Search Results - "Schad, Manuel"

Microbial anaerobic Fe(II) oxidation – Ecology, mechanisms and environmental implications by Bryce, Casey, Blackwell, Nia, Schmidt, Caroline, Otte, Julia, Huang, Yu‐Ming, Kleindienst, Sara, Tomaszewski, Elizabeth, Schad, Manuel, Warter, Viola, Peng, Chao, Byrne, James M., Kappler, Andreas

“…Summary Iron is the most abundant redox‐active metal in the Earth's crust. The one electron transfer between the two most common redox states, Fe(II) and…”
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Microbial processes during deposition and diagenesis of Banded Iron Formations by Dreher, Carolin L., Schad, Manuel, Robbins, Leslie J., Konhauser, Kurt O., Kappler, Andreas, Joshi, Prachi

“…Banded Iron Formations (BIFs) are marine chemical sediments consisting of alternating iron (Fe) - rich and silica (Si)-rich bands which were deposited…”
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Resolving the fate of trace metals during microbial remineralization of phytoplankton biomass in precursor banded iron formation sediments by Rico, Kathryn I., Schad, Manuel, Picard, Aude, Kappler, Andreas, Konhauser, Kurt O., Mahmoudi, Nagissa

“…Banded Iron Formations (BIFs) have long been considered a sedimentary record of seawater trace metal composition during the Precambrian. However, recent work…”
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Temperature fluctuations in the Archean ocean as trigger for varve-like deposition of iron and silica minerals in banded iron formations by Schad, Manuel, Halama, Maximilian, Bishop, Brendan, Konhauser, Kurt O., Kappler, Andreas

“…Banded iron formations (BIFs) are Fe- and Si-rich chemical sediments that were deposited in the oceans throughout the Archean Eon (4.0–2.5 billion years ago;…”
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Microbial Fe cycling in a simulated Precambrian ocean environment: Implications for secondary mineral (trans)formation and deposition during BIF genesis by Schad, Manuel, Byrne, James M., ThomasArrigo, Laurel K., Kretzschmar, Ruben, Konhauser, Kurt O., Kappler, Andreas

“…Banded Iron Formations (BIFs) are ancient marine chemical sediments that contain various Fe-bearing minerals such as hematite (Fe2O3), magnetite (Fe3O4),…”
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How did the evolution of oxygenic photosynthesis influence the temporal and spatial development of the microbial iron cycle on ancient Earth? by Schad, Manuel, Konhauser, Kurt O., Sánchez-Baracaldo, Patricia, Kappler, Andreas, Bryce, Casey

“…Iron is the most abundant redox active metal on Earth and thus provides one of the most important records of the redox state of Earth's ancient atmosphere,…”
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Inhibition of phototrophic iron oxidation by nitric oxide in ferruginous environments by Nikeleit, Verena, Mellage, Adrian, Bianchini, Giorgio, Sauter, Lea, Buessecker, Steffen, Gotterbarm, Stefanie, Schad, Manuel, Konhauser, Kurt, Zerkle, Aubrey L., Sánchez-Baracaldo, Patricia, Kappler, Andreas, Bryce, Casey

“…Anoxygenic phototrophic Fe(II) oxidizers (photoferrotrophs) are thought to have thrived in Earth’s ancient ferruginous oceans and played a primary role in the…”
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Phosphate remobilization from banded iron formations during metamorphic mineral transformations by Schad, Manuel, Halama, Maximilian, Jakus, Natalia, Robbins, Leslie, Warchola, Tyler, Tejada, Julian, Kirchhof, Rainer, Lalonde, Stefan, Swanner, Elizabeth, Planavsky, Noah, Thorwarth, Harald, Mansor, Muammar, Konhauser, Kurt, Kappler, Andreas

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Phosphate remobilization from banded iron formations during metamorphic mineral transformations by Schad, Manuel, Halama, Maximilian, Jakus, Natalia, Robbins, Leslie J., Warchola, Tyler J., Tejada, Julian, Kirchhof, Rainer, Lalonde, Stefan V., Swanner, Elizabeth D., Planavsky, Noah J., Thorwarth, Harald, Mansor, Muammar, Konhauser, Kurt O., Kappler, Andreas

“…Ratios of phosphorous (P) to iron (Fe) in Precambrian banded iron formations (BIFs) have previously been used to estimate dissolved seawater phosphate…”
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