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1.
Jan Esper Rolf Niederer Peter Bebi David Frank 《Forest Ecology and Management》2008,255(11):3783-3789
A potential limitation of tree-ring based climate reconstructions is related to climate signal age effects (CSAE). CSAE may arise if the climatic response of young tree-rings differs from that of old tree-rings. This could mean that climatic signals become stronger (or weaker) with tree aging, or that the seasonality of signals or the sensitivity to a specific element (e.g., temperature, precipitation) changes over time. Such changes would affect the interpretation of dendroclimatic reconstructions, as the tree-rings included in these records are generally oldest at the end of a record (e.g., 21st century)—which is the time period generally used for calibration with instrumental data.We here addressed this concern by analyzing young and old Pinus cembra trees from three high elevation sites in the central European Alps. Core and disc samples were collected in pre-defined plots to allow for a representative analysis of tree ages with tree-ring width (TRW) measurement series categorized into age classes (i) >1880, (ii) 1880–1939, and (iii) 1940–2002. Notably we report on the signal of the very young category (iii) not yet described in literature, and thus allow estimation of climate response and signal strength characteristics during the first years of the trees’ lifespans.Comparison of age classes (i)–(iii) revealed differences in TRW coherence and size, but little change in climatic signal. CSAE are in the order of the differences recorded among high elevation sites—a conclusion that holds for inter-annual to decadal scale TRW variations at near-treeline Swiss stone pine. Such data are typically included in regional and larger-scale temperature reconstructions; thus, our results add confidence to long-term climate estimates integrating a range of tree-ring age classes. Other findings, such as the reaction wood in juvenile tree-rings, and sensitivity of the climate signal to sample replication, suggest that comparisons of young and old age classes, and separate calibration of these categories against instrumental climate data might further the estimation of long-term uncertainty changes in tree-ring based climate reconstructions. 相似文献
2.
Size-mediated climate-growth relationships in temperate forests: A multi-species analysis 总被引：1，自引：0，他引：1
In most dendrochronological studies, climate-growth relationships are established on dominant trees to minimize non-climatic signals. However, response to environmental factors may be affected by tree-size, which begs the question of the representativeness of dominant trees on the stand level. To highlight the variations in climate-growth relationships among sizes and species, under a wide range of ecological conditions (climate and soil properties), 61 pure even-aged stands were sampled across France. At each stand, two tree-ring chronologies were established from 10 big- to 10 small-diameter trees. Our objectives were, (1) to assess variations in climate sensitivity between the two size-diameter classes, and (2) to investigate the role of species and ecological conditions on these variations. The climate-growth relationships were evaluated from 122 tree-ring chronologies (1 220 trees) through extreme growth years and correlation function analyses. Sensitivity to climate of shade-intolerant and moderately shade-tolerant species (Picea abies (L.) Karst., Pinus sylvestris L. and Quercus petraea (Matt.) Liebl.) remained constant between the size-diameter classes for both temperature and hydric balance, while the shade-tolerant species Abies alba Mill. and Fagus sylvatica L. displayed significant differences, with larger trees being more sensitive to summer drought than smaller trees. This difference increased with increasing climatic xericity. Our results suggest that, for shade-tolerant species, (1) big trees could be more sensitive to climatic change especially under xeric climate, and (2) future tree ring studies should include trees stratified by size to produce unbiased estimation of sensitivity to climate. 相似文献
3.
Climate-growth variability in Quercus ilex L. west Iberian open woodlands of different stand density
Guillermo Gea-Izquierdo Dario Martín-Benito Paolo Cherubini Isabel Cañellas 《Annals of Forest Science》2009,66(8):802-802
4.
The positive growth response of healthy young trees to density reduction is well known. In contrast, large old trees are usually thought to be intrinsically limited in their ability to respond to increased growing space; therefore, density reduction is seldom used in stands of old-growth trees. We tested the null hypothesis that old-growth trees are incapable of responding with increased growth following density reduction. The diameter growth response of 271 Douglas-fir (Pseudotsuga menziesii (Mirb.) Franco), ponderosa pine (Pinus ponderosa Dougl. ex Laws) and sugar pine (Pinus lambertiana Dougl.) trees ranging in age from 158 to 650 years was examined 20 to 50 years after density reduction. Density reduction involved either light thinning with removal of less vigorous trees, or shelterwood treatments in which overstory trees were not removed. Ratios of basal area growth after treatment to basal area growth before treatment, and several other measures of growth, all indicated that the old trees sometimes benefited and were not harmed by density reduction. Growth increased by 10% or more for 68% of the trees in treated stands, and nearly 30% of trees increased growth by over 50%. This growth response persisted for at least 20 years. During this 20-year period, only three trees in treated stands (1.5%) exhibited a rapid decrease in growth, whereas growth decreased in 64% of trees in untreated stands. The length of time before a growth response to density reduction occurred varied from 5 to 25 years, with the greatest growth response often occurring 20 to 25 years after treatment. These results have important implications both for the basic biology of aging in woody plants as well as for silvicultural practices in forests with old-growth trees. 相似文献
5.
The characteristic decline in height growth that occurs over a tree's lifespan is often called "age-related decline." But is the reduction in height growth in aging trees a function of age or of size? We grafted shoot tips across different ages and sizes of Douglas-fir (Pseudotsuga menziesii (Mirb.) Franco) trees to determine whether the decline in height growth is mediated by tree size or by the age of the apical meristem. We also evaluated whether reduced carbon assimilation plays an important role in height growth decline. In one experiment we cut shoot tips from old-growth, young-mature and seedling trees and grafted them onto 2-year-old graft-compatible rootstock in a seed orchard in Lebanon, Oregon. In another experiment we performed reciprocal grafts between lateral branches of old-growth trees accessible from the canopy crane at Wind River, Washington and young-mature trees in a nearby plantation. We measured growth (diameter and elongation of the dominant new stem) and mortality annually for three years in the Seed Orchard experiment and for two years in the Reciprocal Graft experiment. In the Seed Orchard experiment we also measured photosynthetic capacity (determined from the response of net carbon assimilation to the intercellular CO(2) concentration of the leaf, or A/C(i) curves), leaf mass per area (LMA) and carbon isotope composition (delta(13)C) of cellulose in 1-year-old foliage. Grafting caused changes in both growth and physiology of the grafted stems. Within two years after grafting, growth and physiology of all combinations of scions and rootstock exhibited characteristics of the rootstock. In some cases, the change in growth was dramatic-cuttings from old-growth trees showed a 10-fold increase in stem elongation rate within 2 years of grafting onto seedling rootstock. Similarly, carbon isotope discrimination of new foliage on shoots from old-growth trees increased by nearly 3 per thousand and 2 per thousand after grafting onto young-mature and seedling rootstock, respectively, whereas discrimination decreased by a similar magnitude in scions from young-mature trees after grafting on old- growth trees. Furthermore, differences in carbon assimilation estimated from carbon isotope discrimination and A/C(i )relationships were small relative to growth differences. Our results confirm that size, not age, drives developmental changes in height growth in Douglas-fir. Reduced carbon assimilation does not play an important role in height growth decline. 相似文献
6.
Giovanna Battipaglia Matthias Saurer Paolo Cherubini Rolf T.W. Siegwolf M. Francesca Cotrufo 《Forest Ecology and Management》2009
Climate changes induced by the anthropogenic alteration of the atmospheric radiative balance are expected to change the productivity and composition of forest ecosystems. In Europe, the Mediterranean is considered one of the most vulnerable regions according to climatic forecasts and simulations. However, although modifications in the inter-specific competition are envisaged, we still lack a clear understanding of the ability of the Mediterranean vegetation to adapt to climate changes. We investigated how two co-occurring tree species commonly used in afforestation programmes, the native Abies alba Mill. and the nonnative Picea abies L. Karst., adapt to climate change by assessing their growth performance and physiological responses in relation to past climate variability. Growth was addressed by analysing tree-ring width and carbon and oxygen stable isotopes. Statistical relationships between isotopic value and monthly climate data suggest that the two species underwent ecophysiological adaptation to Mediterranean climatic constraints. These adaptations are also expressed in the ring-width data. Based on the carbon isotope ratio reflecting the stomatal response to drought, we found that the precipitation in the first period of the growing season, i.e. early spring, is a major factor influencing the annual growth of A. alba, which although native, proved to be sensitive to drought. P. abies, on the other hand, showed a higher tolerance to summer drought stress. These findings should help define criteria for sustainability and effective forest conservation in the Mediterranean region. 相似文献
7.
There is limited understanding of the carbon (C) storage capacity and overall ecological structure of old-growth forests of western Montana, leaving little ability to evaluate the role of old-growth forests in regional C cycles and ecosystem level C storage capacity. To investigate the difference in C storage between equivalent stands of contrasting age classes and management histories, we surveyed paired old-growth and second growth western larch (Larix occidentalis Nutt)–Douglas-fir (Pseudostuga menziesii var. glauca) stands in northwestern Montana. The specific objectives of this study were to: (1) estimate ecosystem C of old-growth and second growth western larch stands; (2) compare C storage of paired old-growth–second growth stands; and (3) assess differences in ecosystem function and structure between the two age classes, specifically measuring C associated with mineral soil, forest floor, coarse woody debris (CWD), understory, and overstory, as well as overall structure of vegetation. Stands were surveyed using a modified USFS FIA protocol, focusing on ecological components related to soil, forest floor, and overstory C. All downed wood, forest floor, and soil samples were then analyzed for total C and total nitrogen (N). Total ecosystem C in the old-growth forests was significantly greater than that in second growth forests, storing over 3 times the C. Average total mineral soil C was not significantly different in second growth stands compared to old-growth stands; however, total C of the forest floor was significantly greater in old-growth (23.8 Mg ha−1) compared to second growth stands (4.9 Mg ha−1). Overstory and coarse root biomass held the greatest differences in ecosystem C between the two stand types (old-growth, second growth), with nearly 7 times more C in old-growth trees than trees found on second growth stands (144.2 Mg ha−1 vs. 23.8 Mg ha−1). Total CWD on old-growth stands accounted for almost 19 times more C than CWD found in second growth stands. Soil bulk density was also significantly higher on second growth stands some 30+ years after harvest, demonstrating long-term impacts of harvest on soil. Results suggest ecological components specific to old-growth western larch forests, such as coarse root biomass, large amounts of CWD, and a thick forest floor layer are important contributors to long-term C storage within these ecosystems. This, combined with functional implications of contrasts in C distribution and dynamics, suggest that old-growth western larch/Douglas-fir forests are both functionally and structurally distinctive from their second growth counterparts. 相似文献
8.
Nectandra is one of the most representative genera of Lauraceae in the subtropical Atlantic Forest of Brazil. The objective of this work was to study the dendrochronological potential of Nectandra oppositifolia Nees and Mart. from two sites in Santa Catarina State in southern Brazil. A tree-ring chronology of 34 trees was developed. The time span ranged from 1843 to 2013. The oldest and youngest trees were 171 and 47 years-old and the average length of the series was 103 years. Average diameter and annual increment were 20.64 cm and0.74 mm a-1; diameter and age were unrelated. The species has good dendrochronological potential with an intercorrelation of 0.61 between sites, indicating the existence of a synchronous pattern in the development of the trees. The climate response of the species could be seen by negative tree growth effects for previous hot and current rainy growth seasons. 相似文献
9.
Elisabeth Düthorn Lea Schneider Björn Günther Simon Gläser Jan Esper 《Scandinavian Journal of Forest Research》2016,31(8):750-757
Shifts in the climate sensitivity of trees throughout the twentieth century might indicate climate change effects in the boreal forest ecosystem. We here evaluated such potential changes by analyzing six tree-ring width (TRW) and maximum latewood density (MXD) chronologies from northern, central and southern boreal forests in Finland (60°N–69°N). Besides latitudinal effects, differing micro-sites (lakeshore and inland) were considered to evaluate the influence of ground water access on twentieth-century tree-ring formation and climate sensitivity. Overall, the boreal MXD chronologies appeared less affected by micro-site conditions compared to the TRW chronologies. Along the boreal transect, mean growth rates decrease with increasing latitude, but the ratio of earlywood-to-latewood (～70%/～30%) remains stable. However, latewood is slightly denser at the dry inland micro-sites. The correlations with climate data showed that TRW and MXD at all sites are positively related with summer temperature. The MXD chronologies are also negatively correlated with precipitation, a feature that is largely missing in TRW. A recent trend toward wetter and cloudier conditions in the study region coincides with a shift of the MXD signal from a distinct temperature limitation toward an additional sensitivity to precipitation, which in turn stimulated the trees’ competition for sunlight. 相似文献
10.
根据采自山东蒙山地区两组幼龄黑松树木年轮样本,研制出单点和区域树轮宽度年表,分析了蒙山黑松树轮宽度年表的统计参数和径向生长的气候限制因子,并尝试重建相关密切的气候因子,探讨蒙山黑松径向生长与大范围气候变化的关联。研究结果表明,（1）蒙山黑松树轮宽度年表的统计参数都比较高,说明蒙山黑松树轮宽窄变化包含有较多的气候环境变化信息。（2）蒙山黑松径向生长变化与当年4-9月降水量呈显著正相关。同时,当年5-7月异常高温也对蒙山黑松径向生长变化产生显著抑制。通过黑松树轮宽度年表对4-9月降水量的模拟重建结果表明蒙山黑松具有较大树轮气候研究潜力。（3）蒙山黑松树轮宽度生长与太平洋大范围气候波动存在显著关联。 相似文献
11.
Abstract Six Douglas fir (Pseudotsuga menziesii Franco) stands were selected in both the Sudety Mountains and the Great Poland Lowland. These two regions are distinctly different with regard to thermal and pluvial conditions. In each stand, two increment cores per tree were extracted from 20 approximately 100-year-old trees and the tree-ring widths measured. It is clear from the different growth reactions of the study trees to the climatic conditions that the Sudety Mountains and the Great Poland Lowland are two dendrochronologically separate regions. The tree-ring width chronologies form homogeneous groups for each region. The tree ring–climate models for Douglas fir in both regions indicate similarities and differences. The similarities among chronologies are attributed to winter temperature. The differences are attributed to rainfall (which changes with longitude and altitude of sites) during the vegetation season. 相似文献
12.
Marieke van der Maaten-Theunissen Hans-Peter Kahle Ernst van der Maaten 《Annals of Forest Science》2013,70(2):185-193
Context
For Central Europe, climate projections foresee an increase in temperature combined with decreasing summer precipitation, resulting in drier conditions during the growing season. This might negatively affect forest growth, especially at sites that are already water-limited, i.e., at low elevation. At higher altitudes trees might profit from increasing temperatures.Aims
We analyzed variations in radial growth of silver fir (Abies alba Mill.) and Norway spruce (Picea abies (L.) Karst.) along an altitudinal gradient from 400 until 1,140 m a.s.l. in the Black Forest, to assess climate responses with increasing elevation.Methods
Climate–growth relationships were analyzed retrospectively using tree-ring and climate data. In total, we sampled stem discs of 135 trees to build 27 species- and site-specific chronologies (n fir?=?13, n spruce?=?14).Results
Our results indicate distinct differences in climate–growth relations between fir and spruce along the gradient. Growth of high-altitude fir was positively related to temperature from January till March. Growth of low-altitude fir and spruce at all elevations was positively related to precipitation and negatively to temperature during the growing season, particularly in July. A self-calibrating Palmer drought severity index underlined summer drought sensitivity of these trees.Conclusion
Overall, we found that climatic control of tree growth changes over altitude for fir. For spruce, a remarkable synchrony in growth variation and climate response was shown, which indicates that this species is drought sensitive at all studied elevations. In a future warmer climate, the growth of low-altitude fir and spruce along the entire studied gradient may be negatively affected in the Black Forest, if an increased evaporative demand cannot be compensated by increased water supply. 相似文献13.
Forest decline: modeling the effect of climate in tree rings 总被引：1，自引：0，他引：1
Tree rings provide an historical record of forest growth that reflects changes with time in site factors including, competition, tree and stand age, fire and other disturbances, and climate. Statistical methods can be used to factor out climatic influences on radial growth to yield a climate response model that can indicate whether declines in forest productivity are related to the modeled climatic variables or to other influences such as atmospheric pollutants. A general method, based on ordinary least squares, is presented for creating climatic response models for forest decline studies. The crux of the method is model verification, whereby the time-stability of the model is tested before it is used to forecast tree-ring variations during a period of decline. Three studies are described that employ monthly mean temperatures to predict tree-ring indices in declining red spruce (Picea rubens Sarg.) stands in the Appalachian Mountains of North America. The results indicate that, since 1960, red spruce trees at most of the sites sampled have undergone a period of growth decline that is unrelated to changes in mean monthly temperature. However, an association between annual ring width and unusual departures from the mean summer and winter temperatures during both present and past periods of decline suggests that climatic effects are implicated to some degree in the current decline. 相似文献
14.
Apple M Tiekotter K Snow M Young J Soeldner A Phillips D Tingey D Bond BJ 《Tree physiology》2002,22(2-3):129-136
Morphological differences between old-growth trees and saplings of Douglas-fir (Pseudotsuga menziesii (Mirb.) Franco) may extend to differences in needle anatomy. We used microscopy with image analysis to compare and quantify anatomical parameters in cross sections of previous-year needles of old-growth Douglas-fir trees and saplings at the Wind River Canopy Crane site in Washington and at three sites in the Cascade Mountains of Oregon. We also compared needle anatomy across a chronosequence of 10-, 20-, 40- and 450-year-old Douglas-fir trees from the Wind River site. Anatomy differed significantly between needles of old-growth trees and saplings at all sites, suggesting a developmental change in needle anatomy with increasing tree age. Compared with needles of old-growth trees, needles of saplings were longer and had proportionately smaller vascular cylinders, larger resin canals and few hypodermal cells. Astrosclereids, which sequester lignin in their secondary cell walls and occupy space otherwise filled by photosynthetic cells, were scarce in needles of saplings but abundant in needles of old-growth trees. Needles of old-growth trees had an average of 11% less photosynthetic mesophyll area than needles of saplings. The percentage of non-photosynthetic area in needles increased significantly with increasing tree age from the chronosequence of 10-, 20-, 40- and 450-year-old trees at the Wind River site. This reduction in photosynthetic area may contribute to decreased growth rates in old trees. 相似文献
15.
Darío Martín-Benito Miren Del Río Ingo Heinrich Gerhard Helle Isabel Cañellas 《Forest Ecology and Management》2010
Thinning is the main forestry measure to increase tree growth by reducing stand tree density and competition for resources. A thinning experiment was established in 1993 on a 32-year-old Pinus nigra Arn. stand in central Spain. The response of growth, climate-growth relationships and intrinsic water use efficiency (WUEi) to a stand density reduction were compared between moderate thinned plots and a control plot by a combined analysis of basal area increments (BAI), and C and O stable isotope ratios (δ13Cc and δ18Oc). BAI in the control plot showed a decreasing trend that was avoided by thinning in the thinned plot. Thinning also partially buffered tree-ring response to climate and trees were less sensitive to precipitation although more sensitive to temperature. Δ13Cc in the thinned plot was not modified indicating that stomatal conductance (g) and photosynthetic capacity (A) did not change or change in the same direction. However, δ18Oc decreased in the control plot (unrelated to δ18O of precipitation) but not in the thinned plot, suggesting a relative increase of temperature and irradiance and/or a decrease of air humidity after reducing the density consistent with an increase in A, g and BAI. As WUEi did not increase in the thinned plot, faster growth in this plot was caused by higher abundance of resources per tree. The trend of WUEi in both plots indicated low-moderate CO2-induced improvements. Thinning might be a useful adaptation measure against climate change in these plantations reducing their vulnerability to droughts. However, because WUEi was not affected, the positive growth response might be limited if droughts and warming continue and certain thresholds are exceeded. 相似文献
16.
Tree growth is regulated by a combination of exogenous and endogenous factors. Such factors also interact with each other, complicating the understanding of causal links. IN particular, resource allocation is sensitive to reproductive investment, especially in masting species, which in turn is regulated by climatic variables. Both resource allocation and seed production patterns are also sensitive to tree age. This study aims to (1) evaluate the effects of tree age and local and regional climate on tree ring width and seed production by Spanish black pine (Pinus nigra Arn. ssp. salzmannii) forest in Cuenca Mountains (Spain), and (2) assess the relationship between seed production and secondary growth of Spanish black pine. Seed fall was estimated using 60 rectangular seed traps (40 × 50 × 15 cm) from 2000 to 2014, randomly distributed across the study area. Standardized tree-ring chronologies were calculated using a random sample of 106 trees stratified into three age classes (> 80 years; 26–80 years, and ≤ 25 years). Local climate data was obtained from a meteorological station, and regional climate data from the CRU-TS 3.1 dataset. Average seed production ranged over time from 2 to 189 seeds m?2 (coefficient of variation = 157%). We identified four masting years (2000, 2003, 2006, and 2014) using a classification based on percentile seed production. Seed production was regulated by climate of the previous 2–3 years, while tree growth responded to precipitation and temperature in the previous and current year. Independent of climate, high seed production had a negative effect on tree ring width and weakened climate growth relationships, indicating resource depletion. Tree age modulated climate sensitivity, increasing correlations between climate and tree-ring index in older trees. P. nigra has been showed to be a climate sensitive species with a bimodal masting behaviour, which should be taking into account for management purposes and silvicultural guidelines under climate change scenarios. 相似文献
17.
Fire scars in dated sequences of tree-rings are regularly used for the reconstruction of histories of forest fire frequency and investigations of various exogenous factors (climate in particular) which may control such events. The potential of the tree-ring archive in this regard is such that in circumstances where no scarring occurs following a particular fire, or where sampling is limited to increment cores which may miss the zone of scarring, alternate means of detecting tree-ring evidence for fire impact must be sought. One possible alternative may be detection of changes in tree-ring chemistry associated with growth years following forest fires. If it was possible to characterize such a change in chemistry an independent proxy for forest fires in tree-ring series might be established. The behavior of various elements within the xylem is however extremely complex so for a dendrochemical approach to fire history to be established, new techniques are required to enhance existing knowledge of elemental behavior in trees affected by fire. In this study, elemental intensities were mapped across scarred and un-scarred vectors of Pseudotsuga macrocarpa (Vasey) Mayr (bigcone Douglas-fir) tree-rings from a site in the Los Padres National Forest, Southern California, using Scanning X-Ray Fluorescence Microscopy (SXFM). The aims were: to assess the potential of this technique for understanding elemental change in relation to fire scars and undamaged contemporary growth; to provide new information on specific elemental behavior in this species; and to contribute to wider research for dendrochemically establishing fire histories. The results highlight the potential of SXFM for mapping elemental changes associated with compartmentalization, callus and woundwood as well as providing some evidence for depletion of certain elements in contemporary un-scarred rings. They also provide a first step towards future work to use cores for dendrochemical construction of fire histories. 相似文献
18.
Tree-ring chronologies were developed fromAbies mariesii Masters andPicea jezoensis ssp.hondoensis (Mayr) P. Schmidt collected at different altitudes of Mt. Norikura, central Japan. The tree-ring parameters of ring width and maximum density were measured by soft X-ray densitometry. The measurement series were detrended by fitting a 33-year cubic smoothing spline and autoregressive model. The correlation between species and between sites showed different responses of the species to climate in terms of ring width and maximum density. The correlation coefficient between sites within a species was higher than that between species for a site in the ring width, and the coefficient between species for a site was higher in maximum density. The correlation coefficient between tree-ring chronology and monthly climate data set showed different responses of radial growth to climate. The different response was probably explained by the difference in the length of the growing season. High summer temperature increased the maximum density of the two species and the radial growth inAbies mariesii. Summer precipitation correlated negatively to maximum density, but it did not affect the ring width of either species. The climatic signals could be extracted from ring-width and maximum-density chronologies of both species. 相似文献
19.
The scarcity of large old-growth forests has made it challenging to quantify disturbance regimes in Central Europe. The objective of this study was to reconstruct the history of disturbance in an old-growth Fagus-Abies forest reserve in Slovenia using a dendroecological approach. We extracted cores from canopy trees blown down during a recent windthrow event and identified growth releases in the tree-ring series using boundary-line release criteria to infer past disturbances. A total of 216 release events were identified from 88 trees. Between 1790 and 1990, moderate, asynchronous release events were present in nearly every decade of the disturbance chronology, suggesting a history of frequent, low severity disturbance. However, there were also peaks in the chronology corresponding to synchronous release events in a large proportion of the trees, suggesting that less frequent, intermediate severity disturbance events played an important role in forest development. These events are likely caused from wind damage associated with local thunderstorms, which seem to occur at intervals between 20–80 years on the study site. Thus, in addition to the small-scale gap phase processes operating in the forest, the results indicate that periodic intermediate severity disturbance events are an important component of the disturbance regime in mountain forests of Central Europe. 相似文献
20.
The natural abundance of stable carbon isotopes in the annual rings of forest trees is used as a tracer of environmental changes such as climate and atmospheric pollution. Although tree-ring delta(13)C varies by about 2 per thousand from year to year, variability within the foliage can be as high as 6 per thousand. Recent studies have shown that branch length affects stomatal response, which influences the integrated foliar delta(13)C signal. To improve the ability of delta(13)C to predict climate differences, we examined the relationship between branch length and foliar delta(13)C in Pseudotsuga menziesii (Mirb.) Franco from four sites across a steep climate gradient in Oregon. The transect spanned the boundary between the ranges of the coastal variety, P. menziesii var. menziesii (three sites), and the Rocky Mountain variety, P. menziesii var. glauca (one site). At the most maritime site, branch length explained 76% of within-site variation of 5 per thousand, whereas at the harshest site, branch length accounted for only 15% of this variation. We considered the possibility that cavitation in the water-conducting xylem obscures the branch length effect in the harsher climates. Cavitation, as measured by dye perfusion, was most extensive at sites where the branch length effect in the coastal variety was weakest. Trees at the site with the most substantial cavitation displayed seasonal xylem refilling. Branch length standardization significantly improved the relationship between delta(13)C and climate. With standardization to constant length, delta(13)C values were significantly related to the degree that climatic variables, as modeled with a forest growth simulation model, constrain transpiration (R(2) = 0.69, P < 0.0001). Without standardization, the R(2) was 0.27. We conclude that sampling standard length branches or tree rings from trees of similar shape and size is desirable when seeking correlations between isotopic composition and climate. 相似文献