Short (<1 m) lowland heaths on acid, leached soils, eroded by winter rains after human deforestation, impoverished and thinned, all of which reduces their capacity to store water and may occasionally lead to severe drought.
The most likely original position of this shrubland, as revealed by the tiny, very dispersive seeds of Erica and its massive flowering, seen from afar, were scattered steep siliceous ridges where trees couldn't stand, soils were heavily leached by rains and wind in winter and, in summer, very dry as a consequence of their thinness and, hit by lightning, exposed to episodic spontaneous fires. All this set the selective pressures leading to these short, profusely flowering, ligneous, evergreen, small-leaved, tiny-seeded, resprouting shrubs and their characteristic fungal root partnership with lignolytic fungi. Anthropic deforestation through fire, initiated some 6000 years ago but aggravated around 1000 BC, eliminated taller competitors and chronically impoverished soils, giving heaths an unexpected advantage and inverting the ancient picture: the original shrubby islands became the new matrix and forests were relegated to isolated pockets. In recent decades, heathlands in coastal areas have experienced a substantial regression, replaced by industrial pine or eucalyptus plantations or, in flat areas suitable for mechanised agriculture, by fodder crops or artificial meadows, plowed and improved with synthetic fertilisers. Heathlands in S42y, for mutually reinforced climatic, topographic and socioeconomic reasons, are less affected by these regressive trends.
Known occurrences and potential area of occupancy of the habitat type in the study region.