McIntyre Patrick J, Thorne James H, Dolanc Christopher R, Flint Alan L, Flint Lorraine E, Kelly Maggi, Ackerly David D
Berkeley Initiative for Global Change Biology and Department of Integrative Biology, University of California, Berkeley, CA 94720;
Information Center for the Environment, Department of Environmental Science and Policy, University of California, Davis, CA 95616;
Proc Natl Acad Sci U S A. 2015 Feb 3;112(5):1458-63. doi: 10.1073/pnas.1410186112. Epub 2015 Jan 20.
We document changes in forest structure between historical (1930s) and contemporary (2000s) surveys of California vegetation through comparisons of tree abundance and size across the state and within several ecoregions. Across California, tree density in forested regions increased by 30% between the two time periods, whereas forest biomass in the same regions declined, as indicated by a 19% reduction in basal area. These changes reflect a demographic shift in forest structure: larger trees (>61 cm diameter at breast height) have declined, whereas smaller trees (<30 cm) have increased. Large tree declines were found in all surveyed regions of California, whereas small tree increases were found in every region except the south and central coast. Large tree declines were more severe in areas experiencing greater increases in climatic water deficit since the 1930s, based on a hydrologic model of water balance for historical climates through the 20th century. Forest composition in California in the last century has also shifted toward increased dominance by oaks relative to pines, a pattern consistent with warming and increased water stress, and also with paleohistoric shifts in vegetation in California over the last 150,000 y.
通过比较加州全州及几个生态区域内树木的丰度和大小,我们记录了从历史时期(20世纪30年代)到当代(21世纪00年代)加州植被调查中森林结构的变化。在整个加州,两个时期之间森林地区的树木密度增加了30%,而同一地区的森林生物量却下降了,胸径断面积减少19%就表明了这一点。这些变化反映了森林结构的人口统计学转变:大树(胸径>61厘米)数量减少,而小树(<30厘米)数量增加。在加州所有被调查地区都发现了大树数量的减少,而除了南海岸和中部海岸之外的每个地区都发现了小树数量的增加。根据20世纪历史气候水平衡的水文模型,自20世纪30年代以来,气候水分亏缺增加幅度更大的地区大树数量减少更为严重。上个世纪加州的森林组成也已向橡树相对于松树的优势增加转变,这一模式与气候变暖和水分胁迫增加相一致,也与过去15万年加州植被的古历史变化一致。