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<strong>Additions</strong> <strong>to</strong> <strong>the</strong> <strong>lichen</strong> <strong>flora</strong> <strong>of</strong> <strong>Finl<strong>and</strong></strong>. <strong>II</strong>. <strong>Calcareous</strong> <strong>rocks</strong> <strong>and</strong><br />

associated soils in Lohja<br />

JUHA PYKÄLÄ<br />

Pykälä, J. 2007. <strong>Additions</strong> <strong>to</strong> <strong>the</strong> <strong>lichen</strong> <strong>flora</strong> <strong>of</strong> <strong>Finl<strong>and</strong></strong>. <strong>II</strong>. <strong>Calcareous</strong> <strong>rocks</strong> <strong>and</strong> associated<br />

soils in Lohja. Graphis Scripta 19: 17–32. S<strong>to</strong>ckholm. ISSN 0901-7593.<br />

The <strong>lichen</strong> <strong>flora</strong> <strong>of</strong> calcareous <strong>rocks</strong> <strong>and</strong> lime quarries <strong>and</strong> <strong>the</strong>ir associated soils were studied<br />

in Lohja, in <strong>the</strong> inl<strong>and</strong> <strong>of</strong> SW <strong>Finl<strong>and</strong></strong>. 49 species are new <strong>to</strong> <strong>Finl<strong>and</strong></strong>: Acrocordia conoidea,<br />

Agonimia gelatinosa, A. globulifera, A. vouauxii*, Bacidina arnoldiana, B. delicata, B.<br />

egenula, Bagliet<strong>to</strong>a baldensis, B. parmigerella, Diplo<strong>to</strong>mma lu<strong>to</strong>sum, Hymenelia carnosula,<br />

Lecania sylvestris, Lecanora perpruinosa, L. xanthos<strong>to</strong>ma, Lemmopsis pelodes, Lep<strong>to</strong>gium<br />

magnussonii, Moelleropsis nebulosa, Polyblastia agraria, P. helvetica, P. sepulta,<br />

Pseudosagedia gr<strong>and</strong>is, P. linearis, Sarcogyne distinguenda, Thelidium cataractarum, T.<br />

incavatum, T. olivaceum*, T. pyrenophorum, T. zwackhii, Verrucaria caerulea, V.<br />

cinereoatrata, V. devergens, V. dolosa, V. floerkeana, V. foveolata, V. fusconigrescens, V.<br />

geophila*, V. glauconephela, V. hochstetteri, V. hydrela, V. macros<strong>to</strong>ma, V. maculiformis, V.<br />

murina, V. ochros<strong>to</strong>ma*, V. rejecta, V. ruderum, V. schindleri, V. transiliens*, V. viridula<br />

<strong>and</strong> Vezdaea retigera. Verrucaria pycnosticta is considered as a synonym <strong>of</strong> Bagliet<strong>to</strong>a<br />

baldensis. Species with an asterisk are also new <strong>to</strong> Fennosc<strong>and</strong>ia.<br />

Juha Pykälä, Finnish Environment Institute, Research Programme for Biodiversity, P.O.<br />

Box 140, FIN-00251 Helsinki, <strong>Finl<strong>and</strong></strong>. E-mail: juha.pykala@ymparis<strong>to</strong>.fi<br />

Exposed calcareous rock is known <strong>to</strong> be very rich<br />

in <strong>lichen</strong> species. However, in Fennosc<strong>and</strong>ia<br />

ra<strong>the</strong>r few local or regional <strong>lichen</strong> studies have<br />

been carried out (e.g. Magnusson 1952, Degelius<br />

1956, Fröberg 1989). In <strong>Finl<strong>and</strong></strong> calcareous <strong>rocks</strong><br />

are rare; only 0.1 % percent <strong>of</strong> <strong>the</strong> Finnish<br />

bedrock is calcareous (Söderholm 1925).<br />

Macro<strong>lichen</strong>s <strong>of</strong> calcareous rock in sou<strong>the</strong>rn<br />

<strong>Finl<strong>and</strong></strong> have frequently been collected <strong>and</strong><br />

deposited in Finnish herbaria, but collections <strong>of</strong><br />

crustaceous <strong>lichen</strong>s are ra<strong>the</strong>r scarce <strong>and</strong> mostly<br />

date back <strong>to</strong> <strong>the</strong> late 1800s or early 1900s (e.g.<br />

Vainio 1921).<br />

This paper presents a report <strong>of</strong> species new <strong>to</strong><br />

<strong>Finl<strong>and</strong></strong> from calcareous <strong>rocks</strong>, lime quarries <strong>and</strong><br />

soils associated with <strong>the</strong>se habitats from Lohja,<br />

in <strong>the</strong> inl<strong>and</strong> <strong>of</strong> SW <strong>Finl<strong>and</strong></strong>. Al<strong>to</strong>ge<strong>the</strong>r 49<br />

species new <strong>to</strong> <strong>Finl<strong>and</strong></strong> were identified. Three <strong>of</strong><br />

<strong>the</strong>m have already been listed <strong>to</strong> occur in <strong>Finl<strong>and</strong></strong><br />

by Santesson et al. (2004), based on data from<br />

this work: Bagliet<strong>to</strong>a baldensis, Lep<strong>to</strong>gium<br />

magnussonii <strong>and</strong> Verrucaria viridula. Five<br />

species are new <strong>to</strong> Fennosc<strong>and</strong>ia. Many<br />

specimens are still unidentified, <strong>and</strong> particularly<br />

many Verrucaria specimens do not fit with <strong>the</strong><br />

species previously reported in <strong>Finl<strong>and</strong></strong>.<br />

Material <strong>and</strong> methods<br />

The l<strong>and</strong> area <strong>of</strong> Lohja municipality is c. 278<br />

km 2 . Lohja is well known for its exposed<br />

calcareous bedrock. Limes<strong>to</strong>ne occurs in Lohja<br />

as ra<strong>the</strong>r narrow lenses within a gneissic<br />

substrate (Parras 1954). The largest areas are 50–<br />

100 m wide <strong>and</strong> have been commercially mined<br />

(Parras & Tavela 1954). Fur<strong>the</strong>rmore, many<br />

small lime quarries occur in <strong>the</strong> area. At present,<br />

all open-cast lime quarries are ab<strong>and</strong>oned, but


18 Juha Pykälä GRAPHIS SCRIPTA 19 (2007)<br />

mining continues deep under lake Lohjanjärvi.<br />

The limes<strong>to</strong>ne consists in general <strong>of</strong> calcite<br />

(Parras & Tavela 1954). Limes<strong>to</strong>ne deposits that<br />

have not been mined are very small <strong>and</strong> narrow.<br />

Most calcareous <strong>rocks</strong> in Lohja are mixtures <strong>of</strong><br />

limes<strong>to</strong>ne <strong>and</strong> siliceous <strong>rocks</strong> (mainly quartz or<br />

feldspar gneisses), <strong>the</strong> latter minerals <strong>of</strong>ten<br />

predominating.<br />

<strong>Calcareous</strong> rock is ra<strong>the</strong>r rare in Lohja.<br />

Al<strong>to</strong>ge<strong>the</strong>r, a little more than 60 sites with<br />

exposed calcareous bedrock <strong>and</strong>/or calcareous<br />

boulders are known from in <strong>the</strong> area (Pykälä<br />

1992 <strong>and</strong> unpublished). The calcareous bedrock<br />

is usually shallow, <strong>and</strong> <strong>of</strong>ten mostly covered by<br />

soil. Areas <strong>of</strong> exposed rock or rock with such a<br />

thin layer <strong>of</strong> soil that calcicolous <strong>lichen</strong>s can be<br />

found are <strong>of</strong>ten mosaic-like <strong>and</strong> mixed with<br />

thicker soils with forests. Due <strong>to</strong> <strong>the</strong> mosaic-like<br />

occurrence <strong>of</strong> siliceous <strong>and</strong> calcareous minerals,<br />

as well as forested <strong>and</strong> non-forested areas, it is<br />

somewhat difficult <strong>to</strong> measure <strong>the</strong> <strong>to</strong>tal area <strong>of</strong><br />

exposed calcareous rock. However, most <strong>of</strong> <strong>the</strong>se<br />

sites are very small (1–1000 m 2 ), <strong>the</strong> largest<br />

being c. 2–3 hectares. The largest lime quarries<br />

in Tytyri <strong>and</strong> Ojamo are surrounded by large<br />

areas with waste soils covering some hectares.<br />

Most <strong>of</strong> Lohja belongs <strong>to</strong> <strong>the</strong> biogeographical<br />

province Varsinais-Suomi (V), <strong>and</strong> all sites with<br />

calcareous rock in Lohja are situated within this<br />

province.<br />

In this study 95 % <strong>of</strong> all known sites with<br />

calcareous rock in Lohja were visited. Al<strong>to</strong>ge<strong>the</strong>r<br />

60 sites were studied (55 sites with exposed<br />

calcareous bedrock <strong>and</strong> five with only calcareous<br />

boulders). Species were collected both from<br />

limes<strong>to</strong>ne <strong>and</strong> lime-influenced siliceous minerals.<br />

Both species occurring directly on <strong>the</strong> rock<br />

surface <strong>and</strong> those growing on thin calcareous soil<br />

were studied. <strong>Calcareous</strong> soils by lime quarries<br />

(i.e. quarry waste soil) <strong>and</strong> calcareous boulders<br />

were also studied. This study was mainly carried<br />

out during <strong>the</strong> years 2002–2005, but studies were<br />

also made earlier during <strong>the</strong> period 1990–2001.<br />

Most <strong>of</strong> <strong>the</strong> sites were fully accessible, but inside<br />

<strong>the</strong> Tytyri <strong>and</strong> Ojamo lime quarries some steep<br />

walls occur that could not be studied.<br />

Al<strong>to</strong>ge<strong>the</strong>r c. 2000 specimens were collected.<br />

Particularly, crustaceous <strong>lichen</strong>s were intensively<br />

collected in order <strong>to</strong> cover every locality as<br />

accurately as possible. Specimens are or will be<br />

deposited in H.<br />

Some <strong>of</strong> <strong>the</strong> species reported that are new <strong>to</strong><br />

<strong>Finl<strong>and</strong></strong> were also found from artificial<br />

calcareous habitats such as concrete, cement,<br />

bricks <strong>and</strong> calcareous waste soils or from<br />

siliceous rock. These habitats have been studied<br />

much less intensively. Fur<strong>the</strong>rmore, a few sites<br />

with exposed calcareous rock outside <strong>the</strong> Lohja<br />

area were studied in 2004–2005, <strong>and</strong> some<br />

<strong>lichen</strong>s new <strong>to</strong> <strong>Finl<strong>and</strong></strong> were also found in <strong>the</strong>se<br />

sites. These localities are given after <strong>the</strong> finds<br />

made in Lohja.<br />

The species<br />

Acrocordia conoidea<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. A. conoidea occurred on ra<strong>the</strong>r<br />

shady walls <strong>of</strong> calcareous <strong>rocks</strong> <strong>and</strong> lime<br />

quarries. The species also grows elsewhere in<br />

shady habitats (Purvis 1992a). Peri<strong>the</strong>cia were<br />

smaller (0.2–0.4 mm) than reported in von<br />

Keissler (1938), Purvis (1992a), <strong>and</strong> Foucard<br />

(2001).<br />

Specimens examined: Hermala, Pietilä, lime<br />

quarry, on S-facing wall, 60°13'N, 23°51'E,<br />

30.IX.2004, 25875; Ojamo, Kalkkisaari, small<br />

lime quarry, on N-facing wall, 60°14'N, 24°01'E,<br />

31.<strong>II</strong>I.2005, 26400; Torhola, Torhola cave, on<br />

high shady SW-facing wall <strong>of</strong> calcareous rock,<br />

60°15'N, 23°51'E, 25.V<strong>II</strong>.2005, 27427.<br />

Agonimia gelatinosa<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. A. gelatinosa is widely<br />

distributed in Sweden <strong>and</strong> Norway (Santesson et<br />

al. 2004) <strong>and</strong> has apparently been overlooked in<br />

<strong>Finl<strong>and</strong></strong>.<br />

Specimens examined: Ojamo, Ojamo lime quarry,<br />

waste soil (s<strong>and</strong> <strong>and</strong> gravel), on open S-facing<br />

slope <strong>and</strong> on bushy NW-facing slope, 60°14'N,<br />

24°02'E,15.XI.2003, 24092, 18.IV.2005, 26564,<br />

26565, 26567, 26577, 26607; Lohja, Tytyri, lime


GRAPHIS SCRIPTA 19 (2007) <strong>Additions</strong> <strong>the</strong> <strong>the</strong> <strong>lichen</strong> <strong>flora</strong> <strong>of</strong> <strong>Finl<strong>and</strong></strong> 19<br />

quarry, on soil, 60°16'N, 24°04'E, 8.XI.2003,<br />

24017; Hermala, Kalkkimäki, 60°13'N, 23°52'E,<br />

SW slope on thin soil among bryophytes,<br />

15.V.2004, 24659, SE-facing c. 1 m high wall <strong>of</strong><br />

calcareous rock in Picea abies dominated forest,<br />

on bryophytes, 19.V<strong>II</strong>.2004, 25131, <strong>and</strong> on semiopen<br />

flat calcareous rock among bryophytes<br />

1.IX.2005, 27834; Ojamo, Kalkkisaari, lime<br />

quarry, S slope, on silty soil, 60°14'N, 24°01'E,<br />

31.<strong>II</strong>I.2005, 26403.<br />

Agonimia globulifera<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. A. globulifera has a diminutive<br />

thallus <strong>and</strong> is characterized by many small (70–<br />

200 µm), black, shiny globules (Sérusiaux et al.<br />

1999). Peri<strong>the</strong>cia are rare. In Fennosc<strong>and</strong>ia A.<br />

globulifera has been previously found in Öl<strong>and</strong><br />

(Santesson et al. 2004) <strong>and</strong> <strong>the</strong> species was also<br />

recently recorded in Es<strong>to</strong>nia (Suija et al. 2005).<br />

Specimens examined: Skraatila, Kirkkovuori,<br />

calcareous rock, SW-slope, on bryophytes,<br />

scarce, 60°15'N, 23°54'E, 21.V<strong>II</strong>.2004, 25217,<br />

det. B. J. Coppins 2006; Lohja, Pitkäniemi<br />

industrial area, 5 m from shore <strong>of</strong> lake<br />

Lohjanjärvi, deciduous forest, lime-influenced<br />

quartz-feldspar gneiss rock, on W-facing wall, on<br />

bryophytes, 60°15'N, 24°02'E, 19.V<strong>II</strong>I.2005,<br />

27636.<br />

Agonimia vouauxii (de Lesd.) Br<strong>and</strong> & Diederich<br />

New <strong>to</strong> Fennosc<strong>and</strong>ia. A. vouauxii usually grows<br />

on mosses or soil. It resembles Polyblastia<br />

agraria, but has a granulose-squamulose thallus,<br />

subspherical peri<strong>the</strong>cia <strong>and</strong> larger hyaline spores<br />

(40–)60–72(–87) × 15–24 (–31) µm; Sérusiaux et<br />

al. 1999). In <strong>the</strong> Lohja collection, spore size was<br />

60–73 x 23–33 µm. The very few asci seen with<br />

spores had three spores, which is somewhat<br />

curious. Only few collections <strong>of</strong> A. vouauxii are<br />

known from France, Belgium <strong>and</strong> Austria<br />

(Sérusiaux et al. 1999), Germany (Rätzel et al.<br />

2004), Denmark (Søchting & Alstrup 2002) <strong>and</strong><br />

Hong Kong (Aptroot & Seaward 1999).<br />

Specimen examined: Hiittinen, SW exposed<br />

calcareous rock, scarcely growing on bryophytes,<br />

60°16'N, 24°03'E, 21.V<strong>II</strong>.2005, 27384.<br />

Bacidina arnoldiana<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. B. arnoldiana grows on shady<br />

calcareous <strong>rocks</strong>, on s<strong>to</strong>nework <strong>and</strong> on bark <strong>of</strong><br />

deciduous trees (Coppins 1992, Foucard 2001).<br />

Specimen examined: Hermala, Laakspohja, on Sfacing<br />

wall <strong>of</strong> small calcareous rock in deciduous<br />

herb-rich forest, 60°13'N, 23°50'E, 30.V<strong>II</strong>I.2003,<br />

23544.<br />

Bacidina delicata<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. B. delicata grows on deciduous<br />

trees, calcareous <strong>rocks</strong>, concrete <strong>and</strong> s<strong>to</strong>nework<br />

(Coppins 1992, Wirth 1995). In Sweden <strong>the</strong><br />

species has been found growing in semi-open<br />

forests mainly on Sambucus nigra, but also on<br />

o<strong>the</strong>r deciduous trees (Arup 1999).<br />

Specimens examined: Lohja, Kiviniemi, lime<br />

quarry, on N-facing rock wall, scarce, 60°15'N,<br />

24°03'E, 11.V<strong>II</strong>.2003, 23179; Lohja, gravelly soil<br />

by building on Lohjanharju esker, on pebbles,<br />

scarce, 60°14'N, 24°04'E, 31.X.2003, 23939.<br />

Bacidina egenula<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. B. egenula is mainly a species <strong>of</strong><br />

siliceous <strong>rocks</strong> (Wirth 1995, Foucard 2001).<br />

However, <strong>the</strong> find in Lohja was from calcareous<br />

rock where <strong>the</strong> species was associated with e. g.<br />

Bagliet<strong>to</strong>a baldensis.<br />

Specimen examined: Lohja, Pohjolanmäki, on<br />

small, flat calcareous rock, shaded by trees,<br />

scarce, 60°15'N, 24°04'E, 24.IX.2005, 28054.<br />

Bagliet<strong>to</strong>a baldensis<br />

The species grew on calcareous <strong>rocks</strong> on flat,<br />

sloping <strong>and</strong> vertical surfaces. It is a ra<strong>the</strong>r shade<strong>to</strong>lerant<br />

species occurring mainly on half-shady<br />

or shady habitats in <strong>the</strong> study sites. According <strong>to</strong><br />

Halda (2003), two Bagliet<strong>to</strong>a species occur in<br />

Fennosc<strong>and</strong>ia: B. baldensis has a white – grey<br />

thallus <strong>and</strong> <strong>the</strong> size <strong>of</strong> <strong>the</strong> involucrellum is 200–


20 Juha Pykälä GRAPHIS SCRIPTA 19 (2007)<br />

300 µm. B. parmigerella has a green – blue green<br />

thallus <strong>and</strong> <strong>the</strong> size <strong>of</strong> <strong>the</strong> involucrellum is 100–<br />

150 µm. However, in <strong>the</strong> Lohja material <strong>of</strong> B.<br />

baldensis <strong>the</strong> involucrellum size varied between<br />

130–300 µm. No spores were found in <strong>the</strong><br />

Finnish material. Apparently spore formation <strong>of</strong><br />

<strong>the</strong> species is rare in <strong>Finl<strong>and</strong></strong>, if it occurs at all.<br />

Therefore, B. baldensis disperses poorly <strong>to</strong><br />

worked rock surface. Fur<strong>the</strong>rmore, o<strong>the</strong>r fac<strong>to</strong>rs<br />

such as poor establishment <strong>of</strong> <strong>the</strong> species on<br />

worked surfaces may also be putative<br />

explanations for <strong>the</strong> general lack <strong>of</strong> <strong>the</strong> species in<br />

lime quarries. Only one population was found on<br />

rock surface exposed after mining. The species<br />

occurred c. 10–30 centimetres from <strong>the</strong> edge <strong>of</strong><br />

<strong>the</strong> mined rock, <strong>and</strong> probably dispersed<br />

vegetatively <strong>to</strong> <strong>the</strong> mined rock. Because <strong>of</strong> its<br />

poor spore formation B. baldensis has probably<br />

clearly declined due <strong>to</strong> mining <strong>of</strong> calcareous<br />

<strong>rocks</strong>. The overgrowth <strong>of</strong> <strong>rocks</strong> by bryophytes<br />

may also be a problem for <strong>the</strong> species, because<br />

populations <strong>of</strong> B. baldensis are <strong>of</strong>ten surrounded<br />

by empty pits on <strong>rocks</strong> beneath bryophytes.<br />

Specimens examined: 14 localities in Lohja, first<br />

collection: Hermala, Tolpoonkallio, 60°13'N,<br />

23°50'E, 18.VI.1996, 16845. Varsinais-Suomi:<br />

Karjalohja, Niku, Pyöli, 60°12'N, 23°49'E,<br />

6.V<strong>II</strong>.2004, 24976; Karjalohja, Karkali, E <strong>of</strong><br />

Karkali nature reserve, 60°14'N, 23°50'E,<br />

19.X.2004, 26094; Nummi-Pusula, Pusula,<br />

Kalkkimäki, 60°28'N, 24°00'E, 14.X.2004,<br />

26033, 26039.<br />

Type specimens <strong>of</strong> Verrucaria pycnosticta Vain.<br />

(Vainio 1921) (Varsinais-Suomi, Särkisalo,<br />

Kaukasalo, 1920, E. Vainio (TUR-V)) are<br />

considered <strong>to</strong> belong <strong>to</strong> B. baldensis. They have<br />

radiating ostioles, <strong>and</strong> <strong>the</strong>y look similar <strong>to</strong> B.<br />

baldensis. No spores were found in <strong>the</strong> type<br />

material. According <strong>to</strong> <strong>the</strong> pro<strong>to</strong>logue (Vainio<br />

1921) <strong>the</strong> size <strong>of</strong> <strong>the</strong> spores <strong>of</strong> V. pycnosticta is<br />

6–10 × 5–6 µm <strong>and</strong> Vainio described <strong>the</strong>m as<br />

scarce <strong>and</strong> not well developed. The spore size<br />

given by Vainio is apparently erroneous. Vainio<br />

also assigned a specimen from Norway (1910 J.<br />

J. Havaas, TUR-V) <strong>to</strong> V. pycnosticta. According<br />

<strong>to</strong> Vainio's annotation label no spores were found<br />

in <strong>the</strong> Norwegian specimen. This specimen also<br />

belongs <strong>to</strong> B. baldensis.<br />

Bagliet<strong>to</strong>a parmigerella (Zahlbr.) Vĕzda & Poelt<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. B. parmigerella occurs in central<br />

<strong>and</strong> sou<strong>the</strong>rn Europe <strong>and</strong> Asia <strong>and</strong> in<br />

Fennosc<strong>and</strong>ia it has been collected a few times<br />

from Gotl<strong>and</strong> (Halda 2003). In Lohja B.<br />

parmigerella occurs in habitats similar <strong>to</strong> those<br />

occupied by B. baldensis, but is a rarer species.<br />

No spores were found in <strong>the</strong> Finnish material. In<br />

Ojamo lime quarry only rock exposed after<br />

mining appears <strong>to</strong> be available. However, it is<br />

uncertain that <strong>the</strong> small population (c. 10 cm 2 ) <strong>of</strong><br />

B. parmigerella has originated by recent spore<br />

dispersal. It is also possible that <strong>the</strong> species has<br />

persisted on rock despite <strong>the</strong> mining process.<br />

Specimens examined: Ojamo, Liessaari, on NWfacing<br />

wall <strong>of</strong> calcareous rock, 60°14'N, 24°01'E,<br />

22.IV.2003, 22632, 15.IV.2005, 26523; Hermala,<br />

Kalkkimäki, on small flat calcareous rock <strong>and</strong> on<br />

c. 0.7 m high SE-facing rock wall <strong>of</strong> calcareous<br />

rock, 60°13'N, 23°51'E, 29.V<strong>II</strong>I.2003, 23492,<br />

19.V<strong>II</strong>.2004, 25132; Lylyinen, Sääksniemi, on<br />

small ra<strong>the</strong>r flat calcareous rock, 60°15'N,<br />

23°58'E, 16.IX.2003, 23701; Ojamo, Ojamo lime<br />

quarry, open SW slope, very scarce, 60°14'N,<br />

24°02'E, 15.XI.2003, 24085; Paavola,<br />

Rautaniemi, on calcareous s<strong>to</strong>nes, 60°13'N,<br />

23°54'E, 21.V.2005, 26870, 26881.<br />

Diplo<strong>to</strong>mma lu<strong>to</strong>sum<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. D. lu<strong>to</strong>sum is a rare species in<br />

Fennosc<strong>and</strong>ia, occurring mainly on calcareous<br />

rock walls in open situations (Nordin 2000).<br />

Specimen examined: Lohja, Pitkäniemi industrial<br />

area, 5 m from shore <strong>of</strong> lake Lohjanjärvi,<br />

deciduous forest, lime-influenced quartz-feldspar<br />

gneissic rock, on overhanging W-facing rock<br />

wall, 60°15'N, 24°02'E, 19.V<strong>II</strong>I.2005, 27634, det.<br />

A. Nordin 2006.


GRAPHIS SCRIPTA 19 (2007) <strong>Additions</strong> <strong>the</strong> <strong>the</strong> <strong>lichen</strong> <strong>flora</strong> <strong>of</strong> <strong>Finl<strong>and</strong></strong> 21<br />

Hymenelia carnosula<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. H. carnosula was mainly found<br />

in lime quarries <strong>and</strong> on rock cuttings <strong>of</strong> road<br />

banks. It was only once seen on non-worked<br />

calcareous rock, growing very sparsely on flat<br />

calcareous rock surrounded by dry grassl<strong>and</strong>. The<br />

material collected from Lohja differs from <strong>the</strong><br />

description <strong>of</strong> H. carnosula by Magnusson<br />

(1933) <strong>and</strong> Foucard (2001) in having a higher<br />

hymenium <strong>and</strong> slightly bigger spores. The height<br />

<strong>of</strong> <strong>the</strong> hymenium varies between 50 <strong>and</strong> 100 µm.<br />

However, <strong>the</strong> apo<strong>the</strong>cia are small (0.2 mm) <strong>and</strong><br />

<strong>the</strong> hymenium is I+ blue, which are diagnostic<br />

characters <strong>of</strong> H. carnosula (Jørgensen 1989).<br />

Specimens examined: Hermala, Kalkkimäki, on<br />

wall <strong>of</strong> two lime quarries, 60°13'N, 23°52'E,<br />

18.VI.2003, 23009, 29.V<strong>II</strong>I.2003, 23498; Lohja,<br />

by <strong>the</strong> Tytyri lime processing fac<strong>to</strong>ry, on road<br />

cutting <strong>of</strong> calcareous rock, scarce, 60°15'N,<br />

24°04'E, 8.XI.2003, 24008; Hermala,<br />

Tolpoonkallio, in a lime quarry, 60°13'N,<br />

23°50'E, 29.V.2004, 24806, 24810; Hermala,<br />

Kyttälä, on flat calcareous rock, very scarce,<br />

60°13'N, 23°51'E, 6.V<strong>II</strong>.2004, not collected due<br />

<strong>to</strong> scarcity; Hermala, Pietilä, on road cutting <strong>of</strong><br />

calcareous rock, 60°13'N, 23°51'E, 30.IX.2004,<br />

25915; Ojamo, Ojamo lime quarry, ra<strong>the</strong>r<br />

abundant, 60°14'N, 24°02'E, 6.X.2004, 25947,<br />

25960, 26019; Lohja, Tytyri, lime quarry, on<br />

high wall, 60°16'N, 24°04'E, 9.XI.2004, 26177;<br />

Lehmijärvi, ab<strong>and</strong>oned s<strong>and</strong> pit, on concrete<br />

boulders, 60°16'N, 24°08'E, 6.V<strong>II</strong>I.2005, 27469,<br />

27488.<br />

Lecania sylvestris<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. L. sylvestris mainly grows on<br />

shaded calcareous <strong>rocks</strong> (James & Purvis 1992).<br />

The species has been previously found in<br />

Fennosc<strong>and</strong>ia only in Gotl<strong>and</strong> in <strong>the</strong> mid-1800s<br />

(Santesson et al. 2004). It was recently found in<br />

Denmark (Alstrup et al. 2004).<br />

Specimens examined: Seppälä, Mustasaari, on<br />

calcareous rock on <strong>the</strong> shore <strong>of</strong> lake Lohjanjärvi,<br />

scarce, 60°14'N, 23°51'E, 10.V<strong>II</strong>I.2004, 25391 &<br />

R. Mur<strong>to</strong>; Hiittinen, on N-facing road cutting <strong>of</strong><br />

calcareous rock, in shady microhabitat, scarce,<br />

60°16'N, 24°03'E, 21.V<strong>II</strong>.2005, 27394.<br />

Lecanora perpruinosa<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. L. perpruinosa may be a ra<strong>the</strong>r<br />

rare, but widely distributed species in Europe<br />

(Fröberg 1989, Poelt & Leuckert 1995). It is also<br />

recorded from Canada (McMillan & Larson<br />

2002). In Lohja L. perpruinosa grew on sunexposed<br />

calcareous <strong>rocks</strong>.<br />

Specimens examined: Hermala, Kyttälä, back<br />

yard, on flat calcareous rock, scarce, 60°13'N,<br />

23°51'E, 6.V<strong>II</strong>.2004, 24988, det. L. Fröberg<br />

2006; Skraatila, Kirkkovuori, on steep SW-facing<br />

calcareous rock, 60°15'N, 23°54'E, 21.V<strong>II</strong>.2004,<br />

25220, det. L. Fröberg 2006; Lohja, Tytyri lime<br />

quarry, on probably gneissic s<strong>to</strong>ne enriched by<br />

calcareous dust, 60°16'N, 24°04'E, 12.V<strong>II</strong>I.2004,<br />

25455, det. L. Fröberg 2006.<br />

Lecanora xanthos<strong>to</strong>ma<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. L. xanthos<strong>to</strong>ma may have been<br />

overlooked as a small-sized L. flo<strong>to</strong>wiana. The<br />

species is difficult <strong>to</strong> separate from L. flo<strong>to</strong>wiana<br />

<strong>and</strong> intermediates are <strong>of</strong>ten found (Fröberg<br />

1997).<br />

Specimens examined: Lohja, Tytyri, on edge <strong>of</strong><br />

Tytyri lime quarry, on flat rock surface, 60°16'N,<br />

24°04'E, 20.IV.2005, 26618 & J. Rikkinen, conf.<br />

L. Fröberg 2005; Marttila, on small calcareous<br />

rock, 60°14'N, 23°52'E, 21.VI.2005, 27081;<br />

Lohja, Pitkäniemi, in a lime quarry, 60°15'N,<br />

24°03'E, 23.V<strong>II</strong>I.2005, 27724.<br />

Lemmopsis pelodes<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. L. pelodes is a globally rare<br />

pioneer species <strong>of</strong> ra<strong>the</strong>r naked calcareous soil.<br />

The species has been found only once before in<br />

Fennosc<strong>and</strong>ia (Uppl<strong>and</strong>, Sweden in 1947)<br />

(Jørgensen & Motiejūnaité 2005). In <strong>the</strong> Tytyri<br />

locality some o<strong>the</strong>r rare species <strong>of</strong> calcareous<br />

soils occurred: Lep<strong>to</strong>gium bia<strong>to</strong>rinum, Thelidium<br />

zwackhii, Verrucaria bryoc<strong>to</strong>na <strong>and</strong> V. xyloxena.<br />

In Hermala L. pelodes was accompanied by<br />

Lep<strong>to</strong>gium tenuissimum.


22 Juha Pykälä GRAPHIS SCRIPTA 19 (2007)<br />

Specimens examined: Pappila, E <strong>of</strong> Tytyri lime<br />

quarry, open quarry waste soil (c. 10 years old),<br />

on clay soil heap, scarce, 60°16'N, 24°04'E,<br />

27.X.2001, 21100, conf. P. M. Jørgensen 2006;<br />

Hermala, Kalkkimäki, road cutting <strong>of</strong> calcareous<br />

rock, on thin soil over a rock, scarce, 60°13'N,<br />

23°51'E, 18.VI.2003, 23017, conf. P. M.<br />

Jørgensen 2006.<br />

Lep<strong>to</strong>gium magnussonii<br />

This species was described from Sweden <strong>and</strong><br />

Norway by Jørgensen (1994) from siliceous<br />

<strong>rocks</strong> with fresh-water seepage. Later L.<br />

magnussonii has been reported from several o<strong>the</strong>r<br />

European countries: Austria (Berger 1996),<br />

Portugal (van den Boom & Giralt 1996),<br />

Belgium, Luxembourg, France <strong>and</strong> Germany<br />

(Sérusiaux et al. 1999), Czech (Gut<strong>to</strong>va 2000),<br />

Bulgaria (Pisūt 2001) <strong>and</strong> Hungary (Czeika et al.<br />

2004). In Sweden L. magnussonii mainly grows<br />

on open, grazed, flowing water influenced <strong>rocks</strong><br />

(Hultengren 1999). The locality in Lohja is<br />

situated at <strong>the</strong> edge <strong>of</strong> an arable field. The<br />

population is just above rock cutting <strong>of</strong> a road<br />

bank or perhaps partly on previously cut rock.<br />

Specimen examined: Paloniemi, Luhtalahti, on<br />

SW-facing calciferous quartz-feldspar gneissic<br />

rock, scarce, 60°16'N, 24°01'E, 2.IX.1993,<br />

12263, det. P. M. Jørgensen 1998.<br />

Moelleropsis nebulosa<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. There are very few recent finds<br />

<strong>of</strong> M. nebulosa in Fennosc<strong>and</strong>ia (Ekman et al.<br />

2000). The species is red-listed in Sweden<br />

(Gärdenfors 2005). M. nebulosa has also<br />

declined in <strong>the</strong> British Isles (Purvis & James<br />

1992). No apo<strong>the</strong>cia were found in <strong>the</strong> Finnish<br />

populations, which were small. The species is<br />

easily overlooked <strong>and</strong> probably more common<br />

than is known at present. However, due <strong>to</strong><br />

eutrophication <strong>and</strong> overgrowth after<br />

ab<strong>and</strong>onment <strong>of</strong> grassl<strong>and</strong>s M. nebulosa is<br />

probably also in decline in <strong>Finl<strong>and</strong></strong>.<br />

Specimens examined: Paavola, N <strong>of</strong> Paavola<br />

school, small calcareous rock, on thin soil,<br />

scarce, 60°13'N, 23°53'E, 18.VI.2005, 27040;<br />

Marttila, calcareous rock, on thin soil, scarce,<br />

60°14'N, 23°52'E, 21.VI.2005, 27082. Varsinais-<br />

Suomi: Karjalohja, Pyöli, Niku, calcareous rock,<br />

on thin soil, scarce, 60°12'N, 23°48'E,<br />

6.V<strong>II</strong>.2004, 24982; conf. P. M. Jørgensen 2006;<br />

Halikko, Kuttila, Päivärinne, SW slope, mesic<br />

semi-natural grassl<strong>and</strong> grazed by cattle, on<br />

clayey soil, 60°28'N, 23°00'E, 24.V<strong>II</strong>I.2004,<br />

25563; conf. P. M. Jørgensen 2006.<br />

Polyblastia agraria<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. P. agraria is a rare calcicolous<br />

species found in central <strong>and</strong> nor<strong>the</strong>rn Europe. It<br />

is known from Sweden (Santesson et al. 2004),<br />

<strong>the</strong> British Isles (Swinscow 1971), Pol<strong>and</strong><br />

(Ceynowa-Gieldon 1998), Czech (Vězda & Liskǎ<br />

1999), Lithuania (Motiejūnaité et al. 1998) <strong>and</strong><br />

Denmark (Alstrup et al. 2004). P. agraria<br />

occurred in <strong>the</strong> study area on moribund <strong>lichen</strong> or<br />

bryophyte thalli in calcareous habitats.<br />

Populations appeared <strong>to</strong> be small. Due <strong>to</strong> its<br />

minute size <strong>the</strong> species is difficult <strong>to</strong> observe in<br />

<strong>the</strong> field.<br />

Specimens examined: Hermala, Kyttälä, flat<br />

calcareous rock, on dead thallus <strong>of</strong> Peltigera,<br />

60°13'N, 23°51'E, 6.V<strong>II</strong>.2004, 24984; Vappula,<br />

N <strong>of</strong> Väinölä, on bank <strong>of</strong> Lohjanharju road,<br />

60°13'N, 24°01'E, 30.IX.2004, within 25935,<br />

Vezdaea acicularis (Pykälä 2006); Hermala,<br />

Tolpoonkallio, flat calcareous rock, thin soil, on<br />

moribund <strong>lichen</strong> thallus, scarce, 60°13'N,<br />

23°50'E, 18.VI.2005, 27059; Skraatila,<br />

Päiväranta SW, on calcareous rock, among<br />

bryophytes, scarce, 60°15'N, 23°53'E,<br />

24.V<strong>II</strong>I.2005, 27771.<br />

Polyblastia helvetica<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. P. helvetica is a rare arcticalpine<br />

species. It is known from <strong>the</strong> Alps<br />

(Zschacke 1933), Carpathians (Bielczyk et al.<br />

2004, Lisická 2005), Scotl<strong>and</strong> (Swinscow 1971),<br />

<strong>the</strong> Faroe Isl<strong>and</strong>s (Degelius 1982), Greenl<strong>and</strong><br />

(Hansen 1998) <strong>and</strong> Icel<strong>and</strong> (Berger 2000). Only


GRAPHIS SCRIPTA 19 (2007) <strong>Additions</strong> <strong>the</strong> <strong>the</strong> <strong>lichen</strong> <strong>flora</strong> <strong>of</strong> <strong>Finl<strong>and</strong></strong> 23<br />

one previous collection from nor<strong>the</strong>rn Norway is<br />

known from Fennosc<strong>and</strong>ia (Degelius 1982). The<br />

find in <strong>Finl<strong>and</strong></strong> on <strong>the</strong> border <strong>of</strong> <strong>the</strong> sou<strong>the</strong>rn <strong>and</strong><br />

hemiboreal vegetation zones is a considerable<br />

range extension for this arctic-alpine species. P.<br />

helvetica is easily recognized by having only two<br />

very large, brown spores per ascus (Zschacke<br />

1933, Swinscow 1971). In <strong>the</strong> Lohja collection<br />

spore size was 75–94 × 30–37 µm.<br />

Specimen examined: Ojamo, Ojamo lime quarry,<br />

on open quarry waste l<strong>and</strong> on s<strong>to</strong>ny <strong>and</strong> gravelly<br />

soil, scarce, 60°14'N, 24°02'E, 18.IV.2005,<br />

26594.<br />

Polyblastia sepulta<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. P. sepulta is a calcicolous <strong>lichen</strong><br />

known from <strong>the</strong> central European mountains<br />

(Zschacke 1933, Moruzi et al. 1967) <strong>and</strong> Norway<br />

<strong>and</strong> Sweden (Santesson et al. 2004).<br />

Specimens examined: Lohja, Tytyri lime quarry,<br />

on flat calcareous rock, 60°16'N, 24°04'E,<br />

20.IV.2005, 26619 & J. Rikkinen; Lohja,<br />

Pitkäniemi, calcareous rock, 60°15'N, 24°02'E,<br />

19.V<strong>II</strong>I.2005, on NW-facing wall, 27630, on Wfacing<br />

wall <strong>of</strong> calcareous boulder, 27643, <strong>and</strong> on<br />

flat rock on lakeshore, 27557.<br />

Pseudosagedia gr<strong>and</strong>is<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. P. gr<strong>and</strong>is is a rare species <strong>of</strong><br />

wet siliceous or moderately calcareous <strong>rocks</strong> <strong>of</strong><br />

shady habitats (Botnen & Tønsberg 1988). It is<br />

known from Germany, Scotl<strong>and</strong>, Sweden <strong>and</strong><br />

Norway (Thor 1999a). The species has not been<br />

refound in its only known Swedish locality (Thor<br />

1999a). Peri<strong>the</strong>cia <strong>of</strong> P. gr<strong>and</strong>is are large (0.5–<br />

0.8 mm). Thus, <strong>the</strong> species is ra<strong>the</strong>r conspicuous.<br />

In Lohja P. gr<strong>and</strong>is grew sparsely on limeinfluenced<br />

gneissic rock a few meters from <strong>the</strong><br />

shore <strong>of</strong> lake Lohjanjärvi. Before <strong>the</strong> lowering <strong>of</strong><br />

<strong>the</strong> water table <strong>of</strong> lake Lohjanjärvi c. 150 years<br />

ago, <strong>the</strong> site was probably situated in <strong>the</strong> lit<strong>to</strong>ral<br />

zone. The small population may be <strong>of</strong> relict<br />

occurrence.<br />

Specimen examined: Paloniemi, Muutettavanniemi,<br />

on small NW-facing wall <strong>of</strong> limeinfluenced<br />

gneiss rock, very scarce, 60°15'N,<br />

24°01'E, 28.IV.2005, 26676.<br />

Pseudosagedia linearis<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. P. linearis is rare in<br />

Fennosc<strong>and</strong>ia, <strong>and</strong> is known in Sweden only<br />

from Gotl<strong>and</strong> <strong>and</strong> Öl<strong>and</strong> (Santesson et al. 2004).<br />

The Finnish locality was shaded by deciduous<br />

trees. P. linearis grew on an overhanging surface<br />

accompanied by <strong>the</strong> rare shade-dem<strong>and</strong>ing<br />

bryophyte Seligeria donniana.<br />

Specimen examined: Torhola, Torhola cave, on a<br />

SW-facing wall <strong>of</strong> calcareous rock, scarce,<br />

60°15'N, 23°51'E, 16.V<strong>II</strong>.2004, 25061.<br />

Sarcogyne distinguenda<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. S. distinguenda is a rarely<br />

collected species <strong>of</strong> calcareous <strong>rocks</strong> in Norway<br />

<strong>and</strong> Sweden (Botnen & Tønsberg 1988, Thor<br />

1999b) <strong>and</strong> has also been reported from Austria<br />

(Hafellner & Türk 2001). In Norway it has been<br />

collected once on cement (Thor 1999b).<br />

Specimens examined: Paloniemi, Luhtalahti, road<br />

cutting <strong>of</strong> calcareous quartz-feldspar gneissic<br />

rock, on a SW-facing rock wall, scarce, 60°16'N,<br />

24°01'E, 28.IV.2005, 26710; Laakspohja, W <strong>of</strong><br />

Lempolantie road, pine plantation, on concrete<br />

boulder, 60°15'N, 24°06'E, 30.X. 2005, 28238.<br />

Thelidium cataractarum<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. The species may have been<br />

overlooked, because it is macroscopically similar<br />

<strong>to</strong> Verrucaria muralis. The Lohja locality was<br />

strongly enriched by calcareous dust. T.<br />

cataractarum occurred sparsely with <strong>the</strong> more<br />

abundant V. muralis.<br />

Specimens examined: Lohja, by <strong>the</strong> Tytyri lime<br />

processing fac<strong>to</strong>ry, on a road cutting with<br />

calcareous rock, 60°15'N, 24°04'E, 14.I.2005,<br />

26204. Uusimaa: Helsinki, Vuosaari, Kalkkisaari,<br />

calcareous rock by a lime quarry, on<br />

pebble, 60°13'N, 25°11'E, 20.IX.2005, 27954.


24 Juha Pykälä GRAPHIS SCRIPTA 19 (2007)<br />

Thelidium incavatum<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. T. incavatum is a species <strong>of</strong><br />

calcareous <strong>rocks</strong>, s<strong>to</strong>nes <strong>and</strong> pebbles occurring<br />

usually close <strong>to</strong> <strong>the</strong> ground (Fröberg 1989,<br />

Foucard 2001). In Lohja <strong>the</strong> species occurs both<br />

on sun-exposed <strong>and</strong> shady calcareous <strong>rocks</strong> <strong>and</strong><br />

pebbles.<br />

Specimens examined: Lohja, Tytyri, lime quarry,<br />

on pebbles <strong>and</strong> on a small rock wall, 60°16'N,<br />

24°04'E, 24.V.2003, 22861b, 8.XI.2003, 24020,<br />

14.1.2005, 26229; Lohja, by <strong>the</strong> Tytyri lime<br />

processing fac<strong>to</strong>ry, on a road cutting <strong>of</strong><br />

calcareous rock, 60°15'N, 24°04'E, 14.I.2005,<br />

26198; Marttila, on a small flat calcareous rock,<br />

60°14'N, 23°52'E, 21.VI.2005, 27083; Moisio,<br />

Lohjanharju esker, on a calcareous boulder,<br />

60°15'N, 24°06'E, 30.X.2005, 28218, 28219.<br />

Varsinais-Suomi: Karjalohja, Pyöli, on a very<br />

gently SW-facing almost flat calcareous rock,<br />

60°12'N, 23°48'E, 6.V<strong>II</strong>.2004, 24956, 24965.<br />

Uusimaa: Helsinki, Vuosaari, Kalkkisaari, on<br />

wall <strong>of</strong> lime quarry, <strong>and</strong> on pebbles, 60°13'N,<br />

25°11'E, 20.IX.2005, 27934, 27944, 27956.<br />

Thelidium olivaceum (Fr.) Körb.<br />

New <strong>to</strong> Fennosc<strong>and</strong>ia. T. olivaceum is a<br />

circumboreal species, which is most frequent in<br />

<strong>the</strong> central <strong>and</strong> sou<strong>the</strong>rn European mountains<br />

(Nimis 1993). The nearest sites <strong>to</strong> <strong>Finl<strong>and</strong></strong> are in<br />

Latvia (Lichen <strong>flora</strong> <strong>of</strong> Latvia) <strong>and</strong> Denmark<br />

(Søchting & Alstrup 2002). The T. olivaceum<br />

material from Lohja has a thin, brown thallus,<br />

small 1/4–3/4-immersed peri<strong>the</strong>cia (0.15–0.3<br />

mm), <strong>and</strong> <strong>the</strong> spores are (0–)1-septate <strong>and</strong> 15–22<br />

× (5–)6–9 µm in size. The involucrellum <strong>of</strong>ten<br />

reaches <strong>to</strong> <strong>the</strong> base <strong>of</strong> <strong>the</strong> peri<strong>the</strong>cia, <strong>and</strong> <strong>the</strong><br />

exciple is pale. The characters <strong>of</strong> <strong>the</strong> collections<br />

<strong>of</strong> Lohja fit well with <strong>the</strong> description <strong>of</strong> T.<br />

olivaceum by Zschacke (1933). According <strong>to</strong><br />

Wirth (1995), <strong>the</strong> spores <strong>of</strong> T. olivaceum tend <strong>to</strong><br />

be broader: 16–22(–34) × 7–12(–14) µm.<br />

Specimens examined: Lohja-Pappila, Tytyri, lime<br />

quarry, on calcareous s<strong>to</strong>nes, 60°16'N, 24°04'E,<br />

7.X. 2000, 20045, 24.V.2003, 22848, 22850;<br />

Lohja, Pitkäniemi, shore <strong>of</strong> lake Lohjanjärvi,<br />

60°15'N, 24°02'E, 19.V<strong>II</strong>I.2005, on a flat<br />

calcareous rock, 27563, <strong>and</strong> on a NW-facing rock<br />

wall, 27598.<br />

Thelidium pyrenophorum<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. T. pyrenophorum is a<br />

circumboreal species (Nimis 1993), which is<br />

widely distributed on calcareous <strong>rocks</strong> <strong>of</strong> Sweden<br />

<strong>and</strong> occurs in all biogeographical provinces<br />

(Santesson et al. 2004).<br />

Specimen examined: Ojamo, Kalkkisaari, shore<br />

<strong>of</strong> lake Lohjanjärvi, near <strong>the</strong> <strong>to</strong>p <strong>of</strong> a SW-facing<br />

calcareous rock in a ra<strong>the</strong>r sun-exposed<br />

microhabitat, 60°14'N, 24°01'E, 31.<strong>II</strong>I.2005,<br />

26415.<br />

Thelidium zwackhii<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. T. zwackhii is a pioneer species<br />

<strong>of</strong> calcareous soils <strong>and</strong> <strong>rocks</strong>. In Tytyri it grew on<br />

quarry waste soil shaded by young deciduous<br />

trees <strong>and</strong> in an open area dumped with soil c. 10<br />

years ago.<br />

Specimens examined: Isoteutari, Pyttberget,<br />

dump, on calcareous soil, 60°09'N, 23°59'E,<br />

17.V<strong>II</strong>I.2003, 23387, 23388, this locality was<br />

destroyed in 2004; Lohja-Pappila, Tytyri lime<br />

quarry, on quarry waste soil, 60°16'N,<br />

24°04'E,15.V.2004, 24665, 20.IV.2005, 26621,<br />

26775; Kirkonkylä, N <strong>of</strong> Virkkala church, in<br />

gravel pit enriched by calciferous dust, 60°11'N,<br />

24°00'E, 20.V<strong>II</strong>.2004, 25167; Paloniemi,<br />

Luhtalahti, on road bank by calcareous rock,<br />

60°16'N, 24°01'E, 28.IV.2005, 26704.<br />

Verrucaria caerulea<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. V. caerulea is a widely<br />

distributed species <strong>of</strong> calcareous <strong>rocks</strong>, which<br />

was found on sun-exposed <strong>to</strong> half-shady dry<br />

calcareous <strong>rocks</strong> <strong>and</strong> lime quarries. It was also<br />

collected from a mortar wall <strong>and</strong> from cement.<br />

All populations were small. In Öl<strong>and</strong> <strong>the</strong> species<br />

also occurs in shaded <strong>and</strong> moist habitats (Fröberg<br />

1989).


GRAPHIS SCRIPTA 19 (2007) <strong>Additions</strong> <strong>the</strong> <strong>the</strong> <strong>lichen</strong> <strong>flora</strong> <strong>of</strong> <strong>Finl<strong>and</strong></strong> 25<br />

Specimens examined: Ten localities, first find:<br />

Hermala, Kalkkimäki, 60°13'N, 23°51'E,<br />

29.V<strong>II</strong>I.2003, 23471.<br />

Verrucaria cinereoatrata<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. V. cinereoatrata occurs on<br />

siliceous <strong>rocks</strong> on lake shores. It is known from<br />

Sweden <strong>and</strong> Norway (Santesson et al. 2004) <strong>and</strong><br />

Austria (Poelt 1961). All three populations found<br />

in this work occurred in <strong>the</strong> geolit<strong>to</strong>ral zone on<br />

<strong>the</strong> shore <strong>of</strong> lake Lohjanjärvi.<br />

Specimens examined: Paloniemi, small isl<strong>and</strong> E<br />

<strong>of</strong> Mustasaari, on iron-rich gneissic rock,<br />

60°15'N, 24°00'E, 15.IV.2003, 22438, Skraatila,<br />

Selkäsaaret, on calciferous gneissic rock,<br />

60°15'N, 23°53'E, 16.V<strong>II</strong>.2003, 23252 & R.<br />

Mur<strong>to</strong>; Ojamo, Lahokallio, on slightly limeinfluenced<br />

gneissic rock, 60°14'N, 24°00'E,<br />

7.IV.2004, 24380.<br />

Verrucaria devergens<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. V. devergens is a nor<strong>the</strong>rn<br />

species. It was first found in Russian Karelia<br />

(Vainio 1921). Later, it has been reported from<br />

nor<strong>the</strong>rn Sweden (Magnusson 1952), nor<strong>the</strong>rn<br />

Norway (Degelius 1956, 1982), Canada<br />

(Thomson et al. 1969) <strong>and</strong> Alaska (Thomson &<br />

Ahti 1994). V. devergens may have been<br />

overlooked, but it is also possible that <strong>the</strong><br />

localities in <strong>the</strong> Lohja district are isolated<br />

sou<strong>the</strong>rn outposts <strong>of</strong> <strong>the</strong> species. Some vascular<br />

plant <strong>and</strong> bryophyte species in <strong>Finl<strong>and</strong></strong> also have<br />

sou<strong>the</strong>rn, isolated populations on rocky outcrops<br />

on <strong>and</strong> by <strong>the</strong> shores <strong>of</strong> lake Lohjanjärvi (Pykälä<br />

1992).<br />

Specimens examined: Torhola, E <strong>of</strong> Torhola<br />

cave, on SW-facing calcareous rock on <strong>the</strong> shore<br />

<strong>of</strong> lake Lohjanjärvi, 60°15'N, 23°51'E,<br />

20.IX.2004, 25688. Varsinais-Suomi: Karjalohja,<br />

Karkali, E <strong>of</strong> Karkali nature reserve, SW-facing<br />

calcareous rock on <strong>the</strong> shore <strong>of</strong> lake Lohjanjärvi,<br />

on a calcareous boulder, 60°14'N, 22°50'E,<br />

19.X.2004, 26096.<br />

Verrucaria dolosa<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. V. dolosa is apparently<br />

frequently overlooked in Fennosc<strong>and</strong>ia. It occurs<br />

on shadier <strong>and</strong> moister microhabitats than most<br />

o<strong>the</strong>r Verrucaria species <strong>of</strong> calcareous <strong>rocks</strong>. In<br />

Lohja it grew on <strong>the</strong> bases <strong>of</strong> vertical rock<br />

surfaces, <strong>and</strong> on calcareous s<strong>to</strong>nes <strong>and</strong> pebbles,<br />

preferably shaded by deciduous trees.<br />

Fur<strong>the</strong>rmore, in Lohja V. dolosa appears <strong>to</strong> be<br />

among <strong>the</strong> most common pyrenocarpous species<br />

on concrete <strong>and</strong> bricks in shady habitats. V.<br />

dolosa is usually a characteristic species having<br />

small, almost superficial peri<strong>the</strong>cia, pale exciple,<br />

green thallus <strong>and</strong> small spores (11–17 × 5–7 µm)<br />

(McCarthy 1988).<br />

Specimens examined: Al<strong>to</strong>ge<strong>the</strong>r 25 localities,<br />

first collection: Lohja, Tytyri, 60°16'N, 24°04'E,<br />

26.VI.2001, 20620 & K. Syrjänen.<br />

Verrucaria floerkeana<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. V. floerkeana is a taxonomically<br />

somewhat difficult species or species complex<br />

(Foucard 2001). Some authors have reported it<br />

from siliceous <strong>rocks</strong> (Hafellner & Türk 2001,<br />

Santesson et al. 2004) <strong>and</strong> o<strong>the</strong>rs from calcareous<br />

<strong>rocks</strong> (Zschacke 1933, Servit 1950, Magnusson<br />

1952).<br />

Specimens examined: Paloniemi, Kuoppanokka,<br />

by <strong>the</strong> shore <strong>of</strong> lake Lohjanjärvi, quartz-feldspar<br />

gneiss rock, on <strong>the</strong> base <strong>of</strong> SW-facing rock wall,<br />

60°15'N, 24°01'E, 15.IV.2003, 22471; Paloniemi,<br />

Muutettavanniemi, on calciferous gneissic rock<br />

close by <strong>the</strong> shore <strong>of</strong> lake Lohjanjärvi, 60°15'N,<br />

24°01'E, 28.IV.2004, 26686; Torhola, Torhola<br />

cave, on calciferous gneissic rock, 60°15'N,<br />

23°51'E, 16.V<strong>II</strong>.2004, 25054.<br />

Verrucaria foveolata<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. V. foveolata is one <strong>of</strong> <strong>the</strong> most<br />

common Verrucaria species in <strong>the</strong> study sites. It<br />

prefers half-shady calcareous <strong>rocks</strong>, <strong>and</strong> also<br />

occurs in lime quarries. The broad species<br />

concept concerning V. foveolata applied in <strong>the</strong><br />

Nordic literature (Fröberg 1989, Foucard 2001,<br />

Santesson et al. 2004) is for <strong>the</strong> time being


26 Juha Pykälä GRAPHIS SCRIPTA 19 (2007)<br />

followed pending a closer examination <strong>of</strong> <strong>the</strong><br />

variation <strong>of</strong> <strong>the</strong> species (but see Breuss 2002).<br />

Specimens examined: 14 localities, first<br />

collection: Hermala, Kalkkimäki, 60°13'N,<br />

23°51'E, 18.VI.1996, 16818, 16826.<br />

Verrucaria fusconigrescens<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. V. fusconigrescens is <strong>of</strong>ten<br />

reported <strong>to</strong> occur on seashore <strong>rocks</strong>, but most<br />

finds in Sweden are from wet siliceous or slightly<br />

calcareous <strong>rocks</strong> in inl<strong>and</strong> sites (Foucard 2001).<br />

The habitat <strong>of</strong> <strong>the</strong> species in Lohja is not typical.<br />

Specimen examined: Skraatila, Kirkkovuori, SWfacing<br />

sun-exposed calcareous rock, 60°15'N,<br />

23°54'E, 21.V<strong>II</strong>.2004, 25211.<br />

Verrucaria geophila Zahlbr.<br />

New <strong>to</strong> Fennosc<strong>and</strong>ia. V. geophila is a rare<br />

species <strong>of</strong> calcareous soils found in central <strong>and</strong><br />

sou<strong>the</strong>rn Europe. The closest sites <strong>to</strong> <strong>Finl<strong>and</strong></strong> are<br />

in Austria (Hafellner & Türk 2001) <strong>and</strong> Slovakia<br />

(Palice et al. 2006). V. geophila is ra<strong>the</strong>r similar<br />

<strong>to</strong> V. foveolata (Zschacke 1933), but <strong>the</strong> latter<br />

species grows on calcareous <strong>rocks</strong> ra<strong>the</strong>r than on<br />

soil.<br />

Specimen examined: Hermala, Kalkkimäki, ra<strong>the</strong>r<br />

sun-exposed small calcareous rock, on thin soil,<br />

scarce, 60°13'N, 23°52'E, 18.VI.2003, 23019.<br />

Verrucaria glauconephela<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. V. glauconephela is one <strong>of</strong> <strong>the</strong><br />

many poorly known Verrucaria species. It has<br />

been reported from Hungary (Zschacke 1933),<br />

Sweden (Magnusson 1946), Czech (Vezda &<br />

Liskǎ 1999) <strong>and</strong> Austria (Das L<strong>and</strong><br />

Niederösterreich 2006). Collections from two<br />

sites in Lohja are tentatively placed under V.<br />

glauconephela. They resemble V. muralis, but<br />

<strong>the</strong> spores (<strong>and</strong> asci) are smaller. The Lohja<br />

material fits with <strong>the</strong> description <strong>of</strong> V.<br />

glauconephela presented by Foucard (2001), but<br />

spores were slightly broader: 11–16 × 7–9 µm.<br />

However, Servit (1950) reported a spore size <strong>of</strong><br />

15–18 × 6–9 µm for <strong>the</strong> species.<br />

Specimens examined: Ojamo, Liessaari, on NWfacing<br />

wall <strong>of</strong> calcareous rock on <strong>the</strong> shore <strong>of</strong><br />

lake Lohjanjärvi, 60°14'N, 24°01'E, 22.IV.2003,<br />

22625, 15.IV.2005, 26526, 26533; Paloniemi,<br />

Luhtalahti, road cutting <strong>of</strong> a calciferous quartzfeldspar<br />

gneissic rock, on a pebble, 60°16'N,<br />

24°01'E, 28.IV.2005, 26707.<br />

Verrucaria hochstetteri<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. V. hochstetteri is probably a rare<br />

species, but it may occur throughout Fennosc<strong>and</strong>ia.<br />

All populations were small <strong>and</strong> appeared<br />

on ra<strong>the</strong>r sun-exposed microhabitats. V. hochstetteri<br />

may be a species occurring only on<br />

species-rich calcareous <strong>rocks</strong>. In all localities it<br />

was accompanied by o<strong>the</strong>r rare calcicolous<br />

species.<br />

Specimens examined: Hermala, Kalkkimäki, on<br />

open calcareous rock, 60°13'N, 23°51'E,<br />

29.V<strong>II</strong>I.2003, 23446; Lohja, Tytyri, on a small<br />

rock wall on <strong>the</strong> edge <strong>of</strong> a lime quarry, 60°16'N,<br />

24°04'E, 8.XI.2003, 24026. Varsinais-Suomi:<br />

Karjalohja, Pyöli, Niku, on an open ra<strong>the</strong>r flat<br />

SW-facing calcareous rock, 60°12'N, 23°48'E,<br />

6.V<strong>II</strong>.2004, 24975; Karjalohja, Karkali, Karkali<br />

nature reserve, on a small SW-facing calcareous<br />

rock wall, 60°14'N, 23°47'E, 19.X.2004, 26136.<br />

Verrucaria hydrela<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. V. hydrela was found in ra<strong>the</strong>r<br />

shady, mesic or moist microhabitats with a<br />

mixture <strong>of</strong> calcareous <strong>and</strong> siliceous rock. They<br />

were mainly lime-influenced gneissic <strong>rocks</strong> <strong>and</strong><br />

s<strong>to</strong>nes, close <strong>to</strong> calcareous <strong>rocks</strong>. V. hydrela<br />

usually occurs on siliceous <strong>rocks</strong> on lake <strong>and</strong><br />

river shores (Foucard 2001), <strong>and</strong> <strong>the</strong> habitats in<br />

this study are thus abnormal.<br />

Specimens examined: Torhola, Torhola cave, SW<br />

slope <strong>of</strong> calciferous gneissic rock, shaded by a<br />

st<strong>and</strong> <strong>of</strong> Ulmus laevis, 60°15'N, 23°51'E,<br />

16.V<strong>II</strong>.2004, 25052, conf. O. Breuss 2005;<br />

Paloniemi, Muutettavanniemi, on NW-facing<br />

calciferous gneiss rock, 60°15'N, 24°01'E,<br />

28.IV.2005, 26659, 26689; Kunnarla, on a small


GRAPHIS SCRIPTA 19 (2007) <strong>Additions</strong> <strong>the</strong> <strong>the</strong> <strong>lichen</strong> <strong>flora</strong> <strong>of</strong> <strong>Finl<strong>and</strong></strong> 27<br />

S-facing calcareous rock wall in herb-rich forest,<br />

60°13'N, 24°04'E, 5.V.2005, 26742; Pappila,<br />

Tytyri, by <strong>the</strong> lime quarry, herb-rich forest on <strong>the</strong><br />

shore <strong>of</strong> lake Lohjanjärvi, on s<strong>to</strong>nes, 60°16'N,<br />

24°04'E, 7.V.2005, 26785; Marttila,<br />

Savilahdensalmi, herb-rich forest, on a probably<br />

lime-influenced siliceous s<strong>to</strong>ne, 60°14'N,<br />

23°51'E, 21.VI.2005, 27094.<br />

Verrucaria macros<strong>to</strong>ma<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. V. macros<strong>to</strong>ma occurs on<br />

calcareous <strong>rocks</strong> <strong>and</strong> artificial calcareous habitats<br />

(Hawskworth et al. 1992, Foucard 2001). It is not<br />

rare in sou<strong>the</strong>rn Sweden (Foucard 2001).<br />

Specimens examined: Lohja, Tytyri, on edge <strong>of</strong> a<br />

lime quarry, 60°16'N, 24°04'E, 24.V.2003,<br />

22861c, 8.XI.2003, 24030.<br />

Verrucaria maculiformis<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. V. maculiformis occurred on<br />

various kinds <strong>of</strong> calcareous <strong>rocks</strong> both in ra<strong>the</strong>r<br />

shady <strong>and</strong> sun-exposed microhabitats, perhaps<br />

preferring half-shade. It also grew on concrete<br />

<strong>and</strong> cement. The species was found both on<br />

vertical <strong>and</strong> flat rock surfaces, <strong>and</strong> also in lime<br />

quarries. It may prefer pebbles on quarry waste<br />

l<strong>and</strong>. Despite <strong>the</strong> wide variation in its habitats,<br />

<strong>the</strong> species appears <strong>to</strong> be rare in Lohja. In<br />

Fennosc<strong>and</strong>ia V. maculiformis has previously<br />

been found on bricks (Santesson et al. 2004).<br />

Specimens examined: Al<strong>to</strong>ge<strong>the</strong>r 10 localities,<br />

first collection 1996: Hermala, Kalkkimäki,<br />

60°13'N, 23°51'E, 18.VI.1996, 16821.<br />

Verrucaria murina<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. V. murina has an almost<br />

immersed grey-green-brown thallus (in <strong>the</strong> Lohja<br />

collections clearly epilithic, but very small <strong>and</strong><br />

thin brown thallus), entire involucrellum, small<br />

1/3 <strong>to</strong> almost immersed peri<strong>the</strong>cia <strong>and</strong> relatively<br />

small (14–20(–25) × 6–9(–10) µm) spores<br />

(Hawskworth et al. 1992). The species has<br />

previously been recorded in Fennosc<strong>and</strong>ia from<br />

Gotl<strong>and</strong> (Santesson et al. 2004). Santesson et al.<br />

(2004) suggested that V. murina might be<br />

conspecific with V. deversa. However, V.<br />

deversa has an inconspicuous thallus, spore<br />

length usually exceeds 20 µm <strong>and</strong> <strong>the</strong> peri<strong>the</strong>cia<br />

tend <strong>to</strong> be larger than in V. murina.<br />

Specimens examined: Hermala, Tolpoonkallio,<br />

flat calcareous rock, on s<strong>to</strong>nes, 60°13'N, 23°51'E,<br />

29.V.2004, 24808; Hermala, Kalkkimäki, in a<br />

small lime quarry, 60°13'N, 23°52'E,<br />

19.V<strong>II</strong>.2004, 25138; Pietilä, Pietilänlahti, on a Nfacing<br />

wall <strong>of</strong> calcareous rock, 60°14'N, 23°54'E,<br />

22.IX.2004, 25741.<br />

Verrucaria ochros<strong>to</strong>ma (Borrer ex Leigh<strong>to</strong>n)<br />

Trevisan<br />

New <strong>to</strong> Fennosc<strong>and</strong>ia. V. ochros<strong>to</strong>ma has been<br />

found in central Europe (Wirth 1995, Bayerova<br />

et al. 2004), Engl<strong>and</strong> (Hawksworth et al. 1992)<br />

<strong>and</strong> Asia (e.g. Aptroot & Seaward 1999). The<br />

species has a pale, areolate thallus in which<br />

peri<strong>the</strong>cia are immersed (Hawksworth et al.<br />

1992). The exciple is dark, <strong>and</strong> <strong>the</strong> involucrellum<br />

is lacking. The spore size is 18–23 × 8–12 µm.<br />

Specimens examined: Paloniemi, Ollisaari, on<br />

small flat calcareous rock on <strong>the</strong> shore <strong>of</strong> lake<br />

Lohjanjärvi, 60°15'N, 24°01'E, 17.V<strong>II</strong>I.2004,<br />

25529 & R. Mur<strong>to</strong>, V. cf. ochros<strong>to</strong>ma, det. O.<br />

Breuss 2005 (very scarce material); Hermala,<br />

Pietilä, on a road cutting with calcareous rock<br />

<strong>and</strong> on pebbles, 60°13'N, 23°51'E, 30.IX.2004,<br />

25913; 25916.<br />

Verrucaria rejecta<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. V. rejecta has small peri<strong>the</strong>cia<br />

(0.15–0.3 mm), that are half- <strong>to</strong> 3/4-immersed.<br />

The involucrellum covers <strong>the</strong> exciple <strong>to</strong> <strong>the</strong> base,<br />

<strong>the</strong> exciple is pale <strong>and</strong> <strong>the</strong> spores are 12–19 × (5–<br />

)6–9 µm. The thallus is granular <strong>to</strong> small<br />

areolate, <strong>and</strong> dark brown <strong>to</strong> black. In <strong>the</strong> lime<br />

quarry collection, <strong>the</strong> thallus was paler brown<br />

(medium brown) <strong>and</strong> slightly larger than in o<strong>the</strong>r<br />

collections. V. rejecta is an arctic species<br />

previously reported from Fennosc<strong>and</strong>ia in<br />

nor<strong>the</strong>rn Sweden (Magnusson 1952) <strong>and</strong> nor<strong>the</strong>rn<br />

Norway (Degelius 1956). However, <strong>the</strong> present


28 Juha Pykälä GRAPHIS SCRIPTA 19 (2007)<br />

finds suggest that V. rejecta may be more widely<br />

distributed, also occurring on artificial calcareous<br />

habitats.<br />

Specimens examined: Paavola, Hausnummi, on<br />

small flat calcareous rock, 60°13'N, 23°52'E,<br />

6.VI.2005, 26958; Kirkonkylä, former Virkkala<br />

cement fac<strong>to</strong>ry, on cement, 60°11'N, 23°59'E,<br />

15.V<strong>II</strong>.2005, 27324; Lohja, Pitkäniemi, shore <strong>of</strong><br />

lake Lohjanjärvi, on flat calcareous rock,<br />

60°15'N, 24°02'E, 19.V<strong>II</strong>I.2005, 27550; Lohja,<br />

Pitkäniemi, on lime quarry, 60°15'N, 24°03'E,<br />

23.V<strong>II</strong>I.2005, 27665.<br />

Verrucaria ruderum<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. V. ruderum has a thin white<br />

thallus, small (0.2 mm large) immersed<br />

peri<strong>the</strong>cia, a thick apical involucrellum, a pale<br />

exciple <strong>and</strong> large spores (23–30 × 13–18 µm;<br />

Zschacke 1933). The species has previously been<br />

found once in Fennosc<strong>and</strong>ia, in Sweden<br />

(Santesson et al. 2004). V. ruderum is clearly<br />

different from any o<strong>the</strong>r Fennosc<strong>and</strong>ian<br />

Verrucaria species, <strong>and</strong> <strong>the</strong> few finds <strong>the</strong>refore<br />

suggest that it is truly rare.<br />

Specimens examined: Ojamo, Liessaari, on shore<br />

<strong>of</strong> lake Lohjanjärvi, on a NW-facing calcareous<br />

rock wall, scarce, 60°14'N, 24°01'E, 15.IV.2005,<br />

26520; Moisio, Lohjanharju esker, pine forest, on<br />

<strong>to</strong>p <strong>of</strong> a calcareous s<strong>to</strong>ne, scarce, 60°15'N,<br />

24°06'E, 30.X.2005, 28195.<br />

Verrucaria schindleri<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. V. schindleri is similar <strong>to</strong> V.<br />

muralis, but has a brown exciple (Breuss 2002).<br />

The exciple <strong>of</strong> V. muralis <strong>of</strong>ten turns brown in<br />

overmature peri<strong>the</strong>cia (Breuss 2002). Thus, <strong>the</strong>se<br />

two species are difficult <strong>to</strong> separate from each<br />

o<strong>the</strong>r. V. schindleri may be conspecific with V.<br />

epili<strong>the</strong>a sensu Vainio (1921).<br />

Specimens examined: C. 20 localities, on<br />

calcareous <strong>rocks</strong>, lime quarries, concrete <strong>and</strong><br />

cement. Hermala, Kyttälä, on flat calcareous<br />

rock, 60°13'N, 23°51'E, 6.V<strong>II</strong>.2004, 24987, det.<br />

O. Breuss 2005.<br />

Verrucaria transiliens (Arnold) Lettau<br />

New <strong>to</strong> Fennosc<strong>and</strong>ia. In V. transiliens, <strong>the</strong><br />

involucrellum surrounds <strong>the</strong> peri<strong>the</strong>cium <strong>and</strong> <strong>the</strong><br />

epilithic thallus is brown (Breuss 2004). In <strong>the</strong><br />

Lohja collection spores (22–28 × 11–13 µm) are<br />

narrower than those reported in Zschacke (1933)<br />

<strong>and</strong> Breuss (2004), but close <strong>to</strong> <strong>the</strong> size given by<br />

Servit (1950): 22–26 × 12–15 µm.<br />

Specimens examined: Skraatila, Päivärinta SW,<br />

by <strong>the</strong> shore <strong>of</strong> lake Lohjanjärvi, on a small<br />

ra<strong>the</strong>r flat calcareous rock surrounded by gneissic<br />

<strong>rocks</strong>, 60°15'N, 23°53'E, 24.V<strong>II</strong>I.2005, 27777,<br />

27779.<br />

Verrucaria viridula<br />

V. viridula grew on south-facing calcareous <strong>rocks</strong><br />

<strong>and</strong> on south- <strong>and</strong> west-facing surfaces <strong>of</strong> lime<br />

quarries close <strong>to</strong> unmined <strong>rocks</strong>. All populations<br />

were small.<br />

Specimens examined: Lohja, Kiviniemi, on a Wfacing<br />

wall <strong>of</strong> a lime quarry, 60°15'N, 24°03'E,<br />

11.V<strong>II</strong>.2003, 23162, <strong>the</strong> locality was destroyed in<br />

2004 due <strong>to</strong> building; Torhola, E <strong>of</strong> Torhola<br />

cave, on a SW-facing calcareous rock, 60°15'N,<br />

23°52'E, 30.V<strong>II</strong>.2003, 23338; Hermala,<br />

Kalkkimäki, in a lime quarry, 60°13'N, 23°51'E,<br />

29.V<strong>II</strong>I.2003, 23495, 19.V<strong>II</strong>.2004, 25115;<br />

Hermala, Pietilä, in a lime quarry, 60°13'N,<br />

23°51'E, 30.IX.2004, 25879; Seppälä, Mustasaari,<br />

on calcareous rock, 60°14'N, 23°51'E,<br />

10.V<strong>II</strong>I.2004, 25394 & R. Mur<strong>to</strong>; Lohja, Lindkullanmäki,<br />

on calcareous rock, 60°15'N,<br />

24°04'E, 18.IV.2004, 24446b.<br />

Vezdaea retigera<br />

New <strong>to</strong> <strong>Finl<strong>and</strong></strong>. V. retigera has previously been<br />

reported only once in Fennosc<strong>and</strong>ia, on a mortar<br />

wall in Norway (Tønsberg 1990). The finds in<br />

Lohja were on calcareous soil. In <strong>the</strong> British<br />

Isles, V. retigera is usually found on lead-rich<br />

soil (Coppins 1987, Purvis 1992b), <strong>and</strong> a Danish<br />

find was made on Peltigera rufescens on a s<strong>to</strong>ne<br />

fence (Alstrup et al. 2004).


GRAPHIS SCRIPTA 19 (2007) <strong>Additions</strong> <strong>the</strong> <strong>the</strong> <strong>lichen</strong> <strong>flora</strong> <strong>of</strong> <strong>Finl<strong>and</strong></strong> 29<br />

Specimens examined: Ojamo, Ojamo lime quarry,<br />

60°14'N, 24°02'E, NW-facing slope on quarry<br />

waste soil with young deciduous trees,<br />

15.IV.2005, 26549, <strong>and</strong> <strong>the</strong> <strong>to</strong>p <strong>of</strong> a moderately<br />

shaded SW-facing rock wall, on soil, 18.IV.2005,<br />

26561; Pappila, Tytyri, by <strong>the</strong> lime quarry,<br />

deciduous forest, on a boulder, on <strong>the</strong> dead<br />

thallus <strong>of</strong> Peltigera praetextata, 60°16'N,<br />

24°04'E, 7.V.2005, 26791; Kukkumäki, on <strong>the</strong> N<br />

slope <strong>of</strong> an ab<strong>and</strong>oned back yard by <strong>the</strong> shore <strong>of</strong><br />

lake Lohjanjärvi, on ra<strong>the</strong>r thin secondary<br />

calcareous soil, 60°11'N, 23°58'E, 14.V.2005,<br />

26830.<br />

Acknowledgements<br />

Othmar Breuss, Brian J. Coppins, Lars Fröberg,<br />

Per M. Jørgensen <strong>and</strong> Anders Nordin are thanked<br />

for determining or confirming several difficult<br />

specimens. Ris<strong>to</strong> Mur<strong>to</strong> arranged boat transport<br />

<strong>to</strong> small isl<strong>and</strong>s with calcareous rock. Lars<br />

Fröberg <strong>and</strong> Orvo Vitikainen provided useful<br />

comments on <strong>the</strong> manuscript.<br />

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Rabenhorst's Kryp<strong>to</strong>gamen-Flora von<br />

Deutschl<strong>and</strong>, Österreich und der Schweiz 9,<br />

1(1): 44–695.

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