Abstract
Micropsalliota is a genus of small to relatively medium-sized saprotrophic mushrooms, with fibrillose-squamulose pileus surface, ellipsoid to amygdaliform or cymbiform basidiospores, usually with capitate cheilocystidia, and encrusted pileus hyphae. In this study, two new species, namely Micropsalliota latiumbonata and M. striata are described from Oman, based on morphology and multigene (ITS-28S-rpb2-tef1-α) phylogenetic analysis. Micropsalliota latiumbonata is characterized by a broadly umbonate pileus disc with fibrillose-squamulose surface, fibrils dark-brown and more or less recurved, cheilocystidia capitate with olivaceous capitulum, broadly fusiform to amygdaliform basidiospores measuring 6.0–7.0 × 4.0–4.5 µm, and occurring gregariously around termite mounds. Micropsalliota striata is another small-sized species with an acute papillate pileus disc with appressed fibrils, striate-appendiculate pileus margins, utriform cheilocystidia without a capitate apex, clavate to subglobose pileocystidia, and comparatively larger basidiospores (6.5–7.5 × 3.7–4.1 µm). Both the new species belong to Clade megaspora. A detailed description, photographs of basidiomata, illustrations of anatomical characteristics, a multigene phylogenetic tree, and morphological comparison with similar species are provided. With the description of these two species, the number of known species in Micropsalliota rises to 108.
Key words: Agarics, clade, megaspora, taxonomy, termite mounds
Introduction
The genus Micropsalliota Höhn. is a group of small, slender mushrooms, forming the basal lineage in the subfamily Leucocoprinoideae R.L. Zhao & J.X. Li within Agaricaceae Chevall. (Li et al. 2025). Morphologically, Micropsalliota has the following combination of characters, including agaricoid, small to relatively medium-sized basidiomata (except M. geesterani (Bas & Heinem.) R.L.Zhao & L.A.Parra with large basidiomata), fibrillose to squamulose pilei with fibrils/squamules often brownish, reddish or whitish in color, usually with umbonate pileus disc, annulus membranous (if present), brownish spore print, basidiospores ellipsoid to amygdaliform usually with apical thickening, cheilocystidia mostly capitate or subcapitate, and more or less with incrusted pileus hyphae (Al-Kharousi et al. 2022; Li et al. 2025).
In recent years, the taxonomic work on Micropsalliota has been accelerated with the introduction of many new species on the basis of morphology and DNA sequence data (Zhao et al. 2010; Wei et al. 2015; Chen et al. 2016; He et al. 2020; Li et al. 2021; Patil et al. 2022, 2025; Yan et al. 2022; Gao et al. 2024; Li et al. 2025; Wang et al. 2026). In a systematic study of Agaricaceae s.l. using genomic data, it was found that Micropsalliota forms a basal lineage with genera such as Leucocoprinus, Leucoagaricus, and Macrolepiota, collectively forming the subfamily Leucocoprinoideae (Li et al. 2025).
Currently, more than 100 Micropsalliota species have been described worldwide, distributed in tropical and subtropical regions of Africa (Heinemann 1983; Cao et al. 2025; Liu et al. 2025), Americas (Heinemann 1989; Guzmán-Dávalos and Heinemann 1994) and Asia (Zhao et al. 2010; Wei et al. 2015; Chen et al. 2016; He et al. 2020; Li et al. 2021; Patil et al. 2022, 2025; Yan et al. 2022; Gao et al. 2024; Li et al. 2025; Wang et al. 2026). Previously, only Micropsalliota ventricocystidiata Al-Sadi & S. Hussain has been reported from Oman (Al-Kharousi et al. 2022).
The southern part of Oman (Dhofar Governorate) experiences monsoon rains in July to September each year, which influence the growth and development of various kinds of mushrooms (Hussain et al. 2022, 2024a, 2024b, 2025a, 2025b). The area of Dhofar which is under the influence of monsoon rains, has a large population of a termite species (Macrotermes subhyalinus), making huge termite mounds (AlShamakhi et al. 2024). It was observed that these termite mounds provide a favorable habitat for the growth of various mushrooms (Hussain et al. 2024b, 2024c, 2026).
In this study, several mushroom specimens were collected during the 2025 monsoon season. Morphological characterization of basidiomata and multigene phylogenetic analyses showed that these collections represent two new species in the genus Micropsalliota, which are described here.
Materials and methods
Specimen collections and morphology
Basidiomata were collected during the rainy season, in August-September 2025, from Ain Athum, Ashwur and Qashrub areas, near Salalah, Dhofar Governorate, the southern region of the Sultanate of Oman. The basidiomata were photographed in their natural habitat, tagged with collection information (Rathnayaka et al. 2025), and macromorphological characters, including basidiomata size, shape, and color (according to Munsell Soil Color Charts; Munsell 1975) were recorded. The specimens were brought to the field station, where the fruiting bodies were dried at 45 °C in a fruit dehydrator (Semikorn Electronic Technology Co., Ltd., Guangdong, China). After drying, the samples were sealed in zipper bags and stored at −80 °C for two weeks to eliminate any insect eggs or larvae. The studied materials were deposited in the Fungal Collections at the Center for Environmental Studies and Research (CESAR), Sultan Qaboos University, Oman.
A thin hand-cut section from pileus covering, lamellae, and stipe was prepared for microscopic observation, using 5% aqueous KOH (w/v) and stained in 1% Congo red (w/v) for better contrast. Microscopic features, including the size, shape, color, surface features of basidiospores, basidia, cheilo-, pleuro-, and caulocystidia, and pileipellis were observed under a light microscope (ECLIPSE Ni-U, Nikon Co., Ltd., Japan). Basidiospores’ notations are presented as: [n/o/p] where n is the number of basidiospores measured, from o number of basidiomata, and from p collections; the dimensions (a)b–c(d), where b–c includes at least 90% of measurements and ‘a’ and ‘d’ are extreme values. Q is the length/width ratio for individual spores; av. Q is the mean Q. For morphological description, Bas et al. (2011) was followed.
DNA extraction, amplification, and sequencing
DNA was extracted from dried specimens using Tissue DNA Preparation – Column Kit (Jena Bioscience GmbH, Jena, Germany). Three DNA regions were amplified, including internal transcribed spacer (ITS) and D1/D2 domains of the large subunit of nuclear ribosomal DNA (28S), and a segment of a protein-coding gene, the translation elongation factor 1 alpha (tef1-α). The primers were ITS5/ITS4 for ITS (Gardes and Bruns 1993; White et al. 1990), LR0R/LR5 for 28S (Vilgalys and Hester 1990), and EF1-983F/EF1-1567R for tef1-α (Rehner and Buckley 2005), respectively. Conditions for polymerase chain reactions (PCR) were set as: an initial denaturation at 94 °C for 3 min, followed by 35 cycles of denaturation at 94 °C for 30 s, annealing at the gene-specific temperature and duration (ITS: 56 °C for 40 s; 28S: 52 °C for 45 s; tef1-α: 60 °C for 46 s), extension at 72 °C for 50 s, and a final extension at 72 °C for 10 min, followed by a 4 °C soak. PCR reactions were performed with PuReTaq Ready-To-Go PCR beads (GE Healthcare UK Limited, Buckinghamshire, UK). These reagents were added to each PCR bead: 1.0 µL of each primer (10 µmol/L), 2 µL of DNA template, and 21 µL nuclease-free water. The amplified regions were purified and sequenced with same primers at Macrogen Inc. © (Seoul, Republic of Korea).
Sequence alignment and phylogenetic analyses
The newly generated sequences of both forward and reverse primers of ITS, 28S, and tef1-α were cleaned to consensus sequences using BioEdit v. 7.0.9 (Hall 1999). In BLAST searches, the ITS sequences of the proposed new species Micropsalliota latiumbonata showed the highest similarity of 96.56% with an undescribed species from Oman M. sp. DRB-23-013 (PV088726) and 95.01% with M. appendiculata LE F-315913 (OR161109, Vietnam), while 2nd new species M. striata has 97.50% similarity with the undescribed species M. sp. DRB-23-013 (PV088726, Oman). A combined dataset of ITS-28S-rpb2-tef1-α was constructed (Gao et al. 2024; Yan et al. 2025). The final dataset comprised 112 specimens, including 109 Micropsalliota specimens and three outgroup taxa (Agaricus arabiensis SQUH-SNT007, Coniolepiota spongodes PNG012/MFLU 09-0012, and Hymenagaricus wadijarzeezicus JHN-22-019). These taxa were used as outgroups because they belong to the subfamily Agaricoideae R.L. Zhao & J.X. Li (Agaricaceae), a lineage phylogenetically distinct from the ingroup taxa, making them suitable for rooting the phylogenetic tree (Li et al. 2025). The dataset was based on the sequences employed in the recent phylogenetic studies of Micropsalliota (Yan et al. 2022; Gao et al. 2024; Yan et al. 2025). The dataset was aligned using MAFFT v.7 (Katoh et al. 2019), and adjusted in BioEdit v.7.0.9.0 (Hall 1999) and finally in ClustlX v. 2.1 (Larkin et al. 2007). Details of the sequences used in this study are given in Table 1.
Table 1.
Sequence information used in the phylogenetic analyses of Micropsalliota, bold are the newly generated sequences, (–) means data unavailable.
| Taxa | Vouchers | Country | ITS | 28S | rpb2 | tef1-α | Reference |
|---|---|---|---|---|---|---|---|
| Micropsalliota alba | – | India | EF069420 | – | – | – | Gao et al. 2024. |
| M. albella | LE2016123 | Thailand | MN294514 | MN294516 | – | – | He et al. 2020. |
| M. albofelina | LE312536 | Vietnam | OK257212 | OK257209 | – | – | Crous et al. 2021. |
| M. albofelina | HKAS70329 | China | OR799877 | OR799922 | OR962218 | OR962180 | Gao et al. 2024. |
| M. albosericea | SFSU-zrl-3049 | Thailand | HM436644 | – | – | – | Zhao et al. 2010. |
| M. allantoidea | SFSU-zrl-2038 | Thailand | HM436648 | HM436597 | – | – | Zhao et al. 2010. |
| M. appendiculata | HKAS131127 | China | OR799912 | OR799956 | OR962247 | OR962204 | Gao et al. 2024. |
| M. appendiculata | LE F-315913 | Vietnam | OR161109 | OR161104 | – | – | Ivanova et al. 2023. |
| M. arginophaea | SFSU-zrl-3110 | Thailand | HM436617 | HM436577 | – | – | Zhao et al. 2010. |
| M. arginophaea | HKAS60309 | China | OR799878 | OR799923 | OR962219 | OR962208 | Gao et al. 2024. |
| M. bifida | SFSU-zrl-3067 | Thailand | HM436640 | HM436591 | – | – | Zhao et al. 2010. |
| M. bifida | HFJAU2998 | China | OM650272 | OM650252 | OM669858 | – | Yan et al. 2022. |
| M. bispora | HFJAU3833 | China | PQ345346 | PQ345351 | PQ358515 | PQ358519 | Yan et al. 2025 |
| M. bispora | HFJAU4253 | China | PQ345347 | PQ345352 | PQ358516 | PQ358520 | Yan et al. 2025 |
| M. brunneosquamata | LD201236 | Thailand | KP316210 | – | – | – | Chen et al. 2016. |
| M. cortinata | SFSU-zrl-2129 | Thailand | HM436630 | HM436593 | – | – | Zhao et al. 2010. |
| M. cortinata | HKAS92221 | China | OR799879 | OR799924 | OR962220 | OR962183 | Gao et al. 2024. |
| M. delicatula | HKAS54332 | China | OR799880 | OR799925 | OR962221 | OR962209 | Gao et al. 2024. |
| M. delicatula | ZRL2015234 | China | MT671229 | – | – | – | Li et al. 2021. |
| M. dentatomarginata | GX20170202 | China | MT671228 | MT671242 | – | – | Li et al. 2021. |
| M. digitatocystis | HKAS123832 | China | OR799883 | OR799928 | OR962224 | OR962185 | Gao et al. 2024. |
| M. digitatocystis | ZRL20180564 | China | MT671239 | MT671250 | – | – | Li et al. 2021. |
| M. ferruginea | HKAS131130 | China | OR799885 | OR799930 | OR962226 | OR962182 | Gao et al. 2024. |
| M. ferruginea | HKAS70562 | China | OR799884 | OR799929 | OR962225 | OR962181 | Gao et al. 2024. |
| M. fimbriata | HKAS60241 | China | OR799886 | OR799931 | OR962227 | OR962198 | Gao et al. 2024. |
| M. fimbriata | HKAS60261 | China | OR799887 | OR799932 | – | OR962199 | Gao et al. 2024. |
| M. furfuracea | SFSU-zrl-3006 | Thailand | HM436621 | HM436603 | – | – | Zhao et al. 2010. |
| M. furfuracea | HKAS60229 | China | OR799889 | OR799934 | OR962229 | OR962201 | Gao et al. 2024. |
| M. geesterani | LAPAG520 | Thailand | KM923965 | KM923966 | – | – | Parra et al. 2016. |
| M. geesterani | E.C. Vellinga 2263(L) | Netherlands | AF482857 | AF482888 | – | – | Parra et al. 2016. |
| M. gigaspora | HKAS131118 | China | OR799890 | OR799935 | OR962230 | – | Gao et al. 2024. |
| M. gigaspora | HKAS131119 | China | OR799891 | OR799936 | – | – | Gao et al. 2024. |
| M. globocystis | HKAS131120 | China | OR799892 | OR799937 | – | OR962186 | Gao et al. 2024. |
| M. globocystis | HFJAU1518 | China | OM650277 | OM650255 | OM669852 | – | Yan et al. 2022. |
| M. globocystis | HKAS131133 | China | OR799895 | OR799940 | OR962234 | OR962197 | Gao et al. 2024. |
| M. globocystis | HKAS92202 | China | OR799894 | OR799939 | OR962233 | OR962196 | Gao et al. 2024. |
| M. globocystis | VDW1278 | South Africa | MT304640 | – | – | – | Yan et al. 2022. |
| M. globocystis | SFSU-zrl-2049 | Thailand | HM436635 | – | – | – | Zhao et al. 2010. |
| M. globocystis | HFJAU2709 | China | OM650278 | OM650262 | OM669856 | – | Yan et al. 2022. |
| M. globovelveta | HFJAU3842 | China | PV277734 | PV269809 | PV289604 | PV289605 | Liu et al. 2025 |
| M. gracilis | SFSU-zrl-2041 | Thailand | HM436647 | HM436583 | – | – | Zhao et al. 2010. |
| M. gracilis | HNL503432 | Laos | MW192914 | – | – | – | Yan et al. 2022. |
| M. inflata | LE F-315912 | Vietnam | OR161110 | OR161106 | – | – | Ivanova et al. 2023. |
| M. jiangxiensis | THJ20018 | China | ON117420 | ON117438 | – | – | Ji and He 2023. |
| M. jiangxiensis | THJ20019A | China | ON117421 | ON117439 | – | – | Ji and He 2023. |
| M. latiumbonata | QRB-14-25 | Oman | PZ127411 | PZ127514 | – | PZ390627 | This study |
| M. latiumbonata | ASH-005-25 | Oman | PZ127410 | PZ127513 | – | PZ390625 | This study |
| M. latiumbonata | ASH-006-25 | Oman | PZ127412 | PZ127515 | – | PZ390626 | This study |
| M. latiumbonata | ASH-007-25 | Oman | PZ127413 | PZ127516 | – | PZ386150 | This study |
| M. latiumbonata | ASH-009-25 | Oman | PZ127414 | PZ127517 | – | PZ176529 | This study |
| M. lateritia | SFSU-zrl-2073 | Thailand | HM436631 | – | – | – | Zhao et al. 2010. |
| M. lateritia | HKAS131124 | China | OR799896 | OR799941 | OR962235 | OR962202 | Gao et al. 2024. |
| M. longicystis | HKAS131121 | China | OR799897 | OR799942 | OR962257 | – | Gao et al. 2024. |
| M. longicystis | HKAS131126 | China | OR799898 | OR799943 | OR962258 | – | Gao et al. 2024. |
| M. megarubescens | SFSU-zrl-2086 | Thailand | HM436620 | – | – | – | Zhao et al. 2010. |
| M. megarubescens | HKAS60253 | China | OR799900 | OR799945 | OR962237 | OR962189 | Gao et al. 2024. |
| M. megaspora | SFSU-zrl-3068 | Thailand | HM436624 | – | – | – | Zhao et al. 2010. |
| M. megaspora | HFJAU1255 | China | OM650282 | OM650258 | OM669876 | – | Yan et al. 2022. |
| M. minor | HFJAU2796 | China | OM650294 | OM650266 | OM669865 | – | Yan et al. 2022. |
| M. nana | HKAS114619 | China | OR799901 | OR799946 | OR962238 | OR962216 | Gao et al. 2024. |
| M. nana | HKAS115226 | China | OR799902 | OR799947 | – | OR962217 | Gao et al. 2024. |
| M. ovalispora | HFJAU2010 | China | OM650295 | OM650269 | OM669866 | – | Yan et al. 2022. |
| M. ovalispora | HFJAU3179 | China | OM650296 | – | OM669867 | – | Yan et al. 2022. |
| M. pakistanica | LAH38139 | Pakistan | PP357040 | PP383879 | – | – | Maula et al. 2025 |
| M. pakistanica | LAH38140 | Pakistan | PP357041 | PP383880 | – | – | Maula et al. 2025 |
| M. pileocystidiata | AMH9975 | India | MG917970 | – | – | – | Patil et al. 2022. |
| M. pileocystidiata | MMH1114 | India | MZ598496 | – | – | – | Patil et al. 2022. |
| M. pleurocystidiata | SFSU-zrl-2023 | Thailand | HM436636 | – | – | – | Zhao et al. 2010. |
| M. pseudoarginea | HKAS131125 | China | OR799903 | OR799948 | OR962239 | OR962212 | Gao et al. 2024. |
| M. pseudoarginea | HFJAU2122 | China | OM650284 | OM650260 | OM669861 | – | Yan et al. 2022. |
| M. pseudodelicatula | HKAS131129 | China | OR799905 | OR799950 | OR962241 | OR962213 | Gao et al. 2024. |
| M. pseudodelicatula | HFJAU2228 | China | OM650288 | OM650264 | OM669863 | – | Yan et al. 2022. |
| M. pseudoglobocystis | HKAS87127 | China | OR799908 | OR799953 | OR962244 | OR962190 | Gao et al. 2024. |
| M. pseudoglobocystis | ZRL2013321 | China | KM889913 | – | – | – | Wei et al. 2015. |
| M. purpureobrunneola | LE2016124 | Thailand | MN294513 | MN294517 | – | – | He et al. 2020. |
| M. pusillissima | SFSU-zrl-3047 | Thailand | HM436645 | HM436594 | – | – | Zhao et al. 2010. |
| M. repanda | LAPAF8 | Togo | KP739805 | KP739804 | – | – | Parra et al. 2016. |
| M. rosea | LAH38149 | Pakistan | PP377825 | PP378506 | – | – | Maula et al. 2025 |
| M. rosea | LAH38186 | Pakistan | PQ623104 | PQ623106 | – | – | Maula et al. 2025 |
| M. roseipes | HFJAU2494 | China | OM650297 | OM650270 | OM669870 | – | Yan et al. 2022. |
| M. rubrobrunnescens | SFSU-zrl-2120 | Thailand | HM436628 | HM436588 | – | – | Zhao et al. 2010. |
| M. rubrobrunnescens | HKAS96929 | China | OR799914 | OR799958 | OR962249 | OR962206 | Gao et al. 2024. |
| M. rubrobrunnescens | SFSU-zrl-2121 | Thailand | HM436629 | HM436589 | – | – | Zhao et al. 2010. |
| M. rufosquarrosa | HFJAU1208 | China | OM650291 | OM650267 | OM669868 | – | Yan et al. 2022. |
| M. rufosquarrosa | HFJAU1236 | China | OM650292 | OM650268 | OM669869 | – | Yan et al. 2022. |
| M. squarrosa | HKA128713 | China | OR799916 | OR799960 | OR962251 | – | Gao et al. 2024. |
| M. squarrosa | HKAS128633 | China | OR799915 | OR799959 | OR962250 | – | Gao et al. 2024. |
| M. sp. | DRB-23-013 | Oman | PV088726 | PV093920 | – | – | Unpublished |
| M. striata | ATM-009-25 | Oman | PZ127415 | PZ127518 | – | – | This study |
| M. subalba | SFSU-zrl-2080 | Thailand | HM436646 | HM436596 | – | – | Zhao et al. 2010. |
| M. subalba | HKAS105828 | China | OR799917 | OR799961 | – | OR962211 | Gao et al. 2024. |
| M. subarginea | SFSU-zrl-2052 | Thailand | HM436612 | HM436573 | – | – | Zhao et al. 2010. |
| M. subarginea | SFSU-zrl-2092 | Thailand | HM436611 | HM436574 | – | – | Zhao et al. 2010. |
| M. subumbonata | AMH 10512 | India | PP837559 | PQ576415 | – | – | Patil et al. 2025. |
| M. subumbonata | MMH 2312 | India | PQ577838 | PQ580740 | – | – | Patil et al. 2025. |
| M. suricatoides | LE F-348071 | Vietnam | OR161111 | OR161105 | – | – | Ivanova et al. 2023. |
| M. suricatoides | LE F-348072 | Vietnam | OR161112 | – | – | – | Ivanova et al. 2023. |
| M. tenuipes | HFJAU1536 | China | OM650289 | – | – | – | Yan et al. 2022. |
| M. tenuipes | HFJAU3180 | China | OM650290 | OM650265 | – | – | Yan et al. 2022. |
| M. umbonata | HKAS131131 | China | OR799920 | OR799964 | OR962254 | OR962194 | Gao et al. 2024. |
| M. umbonata | HKAS131132 | China | OR799921 | OR799965 | OR962255 | OR962195 | Gao et al. 2024. |
| M. ventricocystidiata | SQUH-ATR004 | Oman | OM397373 | OM630413 | – | – | Al-Kharousi et al. 2022. |
| M. ventricocystidiata | SQUH-GOB002 | Oman | OM397374 | OM630414 | – | – | Al-Kharousi et al. 2022. |
| M. ventricocystidiata | JEB-001-25 | Oman | PZ127409 | PZ127512 | – | PZ176528 | This study |
| M. vulgaris | HFJAU3350 | China | PQ345344 | PQ345349 | PQ358513 | PQ358517 | Yan et al. 2025. |
| M. vulgaris | HFJAU5707 | China | PQ345345 | PQ345350 | PQ358514 | PQ358518 | Yan et al. 2025. |
| M. wuyishanensis | HFJAU3048 | China | OM650298 | – | OM669878 | – | Yan et al. 2022. |
| M. xanthorubescens | SFSU-zrl-3083 | Thailand | HM436638 | HM436598 | – | Zhao et al. 2010. | |
| M. xanthorubescens | SFSU-zrl-3096 | Thailand | HM436637 | HM436599 | – | Yan et al. 2022. | |
| Agaricus arabiensis | SQUH-SNT007 | Oman | OM971855 | OM971859 | ON568585 | Hussain et al. 2022. | |
| Hymenagaricus wadijarzeezicus | JHN-22-019 | Oman | OR612998 | OR613021 | OR729600 | Hussain et al. 2024b. | |
| Coniolepiota spongodes | PNG012/MFLU 09-0012 | Thailand | HM488756 | HM488774 | HM488796 | HM488883 | Vellinga et al. 2011. |
Maximum likelihood (ML) and Bayesian Inference (BI) methods were used for phylogenetic analyses. The BI phylogeny was performed using MrBayes v. 3.2.6 (Ronquist et al. 2012), and the best-fit model (GTR+F+I+G4) was selected following ModelFinder (Kalyaanamoorthy et al. 2017). Four Markov chains were run each for one million generations and sampled every 100th generations. Burn-in was determined by checking the likelihood trace plots in Tracer v. 1.7 (Rambaut et al. 2018) and subsequently discarded. Maximum likelihood (ML) analyses were tested with RAxML v. 8 (Stamatakis 2014) with 1000 bootstrap replicates. The best model (GTR+I+G) was chosen according to the corrected Akaike information criteria (AICc) (Lanfear et al. 2017). The BI posterior probabilities (PPs) and ML bootstrap percentages (BT) of ≥ 0.95 and ≥ 70%, respectively were considered significant and shown on phylogenetic tree (Fig. 1) in order of (BT/PPs). Tree files were visualized with FigTree v.1.4.2 (Rambaut 2012) followed by annotation in Adobe Illustrator CC2019.
Figure 1.
Multigene phylogeny of Micropsalliota generated by ML analyses, based on combine sequence data of ITS-28S-rpb2-tef1-α, with Agaricus arabiensis, Coniolepiota spongodes, and Hymenagaricus wadijarzeezicus as outgroup taxa. Bayesian posterior probabilities (PPs) and ML bootstrap percentage (BT) ≥ 0.95 and ≥70%, respectively, are shown above the nodes. Eleven clades were recovered, each branch represents species name, followed by voucher number, and country of origin, specimens studied during this work are in bold fonts, and both the new species are grouped in Clade megarspora.
Results
Phylogenetic analyses
The final aligned multigene dataset consisted of 112 specimens with 3310 characters long, including 1875 constant sites, 980 informative sites, and 455 uninformative sites. These 112 specimens represent 55 named species, and one unnamed species of the genus Micropsalliota, along with the three outgroup taxa. Both ML and BI methods generated phylogenies with similar topologies. The ML tree is shown (Fig. 1) with values of both maximum likelihood BT percentage and Bayesian PPs. The presented tree is almost similar to previous phylogenies of Micropsalliota (Gao et al. 2024; Yan et al. 2025), where 109 specimens of the genus grouped in 11 clades, each with strong to excellent phylogenetic support. The representative new species, Micropsalliota latiumbonata and M. striata, are grouped in the Clade megaspora with strong phylogenetic support (98%/0.97).
Taxonomy
Micropsalliota latiumbonata
S. Hussain, Al-Nadabi & Al‐Sadi sp. nov.
63BE31AA-8667-513D-A072-E6C7143605B3
862914
Figure 2.
Basidiomata of the new species of Micropsalliota. a–d. Micropsalliota latiumbonata. a, b. (CESAR-ASH-007-25, holotype); c. ASH-009-25; d. QRB-14-25; e, f. Micropsalliota striata (CESAR-ATM-009-25, holotype). Scale bars: 15 mm.
Figure 3.
Illustrations of microscopic features of Micropsalliota latiumbonata (CESAR-ASH-007-25, holotype). a. Basidiospores; b. Basidia; c. Cheilocystidia (black dots represent the olivaceous content); d. Caulocystidia; e. Pileus squamules. Scale bar: 5 µm (a); 15 µm (b–e).
Etymology.
The specific epithet ‘latiumbonata’ refers to the broadly umbonate pileus disc of the new species.
Diagnosis.
Micropsalliota latiumbonata is a very small-sized species, characterized by a broadly umbonate pileus center, occurring gregariously in a specific habitat of termite mounds, and microscopically with olivaceous capitulum at the apex of cheilocystidia.
Holotype. •
Sultanate Of Oman: Dhofar, Salalah, Ashwur, on soil with grasses on termite mounds, 28 August 2025, S. Hussain, Al-Nadabi, A. Al Sidairi, K. Al-Zeidi & A. Al-Raeesi, ASH-007-25 (CESAR-ASH-007-25, holotype), GenBank accession: ITS = PZ127413, 28S = PZ127516, tef1-α = PZ386150.
Description.
Basidiomata small-sized. Pileus 10–18 mm, at young stage campanulate to hemispherical, becoming convex to plano-convex at mature stage, finally becoming plano-concave to concave in old specimens, with broadly umbonate disc; surface fibrillose-squamulose, fibrils more or less recurved, reddish-brown (10R 5/4–2.5YR 6/4) to dark reddish-brown (10R 3/10–10R 3/14), concentrated at the center, sparser towards the margins; margin appendiculate, whitish; in old specimens the entire basidiomata becoming dark-brown (5YR 1/2–7.5YR 1/2). Context membranous, whitish. Lamellae free, pale pinkish (10R 9/2–7.5YR 9/2) to dark grayish-brown (2.5YR 1/4–7.5R 2/4), broad to ventricose, with fimbriate edge, close with 0–3 series of lamellulae. Stipe 15–30 × 2–3 mm, central, cylindrical, slender, white, surface pruinose to furfuraceous downwards. Context of stipe secreting brownish red (5R 3/10–7.5R 3/10) liquid in some specimens on cutting. Annulus cortinate, whitish.
Basidiospores [141/2/2] (4.5)6.0–7.0(7.8) × (3.5)4.0–4.5(4.7) µm, on average 6.5 × 4.2 µm, Q = 1.4–1.7, av. Q = 1.6, in face view broadly fusiform with a truncate apex, in side view oblong to amygdaliform with slightly flattened on one side, pale brownish, slightly thick-walled, with a prominent apiculus, without germ-pore. Basidia 18–23 × 7.0–8.0 µm, clavate, hyaline, 4-spored, rarely 2-spored. Pleurocystidia absent. Cheilocystidia 32–46 × 9.0–12 µm, hyaline, narrowly utriform to tibiiform capitate apex, capitulum 5–8 µm in diam, smooth, with olivaceous content. Pileus squamules is a cutis, consisting of hyphae 11–15 µm in diam, pale brownish, smooth, cylindrical to elongated, constricted at septa, rarely branched. Caulocystidia 46–88 × 8.0–12 µm, tibiiform to cylindrical, with capitate apex, hyaline. Clamp connection absent in all tissues.
Habit, habitat and distribution.
Gregarious or scattered in small groups, saprotrophic, on the soil of a termite mound. Currently only known from southern Oman.
Additional specimens examined.
• Sultanate Of Oman: Dhofar, Salalah, Qashrub, on soil under herbaceous plants, 27 August 2025, S. Hussain, Al-Nadabi, K. Al-Zeidi & A. Al-Raeesi, QRB-14-25 (paratype CESAR-QRB-14-25), GenBank accession: ITS = PZ127411, 28S = PZ127514, tef1-α = PZ390627; Salalah, Ashwur, on soil with grasses on termite mounds, 28 August 2025, S. Hussain, Al-Nadabi, A. Al Sidairi, K. Al-Zeidi & A. Al-Raeesi, ASH-005-25 (paratype CESAR-ASH-005-25), GenBank accession: ITS = PZ127410, 28S = PZ127513, tef1-α = PZ390625; same area and same date, S. Hussain, Al-Nadabi, A. Al Sidairi, K. Al-Zeidi & A. Al-Raeesi, ASH-006-25 (paratype CESAR-ASH-006-25), GenBank accession: ITS = PZ127412, 28S = PZ127515, tef1-α = PZ390626; same area and same date, S. Hussain, Al-Nadabi, A. Al Sidairi, K. Al-Zeidi & A. Al-Raeesi, ASH-009-25 (paratype CESAR-ASH-009-25), GenBank accession: ITS = PZ127414, 28S = PZ127517, tef1-α = PZ176529.
Note.
The new species Micropsalliota latiumbonata can be recognized by its growing habit, which mainly fruits on a termite mound; pileus with a broadly umbonate center, covered with reddish-brown squamules; and capitate cheilocystidia, with the capitulum containing olivaceous material. There are several species in the genus with a similar combination of characteristics, such as M. albosericea Heinem. & Leelav., M. ferruginea T. Gao & Z.W. Ge, M. fimbriata T. Gao & Z.W. Ge, M. gracilis Heinem., M. longicystis T. Gao & Z.W. Ge, M. nana T. Gao, H. Qu & Z.W. Ge. Micropsalliota albosericea has a whitish fibrillose pileus, basidiospores ovoid or cymbiform with apical thickening and smaller (5–5 × 2.8–3.2 µm), utriform cheilocystidia with capitate apex and hyaline (Heinemann and Leelavathy 1991). Micropsalliota ferruginea was recently reported from China, with a larger pileus (35–50 mm diam), covered with recurved squamules, without a prominent umbo, and smaller cheilocystidia (15–33 × 3–10 µm) with hyaline capitulum (Gao et al. 2024). Similarly, M. gracilis with an umbonate pileus center, covered with brownish-red squamules, basidiospores amygdaliform to ellipsoid and smaller (5.5–6.5 × 3.0–4.0 µm), ventricose to irregularly tibiiform cheilocystidia with hyaline capitate apex (Zhao et al. 2010). Micropsalliota longicystis shares capitate caulo- and cheilocystidia with the new species; however, it is differentiated from M. latiumbonata by its smaller basidiospores (5.0–6.0 × 3.0–3.5 µm), hyaline capitulum of cheilocystidia, and the presence of pleurocystidia (Gao et al. 2024). Micropsalliota nana differentiated from the new species by its silky fibrillose pileus with obtuse umbo, persistent annulus, basidiospores smaller (4.5–6.0 × 3.0–4.0 µm) ellipsoid to amygdaliform, hyaline capitulum of cheilocystidia, with encrusted hyphae in pileus squamules (Gao et al. 2024).
Based on multigene phylogeny, the close relatives of Micropsalliota latiumbonata are M. appendiculata D.D. Ivanova & O.V. Morozova, M. megaspora R.L. Zhao, Desjardin, Soytong & K.D. Hyde, M. repanda Heinem., M. jiangxiensis X.H. Ji & G. He, M. ferruginea, and the proposed new species M. striata sp. nov. Micropsalliota appendiculata has been reported from China and Vietnam under broad-leaved trees, with pyriform to subglobose cheilocystidia, presence of pleurocystidia (broadly clavate to clavate-capitate), with encrusted hyphae of pileus squamules (Gao et al. 2024). Micropsalliota megaspora can be differentiated from the new species by its larger basidiospores (6–8 × 3.8–4.5 µm), ventricose cheilocystidia with hyaline, subcapitate apices, and incrusted hyphae in pileus squamules (Zhao et al. 2010). Basidiomata of Micropsalliota repanda are comparatively larger (pileus diam up to 45 mm), with purplish-red pileal squamules, capitate hyaline (Heinemann 1980). Micropsalliota jiangxiensis with pileus 25–32 mm diam, covered with wood-brown fibrils, basidiospores 5.3–6.7 × 2.9–3.4 µm, ellipsoid, cheilocystidia cylindrical to subclavate with capitate apex, hyaline (Ji and He 2023).
Nucleotide differences in the ITS region of both the new species (Micropsalliota latiumbonata, M. striata) with their close relative M. appendiculata is given in Table 2.
Table 2.
Nucleotide differences in the ITS sequences of the new species and with their closely similar species, - means deletion.
| Species | Collection | Variable positions | ||||||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 73 | 103 | 189 | 193 | 208 | 220 | 229 | 268 | 281 | 445 | 478 | 502 | 590 | 605 | 612 | 622 | 628 | 629 | 639 | ||
| M. latiumbonata | ASH-005-25 | C | T | A | G | G | A | T | T | A | T | T | A | G | T | A | T | T | C | G |
| M. latiumbonata | ASH-006-25 | C | T | A | G | G | A | T | T | A | T | T | G | G | T | A | T | T | C | G |
| M. latiumbonata | ASH-007-25 | C | T | A | G | G | A | T | T | A | T | T | G | G | T | A | T | T | C | G |
| M. latiumbonata | ASH-009-25 | C | T | A | G | G | A | T | T | A | T | T | G | G | T | A | T | T | C | G |
| M. latiumbonata | QRB-14-25 | C | T | A | G | G | A | T | T | A | T | T | G | G | T | T | T | T | C | G |
| M. striata | ATM-009-25 | T | G | G | T | A | A | C | G | T | A | G | G | A | T | A | C | T | T | - |
| M. appendiculata | LE F-315913 | T | G | G | T | A | T | C | G | T | A | G | G | A | T | A | T | A | - | T |
| M. appendiculata | HKAS131127 | T | G | G | T | A | T | C | G | T | A | G | G | A | T | A | T | A | - | T |
Micropsalliota striata
S. Hussain, Al-Nadabi & Al‐Sadi sp. nov.
3039901B-ED86-5E12-BF24-42CCFD9BD4C2
862916
Figure 4.
Illustrations of microscopic features of Micropsalliota striata (CESAR-ATM-009-25, holotype). a. Basidiospores; b. Basidia; c. Cheilocystidia; d. Pleurocystidia; e. Caulocystidia; f. Pileus squamules (back dashes showing the encrusted walls); g. Pileocystidia. Scale bar: 5 µm (a); 15 µm (b–g).
Etymology.
The specific epithet ‘striata’ refers to the fine striate pileus margin of the new species.
Diagnosis.
Micropsalliota striata is a small-sized species characterized by a striate pileus margin, a papillate disc, microscopically with the presence of pileocystidia and caulocystidia.
Holotype.
• Sultanate Of Oman: Dhofar, Salalah, Ain Athum, on moist soil with mosses, 25 August 2025, S. Hussain, Al-Nadabi, A. Al Sidairi, K. Al-Zeidi & A. Al-Raeesi, ATM-009-25 (CESAR-ATM-009-25, holotype), GenBank accession: ITS = PZ127415, 28S = PZ127518.
Description.
Basidiomata small-sized. Pileus 15–20 mm, at young stage paraboloid to hemispherical, becoming convex to plano-convex and applanate at mature stage, with acute papillate disc; surface fibrillose, fibrils appressed, sparse towards the margin, light-pinkish (2.5R 9/4–10RP 9/4) to light yellowish-pink (7.5R 9/4–7.5R 9/6), concentrated at the disc, light-brown (5YR 4/4–7.5YR 4/4) to reddish-brown (10R 5/4–2.5YR 6/4); margins finely striate, exceeding the lamellae, appendiculate, whitish. Context membranous, whitish. Lamellae free, pale pinkish (10R 9/2–7.5YR 9/2) to light reddish-brown (2.5YR 5/4–2.5YR 6/4), ventricose, with fimbriate edge, close with 1–3 series of lamellulae. Stipe 25–40 × 2–3 mm, central, equal, slightly flexuous, slender, pale-pinkish (2.5YR 9/2–7.5R 9/2) to pale-brownish (10R 5/4–10R 6/4), surface pruinose to pulverulent downwards, glabrous upwards. Context of stipe unchanging on bruising or cutting. Annulus absent.
Basidiospores [104/2/1] (6.2)6.5–7.5(8.3) × (3.5)3.7–4.1(4.5) µm, on average 7.0 × 3.9 µm, Q = 1.6–1.8, av. Q = 1.7, in face view oblong to broadly fusiform with truncate apex, in side view amygdaliform to ellipsoid with slightly flattened on one side, pale brownish, slightly thick-walled, with prominent apiculus, without germ-pore. Basidia 14–17 × 5.5–7.0 µm, clavate to cylindrical, hyaline, regularly 4-spored. Pleurocystidia 28–36 × 9.5–11.5 µm, oblong to clavate or narrowly utriform to cylindrical, abundant, hyaline. Cheilocystidia 23–30 × 8.5–11.5 µm, narrowly utriform to utriform without a capitate apex, hyaline. Pileus squamules is a cutis, consisting of encrusted hyphae, 10–25 µm in diam, pale brownish, cylindrical to elongated, constricted at septa, rarely branched. Pileipellis is a hymeniderm to epithelium, consisting of subglobose to clavate pileocystidia, measuring 11.5–20.5 × 7.0–10.5 µm, hyaline, smooth. Caulocystidia 40–51 × 8.5–10 µm, clavate to cylindrical or cylindro-clavate, without a capitate apex, hyaline. Clamp connection absent in all tissues.
Habit, habitat and distribution.
Gregarious or scattered in small groups, saprotrophic, on moist soil with mosses. Currently only known from southern Oman.
Note.
The new species Micropsalliota striata is characterized by its acute papillate pileus disc, with striate pileus margins, having clavate to cylindrical caulocystidia, narrowly utriform to utriform pleuro- and cheilocystidia without a capitate apex, and comparatively larger basidiospores (6.5–7.5 × 3.7–4.1 µm) than M. latiumbonata. In the genus, there are several species with similar kind of characteristics, like: M. appendiculata, M. gigaspora T. Gao & Z.W. Ge, M. pileocystidiata P.B. Patil & S.A. Vaidya, M. pleurocystidiata Heinem. & Little Flower, M. pseudoarginea Heinem. and M. xanthorubescens Heinem. Micropsalliota appendiculata can be differentiated from the new species by its pyriform to subglobose cheilocystidia measuring (16–25 × 10–13 µm), pleurocystidia broadly clavate to clavate-capitate, pileipellis without pileocysidia (Gao et al. 2024). Micropsalliota gigaspora with a subumbonate to applanate pileus disc with crenate margins, stipe with a persistent annulus, lengthy basidiospores (7–9 × 4–5.5 µm), broadly-clavate to clavate cheilocystidia, and 2- and 4-spored basidia (Gao et al. 2024). Micropsalliota pileocystidiata, only known from the type location (Maharashtra, India), is a medium- to large-sized species with pyriform pileocystidia (Patil et al. 2022). Micropsalliota pleurocystidiata is a large-sized species, with a broadly umbonate pileus disc, basidiospores amygdaliform and smaller (5.0–6.0 × 3.0–4.0 µm), broadly ventricose to subcylindrical cheilocystidia (Zhao et al. 2010). Micropsalliota pseudoarginea with glabrous to finely pruinose cap surface, smaller basidiospores (4.0–5.0 × 2.5–3.2 µm), ellipsoid to subcymbiform shape, with clavate to ventricose cheilocystidia (Zhao et al. 2010). Micropsalliota xanthorubescens is a medium-sized species with a subumbonate pileus disc, clavate to ventricose cheilocystidia (Zhao et al. 2010).
Both the newly proposed species, Micropsalliota striata and M. latiumbonata, can be differentiated by several characteristics. Pileus disc in the former is acute papillate as compared to the broadly umbonate disc in the latter; the cap surface is sparsely covered with pinkish, appressed fibrils in M. striata, in contrast to much denser, recurved, and brownish fibrils in M. latiumbonata. Pleurocystidia and pileocystidia are completely absent in M. latiumbonata. Cheilocystidia in M. striata are without a prominent capitate apex; however, the cheilocystidia of M. latiumbonata have a characteristic capitulum with olivaceous content.
Discussion
The present study contributes to the description of two new species of Micropsalliota from Oman, a region that remains underexplored for agaric diversity. In the phylogenetic analyses (Fig. 1), both the proposed new species were grouped in the Clade megaspora. Species in this clade have small pilei with fibrillose-squamulose surface, fibrils/squamules usually brownish, concentrated at the center, the center more or less umbonate, basidiospores ellipsoid to amygdaliform with apical thickening, cheilocystidia ventricose to clavate or subglobse with capitate or subcapitate apex. To the best of our knowledge, M. latiumbonata is the only species having capitate cheilocystidia with olivaceous content in the capitulum.
In this study, species of Micropsalliota were recovered in eleven major clades, similar to a previous phylogeny of the genus (Gao et al. 2024). A couple of species M. bispora J.Q. Yan, S.Nan Wang & H. Zeng and M. vulgaris J.Q. Yan, S.N. Wang & H. Zeng, were described after Gao et al. (2024), however, these species were not placed in any known clade of the genus (Yan et al. 2025). In the current phylogeny, M. bispora was grouped in Clade furfuraceae. Species in this clade have larger basidiospores size about 6.9 × 3.8 µm on average (Zhao et al. 2010; Gao et al. 2024). Similarly, M. vulgaris recovered in Clade cortinata. Species in this clade have a cortinate partial veil remnants at the pileus margin (Zhao et al. 2010; Gao et al. 2024). Clade bifida being the largest clade in Micropsalliota in terms of species, with the inclusion of M. pakistanica Maula, Saba, Asif & Akram (Maula et al. 2025), the number of species increased to 26. Most of the species in Clade bifida have small-sized basidiomata, except M. brunneosquamata Linda J. Chen, R.L. Zhao & K.D. Hyde and M. geesterani with large basidiomata and thickened fleshy pileus (Gao et al. 2024). One species was recently published with valid description; however, the name was invalid (as Micropsalliota rosea Akram, Maula, Saba & Asif (Maula et al. 2025). The species was redescribed with valid name Micropsalliota rosea Akram, Maula, Saba & Asif, but not assigned to any clade of the genus (Javeed et al. 2025). In the present study, M. rosea was grouped in Clade lateritia.
Species of Micropsalliota are saprotrophs in tropical habitats, usually fruiting on humus-rich degrading soil, under forest trees or roadsides (Zhao et al. 2010). In the present study, four collections of one of the new species Micropsalliota latiumbonata (ASH-005-25, ASH-006-25, ASH-007-25 and ASH-009-25) were found on termite mound, suggesting a possible ecological association between these mushrooms and termites. To the best of our knowledge, no species in Micropsalliota has been found on any termite mounds. However, four species of Hymenagaricus were recently reported from Dhofar region, Oman, occurring on termite mounds (Hussain et al. 2024b, 2026). Beside the termite-associated mushroom genus Termitomyces, a number of other mushroom genera, such as Agaricus, Lepiota, Leucocoprinus, Xanthagaricus, Conocybe, and Clitopilus were encountered fruiting on termite mounds in Dhofar region (person. Comm.). Termite mounds that contain abundant moisture and nutrients may provide a suitable habitat for mushroom growth and development. Consequently, further research is necessary to investigate the association between mushrooms and termite mounds in greater detail.
Supplementary Material
Acknowledgements
We would like to thank Said Al-Abri, Administrator, Research Centers, Sultan Qaboos University for facilitating the field visits. This research was funded by Sultan Qaboos University.
Citation
Al-Nadabi H, Hussain S, Al Sidairi A, Al-Zeidi K, Al-Raeesi A, Al-Badi R, Al-Rashdi L, Al-Jashmi J, Velazhahan R, Al-Sadi AM (2026) Morphology and multigene phylogeny reveal two new species of Micropsalliota (Agaricaceae, Basidiomycota) from Dhofar region, southern Oman. MycoKeys 137: 317–336. https://doi.org/10.3897/mycokeys.137.192271
Contributor Information
Hamed Al-Nadabi, Email: hamed@squ.edu.om.
Shah Hussain, Email: s.hussain2@squ.edu.om.
Additional information
Conflict of interest
The authors have declared that no competing interests exist.
Ethical statement
No ethical statement was reported.
Artificial Intelligence (AI) use
The authors accept full responsibility for the content of the manuscript, including the disclosure of any use of AI.
No AI tools were used in the preparation of this manuscript.
Funding
IG Grants, Sultan Qaboos University, Muscat, Oman, grant no. IG/-/DVC/CES/26/421.
Author contributions
Shah Hussain and Hamed Al-Nadabi: conceptualization, sampling, writing – original draft and review and editing, data curation, formal analysis, investigation, methodology, project administration, resources, supervision and visualization. Ahmed Al Sidairi, Khalifa Al-Zeidi, and Ahmed Al-Raeesi: sampling, review and editing. Rahil Al-Badi, Lujain Al-Rashdi, and Jumana Al-Jashmi: sample processing, molecular investigation. Rethinasamy Velazhahan and Abdullah M. Al-Sadi: review-editing, and supervision.
Author ORCIDs
S. Hussain https://orcid.org/0000-0002-5772-7206
A. Al Sidairi https://orcid.org/0009-0008-5476-2621
A.M. Al-Sadi https://orcid.org/0000-0002-3419-8268
Data availability
All sequence data generated in this study (Table 1) are available in NCBI GenBank (https://www.ncbi.nlm.nih.gov/genbank/). The multigene dataset used for phylogenetic analyses is available at Figshare (https://doi.org/10.6084/m9.figshare.32259831).
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Associated Data
This section collects any data citations, data availability statements, or supplementary materials included in this article.
Supplementary Materials
Data Availability Statement
All sequence data generated in this study (Table 1) are available in NCBI GenBank (https://www.ncbi.nlm.nih.gov/genbank/). The multigene dataset used for phylogenetic analyses is available at Figshare (https://doi.org/10.6084/m9.figshare.32259831).




