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Bryopsida

Bryopsida, the true mosses, is the largest class of mosses within the division Bryophyta, encompassing approximately 12,000 species that account for about 95% of all moss diversity worldwide. These non-vascular plants are characterized by their gametophyte-dominant life cycle, where the leafy gametophyte alternates with a dependent sporophyte that produces spores for reproduction. Bryopsida mosses are ubiquitous in terrestrial ecosystems, from arctic tundras to tropical rainforests, and play key roles in ecosystem processes including water retention and providing microhabitats for small organisms. A defining feature of Bryopsida is the arthrodontous surrounding the spore capsule's mouth, consisting of 16 teeth formed from four layers of s that hygroscopically move to regulate spore release in response to environmental . Growth forms vary widely, including acrocarpous with upright stems and terminal sporangia, and pleurocarpous with prostrate, branching stems bearing lateral sporangia, allowing for dense mat formation. Leaves are typically simple, one thick, and arranged spirally or in two or three ranks, often with midribs and marginal features adapted to retention. Taxonomically, Bryopsida includes numerous families and genera, organized into various orders such as Bryales, Hypnales, and Orthotrichales, reflecting extensive evolutionary diversification. This class dominates due to adaptations like efficient water-dependent fertilization via flagellated and through gemmae in some species. Ecologically, Bryopsida species contribute to by providing microhabitats for and influencing in forests.

Taxonomy

Definition and Scope

Bryopsida represents the largest class within the mosses ( Bryophyta), encompassing approximately 95% of all moss , or around 12,000 distributed worldwide. These mosses are commonly referred to as "joint-toothed" or arthrodontous mosses, a name derived from the distinctive articulated structure of the teeth surrounding the capsule opening, which facilitates controlled release. The class includes a diverse array of forms, from small turf-forming to larger cushions and mats, adapted to a wide range of terrestrial habitats. Historically, Bryopsida was broadly defined to include all mosses under the traditional grouping Musci, but modern classifications have narrowed its scope based on molecular and morphological evidence. The 2000 revision by Goffinet et al. separated non-Bryopsida lineages into distinct classes, excluding Sphagnopsida (peat mosses), Andreaeopsida (lantern mosses), and others like Takakiopsida and Polytrichopsida, to reflect evolutionary divergences in reproductive and structural traits. This refinement highlights Bryopsida's monophyletic nature within the mosses, emphasizing shared innovations such as the . Bryopsida is distinguished from other classes by its dominant, leafy phase, which in some features specialized conducting tissues resembling hydroids for and leptoids for photosynthate movement, absent in most other classes. In contrast, Sphagnopsida, exemplified by , forms extensive peatlands with unique cells for water storage but lacks true conducting strands and has capsules elevated on a gametophyte-derived pseudopodium rather than a sporophyte . Similarly, Andreaeopsida like Andreaea exhibit scale-like leaves and capsules that split longitudinally without a , adapting them to rocky, exposed environments unlike the more versatile Bryopsida forms.

Classification

The class Bryopsida is divided into seven subclasses: Buxbaumiidae (1 family), Diphysciidae (1 family), Gigaspermidae (1 family), Funariidae (4 families), Timmiidae (1 family), Dicranidae (39 families), and Bryidae (71 families). This structure encompasses the majority of moss diversity, with Bryidae representing the largest group. Within these subclasses, key orders include Buxbaumiales in Buxbaumiidae, Diphysciales in Diphysciidae, Gigaspermales in Gigaspermidae, Funariales (along with Disceliales and Encalyptales) in Funariidae, Timmiales in Timmiidae, Dicranales (along with Grimmiales and Pottiales) in Dicranidae, and Bryales (along with Hypnales and Orthotrichales) in Bryidae. These orders reflect traditional groupings based on sporophyte and gametophyte features. Classification within Bryopsida relies primarily on characteristics, distinguishing haplolepidous types (a single ring of 16 teeth, typical in Dicranidae) from diplolepidous types (two rings with an outer exostome and inner endostome, seen in Bryidae and Funariidae). Additional criteria include , which ranges from erect (common in epiphytic species) to inclined, horizontal, or pendulous (adaptive to terrestrial habitats), and branching patterns, such as acrocarpous (upright with terminal gametangia and ) versus pleurocarpous (prostrate with lateral gametangia and monopodial branching). These traits, combined with the arthrodontous as a defining feature of the class, provide the foundation for delimiting taxa. Recent molecular phylogenetic studies have prompted revisions, such as the integration of Archidiaceae into Funariidae based on phylogenomic analyses showing nesting within this subclass, alongside related families like Micromitriaceae. These updates refine the by incorporating and data to resolve previously ambiguous placements.

Phylogenetic Relationships

Bryopsida constitutes the most diverse class within the phylum Bryophyta, encompassing over 95% of all species and forming the dominant monophyletic within Bryophytina, following the earlier-diverging moss classes such as Sphagnopsida and Andreaeopsida. Phylogenetic reconstructions based on genomes place Sphagnopsida as the basalmost class among mosses, followed by Andreaeopsida, with Bryopsida emerging as the dominant in Bryophytina. This positioning highlights Bryopsida's evolutionary success relative to the smaller, more specialized Sphagnopsida ( mosses) and Andreaeopsida ( mosses). Internally, Bryopsida exhibits a structured phylogeny marked by early divergences of non-arthrodontous subclasses. Molecular supports Buxbaumiidae as to the remaining Bryopsida, followed by a including Diphysciidae, with the core arthrodontous es—comprising Dicranidae and Bryidae—forming a robust monophyletic group characterized by complex structures. Seminal taxonomic syntheses, such as Novíkov and Barabaš-Krasni (2015), delineate these subclass relationships through integrated morphological and molecular data across orders. Recent phylogenomic analyses using hundreds of exons further refine this framework, resolving in groups like Dicranidae and establishing 10 new orders within Bryopsida. Molecular clock calibrations indicate that Bryopsida diversified during the Permian or (ca. 299–201 million years ago), aligning with the broader radiation of early land plants. evidence complements these estimates, with the earliest unequivocal remains—primarily spores—dating to the around 385 Ma, though definitive Bryopsida fossils, such as gametophytes and sporophytes, appear in the , suggesting cryptic Devonian origins for the class amid taphonomic biases favoring delicate bryophyte preservation.

Morphology

Gametophyte Structure

The of Bryopsida, the dominant and independent phase of the moss life cycle, typically exhibits a leafy consisting of erect or prostrate stems anchored by rhizoids. These gametophytes, known as gametophores, develop from protonemal filaments and form either upright structures in acrocarpous or sprawling, mat-forming habits in pleurocarpous . Rhizoids, which are multicellular and branched, arise from the base of stems or leaves and primarily serve for attachment to substrates, with limited roles in water and nutrient absorption. Leaves, or phyllids, are spirally arranged around the in more than three rows and are usually one to two s thick, lacking true or cuticles. A prominent , or midrib, composed of elongated, narrow s, extends along the length, providing and facilitating conduction in some . Specialized features such as alar s at the base, which are enlarged and for , and lamellae—vertical plates of chlorophyllose s on the in taxa like Leucobryum—enhance retention. In certain hygrophilous mosses, walls are thickened and porose, aiding in movement. Stem anatomy includes a central strand in many species, comprising hydroids—dead, thin-walled cells analogous to for transport—and surrounding leptoids, living cells with degenerate nuclei that function in photosynthate conduction similar to . Pleurocarpous mosses often bear paraphyllia, small leaf-like or filamentous outgrowths on the surface that increase surface area for retention and . patterns differ markedly: acrocarpous mosses exhibit sympodial , with branching occurring below the via lateral innovations, while pleurocarpous forms display monopodial , with continuous apical extension and lateral branches bearing reproductive structures.

Sporophyte Structure

The sporophyte of Bryopsida is a diploid, unbranched structure that remains attached to the maternal throughout its development, consisting of three main regions: the foot, the , and the capsule. The foot is the basal portion, embedded within the tissue, and features specialized transfer cells with convoluted walls that facilitate nutrient absorption from the to support sporophyte growth. The , a slender stalk-like region above the foot, elongates rapidly after fertilization through an intercalary , elevating the capsule to enhance dispersal; it is composed of cells, often with supportive stereids and conducting hydroids or leptoids, and may twist upon in some taxa. The capsule, or , is the terminal region where occurs to produce haploid s, typically developing within a protective covering and varying in shape from to elongate-cylindric. It includes a central , a sterile of parenchymatous cells extending from the to the , which provides and aids in spore maturation by suspending the spore sac. The capsule features an operculum, a lid-like structure that dehisces to expose the spore-releasing mouth, attached via an annulus—a ring of specialized cells that may be revoluble or otherwise differentiated to facilitate operculum separation. In Bryopsida, the capsule mouth is typically surrounded by an arthrodontous , consisting of 16 articulated teeth derived from the amphithecium, which hygroscopically respond to humidity changes to regulate release. Peristome morphology in Bryopsida exhibits variation that is taxonomically significant, primarily falling into two arthrodontous types: haplolepidous and diplolepidous. Haplolepidous s feature a single ring of 16 solid teeth (peristomial formula 0:2:3), lacking median lines, and are characteristic of subclasses like Dicranidae, where teeth may resemble nematodontous structures in rigidity but retain arthrodontous articulation. Diplolepidous s, prevalent in Bryidae, comprise a double ring with an outer exostome of 16 teeth and an inner endostome, often with segmented segments and cilia that interlock or alternate with the exostome to finely control dispersal under varying environmental conditions. Some Bryopsida, such as certain Bartramiaceae, lack peristome teeth entirely (ap peristomate), while others like Dawsonia exhibit elongate, bristle-like modifications. The developing capsule is enclosed by a calyptra, a cap of haploid gametophytic tissue derived from the archegonium wall, which protects the immature sporangium from desiccation and mechanical damage until maturation. In most Bryopsida, the calyptra is smooth or naked (mitrate or cucullate), splitting longitudinally to shed at capsule maturity, though it is hairy or fringed in Polytrichidae (e.g., Polytrichum), enhancing protection in exposed habitats. The calyptra's separation often reveals the operculum, marking the onset of spore dispersal readiness.

Morphological Groups

Bryopsida, the true mosses, exhibit diverse growth forms primarily categorized into three morphological groups based on the position of perichaetia on the : acrocarps, pleurocarps, and cladocarps. These groups reflect adaptations in shoot architecture and branching patterns that influence occupancy and reproductive strategies. Acrocarps are characterized by erect or ascending shoot systems that are unbranched or sparingly branched, with perichaetia and subsequent sporophytes developing at the apex of the main axis, thereby terminating its growth. This sympodial growth pattern allows for subfloral innovations to continue shoot elongation. A representative example is , which forms dense cushions or turfs. Acrocarps predominate in open, dry, and xeric s, such as sunny rock outcrops or disturbed soils, where their upright habit facilitates dispersal in exposed conditions. In contrast, pleurocarps feature prostrate or creeping primary stems with extensive lateral branching, where perichaetia arise on short, specialized lateral branches, resulting in sporophytes that appear scattered along the main axis. This enables the formation of dense mats or wefts. Hypnum serves as a typical example, often creating interwoven carpets. Pleurocarps are most abundant in shaded, moist environments, such as forest floors or humid rock crevices, benefiting from their low profile and branching for water retention and colonization. Cladocarps represent an intermediate form, producing perichaetia at the tips of unspecialized vegetative lateral branches that remain capable of further elongation and branching, without the terminal restriction of acrocarps or the specialization of pleurocarps. This heteroblastic development allows for flexible shoot architectures. Certain in the Orthotrichaceae, such as Orthotrichum kellmanii, exemplify cladocarps, forming cushions with differentiated stem and branch leaves. Phylogenetically, the acrocarpous condition is plesiomorphic among Bryopsida, representing the ancestral state, while pleurocarps form a monophyletic nested within the paraphyletic acrocarps, indicating multiple evolutionary shifts toward pleurocarpy. Cladocarpy has arisen independently in several lineages, bridging the two major groups through transitional branching habits. These morphological variations in branching underscore adaptive radiations in diverse ecological niches.

Reproduction and Life Cycle

Sexual Reproduction

Sexual reproduction in Bryopsida, the true mosses, occurs through an , with the dominant haploid phase producing gametes via . Male gametes, or , are generated in multicellular antheridia, while female gametes, or eggs, are produced in archegonia, both structures developing on the body. Bryopsida exhibit either dioicous (separate male and female gametophytes) or monoicous (bisexual gametophytes on the same ) sexual systems, with approximately 60% of moss being dioicous. Antheridia and archegonia are often organized into specialized clusters known as perigonia and perichaetia, respectively, which facilitate production and accessibility. Perigonia, containing multiple antheridia, typically form at the tips of stems or short lateral branches, while perichaetia, housing archegonia, are positioned at the apices in acrocarpous mosses or on lateral branches in pleurocarpous forms. These clusters enhance the efficiency of gamete dispersal within the colony. Fertilization requires external and involves the release of biflagellate from mature antheridia, which swim through a thin film of to reach the within the archegonium's venter. The releases chemical attractants, such as sugars, to guide the motile down its neck canal, where fusion with the produces a diploid . The then develops into a multicellular , which remains attached to and nutritionally dependent on the parental . This process is highly dependent on environmental conditions, particularly , as and dispersal rely on rain or forming continuous films; dry conditions prevent fertilization entirely. In many species, is seasonal, triggered by periods of increased rainfall that promote antheridial and archegonial maturation, often spanning weeks in temperate regions. Arthropods, such as springtails and mites, can occasionally aid sperm transport over short distances up to 2 meters.

Asexual Reproduction

Asexual reproduction in Bryopsida primarily occurs through vegetative propagation, allowing these mosses to themselves without fusion or . One common mechanism involves the production of gemmae, which are multicellular, undifferentiated buds formed in specialized structures called gemmifers located on leaves, stems, or apices. These gemmae detach and develop into new gametophytes upon landing in suitable moist environments, facilitating local dispersal and establishment. For instance, in genera like Physcomitrium within the Funariaceae family, gemmifers produce gemmae that enable rapid clonal expansion in disturbed or ephemeral habitats. Fragmentation represents another widespread form of in Bryopsida, particularly prevalent among pleurocarpous mosses where horizontal branching promotes the detachment of branches, leaves, or stem segments. These fragments can regenerate into independent plants when conditions are favorable, such as in humid, shaded forest floors or aquatic settings. Species like Pohlia nutans exemplify this strategy, with detachable catkin-like branches that break off and root to form new colonies, enhancing persistence in stable but fragmented microhabitats. This method is especially effective in pleurocarps due to their sprawling growth habit, which inherently facilitates breakage and regrowth. Apomixis, the production of a without fertilization, is rare in Bryopsida and typically results in clonal spores that develop into genetically identical . This process bypasses , maintaining diploidy in some cases, but it occurs infrequently in natural populations and is more commonly studied in model species like Physcomitrium patens through genetic modifications that induce diploid formation. While not a dominant reproductive mode, contributes to genetic uniformity in isolated clones. These strategies provide adaptive advantages by enabling rapid colonization of unstable or water-limited habitats, where sexual reproduction's reliance on motile is impractical. Vegetative and fragmentation allow Bryopsida to exploit short-lived opportunities for growth, outpacing sexual cycles and ensuring survival in dynamic environments like floodplains or rock surfaces without the need for synchronous mating.

Developmental Stages

The life cycle of Bryopsida exhibits , with the haploid serving as the dominant, photosynthetic phase and the diploid being nutritionally dependent on it. This cycle begins with the of haploid s, which occurs under moist conditions and , producing a multicellular, filamentous that superficially resembles . The develops from the through apical , initially forming chloronema—filaments rich in chloroplasts with transverse cell walls that promote lateral expansion—and later transitioning to caulonema, which have fewer chloroplasts, oblique , and faster longitudinal growth for efficient exploration of substrates. From the , buds emerge under environmental cues such as nutrient availability and light intensity, differentiating into upright gametophores that mature into the characteristic leafy . This maturation phase involves the elongation of stems (axes) and the formation of phyllids (leaves) arranged spirally or in two or three ranks, with rhizoids at the base facilitating anchorage and nutrient absorption from the substrate via diffusion and . The remains the primary life form, capable of indefinite growth through apical meristems, and serves as the site for production, though the arises directly from it post-fertilization. Nutrient translocation within the occurs acropetally, from older basal segments to younger apical regions, supporting sustained and . Sporophyte development initiates from the diploid embedded in the atop the , forming an that differentiates into a foot (for nutrient uptake from the gametophyte), a (elongating stalk), and a capsule (). The foot anchors into gametophyte tissue and features transfer cells that facilitate the unidirectional flow of sugars, , and minerals from the gametophyte via symplastic and apoplastic pathways. As the seta elongates—often rapidly under hormonal —the capsule matures, developing a for structural support and, in many species, a (a ring of teeth-like structures) around the mouth for controlled release through hygroscopic movements. within the capsule produces haploid spores, which accumulate until dehiscence. Upon maturation, the capsule dehisces irregularly or via mechanisms, releasing s that are dispersed by wind or ; these s then germinate under moist conditions to form new ta, completing the cycle. The 's role in gradual spore dispersal enhances dispersal efficiency while protecting against premature release in dry conditions. While cycle duration varies by species and environment, the transition from to mature can occur within weeks, with development spanning months, allowing perennial populations to persist through repeated cycles.

Distribution and Ecology

Global Distribution

Bryopsida, the largest class of mosses, exhibit a nearly ubiquitous global distribution, occurring on every continent, including extreme environments such as . In , species like Sanionia uncinata are prominent in ice-free coastal regions of Maritime , including the and the western , where they form dense mats in valleys and on beaches. This cosmopolitan presence underscores their adaptability to diverse climates, from polar to tropical zones. The class comprises approximately 11,500 across roughly 600 genera, accounting for over 95% of all moss diversity. Within Bryopsida, the subclass Bryidae is particularly widespread, encompassing the majority of genera and dominating in various ecosystems worldwide due to its versatile sporophytic features. High levels of endemism are notable in isolated regions, such as , where about 108 of the roughly 500 moss species are unique to the , reflecting historical and events. Biogeographic patterns in Bryopsida reveal a strong Holarctic influence in temperate zones of the , where many species originated and subsequently dispersed southward across equatorial barriers. In contrast, southern hemispheric distributions often include Gondwanan relics, such as certain lineages in the region that later colonized , , and through long-distance dispersal. species, like Sanionia uncinata, exemplify these dynamics, with most showing Holarctic ancestry and trans-equatorial migration to the south. Diversity patterns indicate that Bryopsida richness peaks in tropical montane regions, particularly in the , where montane forests host exceptional species accumulation due to topographic heterogeneity and climatic stability. Molecular analyses further suggest overall higher phylogenetic diversity in the compared to the Northern, with temperate and boreal forests supporting a substantial portion of global species through their moist, shaded understories. These correlations highlight the role of historical climate gradients in shaping current distributions.

Habitat Preferences

Bryopsida, commonly known as true mosses, exhibit a strong preference for humid and shaded environments that provide consistent moisture, as their poikilohydric nature allows them to absorb directly from the atmosphere and substrates. Acrocarpous species, which grow upright in tufts, often occupy more exposed sites where they can tolerate periodic due to enhanced dehydration resistance, while pleurocarpous species, forming prostrate mats, favor sheltered forest understories with higher and reduced . This moisture dependency is evident in their role as indicators of microclimatic conditions, thriving in areas with frequent precipitation or but capable of surviving dry spells through physiological adaptations like rapid water loss and revival upon rehydration. These mosses demonstrate remarkable versatility in substrate utilization, colonizing a wide array of surfaces including , rocks, , and other as epiphytes, which enables them to exploit diverse microhabitats from terrestrial to semi- settings. For instance, many species anchor to rocky outcrops or logs in shaded ravines, stabilizing substrates and facilitating soil development, while epiphytic forms drape over in humid canopies. Some genera, such as Fontinalis, are fully , attaching to submerged rocks or logs in streams and lakes where they remain immersed for extended periods, highlighting their adaptation to permanently wet conditions. Bryopsida occupy an extensive altitudinal gradient, ranging from coastal zones to high elevations above 3,000 meters, where their tolerance via poikilohydry permits survival in fluctuating regimes across elevational climates. In lower elevations, they benefit from warmer, moister conditions, whereas in habitats, species endure harsher winds and lower temperatures by forming compact cushions that minimize water loss. Regarding soil preferences, Bryopsida generally favor neutral to acidic substrates ( 4–7), with many showing optimal growth in mildly acidic conditions that reflect low availability and minimal disturbance. Their sensitivity to shifts makes them effective bioindicators of , as changes in community composition can signal alterations in acidity, enrichment, or levels from and atmospheric deposition. For example, acid-tolerant dominate in oligotrophic, low- soils, while declines in diversity often correlate with or .

Ecological Roles

Bryopsida, commonly known as mosses, play a crucial role in within various ecosystems. Their dense mats bind particles, preventing from and , particularly in exposed or disturbed areas such as riverbanks and slopes. As , they colonize bare substrates early in , facilitating the establishment of later-successional plants by improving and nutrient availability. Through , Bryopsida contribute to nutrient cycling by releasing essential elements like , , and carbon back into the , enhancing fertility in nutrient-poor environments. These mosses also provide microhabitats that support . Their cushion-like or turf-forming growth habits offer shelter and breeding sites for small , such as mites and springtails, which in turn serve as prey for larger organisms. In some forest ecosystems, Bryopsida biomass contributes significantly to , storing substantial amounts of atmospheric CO₂ in peatlands and temperate rainforests. Additionally, their moisture-retention properties create humid refugia that briefly complement habitat preferences in drier settings. Bryopsida serve as effective indicator species for environmental quality, particularly . Due to their lack of cuticles and , they readily absorb like lead and from the atmosphere, making them sensitive bioindicators of contamination levels. They are widely used in programs to assess atmospheric deposition and track trends in urban and industrial areas. In terms of symbioses, many Bryopsida form associations with nitrogen-fixing , especially in forests, where these partnerships supply up to 50% of ecosystem inputs through atmospheric fixation. Some also exhibit mycorrhizal-like links with fungi, such as arbuscular mycorrhizal fungi, which enhance nutrient uptake in nutrient-limited soils.

Evolutionary and Human Significance

Evolutionary History

The Bryopsida, representing the largest class of mosses, trace their origins to the Ordovician-Silurian transition approximately 450 million years ago, evolving from charophyte green algae as part of the broader bryophyte lineage that colonized terrestrial environments. This emergence marked a pivotal step in land plant evolution, with Bryopsida developing key innovations such as the articulated (arthrodontous) peristome—a structure of cell-walled teeth surrounding the spore capsule that enables hygroscopic movements for precise spore release and dispersal. Fossil evidence for Bryopsida is sparse in the early record due to their delicate structure, but molecular clock estimates place the crown group origin around 420 million years ago in the late Silurian to early Devonian, with the first unequivocal fossils appearing in the Carboniferous period (~330–350 million years ago), including forms resembling modern Polytrichales through tubular microfossils and gametophyte impressions. During the Mesozoic era, Bryopsida underwent significant diversification following the breakup of the supercontinent Pangaea around 200 million years ago, which facilitated geographic isolation and adaptation to varied habitats. A major evolutionary milestone was the origin of the pleurocarpous growth form—characterized by lateral production along creeping stems—estimated at 194–161 million years ago in the , enhancing vegetative propagation and colonization efficiency in shaded, moist understories. This radiation intensified in the (~145–66 million years ago), coinciding with the rise of angiosperms, which altered forest structures and microhabitats; Bryopsida responded by shifting lineage compositions, with increased diversification in epiphytic and forest-floor niches, though overall rates remained lower than those of ferns. Advanced lineages further evolved the diplolepidous , featuring a double-layered structure with opposing or alternating teeth for finer dispersal control, prominent in groups like the Bryidae. The modern diversity of Bryopsida was profoundly shaped by glaciations (2.58 million years ago to present), which drove range contractions, refugial survival in unglaciated areas, and post-glacial recolonization, leading to current patterns of and genetic structuring particularly in northern hemispheres. records from this period document continuity in lineages like pleurocarps, underscoring resilience amid climatic oscillations.

Uses and Conservation

Bryopsida mosses have been utilized traditionally in and . Species such as serve as additives and stabilizers in cultivation due to their moisture retention properties, while in folk practices, ash mixed with fat and is applied as an ointment for cuts and burns. Medicinally, various Bryopsida taxa exhibit and wound-healing effects; for instance, extracts from demonstrate antibacterial activity, and traditional uses by Native North Americans and in Chinese include treatments for infections and skin ailments. In modern applications, Bryopsida mosses function as bioindicators for and policy-making. Their ability to accumulate and pollutants without roots makes them effective for assessing air quality and contamination levels, as seen in urban and industrial studies where species like reflect atmospheric pollution. Research on leverages model species such as , which exhibits tolerance mechanisms that inform agricultural and ecological adaptations to water stress. Additionally, non-peat Bryopsida mosses are explored as sustainable alternatives in for conditioning and , reducing reliance on peat. Bryopsida face significant threats from habitat loss due to and , which degrade and environments essential for their survival. Climate change exacerbates these issues by drying wetlands through increased droughts and temperature extremes, affecting water-dependent . Invasive alien further compete with native Bryopsida, impacting 161 European bryophyte taxa, including 79 threatened ones, by altering habitats and resource availability. Conservation efforts emphasize protected areas and targeted interventions, with 88.2% of European Bryopsida species occurring in such sites. The assesses approximately 22.5% of European mosses (283 out of 1,327 species) as threatened, highlighting the need for habitat restoration in bogs and forests. Ex situ propagation techniques, including and spore banking, support recovery programs for rare taxa like Podperaea krylovii, enabling reintroduction and genetic preservation.

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