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Bahn, M., Reichstein, M., Davidson, E. A., Grumzwig, J., Jung, N., Carbone, M. S., Epron, D., Misson, L., Nouvellon, Y., Roupsard, O., Savage, K., Trumbore, S. E., Gimenci, C., Curiel Yuste, J., Tang, J., Vargas, R., & Janssens, I. A. (2010). Soil Respiration at Mean Annual Temperature Predicts Annual Total over Vegetation Types and Biomes. Biogeosciences, 7, 2147-2157.
http://dx.doi.org/10.5194/bg-7-2147-2010

has been cited by the following article:

• TITLE: Cycling of Carbon and Other Elements in a Beech Forest Hestehave, Jutland, Denmark, in the Past 50 Years

  AUTHORS: Folke O. Andersson

  KEYWORDS: Plant Biomass, Primary Production, Litterfall, Deposition, Cycling of C, N, P, S and Carbon Sink

  JOURNAL NAME: Open Journal of Forestry, Vol.5 No.3, March 19, 2015

  ABSTRACT: Plant biomass, primary production and mineral cycling in the beech forest (Fagus sylvatica L.), Hestehave in Jutland, Denmark were studied over a 50-year period. The role of the forest as a carbon sink was also assessed. Aboveground tree biomass was 226 t·ha-1 in 1970 and after a 50-year 539 t·ha-1 in 2014, an unexpected increase with 313 t·ha-1. Annual production at those two points in time was 13.4 and 20.5 t·ha-1, respectively. It was apparent that the tree biomass was still acting as a sink for carbon, which was the dominant element in the aboveground parts. The concentration of other elements (N > K > Mg > P > S > Na > Mn > Zn > Fe > Cu) ranged from 495 to 0.4 kg·ha-1. Annual litterfall restored 3.2 t·ha-1 to the soil as organic matter or 1.6 t·ha-1 as carbon. Over the year 53% of the litterfall was decomposed. A pH decrease of 0.95 units in the soil was observed between 1968 and 1993. This was attributed to fallout from a neighbouring thermal heating station affecting sulfur deposition and increasing soil acidification. After 1993, when filters were fitted in the heating station, the pH decrease in the soil was smaller, only 0.09 pH-units up to 2011. The increased tree growth is an additional, likely explanation for the observed soil acidification. Deposition of the growth-limiting element nitrogen increased during later years and is now, most likely around 20 kg·ha-1 per annum, which may partly contribute to the increased production.