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Bulletin of the British Museum (Natural History)

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144 BRIAN JOHN COPPINS<br />

incrassate and coloured with green or greenish brown pigment and <strong>the</strong>n up to 3 /xm wide, usually<br />

coherent (even in K) and, toge<strong>the</strong>r with <strong>the</strong> surrounding pigmented matrix, form an epi<strong>the</strong>cium.<br />

Hypo<strong>the</strong>cium c. 100-230(-350) /xm tall, dilutely pigmented with pigment confined to gel matrix;<br />

upper part dull aeruginose or olive-brownish K- or + dulling, HNO3+ reddish); lower part<br />

<strong>of</strong>ten without greenish tinge, and <strong>the</strong>n being dilute brownish or ± hyaline; hyphae interwoven or<br />

some ± vertically orientated near <strong>the</strong> hymenium, c. 1-1-7 /am wide; ascogenous hyphae with<br />

short, swollen cells c. 2-5-4 /xm wide. Excipulum ± distinct in sections <strong>of</strong> young, hemispherical<br />

apo<strong>the</strong>cia, but soon becoming strongly reflexed and not sharply delimited from <strong>the</strong> hymenium,<br />

dilute brown or sometimes darkish brown along <strong>the</strong> outer edge. Hypo<strong>the</strong>cial and excipular<br />

tissues sometimes elongated vertically to form a stipe ('f. gomphillaced')<br />

Pycnidia inconspicuous, ± immersed, with walls green (K-, HNO3-I- red) in exposed upper<br />

parts and ± hyaline in immersed lower parts; <strong>of</strong> three types [only type (c) is common]: (a) c. 100<br />

ixm diam; conidia {macroconidia) curved or hamate, 0-3-septate, 16-22 Xc. 1 /xm; (b) c. 100-140<br />

/xm diam; conidia (mesoconidia) ± cylindrical, oblong-ellipsoid, obovoid or oblong-obovoid,<br />

usually distinctly truncate at proximal end, <strong>of</strong>ten 2-3-guttulate, 4-7(-7-6)xl-2-l-8 fxm; (c) c.<br />

40-50 ^im diam; conidia (microconidia) narrowly cylindrical, only faintly truncated at proximal<br />

end, eguttulate, (4-5-)5-7(-8)x 0-8-1 /xm.<br />

Chemistry: Thallus K-, C-, KC-, PD-I- red; sections <strong>of</strong> apo<strong>the</strong>cia C-, PD-; t.l.c:<br />

argopsin.<br />

Observations: Micarea lignaria is characterized by its whitish to grey, convex to ± globose<br />

areolae which are PD+ red (argopsin; but see var. endoleuca), black, markedly convex to ±<br />

globose apo<strong>the</strong>cia, green upper hymenium, dilute greenish or dilute olive-brownish hypo<strong>the</strong>cium,<br />

'^nd 3-7-septate, fusiform spores. When on lignum <strong>the</strong> thallus is <strong>of</strong>ten reduced to small<br />

scattered areolae and sometimes it is ± entirely endoxylic. The apo<strong>the</strong>cia are less variable in<br />

appearance, and pale (shade) forms are very rare. However, <strong>the</strong> apo<strong>the</strong>cia are occasionally<br />

found (especially on rock in dry underhangs) to be stipitate with a 'stipe' (composed <strong>of</strong> vertically<br />

extended hypo<strong>the</strong>cial and excipular tissues) up to 0-4 mm, or even 1 mm, tall (Fig. 3E). These<br />

forms have been ascribed <strong>the</strong> status <strong>of</strong> form, variety, species and even genus, viz.: Nylander's<br />

new species and genus Stereocauliscum gomphillaceum. In <strong>the</strong> type material <strong>of</strong> this, some<br />

'stipes' are extremely tall (up to 1 mm) and composed <strong>of</strong> vertically proliferating apo<strong>the</strong>cia, with<br />

<strong>the</strong> apical apo<strong>the</strong>cia being <strong>the</strong> youngest; <strong>the</strong> apo<strong>the</strong>cia are immature (or arrested in <strong>the</strong>ir<br />

development) with few asci and spores. In my opinion <strong>the</strong>se stalked forms <strong>of</strong> A/, lignaria result<br />

from abnormal development in response to adverse environmental conditions and are, <strong>the</strong>re-<br />

fore, not worthy <strong>of</strong> taxonomic recognition at any rank.<br />

M. lignaria is <strong>of</strong>ten confused with M. cinerea and M. peliocarpa, but <strong>the</strong>se two species have<br />

usually more flattened and <strong>of</strong>ten paler apo<strong>the</strong>cia, more richly branched paraphyses, and a<br />

hyaline hypo<strong>the</strong>cium. In addition, <strong>the</strong>y contain gyrophoric acid, resulting in <strong>the</strong> C-l- orange-red<br />

(quickly fading) , PD<br />

— reactions <strong>of</strong> <strong>the</strong>ir thalli and apo<strong>the</strong>cia. M. ternaria {q. v. ) is very similar to<br />

M. lignaria, but has more flattened apo<strong>the</strong>cia with a more discernible excipulum and spores<br />

which are never more than 3-septate; fur<strong>the</strong>rmore, it lacks any lichen substances.<br />

Habitat and distribution: M. lignaria occurs on a wide range <strong>of</strong> substrata, but is most common<br />

in upland districts, growing over bryophytes or plant debris on siliceous rocks and walls, or on<br />

exposed peaty ground. Associated lichens found in such habitats in Britain include<br />

Arthrorhaphis citrinella, Baeomyces rufus, Cladonia coccifera, C. floerkeana, C. squamosa, C.<br />

subcervicornis, Coelocaulon aculeatum s. lat., Lecidea granulosa, L. icmalea, Lecidoma demissum,<br />

Lepraria neglecta, Micarea leprosula, M. peliocarpa, Ochrolechia frigida, Parmelia<br />

saxatilis, and Pseudephebe pubescens. It <strong>of</strong>ten grows over bryophyte mats that are heavily<br />

invaded by gelatinous algae, and in such situations in Scotland it has been found with <strong>the</strong> rare, or<br />

overlooked, Arctomia delicatula and Belonia incarnata. When growing directly on rock M.<br />

lignaria is mostly confined to sheltered, shaded situations and is sometimes present in <strong>the</strong><br />

Micareetum sylvicolae in rock underhangs. It is usually present in abundance in <strong>the</strong> old lead and<br />

zinc mine workings <strong>of</strong> <strong>the</strong> Pennines and Scotland, where it grows over decaying bryophytes and<br />

.

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