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Biota Neotropica

Print version ISSN 1678-6424On-line version ISSN 1676-0611

Biota Neotrop. vol.15 no.1 Campinas  2015  Epub Jan 30, 2015

https://doi.org/10.1590/1676-06032014004314 

Article

Acanthoceras and Urosolenia species (Diatomeae) in subtropical reservoirs from South Brazil: Ultrastructure, distribution and autoecology

Espécies de Acanthoceras e Urosolenia(Diatomeae) em reservatórios subtropicais do sul do Brasil: ultraestrutura, distribuição e autoecologia

Priscila Izabel Tremarin1  2 

Eduardo Gomes Freire1 

Vanessa Majewski Algarte1 

Thelma Veiga Ludwig1 

1Departamento de Botânica, Universidade Federal do Paraná, Curitiba, PR, Brazil


ABSTRACT

Acanthoceras Honigmann and Urosolenia Round & Crawford emend. Rott, Kling & McGregor species were studied based on samples of 19 hydroelectric power plants reservoirs located in the State of Paraná, Southern Brazil. Autoecological informations of Urosolenia species complement the study. One Acanthoceras and four Urosolenia species were identified: A. zachariasii (Brun) Simonsen, U. amazonica Sala, Núãez-Avellaneda & Vouilloud, U. eriensis var. morsa (West & G.S.West) Bukhtiyarova, U. longiseta Zacharias and U. obesa Freire, Tremarin & Ludwig. Morphological variation of frustules was described and illustrated by optical and scanning electron microscopy, and compared with similar species such as U. delicatissima Sala, Núãez-Avellaneda & Vouilloud and U. eriensis var. eriensis (H.L.Smith) Round & Crawford. The pioneer record of U. amazonica to Brazil and unprecedent details of the ultrastructure of A. zachariasii and U. longiseta are included in this study. Cellular densities differed among evaluated reservoirs showing strong correlations with inorganic nitrogen concentrations, N/P ratio and temperature. The results suggested higher densities in periods of warmer temperatures and low availability of the nitrogen compounds and confirmed that species respond strongly to local environmental gradients.

Key words: centric diatom; lentic environments; State of Paraná; taxonomy

RESUMO

Espécies de Acanthoceras Honigmann e Urosolenia Round & Crawford emend.Rott, Kling & McGregor foram estudadas com base em amostras provenientes de 19 reservatórios de usinas hidrelétricas do estado do Paraná, sul do Brasil. Informações sobre a autoecologia das espécies de Urosolenia complementam o estudo. Uma espécie de Acanthoceras e quatro de Urosolenia foram identificadas: A. zachariasii (Brun) Simonsen, U. amazonica Sala, Núãez-Avellaneda & Vouilloud, U. eriensis var. morsa (West & G.S.West) Bukhtiyarova, U. longiseta Zacharias e U. obesa Freire, Tremarin & Ludwig. A variação morfológica das frústulas foi descrita e ilustrada através de microscopia óptica e eletrônica de varredura e comparada com a de espécies similares, como U. delicatissima Sala, Núãez-Avellaneda & Vouilloud e U. eriensis var. eriensis(H.L.Smith) Round & Crawford. O registro pioneiro de U. amazonica para o Brasil e detalhes inéditos da ultraestrutura de A. zachariasii e U. longisetaestão contemplados neste estudo. As densidades celulares diferiram entre os reservatórios avaliados e mostraram forte correlação com concentrações de nitrogênio inorgânico, relação N/P e temperatura. Os resultados sugeriram densidades mais elevadas em períodos de temperaturas mais quentes e baixa disponibilidade de compostos nitrogenados e confirmaram que as espécies respondem fortemente aos gradientes ambientais locais.

Palavras-Chave: ambientes lênticos; diatomácea cêntrica; estado do Paraná; taxonomia

Introduction

Acanthoceras Honigmann and UrosoleniaRound & Crawford emend. Rott, Kling & McGregor are centric diatoms worldwide distributed, occurring primarily in plankton of lentic environments (Rott et al. 2006). These genera are mainly characterized by having open girdle bands, cylindrical or subcylindrical frustules, conical to semi-conical valves ornamented or not, calyptra and the presence or not of the seta (Round et al. 1990, Rott et al. 2006). The valves of Acanthoceras presents two calyptra while Urosolenia have only one (Round et al. 1990).

Detailed research on Acanthoceras and Urosoleniataxa is difficult to realize due to weakly silicified frustules, which are often destroyed by the usual techniques of cleaning and preservation. This fact may be the reason of so scarce records of these genera. Scanning and transmission electron microscopies have been useful and often essential to distinguish among species, since they enable the visualization of structures indistinguishable in optical microscopy (Morales 2005). Accordingly, identifications of some species performed only with light microscopy should be reviewed (Rott et al. 2006).

Recent studies on Acanthoceras and Urosolenia were developed by Rott et al. (2006), Sala et al. (2008), Li et al. (2009), Karthick & Kociołek (2011) and Tremarin et al. (2013), with descriptions of eight new species and some new combinations.

Brazilian surveys have found Acanthoceras zachariasii(Brun) Simonsen and five taxa of Urosolenia: U. brauni(Hustedt ) Rott & Kling, U. longiseta (Zacharias) Edlund & Stoermer, U. eriensis (H.L.Smith) Round & Crawford var. eriensis, U. eriensis var. morsa (West & G.S West) Bukhtiyarova and U. obesa Freire, Tremarin & Ludwig (Torgan et al. 1999, Rott et al. 2006, Melo et al. 2004, Raupp et al. 2009, Tremarin et al. 2009, Silva et al. 2011, Eskinazi-Leça et al. 2012, Tremarin et al. 2013). Informations about the ultrastructure of Urosolenia species found in Brazil are not routinely added to the studies, except for Torgan & Becker (1998) who described the morphology of U. eriensis var. morsa, and Tremarin et al. (2013) when proposed U. obesa.

According to Reynolds et al. (2002), Urosolenia are included within functional A-group (centric diatoms) characterized by preferring lakes with clear and often well-mixed water, tolerating nutrients deficiency. Representatives of the genus were detected in shallow Amazonian high-waters stages. In Brazilian subtropical reservoirs, Urosolenia species occurred in winter mixed waters (Silva et al. 2005). Ramberg (1987) found A. zachariasii and U. eriensis during stratification of water column, both disappearing in the mixing period. Edlund & Stoermer (1993) remark that Acanthoceras is largely distributed and may be found in alcalin, shallow and eutrophic lakes and rivers from Norh America. Urosolenia may occur in highly diverse habitats and in oligotrophic to eutrophic conditions.

Thus, this study aimed to describe the morphology and expand the geographic distribution of Acanthoceras and Urosoleniaspecies that occurred in plankton from hydropower plants reservoirs in the State of Paraná, Southern Brazil. Also, we identified the environmental factors closer correlated with Urosolenia species densities.

Material and methods

For the taxonomic analysis, samplings were carried out quarterly at 19 hydroelectric power plants reservoirs from the State of Paraná, Southern Brazil (Figure 1, Table 1), over four consecutive years (2007-2010), at subsurface (≅ 30 cm depth) and at the limit of the photic zone. A total of 768 phytoplanktonic samples were collected with a van Dorn sampler and were preserved with Lugol’s iodine acetic solution (1%) (Bicudo & Menezes 2006). The material was washed with distilled water to prepare permanent slides mounted with Naphrax¯ (R.I. = 1.74). The specimens found were measured and photographed under Olympus BX40 light microscopy (LM) equipped with Olympus DP71 image capture, using phase contrast (1000x). Some of the material was dried on aluminum stubs and covered with gold and studied using a JEOL JSM 6360LV scanning electron microscopy (SEM), operated at 15 kV and 8 mm working distance, at the Electron Microscopy Center of the Universidade Federal do Paraná. Analyzed samples (2007-2010) were stored in the Herbarium of the Universidade Federal do Paraná (UPCB). The terminology used in the description of species was based on Round et al. (1990)and Rott et al. (2006).

Figure 1 Sampling locations in the State of Paraná, Brazil. Hydroelectric power plants reservoirs: 01- Capivari, 02- Marumbi, 03- São Jorge, 04- Pitangui, 05- Apucaraninha, 06- Mourão, 07- Melissa, 08- Rio dos Patos, 09- Chopim, 10- Cavernoso, 11- Segredo, 12- Foz do Areia, 13- Salto do Vau, 14- Jordão, 15- Chaminé, 16- Guaricana, 17- Fundão, 18- Santa Clara, 19- Salto Caxias. 

Table 1 Data of the sampling sites in the State of Paraná and register number in the herbarium of Universidade Federal do Paraná (UPCB). 

Reservoir Station UPCB/Date Municipality Geographic coordinates
Apucaraninha E2 69524-2007; 60508-2008; 68842-2009; 68866-2010 Tamarana 23°44′56-S/50°56′33-W
Capivari E2 59525-2007; 60509-2008; 68843-2009; 68867-2010 Antonina 24°59′10-S/48°47′20-W
Cavernoso E2 59526-2007; 60510-2008; 68844-2009; 68868-2010 Virmond 25°23′49-S/52°11′24-W
Chaminé E2 59527-2007; 60511-2008; 68845-2009; 68869-2010 São José dos Pinhais 25°41′36-S/49°01′14-W
E4 59528-2007; 60512-2008; 68846-2009; 68870-2010
Chopim E2 59529-2007; 60513-2008; 68847-2009; 68871-2010 Itapejara d’Oeste 25°53′26-S/52°43′05-W
Foz do Areia E2 59530-2007; 60514-2008; 68848-2009; 68872-2010 Pinhão 26°03′39-S/51°30′09-W
E3 59531-2007; 60515-2008; 68849-2009; 68873-2010
E5 59532-2007; 60516-2008; 68850-2009; 68874-2010
Fundão E3 65977-2008; 68864-2009; 68888-2010 Candói 25°32′04-S/51°48′55-W
Guaricana E2 59533-2007; 60517-2008; 68851-2009; 68875-2010 Guaratuba 25°42′31-S/48°58′18-W
Jordão E2 59534-2007; 60518-2008; 68852-2009; 68876-2010 Reserva do Iguaçu 25°45′14-S/52°04′54-W
Marumbi E2 68865-2009; 68889-2010 Morretes 25°25′35-S/48°55′44-W
Melissa E2 59535-2007; 60519-2008; 68853-2009; 68877-2010 Corbélia 24°32′12"S/53°12′28"W
Mourão E2 59536-2007; 60520-2008; 68854-2009; 68878-2010 Campo Mourão 24°06′20"S/52°19′42"W
Pitangui E2 59537-2007; 60521-2008; 68855-2009; 68879-2010 Ponta Grossa 25°01′41"S/50°06′06"W
Rio dos Patos E2 59538-2007; 60522-2008; 68856-2009; 68880-2010 Prudentópolis 25°10′37"S/50°56′29"W
Salto Caxias E3 59539-2007; 60523-2008; 68857-2009; 68881-2010 Capitão Leônidas Marques 25°32′43"S/ 53°06′05"W
E5 59540-2007; 60524-2008; 68858-2009; 68882-2010
Salto do Vau E2 59541-2007; 60525-2008; 68859-2009; 68883-2010 União da Vitória 25°58′50"S/51°43′14"W
Santa Clara E3 65976-2008; 68863-2009; 68887-2010 Candói 25°39′14"S/51°54′26"W
São Jorge E2 59542-2007; 60526-2008; 68860-2009; 68884-2010 Ponta Grossa 24°59′45-S/49°59′39-W
Segredo E2 59543-2007; 60527-2008; 68861-2009; 68885-2010 Mangueirinha 26°00′47-S/51°52′43-W
E3 59544-2007; 60528-2008; 68862-2009; 68886-2010

Source: Ribeiro et al. (2006).

For the quantitative and ecological analysis, samplings were carried out quarterly over six consecutive years (2007-2012). Urosolenia quantification was performed in Ütermohl’ chambers (1958) under Olympus IX70 inverted microscope at a magnification of 600 x, enumerated in random fields (Uhelinger 1964) and followed the stabilization curve of the number of species. Sedimentation time of the samples was carried out according to Lund et al. (1958). The physical and chemical analyses (Table 2) were performed by the technical staff of the Instituto de Tecnologia para o Desenvolvimento (LACTEC) following the Standard Methods (APHA 1989).

Table 2 Physical and chemical characteristics of the sampling stations (mean values among sampling periods). 

Apucaraninha(n=4) Capivari (n=3) Chaminé(n=20) Fundão (n=4) Guaricana(n=20) Jordão(n=10) Mourão (n=9) Pitangui (n=18) Rio dos Patos(n=6) Salto Caxias (n=2) Santa Clara (n=6) Segredo (n=14) São Jorge (n=14)
Dam depth 9.75 13 13.5 38.5 8.06 58.6 12.11 2.86 3.5 56.5 43.83 46.25 7.6
Secchi (m) 1.66 2.36 1.84 1.37 1.41 1.52 1.37 0.74 0.41 2.1 1.47 1.44 0.84
Water temperature (°C) 20.1 19.13 20.99 23.68 20.58 22.06 22.66 19.25 17.75 20.25 24.06 20.65 20.88
Dissolved oxygen (mg.L-1) 7.6 5.16 6.9 7.9 8.19 6.68 6.49 7.47 7.21 7.8 7.67 6.58 7.24
pH 7.32 7.4 7.66 7.25 7.52 6.89 7.37 7.52 7.13 7.35 7.25 7.17 7.89
Conductivity (µS.cm-1) 31.75 70.33 43.12 28.75 25.75 26.7 26.88 48.05 51.5 44.5 31.16 49.14 51.5
Total phosphorus (mg.L-1) 0.015 0.013 0.017 0.02 0.024 0.015 0.015 0.043 0.061 0.015 0.018 0.024 0.034
N-NO3-(mg.L-1) 0.097 0.263 0.091 0.37 0.088 0.414 0.186 0.157 0.575 0.67 0.355 0.745 0.097
Total inorganic nitrogen (mg.L-1) 0.2 0.393 0.21 0.482 0.189 0.525 0.295 0.31 0.763 0.78 0.468 0.858 0.192
Total Nitrogen (mg.L-1) 0.762 1.45 0.875 0.662 0.82 0.99 0.916 0.816 1.52 2.3 0.825 1.182 0.73
Turbidity (NTU) 6.25 3 3.25 6.75 4.4 5.9 9.44 9.61 26.16 6.5 5.5 7.57 10.65
N/P Ratio 129.6 231.7 146.9 94.7 98.07 171.8 185.3 46.19 56.8 463.5 128.7 120.5 58
Water retention time 14 107 121 4 12 10 53 2 2 31 48 45 43
Classification lentic-lotic lentic lentic lotic lentic-lotic lentic-lotic lentic lotic lotic lentic-lotic lentic lentic lentic

Environmental data were summarized by a principal component analysis (PCA, Legendre & Legendre 1998) with log transformed and standardized variables. The selection of the axes for the interpretation of the results followed the Broken Stick criteria (Jackson 1993). Spearman rank correlation coefficients were used to measure the degree of association between the densities of Urosolenia amazonica, U. longiseta and U. obesa and abiotic variables. The relationship between the environmental variables and the density of three species of Urosolenia was evaluated by means of stepwise multiple regression analysis. The method consists of starting with a single predictor variable and then adding variables one at a time until the addition of further variables does not produce an appreciable increase in the coefficient of determination (Sokal & Rohlf 1981). Except for pH, other variables were log-transformed. Data distribution and multicollinearity among the abiotic factors were checked before performing the analysis (Zar 2010). The principal component analysis (PCA), Spearman correlations and multiple regressions were carried out respectively using PC-ORD (McCune & Mefford 1999) and STATISTICA (StatSoft 2005).

The autoecology of Urosolenia species was performed with the taxa that present densities >3 cells.mL-1 in the quantitative analysis (U. amazonica, U. longisetaand U. obesa) and only with reservoirs that have had regular sampling of physical and chemical data.

Results and discussion

Five taxa were identified in the qualitative analysis: A. zachariasii, U. amazonica, U. eriensis var. morsa, U. longiseta and U. obesa. The taxa occurred in 15 of the 19 reservoirs (except for Cavernoso, Chopim, Marumbi and Melissa reservoirs). Specimens of Acanthoceras and Urosolenia were registered in 12% of analyzed samples, being Urosolenia amazonicapresent in 87% of these samples, followed by U. obesa(80%), U. longiseta (60%), U. eriensis var. morsa (16%) and A. zachariasii (10%).

Acanthoceras zachariasii (Brun) Simonsen, Bacillaria 2: 55, 1979.

Basionym: Attheya zachariasii Brun, Forschungsberichte aus der Biologischen Station zu Plön 2: 53, pl. 1, fig. 11, 1894.

Figure 2–5 5. Acanthoceras zachariasii. LM. Scale: 10 µm. 

Figure 6–11 11.Acanthoceras zachariasii. SEM. Figs 6-7. Valve surface. Scales: 2 µm. Fig. 8. Girdle bands in the median region of frustule. Scale: 2 µm. Figs 9-11. Teeth of the calyptra. Scales: 1 µm. 

Synonyms: Acanthoceras magdeburgense Honigmann, Archiv für Hydrobiologie und Planktonkunde 5: 77, pl. 2, fig. a, 1910.

Acanthoceras magdeburgense var. lataHonigmann, Archiv für Hydrobiologie und Planktonkunde 5: 78, pl. 2, fig. b, 1910.

Rhizosolenia eriensis var. zachariasii(Brun) Playfair, Proceedings of the Linnean Society of New South Wales 37(3): p. 538; pl. 56, fig. 33-35, 1913.

Frustules solitary, subcylindrical, straight, 56.5-73.4 µm total long, 6.1-13.5 µm width (Figures 2-5). Valve face straight with conical apices, ornamented with round to irregular areolae, 50-55 in 10 µm, arranged in rows and extending onto the calyptra base (Figures 6, 7). Valve mantle edge surrounded by a thin hyaline margin (Figure 7). Calyptra straight, positioned in the valve apices, 14.9-17.8 µm long, positioned at right to strongly oblique angle with the pervalvar axis. Tip of spine-like extension with four small teeth (Figures 9-11). Terminal seta not observed. Cingulum with several semi-circular open and narrow bands, 9-14 in 10 µm, perforated by round poroids, ca. 7 in 1 µm (Figure 8). Bands of the median region of frustule perforated by a few poroids, scarcely distributed. Coarser rounded pores, varying in size and number, present on the girdle bands (Figure 8). Two to four discoid to plate-like chloroplasts per cell (Figures 2-5).

The genus Acanthoceras was proposed by Honigmann (1910) when describing A. magdeburgense Honigmann, a later synonym of Attheya zachariasii Brun. The name Acanthoceras had already been proposed by Kützing (1842) for a red alga genus currently considered a later homonym of CeramiumRoth (Edlund & Wynne 1996). Since the name Acanthoceras Kützing was not in use and that Acanthoceras Honigmann was reported for a diatom, Edlund & Wynne (1996) suggested the conservation of the name Acanthoceras that was recommended by the Committee for Algae (see Compàre 1999).

Although the ultrastructure of Acanthoceras zachariasiihas been illustrated and described by Round et al. (1990) and the morphology of its resting spores analyzed by Edlund & Stoermer (1993), some taxonomically important details on the frustule morphology of this species remained unknown. The number of calyptra teeth and density of poroids in the girdle bands are recorded for the first time in this study.

The specimens of Acanthoceras zachariasii from Brazilian reservoirs showed smaller individuals than the type material of the species, but they were similar to other studied specimens, with intermediate sizes, as can be seen on Table 3. The Brazilian material has smaller calyptra length and higher number of girdle bands when compared with materials analyzed by Huber-Pestalozzi (1942), Rivera (1974), Shirata & Valente-Moreira (1987) and Ferrario et al. (1992) (Table 3). There are few records of the metric variation of A. zachariasii.Rivera (1974) remarked that the number of bands is not a constant feature in A. zachariasii, so we believe that the specimens analyzed in our study represent an extreme of the population and would not justify the proposition of a new taxon. Anyway, it is necessary to analyze the type material of A. zachariasii, especially in SEM, to study the fine ornamentation of the frustules (ex. calyptra teeth, details of the valve, calyptra and bands), for comparison among different populations. However, we advise on this difficult task, given the frequent and fast disappearing of Acanthocerasindividuals in the stored samples. The low silicified frustules of Acanthoceras, as well as Urosolenia, do not resist long time in chemical preserved samples (Tremarin et al. 2013).

Table 3 Morphometric features of Acanthoceras zachariasiivar. zachariasii and A. zachariasiivar. curvata. 

A. zachariasiivar. zachariasii A. zachariasii var. curvata
Reference this study Brun (1874) Huber-Pestalozzi (1942) Rivera (1974) Shirata & Valente-Moreira (1987) Ferrario et al. (1992) Rivera (1974)
Total frustule length (µm) 56.5-73.4 ... 12-100 ... ... ... ...
Frustule length (µm) 29.1-39.7 60-100 ... 42-86 31-45.6 20-36 43-90
Frustule width (µm) 6.1-13.5 15-20 15-25 8.5-17 9.7-18.1 11-12 8-11
Calyptra length (µm) 14.9-17.8 40-70 24-32 18.6-30.1 20-25 20-30
Girdle bands (in 10 µm) 9-14 3.4-4 4-6 4-4.5 4.5-5
Porous of the bands (in 1 µm) 7 ... ... ... ... ... ...
Teeth of the calyptra 4 ... ... ... ... ... ...
Country Brazil Germany Switzerland and Germany Chile Brazil Argentina Chile

The species has only one variety, Acanthoceras zachariasii var. curvata Rivera, proposed by Rivera (1974)based on the frustule curvature in relation to the pervalvar axis.

Acanthoceras zachariasii is a freshwater taxon, worldwide distributed, recorded to Germany, Australia, Switzerland, Sweden, Finland, Russia, United States, Chile, Argentina and Brazil (Brun 1874, Hustedt 1930, Cleve-Euler 1951, Rivera 1974, Shirata & Valente-Moreira 1987, Ferrario et al. 1992, Edlund & Stoermer 1993, Medvedeva et al. 2009).

Occurrence in samples (UPCB) - São Jorge reservoir 68884; Pitangui reservoir 68879.

Urosolenia amazonica Sala, Núãez-Avellaneda & Vouilloud, Diatom Research 23(1): 164, pl. 1, figs 1-9, 2008.

Frustules solitary or in pairs, cylindrical, straight, 78-194 µm total long, 7.2-12.8 µm width (Figures 12-19). Valve face conical, 2.4-5.4 length, ornamented with rounded areolae 7-9 in 1 µm, randomly arranged and extending onto the calyptra base (Figures 20-22). Valve mantle edge surrounded by a thin hyaline margin (Figures 21, 22). Calyptra straight and eccentric, 24.8-38.2 µm long, positioned at right to slightly oblique angle with the pervalvar axis. Tip of spine-like extension with 4-6 small teeth (Figures 23-26). Terminal seta not observed. Cingulum with several semi-circular open and narrow bands, 8-11 in 10 µm, perforated by round poroids, ca. 7-10 in 1 µm (Figure 27). Valvocopula wider than the other bands, with poroids irregularly distributed and serrated margin (Figures 20, 22).

Figure 12–19 19.Urosolenia amazonica, LM. Scale: 10 µm. 

Figure 20–27 27.Urosolenia amazonica, SEM, external view. Fig. 20. Aspect of valve and the insertion site of the calyptra of adjacent cell. Scale: 1 µm. Figs 21, 22. Overview of valve. Note the serrated valvocopulae. Scales: 1 µm. Figs 23-26. Detail of calyptra teeth. Scales: 1 µm. Fig. 27. Detail of girdle bands showing the poroids and imbrication line in the median region of frustule. Scale: 1 µm. 

Figure 28–31 31.Urosolenia eriensis var. morsa, LM. Scale: 10 µm. 

Figure 32–38 38.Urosolenia eriensis var. morsa, SEM. Fig. 32. External view of frustule showing the insertion site of the calyptra of adjacent cell. Scale: 2 µm. Figs 33, 34. Aspect of valve in external view and valvocopulae. Scales: 1 µm and 2 µm, respectively. Fig. 35. Detail of girdle bands showing the poroids and imbrication line. Scale: 1 µm. Figs 36-38. Detail of calyptra teeth. Scales: 1 µm. 

Urosolenia amazonica is similar to U. eriensis var. eriensis, mainly by the dimensions and shape of frustules, but differs by higher number of girdle bands and valvocopula with serrate margin (Table 4) (Huber-Pestalozzi 1942, Krammer & Lange-Bertalot 1991, Sala et al. 2008). The absence of more detailed features of U. eriensis var. eriensis, as number of calyptra teeth, calyptra length and density of poroids in the bands, difficult a more precise comparison between the two species.

Table 4 Morphometric and morphological variation of Urosolenia amazonica and related taxa. 

U. amazonica U. erienses var. eriensis U. eriensis var. morsa
Reference this study Sala et al. (2008) Krammer & Lange- Bertalot (1991) Huber-Pestalozzi (1942) Huber-Pestalozzi (1942), Krammer & Lange-Bertalot (1991) Torgan & Becker (1998)
Total frustule length (µm) 78-194 76-120 40-150 40-150 80-135*
Frustule width (µm) 7.2-12.8 6-18 6-15 6-15 5-20 6.0-12.0
Frustule length (µm) 32.8-118.8 40-68 40-84
Girdle bands (in 10 µm) 8-11 8-16 3-4 3-4 6-9 5-10(12)
Porous in the bands (in 1 µm) 7-10 7-14 7-9
Calyptra length (µm) 24.8-38.2 27-48 28-38 22-36 22-45
Valve length (µm) 2.4-5.4 3-9.5 2-15 5-20 6-12
Teeth in the calyptra 4-6 4-6 2+ligula*
Valvocopula serrate serrate smooth*

data measured or observed in the illustrations.

Urosolenia eriensis var. morsa is very similar to U. amazonica in light microscopy. However, the former may have larger valves and valvocopulae with smooth edge (Huber-Pestalozzi 1942, Krammer & Lange-Bertalot 1991, Torgan & Becker 1998). Furthermore, Urosolenia eriensis var. morsa have three teeth in the calyptra as documented by Torgan & Becker (1998) (Table 4). We believe that some Brazilian exemplars recorded as U. eriensis var. morsa in previous studies may be U. amazonica, due to the similarities between the species in light microscopy.

We found some exemplars of U. amazonica with longer total length of frustule and smaller valve length than that reported by Sala et al. (2008) (Table 4), but the valvocopulae serrate and calyptra teeth were always present in the observed specimens.

Urosolenia amazonica was proposed based on material from the Colombian and Peruvian Amazon (Sala et al. 2008), with no subsequent records. Thus, this is the first citation of the species in Brazil.

Occurrence in samples (UPCB) - Apucaraninha reservoir 59524, 60508, 68842; Guaricana reservoir 59533, 60517, 68875, 68875; São Jorge reservoir 59542, 60526, 68860, 68884; Pitangui reservoir 59537, 60521, 68855, 68879; Fundão reservoir 68864, 68888; Foz do Areia reservoir 60515, 60516, 60517, 68872, 68874; Santa Clara reservoir 68863, 68887; Jordão reservoir 59520, 68852, 68876; Segredo reservoir 59543, 59544, 60527, 60528, 68861, 68862, 68885, 68886; Salto Caxias reservoir 68857, 68858, 68881, 68882; Mourão reservoir 59536, 60520, 68854; Chaminé reservoir 59527, 59528, 60511, 60512, 68845, 68846, 68869, 68870; Rio dos Patos reservoir 68856, 68880.

Urosolenia eriensis var. morsa (West & G. S. West) Bukhtiyarova, Algologia 5(4): 417, 1995.

Basionym: Rhizosolenia eriensis var. morsa W. & G. S. West, Transactions of the Royal Society of Edinburgh 41(3): 509, pl. 6, fig. 23, 1905.

Synonyms: Rhizosolenia morsa (W. & G. S. West) W. & G.S. West, Transactions of the Royal Irish Academy 33: 109, pl. 11, fig. 5, 1906.

Urosolenia eriensis var. morsa (W. West & G. S. West) Torgan in Torgan & Becker, Iheringia, Série Botânica 50: 90; figs 2-9, 1998.

Frustules solitary or in pairs, cylindrical, straight, 73.1-143.4 µm total long, 6.9-20.3 µm width (Figures 28-31). Valve face conical, 3.8-7.6 length, ornamented with rounded areolae 7-10 in 1 µm, randomly arranged and extending onto the calyptra base (Figures 32-34). Valve mantle edge surrounded by a thin hyaline margin (Figure 33, 34). Calyptra straight and eccentric, 22.4-35.5 µm long, positioned at right to slightly oblique angle with the pervalvar axis. Tip of calyptra with 2-3 small teeth and one ligula (Figures 36-38). Terminal seta not observed. Cingulum with several semi-circular open and narrow bands, 7-11(18) in 10 µm, perforated by round poroids, ca. 8-9 in 1 µm (Figure 35). Valvocopula wider than the other bands, with poroids irregularly distributed and smooth margin (Figures 32, 34).

The ultrastructure of U. eriensis var. morsa was documented by Torgan & Becker (1998), based on samples from Patos lagoon, Southern Brazil. The illustrations show the similarities with the material from the State of Paraná, except by the number of teeth in the calyptra apex. We found exemplars with 2 or 3 teeth and one ligula, while Torgan & Becker (1998)recorded only 2 teeth and the ligula.

Urosolenia eriensis var. morsa differs from the typical variety of species by higher number of girdle bands (Table 4) (Huber-Pestalozzi 1942, Krammer & Lange-Bertalot 1991, Torgan & Becker 1998). Urosolenia eriensisvar. morsa was found in countries such as Britain, New Zealand, Russia and Brazil (Medvedeva et al. 2009, Tremarin et al. 2009, Guiry & Guiry 2014).

Few specimens of U. eriensis var. morsawere found in Brazilian reservoirs samples, and occur together with U. amazonica.

Occurrence in samples (UPCB) - Chaminé reservoir 68845, 68846; Guaricana reservoir 59533; São Jorge reservoir 60526.

Urosolenia longiseta (Zacharias) Edlund & Stoermer, Journal of Paleolimnology 9(1): 59, pl. 1, figs 5-6, 1993.

Basionym: Rhizosolenia longiseta Zacharias, Forschungsberichte aus der Biologischen Station zu Plön 1: 38; fig. 7, 1893.

Synonym: Urosolenia longiseta (Zacharias) Bukhtiyarova, Algologia 5(4): 417, 1995.

Frustules solitary, cylindrical, straight to slightly curved, 216-273 µm total long, 5.8-8.5 µm width (Figures 39-46). Valve face conical, 2.4-5.4 µm length, ornamented with rounded to elongate areolae, 6-8 in 1 µm, arranged in almost linear pattern and extending onto the calyptra base (Figures 47, 48). Valve mantle edge surrounded by a thin hyaline margin (Figure 47). Calyptra straight and central, 64-100 µm long, positioned at right to slightly oblique angle with the pervalvar axis. Tip of calyptra with 3-4 small teeth (Figures 51-55). Terminal seta long (Figure 56). Cingulum with several semi-circular open and large bands, 3-4 in 10 µm, perforated by elongate poroids, ca. 7-8 in 1 µm (Figures 49, 50).

Figure 39-46 Urosolenia longiseta, LM. Scale: 10 µm. 

Figure 47-56 Urosolenia longiseta, SEM. Figs 47, 48. External and internal view of valve, respectively. Scales: 1 µm. Fig. 49. Girdle bands in the median region of frustule. Scale: 1 µm. Fig. 50. Detail of bands showing the poroids and imbrication line. Scale: 1 µm. Figs 51-55. Detail of calyptra teeth. Scales: 1 µm. Fig. 56. Seta in the calyptra. Scale: 1 µm. 

When proposed Rhizosolenia longiseta, Zacharias (1893) provided only the length of frustule and calyptra (Table 5). Additional, but limited to light microscopy information on the morphology and metric limits was subsequently reported for this species (ex. Krammer & Lange-Bertalot 1991; Huber-Pestalozzi 1942). The failure to record the frustules details of U. longiseta type material has hampered the comparison of this species with populations from different regions of the world and similar taxa. Attempts to analyze a sample of Rhizosolenia longiseta studied by Zacharias from Schleswig-Holstein, Germany (material number E4347-Hustedt Diatom Collection) failed, because complete frustules were not found. Valves poorly preserved and the lack of integrity of the calyptra did not allow to observe the number and morphology of apical teeth.

Table 5 Metric and morphological variation of Urosolenia longiseta and related species. 

U. longiseta U. delicatissima U. extensa
Reference this study Zacharias (1893) Zacharias (1898) Huber-Pestalozzi (1942) Krammer & Lange-Bertalot (1991) Cleve-Euler (1951) Sala et al. (2008) Li et al. (2009) Karthick & Kociolek (2011)
Total frustule length (µm) 216-273 70-200 40-200 134-280 >179 200-400
Frustule width (µm) 5.8-8.5 4-10 4-10 5-14 3-10 3-10 3,2-5,1
Frustule length (µm) 59-103 160 77-176
Girdle bands(in 10 µm) 3-4 2-3 2.3-4.5 (3)4-7 5-7 5-7
Porous in the bands (in 1 µm) 7-8 6-9
Calyptra length (µm) 64-100 180-200 58-154 90-170 44-99 55-115 15.4-44.4
Valve length (µm) 2.4-5.4 2.3-7.5 3-8 5-7
Teeth in the calyptra 3-4

Our specimens of Urosolenia longiseta had smaller frustules and shorter calyptra than those described by Zacharias (1893), Huber-Pestalozzi (1942)and Krammer & Lange-Bertalot (1991)(Table 5). The metric variation recorded was more related to that cited by Zacharias (1898) and Cleve-Euler (1951).

The ultrastructure of Urosolenia longiseta is still poorly known. Only the morphology of its resting spores was well studied by Edlund & Stoermer (1993). Thus, the number and morphology of the calyptra teeth and the areolation pattern of the valves and girdle bands of U. longiseta are recorded for the first time in this study.

The frustules of U. delicatissima Sala, Núãez-Avellaneda & Vouilloud and U. extensa Karthick & Kociolek are very similar to U. longiseta. However, U. delicatissimadiffers mainly by having a bottom, a large labiate-shaped perforation on the valve (Sala et al. 2008). Furthermore, this species may have longer frustules and higher number of bands (Table 5) (Sala et al. 2008, Li et al. 2009). Urosolenia extensa have elongate openings in the valve, greater number of girdle bands, longer valves, higher density of areolae (8-9 in 1 µm) and shorter calyptra than that U. longiseta (Table 5) (Karthick & Kociolek 2011).

Urosolenia longiseta have a worldwide distribution, recorded in Britain, Ireland, North America, New Zealand, Russia, Germany and Brazil (Krammer & Lange-Bertalot 1991, Medvedeva et al. 2009, Tremarin et al. 2009, Guiry & Guiry 2014).

Occurrence in samples (UPCB) - Guaricana reservoir 59533, 60517, 68851, 68875; São Jorge reservoir 59534, 60526, 68852, 68884; Pitangui reservoir 68855, 68879; Fundão reservoir 68864; Foz do Areia reservoir 59530, 60514, 60515, 60516, 68872; Segredo reservoir 59543, 60527, 68861, 68862, 68885; Salto Caxias reservoir 68857; Chaminé reservoir 59527, 60511, 60512, 68845, 68846; Jordão reservoir 59520, 68852; Santa Clara reservoir 68863.

Urosolenia obesa Freire, Tremarin & Ludwig, Phytotaxa 125(1): 1-9, figs 2-27, 2013.

Frustules solitary, subcylindrical, straight to slightly curved, 27.6-55.2 µm total long, 6.8-14.2 µm width (Figures 57-61). Valve face conical ornamented with rounded to irregular areolae, 8-10 in 1 µm, randomly arranged and extending onto the calyptra base (Figure 62). Valve mantle edge surrounded by a thin hyaline margin. Calyptra straight and eccentric, 9.7-15.9 µm long, positioned at right to strongly oblique angle with the pervalvar axis. Calyptra in variable position to the frustules (Figures 57-61). Calyptra ornamented by irregular rib-like structures that extend from base until the median portion of this valve projection (Figure 62). Tip of calyptra with 2 small teeth and a central ligula (Figure 63). Terminal seta not observed. Cingulum with several semi-circular open and narrow bands, 13-16 in 10 µm, perforated by round poroids, ca. 10-11 in 1 µm. Coarser rounded pores, varying in size and number, present on both sides of the cingulum (Figure 62). Resting spore subcylindrical, with convex/concave wall, smooth, 5.4-6.5 µm long and 10.1-13.5 µm width (Figure 57).

Figure 57–61 61.Urosolenia obesa, LM. Scale: 10 µm. Figures 62-63. Urosolenia obesa, SEM. Fig. 62. External view of frustule showing the ornamentation of the valve and girdle bands. Scale: 2 µm. Fig. 63. Detail of calyptra teeth. Scale: 1 µm. 

Urosolenia obesa is a small and delicate taxa recently proposed to South Brazil. Details of frustule morphology and some ecological data of this species were reported by Tremarin et al. (2013) that proposed this taxon. At present, the species was only found in reservoirs of State of Paraná.

Figure 64 Reservoirs scores (A) derived from principal component analysis and Pearson correlation (B) between the original variables and ordination scores [COND (conductivity); N_INOR (total inorganic nitrogen), NO3 (nitrate), NT (total nitrogen), N/P ratio (N/P molar), DO (dissolved oxygen), PT (total phosphorus), Z (depth reservoir), Secchi (water column transparency); W_temp (water temperature); TURB (turbidity)]. 

Occurrence in samples (UPCB) - Capivari reservoir 59525, 60509, 68843, 68867; Guaricana reservoir 59533, 60517, 68851, 68875; São Jorge reservoir 59523, 60526, 68860, 68884; Pitangui reservoir 59537, 60521, 68855, 68879; Salto do Vau reservoir 59541, 60525, 68859, 68883; Fundão reservoir 68864, 68888; Foz do Areia reservoir 59530, 59531, 59532, 60514, 60515, 60516, 68848, 68849, 68850, 68872, 68873, 68874; Santa Clara reservoir 68863, 68887; Jordão reservoir 59520, 60518, 68852, 68876; Segredo reservoir 59543, 59544, 60527, 60528, 68861, 68862, 68885, 68886; Salto Caxias reservoir 59539, 59540, 60523, 60524, 68857, 68858, 68881, 68882; Mourão reservoir 59536, 60520, 68854, 68878.

Ecology

The ecological preferences of Acanthoceras and Urosolenia species are poorly known. Acanthoceras zachariasii was reported as occasionally abundant and ephemeral in several alkaline and eutrophic environments in Europe, North and South America (Rivera 1974, Beaver 1981, Edlund & Stoermer 1993). In fact, this species was only found at low densities in two studied eutrophic reservoirs in April/2010, (São Jorge reservoir: 37 cells.mL-1 and Pitangui reservoir: 99 cells.mL-1), co-occurring with Urosolenia species. Ramberg (1987), when study of phytoplankton of Lake Kariba, observed that A. zachariasiioccurred in low density in the end of the rainy season and disappeared with the mixing of water column. According to Edlund & Stoermer (1993), the record of Urosoleniaspecies for several environments with different physical and chemical conditions can be a result of the erroneous determination of taxa. Thus, we emphasize the importance of taxonomic studies to better define the differences between species and their geographical distribution, aiding subsequent ecological studies.

The first two axes from Principal Component Analysis (PCA) exceed expectations from the broken-stick distribution, suggesting these axes are significant and explained 52.52% of total variance from environmental variables considering 2007-2012. The first axis (27.66%) showed positive correlations with reservoir depth (r=0.83) and to molar N/P (r=0.83) and negative correlations with total phosphorous (r=-0.56) and pH (r=-0.51). Water column turbidity (r=0.76) and total inorganic nitrogen (r=0.68) had a significantly positive correlation and water transparency was negatively correlated (r=-0.60) with the second axis (24.86%).

In general, the Jordão reservoir was characterized by greater depth, and São Jorge, Pitangui, Guaricana and Chaminé were more alkaline environments. Rio dos Patos and Segredo reservoirs present higher turbidity and nutrient concentrations, but higher transparency characterizes Jordão and Chaminé reservoirs (Figure 64).

Urosolenia amazonica showed occurrence frequency of 78.7%, and despite the density values varied markedly, higher average values were recorded at São Jorge, Pitangui and Chaminé. Spearman rank correlation results revealed positive associations between density and pH, but total inorganic nitrogen, nitrate and reservoir depth were negatively correlated (Table 6). A multiple linear regression model was performed and revealed that total inorganic nitrogen was the main factor influencing U. amazonica cellular densities. Along with conductivity, water temperature and molar N/P ratio the model explained 12% of variance. According to this model, the conductivity was positively associated with U. amazonica density, and negatively correlated to total inorganic nitrogen, water temperature and the molar N/P ratio (Table 7).

Table 6 Values of Spearman’s correlations between species density and environmental variables of the reservoirs. Values in bold = significant correlations. 

U. amazonica U. longiseta U. obesa
pH 0.224 0.179 0.144
Log Depth -0.200 -0.341 -0.260
Log Conductivity 0.136 -0.123 -0.025
Log Water temperature -0.081 -0.292 0.087
Log N/P ratio -0.145 -0.300 -0.475
Log Inorganic nitrogen -0.266 -0.148 -0.314
Log Nitrate -0.234 -0.165 -0.268
Log Total nitrogen -0.093 -0.225 -0.500
Log Turbidity -0.094 0.019 0.223

Table 7 Results of a multiple regression analysis of species densities against environmental variables. 

Predictor variables B t F p
U. amazonica Intercept 3.077 (96) 1.751 3.540 0.009
Log Nitrogen inorganic -2.516 -2.765 0.006
Log Conductivity 0.892 1.636 0.105
Log Water temperature -1.411 -1.514 0.133
Log N/P ratio -0.263 -1.127 0.262
U. longiseta Intercept 8.214 (40) 3.999 2.699 0.000
Log Water temperature -2.977 -2.591 0.013
Log N/P ratio -0.689 -2.403 0.020
Log Conductivity -0.653 -1.324 0.192
Log turbidity -0.334 -1.142 0.259
Log Nitrogen inorganic -1.326 -0.928 0.358
Log depth 0.04 0.140 0.888
U. obesa Intercept -0.035 (38) -0.018 7.242 0.000
Log N/P ratio -0.039 -3.925 0.000
Log Water temperature 2.485 1.889 0.066
Log turbidity 0.366 1.030 0.309

The frequency of U. longiseta occurrence was 34.5%. The density values had higher densities in winter season and in the São Jorge and Guaricana reservoirs. The maximum value registered was 486 ind.mL-1 in São Jorge, during the winter of 2008. Urosolenia longiseta density was negatively correlated with depth, molar N/P ratio and water temperature (Table 6). The multiple linear regression model showed that the water temperature and the N/P molar influenced significantly the density of U. longiseta in the studied reservoirs. These variables along with depth of the water column, inorganic nitrogen, conductivity and turbidity explained 28% of U. longiseta density between environments and established temporal interval. The water body depth was the only variable positively correlated with the density of this species and all the others were negatively correlated (Table 7).

Frequency occurrence of Urosolenia obesa was 17.8% during 2007-2012 and the density values were generally lower compared to U. amazonica and U. longiseta. Higher cell concentrations were achieved at São Jorge and Fundão reservoirs, and greater frequency occurred during fall and winter. Urosolenia obesa was negatively associated with total nitrogen, N/P molar ratio and inorganic total nitrogen (Table 6). Multiple linear regression supported that limnological variables were related to U. obesadensity. Accordingly, N/P molar ratio was the main variable related to species density variation, along with water temperature and turbidity, the model explained 36% of data (Table 7).

The three Urosolenia species showed distinct frequencies of occurrence and wide density variation among different studied reservoirs, in the period 2007-2012. Statistical analysis showed that such variation was correlated with limnological factors associated with particular characters from each reservoir, influencing the distribution pattern of species. Generally, higher densities of Urosolenia were registered in shallower reservoirs (ex., São Jorge, Pitangui and Guaricana), except for Fundão (38 meters). Residence time (which favors nutrients mixing and resuspension) and hydrodynamics are important determinants of phytoplankton densities in shallow reservoirs (Silva et al. 2005; Reynolds 2006; Lopes et al. 2009; Nogueira et al. 2010).

Higher densities of U. amazonica were detected in more alkaline waters and in low inorganic nitrogen and nitrate concentrations, and shallow waters. U. longisetawere also recorded in shallower environments (São Jorge and Guaricana), in cooler temperatures. The species is less restricted by phosphorus (lowest N/P ratio). Finally, more elevated densities of U. obesa were related to lower concentrations of the nitrogenated forms. Higher densities of U. amazonica and U. longiseta were recorded by Silva et al. (2005), in two deep reservoirs from Iguaçu River basin (Foz do Areia and Salto Santiago), during lower temperatures and nitrogen forms minor concentrations, besides greater turbulence of the water column. Reported as r-strategists (Reynolds 2006), these centric diatoms thrive in conditions of turbulent water column and low nutrient concentrations, corroborating the general pattern observed in this study.

The performed model selected inorganic nitrogen as the primary determinant of U. amazonica density, with a negative coefficient. Urosolenia longiseta showed a negative correlation with temperature and N/P molar ratio, both variables were cited as the main determinants with that species density. N/P molar ratio was selected as the most important variable negatively correlated with U. obesa. These results suggest the occurrence of higher densities in periods of warmer temperatures and low levels of nitrogenated forms (inorganic nitrogen and N/P molar ratio), corroborating the results reported by Flynn (2001) for the phytoplanktonic diatoms community.

As shown, Urosolenia species respond more strongly to local environmental gradients, which are highly influenced by particular local characters (as depth and hydrodynamics of the system). Also, the extent of their ecological amplitude determines the distribution and occurrence pattern of these species in the reservoirs of State of Paraná.

Acknowledgments

To Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES) for posdoctoral grant to P. Tremarin, to Fundação Araucária to posdoctoral grant for V. Algarte, and to Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq) by the scientific productivity grant for T. Ludwig. To the Instituto de Tecnologia para o Desenvolvimento (LACTEC) and Companhia Paranaense de Energia (COPEL) for providing physical and chemical data and samples for the study; and to the staff of the Electron Microscopy Center of Universidade Federal do Paraná for technical assistance.

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Received: March 20, 2014; Revised: October 8, 2014; Accepted: November 27, 2014

2Corresponding author: Priscila Izabel Tremarin, e-mail: ptremarin@gmail.com

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