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. 2022 Feb 2;158(1):39–72. doi: 10.1007/s10533-021-00884-7

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Fig. 2 — Comparison of soil P stock speciation at temperate beech forest sites with carbonate a-c and silicate d-f parent material. Absolute and relative contribution of a,d different soil compartments, b,e organic and inorganic fine earth P, and c,f Ca-bound, Al-bound, and Fe-bound mineral soil fine earth P. Sites with dolostone parent material: Mangfallgebirge (MAN; N1, N2: North slope, S1, S2: South slope). Sites with limestone parent material: Tuttlingen (TUT; SW: Southwest slope; NE: Northeast slope), Schänis (SCH), Bärenthal (BAE). Sites with silicate parent material (Data from Prietzel et al. (2016a, b, c) and Lang et al. (2017)): Bad Brückenau (BBR), Mitterfels (MIT), Vessertal (VES), Conventwald (CON), Lüss (LUE)