δ¹³C values of soil organic carbon and their use in documenting vegetation change in a subtropical savanna ecosystem

详细信息    查看全文

• 作者：Boutton ; Thomas W. ; Archer ; Steven R. ; Midwood ; Andrew J. ; et. al.
• 关键词：C₃ plants ; C₄ plants ; ¹⁴C-dating ; savannas ; soil organic matter ; succession
• 刊名：Geoderma
• 出版年：1998
• 出版时间：February, 1998
• 年：1998
• 卷：82
• 期：1-3
• 页码：5-41
• 全文大小：1.04 M

文摘

Plants with C₃, C₄, and CAM photosynthesis have unique δ¹³C values which are not altered significantly during decomposition and soil organic matter formation. Consequently, δ¹³C values of soil organic carbon reflect the relative contribution of plant species with C₃, C₄, and CAM photosynthetic pathways to community net primary productivity, and have been utilized to document vegetation change, to quantify soil organic matter turnover, and to refine our understanding of earth–atmosphere–biosphere interactions. Here, we review the basis of this methodology, and illustrate its use as a tool for studying grass–woody plant dynamics in a savanna ecosystem. In the Rio Grande Plains of southern Texas, C₄ grasslands and savannas have been largely replaced by C₃ subtropical thorn woodlands dominated by Prosopis glandulosa. We used δ¹³C values of soil organic matter, above- and belowground plant biomass, and litter in conjunction with radiocarbon dating and dendrochronology to test the hypotheses that: (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 expanded up-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, δ¹³C values of vegetation (−20‰) were lower than those of soil organic matter (−17‰), suggesting increased C₃ forb abundance in response to long-term, heavy grazing (herbaceous retrogression). In wooded landscape elements, δ¹³C values of current organic matter inputs were characteristic of C₃ plants (−28 to −25‰), while those of the associated soil organic matter were typically −20 to −15‰. These δ¹³C 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 δ¹³C values of organic carbon associated with fine and coarse clay fractions (−18 to −14‰), probably a consequence of the slow organic carbon turnover rates in those soil fractions. When δ¹³C values of soil organic carbon were evaluated in conjunction with radiocarbon measurements of that same carbon, it appeared that herbaceous retrogression and a shift from C₄ grassland to C₃ woodland occurred recently, probably within the last 50–100 years. Demographic characteristics of the dominant tree species corroborated the δ¹³C and ¹⁴C evidence, and indicated widespread establishment of P. glandulosa and associated shrubs over the past 100 years. Together, these data provide direct, spatially explicit evidence that vegetation change has occurred recently across the entire landscape at this site. Environmental conditions where C₃, C₄, and CAM plants coexist (e.g., dry, alkaline soils) generally do not favor the preservation of pollen and phytoliths, and these same areas usually lack historical records of vegetation change. Consequently, vegetation dynamics have been difficult to quantify in grasslands, savannas, and woodlands. However, our results demonstrate clearly that δ¹³C values of soil organic matter afford a direct and powerful technique for reconstructing vegetation change in these areas.