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Molecular data show that Bryoria fremontii and B. tortuosa (Parmeliaceae) are conspecific

Published online by Cambridge University Press:  26 May 2009

Saara VELMALA
Affiliation:
Botanical Museum, Finnish Museum of Natural History, P.O. Box 7, FI-00014 University of Helsinki, Finland. Email: saara.velmala@helsinki.fi
Leena MYLLYS
Affiliation:
Botanical Museum, Finnish Museum of Natural History, P.O. Box 7, FI-00014 University of Helsinki, Finland. Email: saara.velmala@helsinki.fi
Pekka HALONEN
Affiliation:
Botanical Museum, Department of Biology, P.O. Box 3000, FI-90014 University of Oulu, Finland.
Trevor GOWARD
Affiliation:
Herbarium, Department of Botany, University of British Columbia, Vancouver, BC V6G 2B1, Canada.
Teuvo AHTI
Affiliation:
Botanical Museum, Finnish Museum of Natural History, P.O. Box 7, FI-00014 University of Helsinki, Finland. Email: saara.velmala@helsinki.fi
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Abstract

Bryoria fremontii and B. tortuosa are the only species in the lichenized ascomycete genus Bryoria known to contain the pulvinic acid derivative vulpinic acid. In B. fremontii this yellow pigment is restricted to the soralia and apothecia, while in B. tortuosa it can occur throughout the thallus. The actual amount of vulpinic acid produced by B. tortuosa is rather variable, however, with intermediate specimens bearing both white and yellow pseudocyphellae. We studied the relationship between the two species with parsimony analysis using four DNA regions: 1) the internal transcribed spacers of the nuclear rDNA including the 5.8S region (ITS), 2) partial sequences from the intergenic spacer of the nuclear rDNA (IGS), 3) partial sequences from the small subunit of the mitochondrial rDNA (mtSSU), and 4) partial sequences from the protein-coding glyceraldehyde-3-phosphate dehydrogenase gene (GAPDH). Our phylogenetic analysis revealed that B. fremontii and B. tortuosa must be regarded as conspecific, but allowing for some genetic differentiation between European and North American populations. Bryoria tortuosa is therefore synonymized with B. fremontii.

Information

Type
Research Article
Copyright
Copyright © British Lichen Society 2009
Figure 0

Table 1. Specimens used in the phylogenetic analyses with collection data and GenBank accession numbers. Bryoria tortuosa specimens were submitted to GenBank as B. fremontii (see discussion).

Figure 1

Fig. 1. Molecular phylogeny of Bryoria fremontii and B. tortuosa. A strict consensus tree of two trees based on ITS and IGS data. Bootstrap support values are shown above the nodes.

Figure 2

Fig. 2. Molecular phylogeny of Bryoria fremontii and B. tortuosa. A strict consensus tree of 468 trees based on ITS, IGS, mtSSU and GAPDH data. Bootstrap support values are shown above the nodes.

Figure 3

Fig. 3. Bryoria fremontii. A, typical vulpinic acid-deficient chemotype showing reddish brown hue and foveolate branches (Velmala 13b et al.); B, typical vulpinic acid-containing chemotype showing yellow-brown hue and yellow pseudocyphellae (Goward 07020025); C, thallus with yellow soralia and pseudocyphellae (Crawford 52); D, thallus with yellow apothecia and pseudocyphellae (Crawford 32); E, branch with both yellow (yellow arrow) and white (white arrow) pseudocyphellae as seen in fresh material (Crawford 52). Scales: A – C = 2 mm; D = 1 mm; E = 0·5 mm.

Figure 4

Fig. 4. The global distribution of Bryoria fremontii based on Ahlner (1948) and Brodo & Hawksworth (1977), with later additions from the literature as well as herbarium material. The record from the Canary Islands is by Hawksworth (1982). The records accepted from Russia include those in the following papers: Hermansson & Kudryavtseva 1997: 218, Pystina & Hermansson 1998 (map), Petrova 2000 (map), Kravchenko 2003, Urbanavichus & Urbanavichene 2004 (in part), Chkobadze 2004 (map), Kuznetsova et al. 2007, Fadeeva & Kravchenko 2007 (map), Fadeeva et al. 2008 and Urbanavichus et al. 2008. Records from the Altay, Sayan and other mountains in the south of Siberia, Mongolia, the Carpathians, the Caucasus, the Kamchatka Peninsula and Sakhalin (e.g., Sedel'nikova 1985, 1990, 1998; Byazrov et al. 1989; Mikulin 1990; Oxner 1993) could not be confirmed and are mapped as doubtful records (indicated with triangles).