(Table 1) Sapropel analysis from ODP Sites 160-964, 160-966, 160-967 and 160-969
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| Format: | Dataset Open Access |
| Langue: | en |
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PANGAEA
2000
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| _version_ | 1867170915757850624 |
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| author | Nijenhuis, Ivar A de Lange, Gert J |
| author_facet | Nijenhuis, Ivar A de Lange, Gert J |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Seventeen eastern Mediterranean Pliocene sapropels from ODP Sites 964, 966, 967 and 969, some of which are coeval, have been analysed for their geochemistry. The sapropels are characterized by very high organic carbon contents (up to 30%) which are reported to be the result of both increased productivity and improved preservation. Although the organic matter in the sapropels is mainly of marine origin, the d13Corg values and C/N ratios appear "terrestrial". This is the result of anaerobic organic matter degradation which preferentially removed nitrogen- and 13C-rich organic components. A comparison with Ti/Al profiles, which mimic the precession index, and a calculation of organic carbon accumulation rates indicate that sedimentation rates were at most 30% lower or at most 50% higher during sapropel formation. Thus, sapropel formation lasted from between 2000 and 10,000 years at Site 964 to between 4500 and 12,000 years at Site 967. A synthesis of new data and a comparison with existing models indicates that productivity, which increased due to extra nutrients supplied as a result of winter mixing and as a result of enhanced input by the Nile, was the driving mechanism behind sapropel formation. The resulting sapropel formation was simultaneous at different depths, but lasted longer in the part of the basin closest to the Nile. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_767464 |
| institution | PANGAEA |
| language | en |
| publishDate | 2000 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | (Table 1) Sapropel analysis from ODP Sites 160-964, 160-966, 160-967 and 160-969 Nijenhuis, Ivar A de Lange, Gert J 160-964D; 160-964E; 160-966C; 160-967B; 160-967C; 160-969D; 160-969E; Age model; Comment; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Eastern Basin; Event label; Interval comments; Joides Resolution; Leg160; Ocean Drilling Program; ODP; Sample code/label; Sample code/label 2; Sedimentation rate Seventeen eastern Mediterranean Pliocene sapropels from ODP Sites 964, 966, 967 and 969, some of which are coeval, have been analysed for their geochemistry. The sapropels are characterized by very high organic carbon contents (up to 30%) which are reported to be the result of both increased productivity and improved preservation. Although the organic matter in the sapropels is mainly of marine origin, the d13Corg values and C/N ratios appear "terrestrial". This is the result of anaerobic organic matter degradation which preferentially removed nitrogen- and 13C-rich organic components. A comparison with Ti/Al profiles, which mimic the precession index, and a calculation of organic carbon accumulation rates indicate that sedimentation rates were at most 30% lower or at most 50% higher during sapropel formation. Thus, sapropel formation lasted from between 2000 and 10,000 years at Site 964 to between 4500 and 12,000 years at Site 967. A synthesis of new data and a comparison with existing models indicates that productivity, which increased due to extra nutrients supplied as a result of winter mixing and as a result of enhanced input by the Nile, was the driving mechanism behind sapropel formation. The resulting sapropel formation was simultaneous at different depths, but lasted longer in the part of the basin closest to the Nile. |
| title | (Table 1) Sapropel analysis from ODP Sites 160-964, 160-966, 160-967 and 160-969 |
| topic | 160-964D; 160-964E; 160-966C; 160-967B; 160-967C; 160-969D; 160-969E; Age model; Comment; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Eastern Basin; Event label; Interval comments; Joides Resolution; Leg160; Ocean Drilling Program; ODP; Sample code/label; Sample code/label 2; Sedimentation rate |
| url | https://doi.org/10.1594/PANGAEA.767464 |