Romain Guilbaud
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View article: Insights into the acquisition of kinetic iron isotope signatures of pyrite precipitated through the polysulfide pathway
Insights into the acquisition of kinetic iron isotope signatures of pyrite precipitated through the polysulfide pathway Open
International audience
View article: HERFD-XAS evidence for an octahedrally coordinated CoSn-polysulfide precursor as a probe for the mechanism of pyrite formation
HERFD-XAS evidence for an octahedrally coordinated CoSn-polysulfide precursor as a probe for the mechanism of pyrite formation Open
View article: Archaean oxygen oases driven by pulses of enhanced phosphorus recycling in the ocean
Archaean oxygen oases driven by pulses of enhanced phosphorus recycling in the ocean Open
Earth’s first rise in atmospheric oxygen between about 2.43 billion and 2.1 billion years ago fundamentally transformed the atmosphere and oceans, setting the foundation for the evolution of complex life. However, geochemical evidence reve…
View article: Mackinawite partial oxidation to green rust produces a large, abiotic uranium isotope fractionation
Mackinawite partial oxidation to green rust produces a large, abiotic uranium isotope fractionation Open
View article:  Life-Earth coevolution: the role of phosphorus in Archean oxygen accumulation 
 Life-Earth coevolution: the role of phosphorus in Archean oxygen accumulation  Open
Investigating the presence of oxygen on planets within our solar system and beyond is crucial for understanding the potential for life beyond Earth. Oxygen is a key ingredient for life as we know it and serves as a key indicator of habitab…
View article: Sustained increases in atmospheric oxygen and marine productivity in the Neoproterozoic and Palaeozoic eras
Sustained increases in atmospheric oxygen and marine productivity in the Neoproterozoic and Palaeozoic eras Open
View article: Proterozoic evolution of the phosphorus cycle: Was it high or was it low?
Proterozoic evolution of the phosphorus cycle: Was it high or was it low? Open
View article: Iron isotope fractionation during sulfide-promoted reductive dissolution of iron (oxyhydr)oxide minerals
Iron isotope fractionation during sulfide-promoted reductive dissolution of iron (oxyhydr)oxide minerals Open
International audience
View article: Multiple sustained increases in atmospheric oxygen and marine productivity through the Neoproterozoic and Paleozoic Eras
Multiple sustained increases in atmospheric oxygen and marine productivity through the Neoproterozoic and Paleozoic Eras Open
A geologically rapid Neoproterozoic oxygenation event is commonly linked to the appearance of marine animal groups in the fossil record. However, there is still debate about what evidence from the sedimentary geochemical record – if any – …
View article: Phosphorus controls on the formation of vivianite versus green rust under anoxic conditions
Phosphorus controls on the formation of vivianite versus green rust under anoxic conditions Open
View article: Archean carbonates and oxygen-rich oasis: implications for ancient life on Mars
Archean carbonates and oxygen-rich oasis: implications for ancient life on Mars Open
View article: Burial of Fe bearing precursors to ‘chemical sediments’ in the deep past
Burial of Fe bearing precursors to ‘chemical sediments’ in the deep past Open
View article: The Sedimentary Geochemistry and Paleoenvironments Project
The Sedimentary Geochemistry and Paleoenvironments Project Open
We thank the donors of The American
\nChemical Society Petroleum Research Fund for partial support of
\nSGP website development (61017-ND2). EAS is funded by National
\nScience Foundation grant (NSF) EAR-1922966
View article: Curation and Analysis of Global Sedimentary Geochemical Data to Inform Earth History
Curation and Analysis of Global Sedimentary Geochemical Data to Inform Earth History Open
Large datasets increasingly provide critical insights into crustal and surface processes on Earth. These data come in the form of published and contributed observations, which often include associated metadata. Even in the best-case scenar…
View article: Testing links between the pre-GOE iron cycle and oxygenation using triple iron isotopes
Testing links between the pre-GOE iron cycle and oxygenation using triple iron isotopes Open
View article: Triple iron isotope constraints on the role of ocean iron sinks in early atmospheric oxygenation
Triple iron isotope constraints on the role of ocean iron sinks in early atmospheric oxygenation Open
The iron did it What factors controlled the accumulation of atmospheric oxygen gas (O 2 ) early in the history of Earth? Heard et al. used high-precision iron isotopic measurements of Archean-Paleoproterozoic sediments, with ages between 3…
View article: Phosphorus-limited conditions in the early Neoproterozoic ocean maintained low levels of atmospheric oxygen
Phosphorus-limited conditions in the early Neoproterozoic ocean maintained low levels of atmospheric oxygen Open
View article: The Ediacaran–Cambrian transition: the emerging record from Small Carbonaceous Fossils (SCFs)
The Ediacaran–Cambrian transition: the emerging record from Small Carbonaceous Fossils (SCFs) Open
The Ediacaran–Cambrian transition: the emerging record from Small Carbonaceous Fossils (SCFs)
View article: Oxygen minimum zones in the early Cambrian ocean
Oxygen minimum zones in the early Cambrian ocean Open
The relationship between the evolution of early animal 26 communities and oceanic oxygen levels remains unclear. In particular, uncertainty persists in reconstructions of redox conditions during the pivotal early Cambrian (541-510 million …
View article: A palaeoecological model for the late Mesoproterozoic – early Neoproterozoic Atar/El Mreïti Group, Taoudeni Basin, Mauritania, northwestern Africa
A palaeoecological model for the late Mesoproterozoic – early Neoproterozoic Atar/El Mreïti Group, Taoudeni Basin, Mauritania, northwestern Africa Open
View article: A cryptic record of Burgess Shale‐type diversity from the early Cambrian of Baltica
A cryptic record of Burgess Shale‐type diversity from the early Cambrian of Baltica Open
Exceptionally preserved ‘Burgess Shale‐type’ fossil assemblages from the Cambrian of Laurentia, South China and Australia record a diverse array of non‐biomineralizing organisms. During this time, the palaeocontinent Baltica was geographic…
View article: Low-oxygen waters limited habitable space for early animals
Low-oxygen waters limited habitable space for early animals Open
View article: Towards a palaeoecological model of the Mesoproterozoic Taoudeni Basin, Mauritania, Northwestern Africa: implications for early eukaryote evolution
Towards a palaeoecological model of the Mesoproterozoic Taoudeni Basin, Mauritania, Northwestern Africa: implications for early eukaryote evolution Open
peer reviewed
View article: A global transition to ferruginous conditions in the early Neoproterozoic oceans
A global transition to ferruginous conditions in the early Neoproterozoic oceans Open
View article: (Table S7B) Geochemical analysis of Site 6, Arasab: Shales
(Table S7B) Geochemical analysis of Site 6, Arasab: Shales Open
highly reactive Fe to total Fe, (FeHR/FeT).carbonate-associated Fe, (Fecarb; e.g., ankerite and siderite).ferric(oxyhydr)oxides, (Feox; e.g., goethite and hematite).magnetite Fe, (Femag).Fe sulfide minerals, (Fepy; e.g., makinawite and pyr…
View article: (Table S7A) Geochemical analysis of Site 6, Arasab: Carbonates
(Table S7A) Geochemical analysis of Site 6, Arasab: Carbonates Open
highly reactive Fe to total Fe, (FeHR/FeT).carbonate-associated Fe, (Fecarb; e.g., ankerite and siderite).ferric(oxyhydr)oxides, (Feox; e.g., goethite and hematite).magnetite Fe, (Femag).Fe sulfide minerals, (Fepy; e.g., makinawite and pyr…
View article: Geochemical analysis of nine sections from the Nama Group, Namibia
Geochemical analysis of nine sections from the Nama Group, Namibia Open
The first appearance of skeletal metazoans in the late Ediacaran (~550 million years ago; Ma) has been linked to the widespread development of oxygenated oceanic conditions, but a precise spatial and temporal reconstruction of their evolut…
View article: (Table S4) Geochemical analysis of Site 3, Zebra_River
(Table S4) Geochemical analysis of Site 3, Zebra_River Open
highly reactive Fe to total Fe, (FeHR/FeT).carbonate-associated Fe, (Fecarb; e.g., ankerite and siderite).ferric(oxyhydr)oxides, (Feox; e.g., goethite and hematite).magnetite Fe, (Femag).Fe sulfide minerals, (Fepy; e.g., makinawite and pyr…
View article: (Table S9A) Geochemical analysis of Site 8, Pinnacle Reefs: carbonates
(Table S9A) Geochemical analysis of Site 8, Pinnacle Reefs: carbonates Open
highly reactive Fe to total Fe, (FeHR/FeT).carbonate-associated Fe, (Fecarb; e.g., ankerite and siderite).ferric(oxyhydr)oxides, (Feox; e.g., goethite and hematite).magnetite Fe, (Femag).Fe sulfide minerals, (Fepy; e.g., makinawite and pyr…
View article: (Table S2) Geochemical analysis of Site 1, Zwartmodder, Zaris Basin
(Table S2) Geochemical analysis of Site 1, Zwartmodder, Zaris Basin Open
highly reactive Fe to total Fe, (FeHR/FeT).carbonate-associated Fe, (Fecarb; e.g., ankerite and siderite).ferric(oxyhydr)oxides, (Feox; e.g., goethite and hematite).magnetite Fe, (Femag).Fe sulfide minerals, (Fepy; e.g., makinawite and pyr…