Phytoplankton Community Structure of a Mangrove Habitat in the Arid Environment
of Oman: The Dominance of Peridinium quinquecorne
Michel R. Claereboudt,
Little is known about the physical, biological and chemical oceanographic conditions
of Omans Avecenia marina
dominated coastal mangrove ecosystem. This study provided information on the
phytoplankton community structure and biomass (Chla) and their variability in
relation to chemical and physical changes in the coastal mangrove ecosystem
of Bandar Khyran Bay. Monthly assessments of phytoplankton and (chlorophyll
a) accompanied by CTD and nutrient measurements were carried out at one station
from January 2001 to December 2001, Chla were moderately low throughout in all
probability due to the high water temperatures, low nutrient concentrations
and high turbidity as well as the absence of diatoms in the phytoplankton community.
The contribution of net phytoplankton >20 μm to total biomass was minimal
throughout the study period except during December where it accounted for 53%
of the total biomass. Phytoplankton populations within the size range of 0.74-<5
μm accounted for the highest biomass, followed by the size fraction (5-20
μm). A total of 25 net phytoplankton taxa were identified during the study.
The overall composition of the community did not show any marked seasonal variations.
The net plankton was dominated by a single species of dinoflagellate Peridinium
quinquecorne Abe, 1927 throughout the year comprising more the 90% of the
species counts where at times it reached bloom proportions. It has been hypothesized
that ability of this species to thrive under a range of physical and chemical
conditions allows it to survive and outcompete most other phytoplankton species
to cite this article:
Khalid Al-Hashmi, Adnan Al-Azri, Michel R. Claereboudt, Sergey Piontkovski and S.M.N. Amin, 2013. Phytoplankton Community Structure of a Mangrove Habitat in the Arid Environment
of Oman: The Dominance of Peridinium quinquecorne. Journal of Fisheries and Aquatic Science, 8: 595-606.
Received: October 05, 2012;
Accepted: November 02, 2012;
Published: June 06, 2013
In coastal areas, mangroves are ecologically as well as economically important
since they serve as nursery grounds, refuge for many fish and crustacean species
(Harrison et al., 1994) and provide favorable
conditions for algal growth (Faust and Gulledge,1996).
Mangroves represent unique tropical environments and are vital to the productivity
of adjacent coastal marine communities (Odum et al.,
1982).They export their production of organic matter in the forms of detritus
and living organisms to the adjacent coastal waters (Woodroffe,
Throughout the world approximately 54 species of plants belonging to about
20 genera in 16 families have been recognized as mangroves (Tomlinson,
1986). In contrast, the only surviving mangrove species left in the Sultanate
of Oman is the most salt-tolerant of all species, i.e., Avicennia marina
(Fouda and Al-Muharrami, 1996).This is due to the extremely
arid and saline conditions prevailing in the Arabian Peninsula, with very little
rain in most areas and very limited or no other freshwater runoff (Sheppard
et al., 1992).
Currently, the total area of mangrove coverage in the Sultanate of Oman is
estimated at around 1088 hectares (Fouda, 1995; Fouda
and Al-Muharrami, 1996) scattered around the coast at approximately 30 sites.
The BK mangroves occupy an area of 83 ha making it the 5th largest mangrove
in Oman (Fouda, 1995).
To date there has been no study of the physical, biological and chemical oceanography
of Oman mangroves and furthermore their influence on coastal waters remains
poorly understood. This manuscript is part of a one-year study of the Bay of
BK in which we report the seasonality of phytoplankton in relation to environmental
conditions within this mangrove ecosystem.
MATERIALS AND METHODS
Site description: This study was carried out in the Bay of Bandar Khyran
(BK) (Fig. 1), located about 25 km from Muscat. BK is a small
village at the southeastern margin of the capital area at 23°3026N
(Latitude) and 58°4348E (Longitude). The inner region of the
Bay is a shallow tidal mud-flat as result of which the water column is very
turbid. All along its margins, the bay is lined with Avicennia marina
mangrove forest extending about 83 ha (Fouda, 1995).
Sampling strategy: One station was sampled "Mangrove", in the inner
region of western side of the Bay in the mangrove channels. Sampling was carried
out on a monthly basis (except during April, May and June when sampling was
done twice) over the period f from January 22-December 25, 2001.
Water sampling was undertaken during high tide periods in order to offset tidal
influences on our findings and also because it was not possible to reach the
station during low tide to perform effective zooplankton tows.
In situ temperature, salinity, dissolved oxygen, light penetration and
turbidity were measured using a Idronaut-Ocean Seven316 CTD (conductivity,
temperature, depth sensor) probe. Surface water samples (250 mL) were collected
by Niskin bottles for the analyses of nitrate, nitrite, phosphorus and silica.
Samples were immediately frozen and then thawed and analyzed for the detection
of nutrients using a 5-channel SKALAR FlowAccess auto-analyzer according to
the procedure described by Strickland and Parsons (1972).
In situ Chl a profiles were estimated by direct fluorescence using fluorescence
probe mounted on the CTD. Size fractionated biomass of phytoplankton was established
by filtering 2 L of water samples immediately through three different filters:
(1) Whatman GF/F glass fiber filter with 0.74 μm pore size, (2) nytex screening
with 5 μm mesh size and (3) nytex mesh screening with 20 μm mesh size
and the filters were kept frozen under 4°C in darkness until the time of
analysis. In the laboratory, filters were placed into a 90% acetone solution
overnight under cold and dark conditions for extraction of Chl a and then ground
to facilitate extraction of Chl a. Chl a concentrations were determined using
a Turner Design Model 10-AU Fluorometer. Chl a concentrations were corrected
for phaeophytin using the acidification method (Strickland and
Parsons, 1972). Pure Chl a standard was used to calibrate the fluorometer.
Chl a values were calculated using the equation given in (Strickland
and Parsons, 1972).
Five hundred mililiter aliquots of water samples were also collected and preserved
with 1% Lugols Iodine solution for phytoplankton species identification
and cell count determinations. In the laboratory, samples were allowed to settle
in 15 mm diameter tubes before they were counted using an inverted Ix50 Olympus
microscope. For identifying individual marine diatoms, dinoflagellates, silicoflagellates
and large cyanobacteria, the identification and taxonomic studies are based
on Round et al. (1990) and Tomas
(1997). Cell counts were used to determine the abundance of the large phytoplankton
A horizontal tow was made with 250 μm net that was fitted with a Hydrobiosflowmeter.
Samples were preserved in 5% formaldehyde and later were settled in glass graduated
cylinders and sedimentation biovolume was recorded. Density was then calculated
in organisms in cubic meter.
Statistical analysis: The community structure was analyzed with non-parametricmultivariate
methods using Primer v.6. Prior to the analysis, raw abundance data were
fourth-root transformedto reduce the influence ofoverly abundant species on
thepattern. The Bray-Curtis similarity matrix which reflects changes in relative
abundance as well as species composition, was used to calculate a non-metric
multi dimensional scaling (MDS) ordination plot. A permutation test on the matrix
of similarity (1-way ANOSIM) was used to assess seasonal difference in community
structure (Warwick and Clarke, 1991). The BIOENV procedure
in primer v.6 was used to correlate phytoplankton community structure with all
possible environmental variables (temperature, salinity, dissolved oxygen, nitrate,
nitrite, silicate and phosphate). Simpsons biodiversity index was used
as a index of biodiversity of phytoplankton (Simpson, 1949).
This investigation of phytoplankton community in a semi enclosed bay with mangrove plays a crucial role in understanding phytoplankton dynamics in response to environment changes. In the Sultanate of Oman, many fragile costal ecosystems, particularly mangroves, are under increasing human pressure and need to be objectively environmentally assessed. This study fills this important and urgent need for baseline information.
These results provide also a contribution to the understanding of the role of inshore-offshore exchange with adjacent areas and their influence on phytoplankton productivity and community structure. Furthermore mangroves are an important source of organic matter continuously produced and transported to adjacent waters.
Over the study period, Sea Surface Temperatures (SST) fluctuated widely from around 21.7°C on January 22 and 33.8°C on June 27 2003 (Fig. 2). The annual cycle of temperature at the sampling site followed a clear cycle with peak temperatures being recorded during summer and minimum temperatures during winter. On 16th July 2003, the study site experienced a sharp down in SSTs of about 2°C.
Salinity showed little seasonal variation during the sampling periods with an average of 37.3 psu. The lowest salinity (36.6-36.8 psu) was recorded during winter (Jan-Feb) and late summer (Aug-Sep) (Fig. 2), whereas the highest salinity (37.8 psu) during early summer (May). Where, as temperature fluctuation in BK mangrove system were quite high, between months or seasons (Table 1). Moreover, long sunshine periods, intense global radiation and low rainfall are the characteristic features of the area, which can a effect phytoplankton distribution of area.
Nitrite concentrations were low throughout ranging between 0.1 and 0.3 μM over the sampling period (Fig. 3) with the exception of a spike of 0.6 μM on 7 February. Nitrate concentrations also were low varying around 1 μM. As was the case of nitrite-N, the maximum nitrate-N concentration of 2.68 μM was recorded on February 7 (Fig. 3). Phosphate concentrations varied around 1 μM from Jan-23 to July-17, reaching a maximum concentration of 1.5 μM on May 29. Between July-31 and November-16 phosphate concentrations remained below 0.5 μM from (Fig. 3).
|| Climatology parameters of muscat area
||Seasonal fluctuations of (a) Surface temperature and (b) Salinity
||Seasonal fluctuations in surface nutrients (a) Nitrite, (b)
Phosphate, (c) Phosphate and (d) Silicate
|| Seasonal fluctuations in surface chlorophyll a concentrations
|| Changes in diatom and dinoflagellate counts
Silicate concentrations were high (>2.5 μM) throughout the period of study (Fig. 3). Maximum silicate concentrations of 6.9, 5.6 and 7.9 μM were recorded on June 27, July 16 and July 31, respectively.
In general, higher Chl a concentrations (average 1.75 μg L-1) were recorded from during the summer monsoon months from July to September. Chlaconcentrations at other times of the year were lower averaging around 0.4 μg L-1 with the exception of March 13 where the highest concentration of Chl a recorded was 2.57 μg L-1 (Fig. 4).
A total of 25 net phytoplankton taxa were identified during the study. Dinophyceae (dinoflagellates) and Bacillariophyceae (diatoms) contributed an equal number of species (12 each) and only one taxon of Cyanophyceae (cyano-bacteria).The diatom flora consisted of 11 species from the order Pennales and 1 species from the order Centrales. Among the Pennales, Dipliones sp. and Nitzschia sp., were found throughout the year. Diatoms were the minor constituents of the total net phytoplankton cell counts (Fig. 5).
Dinoflagellates contributed considerably to the overall phytoplankton cell counts and were the most abundant net phytoplankton group almost throughout the sampling period making up more than 95% of the total phytoplankton. Oscillatoria belonging to Cyanophyceae were also recorded during the sampling period but their contribution to the total net phytoplankton abundance was negligible.
Large fluctuations in population abundance were observed throughout the year,
with a maximum 115,584 cells L-1. Generally phytoplankton community
within BK mangrove showed a low species diversity (Simpson index = 0.4 on average)
and a poorly defined seasonal cycle and higher diversities during winter.
|| MDS of phytoplankton seasonal structure
||Contribution of dominant dinoflagellates species to the overall
phytoplankton abundance, PQ: Peridinium quinquecorne, PC: Pororocentrum
sp., SC: Scripsiella sp., PP: Protoperidinium species
Although, there was a visible trend in the relative position of the samples
on MDS plot: winter samples appear on the right hand side of the plot (Fig.
6), there was no significant difference between summer and winter samples
(Anosim R = 0.0045; p = 0.31). The BESTENV procedure carried out to identify
possible linkages between community structure and environment variables, showed
that phytoplankton community assemblages were best correlated to changes in
temperature, nitrite and phosphate (BEST Rho = 0.371, p = 0.28) but the linkage
was not significant.
The net plankton was dominated by a single species of dinoflagellate Peridinium quinquecorne (PQ) throughout the year comprising more the 90% of the species counts where it occurred in a bloom condition. In August and December Scrippsiella sp. (SC) was replaced by P. quinquecorne and comprised more than 80% of the total counts (Fig. 7).
|| Chlorophyll a size class contribution
The size fraction (0.74-<5 μm) made up less than 50% of the total biomass during most of the sampling period but phytoplankton belonging to this size fraction dominated the community on May 28, September 9, October 14 and November 15, making up between 60-80% of the total biomass (Table 2). Phytoplankton belonging to the size fraction 5-20 μm accounted for ~35% of the total biomass between March 12 and May 8 (30.9-37.9%) and from 44-51% between July and August 20. The highest contributions of net phytoplankton (>20 μm) occurred on June 27, March 13 and December 13 when this fraction made 53, 37 and 37.8% of the total biomass, respectively.
The temperature fluctuation in the BK mangrove followed a distinct annual cycle
of change with low temperatures being recorded in the winter and high sea surface
temperatures observed in summer. This cycle is typical of the seasonal cycle
in the Sea of Oman. Slight temperature decreases in July were likely due to
the intrusion of colder newly upwelled water from the adjacent Bay. In general,
the BK bay experiences sharp drops in temperature in July and in August accompanied
by shallowing of the thermocline under the influence of wind-driven coastal
upwelling along the north coast of Oman (Al-Hashmi et
al., 2010). Such major changes in temperature have been recognized as
the cause for major shifts in the dynamics of coastal ecosystems (Claereboudt
et al., 2001).
Chlorophyll a concentrations (0.5-2.5 μg L-1) recorded in BK
mangrove system are higher than the published values for the adjacent BK bay
(0.2-1.5 μg L-1) (Al-Hashmi et al.,
2010). The seasonal cycle within BK mangrove system however bore a strong
resemblance to the adjacent bay, with two periods of increase, the first in
March when Chlorophyll a peaked to 2.7 μg L-1 and the second
during the period between July and September, when Chlorophyll a values were
in excess of 1.5 μg L-1 .These increases in phytoplankton biomass
were clearly preceded by nutrient increases within the mangrove system, the
first in February when the bay comes under the influence of convectional overturned
waters due to winter cooling and the second during the summer upwelling season,
from July to September.
The phytoplankton compositions vary greatly among different mangrove ecosystems,
mainly controlled by nutrient flux, either generated or received from adjacent
low land. Phytoplankton biomass within BK mangrove system was made up largely
of phytoplankton forms belonging to <5 μm and the <20 μm size
fractions. The contribution of net phytoplankton, >20 μm, to total biomass
was minimal throughout the year with the exception of December, when it accounted
for 53% of the total biomass. Our observations are similar to those of Teixeira
and Gaeta (1991) who found that nanoplankton (2-20 μm) constituted
over 80% of the total phytoplankton community within a tropical Brazilian mangrove
system. These authors were able to demonstrate that these smaller phytoplankton
were responsible for a significant part of the total productivity with picoplankton
(cells <2 μm) accounting for 3-29% of the total 14C uptake.
The net phytoplankton of Bandar mangrove system are of low diversity and dominated
throughout the year by dinoflagellates which made up more than 95% of the total
phytoplankton abundance. Previous studies have shown that dinoflagellates usually
dominate in aquatic systems with high amounts of humic and fulvic acid (Prakash
and Rashid, 1968). Degrading mangrove litter is known to be an excellent
source of these compounds. Also floating detritus is known to support dinoflagelates
by providing organic matters plus attachments and protection (Faust,
1990a, b) and therefore it comes as no surprise
that dinoflagellates were the dominant phytoplankton group within BK mangrove.
In contrast, the phytoplankton species composition in the mangrove systems in
India, Pakistan and Iran are of high diversity and mostly dominated by large
cells of diatoms (Kannan and Vasantha, 1992; Mani,
1994; Chaghtai and Saifullah 1992; Rajkumar
et al., 2009; Zahed, 2002). The dominance
of these diatoms was related to the high nutrients concentration mainly from
freshwater and low land sources. Whereas BK mangrove system receives negligible
amounts of fresh water from rain, long sun duration and high temperature (Table
1) and therefore has low nutrient concentrations. Also the nutrient availability
from regenerative processes with BK mangrove system appeared to be minimal.
This could be attributed to the nitrogen uptake by mangroves and their associated
bacteria (Zuberer and Silver 1979; Mann,
2000). The nitrate-nitrite levels in this mangrove channel (Fig.
3) remained below the threshold (NO2+NO3>1 μM)
usually required for the dominance of large cells (Agawin
et al., 2000).
Net plankton tows showed that the phytoplankton population in BK mangroves
was dominated by a single species of a heterotrophic dinoflagellate, P. Quinquecorne
(Fig. 7), throughout the year accounting for more than
90% of the species counts during March and July-Sept. periods. P. quinquecorne
has been reported before in mangrove systems (Faust
et al., 2005). This species along with Prorocentrum elegans
was recorded as the most intense bloom-forming species in Douglas Cay and their
primary grazers were observed to heterotrophic ciliates and nematodes. In the
present study, ciliates were found to be very abundant during January and February
corresponding with the decline in the abundance of P. quinquecorne. P.
quinquecorne was also found to be very abundant in the Urdaibai estuary,
Spain, with the concentrations of this organism reaching their peak at high
tide, almost disappearing during the latest stages of the tide (Trigueros
and Orive, 2001).
The dominance of P. quinquecorne appears to be related to its unique
ability to survive under conditions of extreme change in the environment such
as that observed in BK mangrove system. Horstmann (1980)
observed that P.quinquecorne was found close to the surface during the
day, tolerating intense sunlight and descend during the night attaching itself
to the dark undersides of solid objects so as not to be washed out with the
tide. P. quinquecorne is capable of moving at 1.5 mm sec-1,
combining the tidal rhythm with a photic response which enables them to maintain
their dense population in the tidal area (Trigueros and
Orive, 2001). P. quinquecorne cells are adapted to both benthic and
planktonic shallow-tropical waters and present in tropical tide pools tolerating
high temperatures (38-42°C) (Horiguchi and Pienaar,
1991). Also, P. quinquecorne can tolerate a varied range of salinities,
growing best during warmer periods and at relatively high salinities when they
were capable of forming red tide blooms under high light and high temperature
(~38°C) (Horstmann 1980). P. quinquecorne
was also recorded from Tampa Bay, Florida where temperature was close to 30°C
and at salinities above 20% (Gardiner and Dawes, 1987).
Temperature in the BK mangroves averaged at 26°C in winter and above 31°C
in summer during high tide while temperature accede 35°C during low tide
periods. This system receives long hours of sun duration up to 11 hours per
day resulting in a very high air temperature exceeding 39°C during summer
(Table 1). P. quinquecorne appeared to be the only
phytoplankton species capable of tolerating these extremes in temperatures and
outcompeting other phytoplankton. Although, P. quinquecorne is known
to cause anoxia and fish kills during very high cell numbers (Fukuyo
et al., 1990), no incidences of fish mortalities were observed over
the course of our sampling.
BK mangrove ecosystems are located in a tropical, arid climatic environment. It receives a negligible amount of fresh water and is considered nutrient deficient. Phytoplankton biomass within BK mangrove was made up mostly of phytoplankton species that belong to the <5 μm and the <20 μm size fractions. The contribution of net phytoplankton >20 μm to total biomass was minimal. The net phytoplankton is of low diversity and dominated by the heterotrophic dinoflagellate, P. quinquecorne. This dominance was attributed to the ability of this species to thrive under a variety of physical and chemical conditions which allow it to survive and outcompete most other phytoplankton species including diatoms.
Thanks to the Department of Marine Science and Fisheries at Sultan Qaboos University
for supporting this research. Special thanks to Dr. J. Goes for proof-reading
and Harib Al-Habsi for running the nutrient analyses. We wish to extend our
appreciations to the Research Vessels crew and staff in the Department of Marine
Science and Fisheries: Saleh Al-Mashary, ManolitoBarte, Khamis Al-Riyami, Salim
Al-Khusaibi, AiyshaAmbu Ali and Mohammed Al-Gheithi.
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