Title

Dendroecological indicators of historical responses of pines to water and nutrient availability on a superficial aquifer in south-western Australia

Document Type

Journal Article

Faculty

Faculty of Computing, Health and Science

School

School of Natural Sciences / Centre for Ecosystem Management

RAS ID

14421

Comments

This article was originally published as: Stock, W. D., Bourke, L. J., & Froend, R. H. (2012). Dendroecological indicators of historical responses of pines to water and nutrient availability on a superficial aquifer in south-western Australia. Forest Ecology and Management, 264, 108-114.

Abstract

This study investigated the hypothesis that the plantations of Pinus pinaster Ait. growing on the unconfined Gnangara aquifer do so independently of groundwater availability. To test the hypothesis we related annual growth (tree-ring widths and basal area increment (BAI)) with physiological attributes associated with water (water use efficiency (WUE) from δ 13C natural abundance values) and nutrient availability (δ 15N natural abundance values) of trees with shallow (20mbgl) access to ground-water. Annual growth responses were also related to annual climatic variability (growth season rainfall) and silvicultural treatments (thinning, fertilisation and forest floor fuel reduction burning) to assess the relative importance of each on annual tree-ring growth. There is a strong influence of P. pinaster tree age on ring widths and BAI during the establishment phase. Thereafter the effects of the various management treatments (stand thinning, P fertilisation and forest floor burning) all interact to various degrees on ring width and BAI ranges. Stand thinning appears to have the greatest effect on ring growth which is clearly evident for at least 3-4years after the treatment. The stable isotope composition of the tree rings also showed a clear effect of stand thinning at both the shallow and deep groundwater sites and thinning dominates any small effects on water-use efficiency (WUE) caused by forest floor burning and P fertilisation. Thinning also had a major impact leading to increases in ring δ 15N values of 2‰ or more. Multiple regression models developed for P. pinaster tree-ring width growth and BAI had a high predictive power and they always included rainfall as the main factor. Models developed for ring isotopic indicators were more variable and less predictive than those for the ring growth and BAI with no significant models emerging for the shallow depth to groundwater site. Our results show that by using tree-ring growth responses together with climate proxies, such as ring isotope chemistry, we are able to separate the relative influence of climate and other factors which control growth. The overriding effect of rainfall in the models at both depths to groundwater suggests that the pine plantations growing on the Gnangara aquifer do not rely on the direct use of the groundwater resource for growth but rather that they reduce recharge of the superficial Gnangara aquifer through their efficient use of rainfall derived soil water.

DOI

10.1016/j.foreco.2011.09.033

Access Rights

Not open access

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