000202241 001__ 202241
000202241 005__ 20181203023628.0
000202241 0247_ $$2doi$$a10.1016/j.gr.2013.08.014
000202241 022__ $$a1342-937X
000202241 02470 $$2ISI$$a000342524200023
000202241 037__ $$aARTICLE
000202241 245__ $$aRedox variations and bioproductivity in the Ediacaran: Evidence from inorganic and organic geochemistry of the Corumba Group, Brazil
000202241 260__ $$bElsevier$$c2014$$aAmsterdam
000202241 269__ $$a2014
000202241 300__ $$a22
000202241 336__ $$aJournal Articles
000202241 520__ $$aStable isotope ratios combined with elemental compositions and molecular biomass data provide a powerful tool in Neoproterozoic palaeoenvironmental interpretations. Here, we report the results of an extensive organic and inorganic geochemical study performed in the Ediacaran sedimentary succession of the Corumba Group (CG) from SW-Brazil, deposited in a shallow marine basin in southwestern Gondwana. This sedimentary succession and in particular the Tamengo Formation, a unit bearing metazoan fossils, has been investigated by means of stable isotopes from carbonates (delta C-13(car) and delta O-18) and associated organic matter (delta C-13(ker) and delta N-15(ker)) together with hydrocarbon distribution and concentrations of major, trace and rare earth elements (REE). A short post-glacial delta C-13(car) negative excursion, interpreted as a period of water mixing, is recorded in the cap carbonates overlying diamictites of the Puga Formation, related to Gaskiers or end-Cryogenian glaciation. The overlying Tamengo Formation by contrast, represents a return to redox-stratified conditions in the basin before the Precambrian-Cambrian boundary. Two distinct biogeochemical modes alternate during deposition of Tamengo sediments: 1) an eutrophic, redox-stratified basin well defined by carbonaceous marls from the middle part of the unit but also recorded upwards, at the transition between bioclastic limestones and calcisiltites. 2) An anoxic basin well characterized in the shallow facies, particularly by bioclastic limestones of the upper Tamengo Formation. A positive Delta C-13(car-ker) (Delta C-13(car-ker) = delta C-13(car) - delta C-13(ker)) excursion of similar to 5% in the carbonaceous marls is explained by enhanced primary productivity in surface waters probably related to an increase of pCO(2), nutrient supply and possibly also changes of the primary producer communities. Abundant pyrite, a biomarker distribution characterized by the occurrence of gammacerane and a low Pr/Ph ratio (similar to 0.7) are also remarkable signatures of these facies, most probably associated with a sulfate-reducing microbial consortium in an anoxic and sulfidic (euxinic) environment. However, low concentrations in redox-sensitive trace elements in these fades suggest a largely oxygenated water column, thus constraining the euxinic setting to the sediments and/or bottom waters. The shallow-water bioclastic limestones record higher concentrations of redox-sensitive elements and Sigma REE as well as a positive Ce anomaly supporting reducing conditions. Oxygenated conditions and dominance of eukaryotic algae characterize the overlying Guaicurus Formation. Principal component analysis (PCA) was used to assess the major geochemical associations. The most significant component combines parameters involved in primary production, such as P concentrations and delta C-13(ker) values. The bio-chemostratigraphic variations in this part of SW-Gondwana point to a stratified ocean with oxic surface waters, alternating periods of high and low bioproductivity and anaerobic conditions at the bottom waters, in the aftermath of younger Neoproterozoic glaciations and close to the Precambrian-Cambrian boundary. (C) 2013 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.
000202241 6531_ $$aChemostratigraphy
000202241 6531_ $$aEdiacaran
000202241 6531_ $$aSW-Gondwana
000202241 6531_ $$aCorumba Group
000202241 6531_ $$aRedox stratification
000202241 700__ $$uUniv Lausanne, Inst Earth Sci, CH-1015 Lausanne, Switzerland$$aSpangenberg, Jorge E.
000202241 700__ $$uUniv Lausanne, Inst Earth Sci, CH-1015 Lausanne, Switzerland$$aBagnoud-Velasquez, Mariluz
000202241 700__ $$uUniv Sao Paulo, Inst Geociencias, BR-01498 Sao Paulo, Brazil$$aBoggiani, Paulo C.
000202241 700__ $$aGaucher, Claudio
000202241 773__ $$j26$$tGondwana Research$$k3-4$$q1186-1207
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