scholarly journals Native selenium as a byproduct of microbial oxidation of distorted pyrite crystals: the first occurrence in the Carpathians

2013 ◽  
Vol 64 (3) ◽  
pp. 231-236
Author(s):  
Eligiusz Szełęg ◽  
Janusz Janeczek ◽  
Paweł Metelski

Abstract Acicular crystals of native selenium up to 30 μm long occur together with barite on the surface of goethite partial pseudomorphs after millimeter-sized pseudotetragonal-prismatic pyrite crystals in calcite veins that cross-cut Senonian sandstones of the Silesian Nappe in the western Polish Outer Carpathians. Native selenium originated from selenium apparently released during bacteria-induced oxidation of pyrite at neutral or near-neutral pH conditions. Oxidizing bacteria preferentially colonized {100} faces of pyrite relative {111} faces.

2021 ◽  
Vol 122 ◽  
pp. 105127
Author(s):  
P. Madasamy ◽  
M. Mukunthan ◽  
P. Chandramohan ◽  
T.V. Krishna Mohan ◽  
Andrews Sylvanus ◽  
...  

2018 ◽  
Vol 24 (29) ◽  
pp. 7330-7334 ◽  
Author(s):  
Sonya K. Adas ◽  
Vinay Bharadwaj ◽  
Yang Zhou ◽  
Jiuhong Zhang ◽  
Alexander J. Seed ◽  
...  

2010 ◽  
Vol 03 (04) ◽  
pp. 104-112 ◽  
Author(s):  
Hiroyuki Jo ◽  
Katsuyuki Yugi ◽  
Seiichiro Ogawa ◽  
Yoshiyuki Suzuki ◽  
Yasubumi Sakakibara

2011 ◽  
Vol 62 (4) ◽  
pp. 333-343 ◽  
Author(s):  
M. Gasiński ◽  
Alfred Uchman

The Cretaceous-Paleogene boundary in turbiditic deposits identified to the bed: a case study from the Skole Nappe (Outer Carpathians, southern Poland)The Cretaceous-Paleogene (K-T) boundary has been recognized in turbiditic sediments of the Ropianka Formation in the Skole Nappe (Bąkowiec section) on the basis of planktonic foraminiferids with an accuracy of 40 cm. Such precise determination of the K-T boundary for the first time in the Carpathians and in turbiditic flysch sediments in general was possible due to the successive occurrence of the Early Paleocene planktonic taxa of the P1 Zone above the latest MaastrichtianAbathomphalus mayaroensisZone with theRacemiguembelina fructicosaSubzone. The trends in composition of the latest Maastrichtian foraminiferal assemblages are similar to the Gaj section from the adjacent thrust sheet, probably due to the influence of the same paleoenvironmental factors.


2012 ◽  
Vol 56 (Suppl_1) ◽  
pp. s41-s44
Author(s):  
Emiko Kinoshita-Kikuta ◽  
Eiji Kinoshita ◽  
Tohru Koike

2019 ◽  
Vol 66 (1) ◽  
pp. 1-9 ◽  
Author(s):  
Kazuhiro Chiku ◽  
Mami Wada ◽  
Haruka Atsuji ◽  
Arisa Hosonuma ◽  
Mitsuru Yoshida ◽  
...  

2020 ◽  
Vol 13 (12) ◽  
pp. 5104-5116
Author(s):  
Keisuke Obata ◽  
Roel van de Krol ◽  
Michael Schwarze ◽  
Reinhard Schomäcker ◽  
Fatwa F. Abdi

Buoyancy-driven natural convection stabilizes the pH and reduces overpotentials during water splitting, both in near-neutral pH unbuffered and buffered solutions.


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