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| Saline soil vegetation
Diagnostic features for identification in the fieldFor more information on identification of plants associated with saline habitats, click on appropriate photo:
Description of community and habitatSaline soils in the driest Central Otago valleys occur mainly around the bases of hills where salt is being leached from weathered schist and Tertiary sediments, and in patches of alluvium in low parts of the landscape. Once quite extensive, they have been drastically reduced in area and modified by farming. Their survival is precarious. Instead of distinctive communities, there are haphazard assemblages of salt-tolerant plants which, with the exception of Lepidium kirkii (a rare, slender, annual), and Puccinellia raroflorens (salt grass) also grow on Otago coasts. Saline areas with any natural characteristics that remain today are mostly small and fragmented. Cultivation and irrigation have replaced most such areas with exotic pasture. The remaining saltpans have managed to retain some of their native flora and fauna, although exotic flora is generally dominant. Saline areas can often be identified by the presence of grey-white crust of salt on the surface of seemingly bare ground. On closer inspection, inconspicuous plants such as Atriplex buchananii can be seen. The vegetation immediately surrounding the most salty areas tends to be comprised of short grasses and herbs, including cushionfield.
Species presentSpecies which have been recorded on saline areas of the Maniototo Ecological District (from Patrick, 1989) [Note: an updated list can now be found in Rogers et al. 1999 Appendix 4 and iconic species list Table 3, p.8]: (* denotes adventive species) Crucerifae
Chenopodiacae
Crassulaceae
Umbelliferae
Ranunculaceae
Geraniacea
Caryophyllaceae
Fabaceae
Asteraceae
Plantaginaceae
Goodeniaceae
Primulaceae
Scrophulariaceae
Violaceae Graminaceae
Juncaginaceae
Vegetation HistoryThe Central Otago region has a complex history of disturbance. Post-glacial forest may never have extended to the drier basin of Central Otago, and the establishment of grassland, possibly through natural fires, preceded human settlement by several centuries (Wardle, 1985; McGlone, 1989; McGlone et al., 1995). In the driest valleys of Central Otago, saltpans developed around the bases of hills where salt was leached from Tertiary sediments, and in valley floors subject to high water tables where salt in ground water accumulated in the soil. It appears that the saline soils were much more extensively distributed in the past than they are today (see Rogers et al. 1999). The presence and extent of the salty soils was a problem to farmers in the region. Widespread irrigation and cultivation have replaced most saline soil areas with exotic pasture. The remaining areas are mostly small and fragmented, but do retain some of their native flora and fauna, adapted to these salty conditions. Exotic plants, however, generally dominate.
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