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Late Quaternary Halimeda bioherms and aragonitic faecal pellet-dominated sediments on the carbonate platform of the western continental shelf of India

DRS at CSIR-National Institute of Oceanography

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Title Late Quaternary Halimeda bioherms and aragonitic faecal pellet-dominated sediments on the carbonate platform of the western continental shelf of India
 
Creator Rao, V.P.
Veerayya, M.
Nair, R.R.
Dupeuble, P.A.
Lamboy, M.
 
Subject Geology and Geophysics
carbonate sediments
palaeoclimate
sediment properties
Quaternary
outer continental shelf
ISW, Arabian Sea
 
Description The Fifty Fathom Flat is a drowned carbonate platform located on the outer continental shelf of western India. It unique because the carbonate depositional environment prevailed until Early Holocene in spite of its proximity to major siliciclastic tidal embayment. Study of the bathymetry, seismic and sonograph data together with the petrology, mineralogy and geochemistry of the carbonate sediments and limestones recovered from the platform resulted in (a) the discovery of Late Quaternary Halimeda bioherms and (b) aragonitic faecal pellet-dominated sediments. It appears that fluvial sediments largely accumulate in the inner shelf and did not hinder carbonate growth on the platform, lying on the outer shelf. We presume that arid climate and nutrients brought by river runoff and shelf edge currents favoured the growth of algal bioherms dominated by Halimeda between 13,700 (?) and 8300 yr B.P. The absence of Late Holocene and modern carbonates on the platform may be due to the combined influence of climatic change, upwelling and neo-tectonic activity at about 9000 yr B.P. The bioherms dominated by Halimeda, produced abundant aragonite muds. Deposit feeding crustaceans and other invertebrates subsequently excreted these muds as faecal pellets. The platform thus contains faecal pellet-dominated sediments
 
Date 1995-01-24T10:06:29Z
2017-09-30T01:55:43Z
1995-01-24T10:06:29Z
2017-09-30T01:55:43Z
1994
 
Type Journal Article
 
Identifier Marine Geology, vol.121(3-4); 1994; 293-315
0025-3227
http://drs.nio.org/drs/handle/2264/7385
 
Language en
 
Relation Mar Geol
SCI
 
Publisher Elsevier