Dendrochronology of bristlecone pine, Pinus longaeva
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Cited by (4)
Reviewing the Mid-First Millennium BC <sup>14</sup>C "warp" using <sup>14</sup>C/bristlecone pine data
2013, Nuclear Instruments and Methods in Physics Research, Section B: Beam Interactions with Materials and AtomsCitation Excerpt :In 7 instances, we undertook duplicate measurements of the same decadal wood sample. The tree ring-dated ages of these samples had been determined in the 1960s by the late C. Wesley Ferguson of the Laboratory of Tree Ring Research (LTRR), University of Arizona [5,6]. All of these samples had been collected at an elevation above 3000 meters in the White Mountains of east central California (USA).
An annually resolved bristlecone pine carbon isotope chronology for the last millennium
2011, Quaternary ResearchCitation Excerpt :In dry, hot environments trees will narrow their stomatal openings to save water, so ci is commonly limited by moisture availability and vapor pressure deficit, giving strong correlations with rainfall and drought severity indices (Treydte et al., 2001; Wils et al., 2010). Bristlecone pines from the White Mountains of California (Pinus longaeva, D.K Bailey) provide remarkable tree-ring records, extending back thousands of years, largely explored through ring width measurements (LaMarche, 1974; Ferguson, 1979; Salzer et al., 2009). In addition there have been several studies that have used stable isotopes to explore the bristlecone pine record of the White Mountains, (Long et al., 1987; Leavitt and Long, 1992; Feng and Epstein, 1994; Leavitt, 1994; Tang et al., 1999).
Monumental tree trunks as indicators of forest degradation in southern Brazil
2019, Ciencia FlorestalScience-based dating in archaeology
2014, Science-Based Dating in Archaeology