Large old trees influence patterns of δ13C and δ15N in forests

被引:10
|
作者
Weber, Pascale [1 ,3 ]
Bol, Roland [2 ]
Dixon, Liz [2 ]
Bardgett, Richard D. [3 ]
机构
[1] Swiss Fed Res Inst WSL, CH-8903 Birmensdorf, Switzerland
[2] IGER, N Wyke Res Stn, Okehampton EX20 2SB, England
[3] Univ Lancaster, Soil & Ecosyst Ecol Lab, Lancaster LA1 4YQ, England
基金
英国生物技术与生命科学研究理事会;
关键词
D O I
10.1002/rcm.3433
中图分类号
Q5 [生物化学];
学科分类号
071010 ; 081704 ;
摘要
Large old trees are the dominant primary producers of native pine forest, but their influence on spatial patterns of soil properties and potential feedback to tree regeneration in their neighbourhood is poorly understood. We measured stable isotopes of carbon (delta C-13) and nitrogen (delta N-15) in soil and litter taken from three zones of influence (inner, middle and outer zone) around the trunk of freestanding old Scots pine (Pinus sylvestris W trees, to determine the trees' influence on below-ground properties. We also measured delta N-15 and delta C-13 in wood cores extracted from the old trees and from regenerating trees growing within their three zones of influence. We found a significant and positive gradient in Soil delta N-15 from the inner zone, nearest to the tree centre, to the outer zone beyond the tree crown. This was probably caused by the higher input of N-15-depleted litter below the tree crown. In contrast, the Soil delta C-13 did not change along the gradient of tree influence. Distance-related trends, although weak, were visible in the wood delta N-15 and delta C-13 of regenerating trees. Moreover, the wood delta N-15 of small trees showed a weak negative relationship with soil N content in the relevant zone of influence. Our results indicate that large old trees control below-ground conditions in their immediate surroundings, and that stable isotopes might act as markers for the spatial and temporal extent of these below-ground effects. Copyright (C) 2008 John Wiley & Sons, Ltd.
引用
收藏
页码:1627 / 1630
页数:4
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