L - Cochin University of Science and Technology
L - Cochin University of Science and Technology
L - Cochin University of Science and Technology
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cm 2 with a dominance <strong>of</strong> nematodes. In general no distinct transect wise trend was<br />
observed.<br />
Percentage contribution within individual group at different depth (Table 13)<br />
showed that contribution <strong>of</strong> nematodes decreased with increasing depth while, rest <strong>of</strong><br />
the groups showed an opposite trend. Highest contribution <strong>of</strong> nematodes was at 30 m<br />
(56.7%) <strong>and</strong> lowest at 150 m (1.5 %). Copepods contributed maximum at 150 m<br />
zone (37.4%) <strong>and</strong> minimum at 50 m zone (9%). Miscellaneous groups also have<br />
relatively lower percentage contribution at 30 m (19.7%) <strong>and</strong> higher contribution at<br />
deeper depths <strong>of</strong> 100 m (28.5%), but exceptionally low value at 150 m (3.6%).<br />
5.2.4.2. Pre-monsoon<br />
Density followed the similar trend as that <strong>of</strong> biomass with relatively low<br />
density at the 30 m depth <strong>of</strong>f Mormugao <strong>and</strong> Mumbai while, high density was<br />
observed at 30 m depth <strong>of</strong>f Ratnagiri, Veraval <strong>and</strong> Dwaraka (Table 14). Overall<br />
percentage contribution by various groups to the total density (Table 14) showed that<br />
nematodes contributed more to the total density (65.3%) followed by foraminifers<br />
(25%) <strong>and</strong> miscellaneous groups (8%). Copepods were the least abundant group<br />
(1.3%).<br />
5.2.5. Seasonal comparison<br />
In general, average biomass <strong>and</strong> density <strong>of</strong> macrobenthos in the whole study<br />
area were high during pre-monsoon season than post-monsoon period (Fig. 33&34).<br />
In both seasons shallow depth stations registered high biomass <strong>and</strong> density, while it<br />
reduced considerably in deeper stations with some exceptions. During post-monsoon,<br />
even though no regular trend was observed, average biomass showed comparatively<br />
high value in the northern transect than its southern counterpart (Fig. 26). Biomass<br />
showed a northward increase during pre-monsoon. Average value <strong>of</strong> this season also<br />
showed comparatively high value in the northern transect than southern transect<br />
(Fig. 27), however, exceptionally high biomass was observed at 75 m depth otT<br />
101