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Thai) 1:
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Parental soils and cast materials are the same as in Clause et al.(2014). Soils were collected from the top layer (0–20 cm) of threedifferentpermanentgrasslands in Upper-Normandy, France.Climateis temperate oceanic with a mean annual rainfall of 800mm and amean temperature of 10 C. The soil from Saint-Adrien (N492202200 ,E10704100) is a rendzic Leptosol (IUSS, 2006; hereafterRe) supportingvegetation dominated by Brachypodium pinnatum (L.) P. Beauv.,Festuca lemanii Bastard and Carexflacca Schreb. The soil from Yvetot(N493603700, E 04401500) is a NeoLuvisol-Luvisol (IUSS, 2006;hereafter Lu) supporting a vegetation dominated by Agrostiscapillaris (L.), L. perenne (L.) and Ranunculus acris (L.). The soil fromYville-sur-Seine (N492501100, E05205400) is a Histosol (IUSS, 2006;hereafter Hi), where the vegetation is dominated by Poa trivialis (L.),L. perenne and A. capillaris. All soils were hand-sieved within twodays after collection with a 5-mm-mesh sieve and air-dried for aweek. Microcosms were cylindrical pots (13.511 cm)filled with750 g of one type of soil watered with 115 mL water (see Clause et al.,2014 for further details).
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