2014
DOI: 10.7751/cunninghamia.2014.14.007
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Floodplain vegetation of the River Murray in 1987–1988: an important pre-drought benchmark for subsequent studies.

Abstract: Abstract:As part of a wider study of floodplain vegetation along the River Murray, we carried out a field survey in 1987-1988 involving collection of floristic and vegetation condition data from 335 sample plots (each 400 m 2 in area), between Hume Dam and Lake Alexandrina (including the Edward-Wakool anabranch system). The floodplain vegetation is dominated by just two tree species, River Red Gum (Eucalyptus camaldulensis) and Black Box (Eucalyptus largiflorens), but the composition of the understorey shows m… Show more

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Cited by 14 publications
(10 citation statements)
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“…and corresponded to low, moderate and high productivity, respectively. The least productive blackbox sites occurred on upper level floodplains that receive floodwater infrequently (10–40 years; Smith & Smith ). The soils are relatively deep, with a high proportion of fine sediments (silt + clay; Eldridge, Koen & Harrison ; Appendix S2).…”
Section: Methodsmentioning
confidence: 99%
“…and corresponded to low, moderate and high productivity, respectively. The least productive blackbox sites occurred on upper level floodplains that receive floodwater infrequently (10–40 years; Smith & Smith ). The soils are relatively deep, with a high proportion of fine sediments (silt + clay; Eldridge, Koen & Harrison ; Appendix S2).…”
Section: Methodsmentioning
confidence: 99%
“…Our sites were selected based on the overstorey dominance of three focal tree species: white cypress pine ( Callitris glaucophylla ), blackbox ( Eucalyptus largiflorens ) and river red gum ( Eucalyptus camaldulensis ). At the least productive end of the gradient (based on NPP data from MODIS imagery: 0.64 g C m −2 days −1 ) are sites located within the blackbox community (Table ), which is generally found on higher level floodplains that receive floodwater very infrequently (10–40 years; Smith & Smith, ). The soils have uniform and deep profiles and contain relatively high levels of silt (56%) and clay (19.3%, Eldridge, Koen, & Harrison, , Table ).…”
Section: Methodsmentioning
confidence: 99%
“…The soils have gradational profiles consisting of Quaternary colluvium and aeolian deposits, and are generally low in C, N and P. The understorey in these communities varies according to soil type and disturbance (fire, grazing) history. The Black box community occurs on upper level floodplains of inland rivers, lakes and swamps that receive infrequent flooding (10–40 years; Smith & Smith, ). Their soils have a deep uniform profile and are relatively high in silt and clay (Eldridge, Koen, & Harrison, ).…”
Section: Methodsmentioning
confidence: 99%