Among “rusty” lichens are the British forms, Lecanora lacustris, the thallus of which is normally white, though generally more or less tinged with iron; it inhabits rocks liable to inundation. L. Dicksonii owes its ferruginous colour to the same influences. Lecidea contigua var. flavicunda and L. confluens f. oxydata are rusty conditions of whitish-grey lichens.

Nilson[895] found rusty lichens occurring frequently in the Sarak-Gebirge, more especially on glacier moraines where they were liable, even when uncovered by snow, to be flooded by water from the higher reaches. It is the thallus that is affected by the iron, rarely if ever are apothecia altered in colour.

Bachmann’s Pigment Reactions

Name of Pigment or LichenColourKOHNH₃Ba(OH)₂HNO₃H₂SO₄Special Reactions
Lecidea-greengreencopper or brick-redKOH then HCl: blue
Aspicilia-greengreenHNO₃: brighter green
Bacidia-greengreenvioletvioletHCl: violet
Thalloidima-greengreenvioletindistinctly purple-redHCl: indistinctly purple-red
Rhizoid-greenbluish-greenolive-green to brownolive-green
Biatora atrofuscabluedissolves with greenish-blue colourviolet, then yellow, then decolourizeddissolvesH₂O insoluble
Phialopsis rubrabrick-reddirty purple-redviolet
Lecanora-redpurple-reddeep violet
Sagedia declivumbluish-redblue (green)greenish-blue then grey-blackblue
Verrucaria Hoffmanni f. purpurascensrose-reddark-greendark-greenKOH then HNO₃ then H₂SO₄: violet crystals
Bacidia fuscorubellayellowish-brownvioletvioletviolet
Sphaeromphale clopismoidesleather-browndeep olive-greenKOH, then H₂SO₄, then HNO₃: blackish
Segestria lectissima—peritheciayellow-brownrose-redbright yellowdilute H₂SO₄: bright yellow
Segestria lectissima—entire tissuebrown and colourlessStrong H₂SO₄: deep violet, then grey
Parmelia glomelliferaleather-brownblue, then violet, at last greyCaCl₂O₂: blue, then grey; finally decolourized
Parmelia-brownyellow to blackish-browndirty- to olive-brownbright red-brown

CHAPTER VI
BIONOMICS

A. Growth and Duration

Lichens are perennial plants mostly of slow growth and of long continuance; there can therefore only be approximate calculations either as to their rate of increase in dimensions or as to their duration in time. A series of somewhat disconnected observations have however been made that bear directly on the question, and they are of considerable interest.