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A 2-m-long, shallow-water sediment core, representing the last 2,500 years, collected from the tropical Arabian Sea from the inner shelf (22 m water depth) off Karwar, near the mouth of the Kali River, has been studied for sedimentological proxies (granulometry) and foraminiferal tracers of paleomonsoons. The results suggest a considerable decrease in the intensity of monsoons approximately around...
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