Epilithic
diatoms of urban River Dilimi, Jos, Nigeria
Cyril C. Ajuzie
Aquaculture, Freshwater &
Marine Ecology Research Lab, Fisheries Unit, Department of Animal Production,
University of Jos, Nigeria
Abstract: For a long time
now, diatoms have been used to determine the ecological integrity of freshwater
bodies. Despite the ecological significance of diatoms in freshwater bodies,
the taxonomic composition and autecology of diatoms in many freshwater bodies
of Nigeria are yet to be investigated. The present work was carried out to
ascertain the taxonomic composition of epilithic diatoms of River Dilimi in
Jos, Nigeria. The physical and chemical properties of the river at two urban
stations (were diatoms were sampled) were also determined. Mean NO3 (mg l-l) was 0.9 (+
0.14) at the upstream station and 1.06 (+ 0.08) at the downstream
station. Mean PO4 (mg l-l) was 0.03 (+ 0.14) at
the upstream station and 1.3 (+ 0.7) at the downstream station. A total of 28
diatom genera and 83 species were documented from the study sites. Out of the
83 species, 59 occurred at the upstream site and 45 at the downstream site. The
percent community similarity between the two sites was 24.71 %. At the upstream
site the most common species were Meridion
circulare (3.5 %), Navicula mutica
(3.6 %), Nitzschia amphibia (3.0 %)
and Synedra ulna (3.4 %). At the
downstream site the most common species were Cyclothella meneghiniana (4.4 %), Nitzschia amphibia (8.8 %), Nitzschia
palea (5.0 %), Synedra ulna (12.8
%), Tabellaria fenestrate (3.8 %) and
Tabellaria flocculosa (3.1 %). Since
both NO3 and PO4 concentrations in the river indicate
that the river is polluted, the diatoms recorded in this study may be grouped
as pollution tolerant diatoms, bearing in mind, too, that the river water is
discoloured throughout the year.
[Cyril C. Ajuzie. Epilithic diatoms of urban River Dilimi,
Jos, Nigeria. Nat Sci 2016;14(8):88-97]. ISSN 1545-0740 (print);
ISSN 2375-7167 (online). http://www.sciencepub.net/nature. 13. doi:10.7537/marsnsj14081613.
Keywords: epilithic diatoms;
River Dilimi; Jos; Nigeria
1.
Introduction
Awareness of the deleterious effects of human pressures on aquatic
environments has resulted in a long history of monitoring of freshwater bodies
using biological indicators (Hellawell, 1986; De Pauw and Hawkes, 1993;
Rosenberg and Resh, 1993; Knoben et al., 1995). Monitoring of the quality of
running waters involve the use of several diatom-based indices (see Prygiel and
Coste, 1993; Kelly and Whitton, 1995; Whitton and Kelly, 1995). Consequently,
several studies have addressed the tolerances and preferences of diatoms along
a number of environmental gradients (e.g. salinity, pH, trophy, saprobity and
current preference; e.g. Denys, 1991a, b; van Dam et al., 1994; Rott et al.,
1997).
Diatoms are a large and diverse group of single-celled microalgae. They
are distributed throughout the world in nearly all types of aquatic systems and
are one of the most important food resources in marine and freshwater
ecosystems. Because there are many thousands of taxa with diverse ecological
requirements, their siliceous remains are used extensively as environmental
indicators in studies of climate change, acidic precipitation and water quality
(see Stoermer and Smol, 1999; Potapova and Charles, 2002).
Despite the ecological significance of diatoms in freshwater bodies, the
taxonomic composition and autecology of diatoms in many freshwater bodies in
Nigeria are yet to be investigated. This is in agreement with the observations
of Alfinito and Lange-Bertalot (2013) who noted that the freshwater diatom
flora of Tropical West Africa is still poorly investigated. The present paper
presents a report on the community composition of epilithic diatoms of an urban
section of River Dilimi, to contribute to knowledge of freshwater diatoms in
Nigeria. forests.
2. Material
and Methods
Study area
The urban section of Dilimi River runs through Jos North Local
Government Area of Plateau State, Nigeria (Figure 1). Two sampling sites that
included an upstream sampling station at about 200 m away from (and downstream
of) the British-American bridge, and a downstream sampling location at the
University of Jos pedestrian bridge, which links the University of Jos
Students’ Village (located on the left bank of the river) with the university’s
permanent site at the other bank. The areas adjacent to the river banks at the
British-American axis of the river (because of the massive granite rocks that
dot the area) have comparatively sparse human populations than those adjacent
to the river banks at the downstream axis (i.e. from ca. 400m after the
British-American bridge to the pedestrian bridge at the permanent site of the
University). By the time the river reaches the permanent site of University of
Jos, it has passed through many densely populated poor neighbourhoods of Jos
town, where houses and yards have direct links with the river, and the flood
plains intensively farmed. A consequence of encroaching into the river banks
was that in July 2012 the overflow of the river (after heavy rains) washed away
many houses and farm lands that were situated along the banks (Ezema, 2013).
The locals defecate on the banks and in the river channel. House-hold organic
wastes and wastes from business houses are ceaselessly emptied into the river
by inhabitants of these poor neighbourhoods. The poor farming practices on the
floodplains cause the river to be enrich with nutrients and silt. The water is
discoloured throughout the year.
Figure 1: Study area with sampling sites 1 & 2 (N/B: UJSV =
University of Jos Students’ Village; UJPS = University of Permanent Site).
Modified from Adebajo et al. 2012
Physico-chemical parameters studies
Temperature was measured on the spot using a mercury thermometer. Water
conductivity, total dissolved solids (TDS) and pH were also measured on the
spot with a multi-parameter water tester (HANNA® instruments).
Nitrate nitrogen and phosphate phosphorus were equally measured on the spot
with the JBL TESTSETTM reagents for iron, nitrate, and phosphates.
Dissolved oxygen and biochemical oxygen demand (BOD5) were
determined by iodometric (Winkler) method (USGS, 2015).
Collection of epilithic diatoms
According to Stevenson (1990), periphyton samples should be collected
during periods of stable flow, since high flows can scour the stream bed and
result in flushing off the periphyton. Recovery after high discharge can be as
rapid as seven days if severe scouring of substrata did not occur (Stevenson,
1990). Bearing this in mind, the two sites were sampled twice in May 2013. The
first was before the first heavy rain of the year and the second was 10 days
after the rain. Four submerged stones (one each from the riffles, runs, shallow
pools and nearshore areas of the river) were sampled randomly at each sampling
location, by wading into the river. Each stone was placed in a white laboratory
tray. Diatoms were brushed off each of the stones, using a tooth brush and
rinsed with limited quantity of river water. The cap of the sample holder (16.6
cm2) was used to define a sampling circle on each stone, by placing
it on the stone. A circular mark was scratched on the stone around the outside
of the cap with the tip of a scalpel blade (Biggs and Kilroy, 2000). Diatoms
were sampled within the circle. The samples were preserved with 4 % formalin.
This study was planned with emphasis
on the spatial composition of the diatoms, with reference to the study sites.
Thus, even though diatoms were sampled at two different times, samples from
stones at each sampling station were pooled to form a composite sample for that
location (see Kelly et al., 1998; Fetscher et al., 2014). In the
laboratory, the pooled samples were transferred to 250 ml sample bottles and
distilled water added to bring the sample volume to 200 ml.
Table 1. Physical and
chemical parameters measured at the sampling sites (means and standard
deviations)
Parameter Upstream Downstream
Air Temperature (°C) 26.3
+ 3.9 30.8
+ 2.6
Water Temperature (°C) 23.8
+ 3.4 27.8
+ 1.5
Dissolved Oxygen (mg l-l) 7.1
+ 0.07 4.3ns1
+ 0.28
BOD5 0.75*1
+ 0.07 3.7
+ 0.14
Fe (mg l-1) 0.05ns2+0 0.65+0.07
NO3 (mg l-l) 0.9ns3
+0.14 1.06
+0.08
PO4 (mg l-l) 0.03ns4
+0.14 1.3
+0.7
NO3:P04
ratio 30 0.8
pH 7.8
+ 0.3 7.9 + 0.4
Conductivity (µs cm-1) 213*2
+ 1.41 512
+ 51.62
Total Dissolved Solids (ppm) 112ns5
+ 7.07 257
+ 26.16
N/B: ns = not statistically significant; * = statistically significant
(ns1 paired t(1) = 11.4, p = 0.056 ; ns2 paired t(1)
= 12, p = 0.053; ns3 paired
t(1) = 1, p = 0.50; ns4 paired t(1) = 2.49, p = 0.24; ns5
paired t(1) = 10.7, p = 0.059; *1
paired t(1) = 19.67, p = 0.032 ; *2 paired t(1) = 19.67, p =
0.03)
Identification and enumeration
of the diatoms
Each sample bottle was moderately shaken in order to get a homogenous
solution before a subsample of 50 µl was taken for microscopic analysis, which
involved identification and counting of the diatom species. The 50 µl subsample
was dropped on a plane microscope slide and carefully covered with a cover slip
to exclude bubbles. The slide was then transferred to the microscope stage for
analyses. Stancheva et al. (2012) suggested the use of plane microscope slide
instead of a counting chamber for proper identification and counting of mixed
microalgae species. Three hundred (300) diatom cells were identified to species
level and enumerated at 400x magnification. Although larger counts reduce
uncertainty associated with organism counts (Birks, 2010), it has been shown
that the benefit of increasing counts above 300 is not high (Stancheva et al.,
2012). The diatoms were viewed under randomly-selected six viewing fields.
Shear stress may be very high on stone surfaces in lotic freshwater bodies,
resulting in patchy distribution of algae on substrates. This has permitted
some workers to restrict the number of viewing fields to six (e.g. Baffico et
al., 2004). Several diatom identification keys for freshwater ecosystems
(including Durand and Leveque, 1980; Pentecost, 1984; Biggs and Kilroy, 2000)
and the web were used in the identification of the species.
3. Statistics
Species Density
Species density was calculated thus: C/A = (TN x SV x ACS)/(AVF x NVF x
VSS x SA), where C/A is the number of cells or filaments, as the case may be,
per surface area of stone sampled; TN, total number of individuals; SV, sample
volume; ACS, area of cover slip; AVF, area of viewing field at 400x
magnification; NVF, number of viewing fields scanned; VSS, volume of subsample;
and SA, surface area of stone sampled. The area of stone surface sampled was
calculated as the surface area of an individual stone (mm2)
multiplied by the number of stones sampled for that site (see Biggs and Kilroy,
2000).
Percent (%) composition of diatom species at the two
sites
This was calculated for each species by dividing species density (C/A)
of each species by the total density summed from values recorded for each of
the species in the site sampled, and the result multiplied by 100; e.g. %
Composition of a species “A” was given as: A = (a/b) x 100 %, where: a is the calculated C/A for species A,
and b is ∑ C/A for a sampled location
(e.g. Stevenson, 1990).
Shannon Index (H’) was used to calculate the species diversity index at
each study site. This was calculated thus:
H’ = − ∑ [(ni/N) x
ln (ni/N)], where: ni =
number of individuals of each species (the ith species),
N = total number of
individuals for the site, and ln = the natural log of the number.
Percent (%) community similarity
After calculating H’, the percent similarity index of sot algae in the
two sites was calculated. This was obtained by multiplying a calculated Jaccard
index by 100. Jaccard Index (J) was calculated thus:
J = sc/(sa + sb + sc), where: sa and sb are the numbers of species
unique to samples a and b, respectively, and sc is the number of species common
to the two samples.
A Paired Two Sample for Means t-Test [P(T<=t) two-tail] was performed
to further test if differences observed in some of the data set were statistically
significant (ɑ = 0.05).
4. Results
Physico-chemical parameters studies
The river water was discoloured throughout the sampling period (and is
indeed discoloured throughout any given year). Mean water temperature was
23.8°C (upstream) and 27.8°C (downstream). These temperatures were, however,
lower than air temperatures at the respective sites. Water temperature depended
on the time of the day records were taken, with water temperature increasing as
the sun rises. Though dissolved oxygen concentration was relatively higher at
the upstream sampling site than at the downstream station, the difference was
not statistical significant. Biochemical oxygen demand, on the other hand, was
significantly higher downstream. There was no statistically significant
difference in Fe, NO3 and PO4 concentrations at the two
sites. However, NO3 and PO4 concentrations were relatively higher
downstream. N:P ratio approached unity (0.8) downstream, while upstream the
ratio was 30:1. Both sites had similar pH readings, and which indicated that
the river is weakly alkaline. Whereas conductivity was significantly higher at
the downstream site than at the upstream station, the difference in TDS
concentrations was not statistically significant (Table 1).
The diatoms
A total of 28 diatom genera and 83 species were documented from the
study sites. Out of the 83 species, 60 occurred at the upstream site and 46 at
the downstream site (Table 2). Thus, the upstream site was richer in species
than the downstream site. The percent community similarity between the two
sites was 24.71 %. Shannon diversity index was higher (4.06) at the upstream
site than at the downstream site (3.27). These results are shown in Table 3. At
the upstream site the genera Gomphonema
and Navicula were the most common,
and at the downstream site it was Nitzschia
that was the most common genus (Table 4). The percent occurrence of the most
common species at each of the two sites is presented in Table 5. At the
upstream site the most common species were Meridion
circulare (3.5 %), Navicula mutica
(3.6 %), Nitzschia amphibia (3.0 %)
and Synedra ulna (3.4 %). At the
downstream site the most common species were Cyclothella meneghiniana (4.4 %), Nitzschia amphibia (8.8 %), Nitzschia
palea (5.0 %), Synedra ulna (12.8
%), Tabellaria fenestrate (3.8 %) and
Tabellaria flocculosa (3.1 %).
5. Discussion
Physical and Chemical Parameters
Water temperature was dependent on air temperature, which increased as
the sampling time approached noon. Sample collections were carried out at the
two sites on the same day between 09:00 and 12:00, beginning at the upstream
site. The foregoing explains why water temperature was relatively higher at the
downstream site. Although there was no statistically significant difference in
dissolved oxygen concentrations between the two sampling sites, the higher BOD
value at the downstream site could imply that the downstream site was subjected
to more nutrient loads than the upstream site. This view is supported by the
relatively high concentrations of NO3 and PO4 at the
downstream site. The increase in nutrients, especially those of organic origin,
will cause an increase in bacteria that degrade them. The increase in bacterial
activity will, in turn, provoke a high BOD level (see Pearson and Rosenberg,
1978).
Table 2: Diatom
species at the upstream and downstream sampling sites of River Dilimi, Jos
Diatom species Presence
(+) or Absence (-)
Upstream
site Downstream
site
Achnanthes
exigua Grun. - +
Achnanthes exiguoides Compère + -
Achnanthes lanceolata (Bréb.)
Grun. - +
Achnanthes
linearis forma curta H.L. Smith + -
Achnanthidium cf. latecephalum
Kobayasi - +
Achnanthidium
minutissimum (Kütz.) Czarn. + +
Amphora
ovalis (Bréb.) Kütz. + -
Amphora
veneta var. capitata Haw. - +
Anomoeoneis
sphaerophora (Ehr.) Pfitzer + -
Asterionella
formosa Hass. + -
Brachysira sp. + -
Cyclotella
meneghiniana Kütz. - +
Cyclotella stelligera (Cl. & Grun.) Van Heurck - +
Cymbella microcephala Grun. - +
Cymbella minuta Hilse + -
Cymbella ventricosa Kütz. + -
Diatoma hiemale var. mesodon (Ehrenb.) Grun. + -
Diatoma mesodon (Ehr.) Kütz. + -
Diatoma vulgare Bory + -
Diploneis gruendleri (A.S.) Cl. - +
Diploneis puella (Schum.) Cl. + -
Eolimna minima (Grun.) Lange-Bert. + +
Fragilaria construens (Ehr.) Grun. - +
Fragilaria vaucheriae (Kütz.) Peters. + -
Frustulia rhomboides (Ehr.) De Toni + -
Frustulia vulgaris (Thwaites) De Toni + -
Gomphonema affine Kütz. + -
Gomphonema angustatum Kütz. + -
Gomphonema augur Ehr. + +
Gomphonema gracile Ehr. + -
Gomphonema lanceolatum var. insignis (Greg.) Cl. - +
Gomphonema minutum (Ag.) Ag. + -
Gomphonema olivaceum
Lyng. + +
Gomphonema parvulum (Kütz.) Kütz. + +
Gomphonema pumilum (Grun.) Reich &
Lange-Bert. + -
Luticola mutica (Kütz.) Mann in Round & al. + +
Mastogloia smithii Thwaites + +
Melosira granulata (Ehr.) Ralfs + +
Melosira sulcata (Ehr.) Kütz. + -
Melosira varians Ag. + +
Meridion circulare (Grev.) Ag. + -
Navicula amphiceropsis Lange-Bert. & Rumrich - +
Navicula atomus Nægeli + +
Navicula capitoradiata Germ. + +
Navicula cincta (Ehr.) Ralfs - +
Navicula cryptocephala Kütz. + +
Navicula elegans W. Sm. + -
Navicula elkab Müll. + -
Table 2 contd.:
Navicula humilis Donk. + -
Navicula cf. margalithii
Lange-Bert. + -
Navicula minima Grun. + -
Navicula mutica Kütz. + -
Navicula pygmaea Kütz. + -
Navicula radiosa Kütz. + -
Navicula ramosissima (Ag.) Cl. + -
Navicula seminulum Grun. + -
Navicula subrhynchocephala Hust. + -
Navicula tripunctata (Müll.) Bory - +
Navicula tripuctata var. schizonemoides Van Heurck + -
Navicula vaucheriae Peters. + -
Navicula veneta Kütz. - +
Neidium affine var. genuina Cl. - +
Neidium affine var. genuine forma minor Cl. + -
Nitzschia amphibia Grun. + +
Nitzschia capitellata Hust. - +
Nitzchia communis Rabenh. + -
Nitzschia compressa (Bailey) Boyer - +
Nitzschia dissipata (Kütz.) Grun. + +
Nitzschia epithemioides Grun. - +
Nitzschia kuetzingioides Hust. - +
Nitzschia palea (Kütz.) W. Sm. + +
Nitzschia perminuta (Grun.) Perag. - +
Nitzschia sublinearis Hust. - +
Pinnularia biceps Greg. - +
Pinnularia microstauron (Ehr.) Cl. + -
Pinnularia subcapitata Greg. + +
Pinularia viridis Nitzsch. + +
Pleurosira laevis (Ehr.) Compère - +
Rhoicosphenia curvata (Kütz.) Grun. + +
Sellaphora pupula (Kütz.) Mereschk. + +
Sellaphora sp. - +
Stauroneis crucicula (W. Sm.) Donkin + -
Synedra ulna (Nitzsch) Ehr. + +
Tabellaria flocculosa (Roth) Kütz. + +
Tabellaria fenestrata (Lyng.) Kütz. - +
The major source of N and P loadings in the downstream section of the
study sites is untreated sewage from homes and business centres, as well as
direct defecation into the river banks and river channel. Phosphorus
enrichment, for example, is associated with increased microbial biomass and
activity, resulting in faster rates of decomposition and nutrient cycling
downstream of aquatic ecosystems (e.g. McCormick et al., 1998). Jarvie et al.
(2002) observed that phosphorus treatment at selected major sewage treatment
works in the upper Thames basin in the UK resulted in significant reductions in
in-stream P concentrations. To my knowledge, there is no such treatment plant
linked with the Dilimi River. Soil tillage and fertilizer applications are also
common habits in the downstream axis of the river. This, without doubt,
contributed soil materials and nutrients to the river via runoffs.
Inorganic nutrients and organic enrichments are major water quality
concerns in streams and rivers (Porter et al., 2008). Nitrogen and phosphorus
are nutrient sources that may cause increased growth of aquatic plants and
algae. Hence, N and P from farmland runoff or industrial and municipal
discharges have been associated with widespread and expanding eutrophication of
freshwaters (Millennium Ecosystem Assessment, 2005; Carpenter, 2008). Carpenter
(op. cit.) suggested that control
measures for runoff of both N and P would include decreased use of fertilizers,
containment and treatment of manure, and tillage practices that conserve soil.
Though many researchers are of the opinion that P appears to be the major
pollutant that constrains algae production in freshwater ecosystems (Schindler,
1977; Carpenter, 2008), comparison of algal biotest results and chemical
nutrient concentrations in lakes suggest that a mass N:P ratio above 17
indicates P limitation, a ratio below 10 indicates N limitation and values
between 10 and 17 indicate that either of the nutrients may be limiting (see
Ulén, 1978; Forsberg and Ryding, 1980; Fu and Winchester, 1994; Hellström,
1996; McCormick et al., 1998; Ekholm, 2008). From the foregoing it could be
stated that in Dilimi River, P is the limiting nutrient at the upstream site,
and N at the downstream station. This may have resulted from high organic
pollution load downstream (see Kelly and Whitton, 1995).
Although the differences in both NO3 and PO4
concentrations at the upstream and downstream sites were not statistically
significant, the values recorded for these compounds during this study suggest
that the river is rich in N and P loads, and, hence, polluted. It has been
argued that nitrate-nitrogen concentrations above 3 mg/L and any detectable
amounts of total phosphorus (above 0.025 mg/L) may be indicative of pollution
from fertilizers, manures or other nutrient-rich wastes (see Pond Facts #2 of
Penn State Extension). The downstream site is located immediately the river
course has passed through a heavily populated and largely poor neighbourhoods
in Jos North Local Government. Some inhabitants of these neighbourhoods farm on
the floodplains, tilling and applying fertilizers to the soil. Added to this, the amount of municipal wastes and raw
sewage from these settlements that find their way into Dilimi River,
particularly between the upstream sampling site and the downstream site (though
yet to quantified and reported in the literature) is disturbing. Runoffs from
these neighbourhoods empty tons of pollutants into this river every year.
The river is weakly alkaline at both sites. This might imply that the
river is rich in biodiversity. The high number of diatom species documented
during this study corroborates this statement. In contrast, acidic freshwater
bodies are characterized by benthic algal communities with low diversity
(Whitton and Diaz, 1981); and Baffico et al. (2004) reported that the epilithon
of an acidic stream in Argentina was dominated (99% of total biomass) by one
genus: Gloeochrysis (Chrysophyceae).
The high electrical conductivity and TDS values witnessed at the downstream
site are indications that this section of the river had more solutes (including
chemical ions) than the upstream site. Electrical conductivity and the amount
of TDS in a water body are controlled by many factors, including human
activities within the immediate surroundings of the ecosystem. As earlier
noted, the downstream section of the river is heavily impacted by the
activities of the dense human populations along its course. The mineralisation
of pollutants by bacteria will cause the river to have more solutes and, hence,
elevated EC and TDS levels.
Table 3: Species richness,
Shannon diversity and % community similarity of diatoms at the sampling sites
of River Dilimi, Jos, Nigeria
Index Upstream Downstream
Species Richness 60
species 46
species
Shannon Index (H’) 4.06 3.27
Community Similarity (%) 24.71
Table 4: Percent composition
of the most common diatom genera at the sampling sites
Diatom genus %
composition upstream %
composition downstream
Gomphonema 15.0
7.5
Navicula 28.0 12.0
Nitzschia 10.0 25.0
Table 5: Percent
composition of the most common diatom species at the sampling sites
Species %
at upstream site %
at downstream site
Cyclothella meneghiniana
0
4.4
Gomphonema minutum 2.8
0
Gomphonema parvulum 2.8
2.8
Gomphonema pumilum 2.8
0
Meridion circulare 3.5
1.4
Navicula atomus 2.5
2.3
Navicula capitoradiata 2.7
2.0
Navicula mutica 3.6
0
Nitzschia amphibia 3.0
8.8
Nitzschia palea 2.6
5.0
Synedra ulna 3.4 12.8
Tabellaria fenestrata
0
3.8
Tabellaria flocculosa 1.5
3.1
The diatoms
The diatoms recorded in this study could well be described as pollution
tolerant organisms. As already noted, the concentration levels of both N and P
nutrient elements at the study sites suggest that the river is polluted. Kelly
and Whitton (1995) observed that the genus Achnanthes is common across a
wide range of conditions, and that A. minutissima is often the dominant
diatom in oligo/mesotrophic rivers and streams, whereas A. lanceolata tends
to be most common in more nutrient-rich conditions. In the present study,
whereas A. minutissima appeared in
both the upstream and downstream sites, suggesting a wide tolerance to
concentrations of nutrients, A.
lanceolota was only observed in the comparatively more nutrient-loaded
downstream site; thus, corroborating the findings of Kelly and Whitton (1995).
Similarly, Achnanthes exigua was
present only in the downstream site, suggesting high tolerance to nutrient
pollution. Wan Maznah and Mansor (2000) had described A. exigua as a pollution tolerant diatom.
Kelly and Whitton (1995) also reported that many forms of Navicula (and
Sellaphora) are usually abundant in eutrophic waters, and that Gomphonema parvulum is a pollution
tolerant species. These reports strengthen the conclusions drawn from the
present study. Blinn and Herbst (2003) observed, too, that Cyclotella meneghiana is associated with conditions that define
freshwater habitats with lower ecological integrity. Many species of Nitzschia (Kelly
and Whitton, 1995; Blinn and Herbst, 2003),
including Nitzschia amphibia and Nitzschia palea (Wan Maznah and Mansor,
2000) have been described as pollution tolerant species. Synedra ulna is also a pollution tolerant species (Lange-Bertalot,
1979).
6. Conclusion
The urban section of River Dilimi is polluted.
Thus, the diatoms recorded in this study could be described as
pollution-tolerant organisms.
Acknowledgements
This work was supported by Nigerian TETFund research grant 2013. Mr. A.
Uja helped with the determination of DO and BOD of water samples.
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