Nutrients return from leaves and litterfall in a mediterranean cork oak (Quercus suber L.) forest in southwestern Spain

The knowledge of the cycle of nutrients is fundamental for the correct comprehension of the tree–soil relationship and for an adequate forest management. In order to analyse the nutrients return from leaves and litterfall in a Mediterranean cork oak forest in southwestern Spain, 12 trees were randomly selected and litterfall collected for 2 years. Samples were taken monthly and separated in different fractions (leaves, twigs, catkins, acorns and mis- cellaneous), then leaves nutrients were analyzed. Simulta- neously, we analyzed the nutrient content of living leaves from the same trees in each season during 1 year. The ana- lyzed nutrients were C, N, P, K, Ca, Mg, Fe, Mn, S, Cu, Zn and Mo. Annual patterns of each nutrient in fallen leaves were characterized and compared with seasonal values of these nutrients in living leaves. Leaves fall has two annual maximum, first and most important in spring around April coinciding with renewal of foliar cover and second around October. Main concentration patterns of N, P and K are related with phenological patterns, in consequence mini- mumconcentration in leaves fall were obtained in periods of growing and maximum litterfall. Concentrations of Ca, Fe and Mn increase with the age of the leaves and maximum concentrations were obtained before periods of maximum litterfall while concentrations of Cu, Mo and Mg stay stable. Communicated by A. Merino. A. Gonza This article belongs to the special issue ‘‘Plant–soil relationships in Southern European forests’’. E. Andivia (&)  M. Ferna ´lez-Pe Department of Forest Sciences, University of Huelva, Ctra. Palos–La Ra ´rez  R. Tapias Huelva, Spain e-mail: enrique.andivia@dcaf.uhu.es ´ndez  J. Va ´zquez-Pique ´  ´bida, s/n. 21819 Palos de la Frontera, Seasonal analysis of nutrients in living leaves collected from the same trees in four different periods of the year allowed to corroborate the patterns of leaves fall and the probable osmotic function of K.