Acidophilous zonal forests in the lowlands of the northern, maritime territories of the ecoregion, where summer-droughts are rare and mild, soils remaining moist enough for deciduous broadleaved trees to support the high transpiration rates of their competitive light-capturing apparatus. Usually dominated by pedunculate oak, but with a pretty diverse tree layer including sweet chestnut, birch, ash and wild cherry.
These forests were cleared in a great proportion many centuries ago, both as a source of wood and as a way to create more productive, non-ligneous vegetation that humans can consume directly or through livestock intermediation. Most of their ancient domain is currently occupied by grasslands (R1M2, R211), shrublands (especially S332) or, when soil is eroded after burning for pastures, aggravating the intrinsic oligotrophy of these siliceous substrates, by heathlands (S42x); as well as, more recently, by pine or eucalyptus industrial plantations. Most of the remaining stands are quite managed (see above).
Known occurrences and potential area of occupancy of the habitat type in the study region.