Decomposing cones of Norway spruce (Picea abies (L.) H. Karst.): dry weight loss, chemical changes, and vertical transport in a Norwegian raw humus soil profile

Abstract

Naturally shed cones of Norway spruce (Picea abies) were placed on the forest floor, partly on moss-covered ground, and partly on vegetation-free needle mats. Numbered sticks allowed individual recovery after 1, 3, 5, 7, 9, 11, and 13 years. During the first nine years, cones decomposed fastest in the moss site. After 13 years, dry weight loss was about 60% in both habitats, but cones still retained their shape. In the moss site, cones were then situated in the middle of the organic layer, with their underside about 3 cm above the bleached layer. Cones in the needle mat profile had sunk less. One cone with rather intact shape was found below a nylon strip laid out 28 years earlier. Compared to needle litter from Norway spruce and Scots pine, spruce cones had low concentrations of Ca, Mn, and Fe. The concentration of these elements, as well as N, Al, and S, was greatly increased during decomposition. Ca, Mn, Fe, and Al were immobilized for a long time, as their total amount per cone increased with time. Cones decomposed slower than needles, so their role in humus composition and carbon storage may be greater than indicated by their fraction of fresh litter.