S42x Atlantic Erica-Ulex heaths

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Description

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.

Protection

Protected under the code 4030 ("European dry heaths") by the EU Habitat Directive (certain coastal stands might qualify as the prioritary 4040*["Dry Atlantic coastal heaths with Erica vagans"], but, judging by the definition in the official Manual, not those topping sea-cliffs right above N316, as it has been generally but inappropriately accepted).

Floristic Composition

Phytosociology

  • Angelico pachycarpae-Ulicetum maritimae
  • Arctostaphylo crassifoliae-Daboecietum cantabricae
  • Cirsio filipenduli-Ericetum ciliaris
  • Cisto salviifolii-Ulicetum humilis
  • Daboecio cantabricae-Ulicetum gallii
  • Erico tetralicis-Ulicetum gallii
  • Gentiano pneumonanthes-Ericetum mackaianae
  • Halimio alyssoidis-Ulicetum breoganii
  • Halimio umbellati-Daboecietum cantabricae
  • Sileno maritimae-Ulicetum humilis
  • Ulicetum latebracteato-minoris
  • Ulici breogani-Ericetum mackaianae
  • Ulici europaei-Ericetum cinereae
  • Ulici europaei-Ericetum vagantis
  • Ulici gallii-Ericetum ciliaris
  • Ulici humilis-Ericetum vagantis

Relations with other habitat types

These heathlands are mostly interpretable as a dysclimax of the unit T1Bx. In the northernmost areas, cool and cloudy summers keep the organic litter permanently wet, enabling transitions towards S412 and even Q12x. Since, for geographic reasons, EUNIS would include some of the heaths in this unit in its S423 and others in S424, such units are inconsistent with our results and a new regional umbrella level IV unit is in order. In more inland, drier-summer, submediterranean areas, they transition towards S42y.

Regional distribution

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.