Depositional age, provenance, and tectonic and paleoclimatic settings of the late Mesoproterozoic–middle Neoproterozoic Mbuji-Mayi Supergroup, Democratic Republic of Congo

• Published in: Palaeogeography, palaeoclimatology, palaeoecology palaeoclimatology, palaeoecology, 2013-11, Vol.389, p.4-34
• Main Authors: Delpomdor, Franck, Linnemann, Ulf, Boven, Ariel, Gärtner, Andreas, Travin, Aleksey, Blanpied, Christian, Virgone, Aurélien, Jelsma, Hielke, Préat, Alain
• Format: Article
• Language: English
• Subjects: Ages; Chemostratigraphy; Mbuji-Mayi Supergroup; Paleoclimate; Sankuru-Mbuji-Mayi-Lomami-Lovoy Basin
• ISSN: 0031-0182; 1872-616X
• DOI: 10.1016/j.palaeo.2013.06.012

The late Mesoproterozoic–middle Neoproterozoic period (ca. 1300Ma–800Ma) heralded extraordinary climatic and biological changes related to the tectonic changes that resulted in the assembly (~1.0Ga) and the break-up of Rodinia (880Ma–850Ma). In the Democratic Republic of Congo, these changes are recorded in the Mbuji-Mayi Supergroup which was deposited in the SE–NW trending siliciclastic-carbonate failed-rift Sankuru-Mbuji-Mayi-Lomami-Lovoy Basin. New LA-ICP–MS U–Pb laser ablation data on detrital zircon grains retrieved from the lower arenaceous-pelitic sequence (BI group) together with C and Sr isotopic data on carbonates from the upper dolomitic-pelitic sequence (BII group) and an 40Ar/39Ar age determination on a dolerite give a new depositional time frame between 1174±22Ma and ca. 800Ma for the Mbuji-Mayi Supergroup. The upper age limit is based on the assumption that the transition between the BIIb and BIIc subgroups recorded the Bitter Springs anomaly. In terms of tectonic and paleoclimatic settings, the BII group was deposited in the eastern passive margin of the Congo Craton during warm periods interlaced with temporarily dry and wet seasons, suggesting greenhouse conditions during the fragmentation of Rodinia. •Mbuji-Mayi Supergroup deposited in an intracratonic failed-rift basin.•Minimum LA-ICP–MS U–Pb age for detrital BId zircons gave 1174±22Ma.•Provenance of detrital zircon grains is south-east and/or east.•C and Sr isotopic curves for BII group are coeval with the Bitter Springs anomaly.•40Ar/39Ar age on ‘Lomami’ dolerite sill yielded 882.2±8.8Ma.