Published in

Elsevier, Palaeogeography, Palaeoclimatology, Palaeoecology, (506), p. 139-153, 2018

DOI: 10.1016/j.palaeo.2018.06.029

Links

Tools

Export citation

Search in Google Scholar

A multi-proxy climate record from a northwestern Botswana stalagmite suggesting wetness late in the Little Ice Age (1810–1820 CE) and drying thereafter in response to changing migration of the tropical rain belt or ITCZ

This paper was not found in any repository, but could be made available legally by the author.
This paper was not found in any repository, but could be made available legally by the author.

Full text: Unavailable

Green circle
Preprint: archiving allowed
Orange circle
Postprint: archiving restricted
Red circle
Published version: archiving forbidden
Data provided by SHERPA/RoMEO