Risk David, Kellman Lisa, Moroni Martin
Department of Earth Sciences, St. Francis Xavier University, Antigonish, Nova Scotia, Canada.
Isotopes Environ Health Stud. 2009 Sep;45(3):220-30. doi: 10.1080/10256010903083920.
Wholistic isotopic studies provide a necessary foundation on which to build conceptual understanding of ecosystem development processes and provide the basis for further isotopic studies at a site or within an ecophysiological region. This study seeks to broadly characterise delta(13)C spatial variability and spatial patterns within soils and canopy tissues at five forest research sites in eastern Canada. We observe consistent and predictable patterns of leaf delta(13)C variation within trees and a consistent offset between woody and leafy tree tissues. Patterns are similar for both hardwoods and softwoods, but overall hardwoods had canopies that were more depleted in (13)C. Soil carbon delta(13)C enrichment occurred with depth and appeared to vary according to site soil texture. Upper soil delta(13)C was intermediate between leaves and woody tissues, whereas deeper soil values suggested important contributions from more enriched tree tissues, such as persistent woody debris and possibly roots. The relationship between aboveground and belowground signatures suggests functional or developmental differences between study sites.
整体同位素研究为构建对生态系统发育过程的概念理解提供了必要的基础,并为在一个地点或一个生态生理区域内进行进一步的同位素研究提供了依据。本研究旨在广泛描述加拿大东部五个森林研究地点土壤和冠层组织中δ(13)C的空间变异性和空间模式。我们观察到树木叶片δ(13)C变化存在一致且可预测的模式,以及木本和叶状树木组织之间存在一致的偏移。硬木和软木的模式相似,但总体而言硬木的冠层(13)C含量更低。土壤碳δ(13)C随深度增加而富集,且似乎因地点土壤质地而异。上层土壤δ(13)C介于叶片和木本组织之间,而深层土壤值表明来自更富集的树木组织(如持久的木质残体以及可能的根系)有重要贡献。地上和地下特征之间的关系表明研究地点之间存在功能或发育差异。