Acid rain and soils of the Adirondacks. II. Evaluation of calcium and aluminum as causes of red spruce decline at Whiteface Mountain, New York

1994 ◽  
Vol 24 (11) ◽  
pp. 2298-2298
Author(s):  
A.H. Johnson ◽  
T.N. Schwartzman ◽  
J.J. Battles ◽  
R. Miller ◽  
E.K. Miller ◽  
...  

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1990 ◽  
Vol 20 (9) ◽  
pp. 1415-1421 ◽  
Author(s):  
David C. LeBlanc ◽  
Dudley J. Raynal

Understanding the relationship between apical and radial growth decline can contribute toward the evaluation of hypotheses regarding causal mechanisms of red spruce decline. The etiology of red spruce decline in montane spruce-fir forests of the northeastern United States includes loss of foliage at branch apices, crown dieback, and unreversed radial growth decline since the 1960s. Demographic analyses of crown damage and radial growth decline for red spruce on Whiteface Mountain, New York, indicate that large, canopy-emergent trees with exposed crowns exhibit greater decline than codominant trees within an intact canopy. In this paper, radial growth decline is shown to have been coincident with decreased apical growth and increased incidence of injury to terminal leaders. Incidence of leader mortality is greatest for canopy-emergent red spruce or trees with exposed crowns, similar to patterns described for radial growth. This relationship suggests that the post-1960 decline of red spruce on Whiteface Mountain is caused, at least in part, by stresses that act directly on the crown.


1994 ◽  
Vol 24 (4) ◽  
pp. 654-662 ◽  
Author(s):  
A. H. Johnson ◽  
T.N. Schwartzman ◽  
J.J. Battles ◽  
R. Miller ◽  
E.K. Miller ◽  
...  

Several recent publications suggest that acid deposition produces high anion concentrations in the soil solution of high-elevation forests, causing Al-induced Ca deficiency in red spruce (Picearubens Sarg.) root tips. Some authors suggest that this results in decreased growth below and above ground, decline, and ultimately in death. Accordingly, we examined soil solution Al and Ca, soil and foliar chemistry, and their relationship to red spruce decline on Whiteface Mountain, New York, where severe red spruce mortality occurred between the mid-1960s and late 1980s. Spruce mortality and crown condition are strongly related to elevation, but there is no evidence that the occurrence or degree of spruce decline is related to exchangeable Al, Mg, Ca, or their ratios in mineral or organic horizons. Foliar Ca and Mg concentrations that we measured were in the range judged to be sufficient based on field fertilization studies. Soil solution ratios of Ca:Al in mineral and organic horizons were above the threshold (1:1 molar ratio) proposed as detrimental to Ca uptake in all samples collected during three of four growing seasons, and soil-solution Al concentrations were well below levels thought to inhibit spruce root growth. If Al toxicity is a factor in red spruce decline on this mountain, it is acting in a way that is not detectable using soil and foliar analyses.


1995 ◽  
Vol 25 (8) ◽  
pp. 1340-1345 ◽  
Author(s):  
John D. Castello ◽  
George D. Bachand ◽  
Philip M. Wargo ◽  
Volker Jacobi ◽  
Donald R. Tobi ◽  
...  

Tomato mosaic tobamovirus (ToMV) was detected by enzyme-linked immunosorbent assay in the roots of red spruce (Picearubens Sarg.) on Whiteface Mountain, New York. Both virus incidence and concentration in the roots of red spruce vary by site and were greater in trees with little to moderate crown dieback than in trees with severe dieback. There was no significant association between virus incidence or concentration in the roots of red spruce and elevation on Whiteface Mountain. Multiple regression analysis of virus concentration in the roots, as the dependent variable, was performed against nine selected crown and root variables. In the final regression model, the number of live second-order nonwoody roots per length of first-order nonwoody root and length of the live crown were positively and negatively correlated, respectively, with virus concentration in the roots. These results suggest a complex epidemiology and a potentially significant impact of ToMV infection on the growth of red spruce on Whiteface Mountain.


1992 ◽  
Vol 119 (4) ◽  
pp. 418 ◽  
Author(s):  
John J. Battles ◽  
Arthur H. Johnson ◽  
Thomas G. Siccama ◽  
Andrew J. Friedland ◽  
Eric K. Miller

1992 ◽  
Vol 22 (8) ◽  
pp. 1132-1138 ◽  
Author(s):  
Hedda Schlegel ◽  
Robert G. Amundson ◽  
Aloys Hüttermann

To determine the element distribution in fine roots of red spruce (Picearubens Sarg.) at a high-elevation decline site on Whiteface Mountain, New York, fine-root samples were collected and analysed by X-ray microanalysis. Aluminium was found in very high concentrations in the root cortex, but could not be detected in stelar tissues. In contrast, magnesium was found only in the central cylinder in low amounts. The calcium concentration in the cortex was low, but was higher in the stele. Aluminium has been shown to interfere with cation uptake by blocking exchange sites in the cortical apoplast. Thus these results strongly suggest that the low foliar magnesium and calcium contents of the declining red spruce trees are driven by aluminium-induced inhibition of magnesium and calcium uptake. Soil solution chemistry, ion distribution in fine roots, and foliar ion contents at Whiteface Mountain were compared with equivalent data from other forest sites as well as with data from controlled studies on spruce seedlings. These data suggest that aluminium toxicity contributes to red spruce decline at Whiteface Mountain.


1993 ◽  
Vol 71 (6) ◽  
pp. 827-833 ◽  
Author(s):  
Julian L. Hadley ◽  
Robert G. Amundson ◽  
J. A. Laurence ◽  
R. J. Kohut

Terminal bud mortality for shoots produced between 1982 and 1989 was measured for midcanopy branches of mature red spruce trees (Picea rubens Sargent) at two elevations on Whiteface Mountain, New York, U.S.A. Average terminal bud mortality ranged from 15 to 45% in different years, and there was no evidence for a biotic cause of bud mortality. Between branches on different trees, there was a negative correlation between frequency of terminal bud mortality for shoots produced between 1987 and 1989 and the percent change in current-year foliage biomass between 1987 and 1990. Branches with a high frequency of terminal bud mortality also tended to have a high proportion (> 50%) of 1990 shoots developed on adventitious branchlets. In late November 1990, terminal buds from most trees at 710–1120 m elevation were susceptible to freezing injury between −31 and −38 °C when cooled at 4 °C/h under laboratory conditions. Typical winter minimum temperatures at 700–1100 m elevation on Whiteface Mountain are within this range. In a recent controlled study of red spruce seedlings, high foliar nitrogen was associated with an increased risk of freezing injury to terminal buds in autumn. We found that red spruce on Whiteface Mountain had higher foliar nitrogen levels compared with red spruce at a much lower elevation in Maine. Based on these results, we advocate further research on the relationship between foliar nitrogen and bud freezing sensitivity in high elevation red spruce. Key words: Picea rubens, red spruce, bud mortality, freezing injury, nitrogen, red spruce decline.


1990 ◽  
Vol 20 (9) ◽  
pp. 1422-1431 ◽  
Author(s):  
William G. Warren ◽  
David C. LeBlanc

The compound growth function of Warren (W.G. Warren. 1980. Tree-Ring Bull. 40: 35–44) represented an attempt at developing a model-based approach that standardized tree ring width sequences and was more flexible than the monotonic functions that were then commonly used. While the idea was conceptually attractive, operational difficulties of fitting hindered its use as a practical tool. This paper describes the modifications, and what are believed to be improvements, that have recently been made to the method, and which have led to an interactive computer program by which the fitting of the model to any sequence of ring widths may be readily accomplished. The approach also permits the location of both positive and negative departures from a trend (releases and suppressions, respectively) and estimation of the rate of ring-width increase or decrease. For illustration it has been applied to a sample of red spruce (Picearubens Sarg.) cores from Whiteface Mountain, New York. Some synchrony in releases and suppressions was detected, with suppressions being very conspicuous since the late 1950s. Also, the recent reductions in growth rates are as great, or greater, than those previously exhibited by the trees of this sample.


1990 ◽  
Vol 20 (9) ◽  
pp. 1408-1414 ◽  
Author(s):  
David C. LeBlanc

Detailed stem analysis and stand structure and history analyses are used to evaluate relationships between growth decline in populations of red spruce (Picearubens Sarg.) on Whiteface Mountain and elevation, tree age and size, and stand dynamics. The study sites are virgin, uneven-aged spruce-fir forests at 900 and 1100 m elevation. Most red spruce sampled exhibited substantial decreases in annual stem wood volume increment from 1964 to 1984, particularly large trees and trees from higher elevation. While larger trees exhibited more severe growth decline, there is no evidence of a direct causal link between tree age and decline. Inverse relationships between growth and competition indices are evident for periods prior to the onset of decline, but these relationships degrade during the period of growth decline; competition is not causally linked to decline. There is some indication that the decline-inciting stress was particularly severe for canopy-emergent and exposed red spruce, suggesting the action of an atmospheric stress.


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