Cr. Fielding et al., PRESERVATION OF IN-SITU, ARBORESCENT VEGETATION AND FLUVIAL BAR CONSTRUCTION IN THE BURDEKIN RIVER OF NORTH QUEENSLAND, AUSTRALIA, Palaeogeography, palaeoclimatology, palaeoecology, 135(1-4), 1997, pp. 123-144
In sub-humid parts of north Queensland, NE Australia, certain types of
trees are well adapted to living in river bed habitats. The bed of th
e tropical, variable-discharge, upper Burdekin River hosts a community
dominated by the paperbark Melaleucu argentea. Trees grow preferentia
lly in flow-parallel, linear groves, and engineer their own environmen
t by deflecting currents, building sand and gravel bars and stabilisin
g banks. This is the first study to document in-channel bar developmen
t resulting from vegetation growth, rather than the reverse which has
been inferred by previous workers. In the Burdekin River study site, i
ndividual Melaleuca range from seedlings to mature trees over 100 year
s old. These trees survive regular, partial to total submergence and i
mpact damage during wet season runoff events (often reaching over 20,0
00 m(3) s(-1) at peak discharge) partly by adopting structural and gro
wth modifications. These modifications include a reclined, downstream-
trailing habit, multiple-stemmed form, modified crown with weeping fol
iage, development of thick, spongy bark, root regeneration and group s
trategies, notably development of flow-parallel, linear groves. Follow
ing death, in situ remains of trees are preserved within the mainly co
arse sand to gravel channel fill, either as reclined stems/trunks stri
pped of branches and foliage or as more upright trunks snapped at a he
ight of typically 1-2 m above base, both with roots. The morphological
adapations and styles of preservation of in situ vegetation within th
e Burdekin River are considered distinctive of variable-discharge rive
rs, and may be useful in the identification of facies formed in such e
nvironments in the rock record, particularly when associated with bar
development. (C) 1997 Elsevier Science B.V.