• PREFACE-Tree-ring studies in New York State: Past and present

      Barclay, D.J.; Pederson, N.; Griggs, C. (Tree-Ring Society, 2014-07)
      New York State (NYS) has a long and significant history of tree-ring research. Some of the earliest dendroarchaeological and dendroclimatic work in eastern North America was done in NYS, and 1970s studies in Hudson Valley in the east of the state were important for demonstrating that drought records could be reconstructed from trees growing in humid environments. Some recent work in NYS is described in this issue of Tree-Ring Research, including tree-ring dating and provenancing of a boat in New York City, dendroarchaeological studies in a town in northeastern NYS, dendrogeomorphological work in central NYS, and a dendroclimatic investigation of two range-margin Juniperus species growing on alvars. The last of the five NYS papers in this issue provides a personal historical perspective on the beginnings of drought reconstructions in the Hudson Valley. There is considerable potential for future work in New York with extension of existing studies and work in new areas and with new tree species.
    • Dendrochronological potential and productivity of tropical tree species in Western Kenya

      David, E.T.; Chhin, S.; Skole, D. (Tree-Ring Society, 2014-07)
      This study focuses on tropical tree growth rates in Western Kenya. The dendrochronological potential of each study species was determined by visual examination of rings, and then cumulative growth trajectories for diameter were synthesized for species of sufficient sample size (n ≥ 3), based on ring-width chronologies. The 14 tree species considered were: Acacia mearnsii, Bridelia micrantha, Combretum molle, Croton macrostachyus, Cupressus lustianica, Eucalyptus camaldulensis, Eucalyptus grandis, Eucalyptus saligna, Grevillea robusta, Mangifera indica, Markhamia lutea, Persia Americana, Syzygium cumini, and Trilepisium madagascariensis. The species with the highest dendrochronological potential included Acacia mearnsii, Cupressus lusitanica, the Eucalyptus spp. and Mangifera indica, which are all non-native species that successfully crossdated. The results also indicated that the species with highest dendrochronological potential had strong radial growth synchrony, which was reflected in high inter-tree correlation and (or) high growth variance explained by the first principal component axis. Furthermore, A. mearnsii and E. camaldulensis were sensitive to annual precipitation and moisture index. The species with the lowest dendrochronological potential were Grevillea robusta and Markhamia lutea. In terms of productivity, the three fastest growing species in the study, based on annual diameter increment, were Eucalyptus camaldulensis, Eucalyptus grandis, and Acacia mearnsii. This study also has great potential to extrapolate historical patterns of diameter growth to understanding annual aboveground biomass and carbon dynamics in Western Kenya.
    • Dendrochronological dating of the World Trade Center ship, Lower Manhattan, New York City

      Martin-Benito, D.; Pederson, N.; McDonald, M.; Krusic, P.; Fernandez, J.M.; Buckley, B.; Anchukaitis, K.J.; D'Arrigo, R.; Andreu-Hayles, L.; Cook, E. (Tree-Ring Society, 2014-07)
      On July 2010, archaeologists monitoring excavation at the World Trade Center site (WTC) in Lower Manhattan found the remains of a portion of a ship's hull. Because the date of construction and origin of the timbers were unknown, samples from different parts of the ship were taken for dendrochronological dating and provenancing. After developing a 280-year long floating chronology from 19 samples of the white oak group (Quercus section Leucobalanus), we used 21 oak chronologies from the eastern United States to evaluate absolute dating and provenance. Our results showed the highest agreement between the WTC ship chronology and two chronologies from Philadelphia (r  =  0.36; t  =  6.4; p < 0.001; n  =  280) and eastern Pennsylvania (r  =  0.35; t  =  6.3; p < 0.001; n  =  280). The last ring dates of the seven best-preserved samples suggest trees for the ship were felled in 1773 CE or soon after. Our analyses suggest that all the oak timbers used to build the ship most likely originated from the same location within the Philadelphia region, which supports the hypothesis independently drawn from idiosyncratic aspects of the vessel's construction, that the ship was the product of a small shipyard. Few late-18th Century ships have been found and there is little historical documentation of how vessels of this period were constructed. Therefore, the ship's construction date of 1773 is important in confirming that the hull encountered at the World Trade Center represents a rare and valuable piece of American shipbuilding history.
    • Shifting climate sensitivity and contrasting growth trends in Juniperus species growing together at opposite range margins

      Riddle, J.; Pederson, N.; Stella, J.C.; Leopold, D.J. (Tree-Ring Society, 2014-07)
      The long generation time of woody plants inhibits detection of shifts in their distributions induced by climatic change. Consequently, assessing growth changes within existing populations, especially those near species range margins, can increase understanding of climate change impacts. We apply dendrochronological methods to examine recent radial growth of the ecologically similar species Juniperus communis L. and J. virginiana L. growing under the same conditions but at opposite latitudinal range margins. We use moving correlations to analyze changes in relationships between growth and monthly climatic variables, and regional curve standardization to identify trends in growth rate independent of plant age. For J. communis, growth sensitivity to temperature and precipitation shifted earlier in the spring whereas for J. virginiana only temperature sensitivity shifted earlier over the last 50 years. Since 1920, J. virginiana growth displays an upward trend, but J. communis growth shows both increases and decreases. Recent precipitation increase, rather than warming alone, appears to drive the growth trends, but interactions with temperature and vegetation dynamics, instead of range position, likely account for the differences in trends between species. Although these results generally agree with climate change predictions, they also point out potential difficulties in modeling future species ranges based on growth-climate relationships and growth at range margins.
    • Tree-ring dating of historic buildings in Willsboro, northeastern New York, and development of regional chronologies for dendroarchaeology

      Barclay, D.J.; Rayburn, J.A. (Tree-Ring Society, 2014-07)
      Historical timbers have been sampled from buildings at 13 sites in Willsboro, New York, on the west shore of Lake Champlain. Ring-width series from 139 timbers have been successfully crossdated and used to develop tree-ring chronologies for ash (Fraxinus spp.), oak (Quercus spp.), pine (Pinus spp.), eastern hemlock (Tsuga canadensis (L.) Carr.), and spruce (Picea spp.), which collectively span A.D. 1555 to 1878. Tree cutting dates suggest that Windyview Manor was likely built in or soon after 1799, and a barn and farmhouse at the 1812 Homestead were built in or soon after 1812 and 1813, respectively. These dates are all consistent with documentary records for these sites. Aggregate data for the town suggest a shift in wood use for building during the 19th Century, with ash and oak commonly used for large frame timbers from the 1790s to 1820s, and hemlock and spruce dominating from the 1830s to 1860s. Chronologies developed in this project are among the first from historical timbers for northern New York and will facilitate further dendroarchaeological work in the region.
    • Longitudinal variation of ring width, wood density and basal area increment in 26-year-old loblolly pine (Pinus taeda) trees

      Yu, M.; Cheng, X.; He, Z.; Wu, T.; Yin, Z. (Tree-Ring Society, 2014-07)
      Longitudinal variations in select wood quality parameters were examined in 26-year-old loblolly pine trees planted in Anhui Province, China. Wood density and ring width were measured from cross-sections of different heights of merchantable stems. The average ring width decreased from the base to 1.3 m, then increased to the maximum at 7.6 m, and thereafter reduced with stem height. The longitudinal patterns varied with cambial age in ring width. The coefficient of variation in ring widths along the stem height was greater than 21% at the cambial age 5–8 years and 9–12 years, and small variations were observed in other cambial age groups. The average wood density declined from 1.3 m to 7.6 m and then slightly increased with increasing stem height. The wood density showed great variation at different growth stages below 7.6 m, but varied less above 7.6 m. Basal area increment (BAI) gradually increased with increasing ring number (from the pith to the bark) at different stem heights, and markedly reduced after the 22nd ring. These results indicate that the longitudinal variations of wood density, ring width and BAI in loblolly pine are greatly affected by cambial age. The detailed information of the wood properties along stem heights could be useful to wood utilization of loblolly pine.
    • Dating hydrologic and geomorphic change using dendrochronology in Tully Valley, central New York: A summary

      Kappel, W.M. (Tree-Ring Society, 2014-07)
      This report summarizes the results of three case studies where dendrochronology was used to evaluate hydrologic and geomorphic change in parts of Tully Valley, in central New York, over the past 150 years. The case studies evaluate 1) the changes in water quantity and quality in a wetland area several miles north of an area of former solution-brine mining, 2) the development of recent bedrock fractures above former solution brine-mining areas, and 3) the development and timing of landslide movement. The advantage of contemporary dendrochronology is that tree-ring analysis can provide a background of hydrologic and geomorphic change when no direct documentation or data are available.
    • Early days of dendrochronology in the Hudson Valley of New York: Some reminiscences and reflections

      Cook, E.R. (Tree-Ring Society, 2014-07)
      A brief and personal history of the development of dendrochronology in the Hudson Valley of New York in the 1970s and the quantitative reconstruction of climate from tree rings there is provided. Two people stand out in allowing that to happen. Marvin Stokes at the Laboratory of Tree-Ring Research sparked within me a deep and enduring interest in dendrochronology, and Daniel Smiley of Mohonk supported my interest in pursuing tree-ring research in the Shawangunk Mountains through his deep and curious love of its natural environment. The discovery of ancient trees growing in the Shawangunk Mountains, and their use in successfully reconstructing past drought there, truly launched my career as a dendroclimatologist and proved beyond doubt that dendroclimatology and the reconstruction of past climate could be successfully conducted in the northeastern United States.
    • Site and age condition the growth responses to climate and drought of relict Pinus nigrasubsp. salzmanniipopulations in southern Spain

      Navarro-Cerrillo, R.M.; Sánchez-Salguero, R.; Manzanedo, R.D.; Camarero, J.J.; Fernández-Cancio, A. (Tree-Ring Society, 2014-07)
      To assess if tree age may modulate the main climatic drivers of radial growth, two relict Pinus nigra subsp. salzmannii populations (María, most xeric site; Mágina, least xeric site) were sampled in southern Spain near the limits of the species range. Tree-ring width residual chronologies for two age groups (mature trees, age ≤ 100 years (minimum 40 years); old trees, age > 100 years) were built to evaluate their responses to climate by relating them to monthly precipitation and temperature and a drought index (DRI) using correlation and response functions. We found that drought is the main driver of growth of relict P. nigra populations, but differences between sites and age classes were also observed. First, growth in the most xeric site depends on the drought severity during the previous autumn and the spring of the year of tree-ring formation, whereas in the relatively more mesic site growth is mainly enhanced by warm and wet conditions in spring. Second, growth of mature trees responded more to drought severity than that of old trees. Our findings indicate that drought severity will mainly affect growth of relict P. nigra populations dominated by mature trees in xeric sites. This conclusion may also apply to similar mountain Mediterranean conifer relicts.
    • An extractor device for stuck or broken increment borers

      Loader, N.J.; Waterhouse, J.S. (Tree-Ring Society, 2014-07)
      A lightweight, portable device for extracting stuck or broken increment borers is presented and its operation described. The “Decorum” extractor is compact and weighs less than 400 g. It is easily carried in a belt pouch or pocket and is both reliable and easy to operate. The extractor does not require fixed tie points nor does it damage the tree. It offers an effective solution to a widely occurring problem in dendrochronology and forest research.
    • IN MEMORIAM—Won-Kyu Park

      Unknown author (Tree-Ring Society, 2014-07)
    • BOOK REVIEW—Fundamentals of Tree-Ring Research

      Unknown author (Tree-Ring Society, 2014-07)
    • IN MEMORIAM—Elsie Winnifred Downey

      Unknown author (Tree-Ring Society, 2014-07)
    • IN MEMORIAM—James R. McClenahen

      Unknown author (Tree-Ring Society, 2014-07)
    • Dendroclimatic potential of plains cottonwood (Populus deltoidessubsp. monolifera) from the Northern Great Plains, USA

      Edmondson, J.; Friedman, J.; Meko, D.; Touchan, R.; Scott, J.; Edmondson, A. (Tree-Ring Society, 2014-01)
      A new 368-year tree-ring chronology (A.D. 1643–2010) has been developed in western North Dakota using plains cottonwood (Populus deltoides subsp. monilifera) growing on the relatively undisturbed floodplain of the Little Missouri River in the North Unit of Theodore Roosevelt National Park. We document many slow-growing living trees between 150–370 years old that contradict the common understanding that cottonwoods grow fast and die young. In this northern location, cottonwood produces distinct annual rings with dramatic interannual variability that strongly crossdate. The detrended tree-ring chronology is significantly positively correlated with local growing season precipitation and soil moisture conditions (r  =  0.69). This time series shows periods of prolonged low radial tree growth during the known droughts of the instrumental record (e.g. 1931–1939 and 1980–1981) and also during prehistory (e.g. 1816–1823 and 1856–1865) when other paleoclimate studies have documented droughts in this region. Tree rings of cottonwood will be a useful tool to help reconstruct climate, streamflow, and the floodplain history of the Little Missouri River and other northern river systems.
    • Dendrochronological dating of the historic McKenzie Home, Meigs County, Tennessee, USA

      Stachowiak, L.A.; Schneider, E.A.; Rochner, M.L.; Collins, S.A.; Swiney, C.P.; Grissino-Mayer, H.D.; Mackenzie, T.G. (Tree-Ring Society, 2014-01)
      The McKenzie Home is a one-story log structure located in Meigs County, Tennessee. The land tract where the cabin was originally built was purchased by the McKenzie family ca. A.D. 1820 to 1828, which makes the suspected construction date for the home sometime after 1820. Our objective was to date oak (Quercus spp.) cross-sections taken from original logs to accurately determine the year when the trees were cut and therefore when the structure was built. We created a master chronology from measurements taken along 12 radii from five oak sections using program COFECHA to first confirm internal crossdating among the measured radii and then using program ARSTAN to create a floating master chronology. Interactive detrending identified two likely disturbances that affected tree growth on all five oaks and these trends were subsequently removed using 32-year splines. The McKenzie floating chronology was then compared with a composite reference chronology created from four oak chronologies located in Tennessee, Kentucky, and Alabama. An interseries correlation coefficient of 0.412 (n  =  169 years, t  =  5.84, p < 0.0001) was obtained between the floating chronology and the anchored reference chronology, indicating a single year of tree harvesting in A.D. 1876. Cutting dates for the five samples indicate harvesting began in the early part of the growing season in 1876 and lasted until the end of the growing season or possibly into the dormant season of 1876–1877. The graphical and statistical crossdating evidence and cutting dates that confirm 1876 as the year of construction matches historical property and district records, which state the land was purchased by E.G. McKenzie, Sr. from his brother on 1 February 1876. The log structure has since been renamed the “E.G. McKenzie, Sr. Home.”
    • Dendrochronological dating of two tulip poplars on the west lawn of Monticello

      Druckenbrod, D.L.; Chakowski, N. (Tree-Ring Society, 2014-01)
      Two tulip poplars (Liriodendron tulipifera L.) growing at Monticello, the home of Thomas Jefferson, were recently removed because of potential damage to the house; however, their ages were uncertain. Jefferson's writings express his interest in tulip poplars and suggest that he may have planted at least one, but his documents are not conclusive. After the Thomas Jefferson Foundation purchased the property in A.D. 1923, expert opinions on the ages of these trees were divided. This study investigated the ages of both trees (referred to as northwest and southwest). Even though the southwest tree's bole was hollow and decay was present in the northwest tree, usable cross-sections were obtained. The southwest tree's cross-section was from an upper branch, whereas upper and lower cross-sections were extracted from the bole of the northwest tree. Ring widths were crossdated and statistically verified using an oak chronology from Monticello. The innermost rings of the southwest tree dated to A.D. 1852 and those of the upper and lower sections of the northwest tree dated to 1822 and 1808, respectively. These dendrochronological analyses in combination with historical photographs support the conclusion that the northwest tree and likely the southwest tree were Jefferson era, but the evidence for the southwest tree is less certain.
    • Revisiting a small part of the early work of LaMarche and collaborators in South America

      Suarez, M.L. (Tree-Ring Society, 2014-01)
      One of the most extensive dendrochronological field collections in South America was conducted by LaMarche and collaborators from 1973 to 1978. However, no robust chronologies had been developed from these species and/or sites because there were not enough samples collected, or simply because the materials were never processed. Here, I report on results from a re-examination of all Nothofagus dombeyi samples collected during LaMarche and collaborators' field sampling in South America. A tree-ring chronology was developed for the Alto Vilches site in Chile. For the other sites sampled by LaMarche and collaborators, there were not enough samples, or series were not sufficiently long to build a chronology or to provide adequate information about tree growth. The Alto Vilches (VIL) chronology extends into the early 1800s, and shows high mean sensitivity values and a strong common signal. As expected, the VIL chronology evidenced narrow rings for several years that correspond with low precipitation periods in Patagonia. Making available the information kept in unprocessed tree-ring samples reinforces the dendrochronological potential of this species and strengthens chronology networks developed for ecological studies in northern Patagonia. Finally, this study honors the initial work of LaMarche and collaborators and provides closure to a small part of it.