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Influence of Sea Surface Temperature on the Gonadal Development of Sea Urchin Temnopleurus Toreumaticus from the Gulf of Mannar, South East Coast of India

Raju Saravanan 1 * , Paulraj Jawahar 2 , Thommai Francis 2 , Baboonsundaram Ahilan 2 and Rajagopal Santhakumar 2

Corresponding author Email: stingray_mr@yahoo.com

DOI: http://dx.doi.org/10.12944/CWE.11.1.17

This study was conducted for a 20 months period from October 2013 to May 2015 in Gulf of Mannar, south east coast of India. During the investigation the abiotic factors viz., Sea surface temperature (SST), Daylight photoperiod and atmospheric temperature data were collected from International comprehensive Ocean Atmospheric Database (ICOADS) and the reproductive cycle of the sea urchin was studied from the monthly sampling of sea urchin collected from Vedalai landing centre in Gulf of Mannar. The gonads were studied to calculate Gonad index as well  histological to categories them into four different stages of the development  and this data was compared with abiotic factors to study the influence of it on the reproductive behavior of sea urchin. The data were analyzed statistically through Pearson correlation and it was found negative between mean monthly gonad index and day length photoperiod, as well as with SST. This clearly indicates that the gonadal development in sea urchin is very much influenced by these two abiotic factors; however other nutritional factors might play greater role in the development gonad.


Sea urchin; Echinoid; Temnopleurus toreumaticus; Gulf of Mannar; Abiotic factors; Photoperiod; Sea Surface Temperature (SST); Gonad index; Gonadal development

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Saravanan R, Jawahar P, Francis T, Ahilan B, Santhakumar R. Influence of Sea Surface Temperature on the Gonadal Development of Sea Urchin Temnopleurus Toreumaticus from the Gulf of Mannar, South East Coast of India. Curr World Environ 2016;11(1) DOI:http://dx.doi.org/10.12944/CWE.11.1.17

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Saravanan R, Jawahar P, Francis T, Ahilan B, Santhakumar R. Influence of Sea Surface Temperature on the Gonadal Development of Sea Urchin Temnopleurus Toreumaticus from the Gulf of Mannar, South East Coast of India. Curr World Environ 2016;11(1). Available from: http://www.cwejournal.org?p=882/


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Article Publishing History

Received: 2016-02-10
Accepted: 2016-03-01

Introduction

Many countries around the world consume the gonad(roe) of the sea urchin as a delicacy food. Japan and France are the two main countries which consume the maximum global production of sea urchin roe from the wild as well as aquaculture. A number of countries have developed the mariculture technologies for growing sea urchin to cater to this global demand using their local species. Among the two types of sea urchin Viz., Regular and Irregular urchins, the regular urchins are used as food. In India, the diversity of regular sea urchin diversity stands at.  At certain pockets of the east and west coast of India fisher folk consume the gonads of sea urchin, other than this no organized trading or cultivation is being carried out. This is mainly due to the lack of knowledge on the biology of the regular sea urchin species available in India. Hence this study aimed at understanding the gonadal development process with respect to the abiotic factors viz., SST and Photoperiod in the Gulf of Mannar, which boast a diverse variety of sea urchin fauna.

Materials and Methods

The present study was conducted along the Mandapam coast of Gulf of Mannar  and monthly sampling was carried out from  Vedalai  landing centre, where bottom set gill net was operational. 30 individuals of sea urchin species Temnopleurus toreumaticus have been routinely collected for twenty months since October 2013 till May 2015 to study the gonado somatic index. The collected sea urchin were transported to the Central Marine Fisheries Research Institute(CMFRI), Mandapam laboratory in sea water. The total weight of the sea urchin was measured  to the nearest 0.001g, only after draining water from its test. The sea urchin use water to maintain hydrostatic pressure inside test, hence the drained weight is used.  The sea urchin test was opened using a scalpel and the five gonads are removed one after another with care and weighed. This gonad weight is compared with the total drained weight of the whole urchin to arrive at the gonado-somatic index (GSI) (Muthiga and Jaccarini, 2005; Vaitilingonet al., 2005) as follows;

GSI (%) = Wet weight of gonad (g) /Total wet weight of sea urchin (g) x 100

The gonadosomatic index (GSI), which measures the relative changes in weight in the gonads over time, was used on urchins as early as 1934 (Moore 1934), and is based on the assumption that maturation and breeding coincide with maximum gonad weight. A total of 600 individuals of sea urchin  Temnopleurus toreumaticus were collected during 20 month period from October 2013 to May 2015. Differences in mean GSI were evaluated following the methods of Wangensteen et al., (2013).

The data on the Sea surface temperature and atmospheric temperature was obtained from the International Comprehensive Ocean-Atmosphere Data Set (ICOADS) Release 2.5(http://rda.ucar.edu/datasets/ds540.0/) for the period of 20 months since October 2013 to May 2015. The day length photo period was collected from the http://www.sunrise-and-sunset.com/ for the study period from October 2013 to May 2015. Pearson correlation coefficients of monthly mean GSI with photoperiod and effect of sea surface temperature(SST) on mean GSI was assessed by calculating Pearson correlation coefficient for the sea urchin,Temnopleurus toreumaticus. All statistical analysis was performed using SPSS V.20.

Table 1: Correlations table for T.toreumaticus on SST versus Mean GSI

 

SST

MeanGSITT

SST

Pearson Correlation

1

-.319

Sig. (2-tailed)

 

.170

N

20

20

MeanGSITT

Pearson Correlation

-.319

1

Sig. (2-tailed)

.170

 

N

20

20



Table 2: Correlations table for T.toreumaticus on Photoperiod versus Mean GSI

 

Photoperiod

MeanGSITT

Photoperiod

Pearson Correlation

1

-.400

Sig. (2-tailed)

 

.081

N

20

20

MeanGSITT

Pearson Correlation

-.400

1

Sig. (2-tailed)

.081

 

N

20

20


Results and Discussion

The Pearson correlation coefficient was assessed using SPSS V.20 software. The analysis indicated that the strength of the association between SST and Mean monthly gonad index was negative (r = - 0.319) and the p value was (<0.001) (Table.1). Similarly the correlation between photoperiod and mean monthly gonad index was also negative (r= -0.400) and the p value was (p<0.001)(Table.2). This result clearly shows that any increase or decrease in the two abiotic factor viz., SST and Photoperiod would invariably influence the gonadal development process of this sea urchin species in the Gulf of Mannar.  A major peak of gonadosomatic index was observed inthe population of Temnopleurus toreumaticus, from the Gulf of Mannar during December -2013 and October -2014, followed by a spawning period. (Fig. 1&2)

 Fig.1 Temporal variation in mean Gonad index of T. toreumaticus in Gulf of Mannar


Figure 1: Temporal variation in mean Gonad index of T. toreumaticus in Gulf of Mannar
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 Fig. 2 Comparison of Photoperiod and SST variations in Gulf of Mannar during the study period


Figure 2: Comparison of Photoperiod and SST variations in
Gulf of Mannar during the study period

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The Gulf of Mannar is calm during April to September and experiences both the monsoon. The environmental conditions, especially temperature and photoperiod, and the food availability influence the gamete maturation and spawning of marine invertebrates (Pearse and Cameron, 1991). Analysis of SST data from Gulf of Mannar clearly showed a winter cooling of surface water to a level of 4 degree variation between summer and winter (Plate 1-10).  Temperature also can affect spawning duration and thus act directly on the gonad growth and nutrient accumulation that allow gametogenesis. Sea water temperature appears to be an important controlling factor for the onset and duration of the breeding period (Soualili and Guillou, 2009).  Vaitilingon et al. (2005) observed that the gonad index was negatively correlated to temperature and day length, indicating that higher values of GI were noted when temperature and day length were low in the sea urchin Tripneustes gratilla from Madagascar. Byrne et al. (1981) reported that the sea urchin species Centrostephanus rodgersii, a temperate sea urchin species coincide its gonadal maximum development with the increase of photoperiod. Shpigel et al. (2004) presented evidence that temperatures of 18–22 â—¦C enhanced gonad growth in P. lividus but that gametogenesis was controlled by photoperiod: long days reduced rates of gametogenesis and short days increased reproductive development. But in present investigation the sea urchin T.toreumaticusis strongly influenced by both SST and photoperiod. The results of the present study on the influence of abiotic parameters SST and Photoperiod on the gonadal development showed that the influence is greater and other nutritional factors in the Gulf of Mannar ecosystem may play a pivotal role in the reproduction and gonadal maturation in the sea urchin species Temnopleurus toreumaticus.

Fig. 3  SST Map of Gulf of Mannar and Palk bay during October to December 2013 


Figure 3: SST Map of Gulf of Mannar and Palk bay
during October to December 2013

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 Fig. 4  SST Map of Gulf of Mannar and Palk bay during December 2013 to February 2014


Figure 4: SST Map of Gulf of Mannar and Palk bay
during December 2013 to February 2014

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Fig.5 SST Map of Gulf of Mannar and Palk bay during February 2014 to March 2014 


Figure 5: SST Map of Gulf of Mannar and Palk bay
during February 2014 to March 2014

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 Fig.6 SST Map of Gulf of Mannar and Palk bay during March 2014 to May 2014


Figure 6: SST Map of Gulf of Mannar and Palk
bay during March 2014 to May 2014 

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Fig. 7 SST Map of Gulf of Mannar and Palk bay during May 2014 to June 2014 


Figure 7: SST Map of Gulf of Mannar and Palk
bay during May 2014 to June 2014

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Fig. 8 SST Map of Gulf of Mannar and Palk bay during July 2014 to August 2014 


Figure 8: SST Map of Gulf of Mannar and Palk bay
during July 2014 to August 2014

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Fig.9  SST Map of Gulf of Mannar and Palk bay during August 2014 to October 2014 


Figure 9: SST Map of Gulf of Mannar and Palk bay
during August 2014 to October 2014

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 Fig.10 SST Map of Gulf of Mannar and Palk bay during September 2014 to January 2015


Figure 10: SST Map of Gulf of Mannar and Palk bay
during September 2014 to January 2015

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 Fig.11 SST Map of Gulf of Mannar and Palk bay during January 2015 to March 2015


Figure 11: SST Map of Gulf of Mannar and Palk bay
during January 2015 to March 2015

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 Fig.12  SST Map of Gulf of Mannar and Palk bay during March 2015 to May 2015


Figure 12: SST Map of Gulf of Mannar and Palk
bay during March 2015 to May 2015

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Acknowledgement

The authors are thankful to the encouragement and support given by the Director of Central Marine Fisheries Research Institute and Dean of Fisheries College and Research Institute, towards this work.

References
 

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