Evidence for environmental conditions during the last 20 000 years in Southern Africa from 13C in fossil hyrax dung

Scott L & Vogel JC

Eds: Kroepelin S & Petit-Maire N

Global and Planetary Change, vol. 26(1-3), 207-215, 2000

https://doi.org/10.1016/S0921-8181(00)00045-X

This article appears in "Paleomonsoon Variations and Terrestrial Environmental Change", a special issue comprising 18 articles based on papers presented by internationally renown quaternarists at the Berlin (1995) and Siwa (1997) "Paleomonsoons" meetings. It is a contribution to the Paleomonsoons Project of INQUA and PAGES, in coordination with several other international programmes such as the Pole-Equator-Pole Transects (PEP I–III), the International Decade of East African Lakes (IDEAL) and the Paleoclimate Modelling Intercomparison Project (PMIP).

Category: Special issue articles