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Parulekar. A. H., Ansari, Z. A., 1981. Benthic macro fauna of the Andaman Sea. Indian J. Mar. Sci. 10, 280-284. Parulekar, A. H., Harkantra, S. N., Ansari, Z. A., 1982. Benthic production and assessment of demersal fishesry resources of the Indian seas. Indian J. Mar. Sci. 11, 107-114. Parulekar, A. H., Wagh, A. B., 1975. Quantitative studies on the benthic macrofauna of the northeastern Arabian Sea shelf. Indian J. Mar. Sci. 4, 174-176. Prabhu Venkatesh, H., Narayana, A. C., Katti, R. 1., 1993. Macrobenthic fauna in nearshore sediments off Gangolli, West coast of India. Indian J. Mar. Sci. 22, 168-171. Qasim, S. Z., 1982. Oceanography of the northern Arabian Sea. Deep-Sea Research. 29, 1041-1068. Rosenberg, R., 1977. J. Exp. Mar. BioI. EcoI26,107. Sanders, H. L., 1956. Oceanography of Long Island Sound 1952-1954, Biology of marine bottom communities. Bull. Bingham Oceanogr. Coil. 15, 345-414. Sanders, H. L., Hessler, R. R., 1969. Science, 163, 1416 pp. Sanders, H. L., 1968. Marine Benthic diversity: A comparative study. Am. Nat. 102 (925), 243-282. Sanders, H. L., Mangeisdorf, P. C., Hampson, G. R.,1965. Salinity and faunal distribution in the Focasset River, Massachusetts. Limnology and Oceanography 1O(suppl.),216-229. Sarma, N. S. R., Mohan, P. c., 1981. On the ecology of the interstitial fauna inhabiting the Bhimilipatanam coast (Bay of Bengal). Mahasagar 14 (4), 257- 263. Savich, M. S., 1972. Quantitative distribution and food value of benthos from the western Pakistan shelf. Oceanology 12, 113-220. Sibert, J., Broun, T. J., Healy, M. c., Kask, B. A., Naiman, R. 1., 1977. Detritus based food webs: exploitation by juvenile Chum Salmon (Onchorhynchus keta). Science 196, 649-650. 223
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Certificate I hereby certify that t
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Contents Page No. Chapter 1. Introd
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the bottom. Ekman (1935) described
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wonns are the most abundant group a
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leadership of Sir James Clark Ross,
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Ansari et al., (1977b) carried out
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Gopalakrishnan and Nair (1998) cond
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Major objectives:- 1. To understand
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CMFRI (Central Marine Fisheries Res
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Joydas, T.V., Damodaran, R., 2001.
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monitoring committee (Atlantic Mari
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Vizakat Lathika, I-Iarkantra, S. N.
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analysed after acidification by tit
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used as stain prior to sorting and
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space. Therefore, it is very essent
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Fig. I - Station locations 32
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affected at high temperature. Most
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layers exhibit different oceanograp
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Transect wise variation in temperat
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3.2.2.3. Dissolved oxygen (DO) Dist
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monsoon temperature initially incre
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opined that limited mixing. high or
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Naqvi, S. W. A., Noronha, R. J., Re
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orr Mormugao orr Vernal 35.36 35.32
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The continental shelf and its adjoi
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sediments (4 stations). Silty sand
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fine sediments with comparatively h
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Narayana, 1991 ). Limited input of
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In general. two ditlerent patterns
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et al., (1980) reported values in t
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organisms living in the water and t
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Hashimi, N. H., Kidwai, R. M., Nair
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Postma, H., 1967. In Estuaries, Lau
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Depths Sand Silt Clay Organic matte
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• PRE'MONSOON SOUTHERN'TRANSECTS
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as the best indicators of the envir
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showed that northern transects have
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decreased from shallow to deeper de
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different depth zones showed that a
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cm 2 with a dominance of nematodes.
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and 6.08 g/m 2 were recorded during
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were located in the nearshore water
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changes in the hydrographical and t
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factor for such a large difference
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Belegvad, H., 1932. Investigations
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Parulekar, A. H., Harkantra, S. N.,
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Savich, M. S., 1972. Quantitative d
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Traosects Polychaetes Crustaceans M
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Miscellaneous Transects Nematodes C
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Depths Nematodes Cope pods Foramini
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Wagh, 1975; Parulekar et ai, 1976;
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ones and 17 were included in the 'r
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Nephtydae (2%). Among the 20 sedent
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At 75 m zone, 31 groups/species wer
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Porbandar. At 50 m depth zone, fluc
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otTMumbai and Ratnagiri and low eve
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species richness at each depth zone
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E2.2.2.!. Richness (Margalef's inde
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I ):.2.2.2.4. Dominance (Pie/ou's i
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Tablc 17. Contd .. - Sternaspidae 0
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Table 20. contd .. G. alba 20 25 20
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150 Taxa 30m 50m 75m lOOm 150 m m D
Page 186: 9% 1% o poIychaete • crustacea o
Page 203 and 204: a) c) e) g) Plate 5 a) Prinospio sp
Page 205 and 206: a) c) e) Plate 7 a) Cardium sp. d)
Page 207 and 208: 7/. /ntroduct ion 7.2. Hydrography
Page 211 and 212: also showed a similar pattern with
Page 213 and 214: y most of the organisms. It was als
Page 215 and 216: with sand of which total density (r
Page 217 and 218: muddy bottom of the west coast of I
Page 219 and 220: crustaceans and miscellaneous group
Page 221: the organic rich environment with h
Page 225 and 226: Icvci (p
Page 227 and 228: mcioHmna serve primarily as rapid m
Page 229 and 230: surface chlorophyll a was 0.36mg I
Page 231 and 232: Devassy, V. P., Achuthankutty, C. T
Page 233: Longhrust, A. R., Pauly, D., 1987.
Page 237: Faunal groups Silty Clayey Mixed Sa
Page 257: Mannagoa to Porbandar located betwe
Page 260 and 261: against gastropods during pre- mons
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