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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
- 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
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- 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 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
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Icvci (p
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mcioHmna serve primarily as rapid m
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surface chlorophyll a was 0.36mg I
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Devassy, V. P., Achuthankutty, C. T
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Longhrust, A. R., Pauly, D., 1987.
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Sikora, W. B., 1977. The ecology of
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Faunal groups Silty Clayey Mixed Sa
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Mannagoa to Porbandar located betwe
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against gastropods during pre- mons