Working Groups / Subsidence and palaeo sea-level change

Assessment of amounts and rates of long-term subsidence and sediment compaction in coastal sedimentary environments can be obtained measuring the displacement of geological paleo sea-level indicators relative to modelled relative sea-level elevations. In coastal plains, geological indicators are represented by dated intertidal peat sediments. The misfit between measured and modelled palaeo sea-level elevation can be attributed to the combined effect of regional subsidence and local sediment compaction. This can be disentangled using dated intertidal peat unconformably resting on top of the coastal plain substrate. After being corrected for the effect of compaction, the misfit between measured and modelled relative sea-levels provides a quantitative assessment of local subsidence since each of the dated peat layer and present day.

Subsidence and palaeo sea-level change

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