Abstract
Callitris is Australia’s most successful and drought tolerant conifer genus. Callitris species are distributed across a huge geographical range from rainforest to arid zones, and hence they provide a rare opportunity to view plant growth trends across the continent. Here, we make a continental-scale examination of how climate influences basal diameter growth in Callitris. We sampled a total of five species but focused effort (23 of 28 samples) on the most widespread species, C. columellaris. Cores from a total of 23 trees were sampled from 15 sites that spanned a gradient in mean annual rainfall from 225 to 2117 mm and mean annual temperature from 11.5 to 28.2°C. Ring production is not annual across much of the distribution of the genus, so 14C-AMS dating was used to establish the frequency of ring production for each core. Ring width, tracheid lumen diameter and number of tracheids per ring were also measured on each core. Ring production was close to annual at mesic sites with reliable alternation of rainfall or temperature regimes but was more erratic elsewhere. For C. columellaris, ring width significantly increased with mean annual rainfall (r2 = 0.49) as a result of wider and more tracheids per ring. For this species tracheid lumen diameter was correlated with annual rainfall (r2 = 0.61), with a threefold increase from the driest to the wettest sites, lending support to the hypothesis that conifers growing at drier sites will have narrow lumen diameters to maximise mechanical strength of the xylem.
Similar content being viewed by others
References
Ash J (1983) Tree rings in tropical Callitris macleayana F. Muell Aust J Bot 31:277–281
Baker PJ, Palmer JG, D’Arrigo R (2008) The dendrochronology of Callitris intratropica in northern Australia: annual ring structure, chronology development and climate correlations. Aust J Bot 56:311–320
Banks J, Pulsford I (2001) Dendrochronology of Australian cypress pines. In: Dargavel J, Hart D, Libbis B (eds) Perfumed pineries. Environmental history of Australia’s Callitris forests. Centre for Resource and Environmental Studies, Australian National University, Canberra, pp 30–38
Biondi F, Strachan SDJ, Mensing S, Piovesan G (2007) Radiocarbon analysis confirms the annual nature of sagebrush growth rings. Radiocarbon 49:1231–1240
Bowman DMJS, Harris S (1995) Conifers of Australia’s dry forests and open woodlands. In: Enright NJ, Hill RS (eds) Ecology of the southern conifers. Melbourne University Press, Melbourne, pp 252–270
Bowman DMJS, Panton WJ (1993) Decline of Callitris intratropica R.T. Baker & H.G. Smith in the Northern Territory: implications for pre- and post-European colonization fire regimes. J Biogeogr 20: 373–381
Bowman DMJS, Prior LD (2005) Why do evergreen trees dominate the Australian seasonal tropics? Aust J Bot 53:379–399
Brienen RJW, Zuidema PA (2005) Relating tree growth to rainfall in Bolivian rain forests: a test for six species using tree ring analysis. Oecologia 146:1–12
Brodribb TJ, Bowman DJMS, Nichols S, Delzon S, Burlett R (2010) Xylem function and growth rate interact to determine recovery rates after exposure to extreme water deficit. New Phytol 188:533–542
Bureau of Meteorology (2010a) Climate data online. http://www.bom.gov.au/climate/data/index.shtml. Accessed 29 Sept 2010
Bureau of Meteorology (2010b) Australian rainfall and surface temperature data. http://www.bom.gov.au/cgi-bin/silo/cli_var/area_timeseries.pl. Accessed 29 Sept 2010
Dulamsuren C, Hauck M, Leuschner C (2010) Recent drought stress leads to growth reductions in Larix sibirica in the western Khentey, Mongolia. Glob Change Biol 16:3024–3035
Enquist BJ, Leffler AJ (2001) Long-term tree ring chronologies from sympatric tropical dry-forest trees: individualistic responses to climatic variation. J Trop Ecol 17:41–60
Farjon A (2005) A monograph of Cupressaceae and Sciadopitys. Royal Botanic Gardens, Kew
Fichtler E, Clark DA, Worbes M (2003) Age and long-term growth of trees in an old-growth tropical rain forest, based on analyses of tree rings and C-14. Biotropica 35:306–317
Fink D, Hotchkis M, Hua Q, Jacobsen G, Smith AM, Zoppi U, Child D, Mifsud C, van der Gaast H, Williams A, Williams M (2004) The ANTARES AMS facility at ANSTO. Nucl Instrum Meth B 223–224:109–115
Fritts HC (2001) Tree rings and climate. The Blackburn Press, Caldwell
Horne R (1990) Stand height response following variable spacing of wheatfield white cypress pine regeneration in New South Wales. Aust For 53:47–54
Hua Q (2009) Radiocarbon: a chronological tool for the recent past. Quat Geochronol 4:378–390
Hua Q, Barbetti M (2004) Review of tropospheric bomb 14C data for carbon cycle modeling and age calibration purposes. Radiocarbon 46:1273–1298
Hua Q, Barbetti M, Worbes M, Head J, Levchenko VA (1999) Review of radiocarbon data from atmospheric and tree ring samples for the period 1945–1997 AD. IAWA J 20:261–283
Hua Q, Barbetti M, Zoppi U, Fink D, Watanasak M, Jacobsen GE (2004) Radiocarbon in tropical tree rings during the Little Ice Age. Nucl Instrum Method B 223–224:489–494
Kottek M, Grieser J, Beck C, Rudolf B, Rubel F (2006) World map of the Koppen–Geiger climate classification updated. Meteorol Z 15:259–263
La Marche VC, Holmes RL, Dunwiddie PW, Drew LG (1979) Tree-ring chronologies of the southern hemisphere. Australia Laboratory of Tree-Ring Research, University of Arizona, Tucson
Lange RT (1965) Growth ring characteristics in an arid zone conifer. Trans Roy Soc South Aust 89:133–137
Martín JA, Esteban LG, de Palacios P, Garcia Fernandez F (2010) Variation in wood anatomical traits of Pinus sylvestris L. between Spanish regions of provenance. Trees 24:1017–1028
Pearson S, Hua Q, Allen K, Bowman DJMS (2011) Validating putatively cross-dated Callitris tree-ring chronologies using bomb-pulse radiocarbon analysis. Aust J Bot 59:7–17
Pittermann J, Sperry JS, Wheeler JK, Hacke UG, Sikkema EH (2006) Mechanical reinforcement of tracheids compromises the hydraulic efficiency of conifer xylem. Plant Cell Environ 29:1618–1628
Prior LD, McCaw WL, Grierson PF, Murphy BP, Bowman DMJS (2011) Population structures of the widespread Australian conifer Callitris columellaris are a bio-indicator of continental environmental change. For Ecol Manag. doi:10.1016/j.foreco.2011.03.030
Reimer P, Reimer RW (2004) CALIBomb radiocarbon calibration. Interactive program. http://intcal.qub.ac.uk/CALIBomb/frameset.html. Accessed 10 Dec 2010
Reimer PJ, Brown TA, Reimer RW (2004) Discussion: reporting and calibration of post-bomb C-14 data. Radiocarbon 46:1299–1304
Rossi S, Simard S, Rathgeber CBK, Deslauriers A, De Zan C (2009) Effects of a 20-day-long dry period on cambial and apical meristem growth in Abies balsamea seedlings. Trees 23:85–93
Rozendaal DMA, Zuidema PA (2011) Dendroecology in the tropics: a review. Trees 25:3–16
Searson M, Pearson S (2001) A new technique in dendroecology using Callitris. In: Dargavel J, Hart D, Libbis B (eds) Perfumed pineries. Environmental history of Australia’s Callitris forests. Centre for Resource and Environmental Studies, Australian National University, Canberra, pp 39–47
Sperry JS, Hacke UG, Pittermann J (2006) Size and function in conifer tracheids and angiosperm vessels. Am J Bot 93:1490–1500
Stokes MA, Smiley TL (1968) An introduction to tree-ring dating. University of Chicago Press, Chicago
Vieira S, Trumbore S, Camargo PB, Selhorst D, Chambers JQ, Higuchi N, Martinelli LA (2005) Slow growth rates of Amazonian trees: consequences for carbon cycling. Proc Natl Acad Sci USA 102:18502–18507
Walsh RPD, Lawler DM (1981) Rainfall seasonality: description, spatial patterns and change through time. Weather 36:201–208
Wils THG, Robertson I, Eshetu Z, Sass-Klaassen UGW, Koprowski M (2009) Periodicity of growth rings in Juniperus procera from Ethiopia inferred from crossdating and radiocarbon dating. Dendrochronologia 27:45–58
Wils THG, Robertson I, Eshetu Z, Touchan R, Sass-Klaassen U, Koprowski M (2011) Crossdating Juniperus procera from North Gondar, Ethiopia. Trees 25:71–82
Worbes A, Staschel R, Roloff A, Junk WJ (2003) Tree ring analysis reveals age structure, dynamics and wood production of a natural forest stand in Cameroon. For Ecol Manag 173:105–123
Acknowledgments
We thank Scott Nichols, Phillip Moser, Diane Prior, Lachie McCaw, Kim Whitford, Richard Fairman, Sharyn Yelverton, Herman Mouthaan, Stephen Harris, Kim Webeck, Kathryn Allen and Stuart, Kate, Lily and Ted Pearson for field assistance. Rob Argent, Melbourne Water, collected the Snowy River sample. Scott Nichols and Kathryn Allen prepared the cores, and Zoe Lee helped in sample processing for AMS 14C analysis. Gregor Sanders prepared the map. This project received funding from CERF grant B0016193. Radiocarbon analysis was funded with grants from the Australian Institute of Nuclear Science and Engineering (Grants 00/122, 03/090P and 07/014). We thank the Northern Territory Parks and Wildlife Service, NSW Department of Environment and Climate Change, Queensland Department of Environment and Resource Management, WA Department of Environment and Conservation, Victorian Department of Sustainability and Environment, Parks and Wildlife Service Tasmania, the Consolidated Pastoral Company, Mr Garth Dunford, the Siemer family and the Australian Wildlife Conservancy for help with site selection and permission to sample on their land.
Author information
Authors and Affiliations
Corresponding author
Additional information
Communicated by A. Gessler.
Rights and permissions
About this article
Cite this article
Bowman, D.M.J.S., Prior, L.D., Tng, D.Y.P. et al. Continental-scale climatic drivers of growth ring variability in an Australian conifer. Trees 25, 925–934 (2011). https://doi.org/10.1007/s00468-011-0567-5
Received:
Revised:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00468-011-0567-5