U–Pb ages from the neoproterozoic Doushantuo Formation, China.
about
Origin of the Eumetazoa: testing ecological predictions of molecular clocks against the Proterozoic fossil recordAt the origin of animals: the revolutionary cambrian fossil recordThe Ediacaran emergence of bilaterians: congruence between the genetic and the geological fossil recordsDarwin's dilemma: the realities of the Cambrian 'explosion'Haootia quadriformis n. gen., n. sp., interpreted as a muscular cnidarian impression from the Late Ediacaran period (approx. 560 Ma)Oxidation of the Ediacaran oceanDivergence time estimates and the evolution of major lineages in the florideophyte red algaeEdiacaran Marine Redox Heterogeneity and Early Animal EcosystemsSponge grade body fossil with cellular resolution dating 60 Myr before the CambrianPhosphogenesis in the 2460 and 2728 million-year-old banded iron formations as evidence for biological cycling of phosphate in the early biosphereTowards a quantitative understanding of the late Neoproterozoic carbon cycleComplex embryos displaying bilaterian characters from Precambrian Doushantuo phosphate deposits, Weng'an, Guizhou, ChinaMineralogical constraints on the paleoenvironments of the Ediacaran Doushantuo FormationOn the coevolution of Ediacaran oceans and animalsLarge spinose microfossils in Ediacaran rocks as resting stages of early animalsPulsed oxidation and biological evolution in the Ediacaran Doushantuo FormationThe earliest fossil record of the animals and its significanceExperimental taphonomy shows the feasibility of fossil embryos.A uniquely preserved Ediacaran fossil with direct evidence for a quilted bodyplan.Origin and evolutionary history of freshwater Rhodophyta: further insights based on phylogenomic evidence.An early Ediacaran assemblage of macroscopic and morphologically differentiated eukaryotes.Calibrating the Cryogenian.Giving the early fossil record of sponges a squeeze.Ocean oxygenation in the wake of the Marinoan glaciation.Molecular phylogeny and divergence times of deuterostome animals.Analysis of Conserved Glutamate and Aspartate Residues in Drosophila Rhodopsin 1 and Their Influence on Spectral Tuning.Sedimentary constraints on the duration of the Marinoan Oxygen-17 Depletion (MOSD) event.Episode of intense chemical weathering during the termination of the 635 Ma Marinoan glaciation.Seeking a geochemical identifier for authigenic carbonate.Uncovering the spatial heterogeneity of Ediacaran carbon cycling.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.Multiple sulfur isotope evidence for massive oceanic sulfate depletion in the aftermath of Snowball Earth.Oceanic oxygenation events in the anoxic Ediacaran ocean.Cryogenian evolution of stigmasteroid biosynthesis.Snowball Earth climate dynamics and Cryogenian geology-geobiology.A stratified redox model for the Ediacaran ocean.A unifying model for Neoproterozoic-Palaeozoic exceptional fossil preservation through pyritization and carbonaceous compression.Environmental context for the terminal Ediacaran biomineralization of animals.A hydrothermal origin for isotopically anomalous cap dolostone cements from south China.
P2860
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P2860
U–Pb ages from the neoproterozoic Doushantuo Formation, China.
description
2005 nî lūn-bûn
@nan
2005 թուականի Փետրուարին հրատարակուած գիտական յօդուած
@hyw
2005 թվականի փետրվարին հրատարակված գիտական հոդված
@hy
2005年の論文
@ja
2005年論文
@yue
2005年論文
@zh-hant
2005年論文
@zh-hk
2005年論文
@zh-mo
2005年論文
@zh-tw
2005年论文
@wuu
name
U-Pb ages from the neoproterozoic Doushantuo Formation, China.
@ast
U–Pb ages from the neoproterozoic Doushantuo Formation, China.
@en
type
label
U-Pb ages from the neoproterozoic Doushantuo Formation, China.
@ast
U–Pb ages from the neoproterozoic Doushantuo Formation, China.
@en
altLabel
U-Pb Ages from the Neoproterozoic Doushantuo Formation, China
@en
prefLabel
U-Pb ages from the neoproterozoic Doushantuo Formation, China.
@ast
U–Pb ages from the neoproterozoic Doushantuo Formation, China.
@en
P2093
P356
P1433
P1476
U–Pb ages from the neoproterozoic Doushantuo Formation, China.
@en
P2093
P356
10.1126/SCIENCE.1107765
P407
P577
2005-02-24T00:00:00Z
P5875
P698
P819
2005Sci...308...95C