Biodiversity Data Journal Biodiversity Data Journal Biodiversity Data Journal BDJ 1314-2836 1314-2828 Pensoft Publishers Biodiversity Data Journal 10.3897/BDJ.3.e4297 3555 Taxonomic paper Protozoa Biogeography Ecology Systematics Cenozoic World Africa On the morphology, biometry and biogeography of Lamtopyxis callistoma (Amoebozoa: Arcellinida) Todorov Milcho todorovmilcho@gmail.com † Institute of Biodiversity and Ecosystem Research, Bulgarian Academy of Sciences, 2 Gagarin Str., 1113 Sofia, Bulgaria

Corresponding author: Milcho Todorov (todorovmilcho@gmail.com).

Academic editor: Anne Thessen

 2015 13 01 2015 3 e4297 04 12 2014 07 01 2015 Milcho Todorov This is an open access article distributed under the terms of the Creative Commons Attribution License 4.0 (CC-BY), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.

The ultra-structure of the shell and the morphometric variability of soil inhabiting testate amoeba Lamtopyxis callistoma from Madagascar were studied by using light- and scanning electron microscopy. The biometrical characteristic of the species was made on the basis of 75 specimens measured. In addition to the diameter of the shell, six other shell characters were described biometrically for the first time. The analysis of the variation coefficients shows that the studied population of L. callistoma is comparatively homogeneous and almost all measured characters are weakly to moderate variable (CV less than 10%). Scanning electron microscopy (SEM) studies on the shell ultra-morphology show that it has a smooth apertural surface with a thick layer of porous and fibrous organic cement and a rough dorsal surface composed of bigger and angular pieces of quartz. The shell wall has a thickness of about 5-6 µm and is composed of three layers. Unlike the previously accepted opinion that species is characterized by the presence of four teeth, this study shows that population of L. callistoma from Madagascar is comprised of both, specimens with four teeth and specimens with three teeth, in ratio of about 60% to 40%. Taking into account the restricted geographical distribution, large sizes and characteristic apertural morphology of L. callistoma it is assumed that this species, like some bryophilic ‘Nebelas’ with circumaustral distribution (e.g. Apodera vas, Alocodera cockayni, Certesella certesi, Certesella martiali, etc.), can be used as an example that in free-living microbial eukaryotes ‘not everything is everywhere’.

 Testate amoebae Amoebozoa Arcellinida Lamtopyxis callistoma ultra-structure biometry biogeography. Introduction

The genus Lamtopyxis is one of the testacean genera which include exclusively soil inhabiting species. It was described by Bonnet (1974) and so far only 5 species are known (L. callistoma Bonnet, 1974, L. cassagnaui Bonnet, 1977, L. travei Bonnet, 1977, L. trifoliata Bonnet, 1979 and L. sarocchii Coûteaux et Chardez, 1981). A typical characteristic for the species of this genus is specific apertural morphology with presence of 3-5 apertural teeth. Another feature is that they have been found only in soils of tropical forests from countries situated south of the Tropic of Cancer: Nepal (Bonnet 1977c, Bonnet 1981b), Mexico (Bonnet 1977a), Brazil and Paraguay (Bonnet 1979b), Philippines (Bonnet 1980b), French Guiana (Coûteaux and Chardez 1981), Thailand (Bonnet 1981a, Bonnet 1987, Golemansky and Todorov 2000), Indonesia (Bonnet 1985, Bonnet 1992), Ecuador (Krashevska et al. 2007, Krashevska et al. 2010). This is the reason that they are considered a rare species of the Gondwanan-tropical group, with restricted geographical distribution. Because of their rarity and the fact that they have been described using mainly light microscopy, data about their ultramorphology and biometry are incomplete in the literature. L. callistoma is a type species of the genus which was first described by Bonnet (1974) from gallery forest from Ivory Coast (the Savanna Lamto). Until now it has been recorded from only four tropical countries: Ivory Coast (Bonnet 1974, Bonnet 1976), Papua New Guinea (Bonnet 1980a), Philippines (Bonnet 1980b) and Indonesia (Bonnet 1992) and its ultramorphology and biometry is still poorly studied. During our investigation on the soil testate amoebae from Madagascar we observed an abundant material of L. callistoma. This provided us the opportunity to make more detailed studies on the shell ultramorphology and morphometric variability of this species. The aim of the present study was to describe morphologically and biometrically L. callistoma and to assess the biogeographical importance of this rare species of the Gondwanan-tropical group of soil testate amoebae.

 Materials and methods

The material for the present study (an aggregate sample of about 500 g) was collected in October 2013 from the organic horizon (litter, twigs and woody material) of rainforests at the Maromizaha Protected Area (Madagascar). This Protected Area is located in Central Madagascar, east of the capital Antananarivo and south of the village Anevoka, on the eastern slopes of the Central Highlands (18°57'S, 48°27'E, 950 m a.s.l.). At the laboratory, the material was dried for one day in a thermostat at 60˚C. Then was soaked and mixed in chlorinated tap water for about ten minutes, after which was filtered through a sieve with 500 μm mesh to remove large organic and mineral particles. The resulting filtrate was allowed to precipitate for two hours, the sediment was removed and the shells that floated on the surface were collected for examination. The study was carried out 12 hours after the flotation, when the gas bubbles inside the shells completely disappeared and the structure of the shells was well visible. All filtrate was examined in a petri dish at 100X magnification with Stereomicroscope “STEMI” Citoval-2 (Carl Zeiss Jena). A total of 81 individuals of L. callistoma were determined and isolated. The basic morphometric characters of 75 of them were measured by an optical microscope “Amplival” (Zeiss-Jena, Germany) at 400X magnification. The isolated specimens were transferred in a drop of glycerol in order to maintain them in a given position during the measurements.

Remaining six specimens were studied by scanning electron microscope (SEM). They were extracted using a glass micropipette, washed several times in distilled water, and then individual shells were positioned with a single-hair brush onto a small drop of Araldite on a previously cleaned standard aluminium stub and air-dried. The shells were coated evenly with gold in a vacuum coating unit. The photomicrographs were obtained using a JEOL JSM-5510, operating at 10 kV.

The biometric description was made according to Schönborn et al. (1983). Frequency distribution analysis was carried out in order to describe variation of characters. Statistical analysis was performed using the computer program STATISTICA, version 7.0 (StatSoft 1999).

 Taxon treatments Lamtopyxis callistoma Bonnet, 1974 Materials

Type status: Other material. Occurrence: recordedBy: Milcho T. Todorov; individualCount: 75; Location: country: Madagascar; stateProvince: Maromizaha Protected Area; verbatimLocality: Central Madagascar, east of the capital Antananarivo and south of the village Anevoka, on the eastern slopes of the Central Highlands; verbatimElevation: 950 m; verbatimLatitude: 18°57'S; verbatimLongitude: 48°27'E; Record Level: collectionID: col:ta;prep.24,25,26/2014; institutionCode: IBER; collectionCode: Testate amoebae

 Description

The shell is yellowish or light brown, circular in oral and dorsal views, and hemispherical in lateral view (Figs 1, 2). The apertural surface is smooth, composed of small to medium flattish mineral particles, bound together by a thick layer of porous and fibrous organic cement, which extends over the teeth (Figs 2a, b, c, 3a). The dorsal surface is rough and composed of bigger and angular pieces of quartz, bound together by considerably less amount of organic cement (Figs 2d, e, f, 3c). The shell wall has a thickness of about 5-6 µm and is composed of three layers: an outer layer of organic cement (300-500 nm) with a smooth outer lining, an intermediate layer of porous and fibrous organic cement (2-4 µm) with incorporated mineral particles and an inner layer of organic cement (1-1.5 µm) with a rough inner lining (Fig. 3e, f). Small single pores with a varying diameter of about 50-350 nm are often seen in the cement, in both on the apertural and dorsal shell surface (Fig. 3b). The aperture is central, deeply invaginated (about 40% of the shell depth), with pronounced apertural tube and two openings - external and internal (Figs 1c, d, 3d, e). The external opening is more often four-, less often three-lobed, bordered by 3-4 large and smooth teeth (Figs 1a, b, 2a, b, c). The internal opening is at the bottom of the apertural tube. It varies in shape from oval to almost circular and is surrounded by a small collar (Figs 1a, 3a). The apertural tube is reinforced at its base by a characteristic dark-brown coloured organic frame (visible by LM, but not by SEM) (Fig. 1a). The apertural tube is rough, composed of a mixture of medium to large mineral particles, bound together by a small amount of organic cement (Fig. 3a, d, e).

 Biometry

The basic morphometric characters of 75 individuals from the Maromizaha Protected Area in Madagascar were measured and the results are given in Table 1. The analysis of the variation coefficients shows that the studied population of L. callistoma is comparatively homogeneous and almost all measured characters are weakly to moderately variable (CV less than 10%). The only exception is the length of the teeth, which varies in a wider range (CV = 12.12%). The parameters with minimal variability are depth of apertural tube (3.37%), depth of shell (3.59%), diameter of shell (4.15%) and diameter at the base of apertural tube (5.32%). The large and small axes of the internal opening are moderate variables (9.20% and 9.13%, respectively). These conclusions are also confirmed by the box plots, showing the variability of the shell’s characters in L. callistoma (Fig. 4).

Analysis of the size frequency distribution of the main characters indicates that L. callistoma is size-monomorphic species. The presence of comparatively well-expressed main-size class for the basic characters and the lack of the subsidiary peaks (bell-shaped curves) indicate a normal distribution (Fig. 5a, b, c). For example, 93% of all the individuals have a shell diameter of 166-190 µm and only 7% are smaller than 165 µm (Fig. 5a). Almost all measured individuals range in close limits, regarding the shell’s depth and diameter at the base of apertural tube (Fig. 5b, c). 98% of them have a diameter at the base of apertural tube between 54-64 µm, and in more than three quarters of the individuals (82%), shell depth varies between 122-134 µm. The average values (Mean ± SD) for these three shell characters are respectively 175.8 ± 7.30 (n=75), 128.1 ± 4.60 (n=43) and 59.8 ± 3.19 (n=75). These arithmetical means correlate with the main-size classes of the characters, and testify for monomorphism of the species.

 Discussion

Until present, data on the ultramorphology and biometry of L. callistoma are almost entirely lacking. In the period from its description to the present time, this species was found only in four countries - Ivory Coast, Papua New Guinea, Philippines and Indonesia (Bonnet 1974, Bonnet 1976, Bonnet 1980a, Bonnet 1980b, Bonnet 1992). Data on the species sizes are given only in its original description. On the basis of measurements of 18 specimens the author gives the next sizes: average shell diameter (Mean ± SD = 175 µm ± 8.1), shell depth (2/3 of the diameter) and apertural invagination (1/3-2/3 of the depth). The morphological data and illustrations of the species are also given only in its original description. In other three publications, where L. callistoma was recorded from Papua New Guinea, Philippines and Indonesia data on the species dimensions and illustrations are not given. However in these papers the author published information on the ecology and biogeography of the species and indicated that it is characteristic inhabitant of the humus of acid forest soils. In the biogeographical aspect, the species has been referred to the association of species of the “Gondwanan-tropical” group of soil testate amoebae. In some other publications (Bonnet 1981a, Bonnet 1981b, Bonnet 1984) discusses mainly the biogeographical and palaeogeographic significance of soil testate amoebae. He also included in these discussions information and illustrations about L. callistoma based on his previous studies. In these publications the author traces the line Cyclopyxis-Lamtopyxis-Distomatopyxis in an evolutionary aspect, emphasizing the trend of flattening on the teeth and reducing of pseudostome. He separated species of the genus Lamtopyxis on the basis of the number of teeth and their flatness, as well as of the shape of the internal apertural opening. In almost all papers the author indicated that L. callistoma is usually with four flattened teeth and oval internal apertural opening. From the foregoing it is seen that data on the morphology and biometry of species are quite scarce, and in fact the illustrations of the species are based mainly on the drawings, except LM photos of ventral surface of L. callistoma given by Bonnet 1979a, Bonnet 1981a.

Biometrical characteristic of the species, based on relatively rich material, was made. In addition to the diameter of the shell, six other shell characters were described biometrically for the first time. Our data for the shell diameter (Mean ± SD) fully corresponds to those given by Bonnet (1974) in the original description of the species (175.8 ± 7.3 (n=75) and 175 ± 8.1 (n=18), respectively). Furthermore, it should be noted that three of the characters measured show high variability (length of teeth, large and small axis of the internal opening). The variability of the last two characters is the reason for the great variability in the shape of the internal opening – from a broad oval to nearly circular.

Surprisingly, our study showed that the population of L. callistoma from Madagascar is comprised of both, specimens with four teeth and specimens with three teeth, in ratio of about 60% to 40%. This largely contradicts to the conclusion of Bonnet, who in most of his works emphasized that this species has four teeth. However, even in the original species description the author pointed at that, though rarely, specimens with five teeth have also occurred. Moreover, in his publication for the soil testate amoebae of Papua New Guinea, Bonnet (1980a) stated that in the populations of L. callistoma and L. cassagnaui specimens with two teeth can be observed very rarely. From the above facts it is seen that the number of teeth cannot be the most reliable taxonomic character for the species separation in the genus Lamtopyxis. Moreover, the individuals with three teeth of the external opening are the most typical and are found in all five species of this genus. Maybe for L. callistoma specimens with 4 teeth are more frequent, but specimens with three, five and rarely two teeth can also be observed. So, the separation of the species must be made on the base of a complex assessment of many characters: diameter and depth of shell; number, structure and shape of the teeth; sizes and shape of internal aperture. In this regard, from the five known species of the genus Lamtopyxis the most distinctive is L. sarocchii, with its largest dimensions (Dm = 278-290 µm) and the structure of the apertural opening which is closer to the genus Cyclopyxis than to genus Lamtopyxis (Coûteaux and Chardez 1981). L. travei has similar sizes as L. callistoma (Dm = 168-171 µm), but differs from the last by its characteristic elongated shape of the internal opening and by less-developed teeth of the external opening (Bonnet 1977b). The other two species – L. cassagnaui and L. trifoliata are characterized by three highly developed, flattened and sometimes nearly touching teeth on the external opening and differ from L. callistoma by significantly smaller dimensions – an average Dm of about 100 µm (Bonnet 1977b, Bonnet 1979a). L. trifoliata has a similar elliptical shape of the internal opening as L. callistoma, while L. cassagnaui differs significantly from all other species of the genus by its triangular shape of the internal opening.

Another interesting feature observed in our SEM studies of L. callistoma is that the thick layer of organic cement, of which the apertural shell surface is composed, extends over the teeth which are made mainly by organic cement. This finding differs from that in the original description of the species, where it is stated that the opening in the base of apertural invagination is surrounded by four large, thickened and rounded “siliceous” teeth.

In respect to the biogeography of L. callistoma it is evident that this is a very rare species of the Gondwanan-tropical group of testate amoebae, which has been found only in soils of tropical forests from countries situated south of the Tropic of Cancer. Despite numerous studies on soil testate amoebae carried out in the Northern Hemisphere, it has never been reported from Europe, North America and Asia. Taking into account the restricted geographical distribution, the large sizes and characteristic apertural morphology of L. callistoma we assume that this species, like some bryophilic ‘Nebelas’ with circumaustral distribution (e.g. Apodera vas, Alocodera cockayni, Certesella certesi, Certesella martiali, etc.), can be used as an example that in free-living microbial eukaryotes ‘not everything is everywhere’.

 Acknowledgements

We are grateful to Prof. B. Georgiev for providing the material used as a basis for this work. We thank the referees and editors for some useful suggestions, which helped to improve this paper.

 References Bonnet L. 1974 Les Lamtopyxidae fam. nov. et la structure propylostome chez les Thécamoebiens (Rhizopoda Testacea) Comptes Rendus de l’Academie des Sciences Paris 278, Série D 2935 2937 French Bonnet L. 1976 Le peuplement thécamoebien édaphique de la Côte-d’Ivoire. Sols de la region de Lamto Protistologica 12 4 539 554 French Bonnet L. 1977 Faunistique et biogéographie des Thécamoebiens. I. Thécamoebiens des sols du Mexique Bulletin de la Société d’Histoire Naturelle de Toulouse 113 40 44 French Bonnet L. 1977 Nouveaux thécamoebiens du sol (IX) Bulletin de la Société d’Histoire Naturelle de Toulouse. 113 152 156 French Bonnet L. 1977 Le peuplement thécamoebien des sols du Nepal et son interet biogéographique Bulletin de la Société d’Histoire Naturelle de Toulouse 113 331 348 French Bonnet L. 1979 Nouveaux thécamoebiens du sol (X) Bulletin de la Société d’Histoire Naturelle de Toulouse 115 106 118 French Bonnet L. 1979 Faunistique et biogéographie des Thécamoebiens. V: Thécamoebiens des quelques sols du Brésil et du Paraguay Bulletin de la Société d’Histoire Naturelle de Toulouse 115 119 122 French Bonnet L. 1980 La faune thécamoebienne des sols de la Nouvelle-Guinee (Paponasie) Bulletin de la Société d’Histoire Naturelle de Toulouse 116 266 276 French Bonnet L. 1980 Faunistique et biogéographie des Thécamoebiens. VI: Thécamoebiens de quelques sols des Philippines Bulletin de la Société d’Histoire Naturelle de Toulouse 116 277 282 French Bonnet L. 1981 Faunistique et biogéographie des Thécamoebiens. VII: Thécamoebiens de quelques sols forestiers de Thaïlande Bulletin de la Société d’Histoire Naturelle de Toulouse 117 245 262 French Bonnet L. 1981 L’intérêt biogéographique du peuplement thécamoebien des sols du Népal Paléogéographie et Biogéographie de l’Himalaya et du sous-continent Indien C.N.R.S. Paris 53-60 French Bonnet L. 1984 Intérêt biogéographique et paléogéographique des Thécamoebiens des sols Annales de la Station Biologique de Besse-en-Chandesse 17 298 334 French Bonnet L. 1985 Faunistique et biogéographie des Thécamoebiens. VIII: Thécamoebiens de quelques sols d’Indonésie Bulletin de la Société d’Histoire Naturelle de Toulouse 121 13 15 French Bonnet L. 1987 Faunistique et biogéographie des Thécamoebiens. IX: Thécamoebiens de quelques sols forestiers de Thaïlande (2ème partie) Bulletin de la Société d’Histoire Naturelle de Toulouse 123 115 121 French Bonnet L. 1992 Faunistique et biogéographie des Thécamoebiens. X: Thécamoebiens de quelques sols d’Indonésie (Deuxième partie) Bulletin de la Société d’Histoire Naturelle de Toulouse 128 21 25 French Coûteaux M. M. Chardez D. 1981 Thécamoebiens edaphiques et muscicoles de Guyane Francaise Revue d'Écologie et de Biologie du Sol 18 193 208 French Golemansky V. Todorov M. 2000 Testate Amoebae (Protozoa: Rhizopoda) from Thailand Acta Protozoologica 39 337 344 Krashevska V. Maraun M. Schoe S. 2010 Micro- and macroscale changes in density and diversity of testate amoebae of tropical montane rain forests of Southern Ecuador Acta Protozoologica 49 17 28 Krashevska Valentyna Bonkowski Michael Maraun Mark Scheu Stefan 2007 Testate amoebae (Protista) of an elevational gradient in the tropical mountain rain forest of Ecuador Pedobiologia 51 4 319 331 10.1016/j.pedobi.2007.05.005 Schönborn W. Foissner W. Meisterfeld R. 1983 Licht- und rasterelektronenmikroskopische Untersuchungen zur Schalenmorphologie und Rassenbildung bodenbewohnender Testaceen (Protozoa: Rhizopoda) sowie Vorschläge zur biometrischen Charakterisierung von Testaceen-Schalen Protistologica 19 4 553 566 German StatSoft Inc. 1999 STATISTICA for Windows – Computer program manual (http://www.statsoft.com)

Light micrographs of L. callistoma from Madagascar.

Ventral view of specimen with three teeth, showing oval internal opening at the bottom of the apertural tube (white arrow) and dark coloured organic frame at the base of the tube (black arrow)

Ventral view of specimen with four teeth

Lateral view of the specimen from Fig. 1a, showing invagination of the apertural tube

Lateral view of the specimen from Fig. 1b, showing invagination of the apertural tube

Scanning electron micrographs of L. callistoma from Madagascar.

Ventral view of specimen with three teeth

Ventral view of other specimen with three teeth

Ventral view of specimen with four teeth

Dorsal view, showing rough dorsal surface of the shell

Lateral view, showing rough dorsal and smooth apertural surface of the shell

Lateral view, showing rough dorsal and smooth apertural surface of the shell

Scanning electron micrographs of L. callistoma from Madagascar.

View of aperture to show the smooth teeth and internal opening with collar (arrowed) on the bottom of the apertural tube

Details of organic cement with single and different sized pores

Dorsal view, showing rough dorsal surface of the shell

Lateral view of fractured shell, showing deep apertural invagination and its rough surface

Lateral view of farctured shell, showing deep apertural invagination and its rough surface

Fractured edge of the shell illustrating the shell structure with smooth outer thin layer of organic cement (large black arrow), intermediate layer of porous and fibrous organic cement (small white arrows) with incorporated mineral particles (small black arrow) and inner thick layer of organic cement (large white arrow)

Variability of the shell characters in L. callistoma (Suppl. material 1).

Diameter of shell, depth of shell, diameter at the base of apertural tube

Depth of apertural tube, large axis of internal opening, small axis of internal opening, length of teeth

Size frequency distribution of the main shell characters in L. callistoma (Suppl. material 1).

Biometrical characterization of Lamtopyxis callistoma: M – median; SD – standard deviation; SE – standard error of the mean; CV – coefficient of variation in %; Min – minimum; Max – maximum; n – number of individuals examined (measurements in μm).

Characters Mean M SD SE CV Min Max n
Diameter of shell 175.8 175.0 7.30 0.84 4.15 159 190 75
Depth of shell 128.1 129.0 4.60 0.70 3.59 118 138 43
Diameter at the base of apertural tube 59.8 60.0 3.19 0.37 5.32 54 67 75
Depth of apertural tube 50.0 50.0 1.69 0.26 3.37 47 55 43
Large axis of internal opening 37.1 38.0 3.41 0.41 9.20 27 43 69
Small axis of internal opening 29.2 30.0 2.67 0.32 9.13 23 36 69
Length of teeth 16.2 16.0 1.97 0.23 12.12 12 23 75

Lamtopyxis callistoma

Data type: Biometry_Stattistica

File: oo_31598.STA

Milcho Todorov