Ferruginous conditions dominated later neoproterozoic deep-water chemistry.
about
Anaerobic animals from an ancient, anoxic ecological nicheDevonian rise in atmospheric oxygen correlated to the radiations of terrestrial plants and large predatory fishAnoxygenic photosynthesis modulated Proterozoic oxygen and sustained Earth's middle ageNitrate Storage and Dissimilatory Nitrate Reduction by Eukaryotic MicrobesMolar tooth carbonates and benthic methane fluxes in Proterozoic oceansSelenium isotope evidence for progressive oxidation of the Neoproterozoic biosphereEdiacaran Marine Redox Heterogeneity and Early Animal EcosystemsRise to modern levels of ocean oxygenation coincided with the Cambrian radiation of animalsBacterial influences on animal originsBiochemistry and evolution of anaerobic energy metabolism in eukaryotesMechanism for Burgess Shale-type preservationBiologically induced initiation of Neoproterozoic snowball-Earth eventsTowards a quantitative understanding of the late Neoproterozoic carbon cycleAnimal evolution, bioturbation, and the sulfate concentration of the oceansThe worm turned, and the ocean followedLarge spinose microfossils in Ediacaran rocks as resting stages of early animalsStatistical analysis of iron geochemical data suggests limited late Proterozoic oxygenation.Metabolic evolution and the self-organization of ecosystemsAn early Ediacaran assemblage of macroscopic and morphologically differentiated eukaryotes.Proterozoic oxygen rise linked to shifting balance between seafloor and terrestrial weathering.Nutrient Acquisition and the Metabolic Potential of Photoferrotrophic ChlorobiA contemporary microbially maintained subglacial ferrous "ocean".Proterozoic ocean redox and biogeochemical stasis.The rise of oxygen in Earth's early ocean and atmosphere.Oxygen and animal evolution: did a rise of atmospheric oxygen "trigger" the origin of animals?An early productive ocean unfit for aerobics.Uranium isotopes distinguish two geochemically distinct stages during the later Cambrian SPICE event.Deep-water anoxygenic photosythesis in a ferruginous chemocline.Photoferrotrophy: Remains of an Ancient Photosynthesis in Modern Environments.Chlorophyll biosynthesis gene evolution indicates photosystem gene duplication, not photosystem merger, at the origin of oxygenic photosynthesisControlling the delicate balance of tetrapyrrole biosynthesis.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.Paleoecology and paleoceanography of the Athel silicilyte, Ediacaran-Cambrian boundary, Sultanate of Oman.Oceanic oxygenation events in the anoxic Ediacaran ocean.Origin and early evolution of photosynthetic eukaryotes in freshwater environments: reinterpreting proterozoic paleobiology and biogeochemical processes in light of trait evolution.Genomic Analysis of the Evolution of Phototrophy among Haloalkaliphilic Rhodobacterales.Heterogenous oceanic redox conditions through the Ediacaran-Cambrian boundary limited the metazoan zonation.The onset of widespread marine red beds and the evolution of ferruginous oceans.
P2860
Q21093235-60D79388-4A14-45AD-B1B8-FAF1D4EF6E6DQ24624525-AAD0CF2B-7929-4EB3-BC06-1D2544186538Q24645300-71934772-C19B-4E1C-A8BB-8FEBE3536D9EQ26770679-C3F50063-2B4A-4571-B00E-3F6F67F77813Q28601895-8CA75883-5865-4822-A333-36B4803DCDD9Q28602983-58D2DC02-CB1A-4C87-ADB0-AD66F5EC1AE4Q28607119-6C64942A-5063-41F7-9682-EE458B2045E2Q28647970-94C5AE8D-FA89-43DD-A9CD-3BE3621F3710Q28648297-4D189D54-BC20-44A6-911F-6DB65FDF0699Q28728648-9C43ED16-EDEC-4C65-B6C0-207108148DE9Q28730602-84FDD6F2-1A12-40BD-B2D5-984D40C325FCQ28740330-1CF6E850-0175-4717-9CDA-20CFF2C5AEFFQ28740976-4D5E1E4F-63C5-4564-9EAD-9B8622128251Q28752675-B4E13E2C-6D46-473B-A132-98B01B9DADEAQ28752676-F93140A5-FD60-4BE9-A95E-065A2FF9F4ADQ28754660-BC5DD846-136E-41EB-82FF-876CB0FC253DQ30982109-13ADAA6A-A9FD-4BB3-89D3-399D37B88816Q33569326-8E2ED64A-E3E3-4EB2-BE52-0212CDDC89AEQ33823588-1B7BBB1A-8ED3-432B-9BBC-56F1BC43E998Q33835050-B18E03B2-4FF8-42EC-BBBB-FA668FC5438DQ33875239-AA22E115-8136-4C33-9E36-E39949F464EFQ34017085-098F137C-68E7-4BAC-ABD1-C69BECA1E636Q34334288-A473E3A0-DACB-4B6F-8871-BDFD3A41F491Q34405457-B4617E8E-94D1-40E8-992F-A4059C4657FFQ34439882-C8D46448-330E-4405-BB46-48A765AC7744Q35008947-56AA85D0-489A-4997-8785-F6ACE74E3EA2Q35079855-575E27B8-FF79-493F-889D-57ADCC0BCF67Q35186926-19DFF70C-35F7-4AFE-87B9-BD262F225A2AQ36335197-29B4A729-92C7-46D2-8F91-ABD8360A7869Q36676936-39045DD1-1222-4EBE-AC0A-76D41F72EB5BQ36937107-B2024EF6-F8AD-4A61-80F5-36627116643CQ38780198-EA37ABDA-ABBB-4DB9-BFE2-CC080A137550Q38843106-E43DB7FD-0263-41A0-AEBC-C8451DB01E79Q38848559-16E2322B-C3A1-46EA-9DCD-5587C2E70500Q38848571-800042E1-E598-47F7-B42D-AB2BF6D33678Q39878227-9F173417-B5FE-4B26-BF8C-430AC6483AA2Q39894708-3BC6AE3B-7ADD-4391-813D-6CDEDE9354E7Q40092436-4286FCF7-F4FC-4928-945C-F4C400852799Q41447299-906D15B0-328C-403D-92FB-F9C4F127C0FFQ41564950-E89A65DF-3D88-4136-8CAB-ECA7A1F038E6
P2860
Ferruginous conditions dominated later neoproterozoic deep-water chemistry.
description
2008 nî lūn-bûn
@nan
2008 թուականի Յուլիսին հրատարակուած գիտական յօդուած
@hyw
2008 թվականի հուլիսին հրատարակված գիտական հոդված
@hy
2008年の論文
@ja
2008年論文
@yue
2008年論文
@zh-hant
2008年論文
@zh-hk
2008年論文
@zh-mo
2008年論文
@zh-tw
2008年论文
@wuu
name
Ferruginous conditions dominated later neoproterozoic deep-water chemistry.
@ast
Ferruginous conditions dominated later neoproterozoic deep-water chemistry.
@en
Ferruginous conditions dominated later neoproterozoic deep-water chemistry.
@en-gb
Ferruginous conditions dominated later neoproterozoic deep-water chemistry.
@nl
type
label
Ferruginous conditions dominated later neoproterozoic deep-water chemistry.
@ast
Ferruginous conditions dominated later neoproterozoic deep-water chemistry.
@en
Ferruginous conditions dominated later neoproterozoic deep-water chemistry.
@en-gb
Ferruginous conditions dominated later neoproterozoic deep-water chemistry.
@nl
prefLabel
Ferruginous conditions dominated later neoproterozoic deep-water chemistry.
@ast
Ferruginous conditions dominated later neoproterozoic deep-water chemistry.
@en
Ferruginous conditions dominated later neoproterozoic deep-water chemistry.
@en-gb
Ferruginous conditions dominated later neoproterozoic deep-water chemistry.
@nl
P2093
P50
P356
P1433
P1476
Ferruginous conditions dominated later neoproterozoic deep-water chemistry.
@en
P2093
Gerry Ross
Guy M Narbonne
Harald Strauss
Tatiana Goldberg
P304
P356
10.1126/SCIENCE.1154499
P407
P577
2008-07-17T00:00:00Z