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PDF - CES (IISc)

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LICHEN COMMUNITIES: 385<br />

grass that lichens begin to develop, though in the cool damp weather of<br />

autumn and winter, as observed by Wheldon and Wilson 1<br />

certain ,<br />

species<br />

associated with Myxophyceae, such as Collemaceae, may make their appearance,<br />

among others Leptogium scotinum, Collemodium turgidum and Collcma<br />

ceranoides. Watson 2 makes the same observation in his study of sand-dunes.<br />

When the loose sand on the dunes of South Lancashire becomes cemented<br />

by algae and mosses several rare Lecideae are to be found on the decaying<br />

vegetation, and with further accumulation of humus Cladoniae appear and<br />

spread rapidly along with several species of Peltigera and the ubiquitous Parmelia<br />

physodes. The latter starts on dead twigs of Salix repens and spreads<br />

on to the surrounding soil where it forms patches some inches in diameter.<br />

The association also includes Lecidea uliginosa and Bilimbia sphacroides.<br />

On the more inland portions of the dunes numerous rather poorly de-<br />

veloped Cladoniae and Cetraria aculeata were associated, while on the sides<br />

of "slacks" or "dune-pans" Colleina pulposum, Cladonia sylvatica and several<br />

crustaceous lichens covered the soil. The wetter parts of the dunes were<br />

not found to be favourable to lichen growth.<br />

Sandstede 3 found on the sandy shores of Riigen, from the shore upwards:<br />

first a stretch of bare sand, then a few dune grasses with scattered scraps<br />

of Cladoniae, Peltigerae and Cetraria aculeata. Next in order sandbanks<br />

with Parmelia physodes, Cladonia sylvatica, Cl. alcicornis and Stereocanlon<br />

pascliale. All these are species that occur on similar shores in the British<br />

Islands. Sandstede adds an extensive list of maritime species observed by<br />

him in Riigen.<br />

A very careful tabulation of lichens at Blakeney Point in Norfolk was<br />

made 'by McLean 4 and the table on p. 386 is reproduced from his paper.<br />

Sand, he writes, is present in all the associations and the presence or<br />

absence of stones marks the great difference between the two formations<br />

determined by dune and shingle.<br />

(1) Bare sand, which is the first association listed, is an area practically<br />

the few lichen plants, Cladonia furcata and Cetraria<br />

without phanerogams ;<br />

aculeata f. acanthella, are attached by slight embedding<br />

in the soil.<br />

(2) Grey dune. The sand-loving lichens of the associatipn grow in<br />

company with Hypnnm cupressiforme and attain their greatest development.<br />

Other species which also occur there are Parmelia physodes and Evertiia<br />

prunastri var. stictocera.<br />

(3) Derelict dune. This part of the dune formation occurs here and<br />

there on the seaward margin where the grey dune has been worn down by<br />

the wind. It is more shingly, hence the presence of stone lichens; dune<br />

phanerogams are interspersed and with them a few fruticose lichens, such as<br />

Cladonia furcata.<br />

1 Wheldon and Wilson 1915.<br />

S. L.<br />

- Watson 1918'.<br />

3 Sandstede 1904.<br />

* McLean 1915.<br />

2 5

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