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Conference program and abstracts - Coastal-Change.Org

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Benthic Foraminifera <strong>and</strong> siltation studies along the<br />

Depositional Environment between M<strong>and</strong>apam <strong>and</strong><br />

Kodiyakkarai, Palk Strait, East Coast of India<br />

M.Suresh G<strong>and</strong>hi <strong>and</strong> K. Kasilingam<br />

Department of Geology, University of Madras, Chennai- 600 025<br />

Email: surgan@yahoo.co.uk<br />

ABSTRACT<br />

Palk Strait is situated between India <strong>and</strong> Srilanka endangered with heavy<br />

siltation. It is strategically an important channel, as it is shared by India<br />

<strong>and</strong> Sri Lanka without the scope of international navigation. Of late, the<br />

coastal ecosystem of the strait is endangered by the shallowing nature of<br />

the bay due to silty sedimentation. In order to know the effect of siltation<br />

an attempt has been made in this region using foraminiferal studies. A<br />

total of 72 sediment samples have been collected in nine stations<br />

between M<strong>and</strong>apam <strong>and</strong> Vedaranyam. In that, 122 species belonging to<br />

54genera, 40 families, 24 super families <strong>and</strong> 5 suborders were identified.<br />

Of which, 38 species are provided as living specimens. Among the<br />

species present, Ammonia beccarii, Ammonia dentata, Osangularia<br />

venusta, Elphidium crispum, Asterorotalia trispinosa, Quinqueloqulina<br />

seminulam, Pararotalia nipponica exhibit prolific abundance. From the<br />

distribution of foraminiferal studies, it understood that the species are<br />

more enriched in southern part of Palk Strait compare to the northern<br />

part. The organic carbon content in the study area varies from 0.05 % to<br />

3.40 %. At Kodiyakkarai carbonate content reaches 19.5% at 7m depth.<br />

The higher carbonate content at Thondi <strong>and</strong> Kottaipattinam is probably<br />

due to the accumulation of high order broken shell debris dumped<br />

through the creek. Based upon the living dead ratio <strong>and</strong> the organic<br />

matter distribution it is confirmed that the southern part is more favor for<br />

living condition. Sedimentation also more in the southern part between<br />

M<strong>and</strong>apam <strong>and</strong> Manalmelkudi compare to the northern part. Cluster<br />

analysis indicates that three different genus dominant in particular stations<br />

like M<strong>and</strong>apam <strong>and</strong> Thondi represent the biotope at 0.82 level of<br />

clustering <strong>and</strong> the species Rosalina globularis is more abundant in that<br />

stations. Attankarai <strong>and</strong> Manalmelkudi show the level of clustering of 0.87<br />

with dominant of Ammonia beccarii. The stations Devipattinam,<br />

Kottaipattinam <strong>and</strong> Sethubavachattiram shows the level of clustering at<br />

0.9 <strong>and</strong> dominant of Pararotalia.Some genera like Asterorotalia, Lagena,<br />

Elphidium, Quinqueloqulina, Pararotalia <strong>and</strong> Spiroloculina are in broken,<br />

distorted <strong>and</strong> corroded are noticed in all the stations. The high order of<br />

broken species <strong>and</strong> aberration in forams is stations like M<strong>and</strong>apam,<br />

Devipattinam, Thondi <strong>and</strong> Sethubavachattiram indicate the presence of<br />

higher churning action of currents. The overall depletion of foraminifera in<br />

the strait indicates the unfavorable environmental conditions for living<br />

species.<br />

The Fourth IGCP 588: PREPARING FOR COASTAL CHANGE 19

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