File:Contmargin-glacial hg.png
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| Description |
Scetch of the glaciomarine sedimentation at the margin of an ice-covered continent during interglacials (a) and during glacials (b). (b) During glacials, the gravitational sediment transport is dominant. A lower sea level provides suitable conditions for buldozed deposits on the shelf by the advancing ice sheet. Primary production is reduced due to missing light in surface waters under a continous closed sea ice coverage which also prevents icebergs to calve and to distribute its sediment load. |
| 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 |
| Permission (Reusing this file) |
Creative Commons Attribution 3.0 |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 20:17, 25 December 2009 | | 1,672 × 1,081 (715 KB) | Hgrobe | {{Information |Description=Scetch of the glaciomarine sedimentation at the margin of an ice-covered continent during interglacials (a) and during glacials (b). (b) During glacials, the gravitational sediment transport is dominant. A lower sea level provid |
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