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Large old trees influence patterns of delta C-13 and delta N-15 in forests.

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Large old trees influence patterns of delta C-13 and delta N-15 in forests. / Weber, Pascale; Bol, Roland; Dixon, Liz et al.
In: Rapid Communications in Mass Spectrometry, Vol. 22, No. 11, 15.06.2008, p. 1627-1630.

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Harvard

Weber, P, Bol, R, Dixon, L & Bardgett, RD 2008, 'Large old trees influence patterns of delta C-13 and delta N-15 in forests.', Rapid Communications in Mass Spectrometry, vol. 22, no. 11, pp. 1627-1630. https://doi.org/10.1002/rcm.3433

APA

Weber, P., Bol, R., Dixon, L., & Bardgett, R. D. (2008). Large old trees influence patterns of delta C-13 and delta N-15 in forests. Rapid Communications in Mass Spectrometry, 22(11), 1627-1630. https://doi.org/10.1002/rcm.3433

Vancouver

Weber P, Bol R, Dixon L, Bardgett RD. Large old trees influence patterns of delta C-13 and delta N-15 in forests. Rapid Communications in Mass Spectrometry. 2008 Jun 15;22(11):1627-1630. doi: 10.1002/rcm.3433

Author

Weber, Pascale ; Bol, Roland ; Dixon, Liz et al. / Large old trees influence patterns of delta C-13 and delta N-15 in forests. In: Rapid Communications in Mass Spectrometry. 2008 ; Vol. 22, No. 11. pp. 1627-1630.

Bibtex

@article{953b7696b0744fb4828ce390143ba6fb,
title = "Large old trees influence patterns of delta C-13 and delta N-15 in forests.",
abstract = "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 (13C) and nitrogen (15N) 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 L.) trees, to determine the trees' influence on below-ground properties. We also measured 15N and 13C 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 15N 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 15N-depleted litter below the tree crown. In contrast, the soil 13C did not change along the gradient of tree influence. Distance-related trends, although weak, were visible in the wood 15N and 13C of regenerating trees. Moreover, the wood 15N 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.",
author = "Pascale Weber and Roland Bol and Liz Dixon and Bardgett, {Richard D.}",
year = "2008",
month = jun,
day = "15",
doi = "10.1002/rcm.3433",
language = "English",
volume = "22",
pages = "1627--1630",
journal = "Rapid Communications in Mass Spectrometry",
issn = "0951-4198",
publisher = "John Wiley and Sons Ltd",
number = "11",

}

RIS

TY - JOUR

T1 - Large old trees influence patterns of delta C-13 and delta N-15 in forests.

AU - Weber, Pascale

AU - Bol, Roland

AU - Dixon, Liz

AU - Bardgett, Richard D.

PY - 2008/6/15

Y1 - 2008/6/15

N2 - 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 (13C) and nitrogen (15N) 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 L.) trees, to determine the trees' influence on below-ground properties. We also measured 15N and 13C 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 15N 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 15N-depleted litter below the tree crown. In contrast, the soil 13C did not change along the gradient of tree influence. Distance-related trends, although weak, were visible in the wood 15N and 13C of regenerating trees. Moreover, the wood 15N 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.

AB - 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 (13C) and nitrogen (15N) 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 L.) trees, to determine the trees' influence on below-ground properties. We also measured 15N and 13C 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 15N 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 15N-depleted litter below the tree crown. In contrast, the soil 13C did not change along the gradient of tree influence. Distance-related trends, although weak, were visible in the wood 15N and 13C of regenerating trees. Moreover, the wood 15N 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.

U2 - 10.1002/rcm.3433

DO - 10.1002/rcm.3433

M3 - Journal article

VL - 22

SP - 1627

EP - 1630

JO - Rapid Communications in Mass Spectrometry

JF - Rapid Communications in Mass Spectrometry

SN - 0951-4198

IS - 11

ER -