The Tsitsikamma coastal shelf, Agulhas Bank, South Africa: example of an isolated Holocene sediment trap

Author:

Flemming Burg W.,Keith Martin A.

Funder

Council for Scientific and Industrial Research

Publisher

Springer Science and Business Media LLC

Subject

Earth and Planetary Sciences (miscellaneous),Geotechnical Engineering and Engineering Geology,Environmental Science (miscellaneous),Oceanography

Reference57 articles.

1. Bassetti M-A, Berné S, Sicre M-A, Dennielou B, Alonso Y, Buscail R, Jalali B, Herbert B, Menniti C (2016) Holocene hydrological changes in the Rhône River (NW Mediterranean) as recorded in the marine mud belt. EGU Clim Past 12:1539–1553

2. Birch GF (1980) Nearshore Quaternary sedimentation off the south coast of South Africa. Geol Surv S Afr Bull 67:1–20

3. Birch GF (1981) Bathymetry and geomorphology of the Cape Seal to Cape Recife inner shelf. Trans Geol Soc S Afr 84:233–237

4. Brain CK, Meester J (1964) Past climatic changes as biological isolating mechanisms in southern Africa. In: Davis DHS (ed) Ecological studies in southern Africa. Junk, The Hague, pp 332–340

5. Brown AG, Carey C, Erkens G, Fuchs M, Hoffmann T, Macaire J-J, Moldenhauer K-M, Walling DE (2009) From sedimentary records to sediment budgets: multiple approaches to catchment sediment flux. Geomorphology 108:35–47

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