Abstract

Abstract. Carbon use efficiency (CUE), the ratio of net primary production (NPP) over gross primary production (GPP), is a functional parameter that could possibly link the current increasingly accurate global GPP estimates with those of net ecosystem exchange, for which global predictors are still unavailable. Nevertheless, CUE estimates are actually available for only a few ecosystem types, while information regarding agro-ecosystems is scarce, in spite of the simplified spatial structure of these ecosystems that facilitates studies on allocation patterns and temporal growth dynamics. We combined three largely deployed methods, eddy covariance, soil respiration and biometric measurements, to assess monthly values of CUE, NPP and allocation patterns in different plant organs in an apple orchard during a complete year (2010). We applied a measurement protocol optimized for quantifying monthly values of carbon fluxes in this ecosystem type, which allows for a cross check between estimates obtained from different methods. We also attributed NPP components to standing biomass increments, detritus cycle feeding and lateral exports. We found that in the apple orchard, both net ecosystem production and gross primary production on a yearly basis, 380 ± 30 g C m−2 and 1263 ± 189 g C m−2 respectively, were of a magnitude comparable to those of natural forests growing in similar climate conditions. The largest differences with respect to forests are in the allocation pattern and in the fate of produced biomass. The carbon sequestered from the atmosphere was largely allocated to production of fruit: 49% of annual NPP was taken away from the ecosystem through apple production. Organic material (leaves, fine root litter, pruned wood and early fruit falls) contributing to the detritus cycle was 46% of the NPP. Only 5% was attributable to standing biomass increment, while this NPP component is generally the largest in forests. The CUE, with an annual average of 0.71 ± 0.12, was higher than the previously suggested constant values of 0.47–0.50. Low nitrogen investment in fruit, the limited root apparatus, and the optimal growth temperature and nutritional condition observed at the site are suggested to be explanatory variables for the high CUE observed.

Highlights

  • Solid EarthGlobal greenhouse gases (GHGs) concentration in atmosphere has been growing since preindustrial times due to aanntdhrlaonpdoguesneicchfaonrcgienTg(C,hainneapdCaerltlricyeutolaaslr.,pf2oh0ss0ei7lr;feLueelQcuoemrebuesttiaol.n, 2009), with carbon dioxide (CO2) being the prevalent anthropogenic GHG (IPCC-AR4, 2007; Peters et al, 2011)

  • Given the relevance of Carbon use efficiency (CUE) estimates and the paucity of existing reliable values for different ecosystem types and climates, we addressed as a main question in this study if current methodologies used to quantify C stocks and fluxes can be combined to robustly quantify the CUE in a woody agroecosystem chosen as an exemplary model

  • Budburst occurred on the 18 of March and Net ecosystem exchange (NEE) started to become negative during the first ten days of April and returned positive in the first decade of November, when leaf abscission was almost complete and only the vegetation on grassed alleys carried out photosynthesis

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Summary

Introduction

Solid EarthGlobal greenhouse gases (GHGs) concentration in atmosphere has been growing since preindustrial times due to aanntdhrlaonpdoguesneicchfaonrcgienTg(C,hainneapdCaerltlricyeutolaaslr.,pf2oh0ss0ei7lr;feLueelQcuoemrebuesttiaol.n, 2009), with carbon dioxide (CO2) being the prevalent anthropogenic GHG (IPCC-AR4, 2007; Peters et al, 2011). By sequestering a large amount of atmospheric carbon (C), terrestrial ecosystems are thought to offer a mitigation strategy for reducing global warming (Schimel et al, 2001). D. Zanotelli et al.: Carbon fluxes in an apple orchard anthropogenic emissions and, on a global scale, it has been estimated that the terrestrial biosphere is able to take up about 30 % of anthropogenic CO2 emissions annually (Schulze, 2006; Canadell et al, 2007). Several studies have been carried out to assess the capacity of ecosystems in different natural biomes to sequester C from the atmosphere, most of which related to FLUXNET synthesis activity (Baldocchi, 2008; http://www.fluxnet.ornl.gov/) and results have been recently reviewed in a global dataset (Luyssaert et al, 2007; Schulze et al, 2010)

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