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korová
Zurich-Basel Plant Science Center, Institute of Botany, University of Basel, Hebelstrasse 1, CH-4056 Basel, Switzerland
Ewald Sieverding 1
Institute of Plant Production and Agroecology in the Tropics and Subtropics, University of Hohenheim, Garbenstrasse 13, D-70593 Stuttgart, Germany
| ABSTRACT |
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Acaulospora alpina sp. nov. forms small (6585 µm diam), dark yellow to orange-brown spores laterally on the neck of hyaline to subhyaline sporiferous saccules. The spores have a three-layered outer spore wall, a bi-layered middle wall and a three-layered inner wall. The surface of the second layer of the outer spore wall is ornamented, having regular, circular pits (1.52 µm diam) that are as deep as wide and truncated conical. A "beaded" wall layer as found in most other Acaulospora spp. is lacking. The spore morphology of A. alpina resembles that of A. paulinae but can be differentiated easily by the unique ornamentation with the characteristic pits and by the spore color. A key is presented summarizing the morphological differences among Acaulospora species with an ornamented outer spore wall. Partial DNA sequences of the ITS1, 5.8S subunit and ITS2 regions of ribosomal DNA show that A. alpina and A. paulinae are not closely related. Acaulospora lacunosa, which has similar color but has generally bigger spores, also has distinct rDNA sequences. Acaulospora alpina is a characteristic member of the arbuscular mycorrhizal fungal communities in soils with pH 3.56.5 in grasslands of the Swiss Alps at altitudes between 1800 and 2700 m above sea level. It is less frequent at 13001800 m above sea level, and it so far has not been found in the Alps below 1300 m or in the lowlands of Switzerland.
Key words: Alps, Acaulosporaceae, Acaulospora paulinae, Acaulospora lacunosa, Glomeromycetes, key, molecular identification, mycorrhiza, spore morphology, phylogeny, taxonomy
| INTRODUCTION |
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The genus Acaulospora was described by Gerdemann and Trappe (1974)
who also presented the first key for the two species known at that time. The key differentiated a species known to produce spores with a smooth surface (A. laevis) from another one with an ornamented surface (A. elegans). Today we know 18 Acaulospora spp. with smooth spore surfaces and 15 Acaulospora spp. (including A. alpina) with ornamentation of the outer spore wall. Schenck et al (1984)
presented the latest key to the ornamented species of Acaulospora. They used spines, tubercles, ridges, folds, pits or cracks as differentiating features for the spore wall ornamentations. We use similar characteristics and we present an updated key for Acaulospora spp. with ornamented spore walls.
In recent years molecular biological tools have been applied to identify AM fungi (Clapp et al 1995
, Redecker 2000
, Oehl et al 2005a
). Environmental rDNA sequences are rapidly increasing in number in the public databases. However only a few DNA sequences of Acaulospora originating from morphologically characterized spores are available. This is also true for the highly variable rDNA internal transcribed spacer (ITS) region, which is a useful tool to distinguish many species-level AM fungal taxa (Redecker et al 2003
). Some of these database sequences show strong similarity to fungal groups other than the Glomeromycota and are more likely to originate from contaminant organisms (Millner et al 2001
). Therefore there is a clear need for rDNA sequences from described Acaulospora species.
New species can be adequately characterized only when sequences of morphologically similar species are included in the analysis. To identify the phylogenetic position of A. alpina the sequence of the ITS1, 5.8S rDNA and ITS2 region was determined not only from this new species but also from A. paulinae Blasz. (Blaszkowski 1988
) and A. lacunosa J.B. Morton (Morton 1986
) which produce morphologically similar spores. Sequences obtained for A. alpina also were compared to environmental sequences of Acaulospora spp. available from the public databases.
| MATERIALS AND METHODS |
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AM fungal bait cultures.
Bait cultures were established directly after sampling as follows: 1000 mL pots were half filled with 500 g of an autoclaved substrate (Terragreen; American aluminium oxide, Oil Dry US special, type III R; Lobbe Umwelttechnik Iserlohn, Germany) Loess mixture 3 : 1; pH-KCl 6.2; organic carbon 0.3%; available P (Na-acetate) 2.6 mg kg1; available K (Na-acetate) 350 mg kg1. Fifty g dry weight field samples were placed at one side on the top of the substrate and covered with another 300 g of autoclaved substrate. Above the soil inocula, about 57 seeds of each of the four trap plants, Plantago lanceolata L., Lolium perenne L., Trifolium pratense L. and Hieracium pilosella L. were sown. A total of 0.2 mL of a culture broth with Rhizobium trifolii (DSM 30138, from DSMZ-Deutsche Sammlung von Mikroorganismen und Zellkulturen GmbH, Braunschweig, Germany) grown in liquid DSMZ 98 medium at 27 C for 12 h, was added to the 2 wk old Trifolium pratense plants in each pot. An automated watering system (Tropf-Blumat, Weninger GmbH, A-6410 Telfs) was installed and the cultures were kept in the greenhouse of the Institute of Botany in Basel under ambient natural light and temperature conditions until the end of 2004. The average annual temperature in Basel is about 9.5 C. The formation of spores in the bait cultures was checked JunDec 2004 at bimonthly intervals as described by Oehl et al (2003
, 2004)
. The new fungus only infrequently produced spores in these bait cultures. All trials of monospecies cultures, either initiated with single or multispores, so far failed to establish a successful symbiosis.
Morphological analyses.
The described morphological characteristics of spores and sporiferous saccules and their subcellular structures are based on observations of specimen mounted in polyvinyl alcohol-lactic acid-glycerol (PVLG; Koske and Tessier 1983
), in a mixture of PVLG and Melzers reagent (Brundrett et al 1994
), a mixture of lactic acid to water at 1 : 1, Melzers reagent, and in water. The terminology of the spore structure basically is that of Stürmer and Morton (1999)
which was adapted by INVAM (International Culture Collection of Arbuscular and Vesicular-Arbuscular Endomycorrhizal Fungi, www.invam.caf.wvu.edu), but we use different abbreviations for the walls and wall layers. In detail, we call the outer "spore wall" layers of the Acaulosporaceae sw13, the first flexible inner wall iw1 of Stürmer and Morton (1999)
, the "middle wall" (mw), and the second flexible inner wall iw2 of Stürmer and Morton (1999)
the "inner wall" (iw). Photographs (FIGS. 19
, 1119
) were taken with a digital camera (Olympus model DP70-CU) on a compound microscope (Zeiss Axioplan). To improve the quality of the pictures taken of the ornamentation of different Acaulospora spp., the software Auto-Montage Essentials 5.00 (Olympus) was used (technique used in FIGS. 13, 7, 8
, 14, 15
). Specimen mounted in PVLG and the mixture of PVLG and Melzers reagent were deposited at Z+ZT (Zürich, Switzerland), FB (Freiburg, Germany) and OSC (Corvallis, USA) herbaria.
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Sequences were aligned in PAUP*4b10 (Swofford 2001
) in a dataset comprising rDNA ITS1, 5.8S subunit and ITS2 of other fungi from the family Acaulosporaceae. From a total of 700 positions in the alignment, 315 positions were selected that were in unambiguous alignment. The ITS1 region contains numerous insertions/deletions in long stretches of A or T, which causes serious alignment problems, therefore this region was excluded from the analysis. In all phylogenetic analyses the sequence of the AM fungus Entrophospora colombiana was used as outgroup. The appropriate sequence evolution model for maximum likelihood analysis (HKY+G) was determined with Modeltest 3.5. (Posada 2004
). Bayesian analysis was performed in MrBayes 3.0 (Ronquist and Huelsenbeck 2003
). Four chains were run over 3.6 x 106 generations with a burn-in value of 2000. Neighbor joining analysis was performed with the Kimura 2-parameter model and a gamma shape parameter of 0.5. Maximum likelihood distances obtained by the HKY+G model were used for neighbor joining, which yielded the same tree topology. Bootstrap analysis (Felsenstein 1985
) was performed to estimate the robustness of the phylogeny.
| TAXONOMIC ANALYSIS |
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Sporiferous saccule is hyaline, globose (ca. 6580 µm diam) to subglobose, 6575 x 7592 µm, with one wall layer that is generally 1.02.1 µm thick (FIG. 1
); formed at the end of a hypha in 4080 µm distance from the spore that arises thereafter. The saccule usually collapses after the spore wall has formed and usually is detached from mature spores in soil samples.
Spores (FIGS. 14
) form laterally on the subtending hypha of the sporiferous saccule. The spores are dark yellow, orange to brown, globose to subglobose, (53) 6585(97) µm diam, rarely ovoid to irregular, (53) 6081(91) x 6287(110) µm diam.
Outer spore wall consists of three layers (sw1, sw2 and sw3), in total 2.54.0 µm thick (FIGS. 5, 6
). Outer layer (sw1) is hyaline, unit, 0.51.0 µm thick, sloughing, evanescent and thus, usually absent in mature spores. Second layer (sw2) is light to dark yellow to yellow-orange to orange-brown, laminated, 2.03.0 µm thick including the ornamentation with regular, round and truncated conical pits that are 1.52.2(2.8) µm diam and at least as deep as wide (FIGS. 79
). Due to their truncated cone shape the pits often appear to have a dark central point, but there is no second depression or a projection within the pit. The distance between the pits is (3.0)46(7) µm. The inner spore wall layer (sw3) is concolorous with sw2, 0.51.3 µm thick, usually tightly adherent to sw2 and often difficult to observe when <1.0 µm. None of these wall layers stains in Melzers reagent.
Middle wall is hyaline, bilayered and thin; in total 0.51.2 µm; both layers (mw1 and mw2) are semi-flexible (FIG. 5
), tightly adherent to each other and thus, often appearing as being one wall layer (FIG. 6
). None of the layers reacts to Melzers.
Inner wall is hyaline, with three layers (iw13) that are 1.23.0 µm thick in total (FIG. 5
). The iw1 is about 0.5 µm thick, and not "beaded"; iw2 is 1.22.0 µm thick; iw3 is about 0.5 µm thick and usually difficult to detect due to the close adherence to iw2. Only iw2 shows a light, pale pink reaction to Melzers reagent (FIG. 6
) usually visible only in cracked spores and not observed in all specimen.
Cicatrix (FIGS. 4, 7
) remains after detachment of the connecting hypha (FIG. 4
), (5)712 µm wide. The layer sw2 often continues for a small distance (0.82.2[3] µm) into the detaching hypha forming a short cylindrical pedicel around the pore. While the pore itself is not ornamented, the tapering pedicel wall often has the pitted ornamentation of sw2. The pore is closed by some of the inner laminae of sw2 and by sw3.
Etymology. Latin, alpina, referring to the Swiss Alps where the species was first found.
Specimen examined. SWITZERLAND. GRISCHUN: Sent, Alp Spadla, at 20002700 m a.s.l. (HOLOTYPE: Z+ZT); GRISHUN: Pontresina, Diavolezza at 20002700 m; GRISCHUN, San Murezzano (St. Moritz), Corviglia at 2700 m; GRISHUN: La Punt, Passo DAlvra-Piz Üertsch, at 23002600 m, GRISHUN: Sur, Tschima da Flix, at 20002500 m; GRAUBÜNDEN: Davos, Parsennhütte and Stützalp, at 18002300 m (ISOTYPE: OSC); GRAUBÜNDEN: Chur-Haldenstein, at 16202300 m; GRISHUN: Sumvitg-Surrein, Alp Nadels, at 19502500 m; TICINO, Olivone, Piz Corvo-Paso di Lucomagno, at 18002500 m; TICINO: Airolo, Passo di Gotthardo, at 18002000 m; URI and VALAIS: Realp-Oberwald, Furkapass, at 18502650 m; BERN: Axalp, Axalphorn, at 17002300 m; BERN: Grindelwald, Grosse Scheidegg/Gemschberg, at (1350)18002500 m (ISO-TYPE: FB); VALAIS: Ovronnaz, Grand Muveran, at 17202600 m; VALAIS: Champez, Le Cartogne, at (1350)18002600 m; VALAIS: Col de Grand St Bernhard, Pointe de Drône, at 23002500 m a.s.l.
Commentary. Spores of A. alpina were abundantly isolated from the rhizosphere of alpine grasslands (soil pH 3.55.5) with vegetation dominated by Carex curvula All. and/or Nardus stricta L. Spores were less frequent in alpine grassland soils with pH > 6.0 and plant species communities dominated by Carex ferruginea Scop., Carex sempervirens Vill. or Sesleria caerulea (L.) Scop., or in lower altitude grasslands (15001800 m a.s.l.) with plant species communities dominated by Nardus stricta or by Trisetum flavescens (L.) P. Beauv. The new species was found in a broad range of soils that developed on acidic sandstones, siliceous gneiss and granite rocks, up to ultrabasic serpentinite and calcareous "Bündner Schiefer" schists and carbonatic and dolomitic limestones.
Molecular biological analysis.
Sequences of approximately 550 bp long were obtained, comprising ITS1, the 5.8S rDNA subunit and ITS2. Phylogenetic analysis firmly placed all sequences of A. alpina into the genus Acaulospora and in a single clade, which is clearly distinct from the other Acaulospora spp. that have been analyzed. In particular A. lacunosa and A. paulinae are not closely related to A. alpina or each other. The sister group of A. alpina is made up of environmental sequences obtained from roots from the Schiefergebirge mountains of Thuringia, Germany (Renker et al 2003
) and an alpine meadow near Ramosch (Canton Grischun, Switzerland) (FIG. 10
). One of the environmental sequences from Anthoxanthum roots (ASP504636) appears to be an outlier, grouping somewhat intermediate between A. alpina and the other sequences obtained from roots. These environmental sequences are different from those of A. alpina as indicated by the bootstrap values. Together A. alpina and the environmental sequences form a monophyletic clade that is supported by the bootstrap distance analyses and Bayesian probabilities test. Five major clades were recovered consistently within Acaulospora (FIG. 10
) by distance, maximum likelihood and Bayesian analyses and received good support: (i) A. paulinae/denticulata, (ii) A. morrowiae/mellea, (iii) A. alpina and environmental sequences from mountainous areas, (iv) A. lacunosa, (v) A. laevis/colossica. With the exception of the first two, which were identified as sister groups, the deeper relationships among clades were not resolved well.
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| KEY TO ACAULOSPORA SPP. WITH ORNAMENTED OUTER SPORE WALLS |
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| DISCUSSION |
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Three AM fungal species have similarities in spore morphology with A. alpina. Acaulospora taiwania shares spore size and spore color but forms the spores in sporocarps and not singly in the soil as A. alpina. Furthermore the ornamentation on the spore wall of A. taiwania consists of 45-sided pits that give the appearance of a mesh. The morphological definition of A. paulinae is broad and there is overlap with A. alpina. However the ornamentation structures of A. paulinae are coarser, less regular and consist of concave pits or depressions (FIG. 16
), and not of truncated conic depressions as in A. alpina (FIGS. 5, 8
). Also spores of A. paulinae have a significant "beaded" inner wall layer, and the innermost layer stains strongly in Melzers reagent. Spores of A. lacunosa are similar in color to those of A. alpina but they are bigger. Moreover A. lacunosa has irregular depressions on the spore surface, a beaded inner wall layer, and one of the inner wall layers stains dark purple in Melzers reagent.
Spores size of A. undulata is similar to that of A. alpina. However they are white to creamy and the round concave pits are generally wider in diameter. Furthermore in A. undulata the middle wall is lacking and the inner wall bears some similarity to the inner wall of some species of the genus Archaeospora J.B. Morton & D. Redecker (Morton and Redecker 2001
). The root infection structures of A. undulata stain only weakly with trypan-blue, and vesicles were scarce (E. Sieverding unpublished observations). These features are typical for members of the genus Archaeospora. Spores of A. myriocarpa also lack the middle spore wall (see above) and the root infection structures of A. mycriocarpa (Schenck et al 1986
) resemble those of Archaeosporaceae (Morton and Redecker 2001
) too. Based on these observations it is possible that A. undulata and A. myriocarpa both are members of Archaeosporaceae.
Phylogenetically both A. paulinae and A. lacunosa clearly are separated from A. alpina (FIG. 10
). These three species are not related. Comparison of sequences obtained from spores to those from field-collected roots allows additional insights into the occurrence and ecological range of AM fungal taxa. The closest relatives to A. alpina were detected in roots from a site close to one of our spore sampling sites (Ramosch, Engadin) and from a mountainous grassland (710 m a.s.l.) in central Germany (Renker et al 2003
) (FIG. 10
). These data suggest that species related to A. alpina may occur at alpine as well as lower altitude mountainous areas. Our analyses also show that previously unnamed environmental sequences from Costa Rica (AY248771
[GenBank]
) apparently belong to A. lacunosa. Some other previously published sequences from this species (Millner et al 2001
) are not related to A. lacunosa, and even not to the Glomeromycota. It is likely that the sequences belong to non-Glomeromycota fungi inhabiting AM fungal spores.
Acaulospora lacunosa was described from lower pH soil and soils with high aluminium concentration in West Virginia (Morton 1986
). Acaulospora paulinae was reported to be widespread in grasslands and arable lands of Poland (Blaszkowski 1993
). We found A. paulinae frequently in grasslands and arable lands of the upper Rhine lowland in France, Germany and Switzerland (Oehl et al 2003
, 2004
, 2005b
) and lower mountainous regions, but restricted to decarbonated soils with pH of 46.5. With increasing altitude in the Alps spores of A. paulinae were found in decreasing spore numbers, but spores were found even up to 3000 m a.s.l. (www.nfp48.ch/projekte/projectdocs/17/Wiemken.pdf). In contrast spores of A. alpina were most abundant in grasslands of the high mountainous and alpine regions at 19002600 m a.s.l. Above 2700 m a.s.l. the species rarely was found. So far it was never detected in the lowlands or in the Swiss Alps in mountainous grasslands at altitudes below 1300 m a.s.l.
| ACKNOWLEDGMENTS |
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| FOOTNOTES |
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1 Corresponding author. E-mail: sieverdinge{at}aol.com
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