Dinoflagellate Ceratium
symmetricum Pavillard (Gonyaulacales: Ceratiaceae): Its occurrence in the
Hooghly-Matla Estuary and offshore of Indian Sundarban and its significance
Anirban Akhand 1, Sourav Maity 2,
Anirban Mukhopadhyay 3, Indrani Das 4, Pranabes Sanyal5 & Sugata Hazra 6
1,3,5,6 School of
Oceanographic Studies, Jadavpur University, Kolkata, West Bengal 700032, India
2 Indian
National Centre for Ocean Information Services (INCOIS), Ministry of Earth
Science (MoES), Govt. of India, “Ocean Valley”, PB No. 21, IDA Jeedimetla PO,
Hyderabad, Andhra Pradesh 500055, India
4 Department of Botany, Midnapore College, West Bengal
721101, India
Email: 1anirban_akhand@rediffmail.com
(corresponding author), 2 srv_maity@rediffmail.com, 3 anirban_iirs@yahoo.com, 4 ms_indranidas@yahoo.co.in, 5 pranabes@gmail.com, 6sugata_hazra@yahoo.com
Date of publication (online): 26 July 2012
Date of publication (print): 26 July 2012
ISSN 0974-7907 (online) | 0974-7893 (print)
Editor: S.C. Santra
Manuscript details:
Ms # o2530
Received 29 July 2010
Final received 21 June 2012
Finally accepted 25 June 2012
Citation: Akhand, A., S. Maity, A. Mukhopadhyay, I.
Das, P. Sanyal & S. Hazra (2012). Dinoflagellate Ceratium symmetricumPavillard (Gonyaulacales: Ceratiaceae): Its occurrence in the Hooghly-Matla
Estuary and offshore of Indian Sundarban and its significance. Journal of Threatened Taxa 4(7): 2693–2698.
Copyright: © Anirban Akhand, Sourav
Maity, Anirban Mukhopadhyay, Indrani Das, Pranabes Sanyal & Sugata Hazra
2012. Creative Commons Attribution 3.0 Unported License.JoTT allows unrestricted use of this article in any medium for non-profit
purposes, reproduction and distribution by providing adequate credit to the
authors and the source of publication.
Acknowledgements:Authors wish to thank Mr. Bijan Kumar Saha, Former Senior Deputy Director
General, Geological Survey of India for his
cooperation in this work. The authors are also grateful to National Aeronautics
and Space Administration for providing the SST data through the Ocean Color
website.
Abstract:The Sundarban is the largest mangrove ecosystem, which is presently
vulnerable to climate change related impacts. The western part of it falls in the
state of West Bengal between the estuaries of the Hooghly and
Ichamati-Raymongal Rivers. The diversity of the genus Ceratium Schrank
and the related physicochemical parameters such as Sea Surface Temperature
(SST) was studied in the Hooghly-Matla estuary and offshore. Five species of bio-indicator
dinoflagellate, Ceratium were
identified in the bloom-forming season. The species are: C. furca, C. fusus, C. symmetricum, C. trichoceros and C. tripos. C. symmetricum was not
previously reported from the Indian part of the Sundarban and is now found in low
abundance. The other four species
are less sensitive to warming or rise in SST. A comparative study of the day time SST from the satellite images of the year 2003 to
2009 of the months of January and February reveals a rising winter SST. Compared to the previous years, the
increase in temperature can be one of the causative factors to explain the
lower abundance of C.
symmetricum compared to the others. With further rise of the SST, there is a possibility that this species
may no longer be found in abundance in the western part of adjoining
Hooghly-Matla estuarine system.
Keywards:Biological indicator, Ceratium,
phytoplankton, sea surface temperature, Sundarban.
For figures, images, tables -- click here
The Sundarban, a Biosphere Reserve,
constitutes a complex ecosystem comprising one of the three largest single
tracts of mangrove forests of the world. As neighboring countries, India and Bangladesh share the territories which cover the areas of the Sundarban. The Indian Sundarban (88002’–89006’E
& 21013’–22040’N) including the forest and
nonforest parts consist of three major estuaries. The biodiversity
richness of the Sundarban has been reported by many researchers. However, there are very few studies on
phytoplankton diversity (Santra et al. 1991; Mitra et al. 2003; Sen &
Naskar 2003). Phytoplankton
are the foundation of the foodweb in the marine ecosystem as they
perform the critical ecological function of primary production (Nielsen &
Jensen 1957; Banerjee & Santra 2001, Verlencer & Desai 2004). The knowledge of phytoplankton species
diversity is crucial for any ecological or eco-physiological work on marine
phytoplankton. Phytoplankton
are highly sensitive to environmental changes. Their community composition, biomass and
shifts therein represent an excellent tool to interpret the dynamics of a
pelagic ecosystem, transformation, cycling of key elements and the impact on
coastal water quality. Phytoplankton also help to detect variations induced by
river discharge, eutrophication, pollution and even certain unusual climatic
phenomena (Lepisto et al. 2004; Paerl 2006). Ceratium Schrank, an armoured
dinoflagellate genus has been considered a biological model for a wide range of
studies as utilized by Tunin-Ley et al. (2007, 2009). One of the several advantages offered by
this genus is that identification of species level is more feasible than other
phytoplankton group (Tunin-Ley et al. 2009). Apart from this, Ceratium is
known for its sensitivity to temperature in terms of biogeography (Dodge &
Marshall 1994), seasonality and morphology (Sournia 1967). Ceratium has been considered to
be a biological indicator of water masses (Dodge 1993; Raine et al. 2002;
Tunin-Ley et al. 2009), current regimes (Dowidar 1973) and climate change
(Dodge & Marshall 1994; Johns et al. 2003). In the present paper, diversity and
record of the species Ceratium has been investigated in the Indian part
of the Sundarban estuary to offshore Bay of Bengal and discussed in the context
of ecological change, particularly the change in Sea Surface Temperature (SST).
Materials and Methods
Water samples were collected from
different stations from the case 2 water of Hooghly estuary and offshore off
Bakkhali-Frasergunje (Fig. 1). The
depth of the water varies between 1 to 10 m along a 10km radial vector off the
coast. The cruise was conducted in
the months of January and February, 2009, as December,
January and February are the bloom forming seasons for most of the
phytoplankton in Sundarban (Biswas et al. 2004). Day time SST
data, obtained from Moderate Resolution Imaging Spectro Radiometer (MODIS) with
a wave length of 11µ and spatial resolution of 4km has been used in a 10×10grid around the study area. The
monthly composite data were derived from the year 2003 to 2009 for the months
of January and February. Salinity,
pH and temperature were measured using a portable refractometer (Model no.RHS-10(ATC)), a digital pH meter (Model no. pHTestr 1, Eutech instruments, Oakton Instruments) and a
digital thermometer respectively. Dissolved oxygen was measured using Winkler’s titrimetric method. The transparency of the water column was
measured with the help of a Secchi disc. Phytoplankton samples were collected by plankton net of 20µ mesh size fitted to a wooden stick. Known volume of water was passed through
it with a five litre bucket. Plankton samples were preserved in
Lugol’s iodine solution and sent back to laboratory within 48 hours where it
was counted by a Sedgewick Rafter counting cell. The identification of phytoplankton
species was done with the help of standard manuals and literature (Tomas 1996;
Verlencar & Desai 2004). Relative abundance (RA) was calculated using the formula:
RA of species X (%) of Ceratium =
(No. of species X of Ceratium in each known
volume of sample × 100) / No. of total Ceratiumspecies in the same volume.
Results
All together, five species of Ceratiumwere identified in the months of algal bloom. Ceratium furca (Ehrenberg)
Clapar~de & Lachmann, Ceratium fusus (Ehrenberg) Dujardin,Ceratium trichoceros (Ehrenberg) Kofoid, Ceratium tripos(O.F. Mialler) Nitzsch and Ceratium symmetricum Pavillard have been
found when the day temperature of the surface water ranged between
24.5–25.2 0C, pH between 8.0–8.3, salinity between
26–27 ppt, dissolved oxygen between 4.7–5.2 mg/L and total
alkalinity (TA) between 125–150 mg/L. The least transparency of the water
column was observed to be 39cm during the course of sampling (Table 1). Relative abundance was calculated for
each species (Table 2), and showed highest abundance of Ceratium furca,
followed by C. fusus, C. tripos, C. trichoceros and C.
symmetricum.
Four out of 10 species of Ceratium, reported
from the Indian Sundarban earlier (Santra et al. 1991; Mitra et al. 2003;
Biswas et al. 2009) was also found in the present study. The fifth species found in this study, C.
symmetricum (Image 1) was not reported previously from the Indian
Sundarban.
The analytical data of the monthly
composite SST for seven years (2003 to 2009) derived from satellite images
within the study area for the months of January and February (24.114 and 25.4950C respectively) clearly depicts an increased winter SST in the year
2009, than the previous years (Figs. 2 & 3). The temperature difference is also maximum between 2008 and 2009 (during January and February),
within the last seven years.
Discussion and Conclusions
The distributions of C. symmetricumare comparatively limited and are reported in warm temperate to tropical waters
(Parke & Dixon 1976; Gil-Rodriguez et al. 2003). The species was reported from the water
column of continental shelf of northern and northwestern Australia (Hallegraeff
& Jeffrey 1984) and northwestern Mediterranean Sea (Tunin-Ley et al. 2009).
Several types of biological indicators of
ecological change have been suggested, for example, abundance of individual
taxa, functional attributes of the ecosystem, species
assemblages and phenological traits (Beaugrand 2005). Among the species of Ceratiumfound in this study, available literature suggests: C. furca and C.
tripos are perennial, whereas C. fusus is almost perennial
since it may be absent only for a couple of months. C. trichocerosis one of the species which is not specifically associated with any depth or
environment (Tunin-Ley et al. 2009). Among these species, mixotrophic behavior has been observed in C.
furca (Smalley et al. 1999) and C. fusus (Mikaelyan &
Zavyalova 1999). Mixotrophic
organisms are theoretically supposed to be, less dependent on nutrient
availability and irradiance (Tunin-Ley et al. 2009).
Tunin-Ley et al. (2009) have revealed in
their work that the diminished occurrence of certain Ceratium species during
the warm season (in case of northwestern Mediterranean Sea) in surface water is
an important sign of change. Among
these, C. teres, in the main and C. symmetricum and C.
horridum to a lesser extent, could be proposed as indicators of warming
since they seemed to be limited by a maximum temperature threshold. The temperature of the northwestern
Mediterranean Sea in the warm season (230C in summer, 2002, and
above 250C in summer, 2003 (Tunin-Ley et al. 2007) is comparable to
the temperature (24.5–25.2 0C) of our study area in the winter
as measured during the study period. Thus, similar inferences can be drawn from the present study of limited
abundance of C. symmetricum in the estuary and offshore of Indian
Sundarban.
Ceratium symmetricum was found to be much reduced in number
(Relative Abundance: 3.2±0.2) compared to the other four species during winter
(Table 1), indicating its lesser compatibility with the physico-chemical
features, especially with SST in the study area. The other four species are less
responsive to warming and tolerant of a wide range of physical condition,
whereas the occurrence of a reduced number of C. symmetricum may
be indicative of temperature rise in the Sundarban estuary and offshore.
It is proposed that, long term monitoring
of thermal preference or sensitivity of species of Ceratium along with
various physicochemical features of water can be a useful approach for the
analysis of the impact of climate change on the phytoplankton community of the
northern Bay of Bengal. This study,
thus, opens some new avenues for generation of a long termdataset which would throw some light on various aspects of Sundarban’s mangrove
ecosystem and climate change induced impact on them.
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