2011
DOI: 10.1007/s00468-011-0567-5
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Continental-scale climatic drivers of growth ring variability in an Australian conifer

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… Show more

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Cited by 13 publications
(18 citation statements)
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“…Mean ring widths of C. columellaris were similar in the temperate and arid zones; however, site productivity would be substantially higher in the temperate zone than in the arid zone because there were more and taller C. columellaris trees as well as more trees of other species (Table 1; Prior et al 2011). Furthermore, radiocarbon dating suggests that growth events may also be slightly more frequent in the temperate zone (mean 1.6 compared with 1.4 per year; Bowman et al 2011). …”
Section: Relationships Of Ring Width With Tree Size and Agementioning
confidence: 92%
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“…Mean ring widths of C. columellaris were similar in the temperate and arid zones; however, site productivity would be substantially higher in the temperate zone than in the arid zone because there were more and taller C. columellaris trees as well as more trees of other species (Table 1; Prior et al 2011). Furthermore, radiocarbon dating suggests that growth events may also be slightly more frequent in the temperate zone (mean 1.6 compared with 1.4 per year; Bowman et al 2011). …”
Section: Relationships Of Ring Width With Tree Size and Agementioning
confidence: 92%
“…Furthermore, dendrochronologists generally focus on climatically sensitive sites and species that typically produce annual growth rings. Unfortunately, this approach cannot be applied in large expanses of the world, especially in arid climates with erratic rainfall (La Marche et al 1979;Pearson et al 2011;Bowman et al 2011). Consequently, there is a pressing need to extract ecologically meaningful tree growth data from systems where crossdating, and thus development of annually resolved chronologies, is highly problematic Grierson 2007, 2009).…”
Section: Introductionmentioning
confidence: 95%
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“…Establishing the age of old cultural custodian trees within forest communities in fire‐prone environments can be a useful indicator of past use of controlled fire, low‐intensity fire, fire exclusion or fire control. However, because tree age determination using growth rings is unreliable in tropical and subtropical forests (Bowman et al 2011; Prior et al 2012), and the use of periodic tree growth rates is unverified, radiocarbon dating was used. The aim of this study was to provide age estimates as evidence of potential survival and longevity of trees growing under low‐intensity bushfire management strategies and to obtain tree age data to calibrate an alternative non‐destructive low‐cost tree‐growth‐rate‐based method for ageing trees.…”
Section: Introductionmentioning
confidence: 99%
“…Piraino et al (2015) desarrollaron cronologías de ancho de anillos incluyendo ambas categorías morfológicas, mientras que Giantomasi et al (2013) sugieren descartar los individuos multi-fustales, ante la posibilidad de que sean consecuencia de disturbios, y por consiguiente, aporten efectos de variabilidad sobre el crecimiento radial que no están vinculados al clima. Aún cuando se discute respecto de incluir información derivada de individuos multi-fustales en estudios locales, el tema alcanza a otras investigaciones donde individuos multi-fustales han sido evitados en análisis dendroclimatológicos (Wang et al, 2005;Gareca et al, 2010;Bowman et al, 2011). Por lo previamente expuesto, cabe preguntarse entonces: ¿los algarrobos que difieren por sus características morfológicas presentan variaciones intra-especificas en la relación entre el ancho de los anillos y clima?…”
Section: Introductionunclassified