Leaf metabolic and morphological responses of dwarf willow (Salix herbacea) in the sub-arctic to the past 9000 years of global environmental change
Leaf metabolic and morphological responses of dwarf willow (Salix herbacea) in the sub-arctic to the past 9000 years of global environmental change
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DOI:
10.1046/j.1469-8137.2000.00582.x
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发表时间:
2000-02-01
期刊:
影响因子:
9.4
通讯作者:
Rundgren, M
中科院分区:
文献类型:
--
作者:
Beerling, DJ;Rundgren, M
Ice-core records of the concentration of atmospheric CO2 and its stable isotope ratio (delta(13)C(a)) have shown that the global C cycle has not remained in steady-state over the past 11000 yr, implying a possible change in vegetation activity over this period. Here we evaluated the ecophysiological responses of the dwarf willow (Salix herbacea) over the past 9000 yr by measuring the stable carbon isotope composition and stomatal characters of a unique, well dated, high-latitude (68 degrees N) sub-fossil leaf sequence. After correction for corresponding changes in delta(13)C(a), a 9000- yr record of variations in the ratio of intercellular (c(i)) to atmospheric (c(a)) CO2 concentration was established. Intercellular: atmospheric CO2 concentration ratios provide a time-integrated indicator of the set-point of leaf gas exchange, and the historical variations revealed in this record have been interpreted as an impact of environmental changes on leaf gas exchange. The sequence shows a progressive fall in c(i)/c(a) 9000-3000 yr BP as well as the climatic effects of the Medieval Warm Period, the Little Ice Age and the post-industrial CO2 rise. Leaf stomatal index (proportion of epidermal cells as stomata), but not stomatal density, was significantly (P