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39 2<br />

ECOLOGY<br />

though in dry weather the lichens may be exposed, and can withstand<br />

desiccation for a considerable time :<br />

Pterygium Kenmorensis. Lecidea contigua.<br />

Collema fluviatile.<br />

Lecidea albocoerulescens.<br />

Lecanora lacustris. Dermatocarpon miniatum var. complicaium.<br />

Lecanora epulotica. Dermatocarpon aquaticutil.<br />

Bacidia inundata. Verrncaria laevata.<br />

Rhizocarpum obscuratum. Verrucaria aethiobola.<br />

Rhizocarpum petraeum.<br />

Verrucaria margacea.<br />

The second group of species usually inhabits damp, shaded rocks of<br />

ravines or large boulders by streams or near waterfalls. It includes species<br />

of Collema, Sticta, Peltigera, Solorina, Pannaria, etc., with Opegrapha zonata,<br />

Porina lectissima and Verrucaria nigrescens.<br />

The last-mentioned lichen grows by preference on limestone, but in<br />

excessive moisture 1<br />

importance.<br />

,<br />

as by the sea-side, the substratum seems to be of minor<br />

D. LICHENS AS PIONEERS<br />

a. SOIL-FORMERS. The part played by lichens in the "Economy of<br />

Nature" is of very real importance: to them is allotted the pioneer work<br />

of breaking down the hard rock surfaces and preparing a soil on which<br />

more highly developed plants can grow. This was pointed out by Linnaeus 2<br />

who thus describes the succession of : plants "Crustaceous lichens," he<br />

writes, "are the first foundation of vegetation. Though hitherto we have<br />

considered theirs a trifling place among plants, nevertheless they are of<br />

great importance at that first stage in the economy of nature. When the<br />

rocks emerge from the seas, they are so polished by the force of the waves,<br />

that scarcely any kind of plant could settle on them, seen more especially<br />

near the sea. But very soon, in truth, the smallest crustaceous lichens begin<br />

to cover those arid rocks, and are sustained by minute quantities of soil and<br />

by imperceptible particles brought to them by rain and by the atmosphere.<br />

These lichens in time become converted by decay into a. thin layer of<br />

humus, so that at length imbricate lichens are able to thrust their rhizoids<br />

into it. As these in turn change to humus by natural decay, various mosses<br />

such as Hypnum, BryuDi and Polytrichum follow, and find suitable place<br />

and nourishment. In time there is produced by the dying down of the<br />

mosses such a quantity of soil that herbs and shrubs are able to establish<br />

themselves and maintain their existence."<br />

Similar observations have been made since Linnaeus's day, among others<br />

by Guembel 3 in his account of Lecanora ventosa. Either by the excretion of<br />

carbon dioxide which acidifies the surrounding moisture, or by the mechanical<br />

1 Wheldon and Wilson 1913.<br />

2 Linnaeus 1762.<br />

3 Guembel 1856.

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