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Research Article
Two novel species of arctic-alpine lichen-forming fungi (Ascomycota, Megasporaceae) from the Deosai Plains, Pakistan
expand article infoMuhammad Usman§, Paul S. Dyer§, Matthias Brock§, Christopher M. Wade§, Abdul Nasir Khalid
‡ University of the Punjab, Lahore, Pakistan
§ University of Nottingham, Nottingham, United Kingdom
Open Access

Abstract

Members of the lichen-forming fungal genus Oxneriaria are known to occur in cold polar and high altitudinal environments. Two new species, Oxneriaria crittendenii and O. deosaiensis, are now described from the high altitude Deosai Plains, Pakistan, based on phenotypic, multigene phylogenetic and chemical evidence. Phenotypically, O. crittendenii is characterised by orbicular light-brown thalli 1.5–5 cm across, spot tests (K, C, KC) negative, apothecia pruinose, hymenium initially blue then dark orange in response to Lugol’s solution. Oxneriaria deosaiensis is characterised by irregular areolate grey thalli 1.5–2 cm across, K test (light brown), KC test (dark brown), apothecia epruinose, hymenium initially blue then dark blue in response to Lugol’s solution. Both species share the same characters of thalli with black margins and polarilocular ascospores. The closest previously reported species, O. pruinosa, differs from O. crittendenii and O. deosaiensis in having non-lobate margins, thin thalline exciple (45–80 μm thick), short asci (55–80 × 25–42 μm) and K positive (yellow) and KC negative tests and divergent DNA sequence in the ITS, LSU and mt SSU regions. The newly-described Oxneriaria species add to growing evidence of the Deosai Plains as a region of important arctic-alpine biodiversity.

Key words

Aspicilia, Gilgit-Baltistan, Himalaya, Karakorum, Maximum Likelihood, Pertusariales, Skardu

Introduction

The Deosai Plains are located between the Himalaya and Karakorum, two of the world’s most famous mountain ranges, with an average elevation of over 4,000 m (Woods et al. 1997). They represent one of the most important high altitude alpine grasslands and summer pastures of the trans-Himalayan range in Pakistan. Three important river systems originate from the Deosai Plains, namely the Shatung, Bara Pani and Kala Pani, which combine to form the Shigar River, an important tributary of the Indus River (Hussain 2014). The Deosai Plains are characterised by an undulating topography with a range of edaphic conditions and ecological niches present that are subject to extreme cold conditions for long periods of the year. A diverse range of flora and fauna have been recorded, which are considered to be adapted for survival under such conditions (Woods et al. 1997; Usman et al. 2021). The highland arctic-alpine ecosystem includes herbaceous perennial grasses and sedges which dominate the vegetation of the plateau, forming dense moist grasslands in the valley plains, whilst dwarfed and stunted vegetation, flower fields, rocky outcrops and soil crusts are also present (Stewart 1961; Hussain et al. 2015).

Members of the lichen-forming genus Oxneriaria S.Y. Kondr. & Lőkös are distributed in cold polar and high-altitude localities of Eurasia and the Northern Hemisphere (Nordin et al. 2011; Haji-Moniri et al. 2017; Chesnokov et al. 2018; Halıcı et al. 2018). They are characterised by the presence of a radiating lichen thallus with a wrinkled or lobate peripheral zone, relatively small ascospores, production of substictic acid and positioning as a distinct branch on phylogenetic trees in the Megasporaceae. They grow on rocks and have been observed growing side by side with other taxa of the same and other genera (Haji-Moniri et al. 2017). The genus was first named by Haji-Moniri et al. (2017) who transferred over nine species that were previously included in the genus Aspicilia. A total of fourteen species have, so far, been described for the genus Oxneriaria (Haji-Moniri et al. 2017; Asghar et al. 2023; Iqbal et al. 2023; Zulfiqar et al. 2023).

Four species of the genus Oxneriaria have, so far, been described from Pakistan with a distance of 300 to 650 km from Deosai Plains, namely O. iqbalii R. Zulfiqar, H. S. Asghar, K. Habib & Khalid from Kohistan (350 km) and Swat (500 km), O. kohistaniensis R. Zulfiqar, K. Habib & Khalid from Kohistan (350 km), O. pakistanica M. S. Iqbal, Usman, K. Habib & Khalid from Darel (300 km) and O. pruinosa H. S. Asghar., Usman, K. Habib & Khalid from Chitral (650 km). These were all found at relatively high altitudes up to ca. 2,500 m (Asghar et al. 2023; Iqbal et al. 2023; Zulfiqar et al. 2023). During the period 2019 to 2020, several collections of lichens were made from the Deosai Plains and adjacent localities at altitudes above 4,000 m. From this collection, four samples were attributed to the genus Oxneriaria, which comprised two new species as will be described in this study.

Materials and methods

Sample collection

More than half of the Deosai Plains are situated between an elevation (elev.) of 4,000 and 4,500 m with an average daily temperature ranging from -20 °C (January-February) to 12 °C (July-August). Annual precipitation varies from 350 to 550 mm, mostly received during winter as snow (WAPDA 2012; Usman et al. 2021). Lichen collections were made from both rock and soil crusts during the period May 2019 to Sept 2020 from various locations in the Deosai Plains National Park, Gilgit Baltistan, Pakistan (see later for precise collection site details for particular specimens) at altitudes between 4,177 and 4,689 m. Samples were air dried before storage and examination.

Morpho-anatomical and chemical studies

Methods for the examination of external morphology, macroscopic and microscopic characters and their measurements were followed and recorded according to the terminology of Ryan et al. (2002). All the measurements of anatomical structures were noted in water with an average of 25 ascospores per collection and 5 - 6 sections were prepared for the thallus, apothecia and pycnidia. The algal partner was identified by following Friedl and Büdel (2008). For thallus chemical reactions, standard K (5% potassium hydroxide aqueous solution), C (commercial bleach), KC (commercial bleach after 5% potassium hydroxide aqueous solution) and ultra-violet (UV) tests were done. Solvents A (toluene/dioxane/ acetic acid as 180:45:5) and G (toluene/ ethyl acetate/ formic acid as 139:83:8) were used for the detection of secondary metabolites through thin layer chromatography (TLC) as described by Orange et al. (2010).

Molecular and phylogenetic analyses

Nuclear DNA was extracted from apothecia present on thalli using a GF1 Plant DNA extraction kit according to the manufacturer’s instruction (Vivantis, Selangor Darul Ehsan, Malaysia). Primers used for amplifications were ITS1F 5'-CCT GGT CAT TTA GAG GAA GT A A-3 ' and ITS4 5'-TCC TCC GCT CTA TTG ATA TGC-3' for the internal transcribed spacer (ITS1-5.8S-ITS2) region, while LROR 5'-ACC CGC TGA ACT TAA GC-3' and LR5 5'-TCC TGA GGG AAA CTT CG-3' were used for the nuclear large subunit (LSU) ribosomal RNA region (White et al. 1990; Gardes and Bruns 1993). For the mitochondrial (mt) small subunit (SSU) ribosomal RNA region, SSU1 5'-AGC AGT GAG GAA TAT TGG TC-3' and SSU3R 5'-ATG TGG CAC GTC TAT AGC CC-3' were used (Zoller et al. 1999). Polymerase chain reaction (PCR) conditions adapted from those of Gardes and Bruns (1993) were followed according to Zoller et al. (1999) and Usman and Khalid (2020). The PCR amplicons were purified using a QIAquick PCR Purification Kit (Qiagen, Valencia, CA, USA) and then sent for sequencing to TsingKe, China.

Forward and reverse sequences of the ITS, LSU and mt SSU regions were obtained in FASTA format and sequences were assembled using BIOEDIT v. 7.2.5 (Hall 1999). These were compared with related DNA sequences available online through BLAST at NCBI (https://www.ncbi.nlm.nih.gov/guide). The sequences used in the ITS, LSU and mt SSU dataset were retrieved from the NCBI database, based on similarity of 93% identity or greater, plus all published sequences from the genus Oxneriaria (Nordin et al. 2007; Nordin et al. 2011; Asghar et al. 2023; Iqbal et al. 2023; Zulfiqar et al. 2023). Sequences of Megaspora cretacea Gasparyan, Zakeri & Aptroot were used as an outgroup in the ITS phylogenetic tree, while Megaspora verrucosa (Ach.) Arcadia & A. Nordin was used as outgroup in the LSU and mt SSU phylogenetic trees (Nordin et al. 2010; Sohrabi et al. 2013; Zakeri et al. 2016). Sequences used for the phylogenetic analyses are presented in Table 1 together with GenBank accession numbers, voucher numbers and country distribution. The final alignments of sequences were made in SEAVIEW software version 5.0.5 using the CLUSTAL W method (Gouy et al. 2010). Maximum Likelihood phylogenetic trees were inferred in RAxML-HPC2 using XSEDE (8.2.10) using the GTR+GAMMMA nucleotide substitution model and with 1000 bootstrap replicates. Phylogenetic analyses were undertaken using the CIPRES online portal (https://www.phylo.org/), with substitution model verified using jModelTest 2.1.6 and the Akaike Information Criterion (Akaike 1974; Darriba et al. 2012) to determine the best nucleotide substitution model. Phylogenetic trees were visualised using FigTree v. 1.4.2 (Rambaut 2012). Newly-generated sequences were deposited in GenBank (accession numbers OR037219OR037226, OR037259OR037262, Table 1). These were investigated further by DNA-based phylogenetic analyses and detailed morpho-anatomical and chemical studies as follows.

Table 1.

Sequences used in the phylogenetic analyses. Novel sequences generated during this study are shown in bold. Note that sequences were not available for all regions for certain taxa.

Taxon name Voucher number GenBank accession Country
ITS LSU mt SSU
Oxneriaria crittendenii LAH37193 OR037223 OR037219 OR037259 Pakistan
Oxneriaria crittendenii LAH37194 OR037224 OR037220 OR037260 Pakistan
Oxneriaria dendroplaca UPS:Nordin 5952 HQ259259 HM060744 HM060706 Sweden
Oxneriaria dendroplaca UPS:Nordin 6366 HQ259260 HM060758 Finland
Oxneriaria deosaiensis LAH37200 OR037225 OR037221 OR037261 Pakistan
Oxneriaria deosaiensis LAH37416 OR037226 OR037222 OR037262 Pakistan
Oxneriaria iqbalii LAH37155 ON392710 Pakistan
Oxneriaria iqbalii LAH37156 ON392709 ON392708 Pakistan
Oxneriaria kohistaniensis LAH37152 ON392707 ON392711 Pakistan
Oxneriaria kohistaniensis LAH37151 ON454505 Pakistan
Oxneriaria mashiginensis Nordin 5790 (UPS) EU057912 HM060732 HM060694 Sweden
Oxneriaria mashiginensis UPS:Tibell 23557 HQ259266 Sweden
Oxneriaria pakistanica LAH37495 OP114649 Pakistan
Oxneriaria pakistanica LAH37501 OP627196 Pakistan
Oxneriaria permutata Nordin 6027 (UPS) EU057918 HM060747 HM060709 Sweden
Oxneriaria permutata Nordin 6029 (UPS) EU057919 Sweden
Oxneriaria permutata Nordin 6039 (UPS) EU057921 Sweden
Oxneriaria permutata Nordin 5980 (UPS) EU057930 Sweden
Oxneriaria permutata Wheeler 4463 MW424810 Alaska, USA
Oxneriaria pruinosa LAH37556 OP352770 Pakistan
Oxneriaria pruinosa LAH37555 OP352771 Pakistan
Oxneriaria rivulicola Nordin 5957 (UPS) EU057922 HM060753 Sweden
Oxneriaria rivulicola Nordin 5960 (UPS) EU057923 Sweden
Oxneriaria sp Nordin 6003 (UPS) EU057931 Sweden
Oxneriaria sp Nordin 6004 (UPS) EU057932 Sweden
Oxneriaria supertegens Owe-Larsson H-168a (UPS) EU057935 Sweden
Oxneriaria supertegens Owe-Larsson 9011 (UPS) EU057937 Norway
Oxneriaria supertegens Nordin 6023 (UPS) EU057938 HM060751 Sweden
Oxneriaria supertegens Owe-Larsson 9002 (UPS) HM060742 HM060704 Norway
Oxneriaria verruculosa Owe-Larsson 9007 (UPS) EU057940 HM060741 HM060703 Norway
Oxneriaria verruculosa Owe-Larsson 9003 (UPS) EU057941 Norway
Oxneriaria verruculosa Nordin 5942 (UPS) EU057942 Sweden
Oxneriaria virginea UPS:Nordin 6017a HQ259270 Sweden
Oxneriaria virginea UPS:Ebbestad SVL1-1 HQ259271 Svalbard
Oxneriaria virginea Wheeler 7153 (hb. Wheeler) MW424818 Montana, USA
Outgroup
Megaspora cretacea B 600200932 KX253974 Armenia
Megaspora cretacea B 600199170 KX253975 Armenia
Megaspora verrucosa St. Clair C54042 (BRY) KC667062 Colorado, USA
Megaspora verrucosa UPS:Nordin 6495 HM060687 Sweden

Results

Out of almost 300 samples collected from the Deosai plains and its adjacent areas during the 2019 and 2020 surveys, four lichen thalli were putatively assigned to the genus Oxneriaria on the basis of gross morphological features (Figs 1, 2).

Figure 1. 

Oxneriaria crittendenii sp. nov. holotype (LAH37193) A thallus B margins C apothecia under stereomicroscope D ascospores in Lugol’s solution E conidia F pycnidium. Photos by Muhammad Usman. Scale bars: 5 cm (A); 1 mm (B, C); 20 μm (D, E); 100 μm (F).

Figure 2. 

Oxneriaria deosaiensis sp. nov. holotype (LAH37200) A thallus B margins C apothecia under stereomicroscope D ascospores in Lugol’s solution E conidia F pycnidium. Photos by Muhammad Usman. Scale bars: 1 cm (A); 1 mm (B, C); 20 μm (D); 30 μm (E); 100 μm (F).

Multigene phylogenetic analyses

DNA was extracted from the four different collections and used successfully in PCR to generate amplicons for the ITS, LSU and mt SSU regions, which ranged in size from 500–800, 900–950 and 900–960 base pairs, respectively. Sequence data of amplicons were aligned and used to construct separate ITS, LSU and mt SSU trees via Maximum Likelihood analyses to examine phylogenetic relationships. Distinct, well-supported clades were recovered from all datasets with minimal conflict, each taxon showing a unique position in all phylogenetic analyses with sequence divergence from other taxa. Clade names were provisionally assigned.

The ITS phylogenetic tree (Fig. 3) consisted of sequences from a total of 34 taxa including the outgroup clade A comprised of two sequences of Megaspora cretacea (KX253975, KX253974) and 32 sequences representing an Oxneriaria ingroup (Clade B), which could be further subdivided into two main clades C and D. Clade D consisted of a total of seven species of Oxneriaria including new, well-supported sequences named here O. crittendenii and O. deosaiensis, each represented by two of the four field collections. Within clade D, Oxneriaria deosaiensis formed a separate branch, sister to a clade which consisted of four species, namely O. crittendenii, O. pakistanica, O. pruinosa and O. rivulicola (H. Magn.) S. Y. Kondr. et L. Lőkös and showed 5%, 7.2%, 5.1% and 5% bp differences with O. deosaiensis in the sequences of ITS region, respectively, whilst O. crittendenii showed 6.1%, 5.3% and 5% bp differences with O. pakistanica, O. pruinosa and O. rivulicola, respectively. The closest species to O. crittendenii and O. deosaiensis was O. pruinosa, forming a separate branch.

Figure 3. 

Phylogenetic tree of the genus Oxneriaria as generated by Maximum Likelihood (ML) analyses, based on ITS sequences. Bootstrap values > 70%, based on 1,000 replicates are shown at the branches. Novel sequences, generated during this study, are shown in bold.

The LSU phylogenetic tree (Fig. 4) similarly revealed that O. crittendenii and O. deosaiensis are positioned on well-supported branches and are monophyletic. The tree consisted of a total 15 available sequences of which 14 sequences represent an Oxneriaria ingroup (Clade B), while Megaspora verrucosa (Ach.) Arcadia & A. Nordin (KC667062) formed an outgroup (Clade A). Clade B could be further subdivided into Clades C and D. Oxneriaria deosaiensis, O. crittendenii, O. dendroplaca (H. Magn.) S. Y. Kondr. et L. Lőkös., O. rivulicola and O. mashiginensis (Zahlbr.) S. Y. Kondr. et L. Lőkös. were all positioned in the same clade (Clade D), where they each formed separate branches. Sequences of O. deosaiensis for the LSU region showed 1.2%, 1.5%, 1.2% and 2%, bp differences to O. crittendenii, O. dendroplaca, O. rivulicola and O. mashiginensis, respectively, whilst Oxneriaria crittendenii showed 1.5%, 1.4%, 1.5 and 2% bp differences with O. rivulicola, O. dendroplaca and O. mashiginensis, respectively.

Figure 4. 

Phylogenetic tree of the genus Oxneriaria as generated by Maximum Likelihood (ML) analyses, based on LSU sequences. Bootstrap values > 70%, based on 1,000 replicates are shown at the branches. Novel sequences, generated during this study, are shown in bold.

The mt SSU phylogenetic tree (Fig. 5) consisted of a total 12 available sequences of which 11 sequences represented an Oxneriaria ingroup (Clade B), while Megaspora verrucosa (HM060087) was used as an outgroup (Clade A). Oxneriaria deosaiensis, O. crittendenii, O. dendroplaca and O. mashiginensis formed a clade (Clade D) distinct from O. verruculosa forming clade C. Sequences of O. deosaiensis from the mt SSU region showed 1%, 2% and 2.5% bp differences with the sequences of closest species O. crittendenii, O. dendroplaca and O. mashiginensis, respectively, whilst the O. crittendenii showed 2.1% and 2.4% bp differences with O. dendroplaca and O. mashiginensis, respectively. Thus, the mt SSU analysis again showed that sequences of O. crittendenii and O. deosaiensis are positioned on well-supported branches.

Figure 5. 

Phylogenetic tree of the genus Oxneriaria as generated by Maximum Likelihood (ML) analyses, based on mt SSU sequences. Bootstrap values > 70%, based on 1,000 replicates are shown at the branches. Novel sequences, generated during this study, are shown in bold.

Taxonomy

Oxneriaria crittendenii Usman & Khalid

MycoBank No: 848889
Fig. 1

Etymology

The specific epithet “crittendenii” refers to the British lichenologist Prof. Peter D Crittenden in recognition for his outstanding contributions to lichenology.

Holotype

Pakistan. Gilgit Baltistan: Deosai Plains (35°0'45.73"N, 75°13'25.95"E, elev. 4,651 m) on rocks, 13 May 2019, M. Usman DEO117 (LAH, holotype; LAH37193). GenBank OR037223 [ITS], OR037219 [LSU], OR037259 [mt SSU].

Diagnosis

It differs from its closest species O. pruinosa by having lobate black margins (vs. non-lobate), orbicular thallus 1.5–5 cm (vs. irregular 3–8 cm), K test negative (vs. K positive yellow), distinct proper-exciple 17–40 µm wide (vs. indistinct) and polarilocular ellipsoid ascospores (vs. simple ellipsoid).

Description

Thallus crustose, epilithic, orbicular, 1.5–5 cm across, zonate, fine bullate to areolate in the centre to poorly areolate towards margin, in the centre areoles 0.5–1 mm diam. and a few areoles changing to squamules up to 1.8 mm in length, lobate at margins, determinate and radiate. Hypothallus distinct, shiny light brown. Upper surface grey with white powdery texture and black at margins. Thallus heteromerous, upper cortex 20–60 µm thick, globose to sub-globose hyaline paraplectenchymatous cells, 6–11 µm in diam. Algal layer discontinuous, 90–140 µm thick, photobiont Trebouxia sp, coccoid cells, globose to sub-globose 6–14 µm in diam. Medulla and lower cortex not differentiated and consisting of paraplectenchymatous, globose to sub-globose hyaline cells 25–45 µm in diam.

Apothecia without stipe, aspicilioid, one apothecium per areole, rounded, 600–950 µm in diam., pruinose with black disc 450–700 µm, dull and concave. Proper exciple 17–40 µm thick. Thalline exciple 140–190 µm thick. Epihymenium brown, 10–20 µm thick. Hymenium hyaline, 85–110 µm thick. Hypothecium hyaline, 35–55 µm thick. Asci clavate, 8–spored, 60–100 × 22–30 µm. Ascospores hyaline, ellipsoid, polarilocular, 13–18 × 7–11 µm. Paraphyses moniliform, septate, cylindrical cells 3–10 × 1–2.5 µm, with internally brown terminal cells. Pycnidia roccella type (Ryan et al. 2002), globose to pyriform, 115–200 × 85–200 µm dark brown ostiole, long filiform hyaline conidia, 17–24 × 1 µm.

Ecology

Saxicolous, calcareous, known only from Deosai Plains, Gilgit-Baltistan, occurring at elevations between 4,117 m and 4,651 m in extremely cold conditions.

Chemical study

K -ve, C -ve, KC -ve, UV +ve (light green), hymenium initially blue then turning dark orange after Lugol’s solution. Substictic acid detected through TLC.

Additional material examined

Pakistan. GILGIT BALTISTAN: Deosai Plains, 35°7'22.48"N, 75°36'35.09"E, elev. 4,177 m, on rocks, 3 September 2020, M. Usman & M. Shafiq DEO129 (LAH, paratype; LAH37194; GenBank OR037224 [ITS], OR037220 [LSU], OR037260 [mt SSU].

Oxneriaria deosaiensis Khalid & Usman

MycoBank No: 848890
Fig. 2

Etymology

The specific epithet “deosaiensis” refers to the Deosai Plains, the type locality.

Holotype

Pakistan. Gilgit Baltistan: Deosai Plains (35°0'10.06"N, 75°15'0.45"E, elev. 4,689 m) on soil, 13 May 2019, M. Usman DEO206 (LAH, holotype; LAH37200). GenBank OR037225 [ITS], OR037221 [LSU], OR037261 [mt SSU].

Diagnosis

It differs from its closest species O. pruinosa by having lobate black margins (vs. non-lobate), K test positive light brown (vs. K positive yellow), KC test positive dark brown (vs. KC negative), apothecia epruinose (vs. densely pruinose), distinct proper-exciple 30–50 µm wide (vs. indistinct) and polarilocular ellipsoid ascospores (vs. simple ellipsoid).

Description

Thallus crustose, epilithic, irregular, 1.5–2 cm across, zonate, areolate to poorly bullate up to 0.8 mm in diam. to lobate up to 1.5 mm at margins, determinate and radiate. Hypothallus light grey. Upper surface dull grey, black at margins. Thallus heteromerous, upper cortex 20–55 µm thick, paraplectenchymatous hyaline cells 6–15 µm in diam. Algal layer discontinuous, 50–90 µm thick, photobiont Trebouxia sp, coccoid cells, globose to sub-globose, 13–21 µm in diam. Medulla and lower cortex not differentiated and consisting of paraplectenchymatous, globose to sub-globose hyaline cells, 5–12 µm diam.

Apothecia without stipe, aspicilioid, epruinose, one apothecium per areole, rounded, 520–700 µm in diam., with black disc 350–550 µm in diam., dull, concave. Proper exciple, 30–50 µm thick. Thalline exciple 90–145 µm thick. Epihymenium brown, 10–24 µm thick. Hymenium hyaline, 90–160 µm thick. Hypothecium hyaline, 50–90 µm thick. Asci clavate, 8–spored, 75–110 × 16–27 µm. Ascospores hyaline, ellipsoid, polarilocular 11–18 × 7–10 µm. Paraphyses moniliform, septate, cylindrical cells 4–10 × 1–2 µm, with internally brown terminal cells. Pycnidia roccella type (Ryan et al. 2002), globose to pyriform, 230–320 × 210–280 µm dark brown ostiole, long filiform hyaline conidia, 19–35 × 1 µm.

Ecology

Saxicolous, Quartz, known only from Deosai Plains, Gilgit-Baltistan, occurring at elevations between 4,364 m and 4,689 m in extreme cold conditions.

Chemical study

K +ve (light brown), C -ve, KC +ve (dark brown), UV +ve (light green), hymenium initially blue then turning dark blue after Lugol’s solution. Substictic acid and two unknown substances detected through TLC.

Additional material examined

Pakistan. GILGIT BALTISTAN: Deosai Plains, 35°6'28.58"N, 75°44'27.37"E, 4,364 m, on rocks, 15 May 2019, M. Usman & Kamran Habib DEO666 (LAH, paratype; LAH37416; GenBank OR037226 [ITS], OR037222 [LSU], OR037262 [mt SSU].

Discussion

The genus Oxneriaria was introduced by Haji-Moniri et al. (2017) and is characterised by the presence of radiating thalli with a wrinkled or lobate peripheral zone, relatively small ascospores, the possible presence of substictic acid and phylogenetic divergence from neighbouring taxa. Four species of the genus Oxneriaria have recently been described from Pakistan from relatively high altitude locations, namely O. iqbalii from Dassu and Miandam (at elev. 1,607 m and 1,800 m), O. kohistaniensis from Dassu and Razika Seo Valley (at elev. 1,607 m and 1,811 m), O. pakistanica from Darel Valley (at elev. 1,900 m and 2,000 m) and O. pruinosa from Chitral (at elev. 2,550 m) (Asghar et al. 2023; Iqbal et al. 2023; Zulfiqar et al. 2023). By contrast, the two proposed new species, O. crittendenii and O. deosaiensis, reported in the current study, were found occurring at very high altitude elevations between 4,117 m and 4,689 m in environments subject to periodic extremely cold conditions.

The two new proposed species share some morphological similarities to each other such as dull coloured grey to brown, areolate to bullate, heteromerous thalli with black lobate margins, a discontinuous algal layer, medulla consisting of paraplectenchymatous cells and concave black apothecia showing as light green in response to UV. However, the two species, O. crittendenii and O. deosaiensis, also exhibit differences from each other in thallus growth- pattern (orbicular vs. irregular), hypothallus appearance (shiny brown vs. light grey), algal layer (90–140 µm vs. 50–90 µm), size of algal cells (6–14 µm vs. 13–21 µm), size of lower cortex cells (25–45 µm vs. 5–12 µm), apothecia (pruinose 0.6–0.95 mm diam. vs. epruinose 0.52–0.7 mm diam.) and thalline exciple (140–190 µm vs. 90–145 μm thick) and hypothecium (35–55 µm vs. 50–90 µm thick), respectively. Additionally, in response to Lugol’s solution, the hymenium of O. crittendenii turned dark orange, whilst that of O. deosaiensis turned dark blue.

The two new proposed species O. crittendenii and O. deosaiensis were found to be phylogenetically closely related to certain other Oxneriaria species, in particular O. pakistanica, O. pruinosa and O. rivulicola, although clear molecular differences were apparent in the ITS, LSU and mt SSU sequences. There were, in addition, some striking phenotypic characters showing the distinctive characteristics of the novel taxa along with the closest species and these are shown in Table 2.

Table 2.

Comparison of closely-related species of Oxneriaria with novel taxa.

Characters O. crittendenii O. deosaiensis O. pakistanica O. pruinosa O. rivulicola
Margins lobate, determinate, black lobate, determinate, black areolate, indeterminate, whitish-grey lobate, determinate, whitish-grey Non-elongate areoles
Hypothallus shiny light brown light grey light brown light grey light grey
Upper Cortex 20–60 µm thick 20–55 µm thick 10–25 μm thick 30–50 μm thick 25–40 μm thick
Algal Layer (thick) 90–140 µm 50–90 µm 30–50 μm 70–140 μm 30–50 μm
Algal Cells (in diam.) 6–14 µm 13–21 µm 10–15 μm 10–17 μm 7–15 μm
Apothecia (in diam.) pruinose, 450–700 µm epruinose, 520–700 µm epruinose, up to 2 mm densely pruinose, up to 1 mm up to 2 mm
Hypothecium (thick) 35–55 µm 50–90 µm 90–170 μm 50–120 μm 80–100 μm
Asci 60–100 × 22–30 µm 75–110 × 16–27 µm. 60–80 × 30–40 μm 55–80 × 25–42 μm 70–85 × 20–24 μm
Pycnidia roccella type roccella type absent globose globose
Conidia 17–24 × 1 µm 19–35 × 1 µm absent 14–18 × 1 µm 30–37 × 1 µm
References This Study This Study Iqbal et al. (2023) Asgar et al. (2023) Magnusson (1923); Nordin et al. (2011)

In addition to the differences of Table 2, O. crittendenii and O. deosaiensis have polarilocular ellipsoid ascospores whilst O. pakistanica, O. pruinosa and O. rivulicola have simple ellipsoid ascospores. Chemically, O. crittendenii showed no change to K and KC tests, whilst the thalli of O. deosaiensis turned light brown and dark brown in response to K and KC tests, respectively. By contrast to these tests, O. pakistanica showed positive K (yellowish green) and KC (light green) tests, O. pruinosa showed K positive (yellow) and KC negative tests (Asghar et al. 2023; Iqbal et al. 2023), whilst O. rivulicola showed no change to K and KC tests (Magnusson 1923; Nordin et al. 2011).

Conclusions

In summary, as a result of all the distinct phenotypic and phylogenetic characters, we here propose the addition of two new species in the genus Oxneriaria from high altitudinal environments in Pakistan. Whilst these were found infrequently, the detection of the two new species O. crittendenii and O. deosaiensis add to reports of the discovery of other new species of lichen-forming fungi from the Deosai Plains in Pakistan (Usman et al. 2021, 2023), emphasising the importance of this region as a site of arctic-alpine biodiversity.

Acknowledgements

The corresponding author (MU) thanks the Higher Education Commission of Pakistan for funding research work under the International Research Support Initiative Program (IRSIP) scheme. All the authors are grateful to Prof. Dr. Peter D Crittenden (School of Life Sciences, University of Nottingham, UK) and Prof. Dr. Pradeep Kumar Divakar (Departamento de Farmacología, Farmacognosia y Botánica Facultad de Farmacia, Universidad Complutense de Madrid Plaza de Ramón y Cajal, Madrid, Spain) for providing lichen herbarium specimens for thin layer chromatography.

Additional information

Conflict of interest

The authors have declared that no competing interests exist.

Ethical statement

No ethical statement was reported.

Funding

This research was supported by Higher Education Commission of Pakistan for funding research work under the International Research Support Initiative Program (IRSIP) scheme.

Author contributions

Conceptualization: MU. Data curation: MU. Formal analysis: MU. Funding acquisition: ANK. Investigation: MU. Methodology: MU. Software: MU. Supervision: CMW, ANK, PSD, MB. Validation: ANK, MB, CMW, PSD. Visualization: CMW, ANK, MB, PSD. Writing - original draft: MU. Writing - review and editing: CMW, ANK, PSD, MB.

Author ORCIDs

Muhammad Usman https://orcid.org/0000-0002-3490-058X

Paul S. Dyer https://orcid.org/0000-0003-0237-026X

Matthias Brock https://orcid.org/0000-0003-2774-1856

Christopher M. Wade https://orcid.org/0000-0002-1269-9694

Abdul Nasir Khalid https://orcid.org/0000-0002-5635-8031

Data availability

All of the data that support the findings of this study are available in the main text.

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