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| Description | Major biogeneous components contributing to marine sediments are the remains of single celled plankton and benthos organisms. The hardpart shells are made out of silica (opal), i.e. radiolaria (a, ø=350 µm) and diatoms (b, ø=50 µm) or out of calcium carbonate, i.e. foraminifera (c, ø=400 µm) and coccoliths (d, ø=15 µm). |
| Date | |
| Source | Grobe, H., Diekmann, B., Hillenbrand, C.-D.(2009). The memory of the Polar Oceans, In: Hempel, G. (ed) Biology of Polar Oceans, hdl:10013/epic.33599.d001, pdf 0.4 MB. |
| Author | Hannes Grobe/AWI |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 20:21, 25 December 2009 | | 8,000 × 8,000 (6.18 MB) | Hgrobe | {{Information |Description=Major biogeneous components contributing to marine sediments are the remains of single celled plankton and benthos organisms. Its hardpart shells are made out of silica (opal), i.e. radiolaria (a, ø=350 µm) and diatoms (b, ø= |
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