Foliar δ13C within a temperate deciduous forest: spatial, temporal, and species sources of variation

Abstract

Foliar C-abundance (δC) was analyzed in the dominant trees of a temperate deciduous forest in east Tennessee (Walker Branch Watershed) to investigate the variation in foliar δC as a function of time (within-year and between years), space (canopy height, watershed topography and habitat) and species (deciduous and coniferous taxa). Various hypotheses were tested by analyzing (i) samples collected from the field during the growing season and (ii) foliar tissues maintained in an archived collection. The δC-value for leaves from the tops of trees was 2 to 3%. more positive than for leaves sampled at lower heights in the canopy. Quercus prinus leaves sampled just prior to autumn leaf fall had significantly more negative δC-values than those sampled during midsummer. On the more xeric ridges, needles of Pinus spp. had more positive δC-values than leaves from deciduous species. Foliar δC-values differed significantly as a function of topography. Deciduous leaves from xeric sites (ridges and slopes) had more positive δC-values than those from mesic (riparian and cove) environments. On the more xeric sites, foliar δC was significantly more positive in 1988 (a dry year) relative to that in 1989 (a year with above-normal precipitation). In contrast, leaf δC in trees from mesic valley bottoms did not differ significantly among years with disparate precipitation. Patterns in foliar δC indicated a higher ratio of net CO assimilation to transpiration (A/E) for trees in more xeric versus mesic habitats, and for trees in xeric habitats during years of drought versus years of normal precipitation. However, A/E (units of mmol CO fixed/mol HO transpired) calculated on the basis of δC-values for leaves from the more xeric sites was higher in a wet year (6.6±1.2) versus a dry year (3.4±0.4). This difference was attributed to higher transpiration (and therefore lower A/E) in the year with lower relative humidity and higher average daily temperature. The calculated A/E values for the forest in 1988-89, based on δC, were within ±55% of estimates made over a 17 day period at this site in 1984 using micrometeorological methods.

Climate reconstruction from pollen and δ<sup>13</sup>C records using inverse vegetation modeling – Implication for past and future climates

“…Isotopic niche shifts toward more negative values under higher CO 2 concentration. This is in agreement with the results of Feng and Epstein (1995) that show δ 13 C depletion of about 2‰ for 100 ppm increase of CO 2 and in agreement with other studies that show similar results (Garten and Taylor, 1992;Pasquier-Cardin et al, 1999;Van De Water et al, 2002). The implications for vegetation under future climate conditions are also illustrated.…”

Carbon flux to woody tissues in a beech/spruce forest during summer and in response to chronic O<sub>3</sub> exposure

“…Overall, the t-test for paired comparisons indicated no significant differences in δ 13 C shift between O 3 regimes within CO 2 and solid samples of labeled beech and spruce. (Matyssek, 1986;Garten and Taylor, 1992;Diefendorf et al, 2010).…”

Regional Equivalent Water Thickness Modeling from Remote Sensing across a Tree Cover/LAI Gradient in Mediterranean Forests of Northern Tunisia

“…This seasonal pattern of desiccation/rewetting with a high spatial resolution brings useful information for drought monitoring and forest management trough impact assessments on local-scale forest functioning [63][64][65], tree mortality [59,66] or fire risk [67]. More particularly, this information brings fine-scale information on the spatial pattern of drought, hardly precisely assessed from rough interpolations of meteorological variables [68], particularly when rain gauges are sparse, as in Tunisia [69] and more generally in Africa [70], and still uncertain from global-scale remote sensing [71][72][73].…”