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M, Frahm J-P (in press) Relic or long-distance dispersal? A case study of the rare and endangered moss Campylopus oerstedianus (Mu¨ll. Hall.) Mitt. (Dicranaceae) in Europe. Cryptogamie Bryol Schuster RM (1984) Phytogeography of the bryophytes. In: Schuster RM (ed), New manual of bryology, vol I. The Hattori Botanical Laboratory, Nichinan, pp 463–626 Stech M, Dohrmann J (2004) Molecular relationships and biogeography of two Gondwanan Campylopus species, C. pilifer and C. introflexus (Dicranaceae). Monogr Syst Bot Missouri Bot Gard 98 415–431 Vitt DH, Bellard RJ (1997) Attributes of rarity among Alberta mosses: patterns and prediction of species diversity. Bryologist 100:1–12 Zanten BO (1978) Experimental studies on trans-oceanic long-range dispersal of moss species in the Southern Hemisphere. J Hattori Bot Lab 44:455–482 Zanten BO, Po´cs T (1981) Distribution and dispersal of bryophytes. Adv Bryol 1:479–562 50 W. Foissner et al. (eds) Myxomycete diversity and distribution from the fossil record to the present Steven L. Stephenson · Martin Schnittler · Yuri K. Novozhilov Originally published in the journal Biodiversity and Conservation, Volume 17, No 2, 285–301. DOI: 10.1007/s10531-007-9252-9 © Springer Science+Business Media B.V. 2007 Abstract The myxomycetes (plasmodial slime molds or myxogastrids) are a group of eukaryotic microorganisms usually present and sometimes abundant in terrestrial ecosys- tems. Evidence from molecular studies suggests that the myxomycetes have a signiWcant evolutionary history. However, due to the fragile nature of the fruiting body, fossil records of the group are exceedingly rare. Although most myxomycetes are thought to have very large distributional ranges and many species appear to be cosmopolitan or nearly so, results from recent studies have provided evidence that spatial distribution patterns of these organ- isms can be successfully related to (1) diVerences in climate and/or vegetation on a global scale and (2) the ecological diVerences that exist for particular habitats on a local scale. A detailed examination of the global distribution of four examples (Barbeyella minutissima, Ceratiomyxa morchella, Leocarpus fragilis and Protophysarum phloiogenum) demon- strates that these species have recognizable distribution patterns in spite of the theoretical ability of their spores to bridge continents. Keywords Distribution patterns · Ecology · Long-distance dispersal · Microorganisms · Slime molds Special Issue: Protist diversity and geographic distribution. Guest editor: W. Foissner. S. L. Stephenson Department of Biological Sciences, University of Arkansas, Fayetteville, AR 72701, USA M. Schnittler (&) Institute of Botany and Landscape Ecology, Ernst Moritz Arndt University Greifswald, Grimmer Str. 88, 17487 Greifswald, Germany e-mail: martin.schnittler@uni-greifswald.de Y. K. Novozhilov V.L. Komarov Botanical Institute of the Russian Academy of Sciences, Prof. Popov St. 2, 197376 St. Petersburg, Russia W. Foissner et al. (eds.), Protist Diversity and Geographical Distribution DOI: 10.1007/978-90-481-2801-3_5 51 52 W. Foissner et al. (eds) Introduction The myxomycetes (also called plasmodial slime molds or myxogastrids) are a group of eukaryotic microorganisms usually present and sometimes abundant in terrestrial ecosys- tems. Myxomycetes have been known from their fruiting bodies since at least the middle of the seventeenth century, when the Wrst recognizable description of a member of the group (the very common species now known as Lycogala epidendrum) was provided by the Ger- man mycologist Thomas Panckow. Evidence from molecular studies (e.g., Baldauf and Doolittle 1997; Baldauf et al. 2000) indicates that the myxomycetes should be placed within the “crown” clade of eukaryotes, which would suggest that they have a signiWcant evolutionary history. However, due to the fragile nature of the fruiting body, fossil records of the group are exceedingly rare. Domke (1952) described a species of Stemonitis and Dörfelt et al. (2003) a species of Arcyria from Baltic amber dating from the Eocene, whereas Waggoner and Poinar (1992) reported the fossil of a myxomycete plasmodium in amber from Eocene-Oligocene deposits in the Dominican Republic. The maximum age that could be assigned to any of these fossils would not exceed about 50 million years, which is greater than that of the few records of fossil spores that appear to be those of myxomycetes, which date only from the Oligocene and Pleistocene (Graham 1971). Life cycle The myxomycete life cycle (Fig. 1) encompasses two very diVerent trophic stages, one consisting of uninucleate amoebae, with or without Xagella, and the other consisting of a distinctive multinucleate structure, the plasmodium (Martin et al. 1983). Under favorable conditions, the plasmodium gives rise to one or more fruiting bodies containing spores. IdentiWcation of myxomycetes is based almost exclusively upon features of the fruiting body (Martin and Alexopoulos 1969). The fruiting bodies produced by myxomycetes are somewhat suggestive of those produced by higher fungi, although they are considerably smaller (usually no more than 1–2 mm tall). The spores of the vast majority of myxomycetes range in size from 5 to 15 �m in diameter, with most species producing spores 10 § 2 �m in diameter. Presumably, the spores are wind-dispersed and complete the life cycle by germinating to produce the uninucleate amoeboXagellate cells. These feed and divide by binary Wssion to build up large populations in the various microhabitats in which these organisms occur. Ultimately, this stage in the life cycle gives rise to the plasmodium. This process can result from gametic fusion between compatible amoeboXagellates or it can be apomictic (Collins 1980, 1981). Bacteria apparently represent the main food resource for both trophic stages, but plasmodia are also known to feed upon yeasts, algae (including cyanobacteria), and fungal spores and hyphae (Stephenson and Stempen 1994). Under adverse conditions, such as drying out of the immediate environment or low temperatures, a plasmodium may convert into a hardened, resistant structure called a sclerotium, which is capable of reforming the plasmodium upon the return of favorable conditions. Moreover, amoeboXagellate cells can undergo a reversible transformation to dormant structures called microcysts. Both sclerotia and microcysts can remain viable for long periods of time and are probably very important in the continued survival of myxomycetes in some ecological situations and/or habitats, such as the bark surface of living trees and deserts. The fruiting bodies of many species of myxomycetes can achieve macroscopic dimen- sions and be collected and preserved for study in much the same way as the sporocarps of Protist Diversity and Geographical Distribution 53 fungi or even specimens of bryophytes, lichens, and vascular plants. However, most species of myxomycetes tend to be rather inconspicuous or sporadic in their occurrence and are not always easy to detect in the Weld. Moreover, fruiting bodies of most species are relatively ephemeral and do not persist in nature for very long. Myxomycetes also spend a portion of their life cycle in a state where their very presence in a given habitat can be exceedingly diYcult if not impossible to determine. Because of their life history strategy and inconspicuous nature, these organisms provide an immense challenge in biodiversity assessments and, consequently, often have been neglected in such studies. Taxonomy Approximately 875 species of myxomycetes have been described (Lado 2001), and these have been placed in six diVerent taxonomic orders (Ceratiomyxales, Echinosteliales, Fig. 1 Life cycle of a typical myxomycete. A, Spore. B, Germinating spore. C, Uninucleate amoeboid stage, with (right) or without (left) Xagella. D, Microcyst. E–F, Fusion of two compatible amoebae to produce a sin- gle cell. G, Zygote. H, Early plasmodium. I, Sclerotium. J, Portion