scholarly journals The Role of Redox Processes in Determining the Iron Isotope Compositions of Minerals, Melts, and Fluids

Author(s):  
Paolo A. Sossi ◽  
Baptiste Debret
Keyword(s):  
1990 ◽  
Vol 290 (1-2) ◽  
pp. 269-274 ◽  
Author(s):  
S. Cordoba-Torresi ◽  
C. Gabrielli ◽  
M. Keddam ◽  
H. Takenouti ◽  
R. Torresi

2018 ◽  
Vol 82 (5) ◽  
pp. 1217-1230 ◽  
Author(s):  
Lucas Resmini Sartor ◽  
Robert C. Graham ◽  
Samantha C. Ying ◽  
Xosé Luis Otero ◽  
Célia Regina Montes ◽  
...  

1971 ◽  
Vol 27 (1-2) ◽  
pp. 251-264 ◽  
Author(s):  
K. B. Yatsi-Mirskii
Keyword(s):  

2009 ◽  
Vol 8 (3) ◽  
pp. 371 ◽  
Author(s):  
Alfonso Blázquez-Castro ◽  
Juan C. Stockert ◽  
Francisco Sanz-Rodríguez ◽  
Alicia Zamarrón ◽  
Angeles Juarranz

2021 ◽  
Vol 2 (1) ◽  
Author(s):  
Yanhong Chen ◽  
Yaoling Niu ◽  
Meng Duan ◽  
Hongmei Gong ◽  
Pengyuan Guo

AbstractThe iron isotope contrast between mid-ocean ridge basalts and abyssal peridotites is far greater than can be explained by mantle melting alone. Here we investigate a suite of mid-ocean ridge magma chamber rocks sampled by the Ocean Drilling Project Hole 735B in the Atlantis Bank of the Indian Ocean. We report major and trace element geochemistry from these rocks and measure their iron isotope compositions to investigate the potential role of fractional crystallization during melt evolution. We observe a large range of δ56Fe that defines a significant inverse curvilinear correlation with bulk rock MgO/FeOT. These data confirm that δ56Fe in the melt increases as fractional crystallization proceeds but, contrary to expectation, δ56Fe continues to increase even when oxides begin to crystallize. We conclude that iron isotope fractionation through fractional crystallization during the evolution of mid-ocean ridge basalts from abyssal peridotites reconciles the disparity in isotopic compositions between these two lithologies.


1997 ◽  
Vol 78 (6) ◽  
pp. 423-427
Author(s):  
S. V. Tsurkan ◽  
O. I. Lineva ◽  
F. N. Gilmiyarova ◽  
M. Yu. Zasypkin

Проведено комбинированное обследование 255 беременных женщин, проживающих в различных экологических зонах Самарской области, с акцентом на оценку внутриутробного состояния плода. Значительные изменения выявлены в неблагоприятных экологических зонах: высокая частота симметричных форм синдрома маловесного плода, нарушения в системе антиоксидантной защиты, выражающиеся в угнетении ферментативной активности (каталазы и глутатионредуктазы), снижение содержания ионизированного железа и мочевой кислоты как показателя активности перекисного окисления липоидов и водородного дефицита, а также снижение пластических резервов организма.


Author(s):  
Anita Jasińska ◽  
Dorota Burska ◽  
Jerzy Bolałek

AbstractSulfur is an element commonly occurring in the environment. It is present in the atmosphere, in the hydrosphere, and in live organisms; it is one of the most important physicochemical and geological indicators. Depending on the natural conditions, sulfur compounds in the environment may play the role of electron acceptor or donor in the redox processes. These compounds influence the ion concentration and ion balance in benthic sediments. They also determine the speciation, bioavailability and toxicity of heavy metals. Comprehensive knowledge of the processes mediated by sulfur can be a valuable source of information about the past and present state of the ecosystem.


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