scholarly article | Q13442814 |
review article | Q7318358 |
P819 | ADS bibcode | 2017SciA....3E3076K |
P356 | DOI | 10.1126/SCIADV.1603076 |
P932 | PMC publication ID | 5435417 |
P698 | PubMed publication ID | 28560344 |
P50 | author | Martin A. Nowak | Q87451 |
Andrew H. Knoll | Q505705 | ||
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Historical Development of Zircon Geochronology | Q57877630 | ||
740 Ma vase-shaped microfossils from Yukon, Canada: Implications for Neoproterozoic chronology and biostratigraphy | Q58078734 | ||
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Geologic Time Scale 2004 - why, how, and where next! | Q58337526 | ||
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Mass-Independent Fractionation of Sulfur Isotopes in Archean Sediments: Strong Evidence for an Anoxic Archean Atmosphere | Q70511359 | ||
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Earliest human occupations at Dmanisi (Georgian Caucasus) dated to 1.85-1.78 Ma | Q22066271 | ||
Controls on development and diversity of Early Archean stromatolites | Q22066279 | ||
Evolutionary Morphology, Innovation, and the Synthesis of Evolutionary and Developmental Biology | Q22122453 | ||
Stratigraphic placement and age of modern humans from Kibish, Ethiopia | Q22122476 | ||
The rate of adaptation in asexuals | Q24548116 | ||
Estimating the timing of early eukaryotic diversification with multigene molecular clocks | Q24614721 | ||
Devonian rise in atmospheric oxygen correlated to the radiations of terrestrial plants and large predatory fish | Q24624525 | ||
The Simons Genome Diversity Project: 300 genomes from 142 diverse populations | Q27025297 | ||
Cyanobacterial photosystem II at 2.9-A resolution and the role of quinones, lipids, channels and chloride | Q27653817 | ||
Rapid emergence of life shown by discovery of 3,700-million-year-old microbial structures | Q28005492 | ||
A bottom-up perspective on ecosystem change in Mesozoic oceans | Q28073333 | ||
A critical reappraisal of the fossil record of the bilaterian phyla | Q28139976 | ||
Microfossils of the Early Archean Apex chert: new evidence of the antiquity of life | Q28215389 | ||
Extraterrestrial cause for the cretaceous-tertiary extinction | Q28244869 | ||
Stromatolite reef from the Early Archaean era of Australia | Q28244909 | ||
New light shed on the oldest insect | Q28244996 | ||
Morphological disparity in the cambrian | Q28247992 | ||
Impacts of the Cretaceous Terrestrial Revolution and KPg extinction on mammal diversification | Q28248919 | ||
The Cambrian conundrum: early divergence and later ecological success in the early history of animals | Q28253972 | ||
The geological record of ocean acidification | Q28261134 | ||
The geological record and phylogeny of the Myriapoda | Q28265959 | ||
The Chicxulub asteroid impact and mass extinction at the Cretaceous-Paleogene boundary | Q28274950 | ||
Time scales of critical events around the Cretaceous-Paleogene boundary | Q28285178 | ||
A Devonian tetrapod-like fish and the evolution of the tetrapod body plan | Q28306051 | ||
A genomic history of Aboriginal Australia | Q28314883 | ||
Genomic analyses inform on migration events during the peopling of Eurasia | Q28314885 | ||
Environmental changes define ecological limits to species richness and reveal the mode of macroevolutionary competition | Q28597198 | ||
A Rare Glimpse of Paleoarchean Life: Geobiology of an Exceptionally Preserved Microbial Mat Facies from the 3.4 Ga Strelley Pool Formation, Western Australia | Q28602013 | ||
Decimetre-scale multicellular eukaryotes from the 1.56-billion-year-old Gaoyuzhuang Formation in North China | Q28602482 | ||
Selenium isotope evidence for progressive oxidation of the Neoproterozoic biosphere | Q28602983 | ||
Cyanobacteria and the Great Oxidation Event: evidence from genes and fossils | Q28604242 | ||
Simple versus complex models of trait evolution and stasis as a response to environmental change | Q28648281 | ||
Dynamic evolutionary change in post-Paleozoic echinoids and the importance of scale when interpreting changes in rates of evolution | Q28651088 | ||
On the age of eukaryotes: evaluating evidence from fossils and molecular clocks | Q28655429 | ||
High-precision timeline for Earth's most severe extinction | Q28657988 | ||
Temporal acuity and the rate and dynamics of mass extinctions | Q28657997 | ||
The characteristics and chronology of the earliest Acheulean at Konso, Ethiopia | Q28709259 | ||
Sulfur isotopes of organic matter preserved in 3.45-billion-year-old stromatolites reveal microbial metabolism | Q28727466 | ||
Leaf evolution in Southern Hemisphere conifers tracks the angiosperm ecological radiation | Q28742282 | ||
Rates of speciation in the fossil record | Q28765243 | ||
The oxygenation of the atmosphere and oceans | Q28767425 | ||
Proterozoic and early Cambrian protists: evidence for accelerating evolutionary tempo | Q28775962 | ||
Xylem in early tracheophytes | Q29030124 | ||
Paradigm shift in determining Neoproterozoic atmospheric oxygen | Q29042179 | ||
Absolute diversification rates in angiosperm clades | Q29547826 | ||
U-Pb geochronology of the Deccan Traps and relation to the end-Cretaceous mass extinction | Q29999323 | ||
Evolution of developmental potential and the multiple independent origins of leaves in Paleozoic vascular plants | Q29999879 | ||
Toward major evolutionary transitions theory 2.0. | Q30662242 | ||
Statistical analysis of iron geochemical data suggests limited late Proterozoic oxygenation | Q30982109 | ||
High-precision geochronology confirms voluminous magmatism before, during, and after Earth's most severe extinction | Q31027740 | ||
13C-Depleted carbon microparticles in >3700-Ma sea-floor sedimentary rocks from west greenland | Q31918377 | ||
Rates of evolution on the time scale of the evolutionary process | Q32062523 | ||
Geological history and phylogeny of Chelicerata | Q33525755 | ||
Paleoanthropology. Early Homo at 2.8 Ma from Ledi-Geraru, Afar, Ethiopia. | Q34043353 | ||
Calibrating the Cryogenian. | Q34102170 | ||
Fixation probability and time in subdivided populations | Q34206004 | ||
Dating the rise of atmospheric oxygen | Q34288690 | ||
The speed of evolution and maintenance of variation in asexual populations | Q34330675 | ||
Ocean oxygenation in the wake of the Marinoan glaciation | Q34423481 | ||
Novelty and Innovation in the History of Life | Q34496953 | ||
New geological and palaeontological age constraint for the gorilla-human lineage split. | Q34513363 | ||
The speed of adaptation in large asexual populations | Q34645731 | ||
A Cambrian peak in morphological variation within trilobite species | Q34656504 | ||
The time scale of evolutionary innovation | Q35247990 | ||
Species richness at continental scales is dominated by ecological limits | Q35612419 | ||
The rise of oxygen and siderite oxidation during the Lomagundi Event | Q35669356 | ||
ANTHROPOLOGY. Defining the genus Homo | Q35758046 | ||
The uncertain role of diversity dependence in species diversification and the need to incorporate time-varying carrying capacities | Q35957006 | ||
Sex and the shifting biodiversity dynamics of marine animals in deep time | Q36185033 | ||
Timing and tempo of the Great Oxidation Event | Q36272331 | ||
The molecular origins of evolutionary innovations | Q37923164 | ||
Life: the first two billion years | Q38965411 | ||
Oceanic oxygenation events in the anoxic Ediacaran ocean. | Q39878227 | ||
Evolution of the global phosphorus cycle | Q45049399 | ||
Paleoproterozoic sterol biosynthesis and the rise of oxygen | Q46408672 | ||
Timescales of Oxygenation Following the Evolution of Oxygenic Photosynthesis | Q46682637 | ||
Calibrating rates of early Cambrian evolution | Q47253479 | ||
Biogenicity of morphologically diverse carbonaceous microstructures from the ca. 3400 Ma Strelley pool formation, in the Pilbara Craton, Western Australia | Q47339717 | ||
Rates of evolution: effects of time and temporal scaling | Q47448485 | ||
Critical testing of Earth's oldest putative fossil assemblage from the ∼3.5Ga Apex chert, Chinaman Creek, Western Australia | Q47517097 | ||
Microorganisms from the Gunflint Chert | Q47795957 | ||
Life on the earth its origin and succession | Q51432186 | ||
Epistasis and allele specificity in the emergence of a stable polymorphism in Escherichia coli. | Q51463292 | ||
Mechanisms of Evolutionary Innovation Point to Genetic Control Logic as the Key Difference Between Prokaryotes and Eukaryotes. | Q53606806 | ||
Bangiomorpha pubescensn. gen., n. sp.: implications for the evolution of sex, multicellularity, and the Mesoproterozoic/Neoproterozoic radiation of eukaryotes | Q54086309 | ||
Triggering of the largest Deccan eruptions by the Chicxulub impact | Q55866788 | ||
Anthropogenic carbon release rate unprecedented during the past 66 million years | Q55872475 | ||
Dodging snowballs: Geochronology of the Gaskiers glaciation and the first appearance of the Ediacaran biota | Q55880238 | ||
P275 | copyright license | Creative Commons Attribution-NonCommercial 4.0 International | Q34179348 |
P433 | issue | 5 | |
P921 | main subject | environment | Q2249676 |
biomedical investigative technique | Q66648976 | ||
P304 | page(s) | e1603076 | |
P577 | publication date | 2017-05-01 | |
2017-05-17 | |||
P1433 | published in | Science Advances | Q19881044 |
P1476 | title | The timetable of evolution | |
P478 | volume | 3 |
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