http://www.sciencedirect.com/science/article/pii/S1674987111001356 |
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Authors: | Abhijit Mazumder Rajiv Nigam Pravin J Henriques |
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Institution: | 1. Birbal Sahni Institute of Palaeobotany,53 University Road,Lucknow 226 007,India 2. National Institute of Oceanography,Dona Paula,Goa 403 004,India 3. Department,St. Xavier's College,Mahapalika Marg,Mumbai 400 001,India |
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Abstract: | A total of 103 surface sediment samples collected from the water depth range of 15—3300 m along Vijaydurg-Karwar stretch of central west coast of India were analyzed for foraminiferal content. Relict benthic foraminiferal assemblage was noted within 50—135 m water depth.The relict benthic foraminiferal assemblage that includes Amphistegina,Operculum and Alveolinetta in sediment samples within the water depth of 85—135 m indicates presence of coral reef at this depth during Early Holocene. The presence of barnacle fouling on Relict foraminifera at 60—90 m confirms the paleo-shoreline. The shallow depth zone is characterized by presence of agglutinated relict foraminifera.The agglutinated forms indicate freshwater influx,which eventually increased the sea level and subsequently deteriorated the paleo-coral reef. |
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Keywords: | Relict benthicforaminifera Early Holocene coral reefPaleo-shoreline West coast of India Sea level rise |
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