Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/36153
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dc.contributor.authorNarayana, A C-
dc.contributor.authorSingh, A D-
dc.date.accessioned2016-10-26T04:42:39Z-
dc.date.available2016-10-26T04:42:39Z-
dc.date.issued1997-03-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/36153-
dc.description88-90en_US
dc.description.abstractUpwelling record for the last 1400 years has been documented from an innershelf sediment core based on conventional indices - CaCO3, organic matter and selected planktic foraminiferal species. The study reveals 4-5 intervals of increased abundance during similar to 150-200 y, 300-350 y, 700-800 y, around 900 y and 1100-1200 y BP. The abundance of upwelling indices during these time intervals reflects high productivity.en_US
dc.language.isoen_USen_US
dc.publisherNISCAIR-CSIR, Indiaen_US
dc.rights CC Attribution-Noncommercial-No Derivative Works 2.5 Indiaen_US
dc.sourceIJMS Vol.26(1) [March 1997]en_US
dc.titleUpwelling record in a sediment core from the innershelf off Mangalore, west coast of Indiaen_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.26(1) [March 1997]

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