Seasonal variation of sandy shore crustaceans of Mirya Bay, Ratnagiri, Maharashtra

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Available online at: www.mbai.org.in doi: 10.6024/jmbai.2015.57.1.01841A-10 Seasonal variation of sandy shore crustaceans of Mirya Bay, Ratnagiri, Maharashtra Snehal S. Lokhande*, A. D. Adsul, S. T. Indulkar and R. Pai College of Fisheries Shirgaon, (Dr. Balasaheb Sawant Konkan Krishi Vidyapeeth), Ratnagiri - 415 629 (MS), India. *Correspondence e-mail: snehal.lokhande147@gmail.com Received: 15 Jan 2015, Accepted: 01 Jun 2015, Published: 07 Jun 2015 Original Article Abstract This study highlights the seasonal variation of sandy shore crustaceans of Mirya bay of Ratnagiri, Maharashtra from April 2011 to March 2012. All samples were collected during the lowest low tide of each month, when maximum intertidal exposure prevailed. A total of seven macro-faunal species of crustaceans such as Ocypode cordimanus Ocypode ceratophthalmus, Ashtoret lunaris, Philyra corallicola, Diogenes miles, Emerita holthuisi and Gastrosaccus sp. were recorded. A total density of crustaceans during pre-monsoon (24.31 no m -2 ), monsoon (29.90 no m -2 ) and post-monsoon (58.47 no m -2 ) was recorded of which, Ocypode species were abundant throughout the year. The ghost crab, O. ceratophthalmus was abundant during April to December, while O. cordimanus was not recorded consistently during the study period as it dwells in the burrows amongst the Ipomea shrubs well above the high tide mark in the semiterestrial zone). The left-handed hermit crab D. miles was found near to low tide water mark during all the months except May and June. The moon crab, A. lunaris was observed only during the post-monsoon season (November - December) while the mole crab, E. holthuisi was abundantly found during the late monsoon and post-monsoon seasons. Monthly in-situ parameters such as atmospheric temperature (23.4 to 30.6ºC), interstitial water temperature (22 to 30.5ºC), sediment temperature (22.3 to 32.2ºC), dissolved oxygen of interstitial water (3 to 9.3 mgl -1 ), interstitial water ph (6.5 to 9.5), sediment ph (5.6 and 8.4) and interstitial water salinity (19.83 to 34.77 ) were recorded. Key words: Sandy shore, Crustaceans, interstitial, transect, quadrate Introduction The exposed sandy beaches are physically harsh and highly dynamic environments. Seasonal variation in environmental parameters have direct impact on qualitative and quantitative distribution of bentic crustaceans on the beaches. Sandy shore crustaceans are valuable due to their immense ecological significance. The sandy beaches are mostly studied to understand the species richness and abundance. The diversity and abundance of the crustaceans vary greatly with beach morpho dynamics. Sand is a dynamic substrate that provides J. Mar. Biol. Ass. India, 57 (1), January-June 2015

Snehal S. Lokhande et al. habitats for animals and probably the biggest adaptation of sandy beach animals is their ability to burrow. The crustaceans on sandy beach are burrowing vertical to avoid desiccation and thus, the interesting benthic communities can be observed after digging (Reid, 1967). The structures of interstitial environment play an important role on the morphology and biology of the population inhabiting in it. Monitoring of macro-faunal distribution and abundance over time and space helps us to understand the changes in species diversity (Colombini et al., 2003). The main objective of the present study is to determine seasonal changes in species composition and abundance of crustaceans in the exposed intertidal area of the sandy shore of Mirya bay, Ratnagiri, Maharashtra. Material and methods Ratnagiri is a coastal district of Maharashtra state along the west coast of India. Mirya sandy beach (Lat. 17 00 35.25 N Long.73 16 49.42 E) is located along the western side of Ratnagiri (Fig.1). All samples were collected during lowest low tide of each month when maximum intertidal exposure prevailed, by fixing transects from lowest low tide to highest high tide mark perpendicular to the shoreline (Schoeman et al., 2003) by adopting stratified random sampling method. Total of seven transect lines were fixed with a distance interval of 400 m on the intertidal region of the exposed sandy shore. In each transect, zone-wise three quadrates having size 0.0625 m 2 (Rathod, 2005) were placed with an interval of seven meter between lines and sediment samples upto a depth of 10 cm were collected and removed from sampling grid with the help of spade and collected in the sampling bags. After sieving the sediment samples through 1mm size sieve, the macrofaunal samples (>1mm) were preserved in 5 % formalin solution for further identification. All the macrofaunal crustaceans were studied quantitatively and qualitatively to record their monthly and seasonal variation. Samples were collected during the period from April 2011 to March 2012. Results and discussion Occurrence and abundance During the field observations of twelve month period, a total of seven macro-faunal species of crustaceans such as Ocypode cordimanus (Latreille, 1818), Ocypode ceratophthalmus (Pallas, 1772), Ashtoret lunaris (Forskal, 1775), Philyra corallicola (Alcock, 1896), Diogenes miles (Fabricius, 1787), Emerita holthuisi (Sankolli, 1965) and Gastrosaccus sp. were recorded. A total density of crustaceans during pre-monsoon (24.31 no m -2 ), monsoon (29.90 no m -2 ) and post-monsoon (58.47 no m -2 ) seasons were recorded (Fig. 2) in which the genus Ocypode was Fig. 1. Sampling site abundantly recorded. The ghost crab, O. ceratophthalmus (Fig.3) was abundant during April to December while O. cordimanus (Fig.5) was not recorded consistently during all months of the year. As it dwells in the burrows amongst the Ipomea a shrub well above the high tide mark in the semiterrestrial zone. The maximum density of O. cordimanus was recorded in February (15.2381 no m -2 ) and minimum during October (4.5714 no m -2 ) while O. ceratophthalmus was recorded maximum in November (12.1905 no m -2 ) and minimum during December (0.7619 no m -2 ). The ghost crab, O. ceratophthalmus and O. cordimanus were abundantly recorded above the high tide water mark. Similarly Philip (1970) and Nair (1978) also observed O. ceraptothalmus at the high water mark along the coast of Cochin and Benaulim, Goa. The left-handed hermit crab, D. miles (Fig.4) was found near to the low tide 66 Journal of the Marine Biological Association of India Vol. 57, No.1, Jan-Jun 2015

Seasonal variation of sandy shore crustaceans of Mirya Bay Fig. 2. Annual distribution of crustaceans (no m -2 ) along Mirya sandy shore Fig. 3. O. ceratophthalmus Fig. 4. D. miles Fig. 5. O. cordimanus water mark during all months except May and June. The maximum and minimum density were recorded during the post-monsoon season (25.904 no m -2 ) and pre-monsoon season (7.3684 no m -2 ) respectively. Nair (1978) recorded the single hermit crab species of genus Diogenes viz. Fig. 6. P. corallicola Diogenes custos (Fabricus, 1798) which contributed the maximum component of the fauna. Parulekar (1981) reported the hermit crab, D. miles and D. custos, from Malvan sandy shore, west coast of India. The sandy shore crab, P. corallicola (Fig.6) was prominently recorded in low Marine Biological Association of India 67

Snehal S. Lokhande et al. Fig. 7. A. lunaris Fig. 9. Gastrosaccus sp. tide water mark from September to March with a maximum density (19.0476 no m -2 ) in February and minimum (6.0952 no m -2 ) in September. Nair (1978) recorded Philyra globosa which formed the major component of the fauna along Benaulim, the sandy shore of Goa. The moon crab, A. lunaris (Fig.7) was recorded only during the postmonsoon season (November - December) during the study period. Similar findings were also reported by Rathod (2005) and recorded the Ashtoret sp. during September to March on the Mandovi sandy shore, Ratnagiri, Maharashtra. The mole crab, E. holthuisi (Fig.8) was abundantly found during the late monsoon and post-monsoon seasons. Maximum density of E. holthuisi (7.8095 no m -2 ) was recorded during the late monsoon (September) and postmonsoon season (October - January) at low tide and mid tide water mark. Ansell et al. (1972) reported two main periods of recruitment of E. holthuisi, i.e. one in the pre-monsoon Fig. 8. E. holthuisi season (February and March) and another during the monsoon season (June - September) and the density ranged from 0 to 500 (no m -2 ) at the Sheratallai sandy beach, while at Cochin sandy beach it was densely distributed over 4000 (no m -2 ). Achuthankutty et al. (1978) recorded maximum abundance of E. holthuisi during the post-monsoon season and early pre-monsoon season along Baina coast, Goa. The maximum density of E. holthuisi during the post-monsoon season (390 no m -2 ) along Benaulim, Goa was reported by Nair (1978). Thus the present findings of distribution of Emerita sp., at low tide and mid tide water mark zone on Mirya sandy beach are in agreement with the findings of other researchers. The variation in zonal distribution patterns of genus Emerita may be attributed towards species specificity behaviour. The single species of the mysid, Gastrosaccus sp. (Fig.9) was recorded during the late post-monsoon season (October - January) and pre-monsoon season (February - May) at low tide water mark. The maximum density of Gastrosaccus sp. (0.7619 no m -2 ) was observed during the post-monsoon season (October - January). Achuthankutty et al. (1978) reported the abundance of Gastrosaccus sp. during the late monsoon (September) and post-monsoon season (October - January) along Baina beach, Goa. During the monsoon season Nair (1978) observed the maximum density of the Gastrosaccus sp. (5100 no m -2 ) on Benaulim, Goa. A very high abundance of the Gastrosaccus was reported during the monsoon season at Kalbadevi beach, Ratnagiri by Sivadas et al. (2012). Diversity indices Diversity indices were used to know the macro-faunal richness and species diversity of an area. According to Bakus (2007) the Shannon wiener index varies from 0 (no diversity) to 5 (maximum diversity). The Simpson index varies from 0 (no diversity) to 1 (maximum diversity). 68 Journal of the Marine Biological Association of India Vol. 57, No.1, Jan-Jun 2015

Seasonal variation of sandy shore crustaceans of Mirya Bay The Evenness index varies from 0 (no evenness) to 1 (greatest evenness) and the Dominance index varies from 0 to 1 (greatest dominance). The diversity indices like, the Shannon Wiener index varied from minimum (0.7246) during the monsoon and maximum (1.9852) during the post-monsoon season. The Simpson index was recorded maximum during the post-monsoon (0.7066) and minimum during the monsoon season (0.3238). The Evenness was recorded maximum during the post-monsoon (0.8033) Table 1. Season-wise biodiversity indices for the crustaceans of Mirya sandy shore during 2011-2012 Indices Pre-monsoon Monsoon Post-monsoon H' 0.8318 0.7246 1.9852 S 0.3432 0.3238 0.7066 J' 0.4675 0.5500 0.8033 D 0.0325 0.2001 0.1968 H'- Shannon s diversity index, S Simpson index,j' Evenness index, D- Dominance index while minimum during the pre-monsoon (0.4675) and the Dominance index was recorded maximum during the monsoon (0.2001) and minimum during the pre-monsoon (0.0325) (Table.1). The low diversity indices of Shannon and Simpson during monsoon season may be due to the harsh environmental conditions along the coast which discourages the diversity of crustaceans of the Mirya sandy shore. Abiotic factors are vital and can cause direct impact on diversity and distribution of faunal organisms. Environmental parameters Season-wise variation in environmental parameters: during pre-monsoon (February-May), monsoon (June-September) and post-monsoon (October-January) was recorded. During the investigation period, correlation analysis of the parameters like atmospheric, interstitial water and interstitial sediment temperatures and also the interstitial water salinity did not show any significant correlation with sandy shore of crustaceans, which suggest that all these sandy shore Table 2. Monthly and seasonal variation of environmental parameters of water in Mirya sandy shore Year Months Atm. temp. ºC Water temp. ºC Sand temp. ºC DO of interstitial water (mg/lit) Salinity of interstitial water ( ) ph of water ph of soil 2011 Apr 30 30.57 32.20 4.4 30.03 8.5 7.6 May 29.83 30.27 31.60 4.1 29.23 7.5 6.8 Jun 26.33 24.87 27.40 7.4 28.87 6.5 5.6 Jul 24.87 24.40 25.00 8.5 24.63 7.5 5.9 Aug 26.00 26.23 25.80 9.3 19.83 7.5 6.3 Sep 27.17 26.73 27.70 5.8 24.47 8.5 6.3 Oct 26.17 26.37 27.50 6.6 25.33 8.5 6.8 Nov 27.57 28.47 26.90 4.5 29.73 8.5 7.4 Dec 30.67 30.43 31.10 4.9 34.77 9.5 8.2 2012 Jan 29.60 29.43 29.70 3.4 34.53 8.5 7.7 Feb 28.27 28.17 28.00 5.4 33.23 9.5 8.4 Mar 23.43 22.07 22.30 3 33.27 7.5 8. 1 Table 3. Correlation co-efficient among environmental parameters and crustaceans of Mirya sandy shore Atm TempºC Interstitial Water TempºC Interstitial sediment TempºC Interstitial water DO Sediment ph Interstitial Water ph Interstitial Water Salinity Crustaceans ( no m -2 ) Atm Temp.0C 1 Interstitial Water Temp.ºC 0.974** 1 Interstitial sediment Temp. ºC 0.954** 0.930** 1 Interstitial water DO (mgl-1) -0.400-0.355-0.299 1 Sediment ph 0.384 0.370 0.199-0.744** 1 Interstitial Water ph 0.551 0.579* 0.403-0.359 0.717** 1 Salinity 0.440 0.325 0.297-0.805** 0.788** 0.424 1 Crustaceans ( no m -2 ) -0.280-0.247-0.357 0.042 0.060 0.402-0.144 1 * Significant at the 0.05 level ** Significant at the 0.01 level Marine Biological Association of India 69

Snehal S. Lokhande et al. crustaceans are well adapted to seasonal fluctuation in environmental conditions. Acknowledgements The authors are thankful to the authorities of College of Fisheries, Shirgaon, Ratnagiri (Dr. Balasaheb Konkan Krishi Vidyapeeth, Dapoli) for providing all necessary facilities as well as for giving the needful support during the course of investigation. References Achuthankutty, C. T., A. Stirling, S. Nair, P. A. L. Bharathi and M. R. Menezes. 1978. Sandy beach at Baina, Goa: Its ecology and production. Indian J. Mar. Sci., p. 23-29. Ansell A. D., P. Sivadas, B. Narayanan and A. Trevallion. 1972. The ecology of two sandy beaches in South West India. II. Notes on Emerita holthuisi. Mar. Biol., 17: 311-317. Bakus, G. J. 2007. Quantitative analysis of marine biological communities.235pp. Colombini, I., M. Fallaci, F. Milanesi, F. Scapini and L. Chelazzi. 2003. Comparative diversity analysis in sandy littoral ecosystems of the Western Mediterranean. Estuar. Coast. Shelf. Sci., 58:93-104. Dwivedi, S. N., S. Ayyappan Nair and A. Rahim. 1974. Ecology and production of intertidal macrofauna during monsoon in sandy beach at Calanguta, Gao. J. Mar. Biol. Ass. India, 15(1):274-284. Lakshmana Rao, M. V. and A. Pattnaik. 1986. Physical features of an exposed sandy beach at Gopalpur, (Orissa coast). Mahasagar- Bull. Nat. Inst. Ocea., 19 (3):153-164. Mense, M. N. 1988. The marine intertidal beach ecology of the bay of Ratnagiri. M.Sc. Thesis. College of Fisheries, Konkan Krishi Vidyapeeth, Dapoli, 363. Nair, A. 1978. Production ecology of a tropical sandy beach at Benalium, Goa. Ind. J. Mar. Sci., 7:163-167. Parulekar, A. H. 1981. Marine fauna of Malvan, central west coast of India. Mahasagar- Bull. Nat. Inst. Ocea., 14 (1):33-44. Philip, K. P. 1970. The intertidal fauna of the sandy beaches of Cochin. Mar. Intert. Ecol., 38, B, Nos. 5 & 6. Rathod, R. H. 2005. Efficacy of sampling designs to study macrofaunal assemblage on exposed (Mandovi) sandy beach, M. F. Sc. thesis Dr. Balasaheb Sawant Konkan Krishi Vidyapeeth, Dapoli, 71. Reid, G. K. 1967. Ecology of intertidal zones. Rand McNally and Company, Chicago. 85. Sarma, N. S. R. and C. Mohan. 1981. On the ecology of the interstitial fauna inhabiting the Bhimilipatnam coast (Bay of Bengal). Mahasagar - Bull. Nat. Inst. Ocea., 14 (4):257-263. Schoeman D. S., M. Wheeler and M. Wait. 2003. The relative accuracy of standard estimators for macro-faunal abundance and species richness derived from selected intertidal transect designs used to sample exposed sandy beaches. Estuar. Coast. Shelf Sci., 58: 5-16. Sivadas S. K., B. Ingole, P. Ganesan, S. Sautya and M. Nanajkar. 2012. Role of environmental heterogeneity in structuring the macrobenthic community in a tropical sandy beach, west coast of India. J. Oceanogr., 68:295-305. Wafer, M. V. M., M. D. Rajagopal, M. R. Menezes and A. Stirling. 980. Physico - chemical features and energy input in 3 sandy beaches of West Coast of India. Indian J. Mar. Sci., 9:25-30. 70 Journal of the Marine Biological Association of India Vol. 57, No.1, Jan-Jun 2015