Zhang S., Li, T.*, Yu, Z, Chang, F., Gu, S., Xiong, Z.,Liu,H., Qian, F., Zhang, J., Cheng, X., Li, Baohua*, 2023. Abrupt warming of the equatorial intermediate Pacific during Heinrich Stadial 1. Palaeogeography, Palaeoclimatology, Palaeoecology, doi.org/10.1016/j.palaeo.2023.111600.
Xu, Y., Li, Baohua*, 2023. δ18O and δ13C of planktonic foraminifer Globigerinoides ruber: Effects of test size sampling and laboratory treatment. Palaeoworld, doi.org/10.1016/j.palwor.2023.01.012.
王雨楠，周保春*，李保华*，王亚琼，2023. 江苏盐城大丰滨海岩芯中的全新世介形类及古环境变迁。微体古生物学报，40(1): 43-52。
郭启梅*，刘静，李保华*，2023. 沉积物单/多壳体底栖有孔虫稳定氧碳同位素组成、比较及其指示意义。微体古生物学报，40(1): 53-65。
Guo, Qimei, Li, Baohua*, 2022. Intermediate water variability of the subtropical Northeastern Atlantic during 490–424 ka (late MIS 13 and MIS 12). Marine Geology, 444: 106730.
李保华，张楷，徐烨，范代读，2022. 大丰野鹿荡中全新世以来有孔虫群落及古环境变化。微体古生物学报，39(4): 339-347。
郭启梅，徐烨，刘静*，李保华*，2022. 有孔虫稳定氧碳同位素实验处理、测试与应用。微体古生物学报，39(3): 276-283。
Guo, Qimei, Kim, J.-K., Singh, A.D., Yu, J., Li, Baohua*, 2021. Benthic foraminiferal response to orbital-scale variability in primary productivity off the Portuguese margin over the last 1.3 Myr. Palaeogeography, Palaeoclimatology, Palaeoecology, 557: 110532.
Xu, Ye, Chang, F.-M.*, Li, T.-G., Li, Bao-Hua*, 2021. High-resolution sea surface temperature and salinity dynamics in the northern Okinawa Trough over the last 24 kyr. Palaeoworld, 30: 770-785.
王晓燕，李保华*，黄宝琦，2021. 晚更新世南海不同海区的浮游有孔虫群落特征差异及环境控制因素。微体古生物学报，38(1): 63-71。
Guo, Qimei*, Li, Baohua*, Kim, J.-K., Voelker, A., 2020. Mediterranean Outflow Water dynamics across the middle Pleistocene transition based on a 1.3 million-year benthic foraminiferal record off the Portuguese margin. Quaternary Science Reviews, 247: 106567.
Jin, Xiaobo, Xu, J., Li, Y., Qiao, P., Wu, L., Ling, C., Li, Baohua*, Liu, C.*, 2020. Origin of the rhythmic reddish-brown and greenish-gray sediments in the abyssal South China Sea：Implications for oceanic circulation in the late Miocene. Marine Geology, 430: 106378.
俞宙菲，李保华*，李宏亮，张静静，陈建芳，2020. 现代浮游有孔虫对南海西南部上升流的响应。第四纪研究，40(3): 801-810。
张楷，李保华*，王晓燕，俞宙菲，郭启梅，徐烨，2020. 沉积物中底栖有孔虫的染色方法比较研究。微体古生物学报，37(3): 294-302。
王晓燕，李保华*，郭启梅，钟石兰，2018. 宁波北仑中晚全新世有孔虫群落变化及古环境意义。古生物学报，57(1): 119-124。
Guo, Q, LI, Baohua*, Kim, J.K, IODP Expedition 339 Scientists, 2017. Benthic foraminifera and Mediterranean outflow water evolution at the western Iberian margin since the Middle Pleistocene. Global and Planetary Change, 150: 94-108.
Ke, X., LI, Baohua*, Zhang, Z., Wei, Y.Hu, F., Fan, D., Sun, L., Yao, H., 2017. Post-glacial foraminifera of the paleo-incised Yangtze Valley and its paleoenvironmental implications. Journal of Paleontology, 91(6): 1102-1122.
郭启梅，李保华*，王晓燕，钟石兰，2017. 江门西江全新世有孔虫群落及其古环境意义。微体古生物学报，2017，34(1): 61-66。
王晓燕，郭启梅，李保华*，2014. 长江三角洲DY03孔有孔虫群落演化及其古环境意义。古生物学报，53(1)：85-91。
郭启梅，李保华*，王伟铭，蓝琇，丁金龙，2014. 昆山白莲湖牡蛎层年代及古环境初探。微体古生物学报， 31(2)：147-153。
王晓燕，李保华*，2012. 南海西部MIS12期以来表层海水古温度演化——来自浮游有孔虫群落及其壳体Mg/Ca比值的证据。中国科学, 42(12): 1901-1911。
Wang, X., Li, Baohua*，2012. Surface water temperature of the western South China Sea since the MIS 12: evidence from the planktonic foraminifera and its shell Mg/Ca ratio. Science China (D), 55(11): 1827–1836.
李保华，王晓燕，孔晓敏，林春明，李艳丽，张霞，2012. 浙江钱塘江南岸冰后期有孔虫化石记录及其古环境意义。微体古生物学报，29(2): 121-129。
李保华，孔晓敏，王晓燕，龙江平，2010. 北部湾中部海域底质沉积物中的有孔虫。微体古生物学报，27(2): 99-108。
Li, Baohua, Wang, X., Jian, Z., Wang, P., 2009. Sea surface environment inferred from planktonic foraminifera in the southern South China Sea since the last glacial period. Palaeoworld, 18(1): 23-33.
李保华，王晓燕，2009. 末次冰期以来中国海区浮游有孔虫Pulleniatina obliquiloculata含量变化的地层学意义。微体古生物学报，26(4): 313-322。
李保华，王晓燕，龙江平，2008. 海南岛近岸沉积物中的有孔虫特征与分布。微体古生物学报，25(3): 225-234。
Li, Baohua, Li, T., Ertan, T., Hemleben, C., Hao, J., Li, C., Cao, Q., Yang, Q., 2007. Living planktonic foraminifera from the northwest Pacific Ocean: SSU rDNA sequences and their paleoceanographic significance. Progress in Natural Science, 17(7): 798-802.
李保华，李铁刚，T. Ertan，C. Hemleben，李春香，曹奇原，杨群，2007. 西北太平洋现生浮游有孔虫的SSU rDNA序列研究。自然科学进展, 17(3): 391-395。
LI, Baohua, Jian, Z., Li, Q. Tian, J. and Wang, P., 2005. Paleoceanography of the South China Sea since the middle Miocene: Evidence from planktonic foraminifera. Marine Micropaleontology, 54: 49-62.
李保华，K. T. Ertan，C. Hemleben，2005. 有孔虫分子生物学研究进展。自然科学进展, 15(5)：535-539。
Li Baohua, Ertan, K. T., Hemleben, C., 2005. Molecular biological research in Foraminifera. Progress in Natural Science, 15(8)：673-677.
LI, Baohua, Wang, J., Huang, B., Jian, Z. and Wang, P., 2004. Surface water evolution of the South China Sea over the last 12 Ma: A south-north comparison from ODP sites 1143 and 1146. Paleoceanography，19: 1009, doi: 10.1029/2003PA000906.
李保华，翦知湣，黄宝琦，M. Sarnthein，汪品先，2004. 南海南部表层海水古温度估算与次表层海水特征变化。微体古生物学报，19(1): 37-43。
李保华，翦知湣，2001. 南沙深海区近千万年来浮游有孔虫群及海水温跃层演变。中国科学，31(10)：840-845。
Li, Baohua and Jian, Z., 2001: Evolution of planktonic foraminifera and thermocline in the southern South China Sea since 12 Ma (ODP-184, Site 1143). Science in China (D), 44(10): 889-896.
李保华，赵泉鸿，陈民本，翦知湣，汪品先，2001. 南海中更新世以来的碳酸盐溶解作用与深水古海洋学特征。科学通报, 46(13)：1128-1132。
Li, Baohua, Zhao, Q. Chen, M.-P., Jian, Z., Wang, P., 2001. Carbonate Dissolution and Deep-water Paleoceanography of the South China Sea since the Middle Pleistocene. Chinese Science Bulletin, 46(22): 1908-1912.
李保华，赵泉鸿，陈民本，翦知湣，汪品先，2001. 南沙海区晚第四纪浮游有孔虫演化及其古海洋学意义。微体古生物学报，18（1）：1-9。
LI, Baohua, Yoon, H.-I. and Park, B.-K, 2000. Foraminiferal assemblage and CaCO3 dissolution since the last deglaciation in the Maxwell Bay, King George Island, Antarctica. Marine Geology, 169 (1/2): 239-257.
李保华, Park, B.-K., Kim, D. and Woo, H., 2000. 韩国济洲岛下西归浦组的地层时代及其古环境研究。地层学杂志，24（1）：49-52。
LI, Baohua, Park, B.-K., Kim, D. and Woo, H., 1999. The Geological Age and Paleoenvironment of the Lower Seogwipo Formation, Cheju Island. Geoscience Journal，3(4):181-190
LI, Baohua, Park, B.-K. and Kim, D., 1999. Paleoceanographic Records from the Northern Shelf of the East China Sea since the Last Glacial Maximum. Journal of the Korea Society of Oceanography, 34(3): 151-166
LI, Baohua, Zhao, Q., Wang, Y., Jian, Z., Chen, R., 1998. Paleoceanographic events of the southern Okinawa trough during the last 20,000 years. Acta Oceanologica Sinica, 17(4): 519-530.
LI, Baohua, Jian, Z. and Wang, P., 1997. Pulleniatina obliquiloculata as a paleoceanographic indicator in the southern Okinawa Trough during the last 20,000 years. Marine Micropaleontology, 32(1/2): 59-69.
李保华，赵泉鸿，王永吉，翦知湣，陈荣华，1997. 冲绳海槽南部两万年来的浮游有孔虫与古海洋学事件。海洋学报，19(4)：91-99。