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• PRE'MONSOON SOUTHERN'TRANSECTS Fig. 16a. Triangular diagram showing sediment distribution in southern transects during pre-monsoon season • PRE - MONSOON NORTHERN TRANSECTS ----'''----- -----L-------''----S-IL-'T Fig. 16 b Triangular diagram showing sediment distribution in northern transects during pre-monsoon season 85
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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
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 95 and 96: 5.1. Introduction 5.2. Results 5.2.
Page 97: espectively. Parulekar and Wagh (19
Page 100 and 101: more only at stations off Ratnagiri
Page 102 and 103: elaatively higher average density i
Page 105 and 106: that nematodes contributed 27.3 (10
Page 107 and 108: Ratnagiri. Density was comparal ive
Page 109 and 110: Difference in biomass and density n
Page 111 and 112: (1980) also reported high values in
Page 113 and 114: followed by foraminifers while Rodr
Page 115 and 116: 5.4. References Alongi, D. M., 1990
Page 117 and 118: Harkantra, S. N., Rodringnes, C. L.
Page 119 and 120: Peterson, C. G. J., 1913. Valuation
Page 122 and 123: Transects 30m Polychaetes Crustacea
Page 124 and 125: Transects Polychaetes Crustaceans M
Page 127 and 128: Transects Nematodes Copepods Forami
Page 129: Biomass 30m 50m 75m lOOm 150m ----_
Page 137 and 138: polychaetes, crustaceans contribute
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'abundant', 'moderately abundant' a
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constricta (920/m2), Prionospio pin
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etween 0.68 and 5.85 and in norther
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H2./.l.4. Dominance (Pie/ou's index
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uansects stations it varied from 0.
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transect stations. At 75 m zone als
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Average values of northern and sout
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Table 17. contd .. ._---_. P.ehlers
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Taxa 30m 50m 75m lOO m 150m CRUSTAC
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Table 20. Contd .. Pectinariidae --
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Depths Margalef Evenness Shanon Sim
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'" " 'H :0:0."':01 1 I L-_ _ ______
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a) b) c) d) e ) f) g) h) Plate 6 a)
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a) c) e) Plate 8 a) Atys sp. d) Gra
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(Gupta and Naqvi, 1984). It is also
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Many workers have suggested that sa
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Decrease of benthos with DO agrees
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crustaceans. This indicated that du
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(1987) also found high population d
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uue to the accumulation of OM (6%)
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important parameters were graded as
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Macrobenthos, by feeding on meioben
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a life span of about 3 months (Saja
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7.7. References Ahlstrom, E. H., 19
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Harkantra, S. N., Ayyappan Nair, An
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Parulekar. A. H., Ansari, Z. A., 19
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Polychaetes Crustaceans Molluscs M.
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Chapter 8. Summary and conclusion T
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zones. Low biomass and density obse
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production will be more than that o
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L - Cochin University of Science and Technology

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