1990
DOI: 10.1111/j.1439-0329.1990.tb01277.x
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Decline of radial growth in red oaks is associated with short‐term changes in climate

Abstract: Comparison of basal area increments of paired healthy and declined oak trees shows a marked disjuncture beginning in the early 195O's at 3 of 4 sample locations across the southeastern United States. An argument is presented^ that the change in growth was caused (or accelerated) by a series of severe regional droughts in the early 1950*s that impacted the trees which then responded by formmg two distinct populations consistmg of: I. relatively healthy trees, and 2. declined trees. Both populations produced les… Show more

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Cited by 47 publications
(47 citation statements)
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References 6 publications
(12 reference statements)
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“…A current summer mean temperature signal is present, but it is largely confined to the northern portion of the mountain range and shows much weaker significance regionally. These results contrast with other northern red oak dendroclimatic studies from low-to mid-elevation closedcanopy forest stands across the Southern Appalachian region which have found significant summer drought sensitivity, and indicates that water stress is the dominant control on ring-width variability at lower elevations (e.g., Tainter et al, 1984Tainter et al, , 1990Pan et al, 1997;Speer et al, 2009). On the other hand, at its northern range limits, northern red oak ring-width has shown significant sensitivity to both summer drought (e.g., Conciatori, 2006a, 2006b;Tardif et al, 2006) and winter temperature (e.g., Pederson et al, 2004).…”
Section: Climate-driven Control On Northern Red Oak Ring-width Variabcontrasting
confidence: 55%
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“…A current summer mean temperature signal is present, but it is largely confined to the northern portion of the mountain range and shows much weaker significance regionally. These results contrast with other northern red oak dendroclimatic studies from low-to mid-elevation closedcanopy forest stands across the Southern Appalachian region which have found significant summer drought sensitivity, and indicates that water stress is the dominant control on ring-width variability at lower elevations (e.g., Tainter et al, 1984Tainter et al, , 1990Pan et al, 1997;Speer et al, 2009). On the other hand, at its northern range limits, northern red oak ring-width has shown significant sensitivity to both summer drought (e.g., Conciatori, 2006a, 2006b;Tardif et al, 2006) and winter temperature (e.g., Pederson et al, 2004).…”
Section: Climate-driven Control On Northern Red Oak Ring-width Variabcontrasting
confidence: 55%
“…Northern red oak, a deciduous species that occupies low-to high-elevation sites across the Southern Appalachian mountain range, has received considerable attention in dendroclimatic research (e.g., Tainter et al, 1990;Pan et al, 1997;Fekedulegn et al, 2003;Speer et al, 2009); however, these studies were based on tree-ring records from lower elevation closed-canopy stands where climate is less variable and often markedly differs from higher elevation regions (Konrad, 1996). In this paper, a collection of six open-canopy high-elevation northern red oak (Quercus rubra L.) ring-width records are evaluated for the presence of a common climate-driven growth signal across the Southern Appalachian mountain range in the southeastern United States.…”
Section: Introductionmentioning
confidence: 99%
“…The high electrical conductivity of soils below oaks which could indicate mobility of N compounds as nitrate due to flooding events is also remarkable, explaining the similar N soil data observed in both tree species, or increased salinity and reduced availability for some important nutrients such as P (Table 4). In sites with nutrient-poor or shallow soils, oaks with canopy dieback (defoliation above 60%) show low growth rates and reach a threshold in their ability to recover after drought [65,[74][75][76].…”
Section: Discussionmentioning
confidence: 99%
“…Although the strength of evidence was low, we did identify a negative effect of SI (in the context of the additive model) on BAI resilience during the second drought. Positive relationships between BAI recovery and BAI resilience and SI during the first drought and BAI resistance and SI during the second drought confirms that northern red oak growth during and after drought is reduced to a greater degree on poorly versus highly productive sites (Tainter et al 1990). These positive relationships between drought indices and SI are likely related to the fact that SI is negatively correlated with soil moisture deficit (Klinka and Carter 1990;Kayahara et al 1997;Chen et al 2002).…”
Section: Discussionmentioning
confidence: 56%