Identification of marker horizon in bottom sediments of the Onega Periglacial Lake
A study reports the identificaiton of a marker horizon in bottom sediments of the Onega Periglacial Lake. A sharp decrease in sedimentation rates and OM input fostered the oxidation of bottom sediments. This is reflected in the formation of the pinkish brown, iron oxide-rich, 30-cm-thick horizon of...
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| Veröffentlicht in: | Doklady earth sciences 2006-02, Vol.407 (1), p.213-216 |
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| creator | Demidov, IN |
| description | A study reports the identificaiton of a marker horizon in bottom sediments of the Onega Periglacial Lake. A sharp decrease in sedimentation rates and OM input fostered the oxidation of bottom sediments. This is reflected in the formation of the pinkish brown, iron oxide-rich, 30-cm-thick horizon of varved clays over the entire vast area of the Onega periglacial lake. |
| doi_str_mv | 10.1134/S1028334X06020127 |
| format | Article |
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| ispartof | Doklady earth sciences, 2006-02, Vol.407 (1), p.213-216 |
| issn | 1028-334X 1531-8354 |
| language | eng |
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| source | SpringerNature Journals |
| subjects | Bottom sediments Geochemistry Iron oxides Lakes Limnology Sedimentation rates Sediments |
| title | Identification of marker horizon in bottom sediments of the Onega Periglacial Lake |
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