Deterioration of Early Holocene coral reef due to sea level rise along west coast of India: Benthic foraminiferal testimony

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, Operculina and Alveolinella 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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► Relict benthic foraminifera from 85 to 135 m water depth along West Coast of India.
► Foraminifera indicates presence of Early Holocene coral reef.
► Freshwater influx deteriorated the paleo-coral reef.