5.1.3.1.1 Chalk
Seven main types of chalk grassland are recognised accorc ing to differences in dominance of grass or sedge specie namely: Festuca ovina-F. rubra, Carex humilis, Zerna erecti Brachypodium pinnatum, Arrhenatherum elatius, Helictc trichon pubescens and mixed Gramineae. The Festuca an C. humilis types are those which have come to be regarde as high quality chalk swards, on account of their fit: richness; the former is widespread on the Chalk formatioi but C. humilis swards are confined to the more westerl districts and are best developed in Wiltshire. Within thes two associations various facies are recognised tentative! according to different consistent combinations of othe locally constant species, as follows:
  • Sieglingia decumbens facies, best seen in the Isle of Wight and some of the westernmost chalk grasslands, e.g. a Long Knoll, Wiltshire
  • Carex flacca-Poterium sanguisorba facies, widespread bu characteristic of the Festuca ovina grasslands particularly in the Chilterns.
  • Poterium sanguisorba-Helianthemum chamaecistus facies characteristic of south-facing slopes in the more continental areas, e.g. Chilterns, Kent, East Anglia.
  • Serratula tinctoria-Betonica officinalis-Succisa pratensis facies, a strikingly western facies, often associated with Carex humilis but also in Festuca ovina grasslands.
  • Scabiosa columbaria-Succisa pratensis facies,  a local variant of the western chalk grasslands.
  • Poterium sanguisorba-Filipendula vulgaris facies, local in distribution.
  • Leontodon hispidus facies, widespread, but best developed in Wiltshire and Dorset.
  • Phyteuma tenerum-Scabiosa columbaria-Succisa pratensis facies, restricted to Hampshire and the South Downs. Daucus carota facies, very local and associated with the Poterium facies.
  • Chrysanthemum leucanthemum facies, very local, and always associated with the Festuca ovina or Carex humilis main associations.
These facies or others as yet undescribed appear to have ecological significance, in being related to such factors as geographical position, aspect and slope. J. F. Hope-Simpson has emphasised that northernmost occurrences of chalk grassland, on the Yorkshire Wolds, are a special case which has to be considered on rather different grounds from the rest of the Chalk, for the following reasons: 
  • (i) the Wolds are widely separated from all other chalk grasslands;
  • (ii) northerly aspects in the Wolds are steeper and more common than in the Downs and they have a 'poorer' flora;
  • (iii) many species common on the southern Chalk are absent or at their northern limit on the Yorkshire Chalk (e.g. Cirsium acanion); 
  • (iv) Conopodium majus, virtually unknown on the southern Chalk, is common on the Wolds and other species such as Knautia arvensis are regular members of the Wolds chalk grassland but only occasional members of the southern chalk grassland.
The Zerna erecta and Brachypodium pinnatum communities usually represent stages in the retrogression of chalk grassland following cessation of grazing, resulting both from the removal of sheep stocks and elimination of rabbits by r^atosis. These vigorously competitive grasses spread or increase in luxuriance, thus suppressing the smaller herbs and reducing species diversity. A further stage is the invasion bv medium- to tall-shrub species which grow into a debse scrub and eventually smother most of the grassland slants. These retrogressive changes have been widespread in the remaining chalk grasslands during the last 15 years, and have often produced communities greatly impoverished in both plants and associated animals. Such successional tendencies create management problems for downland areas which it is desired to retain in an original condition. On the other hand, the changes associated with reduction or cessation of grazing are not always detrimental; they may, for instance, allow the flowering and better performance of me species, and may lead to a different balance in which greater diversity of ecosystem is actually attained.
The Arrhenatherum elatius and mixed grass types of chalk sward are often associated with more fundamental disturbance, including heavy grazing and manuring, application of fertilisers, ploughing and even reseeding. These swards usually lack most of the more characteristic herbs of old I ?land and tend to be floristically poor; they show dose relationships with the more modified types of lowland grassland.