Reply to the comment by Dominique Schwartz on the paper “Geochronological arguments for a close relationship between surficial formation profiles and environmental crisis (c. 3000–2000BP) in Gabon (Central Africa)”, by D. Thiéblemont et al., 2013 [C.R. Geoscience 345, 272–283]
Author:
Publisher
Elsevier BV
Subject
General Earth and Planetary Sciences,Global and Planetary Change
Reference17 articles.
1. Loess accumulation and soil formation in Kaokoland (Northern Namibia) as indicators of Quaternary climatic changes;Brunotte;Global Planet. Change,2000
2. A sequence of fluvial and aeolian deposits (desert loess) and palaeosoils covering the last 60 ka in the Opuwu basin (Kaokoland/Kunene Region, Namibia) based on luminescence dating;Brunotte;Quat. Int.,2009
3. Contribution de l’étude exoscopique des quartz à la reconstitution paléogéographique des derniers épisodes du Quaternaire littoral du Congo;Giresse;Quat. Res.,1981
4. Late-Holocene equatorial environments inferred from deposition processes, carbon isotopes of organic matter, and pollen in three shallow lakes of Gabon, west-central Africa;Giresse;J. Paleolimnol.,2009
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