Distinction of marine and terrestrial origin of humic acids in North Sea surface sediments by absorption spectroscopy
A suite of humic acid isolates from terrestrial and marine soils and sediments have been analysed by UV/visible spectroscopy. Marine samples are characterised by a maximum at 407 nm which is lacking in terrestrial ones. The absorbance ratio of 270/407 nm (A2 /A4) can be used to differentiate humic a...
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Veröffentlicht in: | Marine geology 2000-03, Vol.164 (3-4), p.173-181 |
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description | A suite of humic acid isolates from terrestrial and marine soils and sediments have been analysed by UV/visible spectroscopy. Marine samples are characterised by a maximum at 407 nm which is lacking in terrestrial ones. The absorbance ratio of 270/407 nm (A2 /A4) can be used to differentiate humic acid sources as is demonstrated for North Sea surface sediments. Here, the southern coastal samples had high A2/A4 ratios indicating higher terrestrial contributions to the humic acid pool. In contrast, samples from the northern North Sea had low A2/A4 ratios suggesting higher marine contributions. Analysis of core samples and an Eocene oil shale indicates that the A2/A4 ratio is unaffected by early diagenetic processes. |
doi_str_mv | 10.1016/S0025-3227(99)00133-4 |
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Marine samples are characterised by a maximum at 407 nm which is lacking in terrestrial ones. The absorbance ratio of 270/407 nm (A2 /A4) can be used to differentiate humic acid sources as is demonstrated for North Sea surface sediments. Here, the southern coastal samples had high A2/A4 ratios indicating higher terrestrial contributions to the humic acid pool. In contrast, samples from the northern North Sea had low A2/A4 ratios suggesting higher marine contributions. Analysis of core samples and an Eocene oil shale indicates that the A2/A4 ratio is unaffected by early diagenetic processes.</description><identifier>ISSN: 0025-3227</identifier><identifier>DOI: 10.1016/S0025-3227(99)00133-4</identifier><language>eng</language><subject>Marine ; North Sea</subject><ispartof>Marine geology, 2000-03, Vol.164 (3-4), p.173-181</ispartof><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a371t-7ff49d8e33a16cb0085b8a45f59a42330151a6d93e8cdb15f5c1859921d75dc63</citedby><cites>FETCH-LOGICAL-a371t-7ff49d8e33a16cb0085b8a45f59a42330151a6d93e8cdb15f5c1859921d75dc63</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27901,27902</link.rule.ids></links><search><creatorcontrib>Fooken, U</creatorcontrib><creatorcontrib>Liebezeit, G</creatorcontrib><title>Distinction of marine and terrestrial origin of humic acids in North Sea surface sediments by absorption spectroscopy</title><title>Marine geology</title><description>A suite of humic acid isolates from terrestrial and marine soils and sediments have been analysed by UV/visible spectroscopy. 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title | Distinction of marine and terrestrial origin of humic acids in North Sea surface sediments by absorption spectroscopy |
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