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Envirnonmental changes since 32 000 BP at Kathu Pan, northern Cape

Other title
Changements environnementaux depuis 32 000 BP à Kathu Pan au Nord de la province du Cap (fr)
Author
BEAUMONT, P.B1 ; VAN ZINDEREN BAKKER, E.M; VOGEL, J.C
[1] McGregor museum, Kimberley, South Africa
Conference title
Late Cainozic palaeoclimates of the Southern Hemisphere. International symposium held by the South African Society for Quaternary Research; Swaziland
Conference name
Late Cainozic palaeoclimates of the Southern Hemisphere. International symposium held by the South African Society for Quaternary Research; Swaziland (1983-08-29)
Source

Late Cainozic palaeoclimates of the Southern Hemisphere. International symposium held by the South African Society for Quaternary Research; Swaziland. 1984, pp 329-338 ; Illustration , Section , Stratigraphic column ; ref : 1 p

Publisher
A.A.Balkema, Rotterdam
Publication country
Netherlands
Document type
Conference Paper
Language
English
Keyword (fr)
Holocène Le Cap Paléoclimat Pleistocène sup Tourbe Paléochenal Afrique du Sud Quaternaire Roche carbonée Roche sédimentaire République Sud Africaine
Keyword (en)
Holocene Cape Province Paleoclimatology Upper Pleistocene Peat Organic residues Quaternary Sedimentary rocks South Africa Southern Africa
Keyword (es)
Holoceno El Cabo Paleoclima Pleistoceno sup Turba Cuaternario República de Sudáfrica Roca carbonosa Roca sedimentaria África Sur
Classification
Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences / 001E01P Surficial geology / 001E01P02 Marine and continental quaternary

Discipline
Earth sciences
Origin
BRGM
Database
PASCAL
INIST identifier
7268015

Sauf mention contraire ci-dessus, le contenu de cette notice bibliographique peut être utilisé dans le cadre d’une licence CC BY 4.0 Inist-CNRS / Unless otherwise stated above, the content of this bibliographic record may be used under a CC BY 4.0 licence by Inist-CNRS / A menos que se haya señalado antes, el contenido de este registro bibliográfico puede ser utilizado al amparo de una licencia CC BY 4.0 Inist-CNRS

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