首页> 外文期刊>Geoderma: An International Journal of Soil Science >delta13C values of soil organic carbon and their use in documenting vegetation change in a subtropical savanna ecosystem
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delta13C values of soil organic carbon and their use in documenting vegetation change in a subtropical savanna ecosystem

机译:亚热带稀树草原生态系统中土壤有机碳的delta13C值及其在记录植被变化中的用途

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In southern Texas, USA, C4 grasslands and savannas have been largely replaced by C3 subtropical thorn woodlands dominated by Prosopis glandulosa. delta13C values of soil organic matter, above- and below-ground plant biomass, and litter were used with radiocarbon dating and dendrochronology to test whether: (1) C3 Prosopis groves in uplands and C3 Prosopis woodlands in low-lying drainages have been long-term components of the landscape; and (2) Prosopis woodlands of low-lying drainages have expandedup-slope since Anglo-European settlement. Current organic matter inputs were not in isotopic equilibrium with soil organic carbon in any of the patch types sampled. In upland grasslands, delta13C values of vegetation (-20o/oo) were lower than those of soil organic matter (- 17o/oo), suggesting increased C3 forb abundance in response to long-term, heavy grazing (herbaceous retrogression). In wooded landscape elements, delta13C values of current organic matter inputs were characteristic of C3 plants (-28to -25o/oo), while those of the associated soil organic matter were typically -20 to -15o/oo. These delta13C values indicate that woodlands, groves, and shrub clusters dominated almost exclusively by C3 plants now occupy sites once dominated by C4 grasses. A particularly strong memory of the C4 grasslands that once occupied these sites was recorded in the delta13C values of organic carbon associated with fine and coarse clay fractions (-18 to -14o/oo). Herbaceous retrogression and a shift from C4 grassland to C3 woodland probably occurred within the last 50-100 years. Demographic characteristics of the dominant tree species corroborated the delta13C and 14C evidence, and indicated widespread establishment of P. glandulosa and associated shrubs over the past 100 years. The results show that delta13C values of soil organic matter afford a direct and powerful technique for reconstructing vegetation change in these areas.
机译:在美国得克萨斯州南部,C4草原和热带稀树草原已被Prosopis glandulosa为主的C3亚热带刺林取代。将土壤有机质,地上和地下植物生物量以及凋落物的delta13C值与放射性碳测年和树轮年代学一起使用,以测试是否:(1)高地流域的C3 Prosopis树林和低洼排水区的C3 Prosopis林地已经很久了。景观的术语组成; (2)自盎格鲁-欧洲定居以来,低洼排水区的Prosopis林地已向上倾斜。在任何采样的斑块类型中,当前的有机物输入与土壤有机碳都不处于同位素平衡状态。在高地草原上,植被的δ13C值(-20o / oo)低于土壤有机质的δ13C值(-17o / oo),这表明长期重度放牧(草体退化)后,C3的丰度增加。在树木繁茂的景观元素中,当前有机物输入的delta13C值是C3植物的特征(-28至-25o / oo),而与之相关的土壤有机物的典型值是-20至-15o / oo。这些delta13C值表明,几乎完全由C3植物主导的林地,树林和灌木丛现在占据了曾经由C4草主导的场所。 C4草原曾经占据了这些地点,对它们的记忆特别强烈,记录在有机碳的δ13C值中,该值与精细和粗糙粘土组分(-18至-14o / oo)有关。在最近的50至100年中,可能发生了草本倒退和从C4草原向C3树林转变。优势树种的人口统计特征证实了delta13C和14C的证据,并表明在过去100年中广泛建立了P. glandulosa和相关灌木。结果表明,土壤有机质的δ13C值为重建这些地区的植被变化提供了直接而有力的技术。

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