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The Jarrah Forest 1989
DOI: 10.1007/978-94-009-3111-4_2
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The soils and landforms of the northern jarrah forest

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Cited by 47 publications
(51 citation statements)
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“…It ranges from a tall, open, and dry sclerophyll forest in the north to a tall closed forest in the south (Dell and Havel 1989). The NJF harbours over 850 known vascular plant species (in addition to many unnamed) contributing to SWWA being one of the 35 global biodiversity hotspots (Mittermeier et al 2011 (Churchward and Dimmock 1989). The soils are some of the oldest on the planet.…”
Section: Study Areamentioning
confidence: 99%
“…It ranges from a tall, open, and dry sclerophyll forest in the north to a tall closed forest in the south (Dell and Havel 1989). The NJF harbours over 850 known vascular plant species (in addition to many unnamed) contributing to SWWA being one of the 35 global biodiversity hotspots (Mittermeier et al 2011 (Churchward and Dimmock 1989). The soils are some of the oldest on the planet.…”
Section: Study Areamentioning
confidence: 99%
“…1), covers an area of 1 127 600 ha (Havel 1975), and ranges in form from a tall open and dry sclerophyll forest in the north to a tall closed forest in the south (Dell and Havel 1989 (Churchward and Dimmock 1989). The climate is Mediterranean-type, with cool wet winters and most (~80%) rainfall falling between April and October (Bates et al 2008) and a seasonal drought that may last from 4 to 7 months (Gentilli 1989).…”
Section: Study Areamentioning
confidence: 99%
“…Intense and long-lasting weathering resulted in a nutrient poor, deep (up to 50 m to granite bedrock) lateritic profile (Dell and Havel 1989). The topography is undulating with uplands averaging in elevation between 280 and 320 m intersected by shallow and steep valleys up to 100 m below (Churchwood and Dimmock 1989). Uplands generally consist of shallow, sandy to gravely topsoil's (10-20 cm deep) overlying a rock lateritic duricrust (0.5-2 125 m) and underlying clays with a relatively high water storage capacity (Schofield et al 1989).…”
Section: Geologymentioning
confidence: 99%
“…Valley floors predominantly hold loams and sandy loams overlying clays. Granite bedrock frequently intersects these profiles across the NJF forming distinct rock outcrops within the landscape (Churchwood and Dimmock 1989 (Heddle et al 1980). The dominant tree species are highly adapted to the climatic and soil conditions in the NJF, utilising water from the deeper clays during the summer drought using sinker roots penetrating the lateritic duricrust (Abbott et al 1989;Dell and Havel 1989;Schofield et al 1989).…”
Section: Geologymentioning
confidence: 99%