Holocene Relative Sea-Level Change in Nova Scotia
Core samples collected around Atlantic Canada, specifically from the West Head salt marsh, Chezzetcook Inlet, enable temporal and spatial examination of benthic foraminiferal assemblages. Benthic foraminiferal zonations, representing specific environments above mean sea level, occur in salt marshes....
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| Format: | Report |
| Language: | unknown |
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2020
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| Online Access: | http://hdl.handle.net/10222/79956 |