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Service, S. K., Feller, R. J., 1992. Long-tenn trends of subtidal macrobenthos in North Inlet, South Carolina. Hydrobiologia 231,13-40. Seshappa, G., 1953. Observation on the physical and biological features of the inshore sea bottom along the Malabar Coast. Proc. Nat. Inst. Sci. India. 19, 257- 279. Sheeba, P., 2000. Distribution of benthic infauna in the Cochin backwaters in relation to environmental parameters. Ph.D. Thesis. Cochin University of Science and Technology. Snelgrove P. V., Butman, C. A. 1994. Animal-sediment relationships revisited: Causes versus effect, Oceanogr. Mar BioI., 32, 111-177. Sokolova, M. N., Pastemak, F. A., 1962. Quantitative distribution and trophic zoning of the bottom fauna in the Bay of Bengal and Andaman Sea. Trud. Inst. Okeanol., 64, 271-296. Sommer, S. and Pfannkuche, 0., 2000. Metazoan meiofauna of the deep Arabian Sea: Standing stocks, size spectra and regional variability in relation to monsoon induced enhanced sedimentation regimes of particulate organic matter. Deep-sea Res. 11,47(14),2957-2977. Spark, R., 1935. J. Cons. Penn. Int. Explo.r Mer. 10, 3. Sverdrup, H. U., Martin, W. J., Richard, H. F., 1942. In: The Oceans, Their physics, chemistry and general biology. Prentice-Hall, Inc., USA. Swedmark, B., 1971. BioI. Rev. 10,214. Thiel, V. H., 1966. Quantitative investigations of deep-sea meiofauna. VerofT. Inst. Meeresforsch., Bremerh 11, 131-147. Thorson, G., 1957. Bottom communities (Sublittoral or shallow shelf) Geol. Soc. Ann. Mem. 67(1), 461-534. Varshney, P. K., 1985. Meiobenthic study off Mahim (Bombay) in relation to prevailing organic pollution. Mahasagar 18(1),27-35. Varshney, P. K., Govindan, K., Gaikwad, U. D., Desai B. N., 1988. Macrobenthos off Versova (Bombay), West coast of India in relation to environmental condition. Indian J. Mar. Sci. 17,222- 227. 20
Vizakat Lathika, I-Iarkantra, S. N., Parulekar, A. H., 1991. Population ecology and community structure of subtidal soft sediment dwelling macro-invertebrates ofKonkan, West coast ofIndia. Indian J. Mar. Sci. 20 (1), 40-42.
Page 2 and 3: Certificate I hereby certify that t
Page 4 and 5: Contents Page No. Chapter 1. Introd
Page 6: the bottom. Ekman (1935) described
Page 9 and 10: wonns are the most abundant group a
Page 11 and 12: leadership of Sir James Clark Ross,
Page 13 and 14: Ansari et al., (1977b) carried out
Page 15 and 16: Gopalakrishnan and Nair (1998) cond
Page 17 and 18: Major objectives:- 1. To understand
Page 19 and 20: CMFRI (Central Marine Fisheries Res
Page 21 and 22: Joydas, T.V., Damodaran, R., 2001.
Page 23: monitoring committee (Atlantic Mari
Page 28 and 29: analysed after acidification by tit
Page 30: used as stain prior to sorting and
Page 33 and 34: space. Therefore, it is very essent
Page 36 and 37: Fig. I - Station locations 32
Page 39 and 40: affected at high temperature. Most
Page 41 and 42: layers exhibit different oceanograp
Page 43: Transect wise variation in temperat
Page 46 and 47: 3.2.2.3. Dissolved oxygen (DO) Dist
Page 48 and 49: monsoon temperature initially incre
Page 50 and 51: opined that limited mixing. high or
Page 52 and 53: Naqvi, S. W. A., Noronha, R. J., Re
Page 56: orr Mormugao orr Vernal 35.36 35.32
Page 62 and 63: The continental shelf and its adjoi
Page 64: sediments (4 stations). Silty sand
Page 68 and 69: fine sediments with comparatively h
Page 70 and 71: Narayana, 1991 ). Limited input of
Page 73 and 74: In general. two ditlerent patterns
Page 75 and 76:
et al., (1980) reported values in t
Page 77 and 78:
organisms living in the water and t
Page 79 and 80:
Hashimi, N. H., Kidwai, R. M., Nair
Page 81 and 82:
Postma, H., 1967. In Estuaries, Lau
Page 85:
Depths Sand Silt Clay Organic matte
Page 90:
• PRE'MONSOON SOUTHERN'TRANSECTS
Page 96 and 97:
as the best indicators of the envir
Page 99 and 100:
showed that northern transects have
Page 101 and 102:
decreased from shallow to deeper de
Page 103:
different depth zones showed that a
Page 106 and 107:
cm 2 with a dominance of nematodes.
Page 108 and 109:
and 6.08 g/m 2 were recorded during
Page 110 and 111:
were located in the nearshore water
Page 112 and 113:
changes in the hydrographical and t
Page 114 and 115:
factor for such a large difference
Page 116 and 117:
Belegvad, H., 1932. Investigations
Page 118 and 119:
Parulekar, A. H., Harkantra, S. N.,
Page 120:
Savich, M. S., 1972. Quantitative d
Page 123 and 124:
Traosects Polychaetes Crustaceans M
Page 125:
Miscellaneous Transects Nematodes C
Page 128 and 129:
Depths Nematodes Cope pods Foramini
Page 136 and 137:
Wagh, 1975; Parulekar et ai, 1976;
Page 138 and 139:
ones and 17 were included in the 'r
Page 140 and 141:
Nephtydae (2%). Among the 20 sedent
Page 143 and 144:
At 75 m zone, 31 groups/species wer
Page 145 and 146:
Porbandar. At 50 m depth zone, fluc
Page 148 and 149:
otTMumbai and Ratnagiri and low eve
Page 150 and 151:
species richness at each depth zone
Page 153 and 154:
E2.2.2.!. Richness (Margalef's inde
Page 155:
I ):.2.2.2.4. Dominance (Pie/ou's i
Page 172 and 173:
Tablc 17. Contd .. - Sternaspidae 0
Page 176:
Table 20. contd .. G. alba 20 25 20
Page 179:
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 and 234:
Longhrust, A. R., Pauly, D., 1987.
Page 235 and 236:
Sikora, W. B., 1977. The ecology of
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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