Following European settlement of the area, land was extensively cleared to allow for farming and agriculture. Sheep and cattle grazing was a common sight around the Barmah region from the mid to late 1800s. The periodic burning previously undertaken by Indigenous Australians was also halted. This decrease has been attributed to the changes to the flood regimes occurring in the area. In the
Murray-Darling Basin, prior to regulation of the Murray River, extensive
Moira grass (
Pseudoraphis spinescens) dominated floodplain marshes existed in areas that were typically seasonally flooded for 5–9 months duration in most years, to a minimum water depth of 0.5 m, and completely dry during late summer and autumn. Floodplain areas previously dominated by aquatic species, such as Moira grass,
common reed (
Phragmites australis), and
cumbungi (
Typha spp.), are now covered with species adapted to lower levels of flooding, mainly river red gums and
giant rush (
Juncus ingens). The extent of the Moira grass-dominated plains has declined by 96 per cent over the last 80 years in the Barmah Forest, and they are predicted to be extinct in the Barmah Forest by 2026 without management intervention. Reductions in duration and depth of natural flooding due to regulation of the Murray River, grazing and trampling pressure by introduced animals, particularly by
feral horses (and previously cattle), and invasive plant species are the main causes of this decline. == Management ==