In the past two decades, the organometallic chemistry of the alkaline earth elements has experienced a renaissance due in part to developments in ligand stabilization strategies. In order to expand the scope of redox chemistry known for magnesium and beryllium, we have synthesized a set of reduced magnesium and beryllium complexes and compared their resulting structural and electronic properties. The carbene-coordinated alkaline earth−halides, ( Et2 CAAC)-MgBr 2 (1), (SIPr)MgBr 2 (2), ( Et2 CAAC)BeCl 2 (3), and (SIPr)BeCl 2 (4) [ Et2 CAAC = diethyl cyclic(alkyl)(amino) carbene; SIPr = 1,3-bis(2,6-diisopropylphenyl)-4,5-dihydroimidazole-2-ylidene] were combined with an α-diimine [2,2bipyridine (bpy) or bis(2,6-diisopropylphenyl)-1,4-diazabutadiene ( Dipp DAB)] and the appropriate stoichiometric amount of potassium graphite to form singly-and doubly-reduced compounds ( Et2 CAAC)MgBr( Dipp DAB) (5), ( Et2 CAAC)MgBr(bpy) ( 6), ( Et2 CAAC)Mg( Dipp DAB) ( 7), ( Et2 CAAC)Be(bpy) (8), and (SIPr)Be(bpy) (9). The doubly-reduced compounds 7−9 exhibit substantial π-bonding interactions across the diimine core, metal center, and π-acidic carbene. Each complex was fully characterized by UV−vis, FT-IR, X-ray crystallography, 1 H, 13 C, and 9 Be NMR, or EPR where applicable. We use these compounds to highlight the differences in the organometallic chemistry of the lightest alkaline earth metals, magnesium and beryllium, in an otherwise identical chemical environment.