Ring width, climate and wood density relationships in two long-lived Tasmanian tree species

被引:14
作者
Allen, Kathryn [1 ]
Drew, David M. [2 ]
Downes, Geoffrey M. [2 ]
Evans, Robert [3 ]
Baker, Patrick [1 ]
Grose, Michael
机构
[1] Monash Univ, Sch Biol Sci, Clayton, Vic 3800, Australia
[2] CSIRO CSE Hobart, Hobart, Tas 7005, Australia
[3] CSIRO Sir Ian Work Labs, Clayton, Vic 3800, Australia
关键词
Wood density; Dendroclimatology; Tasmania; Australia; Pencil Pine; Celery Top Pine; MAXIMUM LATEWOOD DENSITY; TRANSVERSE DIMENSIONS; NORTHERN-HEMISPHERE; RAPID MEASUREMENT; TIME-SERIES; TEMPERATURE; DENDROCLIMATOLOGY;
D O I
10.1016/j.dendro.2010.12.006
中图分类号
S7 [林业];
学科分类号
0829 ; 0907 ;
摘要
The great majority of dendroclimatological work in Australia has thus far relied on ring-width chronologies only. We report novel results from a pilot study that show the potential to develop density-based climatically sensitive chronologies from two long-lived conifers endemic to Tasmania: Pencil Pine and Celery Top Pine. Cross-dating of average ring density profiles within each of the two sites examined was comparable with the better replicated ring-width chronologies from the sites. Cross-dating potential for maximum density was also indicated. Correlations between density and climate for both species were stronger and more persistent across a window of several months than correlations between ring width and climate. These stronger correlations suggest that temperature reconstructions based on average density may be possible. The ability to develop high resolution temperature-sensitive chronologies would allow for spatial comparisons across regions such as Tasmania that are affected by multiple broad-scale climate systems. A particularly novel result was the finding that maximum density was significantly related to stream-flow at the end of the growing season. Further work is required to assess the potential to reconstruct temperature, and to reconstruct stream-flow for important Tasmanian catchments over the past 500-800 years. (C) 2012 Istituto Italiano di Dendrocronologia. Published by Elsevier GmbH. All rights reserved.
引用
收藏
页码:167 / 177
页数:11
相关论文
共 44 条
[1]   A structural time series approach to the reconstruction of Tasmanian maximum temperatures [J].
Allen, K ;
Francey, R ;
Michael, K ;
Nunez, M .
ENVIRONMENTAL MODELLING & SOFTWARE, 1999, 14 (04) :261-274
[2]   The potential to reconstruct broadscale climate indices associated with southeast Australian droughts from Athrotaxis species, Tasmania [J].
Allen, K. J. ;
Ogden, J. ;
Buckley, B. M. ;
Cook, E. R. ;
Baker, P. J. .
CLIMATE DYNAMICS, 2011, 37 (9-10) :1799-1821
[3]  
Allen K. J., 1998, DENDROCLIMATOLOGICAL
[4]   The climatic response of Phyllocladus aspleniifolius (Labill.) Hook. f in Tasmania [J].
Allen, KJ ;
Cook, ER ;
Francey, RJ ;
Michael, K .
JOURNAL OF BIOGEOGRAPHY, 2001, 28 (03) :305-316
[5]   Effects of environmental factors on wood formation in larch (Larix sibirica Ldb.) stems [J].
Antonova, GF ;
Stasova, VV .
TREES-STRUCTURE AND FUNCTION, 1997, 11 (08) :462-468
[6]   Dendroclimatological reconstructions in South America: A review [J].
Boninsegna, J. A. ;
Argollo, J. ;
Aravena, J. C. ;
Barichivich, J. ;
Christie, D. ;
Ferrero, M. E. ;
Lara, A. ;
Le Quesne, C. ;
Luckman, B. H. ;
Masiokas, M. ;
Morales, M. ;
Oliveira, J. M. ;
Roig, F. ;
Srur, A. ;
Villalba, R. .
PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY, 2009, 281 (3-4) :210-228
[7]   Intra-annual variations in climate influence growth and wood density of Norway spruce [J].
Bouriaud, O ;
Leban, JM ;
Bert, D ;
Deleuze, C .
TREE PHYSIOLOGY, 2005, 25 (06) :651-660
[8]   Tree-ring width and density data around the Northern Hemisphere: Part 2, spatio-temporal variability and associated climate patterns [J].
Briffa, KR ;
Osborn, TJ ;
Schweingruber, FH ;
Jones, PD ;
Shiyatov, SG ;
Vaganov, EA .
HOLOCENE, 2002, 12 (06) :759-789
[9]   A changing temperature response with elevation for Lagarostrobos franklinii in Tasmania, Australia [J].
Buckley, BM ;
Cook, ER ;
Peterson, MJ ;
Barbetti, M .
CLIMATIC CHANGE, 1997, 36 (3-4) :477-498
[10]  
Clapham D, 2001, TREE PHYSIOL SER, V1, P187