The LaMn 1−x Te x O 3+δ (x=0.1, 0.2, 0.3) were synthesized using solid-state reaction method for the first time. X-ray photoemission spectrum (XPS) shows that in the samples the Te ions have a valence of Te 4+ , and Mn 3+ ions are partly converted into Mn 2+ and Mn 4+ due to the excess oxygen and Te doping. The magnetotransport associated with Mn 2+ , Mn 3+ and Mn 4+ was investigated. The experimental results show that the samples are insulator at 0 T when the amount of Mn 3+ is much larger or less than the sum of Mn 2+ and Mn 4+ ; by contrast, the samples display metal to insulator transition with increasing temperature when the amount of Mn 3+ is close to the sum of Mn 2+ and Mn 4+ . These anomalous magnetotransport behaviors were analyzed in the frame of the double-exchange (DE) mechanism.colossal magnetoresistance, La-Te-Mn-O, magnetotransport Doped LaMnO 3 have been widely studied due to a rich variety of physical properties [1][2][3][4] . The prominent one is the colossal magnetoresistance (CMR) effect, a phenomenon of the resistive transition induced by the magnetic transition, and CMR is traditionally explained by the double exchange (DE) [5] interaction. The key role in DE mechanism is played by Mn ions, the unique magnetic ions in LaMnO 3 , which affect not only the transport behaviors of manganites by the network of Mn-OMn, but also the magnetism of materials by the spin variation of Mn ions.As demonstrated by numerous studies, the valence of Mn ions in the manganites varies with the dopant, which is considered the intrinsic factor to understanding CMR effect. Mn ions are usually all trivalent (Mn 3+ ) in LaMnO 3 .When La ions were substituted partially by divalent ions, such as Ca 2+ , Sr 2+ etc., some Mn 3+ would convert into Mn 4+ , and Mn 3+ -Mn 4+ mixed valences are formed in the stable manganites of La 1−x A x MnO 3 [5][6][7][8] .When La ions were substituted partially by tetravalent ions, such as Ce 4+ , Te 4+ ... etc., some Mn 3+ would convert into Mn 2+ , which leads to the Mn 2+ -Mn 3+ mixed valence in La 1−x A x MnO 3 (A=Ce 4+ , Te 4+ ...) [8,9] . The interactions between Mn 4+ (or Mn 2+ ) ions and the neighboring Mn 3+ ions via O 2− are believed to contribute to the DE effect.The influence of the La-site substitution in manganites on DE mechanism is indirect, depending on the conversion of Mn 3+ ions. The direct influence, undoubtedly, is the Mn-site substitution. Recently, most studies on the Mn-site substitution focus on the La 1−x A x MnO 3 or LaMnO 3 . It is found that the manganites with the formula of La 1−x A x Mn 1−y O 3 (A=Ca 2+ , Sr 2+ ...; M=Zr 2+ , Cr 3+ , Ta 4+ ,...) or LaMn 1−x B x O 3 (B=T 4+ , Mo 6+ ...) still remain Mn 3+ -Mn 4+ (or Mn 3+ -Mn 2+ ) mixed-valence, and undergo ferro-to para-magnetism (FM-PM) transition. However, both have the different magnetotransport behavior.