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Lichen communities in the British Isles: A preliminary conspectus

Lichen communities in the British Isles: A preliminary conspectus

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364 P. W. James, D. L. Ilazpksworth and F. Rose<br />

'Iasrn X_cont<strong>in</strong>ued<br />

Species Stand<br />

V. glauc<strong>in</strong>tt<br />

V. hochstetteri<br />

V. muralis<br />

V. sph<strong>in</strong>ctr<strong>in</strong>a<br />

V. airidula<br />

-)- ',<br />

1.2<br />

_L)<br />

J-.0<br />

+.0<br />

)- ')<br />

_J- ')<br />

-l?<br />

-)_ )<br />

+,0<br />

-L)<br />

+.0<br />

1. '.)<br />

-L?<br />

+.0<br />

+.2<br />

1.2<br />

t)<br />

1. Su<strong>the</strong>rland, lnchnadamph, lowcr slopes of<br />

transition between acid rock u"a ti-".ton.,<br />

e 1961, r.w .J .<br />

Ramsey (17 1992462): transition beru,ee n<br />

exposed site, <strong>in</strong>cl. + 10., aspect 270o,<br />

.w.J.<br />

ove Lochan an<br />

st 1.970, p.W.J.<br />

): exposed sitc,<br />

Carsaig, near Nuns.pass (l 7/525205);<br />

ust 1969, p.W.J.<br />

, Great Close (44/90367g): smalt outcrop<br />

, 0.5 x 0.5 m, 16 August 1967, p.\N.I:<br />

centricae Mot. (Motyka, 1926, pp. 219, 226)<br />

this nodum but this was poorly circumscribe.l<br />

<strong>the</strong> non-<strong>British</strong> Leciclea'nioeiatra as a ma<strong>in</strong><br />

VI. Siliceous Rock Communities<br />

have, with <strong>the</strong> notable exception<br />

received scant attention <strong>in</strong> thc<br />

ever, support more lichen species<br />

ish <strong>Isles</strong>. While many <strong>communities</strong><br />

occur, problems of identification of<br />

survey work undertaken mean that<br />

ularly tentative.<br />

t of <strong>the</strong>se <strong>communities</strong> parallel<br />

(see p. 304) with <strong>the</strong> ac{dition of<br />

rdness and friabilitl, and (3) heavy<br />

10. <strong>Lichen</strong> Communilies <strong>in</strong> <strong>the</strong> <strong>British</strong> <strong>Isles</strong> 365<br />

In order to draw similar alliances and associations toge<strong>the</strong>r, <strong>the</strong> siliceous<br />

rock <strong>communities</strong> have been grouped <strong>in</strong>to six broad habitat categories: (A)<br />

shaded, (B) exposed, (C) nutrient-enriched, (D) m<strong>in</strong>eral-rich, (E) mar<strong>in</strong>e<br />

and maritime, and (F) aquatic.<br />

All. 14. Leprarion chlor<strong>in</strong>ae<br />

A. Shaded<br />

Leprarion chlor<strong>in</strong>ae Smarda & Hadad, <strong>in</strong> Klika & Hadad, Pffuoda, Bnto 36,253<br />

(1944).-Cystocoleion nigriWirth, Diss. Bot., Lehre 17,105 (1972).<br />

An alliance of shaded underhangs and recesses <strong>in</strong> hard siliceous rocks<br />

which are sheltered from direct ra<strong>in</strong>; <strong>the</strong> acid rock counterpart of <strong>communities</strong><br />

<strong>in</strong> dry bark recesses (pp.306-313) and similar situations on<br />

limestone (pp. 349-360). Crustose and leprose species predom<strong>in</strong>ate <strong>in</strong> this<br />

alliance and many of hese are abundantly sorediate; <strong>in</strong>deed a high<br />

proportion are unknown fertile.<br />

A comprehensive key to <strong>the</strong> lichens of shaded acid rock crevices and<br />

underhangs <strong>in</strong> Brita<strong>in</strong> is provided by James (1970) and <strong>in</strong>cludes <strong>in</strong>formation<br />

on <strong>the</strong> distribution of <strong>the</strong> species.<br />

Some species-poor <strong>communities</strong> referable to this alliance are also able<br />

to occur on upturned tree roots, soil, pebbles <strong>in</strong> roadside cutt<strong>in</strong>gs or <strong>in</strong> old<br />

acid woodlands, as well as <strong>in</strong> <strong>the</strong> dry overhangs and recesses <strong>in</strong> rock of<br />

which <strong>the</strong>y are characteristic. The essentially corticolous Coniocybeturn<br />

furfuraceae (p. 308) is also able to spread on to rock and dry soil <strong>in</strong> suitably<br />

shaded sites and form <strong>in</strong>tergrades with both <strong>the</strong> Lecideetum lucidae and <strong>the</strong><br />

L. syloicolae. The broad ecological amplitude of <strong>the</strong> Leprarietum <strong>in</strong>canae<br />

(p. 312) <strong>in</strong>cludes siliceous rocks on which it can form transitions to <strong>the</strong><br />

Lecideetum lucidae and Racodietum rupestris <strong>in</strong> particular,<br />

The Sclerophytetum circumscriptae of recesses <strong>in</strong> maritime rocks, u'hich<br />

occupies comparable but more base-rich habitats than <strong>the</strong> Leprarion<br />

chlor<strong>in</strong>ae, is discussed separately below (pp. 387-388), while <strong>the</strong> heavymetal<br />

requir<strong>in</strong>g Lecanoretum epanorae, which also has an aff<strong>in</strong>ity for<br />

dry crevices, is discussed on p. 383.<br />

Mention should also be made here of a community of uncerta<strong>in</strong> syntaxonomic<br />

position which is currently poorly known and thus not recognizecl<br />

formally here: <strong>the</strong> Lecidea phaeops-L. taylori nodum. This'is essentially a<br />

community of damp overhangs oi .*pot.d rocks lvith<strong>in</strong> sheltered woodland<br />

sites to which Gyalidea hyal<strong>in</strong>escens may also be faithful; that it requires<br />

damp rocks <strong>in</strong>dicates that it should be placed <strong>in</strong> an alliance othcr than <strong>the</strong><br />

Leprarion chlor<strong>in</strong>ae and may perhaps be close to l\e Aspicilietum lacustris<br />

(p. 3e1).

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