Abstract: The new materials of Pseudictopidae from Early to Middle Paleocene Wanghudun Formaüon of Qianshan Basin, Anhui are described in the present paper. They represent two genera and three species: Anictops tabiepedis Qiu, 1977, Anictops wanghudunensis sp. nov. and Paranictops aff. P. majuscula Qiu, 1977. The new species differs from type species of the genus mainly in having relatively robust mandible and fransversely wide cheek teeth, more reduced paraconid which is very near to the metaconid on lower cheek teeth, no notch in the middle of metalophid on p4 and no hypoconulid on the first two lower molars, m3 with short hypoconulid and round talonid, and relaüvely wide upper cheek teeth without distinct anterior cingulum. The difference between Paranictops aff. P. majuscula and Paranictops majuscula is mainly in the width of trigonids and talonids of the first two lower molars. In the former the talonids are wider than trigonids while in the latter species it is just the opposite. The new finds further demonstrate that pseudictopids were flourishing in the Early to Middle Paleocene of Qianshan Basin.