Dating the rise of atmospheric oxygen bekker Live cams mom
The Ruwenzori Fold Belt and its rock protoliths are poorly dated, and the age of the volcano-sedimentary succession is only constrained between c. We report here on the stable isotope (C and O) geochemistry of marbles from the Ruwenzori Mountains in western Uganda, which has a bearing on the age of the Buganda Group.
A suite of samples of impure dolomitic and calcitic marbles from the High Peaks Schist and the Kilembe Schist subgroups, Buganda Group, was analyzed.
The Paleoproterozoic Era witnessed crucial steps in the evolution of Earth&amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;#39;s surface environments following the first appreciable rise of free atmospheric oxygen concentrations ∼2.3 to 2.1 Ga ago, and concomitant shallow ocean oxygenation.
While most sedimentary successions deposited during this time interval have experienced thermal overprinting from burial diagenesis and metamorphism, the ca.
"Isotopic dating of the Ongeluk large igneous province, South Africa, revealed that the first Paleoproterozoic global glaciation and the first significant step change in atmospheric oxygenation likely occurred between 2,460 and 2,426 million years ago, approximately 100 million years earlier than previous estimates," says Kevin Chamberlain, a UW research professor in the Department of Geology and Geophysics.Response of the redox state of the deep ocean to the rise of atmospheric oxygen, as well as the 2.22-2.1 Ga carbon isotope excursion that followed, is not known. 2.15 Ga Sengoma Argillite Formation (SAF), Botswana, is correlative with the Silverton Formation (SF), South Africa, which contains carbonates with delta °13°C values ranging from 8.3 to 11.3 0/00The Mbuji-Mayi Supergroup, deposited between 1170 ± 22 Ma and ca.800 Ma , outcrops in the eastern Oriental Kasai Province and western Katanga Province of the Democratic Republic of Congo.The Supergroup is divided into two groups: the lower, ∼ 500-m thick siliciclastics-rich BI Group and the upper, ∼ 1000-m thick carbonate-rich BII Group.Our own and previous sedimentological observations  indicate facies ranging from subtidal, low-energy stromatolitic environments to overlying intertidal to supratidal evaporitic settings of lago...