Molybdenum isotope records of the Chilpi Group, Bastar Craton, India: Implications on atmospheric and shallow-seawater oxygen content in the Orosirian period
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引用次数: 0
Abstract
The Chilpi Group (2050 – 1850 Ma), central India, preserves iron formations of the Paleoproterozoic Era. The PO2 value of 10-3 – 10-5 times the present atmospheric level (PAL) during deposition of the Chilpi Group was reported from the analyses of the geothermometry and oxygen fugacity variations using the mineral chemistry of the rare association of magnetite-greenalite-cronstedtite-siderite in the iron-rich rocks. To validate the results obtained from the mineral chemistry, and to understand the evolution of ocean redox conditions and low PO2 value, we measured the Mo concentration and Mo isotope data of iron-formation samples. The analytical results of δ98/95MoNIST values have a range from –0.2 to 1.2 ‰, similar to the sediments deposited below anoxic (ferruginous – non-euxinic) water columns. The δ98/95MoNIST data calculated for adsorption removal of Mo from the modern seawater value of 2.09 ‰ show a negative offset (Δ 98/95Mo) of –0.7 ‰ for ferrihydrite adsorption model and –0.97 ‰ for magnetite adsorption model. The range of Δ 98/95Mo value of the Chilpi iron-formations is between –0.6 ‰ of 2.5 Ga iron-formations and –1.2 ‰ of 1.85 Ga iron-formations. A comparable range of δ98/95MoNIST (–0.3 to 1.8 ‰) and Δ 98/95Mo of –0.8 ‰ for ferrihydrite adsorption model for the iron-formations of the Animikie Basin, Lake Superior region, corroborate the observations. The results indicate a low value of the paleo-seawater (δ98/95MoNIST = 1.12 ‰) during the Orosirian Period, interpreted to be the result of a low oxygen content of the atmosphere and shallow sea and inefficient Mo-removal from the seawater. The lowered paleoproductivity due to the low level of atmospheric oxygen (between 10–3 and 10–5 PAL) and a reduced content of Mo, a bio-essential element, in seawater during the late Paleoproterozoic Era might have an impeding effect on the development of eukaryotes.
期刊介绍:
Gondwana Research (GR) is an International Journal aimed to promote high quality research publications on all topics related to solid Earth, particularly with reference to the origin and evolution of continents, continental assemblies and their resources. GR is an "all earth science" journal with no restrictions on geological time, terrane or theme and covers a wide spectrum of topics in geosciences such as geology, geomorphology, palaeontology, structure, petrology, geochemistry, stable isotopes, geochronology, economic geology, exploration geology, engineering geology, geophysics, and environmental geology among other themes, and provides an appropriate forum to integrate studies from different disciplines and different terrains. In addition to regular articles and thematic issues, the journal invites high profile state-of-the-art reviews on thrust area topics for its column, ''GR FOCUS''. Focus articles include short biographies and photographs of the authors. Short articles (within ten printed pages) for rapid publication reporting important discoveries or innovative models of global interest will be considered under the category ''GR LETTERS''.