5.1.3 Flora
The preceding account of mire vegetation types has indicated a range of floristic diversity in relation to water nutrient status. Table 23 gives the ecological distribution of each British vascular mire species according to the major divisions of water pH and nutrient status, as far as these are known at present. Species which occur widely in other habitats besides mires are omitted, as are woody species above the size of medium shrub (i.e. most of the willows) as these belong more properly to woodland or lowland scrub classifications. The true hydrophytes belonging essentially to open water are treated under that habitat formation, though the limits of this group have had to be arbitrarily defined, and species characteristic of ombrogenous mire pools are included here.
A few general features emerge from this study of edaphic relationships. Few species appear to be confined to eutrophic fen, but there is a large group of broadly basiphilous species whose tolerances/requirements range from mesotrophic to eutrophic. This could perhaps reflect an inadequacy of data on water chemistry for some species or a badly chosen boundary between the two trophic levels, but it suggests that above a certain level, further increase in nutrient status has no effect on many species. There is a much smaller number of species confined to oligotrophic mire waters, compared with those in the two higher trophic levels. Only a few species show a complete range of tolerance to acidity/alkalinity of mire waters.
There is insufficient information to record the distribution of each species in relation to the six main morphological types of mire. However, chemical factors, and thus species distribution, tend to vary independently of mire morphology, except in ombrogenous mires (raised and blanket mires), for these have only oligotrophic conditions. It is more meaningful to separate oligotrophic ombrogenous from oligotrophic topogenous as there appears to be a real difference between these two in both chemical and floristic terms; some plants belong to raised and/or blanket mire, but not to poor-fen, and vice versa, and the controlling differences may include rate of movement and aeration of the water.
Geographical distribution of mire plants is also shown in Table 23. There is a certain degree of parallelism between ecological and geographical distribution of mire species. The restriction of ombrogenous mire to the west and north ensures that species confined to or occurring mainly in this class of peatland have a similar distribution while the strong representation of mesotrophic and eutrophic fen in southern Britain (especially in East Anglia) is matched by the restriction of some strongly basiphilous species to this part of the country. Since lowland mires have been so widely drained and destroyed in the interests of farming and building, many of their characteristic species have suffered great reduction in range or even extinction. Many wide-spread mire species are much less common and generally distributed in the south and east of Britain than in the north and west because of this effect, and the patchy distribution of some largely reflects the present restricted occurrence of suitable habitats.
To give examples of this retreat, the East Anglian Senecio palustris is extinct while S. paludosus is known in a single ditch in this region: the northern Scheuchzeria palustris is known only on Rannoch Moor in Scotland; and the once rather widespread Carex elongata is now quite rare. Other .restricting factors may operate and it has been suggested that the decline of the rare fern Dryopteris cristata is partly the result of introgressive hybridisation with D. carthusiana, accompanied by selection in favour of the hybrid forms.
As an analysis of mire species geographical distribution .according to presence or absence in particular regions often fails to indicate distinctive patterns, a different and more .meaningful treatment has been adopted. Study of mire species distribution maps suggested that eight main patterns of scatter could be recognised; these have been chosen subjectively and arbitrarily but nevertheless enable a useful analysis to be made. These distribution classes (see Table 23) are defined as follows:   . ,...
WIDESPREAD/COMMON
Species occurring over virtually the whole of Britain, and limited mainly by lack of suitable habitats. These naturally tend to be species with wide ecological amplitude, but the group which find their optimum water nutrient status in the upper oligotrophic to lower mesotrophic range are especially well represented, as waters of this type are probably the most widespread in Britain. Typical examples are Caltha palustris, Lychnis flos-cuculi, Juncus articidatus and Phalaris arundinacea.
WIDESPREAD/LOCAL
Species occurring in most districts of Britain, but much less abundantly than the last group, and often absent from apparently suitable localities. These appear to show no particular ecological bias as a group. Typical examples are Ranunculus lingua, Utricularia vulgaris, Dactylorchis in-carnata, Carex vesicaria and C. acuta.
SCATTERED/VERY LOCAL
Species showing a highly discontinuous scatter, absent from a great many apparently suitable localities, but widely spread and showing an irregular pattern with no single geographical bias. These certainly show no particular ecological bias as a group. They are Dryopteris cristata, Cicuta virosa, Pyrola rotundifolia, Naumburgia thyrsiflora, Dactylorchis traun-steineri, Eriophorum gracilc, Cladium rnariscus, Carex flava, C. elongata and Calamagrostis stricta.
SOUTHERN
Species which become increasingly widespread and abundant with distance south in Britain; they belong essentially to England and Wales, but especially southern England, and though some reach Scotland they are local or rare there.
This group includes a high proportion belonging to mesotrophic and eutrophic mire, e.g. Thalictrum flavum, Berula erecta, Oenanthe fistulosa, Rumex hydrolapathum, Cirsium dissectum, Epipactis palustris, Dactylorchis praetermissa, Carex pseudocyperus and C. riparia.
OCEANIC
Species occurring mainly in coastal districts, but especially along the south and/or west coasts. The most localised is the thermophilous southern oceanic Hypericum undulatum, only in south-west England and west Wales, which contrasts with the northern oceanic Drosera anglica, most abundant in the north-west Highlands. Other characteristic members are Hypericum elodes, Drosera intermedia, Pinguicula lusitanica, Scutellaria minor, Rhynchospora alba and R.fusca. Osmunda regalis, Oenanthe crocata, Eleocharis multicaulis and Schoenus nigricans show the same general pattern but occur more widely away from coastal districts. If the Irish- American Spiranthes romanzoffiana can be regarded as a mire plant in Britain, it belongs here. It is perhaps significant that the majority of species in this group grow also on acidic wet heathland, a characteristic oceanic British vegetational formation.  
EAST ANGLIAN
Species found mainly in eastern England from Suffolk to the Humber, but especially in East Anglia. The rare or very local species which occur in very few places outside this belt are Viola stagnina, Lathyrus palustris, Peucedanum palustre, Sonchus palustris, Liparis loeselii and Carex appropinquata. More widespread and plentiful species which could be regarded as southern, but are more abundant in the Suffolk-Humber region than elsewhere include Thelypteris palustris, Sium latifolium, Juncus subnodulosus, C. data and Calamagrostis canescens. These are without exception plants of rich-fen.     ..

NORTHERN
Species which become increasingly widespread and abundant with distance north in Britain and have their headquarters north of the Midlands, but are confined to fairly low altitudes. This includes extreme rarities such as Carex buxbaumii, C. chordorrhiza, Scheuchzeria palustris and Ledum groenlandicum, and local species such as Listera cordata, C. paupercula, C. pauciflora, C. aquatilis and Corallorhisa trifida. Most of these could be regarded as submontane as they occur mainly in upland districts. Many northern species have a wide distribution in Britain, reaching to the extreme south of England, where they are, however, rare or very local. These include Vaccinium oxycoccus, Utricularia intermedia, Hammarbya paludosa, Carex limosa, C. lasiocarpa, C. curia and C. dioica.
Nearly all the northern species so far mentioned belong to oligotrophic mire, especially of the topogenous kind (poor-fen), thus reflecting the general edaphic trend towards increasing prevalence of base-poor waters in northern Britain. Strongly basiphilous and widespread northern species include Parnassia palustris, Dactylorchis purpurella, Erio-phorum latifolium and Carex lepidocarpa.
Andromeda polifolia is essentially a northern species in mainland Europe, but has a curious British distribution, for it does not reach the Highlands and occurs mainly in northern England and southern Scotland, where it is locally abundant in oligotrophic mires (cf. Primula farinosa in calcareous habitats). Calamagrostis stricta could be regarded as a northern species, but is included in Table 23 as scattered, local. Eriophorum vaginatum and Trichophorum cespitosum occur in the extreme south of England but are regarded as northern as they become really abundant only from Wales northwards.
MONTANE
Species with a northern distribution which are found mainly at high altitudes and are most abundant in or confined to the Scottish Highlands. These are necessarily restricted to the only kinds of mire found at high levels, namely, blanket and soligenous mires. The montane species of blanket mire are Betula nana, Arctostaphylos uva-ursi, Arctous alpinus, Vaccinium uliginosum, V. microcarpum, Empetrum herma-phroditum and Rubus chamaemorus. Those of oligotrophic soligenous mire are Carex rariflora, C. lachenalii, C. bige-lowii and Siaxifraga stellaris. The montane species belonging to mesotrophic or eutrophic soligenous mire are S. hirculus, Thalictrum alpinum, Polygonum viviparum, Kobresia sirn- pliciuscula, Juncus castaneus, C. atrofusca, C. capillaris, C. microglochin and C. norvegica. A few species in this group appear to be indifferent to mire water base- status, e.g. C. saxatilis, C. vaginata, Alopecurus alpinus and Phleum alpinum. Most of these species of montane soligenous mire are omitted from Table 23 as they belong to a wider range of habitats, including flushes, rills, springs and rock ledges, and they are dealt with under the flora of uplands (Chapter 9).
Some northern submontane species also occur in montane mires up to considerable elevations, e.g. Vaccinium vitis-idaea and Empetrum nigrum. It is noteworthy that the northern and montane mire flora has a strong representation of acidophilous dwarf shrubs (mainly Ericaceae) which belong mainly or entirely to ombrogenous mire.
Of the 161 peatland species listed in Table 23 only about half are classified into phytogeographical elements by J. R. Matthews (1937). A few more species have been tentatively classified from literature records and added, but distribution of most of the remainder could not be judged accurately enough and they have been left blank. These classifiable species give the following representation in the various elements: oceanic southern (i), oceanic west European (7), continental southern (2), continental (8), continental northern (43), northern montane (4), oceanic northern (3), Arctic-subarctic (2), Arctic-alpine (9).
The northern continental element thus constitutes over half the total list. The remaining unclassified peatland species would seem to belong either to this or to the continental element, or to be so widespread in Europe that no definite distribution pattern is discernible within this continent.
European and British distributions of mire species show some parallelism but there are certain discrepancies. Most of the oceanic western species in Europe have a western and coastal distribution here, but Drosera anglica, D. intermedia, Rhynchospora fusca and R. alba (all somewhat oceanic and with a western bias in Britain) are either continental or continental northern in Europe. All the European Arctic-alpine or Arctic-subarctic species are northern, and most are montane, in Britain; and the four northern montane species are northern and submontane here. Several continental northern species show no particular northern bias in Britain, and many British southern species are widely distributed in Europe.
The British vascular mire flora contains 13 rare species (present in 1-15 10-km grid squares) fairly well spread through the different ecological and geographical groupings.