The Paleomagnetic Secular Variation (PSV) and Relative Paleomagnetic Intensity (RPI) are the behavior of dipole and non-dipole field of the Earth's interior. The PSV and RPI stacks can be applied for chronological study and regional stratigraphical comparation as the similar feature of dipole field of the earth. However, few of high- resolution Holocene PSV and RPI records from central of China were reported, which hinders the understanding of the geomagnetic field variation and relationship between lacustrine sediments and climate change during the Holocene. In this study, a high-resolution paleomagnetic investigation was undertake in core GH14B from Gonghai Lake (38°54'30.50"N, 112°14′05.80"E; 1858m a.s.l. and water depth 9.3m),Shanxi Province, central of China, for the purpose of acquiring direction and intensity of the geomagnetic field. This study is an effective method to solve dating problem of Holocene lacustrine sediments in central of China, which can also provide basic data for regional paleomagnetic field variation. The previous studies show that the dominant magnetic carrier is magnetite in the pseudo-single-domain (PSD) grain size range and with a relatively small change in concentration, thus is suitable for recording PSV and RPI. We obtained a sediment core (GH14B) from the central part of Gonghai Lake using a UWITEC Piston Corer and focus here on the upper 7.24m which belongs to the Holocene (11.5ka B.P.). Gonghai Lake lacustrine sediments contains stable, continuous and homogeneous finegrained silty clay. The detailed description of the lacustrine sediments as follows: 0 ~ 2.4m, brownish grey silty clay; 2.4~4.5m,light brownish grey mud; 4.5~7.lm,dark brownish organic mud; 7.10~7.24m,brownishyellow silt. There are 18 reliable accelerator mass spectrometry (AMS)~(14)C data which are based on terrestrial plant macrofossils used for absolute age control. Total 159 samples were selected using the plastic box in 8cm~3 every 4cm interval which were used for the measurements of magnetic susceptibility (chi) and alternating demagnetization,and total 77 samples were used for the measurements of anhysteretic remanent magnetization(ARM) and saturation isothermal remanent magnetization (SIRM) every 8cm interval. The relative paleomagnetic intensity proxy (RPI) was established by normalizing the natural remanent magnetization (NRM_(25mT)) with the magnetic susceptibility (chi) after power spectrum tests of RPI and normalization parameters (chi,ARM and SIRM). Here we present the vector paleomagnetic field reconstruction since Holocene. The new record is comparedwith other lacustrine and marine records in the Northern Hemisphere,revealing the generally consistent variabilities to certain extent, however, the obvious spatial differences still exist among the different regions. In addition, our results suggest that it does not exist geomagnetic excursion at least during the Holocene in central of China. Therefore,the PSV and RPI curves from Gonghai Lake are potential tools for stratigraphic correlation and further chronological framework of lake sediment sequence in central of China. The discrepancy in amplitude and pattern among the different regional records may be ascribed to the existence of non-dipole field which comes from magnetic flux lobes at the core-mantle boundary.