Oceanic bogs in initially slightly concave areas, with water input mostly derived from in-situ input of atmospheric moisture, dominated by strictly acidophilous heath and Sphagnum species. The litter shed by this vegetation is poorly decomposed as a consequence of both the strongly acidity it contributes to create and the soggy, anoxic conditions, leading to the build-up of peaty domes.
As an azonal vegetation composed by ecological specialists (able to cope with very selective edaphic conditions whose influence far exceeds that of the thermal regime), and despite the impact of drainings and artificial fertilizations, it occurs scattered across all the territory, even in climatically unsuitable submediterranean southwestern areas, where the lack of summer rains is compensated by siliceous impermeable bedrocks on which the abundant surface runoff during the rainy winters, eventually collected in concave places, hardly differs from rain water, giving rise to boggy valleys reminiscent of EUNIS block Q21 (“Oceanic valley mire“).
Known occurrences and potential area of occupancy of the habitat type in the study region.