“…The JPE has very recently been observed in the organic conductor λ − (BET S) 2 F eCl 4 , for magnetic fields ranging from 18 to 41 T. 5,6 Before that, it had already been seen in pseudoternary chalcogenides of the form Sn x Eu y M o z S 8 , from 4 − 23 T, [7][8][9][10] and there is strong experimental evidence that the JPE is also at work in chalcogenides of the form P b x Eu y M o z S 8 (at up to 70 T), 10,11 in transition-metal systems (M o 1−x M n x Ga 4 at up to 7.6 T), 12,13 in heavy-fermion superconductors (CeP b 3 at up to 15 T 14 and CeCu 2 Si 2 at about 2 T 15,16 ), and perhaps even in high-T c cuprates (Gd 1−x P r x Ba 2 Cu 3 O 7−δ , near 9 T). 17 It is crucially important to recognize that in the standard JPE scenario 2,4 it is only the action of the external magnetic field on the electron spins that is compensated by the internal (exchange) field, not that on the currents.…”