Upward range extension of Andean anurans and chytridiomycosis to extreme elevations in response to tropical deglaciation[1] The African Millennium Villages[2] Using palaeo-climate comparisons to constrain future projections in CMIP5[3] Isotopic reconstruction of the African Humid Period and Congo Air Boundary migration at Lake Tana, Ethiopia[4] Atmospheric circulation patterns during late Pleistocene climate changes at Lake Malawi, Africa .[5]