Response to comment on "Climate-Driven Ecosystem Succession in the Sahara: The Past 6000 Years"

S. Kröpelin; Dirk Verschuren; A.-M. Lézine

doi:10.1126/science.1163483

Journal articles

Response to comment on "Climate-Driven Ecosystem Succession in the Sahara: The Past 6000 Years"

S. Kröpelin ^{1, *} Dirk Verschuren ² A.-M. Lézine ³

* Corresponding author

1 Africa Research Unit - Institute of Prehistoric Archaeology

2 Limnology Unit - Department of Biology

3 GLACCIOS - Glaces et Continents, Climats et Isotopes Stables

LSCE - Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] : DRF/LSCE

Abstract : The Lake Yoa record and archaeological data provide adequate evidence that mid-Holocene aridification did not occur abruptly across all of North Africa. Modeling results on the issue of abrupt versus gradual desiccation of the Sahara are sufficiently diverse that paleoecological data from a continuous natural archive can usefully guide the evaluation of model parameters responsible for this diversity.

Document type :

Journal articles

Domain :

Sciences of the Universe [physics] / Earth Sciences / Climatology

Environmental Sciences / Global Changes

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https://hal-cea.archives-ouvertes.fr/cea-00868626
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Submitted on : Monday, July 5, 2021 - 8:44:21 AM
Last modification on : Monday, May 9, 2022 - 11:58:07 AM

Response to comment on "Climate-Driven Ecosystem Succession in the Sahara: The Past 6000 Years"

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Response to comment on "Climate-Driven Ecosystem Succession in the Sahara: The Past 6000 Years"

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