about
Devonian rise in atmospheric oxygen correlated to the radiations of terrestrial plants and large predatory fishBiogenesis of reactive sulfur species for signaling by hydrogen sulfide oxidation pathwaysEdiacaran Marine Redox Heterogeneity and Early Animal EcosystemsUncertainty in the Timing of Origin of Animals and the Limits of Precision in Molecular TimescalesRise to modern levels of ocean oxygenation coincided with the Cambrian radiation of animalsThe role of microbes in the formation of modern and ancient phosphatic mineral depositsBiochemistry and evolution of anaerobic energy metabolism in eukaryotesTowards a quantitative understanding of the late Neoproterozoic carbon cycleRedox biochemistry of hydrogen sulfide.An early Ediacaran assemblage of macroscopic and morphologically differentiated eukaryotes.Protist diversity in suboxic and sulfidic waters of the Black Sea.Ocean oxygenation in the wake of the Marinoan glaciation.Uncovering the spatial heterogeneity of Ediacaran carbon cycling.A geochemical study of the Ediacaran discoidal fossil Aspidella preserved in limestones: Implications for its taphonomy and paleoecology.Controls on the evolution of Ediacaran metazoan ecosystems: A redox perspective.Integrated carbon, sulfur, and nitrogen isotope chemostratigraphy of the Ediacaran Lantian Formation in South China: Spatial gradient, ocean redox oscillation, and fossil distribution.Oceanic oxygenation events in the anoxic Ediacaran ocean.The onset of widespread marine red beds and the evolution of ferruginous oceans.A carbon isotope challenge to the snowball Earth.Widespread iron-rich conditions in the mid-Proterozoic ocean.A unifying model for Neoproterozoic-Palaeozoic exceptional fossil preservation through pyritization and carbonaceous compression.Environmental context for the terminal Ediacaran biomineralization of animals.Filamentous sulfur bacteria preserved in modern and ancient phosphatic sediments: implications for the role of oxygen and bacteria in phosphogenesis.Evolutionary biology: When life got big.Geochemistry. Ocean chemistry and early animals.Sulphide Resistance in the Cyanobacterium Microcystis aeruginosa: a Comparative Study of Morphology and Photosynthetic Performance Between the Sulphide-Resistant Mutant and the Wild-Type Strain.Extensive marine anoxia during the terminal Ediacaran Period.Earth's youngest banded iron formation implies ferruginous conditions in the Early Cambrian ocean.A Cloudina-like fossil with evidence of asexual reproduction from the lowest Cambrian, South ChinaThe Weng'an biota and the Ediacaran radiation of multicellular eukaryotesTransient marine euxinia at the end of the terminal Cryogenian glaciationPalaeoceanographic controls on spatial redox distribution over the Yangtze Platform during the Ediacaran-Cambrian transitionCo-evolution of eukaryotes and ocean oxygenation in the Neoproterozoic eraIron-dependent nitrogen cycling in a ferruginous lake and the nutrient status of Proterozoic oceansAbiotic Pyrite Formation Produces a Large Fe Isotope Fractionation
P2860
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P2860
description
2010 nî lūn-bûn
@nan
2010年の論文
@ja
2010年学术文章
@wuu
2010年学术文章
@zh-cn
2010年学术文章
@zh-hans
2010年学术文章
@zh-my
2010年学术文章
@zh-sg
2010年學術文章
@yue
2010年學術文章
@zh
2010年學術文章
@zh-hant
name
A stratified redox model for the Ediacaran ocean.
@en
A stratified redox model for the Ediacaran ocean.
@nl
type
label
A stratified redox model for the Ediacaran ocean.
@en
A stratified redox model for the Ediacaran ocean.
@nl
prefLabel
A stratified redox model for the Ediacaran ocean.
@en
A stratified redox model for the Ediacaran ocean.
@nl
P2093
P2860
P356
P1433
P1476
A stratified redox model for the Ediacaran ocean.
@en
P2093
Gordon D Love
Timothy W Lyons
Xuelei Chu
P2860
P356
10.1126/SCIENCE.1182369
P407
P577
2010-02-11T00:00:00Z