Journal of Threatened Taxa | www.threatenedtaxa.org | 26 July
2019 | 11(9): 14087–14100
Species richness and abundance
of monogonont rotifers in relation to environmental factors in the Unesco Sakaerat Biosphere Reserve,
Thailand
Nattaporn Plangklang 1, Chaichat
Boonyanusith 2
& Sujeephon Athibai
3
1,3 Applied Taxonomic Research Center and
Department of Biology, Faculty of Science, Khon Kaen University, Khon Kaen 40002, Thailand.
2 School of Biology, Faculty of Science and Technology, Nakhon Ratchasima Rajabhat University,
Nakhon Ratchasima 30000, Thailand.
1 natt-kung@hotmail.com,
2 chaichat.b@nrru.ac.th, 3 sujiat@kku.ac.th
(corresponding author)
doi: https://doi.org/10.11609/jott.4721.11.9.14087-14100
| ZooBank: urn:lsid:zoobank.org:pub:2FA19E6D-D65D-48C9-B8D4-708B500EFFF8
Editor: R.J. Shiel, University of
Adelaide, Adelaide, Australia. Date of publication:
26 July 2019 (online & print)
Manuscript details: #4721 | Received 22 November
2018 | Final received 22 May 2019 | Finally accepted 03 July 2019
Citation: Plangklang, N., C. Boonyanusith
& S. Athibai (2019). Species richness and abundance of monogonont rotifers
in relation to environmental factors in the Unesco
Sakaerat Biosphere Reserve, Thailand. Journal of Threatened Taxa 11(9): 14087–14100. https://doi.org/10.11609/jott.4721.11.9.14087-14100
Copyright: © Plangklang et al. 2019. Creative Commons Attribution
4.0 International License. JoTT allows unrestricted use, reproduction, and
distribution of this article in any medium by adequate credit to the author(s)
and the source of publication.
Funding: This study
was supported by Khon Kaen University, Centre of
Excellence on Biodiversity and
Science Achievement Scholarship of Thailand.
Competing interests: The authors declare no competing
interests.
Author details: Mr Nattaporn
Plangklang has got master’s degree in Biology and is currently a
PhD student at Department of Biology, Faculty of Science, Khon
Kaen University. During his graduate degree program,
he worked on diversity of zooplankton. Dr
Chaichat Boonyanusith
is a lecturer of the School of Biology, Faculty of Science and Technology,
Nakhon Ratchasima Rajabhat University. His research
is focused mainly on diversity of cave-dwelling copepods, as well as surface
freshwater zooplankton. Dr Sujeephon Athibai is an assistant professor at Department of Biology,
Faculty of Science, Khon Kaen
University. She has focused her research interests on diversity and ecology of
zooplankton in freshwater ecosystem.
Author contribution: NP was responsible for data collection and analysis, laboratory work and
preparation of the manuscript. CB performed multivariate analyses and
preparation of the manuscript. SA designed and participated in providing
funding and facilities, involved in directing and supervising field and
laboratory works, analyzed the data and discussed the results and preparation
of the manuscript.
Acknowledgements:
We are grateful to the director
and the staff at the Sakaerat Environmental Research
Station for facilitating this study.
This work was supported by Khon Kaen University under the Incubation Researcher Project;
Centre of Excellence on Biodiversity (BDC), Office of Higher Education
Commission (BDC-PG4-160020), and in the case of the first author, by a Science
Achievement Scholarship of Thailand (SAST).
The authors also thank David Park for copy editing the manuscript.
Abstract: The UNESCO Sakaerat
Biosphere Reserve plays an important role in nature conservation and
environmental protection. Previous focus
on terrestrial habitats and neglect of aquatic ecosystems has resulted in an
incomplete picture of biodiversity of the area.
Based on the first investigation of planktonic diversity, rotifers were
collected seasonally at five localities from September 2013 to May 2014 using a
Schindler-Patalas plankton trap and a plankton
net. Fifteen families, 25 genera and 71
species of rotifers were identified. The
most diverse families were Lecanidae, Brachionidae, Lepadellidae, and Trichocercidae, accounting for 80% of the total species
count. The maximum species richness was
reported at the reservoir, with 57 species (80% of the total), while the
minimum species richness (34) was observed at the ponds. The rainy season had the highest density,
followed by winter and summer, with 149.15 N/l from an intermittent stream, and
95.43 and 50.68 N/l from a pond, respectively.
Most of the sampling sites at the three seasonal occasions were
dominated by a planktonic species Polyarthra
vulgaris. The results indicate that
the seasonal variation of the rotifer assemblage is related to the seasonal
variation of physicochemical parameters.
Keywords: Mountainous area, northeastern
Thailand, seasonal variation, southeastern Asia,
water quality, zooplankton.
INTRODUCTION
The UNESCO Sakaerat Biosphere Reserve (SBR), the leading biodiversity
hotspot in Thailand, plays an important role in nature conservation and
environmental protection. It is an ideal
place to conduct ecological and environmental research. Several investigations have clearly shown a
high diversity of flora and fauna (e.g., fungi, mushrooms, flowering plants,
insects and vertebrates), and new species continue to be discovered, including
fungi (Lauriomyces sakaeratensis)
and grasshoppers (Arnobia tinae) (Somrithipol et al.
2006; Tan & Artchawakom 2014). Interest in the diversity of aquatic fauna
has been limited to date, however; until recently, only two studies have been
reported. The first involved the
investigation of harpacticoid copepods (Boonyanusith
& Athibai 2014), while the more recent one
focused on the discovery of the rare freshwater sponge of Australasia at an
intermittent stream (Ruengsawang et al. 2017).
Monogonont
rotifers, in general, are the most diverse metazoan zooplankton. On a global scale, they comprise about 1,583
species belonging to 112 genera and 30 families (Segers
2011). In continental water bodies, they
are predominant in the littoral zone of both permanent and temporary waters,
acting as primary consumers in the trophic stage. Additionally, they are used
as bioindicators to study the influence of environmental factors in water
bodies (Negreiros et al. 2010). The diversity and distribution of rotifers in
Thailand has been investigated primarily in surface water-bodies in lowland
areas. Since the first publication for
the country (Ueno 1966), the number of known Thai rotifers has increased
remarkably. Previous comprehensive
studies have provided valuable knowledge of the distribution of rotifers in
Thailand (e.g., Sanoamuang et al. 1995; Sanoamuang & Savatenalinton
1999; Chittapun et al. 2007; Segers
& Savatenalinton 2010; Athibai
et al. 2013; Meksuwan et al. 2013), and 399 taxa of
monogonont rotifer have been recorded (Sa-ardrit et
al. 2013; Meksuwan et al. 2018). Nevertheless, considering the diversity of
zooplankton in SBR it is necessary to fill the gaps in our knowledge. In this contribution, the species list and
abundance of monogonont rotifers are provided based on sampling done in three
seasons (rainy, winter and summer) at five sampling sites with various aquatic
habitats within the Sakaerat Environmental Research
Station (SERS), the core portion of the UNESCO SBR.
MATERIALS
AND METHODS
Study area
Sakaerat Biosphere Reserve, the first of four UNESCO biosphere
reserves in Thailand, is situated in the Sankamphaeng
mountain range on the southwestern margin of the Khorat
Plateau, Nakhon Ratchasima Province, in northeastern
Thailand. Located between 14.445–14.542 0N
and 101.844–101.955 0E, it covers approximately 82,100ha at an
elevation of 250-–762 m. The average
annual temperature in that region is 260C, and the average annual
rainfall is 1,260mm (Ruengsawang et al. 2017). Sakaerat
Environmental Research Station is the core portion of the SBR. It was established to promote long-term
ecological research, and to demonstrate sustainable forest management and
biodiversity conservation (Trisurat 2010). Within the SERS and its buffer zone, nine
habitats have been classified, comprising dry evergreen forest, mixed deciduous
forest, dry dipterocarp forest, grassland, secondary growth vegetative forest,
plantation, agriculture and settlement, old clearing, and water body (Trisurat 2010). In
this study, monogonont rotifers were investigated at five sampling sites (Fig.
1). The location, altitude and habitat
type of each are in Table 1.
Rotifer sampling and identification
and environmental factors measurement
Qualitative
and quantitative samples were collected seasonally in the rainy, summer and
winter seasons between September 2013 and May 2014 from the five sampling
localities, using a Schindler-Patalas plankton trap
and a plankton net (60µm mesh size). The
rotifers were then immediately preserved with 4% formaldehyde solution. Nine physicochemical parameters were
measured: water temperature, transparency, pH, electrical conductivity (EC),
total dissolved solids (TDS), dissolved oxygen (DO), orthophosphate content (PO43-),
nitrate content (NO3-) and total ammonia
content (NH3). The rotifer
specimens were subsequently sorted, counted and identified under an
Olympus-CH30 compound light microscope.
The rotifers were identified to species level, according to Koste & Shiel (1992), Nogrady et al. (1995), Segers
(1995), De Smet & Pourriot (1997), and Nogrady & Segers (2002).
Data analysis
The similarity of the
faunal assemblages among the sampling sites and the seasons was evaluated by
clustering. The operation was based on
the Bray-Curtis dissimilarity coefficient. A canonical correspondence analysis
(CCA) was later performed to examine the relationships between the
environmental factors and the rotifer species.
In
the data matrix of species abundance, taxa that occurred more frequently than
1% of all samples were included in the analysis (Yang et al. 2005). The data of abundance and environmental
parameters were transformed by log10 (x + 1) before analysis. Data analysis was conducted by PC-ORD,
version 5.0 (McCune & Mefford 2006).
The
differences in nine environmental factors and the density of rotifers during
three seasons at five sampling localities were analyzed
using one-way ANOVA and IBM SPSS Statistics for Windows, version 19 (IBM Corp.,
Armonk, NY, USA). Furthermore,
comparisons of the means were conducted using Duncan’s multiple range test (p
< 0.05).
RESULTS
Rotifer richness
Rotifer fauna collected
on three seasonal occasions from five water-bodies within the SERS were
investigated. A total of 71 species,
belonging to 23 genera and 15 families of monogonont rotifers, were found
(Table 2); illustrations of selected species are shown at Image 1. The most diverse family was Lecanidae (26 species, 36.62%) and Brachionidae
(13 species, 18.31%). The next two
most-diverse families were Trichocercidae and Lepadellidae, accounting for eight and six species,
respectively. The greatest number of
rotifer species (56) was reported during the rainy season. Based on the number of species per habitat
(α-diversity), the α-diversity recorded from the rainy season was similar to
that of the summer season. During the
rainy season, the richness of the rotifers varied from nine to 44 species,
compared to nine to 43 species found in summer, but the α-diversity was lower
in winter (seven to 31 species). When comparing the habitat types, the
reservoir had the highest diversity (57 species), followed by the stream (35
species) and the pond (34 species). The
most frequently encountered species were Polyarthra
vulgaris (80% of samples), Keratella tropica (73%), and Lecane
bulla (73%). Ascomorpha
ovalis, Brachionus forficula,
Cephalodella gibba,
Lecane haliclysta,
L. obtusa and Trichocerca
scipio were recorded during the rainy season
only. Lecane
pyriformis, L. stenroosi, Lepadella quadricarinata
and Trichocerca cylindrica
were observed only in winter; in contrast, Brachionus
calyciflorus, Dipleuchlanis
propatula, Euchlanis
dilatata, Lecane
aculeata, L. latissima,
Lecane superaculeata
and L. tenuiseta were present only in
summer. Moreover, Brachionus
calyciflorus, Lecane
haliclysta, L. stenroosi,
and L. quadricarinata were recorded only at the
stream. Brachionus
forficula, Cephalodella
gibba, Dipleuchlanis propatula, Euchlanis
dilatata, Lecane
aculeata, L. latissima,
L. obtusa, L. pyriformis, L. superaculeata, and Trichocerca
scipio were found only at the reservoir. Finally, Lecane
tenuiseta and Trichocerca
cylindrica were observed only at the pond.
Rotifer density
The density
of the rotifers varied by season and sampling site. The densities at S1 (stream; F2, 8
= 23.689, p = 0.001), S2 (reservoir; F2, 8 = 11.396, p = 0.009) and
S5 (intermittent stream; F2, 8 = 42.925, p < 0.001) are
seasonally significant differences; by comparison, those of S3 (pond) and S4
(pond) were not significantly different.
The greatest number of rotifers at S1, S2, and S5 was 13.91N/l in the
rainy season, 29.43N/l in summer, and 149.15N/l in the rainy season,
respectively. The sampling site with the
highest abundance in the rainy season was S5 (the intermittent stream;
149.15N/l), whereas the greatest number during winter (95.43N/l) and summer
(50.68N/l) was at S3 (pond). Filinia longiseta
was most prominent at S5 in the rainy season, with a density of 96.63 ± 28.57
N/l (64.79%); while S3 was dominated by Brachionus
quadridentatus in winter and Polyarthra
vulgaris in summer, with densities of 84.78 ± 51.57 N/l (88.84%) and 28.03
± 19.73 N/l (55.31%), respectively. In
contrast, the lowest densities in the rainy, winter and summer seasons were
observed at S2 (6.25N/l), S5 (0.38N/l) and S1 (1.22N/l), respectively. In addition, of the 15 families encountered, Brachionidae, Lecanidae, Trichocercidae, and Synchaetidae
were the most dominant. The first three
families are most prominent at all of the sampling sites in the rainy
season. The intermittent stream S5 had a
remarkably different rotifer assemblage to the other sites in the rainy season
as the density of Trochosphaeridae was over 60%. During winter, when the highest density of Brachionidae, Synchaetidae, and Trichocercidae occurred, the sampling sites generally
showed a low density of rotifers (< 10N/l) except S3, whose density
(95.43N/l) was noticeably higher, with Brachionidae
accounting for 84.78% of the specimens at the S3 site. Among the 15 families, the Brachionidae was the most frequently observed, being
present at over 50% of the study sites.
In summer, the densities of rotifers obviously increased from those
during winter. Most of the sampling
localities were dominated by Brachionidae, Lecanidae, Synchaetidae, and Trichocercidae (Fig. 2).
The most prominent species during each season varied slightly. Three species, namely, Lecane
bulla, Polyarthra vulgaris, and Trichocerca similis
were predominant and common at several sampling sites in all seasons.
Environmental parameters
The
physicochemical parameters of water data were obtained during three seasons
(rainy, winter and summer) from five sampling sites (S1, S2, S3, S4, and S5);
the grouping was categorized into three different habitat types (pond,
reservoir, and stream). The statistical
analysis showed that five parameters (water temperature, pH, transparency, NH3,
and EC) at each sampling site displayed significant differences among the
seasons (p < 0.05). The value of
water temperature had the highest in summer and lowest in winter. The pH of water in the rainy season was
slightly acidic to neutral (6.51–7.44), whereas that in winter and summer was
slightly acidic (5.17–6.70) and acidic to slightly acidic (4.54–6.32),
respectively. The pH was lowest at S5,
with a mean of 4.54 ± 0.36. The NH3
value at S3 was the highest in all seasons, with 2.04 ± 0.12 mg/l in the rainy
season, 0.93 ± 0.09 mg/l in winter and 1.92 ± 0.04 mg/l in summer. In addition, the NH3 value at S1
(the stream) was high in the summer (1.81 ± 0.22 mg/l).
The Pearson
correlation from the CCA analysis showed that EC and TDS had a strongly
positive correlation with NH3.
The correlation coefficients between EC and TDS, EC and NH3,
and TDS and NH3 were 0.996, 0.937 and 0.953, respectively. In contrast, EC, TDS, and NH3 were
negatively correlated with DO; the coefficients between EC and DO, TDS and DO,
and NH3 and DO, were 0.568, 0.608 and 0.615, respectively. The ranges of EC, TDS, NH3 and DO
during those two seasons were, respectively, 153–161 µS/cm, 74–81 mg/l,
1.92–2.16 mg/l and 1.0–1.7 mg/l in the rainy season, and 125–133 µS/cm, 65–70
mg/l, 1.88–1.96 mg/l and 1.6–2.4 mg/l during the summer.
Seasonal variation of rotifer
community
A cluster
dendrogram was constructed; it was based on the data of 12 species at each
sampling locality in the three seasons.
The results revealed three major groupings (Fig. 3). Sampling sites S1
and S5 were clustered together, which corresponded to the winter
community. Both sites were streams and
had a low density of rotifers; Lecane bulla
was predominant at both sites. Cluster 2
comprised the majority of the sampling sites and could be separated into two
sub-clusters. Cluster 2A was composed
mainly of two lentic habitats (S3 in all seasons, and S4 during the rainy
season and summer) and one lotic water (S5 in the rainy season). This subgroup had a high density of six
dominant species: Anuraeopsis fissa, Brachionus kostei, B. quadridentatus,
Filinia longiseta,
Polyarthra vulgaris, and Trichocerca
pusilla.
Cluster 2B included two water bodies: S2 (the reservoir) in the winter
and the summer, and S4 (one of the ponds) in winter. This sub-cluster was made up of three
predominant species: Filinia opoliensis, Keratella
tropica, and Trichocerca
similis.
Cluster 3 consisted of three sampling sites, S1 (the stream) in the
rainy season and summer, S2 in the rainy season, and S5 in summer. This cluster was grouped by the occurrence of
three species (Lecane bulla, L. curvicornis, and Mytilina
acanthophora).
Focusing on S1 and S2 in the rainy season, both water bodies showed a
strong relationship between them because they were situated in the same
watershed, resulting in the similarity of their species occurrences and the
equality of their densities.
Relationships between rotifer
community structure and environmental factors
Out of the 71
rotifer species, 12 that had a relative density of more than 1% were used for a
CCA analysis. The percentages of the
explained variance on the first and the second axes is 22.1 and 16.7,
respectively. The species that are
positively correlated to EC, TDS, NH3, NO3-,
PO43-, and altitude are Anuraeopsis
fissa, Brachionus
kostei, Polyarthra
vulgaris and Trichocerca pusilla (Fig. 4).
The density of those species was high in the two ponds (S3 and S4 in the
rainy and summer). A high density of Brachionus kostei
was found at S3 in the summer season, with 19.57 N/l. Additionally, Filinia
longiseta, F. opoliensis,
and Trichocerca similis
are positively correlated to water temperature and DO. High densities of the three species were
present at the intermittent stream (S5) in the rainy season and at the
reservoir (S2) in summer, when there were relatively high temperatures and DO
levels. In particular, Filinia longiseta
had the maximum density, with 96.63 N/l at S5 in the rainy season. In contrast, Keratella
tropica showed a negative correlation with the
major factors, including EC, TDS, NH3, NO3-,
PO43-, and altitude.
Keratella tropica
predominated at the sites that had low values for those factors, such as the
pool region of the S1 stream (in winter), the S4 pond (in winter) and the
reservoir (S2, in the rainy season and winter).
Four species, Brachionus quadridentatus, Lecane
bulla, L. curvicornis, and Mytilina acanthophora
were negatively correlated with water temperature and DO. They had high densities at the sites that had
low values for temperature and DO, the stream S1 (in all seasons), the S3 pond
(in winter) and the pool of the intermittent stream (S5, in winter and
summer). However, the Monte Carlo
permutation test showed that the axis does not have any statistical
significance with any of the physicochemical parameters of the water.
DISCUSSION
Rotifer
richness
The 71 species of rotifer within the SERS represent 37.37% of the
190 species known at 77 localities within Nakhon Ratchasima Province (Savatenalinton 1999) and circa 17.79% of the
399 monogonont rotifers recorded in Thailand.
The diversity of rotifer within the SERS is relatively low, compared
with the total number of species of freshwater rotifers recorded in Thailand
(Sa-ardrit et al. 2013; Meksuwan
et al. 2018). This is probably due to
the differences in the number of samples and habitat characteristics. In general, the diversity of plankton is
quite high in lowland areas due to a large number of relatively large, stagnant
waterbodies (Obertegger et al. 2010). In general, monogonont rotifers are
especially diverse in the littoral zones of stagnant waters which have soft,
slightly acidic and under oligo- to mesotrophic conditions (Segers
2008). This contrasts with the situation
in mountainous areas, where running water, such as streams, is common. Flowing water has been identified as a
limiting factor that results in reduced species diversity of rotifers (Sulehria & Malik 2012).
However, rotifer species richness at SERS is numerically higher than
those found at other conservation and mountain areas, such as Nam Nao
National Park, Phetchabun Province, where 11 species
of monogonont rotifers were encountered, and Phu Hin Rong Kla
National Park, Phitsanulok Province, where 12 species
were found in waterfall mosses (Savatenalinton & Segers 2008; Athibai 2014). Only a few species have commonly been
encountered at those two parks. Only one
cosmopolitan species, Keratella tropica, was recorded in the two aforementioned studies
as well as the current study. This
species was considered as tolerant species because they can live in highly
polluted waters (Kulshrestha et al. 1991; Javed 2006) and eutrophic waters (Guevara et al.
2009). This incidence indicates that Keratella tropica
has a wide range of ecology. In addition, Lecanidae
was highly diverse at many sampling sites in the current study, which concurs
with previous studies done in northeastern and
southern Thailand (e.g., Sanoamuang et al. 1995; Chittapun et al. 2007).
Genus Lecane has a high diversity in
tropical regions and has frequently been found in neighboring
countries such as Laos PDR (Segers & Sanoamuang 2007), Cambodia (Sor
et al. 2015), and Vietnam (Dang et al. 2013). Several species in our study were widely
distributed and found in almost every type of water body such as Lecane bulla, L. closterocerca,
L. curvicornis, L. hamata,
L. lunaris, and L. papuana.
Compared with species richness of monogonont rotifers in Nokrek
Biosphere Reserve, India, a number of rotifers in the latter (67 species) were
close to the observed species richness in the present study; particularly,
rotifer species exhibited 60.8% similarity with 42 shared species between this
work and Nokrek Biosphere Reserve (Sharma &
Sharma 2011). The species composition of
the rotifers at the three different habitat types within the SERS,
however, was different. The reservoir
had the most diverse habitat, followed by the stream and then the pond. This indicated that the distribution of a
certain species depends on the habitat type (Gürbüzer
et al. 2017) and whether a habitat shows a high diversity of microhabitats
(Arora & Mehra 2003). In case of SERS, the reservoir and streams
were densely covered by macrophytes in the littoral region, providing various
microhabitats. This has been found to
affect the distribution and composition of rotifers (Duggan et al. 1998). Similarly, Ali et al. (2007) reported
that subtropical freshwater invertebrates had the highest species diversity in
various types of macrophytes.
Furthermore, the species preferences of rotifers have been shown to
differ depending on the macrophyte species (Choi et al. 2014). Given that it is a common species, Polyarthra vulgaris was expected to be common
and dominant in the inland waters of the SERS.
Similarly, this species has been found to be common in certain habitats,
such as the Cambodian Mekong River Basin (Meas & Sanoamuang 2008) and the eight lakes in the central Anatolia,
Marmara, and western Black Sea regions of Turkey (Ergönül
et al. 2016).
Rotifer
density
A seasonal variation in rotifer density was evident at all of the
sampling sites in the SERS; the densities of the rotifers at S1, S2, and S5
differed significantly between the seasons (p < 0.05). At site S5, the density of rotifers was
greatest in the rainy season. The
physical characteristic of the S5 sampling area was rock pool, and the
slow-flowing water was densely covered by free-floating macrophytes (Lemna perpusilla)
during the rainy season. The macrophytes
at that site disappeared in winter but regenerated in summer; during both those
seasons, the water level was lower than in the rainy season. Nitrate and orthophosphate contents seem to
be influencing factors for rotifer composition in SERS. As to the S5 site, both parameters were high
in the rainy season, with 1.93 ± 0.46 and 0.45 ± 0.39 mg/l, respectively. Generally, nitrates and phosphates are common
nutrients in aquatic habitats; they promote phytoplankton growth, and their
concentrations in the water column can significantly increase or decrease the
phytoplankton biomass (Pelczar et al. 2010). Meanwhile, zooplankton growth is impacted by
the phytoplanktonic density because the zooplanktons graze upon the
phytoplankton (Thompson et al. 1982).
Therefore, seasonal variation also influences the plankton
communities. Moreover, this site seems
to be a eutrophic habitat because the nitrate and orthophosphate content in
this study exceeded 1,500µg/l of total nitrogen and 75µg/l of total
phosphorus (Dodds & Smith 2016). Those characteristics of the sampling site
would affect the rotifer density (Rothhaupt
1995). The greatest density of rotifers
was recorded in the rainy season, accounting for 99% of the total density. Three rotifer species were dominant in that
period: Filinia longiseta
(64.78%), Anuraeopsis fissa
(20.81%) and Polyarthra vulgaris
(13.23%). Those three species have also
been found in eutrophic habitats (Saunders-Davies 1989; Basińska
& Kuczynska-Kippen 2009). According to S3 (one of the two ponds), it
was observed to have the highest density of rotifers in winter and summer. Brachionus
quadridentatus was the dominant species in the
winter, with an 88.84% relative density, but that species disappeared in the
summer. Both Polyarthra
vulgaris and Brachionus kostei were found to be predominant in summer, with
relative abundances of 55.31% and 38.61%, respectively. Rotifers in the genus Brachionus
and Polyarthra are euplanktonic
rotifers, and several species of the genera are present in the littoral region
of water bodies (Virro 1993). From our observations during the sampling,
macrophytes were present at only three localities; therefore, the dominant
species were probably both the planktonic and epiphytic rotifers. For example; macrophytes (Hydrilla verticillata) were present at S1 in the rainy season,
and Lecane and Lepadella
were found to be the dominant genera at that site.
Environmental parameters
Seasonal
variations in the physicochemical parameters at the five sampling sites in the
SERS were reported; five parameters, water temperature, pH, transparency,
ammonia, and EC, had seasonally significant differences (p < 0.05).
Ranging from 19.0–32.9°C, the water temperature was the lowest and the highest
in winter and summer, respectively.
Generally, water temperature is mainly influenced by factors such as air
temperature, solar radiation, wind speed, cloud cover, humidity, precipitation,
evaporation, and topography (Li et al. 2017),
however, the sampling time should also be considered because it could
result in differences in temperature readings throughout the day (Orr et al.
2015). As to pH, the mean pH values of
the five sampling sites ranged from highly acidic to circumneutral
(4.54–7.44). During summer (May), water
in the intermittent stream (S5) recorded the lowest value (4.54 ± 0.36). The physical characteristic of this sampling
site was a rock pool with brown water.
The evidence is similar to that of a previous study by Tevapawat & Sangpradub
(2017), who found that the water at S5 in the summer was brown in color and that its pH (5.59 ± 0.26) was slightly higher
than observed in the present study. We
assumed that the brown color and high acidity of the
water resulted from organic decomposition (Winterbourn
& Collier 1987). Moving on to NH3,
high values of NH3 were reported in pond (S3) in all seasons, but
particularly during the rainy season, when it peaked at 2.04 ± 0.12 mg/l. In general, ammonia is considered the first
nitrogenous form to occur in freshwater habitats after its release into natural
waterways through sewage discharges, the excretion of nitrogenous wastes from
animals, and organic matter decomposition (Thurston & Russo 1983). In the present study, the S3 site was a small
pond providing water for wildlife, and much leaf litter fell into the site
during each of the three seasons. It,
therefore, seems probable that the high NH3 value of this site
results from the excretion of nitrogenous wastes from wildlife, leaf litter
decomposition, and nutrient loading during the rainy season. In addition to the litter decay in the S3
pond, dissolved oxygen (DO) would seem to be a limiting factor in the
environment since oxygen is not only a source of aquatic animal respiration but
also an input to the decomposition process.
This study revealed that the DO values at S3 were low during all three
seasons, with their mean ranging between 1.30 and 2.03 mg/l. The trend of the DO and nitrogen values is
similar to the findings of the study by Stoler &
Relyea (2016), which reported that DO showed a negative correlation with the
leaf litter decay rate and the ratio of carbon to nitrogen (C:N) in the pond at
the Pennsylvania State in USA.
Relationship between habitats,
environmental factors and rotifer abundance
The
clustering showed that two factors affect the distribution and diversity of the
rotifers in the SERS. The first is the
connectivity between them (Schöll 2009), and the
second is the habitat type (Sor et al. 2015). In terms of the location of the five sampling
sites, S3 and S4 are the closest. Given
that both sites are man-made water bodies constructed as water sources for the
local wildlife which can connect and distribute through both regions. The resting eggs of rotifers may attach to
the feet, fur and feathers of other wildlife.
So, the dispersion of rotifers between the two sites is probably
generated by animals (Zhdanova et al. 2016). In the case of the S1 and S2 sites, S1 is the
nearest site to S2, S1 is located more in the upper part of the watershed than
S2. The clustering clearly showed a
separation of the two sites. Although
they share the same watershed, the rotifer community of both sites were
different. The S1 was separated from S2
due to the dry period in winter and summer seasons. However, the presence of two Elaphoidella species (harpacticoid copepods) in S1
and S2 that were not observed at other sampling sites and have never previously
been observed elsewhere in Thailand (Boonyanusith
& Athibai 2014), is an indication of the
connection between S1 and S2. The
cluster analysis also revealed that, in the rainy season, S1 and S2 are grouped
together, which is supported by the similarity of their rotifer assemblages. S2 could be classified as a relatively large
reservoir, and its water level was stable throughout the three sampling
occasions. This characteristic supports
the continual presence of macrophytic vegetation in
the reservoir’s littoral zone, in turn ensuring the presence of stable rotifer
microhabitats and hence its high diversity of rotifers.
The CCA triplot showed the effects of electrical conductivity,
total dissolved solids, ammonia, nitrate, orthophosphate and altitude on the
distribution of the rotifer species in the inland waters of the SERS. Anuraeopsis
fissa, Brachionus
kostei, Polyarthra
vulgaris, and Trichocerca pusilla were predominant at S3 and S4 in the rainy and
summer seasons, with relatively high values for those variables. Conde-Porcuna et
al. (2002) reported that the population of Anuraeopsis
fissa correlated with the soluble reactive
phosphorus value in a mesotrophic reservoir in southern Spain. Based on the DO levels and water temperature,
the CCA result indicated that DO seems to be an influential factor for Filinia longiseta. This species was found to be most abundant in
the rock pool of the intermittent stream (S5) in the rainy season (9.13mg/l of
DO), whereas Filinia opoliensis
and Trichocerca similis
were predominant at the reservoir (S2) in summer, when water temperatures there
were at their highest (30.40C).
Similarly, Negreiros et al. (2010) pointed out
that pH, EC and DO probably influenced the fluctuations in the rotifer
population in the Sapucaí River arm of Furnas Reservoir, MG, Brazil. Sharma (2010) reported that variations of
rotifer communities in a Ramsar site, namely Deepor Beel in India were
influenced by several factors such as rainfall, water temperature,
transparency, EC, DO and PO43. Furthermore, Sulehria
et al. (2012) found that water temperature, EC, DO, pH and TDS affected the
rotifer assemblages in floodplains at Dhan, Pakistan;
however, some rotifer species showed a negative correlation with major factors:
Brachionus quadridentatus,
Lecane bulla, L. curvicornis,
and Mytilina acanthophora
were dominant at sites with low values for DO and water temperature, and Keratella tropica had
a high density at sites with low values for EC, TDS, NH3, NO3-,
PO43- and altitude.
The results indicate that seasonal changes are important factors
affecting the environmental factors, seasonal distribution and seasonal
succession in the community of rotifers at each sampling site in the SERS.
CONCLUSİON
The investigation of the monogonont rotifers,
regarding differences found in both seasonal and habitat types, provides a
detailed description of the seasonal variation found within species assemblage,
abundance, and responses to water quality, as well as, the critical factors
which result in their distribution throughout the SBR. Seventy-one rotifers were recorded in this
study with 36.6% of these composed of lecanid
rotifers. The species richness of
rotifers was highest during the rainy season.
The largest habitat type was the reservoir which also had the highest
number of rotifers present. The dominant
species in each of the sampling sites were Lecane
bulla, Polyarthra vulgaris, and Trichocerca similis. Certain species which showed importance were Filinia longiseta which
had a maximum density in the intermittent stream during the rainy season and Brachionus quadridentatus
which showed the highest numbers present in the pond during the winter
season. In addition to this, the
physicochemical parameters of the water data are similar to those found in
natural water bodies throughout conservation areas of Thailand. Water temperature, pH, transparency, ammonia,
and electrical conductivity were found to have both seasonal and spatial
fluctuations. The low pH found in the
intermittent stream during the summer season resulted in the highly acidic
stream found here. Overall, seasons,
habitat types, connectivity and location of sampling sites, as well as the
environmental factors such as water temperature, dissolved oxygen, electrical
conductivity, total dissolved solids, nitrate, orthophosphate, ammonia and
altitude strongly influenced the differences found among the rotifer community
structure in inland waters of the SBR.
To conclude, further studies are required particularly with regard to
crustacean zooplankton in order to gain further knowledge on the overall
zooplankton biodiversity found in Thailand.
Table 1. Geographic coordinates
of the sampling sites within the Sakaerat
Environmental Research Station.
|
Sampling site code |
Latitude 0N |
Longitude 0E |
Altitude (m) |
Habitat type |
|
S1 |
14.476 |
101.888 |
370 |
Stream |
|
S2 |
14.466 |
101.903 |
392 |
Reservoir |
|
S3 |
14.499 |
101.900 |
608 |
Pond |
|
S4 |
14.501 |
101.902 |
560 |
Pond |
|
S5 |
14.506 |
101.919 |
422 |
Stream |
Table
2. Recorded rotifers found at five inland waters with different habitat types,
by season, at the Sakaerat Environmental Research Station. 1—rainy season,
2—winter season, 3—summer season; species occurrence is characterized by
present (+), absent (–).
|
Scientific
name |
Sampling
sites |
||||||||||||||
|
S1 |
S2 |
S3 |
S4 |
S5 |
|||||||||||
|
1 |
2 |
3 |
1 |
2 |
3 |
1 |
2 |
3 |
1 |
2 |
3 |
1 |
2 |
3 |
|
|
Family
Asplanchnidae |
|||||||||||||||
|
Asplanchna sieboldii (Leydig,
1854) |
– |
– |
– |
+ |
+ |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
– |
|
Family
Brachionidae |
|||||||||||||||
|
Anuraeopsis fissa Gosse, 1851 |
– |
– |
+ |
– |
– |
+ |
+ |
– |
+ |
+ |
– |
+ |
+ |
– |
+ |
|
Brachionus calyciflorus Pallas,
1766 |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
+ |
|
Brachionus dichotomus reductus Koste
& Shiel, 1980 |
– |
– |
– |
+ |
– |
+ |
– |
– |
– |
+ |
– |
– |
– |
– |
– |
|
Brachionus donneri Brehm, 1951 |
– |
– |
– |
+ |
– |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
– |
|
Brachionus falcatus Zacharias,
1898 |
+ |
– |
– |
+ |
+ |
+ |
– |
– |
– |
+ |
– |
+ |
– |
– |
+ |
|
Brachionus forficula Wierzejski, 1891 |
– |
– |
– |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
|
Brachionus kostei Shiel,
1983 |
+ |
– |
– |
– |
– |
– |
+ |
+ |
+ |
– |
– |
– |
– |
– |
– |
|
Brachionus quadridentatus
Hermann, 1783 |
+ |
+ |
+ |
+ |
+ |
– |
– |
+ |
– |
– |
+ |
+ |
– |
– |
– |
|
Brachionus quadridentatus mirabilis
Daday, 1897 |
– |
– |
– |
+ |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
|
Keratella cochlearis (Gosse,
1851) |
– |
– |
– |
+ |
+ |
+ |
– |
– |
+ |
– |
– |
– |
+ |
– |
– |
|
Keratella tropica (Apstein,
1907) |
+ |
+ |
+ |
+ |
+ |
+ |
– |
+ |
+ |
+ |
+ |
+ |
– |
– |
– |
|
Plationus patulus (Müller, 1786) |
+ |
– |
+ |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
|
Platyias quadricornis
(Ehrenberg, 1832) |
+ |
– |
+ |
+ |
– |
+ |
– |
– |
– |
+ |
+ |
– |
– |
– |
– |
|
Family
Euchlanidae |
|||||||||||||||
|
Dipleuchlanis propatula (Gosse,
1886) |
– |
– |
– |
– |
– |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
– |
|
Euchlanis dilatata Ehrenberg,
1832 |
– |
– |
– |
– |
– |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
– |
|
Euchlanis incisa Carlin, 1939 |
+ |
+ |
– |
+ |
+ |
+ |
– |
– |
– |
– |
– |
– |
+ |
– |
– |
|
Family
Gastropodidae |
|||||||||||||||
|
Ascomorpha
ovalis (Bergendal,
1892) |
– |
– |
– |
+ |
– |
– |
– |
– |
– |
+ |
– |
– |
– |
– |
– |
|
Family
Hexarthridae |
|||||||||||||||
|
Hexarthra
intermedia (Wiszniewski,
1929) |
– |
– |
– |
+ |
– |
+ |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
|
Family
Lecanidae |
|||||||||||||||
|
Lecane aculeata (Jakubski, 1912) |
– |
– |
– |
– |
– |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
– |
|
Lecane
bulla (Gosse, 1851) |
+ |
+ |
+ |
+ |
+ |
+ |
– |
+ |
– |
+ |
– |
+ |
– |
+ |
+ |
|
Lecane closterocerca (Schmarda, 1859) |
+ |
+ |
– |
+ |
+ |
– |
– |
+ |
– |
+ |
– |
– |
+ |
+ |
– |
|
Lecane curvicornis (Murray,
1913) |
+ |
– |
+ |
+ |
+ |
+ |
– |
– |
– |
– |
+ |
– |
– |
+ |
– |
|
Lecane flexilis (Gosse,
1886) |
– |
+ |
– |
– |
– |
– |
– |
– |
– |
+ |
+ |
– |
– |
– |
– |
|
Lecane furcata (Murray, 1913) |
– |
– |
– |
– |
+ |
– |
– |
– |
– |
– |
– |
– |
+ |
– |
+ |
|
Lecane haliclysta Harring & Myers, 1926 |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
|
Lecane hamata (Stokes, 1896) |
+ |
– |
+ |
+ |
+ |
+ |
– |
– |
+ |
– |
– |
– |
+ |
+ |
+ |
|
Lecane hornemanni
(Ehrenberg, 1834) |
– |
+ |
– |
– |
– |
+ |
– |
– |
+ |
– |
– |
+ |
– |
– |
– |
|
Lecane
lateralis Sharma, 1978 |
– |
– |
– |
– |
+ |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
– |
|
Lecane latissima Yamamoto,
1955 |
– |
– |
– |
– |
– |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
– |
|
Lecane leontina (Turner,
1892) |
– |
– |
– |
+ |
+ |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
– |
|
Lecane ludwigii (Eckstein,
1883) |
+ |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
|
Lecane luna (Müller, 1776) |
– |
– |
– |
+ |
– |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
– |
|
Lecane lunaris (Ehrenberg,
1832) |
+ |
+ |
– |
+ |
+ |
+ |
– |
– |
– |
– |
+ |
+ |
– |
– |
+ |
|
Lecane nitida (Murray, 1913) |
– |
– |
– |
+ |
– |
+ |
– |
– |
+ |
– |
– |
– |
– |
– |
– |
|
Lecane obtusa (Murray, 1913) |
– |
– |
– |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
|
Lecane papuana (Murray,
1913) |
– |
– |
– |
+ |
– |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
– |
|
Lecane
pyriformis (Daday, 1905) |
– |
– |
– |
– |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
|
Lecane quadridentata
(Ehrenberg, 1830) |
+ |
+ |
– |
+ |
+ |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
– |
|
Lecane signifera (Jennings,
1896) |
– |
– |
– |
+ |
+ |
+ |
– |
+ |
– |
– |
– |
+ |
– |
– |
– |
|
Lecane stenroosi (Meissner,
1908) |
– |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
|
Lecane superaculeata Sanoamuang & Segers, 1997 |
– |
– |
– |
– |
– |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
– |
|
Lecane tenuiseta Harring, 1914 |
– |
– |
– |
– |
– |
– |
– |
– |
+ |
– |
– |
– |
– |
– |
– |
|
Lecane unguitata (Fadeev, 1926) |
– |
– |
– |
+ |
– |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
– |
|
Lecane ungulata (Gosse,
1887) |
– |
– |
– |
+ |
– |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
– |
|
Family
Lepadellidae |
|||||||||||||||
|
Colurella uncinata (Müller,
1773) |
– |
– |
– |
– |
– |
– |
– |
+ |
– |
– |
– |
– |
+ |
+ |
+ |
|
Lepadella acuminata
(Ehrenberg, 1834) |
– |
– |
– |
– |
– |
– |
– |
– |
– |
+ |
+ |
– |
– |
– |
– |
|
Lepadella dactyliseta (Stenroos, 1898) |
+ |
+ |
– |
+ |
+ |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
– |
|
Lepadella
patella (Müller, 1773) |
+ |
+ |
– |
+ |
– |
+ |
– |
+ |
+ |
– |
+ |
+ |
– |
– |
+ |
|
Lepadella quadricarinata (Stenroos, 1898) |
– |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
|
Lepadella rhomboides (Gosse,
1886) |
+ |
– |
– |
– |
– |
– |
– |
+ |
+ |
– |
– |
– |
+ |
+ |
+ |
|
Family
Mytilinidae |
|||||||||||||||
|
Mytilina acanthophora Hauer,
1938 |
+ |
+ |
– |
– |
– |
– |
+ |
+ |
+ |
– |
+ |
– |
– |
– |
+ |
|
Mytilina ventralis
(Ehrenberg, 1830) |
+ |
– |
– |
– |
+ |
+ |
+ |
– |
– |
– |
+ |
– |
– |
– |
– |
|
Family
Notommatidae |
|||||||||||||||
|
Cephalodella forficula
(Ehrenberg, 1830) |
– |
– |
– |
+ |
– |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
+ |
|
Cephalodella gibba (Ehrenberg, 1830) |
– |
– |
– |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
|
Monommata longiseta (Müller,
1786) |
– |
– |
– |
+ |
+ |
+ |
– |
– |
– |
– |
– |
– |
– |
+ |
– |
|
Family
Scaridiidae |
|||||||||||||||
|
Scaridium longicaudum (Müller,
1786) |
– |
– |
– |
+ |
– |
+ |
– |
– |
– |
– |
+ |
– |
– |
– |
– |
|
Family
Synchaetidae |
|||||||||||||||
|
Polyarthra
vulgaris Carlin, 1943 |
+ |
+ |
+ |
+ |
+ |
+ |
+ |
+ |
+ |
– |
– |
+ |
+ |
– |
+ |
|
Family
Testudinellidae |
|||||||||||||||
|
Testudinella
patina (Hermann, 1783) |
+ |
– |
– |
+ |
+ |
+ |
– |
– |
– |
– |
+ |
+ |
– |
– |
– |
|
Family
Trichocercidae |
|||||||||||||||
|
Trichocerca bicristata (Gosse,
1887) |
– |
– |
– |
– |
+ |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
– |
|
Trichocerca bidens (Lucks, 1912) |
– |
– |
– |
+ |
+ |
– |
– |
+ |
– |
– |
+ |
+ |
– |
– |
– |
|
Trichocerca capucina (Wierzejski & Zacharias, 1893) |
– |
– |
– |
– |
+ |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
– |
|
Trichocerca cylindrica (Imhof, 1891) |
– |
– |
– |
– |
– |
– |
– |
+ |
– |
– |
– |
– |
– |
– |
– |
|
Trichocerca insulana (Hauer,
1937) |
– |
+ |
– |
+ |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
|
Trichocerca pusilla (Jennings, 1903) |
– |
– |
– |
– |
– |
– |
+ |
– |
+ |
+ |
– |
+ |
– |
– |
– |
|
Trichocerca scipio (Gosse, 1886) |
– |
– |
– |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
|
Trichocerca similis (Wierzejski,
1893) |
– |
– |
– |
+ |
+ |
+ |
+ |
+ |
+ |
+ |
+ |
+ |
– |
– |
– |
|
Family
Trichotriidae |
|||||||||||||||
|
Macrochaetus sericus (Thorpe, 1893) |
– |
– |
– |
+ |
– |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
– |
|
Trichotria tetractis
(Ehrenberg, 1830) |
+ |
– |
– |
+ |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
– |
– |
|
Family
Trochosphaeridae |
|||||||||||||||
|
Filinia longiseta
(Ehrenberg, 1834) |
– |
– |
– |
+ |
+ |
+ |
+ |
– |
– |
+ |
– |
+ |
+ |
– |
– |
|
Filinia opoliensis
(Zacharias, 1898) |
– |
– |
– |
+ |
+ |
+ |
– |
– |
– |
– |
– |
– |
– |
– |
– |
|
Total
number of species during each season |
23 |
17 |
9 |
44 |
31 |
43 |
9 |
14 |
14 |
13 |
14 |
15 |
10 |
7 |
13 |
|
Species
richness at each sampling site |
29 |
57 |
24 |
25 |
19 |
||||||||||
For
figures & image – click here
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