的高分辨率数值模拟(项目编号:41876123), 资助额度:62万元. 起止时间:2019/01-2022/12;

6. 基金委海洋碳汇与生物地球化学基础科学中心开放课题, 上升流系统储碳机 制数值模拟研究:以末次盛冰期热带东印度洋为例, 资助额度:100万元. 起止时间:2022/07-2025/06;

7. 东海实验室开放基金开放课题, 气候变化下人类活动引起东海近海生态系统响应的预测(项目编号:DH-2022KF0207), 资助额度:15万元. 起止时间:2022/10-2023/12;

8. 2015年上海市优秀博士论文;

9. 2021年首届全国教材建设奖二等奖(排名第4)。

代表性科研成果(论文专著、专利及软件)

专著

1.马文涛,李前裕,田军,新生代晚期冰盖与大洋碳储库变化的轨道周期及其数值模型分析,同济大学出版社,2017;

2. 汪品先, 田军, 黄恩清, 马文涛, 地球系统与演变, 科学出版社, 2018。


第一作者/通讯作者

1. Zhang, Z., Ma, W. Dynamical Response of the Arabian Sea Oxygen Minimum Zone to the Extreme Indian Ocean Dipole Events in 2016 and 2019. Geophysical Research Letters, 50(21) e2023GL104226. https://doi.org/10.1029/2023GL104226;

2.Zheng, Y., Ma, W.*, Wang, Y., Liu, Z., & Xiu, P. (2023). Modeling dissolved organic carbon exchange across major straits and shelf breaks in the South China Sea. Progress in Oceanography, 210, 102928. https://www.sciencedirect.com/science/article/pii/S0079661122001872;

3.Jin, X., Ma, W.*, & Liu, C. (2022). Origin of the long-term increase in coccolith size and its implication for carbon cycle and climate over the past 2 Myr. Quaternary Science Reviews, 290, 107642. https://www.sciencedirect.com/science/article/pii/S0277379122002736;

4.Xiu, P., Guo, L., & Ma, W.* (2022). Modelling the influence of submesoscale processes on phytoplankton dynamics in the northern South China Sea. Frontiers in Marine Science, 9. Original Research. https://www.frontiersin.org/articles/10.3389/fmars.2022.967678;

5.Ma, W, Wang, Y., Bai, Y., Ma, X., Yu, Y., Zhang, Z., Xi, J. 2022. Seasonal Variability in Chlorophyll and Air-Sea CO2 Flux in the Sri Lanka Dome: Hydrodynamic Implications, Remote Sensing 14, 14: 3239. https://doi.org/10.3390/rs14143239;

6.Ma, X.*#, Ma, W.#, Tian, J.*, Yu, J., Huang, E. 2022. Ice sheet and terrestrial input impacts on the100-kyr ocean carbon cycle during the Middle Miocene, Global and Planetary Change, https://doi.org/10.1016/j.gloplacha.2021.103723;

7.Ma, W.*, Xiu, P.*, Yu, Y., Zheng, Y., Chai, F. 2022. Production of dissolved organic carbon in the South China Sea: A modeling study. SCIENCE CHINA Earth Sciences 64, 10.1007/s11430-021-9817-2. (中国科学: 地球科学中/英文版);

8.Ma, W.*, Xiu, P., Chai, F., Ran, L., Wiesner M. G., Xi, J., Yan, Y., Fredj , E. 2021. Impact of mesoscale eddies on the source funnel of sediment trap measurements in the South China Sea. Progress in Oceanography 194: 102566, https://doi.org/10.1016/j.pocean.2021.102566;

9.Fan, G., Han, Z.*, Ma, W.*, Chen, S., Chai, F., Mazloff M., Pan J., Zhang, H. 2020. Southern Ocean carbon export efficiency in relation to temperature and primary productivity. Scientific Reports 10: 13494, 10.1038/s41598-020-70417-z;

10.Ma, W, Xiu, P.*; Chai, F*; Li, H., 2019. Seasonal variability of the carbon export in the central South China Sea. Ocean Dynamics, 2019, 69 (8): 955-966;

11.Ma, W.*, Wang, P., Tian, J., 2017. Modeling 400–500-kyr Pleistocene carbon isotope cyclicity through variations in the dissolved organic carbon pool. Global and Planetary Change, 152: 187-198. doi: 10.1016/j.gloplacha.2017.04.001;

12.Ma, W. *, Chai, F., Xiu, P., Xue, H., Tian, J. Simulation of export production and biological pump structure in the South China Sea. Geo-Mar Lett. 34, 541-554. doi: 10.1007/s00367-014-0384-0;

13.Ma, W. *, Tian, J., 2014. Modeling the contribution of dissolved organic carbon to carbon sequestration during the last glacial maximum. Geo-Mar. Lett. 34, 471-482. doi: 10.1007/s00367-014-0378-y;

14.Ma, W. *, Chai, F., Xiu, P., Xue, H., Tian, J., 2013. Modeling the long term variability of phytoplankton functional groups and primary productivity in the South China Sea. J. Oceanogr, 69, 527-544;

15.Ma, W. *, Tian, J., Li, Q., Wang, P., 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;

16.Ma, W. *, Tian, J., Li, Q., 2010. Astronomically modulated late Pliocene equatorial Pacific climate transition and Northern Hemisphere ice sheet expansion. Chinese Science Bulletin,55(2):212-220. (科学通报英文版);

17.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. (科学通报中文版)。