FOBIF’s moss group met at the Castlemaine Botanical Gardens last Saturday to move the project further towards its target: to publish a field guide to mosses of the region in Autumn next year.
This is not an eccentric interest in a picturesque but unimportant corner of our environment. Mosses play a key role in repair of damaged land and protection of soil against erosion. DSE analyses for the Goldfields bioregion show the following interesting figures: in Heathy Dry Forest, 10% of understorey is bryophytes [ie, mosses and liverworts] and lichens, and 10% is ‘soil crust’. In Box Ironbark Forest, 10% of understorey is bryophytes and lichens, and 20% is ‘soil crust’.
That humble term ‘soil crust‘ covers a combination of life forms, including mosses and lichens: which means that your unobtrusive moss is covering a hell of a lot of ground in our region.
The protective action of moss is easy to see. The following picture shows clearly how soil has been washed away from the area not covered by moss:
Moss and soil crusts are vulnerable to disturbance by trampling, or fire. Although mosses are not flammable, and therefore cannot be classed as fuel, they are often destroyed by ‘fuel reduction burns’. The following picture tells a story: