Reproduction and Dispersal of Biological Soil Crust Organisms

Warren, Steven D.; Clair, Larry L.; Stark, Lloyd R.; Lewis, Louise A.; Pombubpa, Nuttapon; Kurbessoian, Tania; Stajich, Jason E.; Aanderud, Zachary T.

doi:10.3389/fevo.2019.00344

REVIEW article

Front. Ecol. Evol., 04 October 2019

Sec. Biogeography and Macroecology

Volume 7 - 2019 | https://doi.org/10.3389/fevo.2019.00344

This article is part of the Research Topic Ecological Development and Functioning of Biological Soil Crusts After Natural and Human Disturbances View all 16 articles

Reproduction and Dispersal of Biological Soil Crust Organisms

$\nSteven D. Warren$ Steven D. Warren¹^*

Larry L. St. Clair^2,3

¹U.S. Forest Service, Rocky Mountain Research Station, Provo, UT, United States
²Department of Biology, Brigham Young University, Provo, UT, United States
³Monte Lafayette Bean Life Science Museum, Brigham Young University, Provo, UT, United States
⁴School of Life Sciences, University of Nevada, Las Vegas, NV, United States
⁵Department of Ecology and Evolutionary Biology, University of Connecticut, Storrs, CT, United States
⁶Department of Microbiology and Plant Pathology, Institute for Integrative Genome Biology, University of California, Riverside, Riverside, CA, United States
⁷Department of Plant and Wildlife Sciences, Brigham Young University, Provo, UT, United States

Biological soil crusts (BSCs) consist of a diverse and highly integrated community of organisms that effectively colonize and collectively stabilize soil surfaces. BSCs vary in terms of soil chemistry and texture as well as the environmental parameters that combine to support unique combinations of organisms—including cyanobacteria dominated, lichen-dominated, and bryophyte-dominated crusts. The list of organismal groups that make up BSC communities in various and unique combinations include—free living, lichenized, and mycorrhizal fungi, chemoheterotrophic bacteria, cyanobacteria, diazotrophic bacteria and archaea, eukaryotic algae, and bryophytes. The various BSC organismal groups demonstrate several common characteristics including—desiccation and extreme temperature tolerance, production of various soil binding chemistries, a near exclusive dependency on asexual reproduction, a pattern of aerial dispersal over impressive distances, and a universal vulnerability to a wide range of human-related perturbations. With this publication, we provide literature-based insights as to how each organismal group contributes to the formation and maintenance of the structural and functional attributes of BSCs, how they reproduce, and how they are dispersed. We also emphasize the importance of effective application of molecular and microenvironment sampling and assessment tools in order to provide cogent and essential answers that will allow scientists and land managers to better understand and manage the biodiversity and functional relationships of soil crust communities.

Biological soil crusts (BSCs) consist of various combinations of living organisms that colonize, organize, and stabilize soil surfaces against the erosive forces of wind and water. Many BSC organisms are photoautotrophic, fixing, and accumulating organic carbon (Green and Proctor, 2016) while other organismal groups fix and distribute organic nitrogen. Groups of organisms known to contribute to the formation BSC communities include cyano-, chemoheterotrophic, and diazotrophic bacteria, free-living, lichenized, and mycorrhizal fungi, terrestrial algae (including diatoms), and bryophytes (Belnap et al., 2001; Weber et al., 2016). To be recognized as a contributor to the formation and maintenance of BSC communities, an organism must be involved in the consolidation and stabilization of soil particles and aggregates, resulting in the formation of an intact BSC community. In this review of BSC organisms, we evaluate each organismal group independently, documenting how they contribute to the formation of BSCs, and how they reproduce and disperse.

Bacteria

Prokaryotic bacteria commonly found in BSC communities include cyanobacteria, chemoheterotrophic bacteria, and free-living diazotrophic (nitrogen fixing) bacteria.

Cyanobacteria

Cyanobacteria are photoautotrophic prokaryotes (Whitton and Potts, 2000). Traditionally, cyanobacteria were classified with the eukaryotic “algae” based on the presence of chlorophyll a and the production of molecular oxygen. However, given the absence of membrane bound subcellular structures (e.g., nuclei, mitochondria, etc.) and the occurrence of prokaryotic type ribosomes, the cyanobacteria are now classified as bacteria. Cyanobacteria also produce a unique cell wall chemistry containing peptidoglycans rather than cellulose. Thallus-types range from unicellular to multicellular filaments, sheets, or globular thalli (Schirrmeister et al., 2011; Herrero et al., 2016). Numerous genera of BSC cyanobacteria have been reported—spanning five orders, Chroococcales, Nostocales, Oscillatoriales, Pleurocapsales, and Synechococcales. Cyanobacteria are recognized as one of the most important and abundant photoautotrophs in many arid land BSC communities (Colesie et al., 2016)—occurring at or just below the soil surface (Hu et al., 2003). Through photosynthesis, cyanobacteria contribute significant fixed carbon to the BSC community. Many species, including many of the filamentous and globular forms, also produce heterocysts, specialized nitrogen fixing structures (Fay, 1992; Bergman et al., 1997; Kumar et al., 2010). Nitrogen fixing cyanobacteria, both as free living and symbiotic forms, also contribute organic nitrogen to the general soil crust community (Bergman et al., 1997). Filamentous species such as Microcoleus are capable of binding together into rope-like structures that allows them to colonize physically unstable sedimentary environments (Garcia-Pichel and Wojciechowski, 2009). Some filamentous species also secrete exopolysaccharides that effectively aggregate soil particles and thus contribute to BSC structure and stability (Rossi and De Philippis, 2015). Terrestrial cyanobacteria are poikilohydric—tolerating severe desiccation as well as high levels of UV light (Karsten and Holzinger, 2014). The UV filtering capacity of terrestrial cyanobacteria is related to the presence of light screening compounds found in their cells and sheath material, often resulting in the characteristic dark color typical of many cyanobacteria-dominated BSC communities (Scherer et al., 1988; Rosentreter et al., 2007; Rastogi and Incharoensakdi, 2014). During winter months, the authors have anecdotally observed that the dark surface of BSC communities in the Great Basin tends to absorb winter sunlight, causing snow and ice to melt providing the BSC community with liquid water that in turn potentially supports brief but important periods of metabolic activity.

Reproduction in the cyanobacteria is strictly asexual (Mur et al., 1999) and may be accomplished by budding (Waterbury and Stanier, 1977), non-specialized thallus fragments (Meeks and Elhai, 2002), binary fission (Kunkel, 1984), or the formation of specialized asexual structures (Somon, 1977) including akinetes (Kaplan-Levy et al., 2010). Hormogonia—specialized thallus fragments commonly produced by some filamentous cyanobacteria (Campbell and Meeks, 1989; Meeks and Elhai, 2002) also function as effective asexual propagules. Cyanobacteria act as pioneer species while also commonly occurring in more mature BSC communities as both free living and symbiotic taxa.

Cyanobacteria have been found in BSC communities on all continents, and upwards of 50 taxa have been identified from regional samples of BSC communities (Rippin et al., 2018). Many terrestrial cyanobacteria have also been collected from the atmosphere (Sharma and Singh, 2010; Genitsaris et al., 2011) and are among the most numerous airborne microorganisms reported from aerial samples (Sharma and Singh, 2010; Després et al., 2012). In terrestrial environments, filamentous cyanobacteria are able to glide along thin layers of water coating soil particles when the soil is moist (Castenholz, 1982; Hoiczyk, 2000). However, in terrestrial environments, local dispersal distances are extremely limited (cm scale) compared to dispersal through the air (km or intercontinental scale). In Antarctica, cyanobacterial communities in close proximity to each other had a low degree of similarity with each other, indicating the probability of longer-distance aerial transport (Namsaraev et al., 2010).

Chemoheterotrophic Bacteria and Free-Living Diazotrophic Bacteria

Chemoheterotrophic bacteria and free-living diazotrophic bacteria commonly integrate and closely interact with other BSC organismal groups. They are, however, one of the least studied and understood constituents of BSCs. These bacteria reside in a nutrient-rich zone where cyanobacteria and other biocrust constituents create a “cyanosphere” (Couradeau et al., 2019) with relatively enhanced organic carbon, nitrogen, and water availability. Large numbers of soil heterotrophic bacteria are positively correlated with BSC stability (Andrade et al., 1998; Makhalanyane et al., 2015; Nunes da Rocha et al., 2015). Many heterotrophic bacteria are filamentous and/or produce exopolysaccharides (Crania et al., 2019), characteristics that contribute to the formation and stabilization of BSCs. The occurrence of these BSC bacteria are ultimately a product of multiple environmental filters (e.g., climate, soil type, and disturbance regimes Eldridge and Delgado-Baquerizo, 2019. Each crust type (cyanobacteria dominated, lichen-dominated, and bryophyte-dominated) exerts control over the bacterial phyla and families present (Maier et al., 2018). To begin to identify the higher-taxonomical convergence among BSC bacteria, other than cyanobacteria, we examined the patterns of abundant bacterial families in the three crust types (Table 1). Of the 24 dominant heterotrophic bacterial orders/families found to occur in BSC communities over eleven studies, nine were cosmopolitan taxa [i.e., present in all three biocrust types, Acidobacteriaceae (Acidobacteria), Rubrobacteraceae (Actinobacteria), Shingomonadaceae (Alphaproteobacteria), Bradyrhizobiaceae (Alphaproteobacteria), Rhodobacterales (Alphaproteobacteria) Chitinophagaceae (Bacteroidetes), Cytophagaceae (Bacteroidetes), Oxalobacteraceae (Betaproteobacteria), Chthoniobacteraceae (Verrucomicrobia)], while five were unique to either cyanobacteria-dominated [i.e., Solirubrobacterales (Actinobacteria), Burkholderiales (Betaproteobacteria), Trueperaceae (Deinicoccus-Thermus) or lichen-dominated crusts [i.e., Armatiomonadaceae (Armatimonadetes), Cystobacteraceae (Deltaproteobacteria)]. The Alphaproteobacteria contained the greatest number of families at five, followed by the Actinobacteria that housed four families or orders. The most commonly found taxon in cyanobacteria-dominated crusts was the Rubrobacteraceae (Actinobacteria), and Shingomonadaceae (Alphaproteobacteria) in lichen- and moss-dominated crusts. These patterns may serve as a starting point for a conversation to find novel community patterns among biocrust copiotrophs. In all BSCs, regardless of the type, heterotrophic bacteria exert significant influence over soil biogeochemistry and structure by regulating carbon and nitrogen cycling (Schimel and Schaeffer, 2012; Nelson et al., 2016). In addition, the production of exopolymeric compounds by many heterotrophic bacteria contributes to soil aggregation that has a direct influence on water infiltration and soil structure (Costa et al., 2018). The presence of free-living diazotrophs (N-fixing bacteria and archaea) within the cyanosphere (Couradeau et al., 2019) adds essential available nitrogen to predominantly nitrogen-limited desert soils. In Microcoleus vaginatus-dominated crusts, Couradeau et al. (2019) identified multiple heterotrophic diazotrophs associated with several taxa from the Alphaproteobacteria, Betaproteobacteria, and Gammaproteobacteria groups. Furthermore, in developing cyanobacteria-dominated BSCs several of the same diazotrophs were identified by Pepe-Ranney et al. (2016) using 15N-DNA SIP methods.

TABLE 1

Table 1. Abundant chemoheterotrophic bacterial families/orders in cyanobacteria-dominated, lichen-dominated, and/or bryophyte-dominated biocrusts based on eleven studies.

Biological soil crust bacteria, like other soil bacteria, reproduce rapidly by binary fission when conditions are favorable. Otherwise, they enter a reversible state of reduced metabolic activity or dormancy. Dormancy establishes reservoirs of inactive individuals that resume metabolic and reproductive activity when appropriate environmental conditions return (Lennon and Jones, 2011; Joergensen and Wichern, 2018). Potentially, as much as 90% of the BSC microbial community is inactive with more than 50% of all bacterial taxa dormant during periods of stress (Alvarez et al., 1998; Lennon and Jones, 2011; Aanderud et al., 2015). Invariably, the single most limiting resource contributing to the onset of dormancy in the BSC community is soil moisture. For example, using H218O RNA-stable isotope probes in a cyanobacteria-dominated BSC community in Israel's Negev Desert, the rewetting of dry crusts caused bacteria to grow, resulting in the development of a distinctly different bacterial community with the previously dominant Actinobacteria population significantly reduced (Angel and Conrad, 2013). BSCs host a diverse bacterial community whose members grow, interact, and alter community composition depending on environmental conditions and activities that may impact BSC structure and health.

The primary dispersal mechanism for heterotrophic bacteria and diazotrophs within the BSC community is bioaerosols. Although BSCs generally stabilize desert soils against wind erosion, dust entrainment is the primary pathway for the movement of BSC bacteria from arid and semi-arid BSC communities. The various biological components of BSCs differ in their contributions and role in reducing soil erosion (Belnap and Gardner, 1993; Mazor et al., 1996; Bowker et al., 2008; Tisdall et al., 2012). Notwithstanding all the erosion benefits provided by BSCs, deserts remain a primary source of dust globally with desert winds aerosolizing several billion tons of soil-derived dust each year (Kellogg and Griffin, 2006). Local dispersal of bacteria occurs through the soil matrix but is extremely limited (at a cm scale) compared to dispersal through the air (intercontinental, at a km scale) (Choudoir et al., 2018). Dust from deserts may travel across continents providing an opportunity for BSC organismal groups to disperse across long distances. For example, dusty snow on Mont Blanc in the alps on the French and Italian border contained soil bacteria deposited by four Saharan desert dust storms over a 3-year period (Chuvochina et al., 2011). Similarly, dust from deserts in Chad were deposited in the Cape Verde Islands with many of the dust-borne bacterial families identical to families commonly reported for BSC communities (Favet et al., 2013). Dust contains an immense diversity of bacteria (Choudoir et al., 2018; Dastrup et al., 2018) and retains much of the diversity profile typical of soil surfaces (Boose et al., 2016; Weil et al., 2017; Dastrup et al., 2018). Dust also acts as a source of wind-borne propagules with dust particles settling in response to gravity or acting as ice nucleators enhancing snowfall (Christner et al., 2008). Dust entrainment from deserts is also enhanced by anthropogenic disturbance of soil surfaces (Belnap and Gillette, 1998). Disturbed BSC communities have been shown to serve as a source of inoculants (Warren et al., 2019), further enhancing dispersal bridges between crust communities or into open habitats—suitable for biocrust development.

Fungi

Three categories of fungi are reported for BSC communities including free-living fungi, lichenized fungi, and mycorrhizal fungi. All three groups of terrestrial fungi play important ecological roles in the establishment and maintenance of BSC communities.

Free-Living Fungi

Free-living fungi are eukaryotic heterotrophs that acquire energy and matter from other organisms (living or dead). They produce a wide range of enzymes that degrade chitin, keratin, cellulose, and lignin (Alexopoulos et al., 1996; Kendrick, 2017), substrates that are not readily degraded by other organisms. Fungi have the unique ability to digest/consume organic substrates while also releasing compounds that are often appropriated by other organisms. Moreover, fungi are also able to survive extreme environments such as temperature extremes, desiccation, pH extremes, etc. (Kendrick, 2017). Fungi in general are recognized for their role as decomposers, and their ability to withstand environmental extremes. They are now often included in the suite of microorganisms that comprise BSCs, primarily because of their contributions to the process of consolidating and stabilizing soil particles and aggregates (Caesar-TonThat and Cochran, 2001; States et al., 2001). Free-living fungi are found in greater abundance in well-developed BSCs than uncrusted neighboring soils (Maier et al., 2016). Although free-living fungi have been recognized as an important component of the BSC micro-community, research on free-living fungal communities in biocrusts has been limited and generally descriptive in nature (Bates and Garcia-Pichel, 2009; Bates et al., 2012; Steven et al., 2015). Ascomycota represents the predominant fungal phylum in BSCs (Maier et al., 2016). However, research has shown that the composition of BSC fungal communities differs based on soil types and geographical location (Reininger et al., 2015). In general, fungi produce vegetative filaments (hyphae) which bind soil particles together and help to consolidate the surface of BSC communities (Tisdall, 1991; Degens et al., 1996). More specifically, many of the major BSC free-living fungi in the Ascomycota are classified in the Dothideomycetes class of the Pleosporales order. Members of this group of fungi are called dark-septate endophytic fungi, due to the dark pigments commonly found in their cell walls. These pigments are usually melanin and mycosporine-like amino acids which provide protection in environments of severe desiccation and high levels of UV light (Oren and Gunde-Cimerman, 2007; Gostinčar et al., 2009). There are two types of melanin produced by melanized fungi: 1,8-DHN melanin and L-Dopa melanin (Henson et al., 1999). Dark-septate fungi have also been suggested as contributors to nutrient links between desert vascular plants and the BSC community (Maier et al., 2016). As a result, free-living fungi have been proposed as an important component in the fungal loop hypothesis that suggests that nutrient exchange and the vascular plant-BSC connection may be mediated by fungi (Collins et al., 2008; Green et al., 2008).

While almost all free-living fungi are capable of sexual reproduction, sex is costly (Aanen and Hoekstra, 2007), and most fungi generally reproduce using a variety of asexual mechanisms (Nieuwenhuis and James, 2016; Ojeda-López et al., 2018). Asexual reproduction may be accomplished by fission or budding of somatic cells, fragmentation of mycelial strands or hyphae, or production of asexual spores. All such processes result in haploid individuals. Because sexual reproduction is possible yet infrequent, outcrossing is, likewise, rare to infrequent (Nieuwenhuis and James, 2016; Ojeda-López et al., 2018). Indeed, sexual reproduction is infrequent in many fungi, yet self-fertility is relatively common (Lee et al., 2010). In BSCs, free-living fungi are generally classified based on their asexual reproductive structures and confirmed more specifically by limited observations of sexual fruiting bodies (Maier et al., 2016). BSCs are dominated by Dothideomycetes fungi (Steven et al., 2015) which are most often found in their anamorph (asexual) state and are recognized as filamentous molds when cultured in the laboratory. They reproduce asexually by producing non-motile conidia type spores that can be dispersed by wind or insects. Black yeasts are a second common morphotype encountered when culturing fungi from BSCs and encompasses two distinct fungal evolutionary lineages, Dothideomycetes and Chaetothyriales (Eurotiomycetes). The black yeasts are characterized by thick, melanized cell walls, and exopolysaccharide production that support a variety of extremophile properties that allow them to endure high UV radiation and extreme desiccation, while also contributing to the consolidation of soil particles. The black yeasts have only been documented to reproduce asexually through the production of conidia type spores and unicellular budding. Some species of black yeasts produce fission or budding divisions when grown in submerged environments while others are capable of producing conidiophores when growing in low moisture environments (Seyedmousavi et al., 2014).

Some free-living fungi produce specialized structures that forcibly eject thousands of spores into the air (Roper et al., 2010; https://www.anbg.gov.au/fungi/dispersal.html). Ascomycota are the dominant group of fungi in BSCs, and are also the dominant fungi found in aerobiota (Frölich-Nowoisky et al., 2016). Generally, fungal species, which rely on windblown dispersal, produce aerodynamically shaped spores that can be transported thousands of kilometers through the atmosphere (Golan and Pringle, 2017). Abundant and diverse numbers of fungal spores have been collected from the atmosphere above Antarctica (Marshall, 1997), Australia (Mitakakis and Guest, 2001), Brazil (Womack et al., 2015), Chile (Ibañez et al., 2001), China (Fang et al., 2005), India (Priyamvada et al., 2017), Iran (Shams-Ghahfarokhi et al., 2014), Italy (Sandrone, 2014), Kuwait (Halwagy, 1994), Mexico (Rosas et al., 1990), Nigeria (Ezike et al., 2016), Poland (Stȩpalska and Wolek, 2005), Spain (Sabariego et al., 2007), and the United States (Dupont et al., 1967), among others. The quantity and diversity of airborne fungal spores is seasonally variable (Reineria Diaz et al., 1998; Kasprzyk and Worek, 2006). Their function is dispersal followed by growth and development of vegetative structures when essential resources and ideal environmental conditions are available (Kendrick, 2017). Due to the arbitrary nature of wind dispersal, spores may not encounter conditions suitable for germination and viability. To increase their chances of reproductive success, many fungi produce and release an “over-abundance” of spores throughout the year to ensure that a sustainable number encounter a suitable environment with essential resources to accommodate germination and establishment (Kendrick, 2017). The regional production of spores is dependent on the availability of water and local spore trapping show a cyclical pattern dependent on moisture patterns. Global dispersal of fungal spores is facilitated by dust-borne transport that in turn supports proliferation processes (Shinn et al., 2003).

Lichenized Fungi

Lichenized fungi include more than 19,000 species (Lücking et al., 2016, 2017). Lichens are composite systems involving complicated symbiotic interactions between heterotrophic fungi primarily of the phylum Ascomycota or less frequently of the phylum Basidiomycota, and a green alga and/or a cyanobacterium (Brodo et al., 2001). The fungus, or mycobiont, provides structure and a favorable living environment in the form of a thallus or vegetative plant-like body undifferentiated into true stems, roots, and leaves, and lacking a vascular system. The green alga and/or cyanobacterium photobionts provide a carbon-based food source for themselves and the mycobiont through photosynthesis. In those cases where the photobiont is a cyanobacterium, it also fixes atmospheric nitrogen. Lichen scientific names are based strictly on the fungal symbiont, which can cause some confusion when trying to determine if a BSC fungus is lichenized or not—unless an intact lichen thallus is observed or collected and identified by a trained lichenologist. Lichens are broadly classified based on their thallus morphology as being crustose, squamulose, foliose, or fruticose. Crustose lichens are crust-like. They are slow-growing and adhere tightly to the substrate or, in some cases, are physically integrated into the surface of the substrate (Armstrong and Bradwell, 2010). Squamulose lichens are composed of tightly clustered or overlapping scale-like structures (squamules) with no or only a poorly developed lower surface. However, squamules of some squamulose species form rhizoidal hyphae on their lower surface that effectively anchor the squamules to the soil surface. Squamulose lichens constitute one of the most common growth forms associated with BSCs (St. Clair et al., 1993). Foliose lichens are leaf-like, with distinctive upper and lower surfaces and are generally loosely attached to the substrate by root-like structures called rhizines (Brodo et al., 2001). Fruticose lichens are highly branched and are either upright and shrubby or pendant with a single point of attachment (Baron, 1999). BSC lichen dominated communities tend to be more common in undisturbed locations with well-developed vertical BSC structure (Rosentreter et al., 2007). Some BSC lichens, mostly foliose forms referred to as “vagrant lichens” (e.g., the lichen genera Xanthoparmelia and Rhizoplaca), occur unattached on the soil surface (Rosentreter, 1993). Generally, some of the more common BSC lichen genera include Psora, Placidium, Xanthocarpia, Lecanora, Circinaria, and Acarospora. Lichens have a broad distribution, occurring on a variety of substrates and occupying habitats ranging from the humid tropics to hyper-arid zones, and from the frigid tundra to hot deserts. When dry, they suspend all metabolic activity and are able to tolerate extremely high temperatures for extended periods of time. Lichens occur on a variety of substrates, including soil, rocks, monuments, statues, roofs, walls, fences, bark, and decorticated wood (St. Clair and Seaward, 2004). Lichens contribute to the weathering of stone substrates by producing weak organic acids (Chen et al., 2000; Souza-Egipsy et al., 2004; Leger and Forister, 2009). Lichens are desiccation-tolerant allowing them to inhabit very harsh environments and experience drought conditions for extended periods (Nash et al., 1990; Kranner et al., 2008).

Some lichens reproduce asexually using unspecialized thallus fragments (Armstrong, 2017; Almeida Pereira et al., 2018) or through the formation of small-specialized asexual structures containing cells of both the mycobiont and the photobiont. These specialized asexual structures include soredia, isidia, and lobules (Ott et al., 1993). Soredia are small, spherical bundles of algal cells wrapped in a mesh of fungal hyphae. Soredia frequently occur as powdery patches (soralia), which erupt through the upper surface (cortex) of some lichens. Isidia are specialized thallus fragments of various shapes and configurations attached to the upper surfaces of lichens. Like soredia, isidia contain both algal cells and fungal hyphae; however, unlike soredia the surfaces of isidia are encased in a layer of cortical cells. Lobules are small, flattened, variously shaped structures that generally occur along the edges of the thallus of some lichens. These specialized asexual regenerative structures are easily detached from the thallus surface by wind, rain, or other physical disturbance (Blackwell et al., 1996) and may subsequently be dispersed to a new suitable substrate where they become attached and form a new lichen thallus. Lichens commonly reproduce sexually as well; however, sexual reproduction in lichens is limited to the fungal partner, which produces sexual spores called ascospores within fruiting bodies called ascocarps. The photobiont (alga or cyanobacterium) is also capable of sexual reproduction, but, unlike the fungus, not while engaged in the lichen symbiosis. The primary limitation to sexual reproduction in lichens is the obstacle of the germinating ascospore encountering a viable photobiont partner in the process of attempting to reconstitute a new lichen thallus (Bowler and Rundel, 1975). However, the fact that many broadly distributed lichen species reproduce only sexually through the production of ascospores suggests that the likelihood of an ascospore germinating and surviving long enough to encounter an appropriate photobiont happens with impressive frequency. Though little is known about the dispersal of lichen gametes, the gametes of the lichen-forming fungus, Lobaria pulmonaria, are known to have an aerial dispersal range of several hundred meters to kilometers from mature individuals. On the other hand, clonal propagules (i.e., soredia and isidia) disperse over a distance of tens of meters while spores may be dispersed for several kilometers (Ronnås et al., 2017). However, joint dispersal of the mycobiont and photobiont does not necessarily imply that the two will be rejoined (Wornik and Grube, 2010). Indeed, they may switch symbiotic partners (Ertz et al., 2018).

Lichen thalli, are readily dispersed into adjacent and expanded habitats as both sexual and asexual propagules. Dispersal of either non-specialized or specialized thallus fragments over significant distances is accomplished by wind, water, or as attached to animal feathers, fur, or feet (Bailey, 1966). Researchers in northeastern Germany, a region not known for high winds, found that the dispersal distance of lichen fragments was negligible, and was measured in centimeters (Heinken, 1999). In contrast, areas where high surface winds are more common, lichen thallus fragments, detached reproductive structures (soredia, isidia, lobules), and spores can be lifted into the atmosphere and transported very long distances (Després et al., 2012). For example, lichen soredia have been collected at high altitudes in southwest Spain (Tormo et al., 2001) and Antarctica (Marshall, 1996). Airborne asexual lichen fragments have been collected from rooftops throughout the continental United States (Tripp et al., 2016). On an ocean voyage from the Polish Antarctic Station on King George Island by way of South Shetland Island to Gdynia, Poland, scientists intended to collect pollen grains daily on blotter paper. In addition to pollen, the scientists commonly found fungal spores, lichen thallus fragments, isidia, and soredia in abundance in all samples, indicating widespread distribution of airborne lichen propagules (Harmata and Olech, 1991). The abundance and distribution of fungal spores vary by species and climate (Marshall, 1997). The lichen genus Ramalina is found on the main island of New Zealand, as well as the outlying islands of New Zealand (Bannister and Blanchon, 2003), suggesting long-distance dispersal. The foliose lichen genus Xanthoparmelia, purportedly originated in South Africa, but is now present in South and North America as well as Australia (Amo de Paz et al., 2012).

Mycorrhizal Fungi

Mycorrhizal fungi are obligate plant root symbionts that provide their host plants with increased water and nutrient absorption capacity while the plant provides the fungus with carbohydrates from photosynthesis (Berruti et al., 2015). The roots of more than 80% of terrestrial plant species are obligatorily associated with mycorrizal fungi (Pirozynski, 1981; Smith and Read, 2008). In a mycorrhizal association, the fungus colonizes the host plant's roots, either intracellularly as in endomycorrhizal fungi or extracellularly as in ectomycorrhizal fungi. In endomycorrhizal fungi, the fungal hyphae penetrate the cortical layer of cells below the epidermis of the plant root. Some endomycorrhizal fungi form an intercellular multi-branched hyphal structure with slightly swollen chambers to store nutrients. Such a structure resembles a tree. Hence, such endomycorrhizal fungi are often referred to as vesicular mycorrhizae or vesicular-arbuscular mycorrhizae, or simply VM or VAM for short. All vesicular or vesicular-arbuscular mycorrizae are formed by members of the Glomeromycota phylum of the kingdom fungi (Kehri et al., 2018). There is a trend toward host-specificity among mycorrhizal fungi (Torrecillas et al., 2012) such that mycorrhizal fugal diversity can be used as an index of plant biodiversity in similar ecosystems (van der Heijden et al., 1998). Soils with vesicular arbuscular mycorrhizal fungi have significantly more stable aggregates than soils without (Andrade et al., 1995). The mycelia of mycorrhizal fungi can extend several centimeters beyond the plant roots, forming a mycelial mesh that binds soil particles (Miller and Jastrow, 1992; Soka and Ritchie, 2014). The mycelia also produce a glue-like glycoprotein, glomalin, that functions as an adhesive that binds soil particles together thus reducing soil erosion (Gianinazzi et al., 2010; Singh, 2012; Gomathy et al., 2018; Prasad et al., 2018), while enhancing the structural integrity of the BSC community (Chaudhary et al., 2009).

Sexual reproduction in Glomeromycota is unknown (Pawlowska, 2005). Hence, reliance on asexual modes of reproduction is essential. Typically, mycorrhizal fungi reproduce by asexual spores (Camargo-Ricalde, 2002; Marleau et al., 2011) or by hyphal fragments or plant roots containing mycorrhizal hyphae (Berruti et al., 2014).

Dispersal of mycorrhizal fungi is facilitated by the activity of burrowing insects, rodents as well as birds that disperse spores or hyphal fragments for short distances or expose them to the erosive forces of water and wind (Camargo-Ricalde, 2002) that can move them much farther. Recent research has documented large numbers of airborne mycorrhizal spores in a variety of different biomes and ecoregions in North America where they were previously unknown (Egan et al., 2014). Spores were most frequent in the air above more arid ecosystems, suggesting that they are more likely dispersed aerially from those systems. Efforts to detect and identify airborne mycorrhizal propagules is often difficult and tends to under-report some fungal taxa. The use of molecular approaches such as DNA metabarcoding, however, can uncover fungal diversity missed by traditional morphological techniques including microscopy (Pashley et al., 2012; Chen et al., 2018), thus providing a more comprehensive estimate of fungal diversity in aerial samples (Banchi et al., 2018).

Terrestrial Algae

Terrestrial eukaryotic algae of BSC communities include green algae, diatoms, xanthophytes, and eustigmatophytes. Like cyanobacteria, eukaryotic algae are photoautotrophic, using energy from sunlight to synthesize energy-rich organic compounds. Unlike cyanobacteria, they possess well-defined, membrane-bound, subcellular structures (e.g., nuclei, mitochondria, etc.) and may reproduce sexually. Although eukaryotic algae are usually aquatic, many species inhabit the soil, and participate in the formation of BSCs. Here we focus specifically on two groups of eukaryotic algae that are known to contribute to the structure of BSCs, namely, the green algae and diatoms.

Green Algae

Green algae of BSCs include free living and lichenized species, and most are unicellular, colonial, or filamentous in morphology. Several classes of green algae (Chlorophyceae, Trebouxiophyceae, Ulvophyceae, Klebsormidiophyceae, and Zygnematophyceae) including dozens of genera are found in BSC communities. In many cases, species of BSC green algae are closely related to aquatic sister species found in freshwater habitats, suggesting that the evolutionary transition to BSC habitats has happened many times in the green algae (Lewis and Lewis, 2005; Fučíková et al., 2014). As a group, green algal cell walls are highly diverse and include cellulose as well as other polysaccharides, and glycoproteins (Domozych and Domozych, 2014). Under certain conditions, filamentous green algae (e.g., Klebsormidium) may achieve high biomass and contribute to the consolidation of soil particles in BSCs due to their sticky polysaccharide-containing cell sheaths and exudates (Hoppert et al., 2004; Warren, 2014; Büdel et al., 2016). Other green algae may have lower biomass, but they also may produce sheath material that directly adheres to cyanobacteria, fungi, and other green algae (Hoppert et al., 2004). Hu et al. (2003) characterized the vertical profile of algae in a BSC “horizon,” intricately mapping the physical locations of green algae and other species. Green algae typically are distributed just below the surface of desert crusts, but they are known to form thick mats at the soil surface in other types of BSC communities (Hu et al., 2003; Hoppert et al., 2004). Some green algal taxa also live symbiotically as lichen photobionts and are typically distributed just below the surface of lichen thalli, their cells protected by fungal sunscreens (Nguyen et al., 2013).

Among BSC green algae, propagules include zygotes, asexual spores, or filament fragments. In nearly all cases, the green algae of BSC are small, unicellular, with dominant haploid vegetative stages. They can reproduce sexually, or asexually by fragmentation of filaments or simple cell division, by autospores (non-motile cells formed inside the mother cell wall), and through zoospores (flagellated cells). In aquatic relatives of BSC green algae, the diploid stage (zygote) is considered the stage that persists under conditions not supporting active growth (e.g., lack of water, freezing temperatures). For example, in temperate regions, the zygotes of pond algae persist in sediments over winter, and in the spring they undergo meiosis directly to form haploid vegetative cells. Likewise, if zygotes were formed by BSC green algae, they also could potentially serve as resistant aerial propagules. Motile cells have been documented in BSC species (Flechtner et al., 2013) but it is not clear if these represent gametes or zoospores because these stages often are morphologically similar. Sexual reproduction is difficult to demonstrate in unicellular terrestrial green algae unless the fusion of motile gametes is observed directly or zygotes are observed. Sex is difficult to induce even in the laboratory, and generally is not tested in cultured algae. It is also impossible to detect directly in field-collected material. That said, sexual reproduction is thought to be possible in these species, even if rare. Support for this is indirect, coming from surveys of genomic and transcriptomic data for meiosis genes in diverse eukaryotes, which are present in many trebouxiophycean genera, including terrestrial taxa (Fučíková et al., 2015). However, compared to algae living in aquatic habitats the opportunities for sexual reproduction in BSC taxa is greatly constrained because green algae require liquid water for their swimming gametes and because green algae in BSCs often are not present in high densities.

Green algae of BSCs do not necessarily need specialized spores or zygotes to disperse. Reproductive propagules of unicellular and multicellular eukaryotic algae are mostly dispersed aerially (Brown et al., 1964; Broady and Smith, 1994; Tesson et al., 2016). Genitsaris et al. (2011) documented 353 morphological taxa that have been reported in the literature related to aerobiology, with more reported regularly. The fact that new, cryptic species are being discovered and described (Cardon et al., 2008) suggests that additional species will be added to the list of aerobionts. Many algae occur in both the Arctic and Antarctic polar regions demonstrating a significant capacity for global long-distance dispersal (Jungblut et al., 2012). In addition to their occurrence in BSCs, airborne algae may also be deposited and survive on a variety of other substrates, including tree bark (Kharkongor and Ramanujam, 2014), glaciers and snow fields (Takeuchi, 2001; Kvíderova, 2012), polar fellfields (Marshall and Chalmers, 1997), and exterior building walls (Nakajima et al., 2015). In fact, the ability of vegetative cells to survive without water can be immediate. Hydrated, actively growing cells from diverse genera of green algae have been shown to survive rapid desiccation (Gray et al., 2007; Cardon et al., 2008) indicating the presence of mechanisms that prepare even actively growing cells for desiccation. In other species, the ability to survive is a function of the age of vegetative cells. For example, compared to young cells of the alpine taxon Zygnema that are tolerant to exposure to high UV-B stress (Holzinger et al., 2018) and Herburger et al. (2015) demonstrated that older vegetative cells (akinetes) are more tolerant to desiccation. Such stages likely are important to the ability of some species to survive long-range dispersal. To be part of the aerial flora, and in order to successfully colonize BSC habitats after dispersal, algae need to produce structures that can be lifted and moved in the air, and they need traits that enhance survival under drying conditions (Sharma and Singh, 2010). These algae exhibit the hallmarks of poikilohydry, by equilibrating to ambient humidity and having rapid responses upon water gain [reviewed in Green and Proctor (2016)]. Green algae, like cyanobacteria, and other photosynthetic species must also be able to survive in high light and possibly high UV habitats (Karsten and Holzinger, 2014), allowing them to survive in harsh, high elevation terrestrial habitats and during transport, deposition, and settlement while airborne (Tesson et al., 2016). Protective compounds including carotenoids, mycosporine-like amino acids, and a variety of phenolics are known in green algae (Kitzing et al., 2014; Holzinger et al., 2018). Diverse airborne green (and other) algae were noted by early researchers including van Overeem (1937) and Brown et al. (1964), with a recent review by Tesson et al. (2016). Given that BSC green algae are so diverse, and that different reproductive stages can survive dispersal, it is reasonable to assume that the underlying mechanisms that allow these species to live in habitats supporting BSCs may also vary (Holzinger and Karsten, 2013). While airborne, microalgae are tolerant to freezing temperatures and desiccation and are important ice nucleators contributing to the formation of ice and snow (Tesson and Šanti-Temkiv, 2018).

Diatoms

Diatoms, the second group of eukaryotic algae included in this section are commonly found in BSC communities (Ettl and Gärtner, 1995; Büdel et al., 2016). Diatoms are species diverse and best known from aquatic habitats, often being in high abundance in both marine and freshwater communities. However, several groups of diatoms include terrestrial species known to occur in damp soils or ephemeral aquatic habitats, as well as more arid habitats. BSC diatoms are phylogenetically diverse but are dominated by pennate species from at least four taxonomic orders. On a broad geographical scale, diatoms occur in diverse BSC habitats on all continents (Sharma et al., 2007; Souffreau et al., 2013a; Büdel et al., 2016), and many of the same species have been found on different continents, indicating that diatoms can be transported great distances (Souffreau et al., 2013a). More locally, diatom diversity in BSCs can be high, with upwards of 50 species reported (Borchhardt et al., 2017). Unlike green algae, whose walls are carbon-based, diatom cell walls are made of silicon dioxide. Often pennate diatoms, typical of many BSC species, have a slit-like channel (raphe) along the length of the cell that produces carbon-based mucilaginous exudates that accommodate motility (Edgar and Pickett-Heaps, 1982). These mucilaginous exudates also likely contribute to soil aggregation and stabilization in BSC habitats. Motile diatoms exhibit vertical movement in BSCs, in response to light and water availability (Hu et al., 2003). A significant diversity of diatom vegetative cells isolated from damp soils have been shown to be tolerant of wide temperature fluctuations (both heating and freezing), but they were not tolerant of desiccation. On the other hand, resting stages of terrestrial diatoms were resistant to periods without water (Souffreau et al., 2010, 2013b). This ability would allow for aerial transport, and a number of viable diatoms have been detected in airborne samples (Brown et al., 1964; Sharma et al., 2007). However, the precise mechanisms used by diatoms to tolerate periods of desiccation are not well-known.

Diatom vegetative cells including other cell types relevant to dispersal and perennation (e.g., auxospores) are diploid (2n). Asexual reproduction in diatoms involves mitotic divisions of vegetative cells (Mann, 1993). Initiation of sexual reproduction is directly related to the size of vegetative cells and is typically triggered when vegetative cell size has been reduced through repeated mitotic cell divisions, to a minimum size—usually smaller than half of the normal size for most species (Edlund and Stoermer, 1997). This overall reduction in cell size, through repeated mitotic divisions, is due to the fact that as vegetative cells divide the overlapping cell halves (valves or frustules) separate with both the top (larger) and bottom (smaller) halves regenerating a new bottom (smaller) half. The specific processes associated with sexual reproduction differs between the two main groups of diatoms—centric and pennate forms. However, the outcome is similar for both groups—production of a diploid structure—the auxospore that eventually restores the vegetative cell to the normal size and form (Kaczmarska et al., 2001). With subsequent mitotic cell divisions again reducing the size of future generations of vegetative cells to a point that sexual reproduction is triggered with meiosis producing gametes, by either oogamy or isogamy depending on the species. Gametes subsequently fuse to form the next generation of diploid auxospores (Mann, 1993).

Aquatic diatoms are generally dispersed by water currents. However, terrestrial diatoms (e.g., vegetative cells and auxospores) are typically dispersed through the atmosphere under very dry conditions (Sharma and Singh, 2010; Aguilera et al., 2018). Research has shown that diatoms can reach the atmosphere in various ways including volcanic eruptions (Pike, 2013; Van Eaton et al., 2013) and dust and sand storms (Griffin et al., 2002). Airborne diatom propagules have been collected by various methods from a variety of locations (Holzapfel, 1978; Vanormelingen et al., 2008; Pearce et al., 2016; Tesson et al., 2016).

Bryophytes

BRYOPHYTES are small spore-producing plants with a dominant and normally persistent gametophyte and include mosses, liverworts, and hornworts. Although without true xylem, many species of mosses are capable of effectively conducting water both endohydrically (in specialized water conducting tissues containing xylem precursors) and ectohydrically by quickly wicking up liquid water along external cell surfaces, often in a matter of seconds from the substrate into the shoot apices (Glime, 2017). Bryophytes, similar to lichens, are poikilohydric, whereby their tissues are capable of exchanging water vapor from ambient air and equilibrating their tissue water content with the water potential of the surrounding air (Glime, 2017). Most bryophytes differ from lichens in being unable to fully activate metabolism using just water vapor, although imbibing water vapor while yet desiccated acts to mitigate desiccation damage to tissues (Pardow and Lakatos, 2013; Slate et al., 2018). Nevertheless, carbon balance can be positive and recovery complete in some mosses without the addition of liquid water (Lange, 1969; Lakatos, 2011). Between the three groups, bryophytes comprise some 20,000 species (Shaw et al., 2011). Although there is a common misconception that bryophytes occur only in damp, shady environments, some species occur in hot, dry environments, or dry polar environments (McCleary, 1959; Scott, 1982). With the exception of the liverwort genus Cryptothallus, virtually all bryophytes contain chlorophyll and are photosynthetic. Cryptothallus has no chlorophyll and gets its photosynthates indirectly from a host tree via a symbiotic relationship with a saprophytic fungus of the Basidiomycota (Wickett and Goffinet, 2008). Most bryophytes are capable of surviving desiccation during rainless periods (Proctor et al., 2007) and desiccation tolerance even extends to antheridia and male gametes (Shortlidge et al., 2012; Stark et al., 2016b), embryonic sporophytes, and asexual propagules (Brinda et al., 2016; Stark et al., 2016a). Upon addition of liquid water, shoots become metabolically active (Harten and Eickmeier, 1987) and require about 24 h to recover in most instances (Coe et al., 2014). Bryophytes are able to anchor themselves to the ground or to other suitable substrates with slender root-like rhizoids that occur on the underside of the thallus, bases of shoots, or when protonemata become subterranean (Odu, 1978; Jang et al., 2011; Glime, 2017).

Bryophytes may reproduce sexually and asexually and these modes may co-occur in time. Although dependent upon liquid water for gamete transfer, in deserts selection has likely favored monoecious over dioecious (monoicy over dioicy) reproduction (Wyatt, 1982). A significant number of dioecious BSC mosses exist, and some of the more common species may (e.g., Bryum argenteum) or may not (e.g., Syntrichia caninervis, S. ruralis) produce aboveground specialized asexual propagules. Such asexual propagules may be cryptic and only produced during periods of abundant moisture, as in the protonemal gemmae of S. caninervis, Funaria hygrometrica, and B. argenteum (Glime, 2017). One of the most successful and widespread BSC species, B. argenteum, is capable of producing not only abundant spore capsules when both sexes are present, but also two kinds of gemmae (bulbils and protonemal gemmae). While the spores of B. argenteum are dispersed by air currents, their gemmae float and are likely instrumental in short distance dispersal by water. In addition to spores and propagules, probably all BSC bryophyte species commonly disperse by fragmentation of the plant body, the cells of which are totipotent (Glime, 2017). In their sexual life cycle bryophytes produce multicellular haploid individuals (gametophytes) which produce gametes through mitosis (Glime, 2017). Male and female gametes then fuse to form diploid individuals (sporophytes) which remain attached to the gametophytes and produce haploid spores by meiosis that in turn divide by mitosis to produce the multicellular haploid gametophyte generation—thus completing the bryophyte life cycle (Glime, 2017). Sexual reproduction in many bryophytes is uncommon in dry environments due to the paucity of sexual spores or the rarity of male plants (Bowker et al., 2000; Stark et al., 2000; Horsley et al., 2011). Asexual reproduction in bryophytes is far more prevalent than sexual reproduction (During and van Tooren, 1987; Hugonnot and Celle, 2012) and generally regarded as the primary avenue of species dispersal (Mishler, 1988). Genetic diversity of at least some BSC bryophyte species can remain high regardless of whether reproduction is sexual or asexual (Paasch et al., 2015). Asexual reproduction is more common in mosses (Pohjamo and Laaka-Lindberg, 2003) whereas sexual reproduction is more common in liverworts (Peñaloza-Bojacá et al., 2018).

Some bryophyte species are capable of producing millions of meiospores from individual sporophyte capsules or from a single m² (Longton, 1997; Australian National Botanic Gardens, 2016). However, the release of aerial propagules and particles can vary significantly over the period of a year based on weather conditions (Barbé et al., 2017), including wind speed and turbulence (Johansson et al., 2014). Aerial dispersal of bryophyte propagules is common (Flø and Hågvar, 2013) and long-distance dispersal rates may exceed shorter-distance dispersal (Lönnell et al., 2012). Long-distance aerial dispersal of diaspores (spores, gemmae, and/or leaf fragments) have all been reported (Laaka-Lindberg et al., 2003). Trans-oceanic and intercontinental dispersal is common (van Zanten, 1978; Shaw et al., 2011) and contributes to the intercontinental and bipolar distribution of species (Piñeiro et al., 2012; Lewis et al., 2014; Biersma et al., 2017). Such long-distance dispersal is now regarded as explanatory for the relative rarity of narrow endemics among bryophytes and other spore-bearing organisms (Shaw and Goffinet, 2000) when compared to seed plants. Gene flow through occasional long-distance dispersal events apparently prevents the evolution of, for example, sister species on different continents. The apparent lack of connectivity of populations is due in large part to the lack of environmental uniformity. Although propagules may be widely dispersed, not all end up in a climate or on a substrate conducive to their survival. Desert soils of the world are often dominated by a relatively few, widely distributed species of bryophytes. These are characterized by strongly developed traits of desiccation tolerance, whereby a constitutive or strongly inducible ecological strategy of desiccation tolerance has evolved (e.g., the genera Syntrichia, Tortula, Bryum, Crossidium, Aloina, Pterygoneurum). Interestingly, an inducible strategy of tolerating desiccation characterizes some of the common arid land mosses in the latter three genera. Such strategies enable the gametophyte shoots of mosses to tolerate rapid or slow rates of drying to the very low equilibrating relative humidity typical of desert habitats. Even so, the life phases of bryophytes exhibit a range of desiccation tolerance, with protonema and juvenile structures normally less resistant to desiccation (Greenwood et al., in review). In Janice Glime's E-book chapter on diaspore dispersal in bryophytes (2017), a number of studies based on several species and lines of reasoning support the idea of long-distance transport of diaspores that in turn lends credibility to the Baas-Becking hypothesis that “everything is everywhere and the environment selects.” Briefly, bryophyte species disperse farther than vascular plants, bryophyte species are generally more widely distributed than those of vascular plants, and the large numbers of disjunct bryophyte taxa between distant regions align with long-distance dispersal as the most supported process underlying these facts. The Baas-Becking hypothesis has been demonstrated for at least two bryophyte species, Bryum argenteum and Plagiobryum zierii, and also for the Sphagnum flora on an archipelago in the Baltic Sea. In addition, her review determined that spore size differences (small vs. large) does not inhibit dispersal, and that trans-continental spore dispersal is occurring. The Sphagnum spore rain is significant and thermal updraft and wind are significant factors controlling the dispersal of spores. Both updrafts and smoke from fires also likely facilitate spore dispersal. In the species Discelium nudum, evidence suggests that the majority of spores “escape the parent colony to travel greater distances” on the order of at least kilometers. Such evidence is consistent with the life history of many bryophyte species. Further, van Zanten (1976, 1978) and van Zanten and Pocs (1981) document spore survival under conditions typical of high altitude atmospheric air currents (i.e., desiccation, wetting, and freezing) and provide evidence that bryophyte spores can enter the jet stream and travel great distances, adding to other studies indicating that spores may be recovered in rainwater. Multiple genetic studies support a long distance dispersal hypothesis. Bryophyte spores are capable of surviving in the desiccated state for decades. Comparisons of spore desiccation tolerance and frost resistance between transoceanic and endemic species support long distance dispersal patterns, and the spore wall chemical composition suggests high survival capability befitting long distance transport.

Summary And Discussion

Biological soil crust communities include a variety of organisms that occupy the surface layer of the soil and consolidate soil particles and aggregates into a distinguishable stable crust resistant to the erosive forces of wind and water. The most common and abundant BSC organismal groups include—cyano-, heterotrophic, and diazotrophic bacteria, free-living, lichenized, and mycorrhizal fungi, eukaryotic algae including diatoms, and bryophytes. Historically, BSCs have been most noticeable and researched in arid and semiarid environments where the vascular plant community tends to be dominated by smaller shrubs with open inter-shrub spaces that offer minimal competition for direct sunlight and provide for more equitable distribution of essential resources. BSCs are becoming more recognized in humid environments, including the humid tropics; particularly, where disturbance has temporarily removed vascular plants that normally compete for sunlight and other essential resources at soil surfaces.

Herein, we provide a thorough discussion of the various modes of reproduction and dispersal employed by the core BSC organismal groups. Modes of reproduction vary between the organismal groups but generally include both sexual and asexual alternatives, although asexual options (e.g., fission, budding, fragmentation, etc.) are far more prevalent among BSC organisms. Following successful reproduction, sexual, and/or asexual propagules must be dispersed to new, suitable environments in order to avoid competition with established local BSC communities. Almost universally, BSCs are dispersed aerially, often for very long distances, sometimes intercontinentally and interhemispherically (Muñoz et al., 2004; Sharma and Singh, 2010; Smith et al., 2013, 2018; Herbold et al., 2014; Maki et al., 2019; Warren et al., 2019).

In spite of the extensive, research concerning arid BSC communities over the last 50 years there are still areas of research that need additional work. Specifically, some of the organismal groups are poorly known—particularly in terms of species diversity and ecological roles. For example, very little is known about the diversity and ecological roles of both the free-living and mycorrhizal fungi associated with BSCs. More work is also needed in terms of better understanding the community and ecosystem dynamics of BSCs. This paper provides important background information about the occurrence, reproduction, and dispersal of the various core organismal groups that contribute to the development and maintenance of BSC communities. However, effective application of modern molecular and microenvironment sampling tools will be pivotal in answering key questions about the diversity and functional attributes and relationships within BSC communities.

Author Contributions

SW and LLS initiated, organized, and directed the endeavor. They jointly composed the section on cyanobacteria. SW composed the section on mycorrhizal fungi. LLS composed the section on lichenized fungi. LRS composed the section on bryophytes. LL composed the section on terrestrial algae. JS, NP, and TK composed the section on free-living fungi. ZA composed the section chemoheterotrophic bacteria.

Funding

LRS contributed to publication fees for this article via the UNLV University Libraries Open Article Fund. Funding for publication was contributed by LLS via the Monte L. Bean Museum, by grant number DEB-1036448 from the National Science Foundation to LL, and by USDA-National Institute of Food and Agriculture Hatch project CA-R-PPA-5062-H to JS. NP was supported by a Royal Thai government fellowship.

Conflict of Interest

The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.

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