Historical Reconstruction of Terrestrial Organic Matter Inputs to Fiordland, NZ Over the Last ~500 Years
Fjords contain a significant quantity of sediments deposited in coastal zones over the last ~100,000 years. Studies of Northern Hemisphere fjords have shown that a large part of the high concentration of sedimentary organic matter (OMsed) is terrestrial in origin (OMterr), composed of a modern detri...
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Format: | Others |
Language: | en_US |
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2012
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Online Access: | http://hdl.handle.net/1969.1/ETD-TAMU-2011-08-10089 |