| scholarly article | Q13442814 |
| P819 | ADS bibcode | 2021ESRv..21803683H |
| P356 | DOI | 10.1016/J.EARSCIREV.2021.103683 |
| P50 | author | Sebastian Viehmann | Q59767407 |
| P2093 | author name string | Simon V. Hohl | |
| P2860 | cites work | Archean Molecular Fossils and the Early Rise of Eukaryotes | Q22065553 |
| Controls on development and diversity of Early Archean stromatolites | Q22066279 | ||
| Structure and metal exchange in the cadmium carbonic anhydrase of marine diatoms | Q27650001 | ||
| Rapid emergence of life shown by discovery of 3,700-million-year-old microbial structures | Q28005492 | ||
| The Archean sulfur cycle and the early history of atmospheric oxygen | Q28143052 | ||
| Stromatolite reef from the Early Archaean era of Australia | Q28244909 | ||
| Fluctuations in Precambrian atmospheric oxygenation recorded by chromium isotopes | Q28258008 | ||
| Mass spectrometry and natural variations of iron isotopes | Q28296057 | ||
| Neodymium in the oceans: a global database, a regional comparison and implications for palaeoceanographic research | Q28597236 | ||
| Sulfur isotopes of organic matter preserved in 3.45-billion-year-old stromatolites reveal microbial metabolism | Q28727466 | ||
| A biomarker based on the stable isotopes of nickel | Q28752299 | ||
| Importance of Cadmium Sulfides for Biogeochemical Cycling of Cd and Its Isotopes in Oxygen Deficient Zones—A Case Study of the Angola Basin | Q112163227 | ||
| Influence of exhumation on the structural evolution of transpressional plate boundaries: An example from the Southern Alps, New Zealand | Q112163228 | ||
| The rare earth element signal in Archaean microbial carbonate: information on ocean redox and biogenicity | Q112163229 | ||
| The Nd and Sr isotopic evolution of Proterozoic seawater | Q112163230 | ||
| Geochemistry of Ediacaran cap dolostones across the Yangtze Platform, South China: implications for diagenetic modification and seawater chemistry in the aftermath of the Marinoan glaciation | Q112163231 | ||
| Uranium Isotope Fractionation | Q112163233 | ||
| The molybdenum isotopic composition of the modern ocean | Q112163235 | ||
| Two Archean Sm-Nd ages of 3.2 and 2.5 Ga for the Marble Bar Chert, Warrawoona Group, Pilbara Block, Western Australia | Q112163236 | ||
| Trace Metal and Cd Isotope Systematics of the Basal Datangpo Formation, Yangtze Platform (South China) Indicate Restrained (Bio)Geochemical Metal Cycling in Cryogenian Seawater | Q112163237 | ||
| Hf-Nd Isotopes in Archean Marine Chemical Sediments: Implications for the Geodynamical History of Early Earth and Its Impact on Earliest Marine Habitats | Q112163238 | ||
| Effect of Zn, Mn, and Fe on Cd accumulation in phytoplankton: Implications for oceanic Cd cycling | Q112163240 | ||
| A normalised seawater strontium isotope curve: possible implications for Neoproterozoic-Cambrian weathering rates and the further oxygenation of the Earth | Q112163242 | ||
| Spatially-resolved isotopic study of carbon trapped in ∼3.43 Ga Strelley Pool Formation stromatolites | Q73894905 | ||
| Microbial U Isotope Fractionation Depends on the U(VI) Reduction Rate | Q92468132 | ||
| Low-temperature isotopic fractionation of uranium | Q94589235 | ||
| Uranium concentrations and 238U/235U isotope ratios in modern carbonates from the Bahamas: Assessing a novel paleoredox proxy | Q96965425 | ||
| Natural fractionation of 238U/235U | Q96965430 | ||
| Uranium isotopic compositions of the crust and ocean: Age corrections, U budget and global extent of modern anoxia | Q96965432 | ||
| Biological Control of Chromium Redox and Stable Isotope Composition in the Surface Ocean | Q97882339 | ||
| Uranium isotope compositions of biogenic carbonates – Implications for U uptake in shells and the application of the paleo-ocean oxygenation proxy | Q104535552 | ||
| Environmental significance of microbialites in reef environments during the last deglaciation | Q105669751 | ||
| Reduction of hexavalent chromium by ferrous iron: A process of chromium isotope fractionation and its relevance to natural environments | Q105727380 | ||
| A trace element and Pb isotopic investigation into the provenance and deposition of stromatolitic carbonates, ironstones and associated shales of the ∼3.0 Ga Pongola Supergroup, Kaapvaal Craton | Q106097153 | ||
| Geochemistry of late Archaean stromatolites from Zimbabwe: evidence for microbial life in restricted epicontinental seas | Q106097185 | ||
| Pb, O, and C isotopes in silicified Mooidraai dolomite (Transvaal Supergroup, South Africa): implications for the composition of Paleoproterozoic seawater and ‘dating’ the increase of oxygen in the Precambrian atmosphere | Q108823398 | ||
| Chromium biogeochemistry and stable isotope distribution in the Southern Ocean | Q109538507 | ||
| The onset of oxidative weathering traced by uranium isotopes | Q109773237 | ||
| Isotopic evidence for oxygenated Mesoarchaean shallow oceans | Q109773251 | ||
| Source composition, fractional crystallization and magma mixing processes in the 3.48–3.43Ga Tsawela tonalite suite (Ancient Gneiss Complex, Swaziland) – Implications for Palaeoarchaean geodynamics | Q109773262 | ||
| Keratolite–stromatolite consortia mimic domical and branched columnar stromatolites | Q110186583 | ||
| Atmosphere oxygen cycling through the Proterozoic and Phanerozoic | Q112163137 | ||
| Uranium in open ocean: concentration and isotopic composition | Q112163138 | ||
| Rare earth and trace elements of microbialites in Upper Jurassic coral- and sponge-microbialite reefs | Q112163139 | ||
| Molybdenum isotopic composition of modern and Carboniferous carbonates | Q112163140 | ||
| Molybdenum isotope fractionation in pelagic euxinia: Evidence from the modern Black and Baltic Seas | Q112163141 | ||
| Contrasting molybdenum cycling and isotopic properties in euxinic versus non-euxinic sediments and sedimentary rocks: Refining the paleoproxies | Q112163142 | ||
| High enrichment of molybdenum in hypersaline microbial mats of Guerrero Negro, Baja California Sur, Mexico | Q112163143 | ||
| A new analytical approach to determining Mo and Re speciation in sulfidic waters | Q112163144 | ||
| Chromium isotope stratigraphy of Ediacaran cap dolostones, Doushantuo Formation, South China | Q112163145 | ||
| Syndepositional diagenetic control of molybdenum isotope variations in carbonate sediments from the Bahamas | Q112163146 | ||
| Decoupled Hf and Nd isotopes in suspended particles and in the dissolved load of Late Archean seawater | Q112163147 | ||
| Cadmium isotopic evidence for the evolution of marine primary productivity and the biological extinction event during the Permian-Triassic crisis from the Meishan section, South China | Q112163149 | ||
| Sulfidization of 3.48 billion-year-old stromatolites of the Dresser Formation, Pilbara Craton: Constraints from in-situ sulfur isotope analysis of pyrite | Q112163151 | ||
| Biogeochemical cycle of chromium isotopes at the modern Earth's surface and its applications as a paleo-environment proxy | Q112163152 | ||
| A global survey of radiogenic strontium isotopes in river sediments | Q112163153 | ||
| Chromium isotope heterogeneity on a modern carbonate platform | Q112163155 | ||
| Signatures of early microbial life from the Archean (4 to 2.5 Ga) eon | Q112163156 | ||
| Global marine redox evolution from the late Neoproterozoic to the early Paleozoic constrained by the integration of Mo and U isotope records | Q112163157 | ||
| Anomalous fractionation of sulfur isotopes during heterogeneous reactions | Q112163159 | ||
| A case for late-Archaean continental emergence from thermal evolution models and hypsometry | Q112163160 | ||
| Mass-dependent cadmium isotopic variations in nature with emphasis on the marine environment | Q112163161 | ||
| Magnetic susceptibility as a biosignature in stromatolites | Q112163162 | ||
| Isotopic evidence for complex biogeochemical cycling of Cd in the eastern tropical South Pacific | Q112163165 | ||
| Post-depositional REE mobility in a Paleoarchean banded iron formation revealed by La-Ce geochronology: A cautionary tale for signals of ancient oxygenation | Q112163166 | ||
| Iron isotope fractionation by Fe(II)-oxidizing photoautotrophic bacteria 1 1Associate editor: D. E. Canfield | Q112163167 | ||
| Inter-mineral Fe isotope variations in mantle-derived rocks and implications for the Fe geochemical cycle | Q112163168 | ||
| Iron isotope fractionation during microbially stimulated Fe(II) oxidation and Fe(III) precipitation | Q112163169 | ||
| Cadmium isotopic composition in the ocean | Q112163170 | ||
| Role of nuclear volume in driving equilibrium stable isotope fractionation of mercury, thallium, and other very heavy elements | Q112163172 | ||
| Determination of the decay-constant of 87Rb by laboratory accumulation of 87Sr | Q112163173 | ||
| Reduced isotope fractionation by denitrification under conditions relevant to the ocean | Q112163174 | ||
| Acidophilic sulfur disproportionation | Q112163176 | ||
| The oceanic mass balance of copper and zinc isotopes, investigated by analysis of their inputs, and outputs to ferromanganese oxide sediments | Q112163177 | ||
| Multiproxy constraints on alteration and primary compositions of Ediacaran deep-water carbonate rocks, Yangtze Platform, South China | Q112163179 | ||
| The effect of redox conditions and bioirrigation on nitrogen isotope fractionation in marine sediments | Q112163180 | ||
| Kinetic stable Cr isotopic fractionation between aqueous Cr(III)-Cl-H2O complexes at 25 °C: Implications for Cr(III) mobility and isotopic variations in modern and ancient natural systems | Q112163181 | ||
| Chromium isotope fractionation in ferruginous sediments | Q112163182 | ||
| Modern rather than Mesoarchaean oxidative weathering responsible for the heavy stable Cr isotopic signatures of the 2.95 Ga old Ijzermijn iron formation (South Africa) | Q112163192 | ||
| Cd isotopes trace periodic (bio)geochemical metal cycling at the verge of the Cambrian animal evolution | Q112163194 | ||
| Correlated molybdenum and uranium isotope signatures in modern anoxic sediments: Implications for their use as paleo-redox proxy | Q112163195 | ||
| Uranium isotopes in marine carbonates as a global ocean paleoredox proxy: A critical review | Q112163196 | ||
| The uranium isotopic record of shales and carbonates through geologic time | Q112163197 | ||
| Metal cycling in Mesoproterozoic microbial habitats: Insights from trace elements and stable Cd isotopes in stromatolites | Q112163199 | ||
| Sulfur and carbon isotope analyses of 2.7Ga stromatolites, cherts and sandstones in the Jeerinah Formation, Western Australia | Q112163200 | ||
| Distribution of high field strength elements (Y, Zr, REE, Hf, Ta, Th, U) in adjacent magnetite and chert bands and in reference standards FeR-3 and FeR-4 from the Temagami iron-formation, Canada, and the redox level of the Neoarchean ocean | Q112163201 | ||
| Molybdenum isotopes in late Archean carbonate rocks: Implications for early Earth oxygenation | Q112163204 | ||
| Micro-scale quadruple sulfur isotope analysis of pyrite from the ∼3480Ma Dresser Formation: New insights into sulfur cycling on the early Earth | Q112163205 | ||
| Geochemical stratigraphy, sedimentology, and Mo isotope systematics of the ca. 2.58–2.50 Ga-old Transvaal Supergroup carbonate platform, South Africa | Q112163206 | ||
| Geochemistry of the Krivoy Rog Banded Iron Formation, Ukraine, and the impact of peak episodes of increased global magmatic activity on the trace element composition of Precambrian seawater | Q112163207 | ||
| Geochemical characterisation of Neoproterozoic marine habitats: Evidence from trace elements and Nd isotopes in the Urucum iron and manganese formations, Brazil | Q112163208 | ||
| Trace element and Nd isotope composition of shallow seawater prior to the Great Oxidation Event: Evidence from stromatolitic bioherms in the Paleoproterozoic Rooinekke and Nelani Formations, South Africa | Q112163210 | ||
| Carbonates and cherts as archives of seawater chemistry and habitability on a carbonate platform 3.35 Ga ago: Insights from Sm/Nd dating and trace element analysis from the Strelley Pool Formation, Western Australia | Q112163211 | ||
| Lithifying microbial mats in Lagoa Vermelha, Brazil: Modern Precambrian relics? | Q112163213 | ||
| Evidence for microbes in early Neoproterozoic stromatolites | Q112163214 | ||
| Applications of accurate, high-precision Pb isotope ratio measurement by multi-collector ICP-MS | Q112163215 | ||
| Two terrestrial lead isotope paradoxes, forward transport modelling, core formation and the history of the continental crust | Q112163217 | ||
| Pb, Sr and Nd isotope systematics of uranium mineralised stromatolitic dolomites from the proterozoic Cuddapah Supergroup, south India: constraints on age and provenance | Q112163219 | ||
| A new approach to the Nd residence time in the ocean: the role of atmospheric inputs | Q112163220 | ||
| The geochemistry of late Archaean microbial carbonate: implications for ocean chemistry and continental erosion history | Q112163221 | ||
| REE geochemistry and isotopic data of Archean silicic volcanics and granitoids from the Pilbara Block, Western Australia: implications for the early crustal evolution | Q112163222 | ||
| Carbon isotopes as biogeochemical recorders of life over 3.8 Ga of Earth history: evolution of a concept | Q112163223 | ||
| Recent discoveries of Proterozoic microfossils in south-central Brazil | Q112163225 | ||
| Iron Isotope Fractionation during Fe(II) Oxidation Mediated by the Oxygen-Producing Marine Cyanobacterium Synechococcus PCC 7002. | Q33635066 | ||
| Atmospheric influence of Earth's earliest sulfur cycle | Q33912369 | ||
| Evidence for decoupling of atmospheric CO2 and global climate during the Phanerozoic eon. | Q33929160 | ||
| Isotopic evidence for microbial sulphate reduction in the early Archaean era. | Q33937305 | ||
| Formation of the 'Great Unconformity' as a trigger for the Cambrian explosion | Q34269532 | ||
| Atmospheric oxygenation three billion years ago. | Q34373369 | ||
| The rise of oxygen in Earth's early ocean and atmosphere | Q34405457 | ||
| Earth history. Low mid-Proterozoic atmospheric oxygen levels and the delayed rise of animals | Q34445685 | ||
| The biogeochemical cycles of trace metals in the oceans. | Q35124331 | ||
| Oxidative elemental cycling under the low O2 Eoarchean atmosphere. | Q36569728 | ||
| Nonspecific uptake and homeostasis drive the oceanic cadmium cycle | Q36616879 | ||
| Microbial nitrogen cycling processes in oxygen minimum zones. | Q37844115 | ||
| Elements of Eoarchean life trapped in mineral inclusions. | Q38368991 | ||
| Stable iron isotopes and microbial mediation in red pigmentation of the Rosso Ammonitico (mid-late Jurassic, Verona area, Italy). | Q38499158 | ||
| Behavior of hexavalent chromium in a polluted groundwater: redox processes and immobilization in soils | Q43343518 | ||
| Mechanism of Uranium Reduction and Immobilization in Desulfovibrio vulgaris Biofilms | Q46687766 | ||
| Redox-independent chromium isotope fractionation induced by ligand-promoted dissolution | Q46799998 | ||
| Pelagic barite precipitation at micromolar ambient sulfate | Q47154081 | ||
| Uranium isotope evidence for two episodes of deoxygenation during Oceanic Anoxic Event 2. | Q52366590 | ||
| A new microfossil assemblage from the Archaean of Western Australia | Q56431896 | ||
| Stromatolites 3,400–3,500 Myr old from the North Pole area, Western Australia | Q56431897 | ||
| Oxygen and sulfur isotope fractionation during anaerobic bacterial disproportionation of elemental sulfur | Q56608833 | ||
| Isotope fractionation and sulfur metabolism by pure and enrichment cultures of elemental sulfur-disproportionating bacteria | Q56608841 | ||
| Biological Fe oxidation controlled deposition of banded iron formation in the ca. 3770Ma Isua Supracrustal Belt (West Greenland) | Q56680895 | ||
| 87Sr/86Sr, δ13C and δ18O evolution of Phanerozoic seawater | Q56764287 | ||
| Coupled Fe and S isotope evidence for Archean microbial Fe(III) and sulfate reduction | Q56853123 | ||
| The nature of O18/O16 and C13/C12 secular trends in sedimentary carbonate rocks | Q56959116 | ||
| Biogeochemical cycling of cadmium isotopes in the Southern Ocean along the Zero Meridian | Q57399131 | ||
| Modulation of the Southern Ocean cadmium isotope signature by ocean circulation and primary productivity | Q57399160 | ||
| The iron isotope composition of microbial carbonate | Q57695774 | ||
| Molybdenum isotope records as a potential new proxy for paleoceanography | Q57695850 | ||
| Isotopic fractionation of cadmium into calcite | Q57813002 | ||
| PbPb and UPb geochronology of carbonate rocks: an assessment | Q57883417 | ||
| Direct dating of stromatolitic carbonates from the Schmidtsdrif Formation (Transvaal Dolomite), South Africa, with implications on the age of the Ventersdorp Supergroup | Q57883437 | ||
| Absolute ages of multiple generations of brittle structures by U-Pb dating of calcite | Q57967782 | ||
| Global-ocean redox variation during the middle-late Permian through Early Triassic based on uranium isotope and Th/U trends of marine carbonates | Q57978424 | ||
| Integrated geochemical-petrographic insights from component-selective δ238U of Cryogenian marine carbonates | Q58041330 | ||
| Nitrogen isotopes in bulk marine sediment: linking seafloor observations with subseafloor records | Q58054924 | ||
| Decoupled Hf-Nd isotopes in Neoarchean seawater reveal weathering of emerged continents | Q58079831 | ||
| Uranium in iron formations and the rise of atmospheric oxygen | Q58391389 | ||
| Iron-oxidizing microbial ecosystems thrived in late Paleoproterozoic redox-stratified oceans | Q58391458 | ||
| Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history | Q58417926 | ||
| Chemical and textural overprinting of ancient stromatolites: Timing, processes, and implications for their use as paleoenvironmental proxies | Q58417935 | ||
| Proposed early signs of life not set in stone | Q58570687 | ||
| Processes of carbonate precipitation in modern microbial mats | Q58866997 | ||
| Reassessing evidence of life in 3,700-million-year-old rocks of Greenland | Q59056069 | ||
| First direct radiometric dating of Archaean stromatolitic limestone | Q59069453 | ||
| Hydrothermal scavenging of rare-earth elements in the ocean | Q59072178 | ||
| On the marine geochemistry of cadmium | Q59074124 | ||
| Cadmium and cobalt substitution for zinc in a marine diatom | Q59074129 | ||
| Microbiological evidence for Fe(III) reductionon early Earth | Q59081082 | ||
| Stromatolites 3,400-Myr old from the Archean of Western Australia | Q59093317 | ||
| Pelagic molybdenum concentration anomalies and the impact of sediment resuspension on the molybdenum budget in two tidal systems of the North Sea | Q59308894 | ||
| Non-conservative behaviour of molybdenum in coastal waters: Coupling geochemical, biological, and sedimentological processes | Q59308966 | ||
| Fractionation of Fe isotopes during Fe(II) oxidation by a marine photoferrotroph is controlled by the formation of organic Fe-complexes and colloidal Fe fractions | Q59346501 | ||
| Extreme 13C-depletions and organic sulfur content argue for S-fueled anaerobic methane oxidation in 2.72 Ga old stromatolites | Q59753622 | ||
| Combined bulk-rock Hf- and Nd-isotope compositions of Mesoarchaean metavolcanic rocks from the Ivisaartoq Supracrustal Belt, SW Greenland: Deviations from the mantle array caused by crustal recycling | Q59764800 | ||
| Sm-Nd and Lu-Hf isotope and trace-element systematics of Mesoarchaean amphibolites, inner Ameralik fjord, southern West Greenland | Q59764803 | ||
| Uranium isotopic fractionation factors during U(VI) reduction by bacterial isolates | Q59786984 | ||
| Ferromanganese crusts as archives of deep water Cd isotope compositions | Q59798187 | ||
| Grain-scale iron isotopic distribution of pyrite from Precambrian shallow marine carbonate revealed by a femtosecond laser ablation multicollector ICP-MS technique: Possible proxy for the redox state of ancient seawater | Q59798357 | ||
| Pb- and Nd-isotope systematics of stromatolitic limestones from the 2.7 Ga Ngezi Group of the Belingwe Greenstone Belt: constraints on timing of deposition and provenance | Q59800691 | ||
| An Image Mapping Approach to U-Pb LA-ICP-MS Carbonate Dating, and Applications to Direct Dating of Carbonate Sedimentation | Q59810030 | ||
| Iron isotope fractionation during pyrite formation in a sulfidic Precambrian ocean analogue | Q59849720 | ||
| Environmental control on microbial diversification and methane production in the Mesoarchean | Q60116931 | ||
| Nitrogen isotope evidence for alkaline lakes on late Archean continents | Q60116955 | ||
| Texture-specific isotopic compositions in 3.4Gyr old organic matter support selective preservation in cell-like structures | Q60123401 | ||
| Volcanic gases, black smokers, and the great oxidation event | Q60843738 | ||
| Isotopic Nd compositions and concentrations of the lithogenic inputs into the ocean: A compilation, with an emphasis on the margins | Q61737395 | ||
| Modeling the neodymium isotopic composition with a global ocean circulation model | Q61737396 | ||
| Calcium and strontium isotope systematics in the lagoon-estuarine environments of South Australia: Implications for water source mixing, carbonate fluxes and fish migration | Q62564656 | ||
| Isotope fractionation during oxidation of tetravalent uranium by dissolved oxygen | Q63389275 | ||
| The isotopic composition of authigenic chromium in anoxic marine sediments: A case study from the Cariaco Basin | Q63389280 | ||
| Global importance of oxic molybdenum sinks prior to 2.6 Ga revealed by the Mo isotope composition of Precambrian carbonates | Q63464352 | ||
| THE STABLE ISOTOPE GEOCHEMISTRY OF MOLYBDENUM | Q63494855 | ||
| Trace element and stable (C, O) and radiogenic (Sr) isotope geochemistry of stromatolitic carbonate rocks of the Mesoarchaean Pongola Supergroup: Implications for seawater composition | Q63645667 | ||
| Uranium isotope fractionation by abiotic reductive precipitation. | Q64980118 | ||
| Multiple sulfur isotopes and the evolution of the atmosphere | Q70511340 | ||
| Rare earth element systematics of the chemically precipitated component in early precambrian iron formations and the evolution of the terrestrial atmosphere-hydrosphere-lithosphere system | Q70941462 | ||
| The evolution of Earth's biogeochemical nitrogen cycle | Q70941471 | ||
| Evolution of Precambrian life in the Brazilian geological record | Q70941777 | ||
| Ca and Sr isotope constraints on the formation of the Marinoan cap dolostones | Q73306239 | ||
| Diagenetic effects on uranium isotope fractionation in carbonate sediments from the Bahamas | Q73306335 | ||
| Role of upper-most crustal composition in the evolution of the Precambrian ocean–atmosphere system | Q73892360 | ||
| Re-assessing the surface cycling of molybdenum and rhenium | Q73894804 | ||
| P2507 | corrigendum / erratum | Corrigendum to “Stromatolites as geochemical archives to reconstruct microbial habitats through deep time: Potential and pitfalls of novel radiogenic and stable isotope systems” [Earth Science Reviews 218 (2021) 103683] | Q112163081 |
| P921 | main subject | stromatolite | Q176739 |
| P304 | page(s) | 103683 | |
| P577 | publication date | 2021-07-01 | |
| P1433 | published in | Earth-Science Reviews | Q15716529 |
| P1476 | title | Stromatolites as geochemical archives to reconstruct microbial habitats through deep time: Potential and pitfalls of novel radiogenic and stable isotope systems | |
| P478 | volume | 218 |
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