Heness, ElizabethSimpson, Edward L.Bumby, Adam JohnEriksson, Patrick GeorgeEriksson, Kenneth A.Hilbert-Wolf, Hannah L.Okafor, O.J.Linnevelt, SarahMalenda, H. FitzgeraldModungwa, Tshepiso2015-11-182015-11-182014-08Heness, E, Simpson, EL, Bumby, AJ, Eriksson, PG, Eriksson, KA, Hilbert-Wolf, HL, Okafor, OJ, Linnevelt, S, Malenda, HF & Modungwa, T 2014, 'Evidence for climate shifts in the similar to 2.0 Ga upper Makgabeng Formation erg, South Africa', Palaeogeography, Palaeoclimatology, Palaeoecology, vol. 409, pp. 265-279.0031-0182 (print)1872-616X(online)10.1016/j.palaeo.2014.05.016http://hdl.handle.net/2263/50495Eolian ergs, and associated environs are sensitive to short- and long-term climate changes. In one of the oldest, erg deposits, the ~2.0 Ga Makgabeng Formation, facies association changes reflect one of the earliest recordings of short-term climatic shifts in a continental setting. The Makgabeng Formation is separated into lower and upper erg deposits by a playa or saline pan deposit. The lower erg deposit consists of dune sets with thin lenses of dry and deflationary interdunes that transitions vertically to thicker damp to wet interdunes. A laterally persistent playa deposit in the middle of the section consists of mudstone with deep and shallow penetrating mud cracks and subordinate siltstone and sandstone interbeds. Above this lower mudstone interval, the playa strata are sandy. Overlying the playa deposit, the upper erg deposit consists of thick eolian sets with thin lenses of dry interdune deposits. Grain size change near the top of the upper erg deposit corresponds to the appearance of fluvial, sheet flood, eolian cross-beds sculpted by mass flows, and thin playa deposits. The vertical facies association demonstrates shifts in precipitation and fluctuating water tables. Fluvial and playa deposits record high water tables whereas low-water tables are reflected in the core erg. The transition from a lower to higher water table is recorded by wet interdune interspersed within the dune strata towards the top of this interval. Rapid climatic amelioration occurred near the termination of the Makgabeng erg resulting in impingement of ephemeral river systems, development of playas, and generation of massive sand flows. This 2.0 Ga erg demonstrates the impact of climate change on erg development, resulting from shifts in the monsoonal impingement through time.en© 2014 Elsevier B.V. All rights reserved. Notice : this is the author’s version of a work that was accepted for publication in Palaeogeography, Palaeoclimatology, Palaeoecology. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Palaeogeography, Palaeoclimatology, Palaeoecology, vol. 409, pp. 265-279, 2014. doi : 10.1016/j.palaeo.2014.05.016.EolianPaleoproterozoicPlayaEphemeral riverMakgabeng FormationPostprint Article