Science. 1984 May 4;224(4648):494-7. doi: 10.1126/science.224.4648.494.
Annual growth rings from short-leaf pine trees in the Great Smoky Mountains National Park show suppressed growth and increased iron content between 1863 and 1912, a period of smelting activity and large sulfur dioxide releases at Copperhill, Tennessee, 88 kilometers upwind. Similar growth suppression and increases of iron and other metals were found in rings formed in the past 20 to 25 years, a period when regional fossil fuel combustion emissions increased about 200 percent. Metals concentrations in phloem and cambium are high, but whether they exceed toxic thresholds for these tissues is not known.
大烟山国家公园的短叶松的年轮显示,在 1863 年至 1912 年间,田纳西州科珀希尔的冶炼活动和大量二氧化硫排放导致生长受到抑制,铁含量增加,该地位于上风向 88 公里处。在过去 20 到 25 年形成的年轮中也发现了类似的生长抑制以及铁和其他金属的增加,这一时期的区域化石燃料燃烧排放量增加了约 200%。韧皮部和形成层中的金属浓度很高,但它们是否超过这些组织的毒性阈值尚不清楚。