13C-isotopic fingerprint of Pinus pinaster Ait. and Pinus sylvestris L. wood related to the quality of standing tree mass in forests from NW Spain.
Pine forest plantations of Pinus pinaster Ait. and P. sylvestris L. located in Galicia, NW Spain, were selected to study the 13C/12C-isotopic fingerprint in wood core samples in order to find possible relationships between the delta(13)C at natural abundance levels and the quality of the standing tree mass. For each pine species, 24 forests growing on acidic soils were studied: half developed over granite and half over schists. Two dominant trees from each plot, corresponding to all possible combinations of forest stands with high or low site index and with adults or young trees, were drilled at the basal part of trunks using a Pressler drill to obtain tree ring samples. The C-isotopic compositions of the litter and the soil organic matter from different soil depths were also determined and statistically significant correlations between these values and the 13C content of the wood were observed. Despite internal variations due to the influence of site index, tree age and parent material, the isotopic fingerprint of P. pinaster wood (mean value delta13C=-26.2+/-0.8 per thousand) significantly differed (P<0.001) from that of P. sylvestris (mean value delta13C=-24.6+/-0.7 per thousand). Relationships between the quality of the stand and the C-isotopic composition of the wood were observed, high quality stands having trees more 13C-depleted than low quality ones. A high correlation between wood delta13C and site index values for P. pinaster stands (r=-0.667, P<0.001) was found, this correlation being even clearer when only P. pinaster growing over schists (r=-0.833, P<0.001) are considered. Again, the correlation between the site index and the wood delta13C of young P. pinaster trees is higher when plots over granite or schists are separately considered. A similar fact occurs for adult P. sylvestris trees from schists stands, high quality specimens being 13C-depleted compared with low quality ones. On the other hand, 13C natural abundance of wood from P. sylvestris trees seems to be also strongly influenced by the underlying parent material, young trees from granite stands having a statistically higher 13C-isotopic composition (P<0.05) than young trees from schists stands.
Fernandez
Irene
I
Departamento de Bioquímica del Suelo, Instituto de Investigaciones Agrobiologicas de Galicia, CSIC, Apartado 122, E-15780 Santiago de Compostela, Spain. ifernandez@iiag.cesga.es
González-Prieto
Serafin J
SJ
Cabaneiro
Ana
A
D018533:Biomass; D001835:Body Weight; D002152:Calorimetry, Differential Scanning; D002247:Carbon Isotopes; D017753:Ecosystem; D013058:Mass Spectrometry; D028223:Pinus / Q000737:chemistry* / Q000254:growth & development; D041605:Pinus sylvestris / Q000737:chemistry* / Q000254:growth & development; D012987:Soil / Q000032:analysis; D013030:Spain; D013818:Thermogravimetry; D014197:Trees / Q000737:chemistry / Q000502:physiology*; D014934:Wood
D002247:Carbon Isotopes; D012987:Soil