• In Memoriam- Henry N. Michael

      Tree-Ring Society, 2006
    • In Memoriam- Robert E. Bell

      Dean, Jeffrey S. (Tree-Ring Society, 2006)
    • Lost and Found: the Bristlecone Pine Collection

      Hallman, Christine; Harlan, Tom; Arnott, Howard; Laboratory of Tree-Ring Research, University of Arizona, Tucson, AZ 85721; The Center for Electron Microscopy, University of Texas at Arlington, Arlington, TX 76019 (Tree-Ring Society, 2006)
    • Root-Zone Hydrology: Why Bald-Cypress in Flooded Wetlands Grow More When It Rains

      Davidson, Gregg R.; Laine, Brian C.; Galicki, Stanley J.; Threlkeld, Stephen T.; University of Mississippi, Department of Geology and Geological Engineering, University, MS 38677; Millsaps College, Jackson, MS 39210; University of Mississippi, Department of Biology, University, MS 38677 (Tree-Ring Society, 2006)
      Bald cypress (Taxodium distichum) is known to respond to increases in precipitation with increased radial growth even when rooted in continuously saturated sediments where water is not a growth-limiting factor. Measurements of δ¹⁸O, Cl⁻, ³H and hydraulic head in surface water and shallow groundwater in an oxbow lake-wetland in northern Mississippi show that rapid downward flow of surface water into the root zone is initiated only after precipitation-induced increases in surface water depth exceed a threshold value. Rapid flow of surface water through the root zone has the potential to introduce oxygen to sediments that would otherwise be anoxic, facilitating nutrient uptake and growth. Climatic reconstruction using tree rings from bald cypress in this environment appears possible because increases in precipitation generally correlate well with increases in water level, which in turn enhances the delivery of oxygenated water to the roots.