TL;DR: Great Basin bristlecone pine (Pinus longaeva) at 3 sites in western North America near the upper elevation limit of tree growth showed ring growth in the second half of the 20th century that was greater than during any other 50-year period in the last 3,700 years.
Abstract: Great Basin bristlecone pine (Pinus longaeva) at 3 sites in western North America near the upper elevation limit of tree growth showed ring growth in the second half of the 20th century that was greater than during any other 50-year period in the last 3,700 years. The accelerated growth is suggestive of an environmental change unprecedented in millennia. The high growth is not overestimated because of standardization techniques, and it is unlikely that it is a result of a change in tree growth form or that it is predominantly caused by CO2 fertilization. The growth surge has occurred only in a limited elevational band within ≈150 m of upper treeline, regardless of treeline elevation. Both an independent proxy record of temperature and high-elevation meteorological temperature data are positively and significantly correlated with upper-treeline ring width both before and during the high-growth interval. Increasing temperature at high elevations is likely a prominent factor in the modern unprecedented level of growth for Pinus longaeva at these sites.
TL;DR: In this paper, remains of dead bristlecone pine (Pinus longaeva Bailey) are found at altitudes up to 150 m above present treeline in the White Mountains.
TL;DR: In this paper, a regional chronology of upper forest border bristlecone pine (Pinus longaeva and Pinus aristata) over the last 5000 yr coincides with known large explosive volcanic eruptions and/or ice core signals of past eruptions.
TL;DR: In this paper, the selection of species which minimizes radial translocation of elements can be critical to the success of dendrochemical research, and the most important xylem-based criteria are heartwood moisture content, permeability and the nature of the sapwood-heartwood transition.
Abstract: Recently, element concentrations in tree rings have been used to monitor metal contamination, fertilization, and the effects of acid precipitation on soils. This has stimulated interest in which tree species may be suitable for use in studies of long-term trends in environmental chemistry. Potential radial translocation of elements across living boundaries can be a confounding factor in assessing environmental change. The selection of species which minimizes radial translocation of elements can be critical to the success of dendrochemical research. Criteria for selection of species with characteristics favorable for dendrochemical analysis are categorized into (1) habitat-based factors, (2) xylem-based factors, and (3) element-based factors. A wide geographic range and ecological amplitude provide an advantage in calibration and better controls on the effects of soil chemistry. The most important xylem-based criteria are heartwood moisture content, permeability, and the nature of the sapwood-heartwood transition. The element of interest is important in determining suitable tree species because all elements are not equally mobile or detectable in the xylem. Ideally, the tree species selected for dendrochemical study will be long-lived, grow on a wide range of sites over a large geographic distribution, have a distinct heartwood with a low number of rings in the sapwood,more » a low heartwood moisture content, and have low radial permeability. Recommended temperate zone North American species include white oak (Quercus alba L.), post oak (Q. stellate Wangenh.), eastern redcedar (funiperus virginiana L.), old-growth Douglas-fir [Pseudoaugu menziesii (Mirb.) Franco] and big sagebrush (Artemisia tridentata Nutt.). In addition, species such as bristlecone pine (Pinus aristata Engelm. syn. longaeva), old-growth redwood [Sequoia sempervirens (D. Don) Endl.], and giant sequoia [S. gigantea (Lindl.) Deene] may be suitable for local purposes. 118 refs., 2 tabs.« less
TL;DR: It is proposed that extended needle fascicle longevity represents an adaptation to arid and especially high elevation environments, and differences between taxa in DSR relate to both genetic and environmental factors.
Abstract: Variation in leaf longevity of gymnosperms has received surprisingly little attention despite its likely adaptive significance. Pinus longaeva, a pine of arid, subalpine environments in the western United States, has the record among conifers for needle longevity, with a maximum dwarf shoot (needle fascicle) retention time of up to about 45 years. Most low elevation pines have dwarf shoot retention times (DSRs) of two to four years. Literature data for the 37 species of Pinus native to the United States and Canada and field data for eight taxa (21 populations) of pines growing at various elevations in California each show a strong positive correlation between elevation and DSR, respectively, r=+0.65, df=35, p<0.001 and r=+0.82; df=19, p<0.001. We propose that extended needle fascicle longevity represents an adaptation to arid and especially high elevation environments. Field data from native stands and common gardens indicate that differences between taxa in DSR relate to both genetic and environmental factors. When grown at the same sites certain species (eg, P. longaeva, P. monophylla) had much longer DSRs than others, indicating a genetic basis for differences in needle fascicle longevity. For six of seven taxa that were each studied at more than one elevation there was a statistically significant increase in DSR in going from the lowest to the highest elevation site, indicating strong environmental control of needle fascicle longevity. The physiological control of dwarf shoot senescence and abscission is poorly understood. For P. longaeva dwarf shoots of a particular age class are not shed simultaneously; rather there is a more or less gradual attrition of dwarf shoots from the long shoot. Although different types of long shoots of pines are known to differ physiologically, for P. longaeva there was no consistent difference in DSR on various types of lateral long shoots (eg, vegetative, pollen cone-bearing, seed cone-bearing), nor was there a statistically significant difference in DSR on trunks versus on their lateral long shoots. In addition, for P. contorta ssp. bolanderi and P. muricata needle fascicle longevity was not affected by the degree of edaphically induced dwarfing (ie, stunting) of the trees.