“…1(a) (blue line). Here the manganite layer is not a ferromagnetic half-metal but an insulator with a CE-type antiferromagnetic order and a combined charge and orbital ordered (CO/OO) state with wave vectors Q OO = (1/4, 1/4, 0) and Q CO = (1/2, 0, 0) or (0, 1/2, 0) (expressed in reciprocal lattice units in pseudocubic notation) that develops below 220-240 K [6,7,36]. While there is evidence that the oxygen ions also play an important role in this CO/OO [37,38], for simplicity in the following we refer to it as Mn-CO/OO.…”