0000000000219302

AUTHOR

Keith M. Prufer

0000-0003-3173-1546

showing 2 related works from this author

Reconstructing the deep population history of Central and South America

2018

We report genome-wide ancient DNA from 49 individuals forming four parallel time transects in Belize, Brazil, the Central Andes, and the Southern Cone, each dating to at least ∼9,000 years ago. The common ancestral population radiated rapidly from just one of the two early branches that contributed to Native Americans today. We document two previously unappreciated streams of gene flow between North and South America. One affected the Central Andes by ∼4,200 years ago, while the other explains an affinity between the oldest North American genome associated with the Clovis culture and the oldest Central and South Americans from Chile, Brazil, and Belize. However, this was not the primary sou…

0301 basic medicineGene Flow010506 paleontologyHistoryPopulationPopulationPopulation ReplacementBiology01 natural sciencesGenomeMedical and Health SciencesDNA MitochondrialGeneral Biochemistry Genetics and Molecular BiologyGene flowAncient03 medical and health sciencesTheoreticalModelsGeneticsHumansGENÉTICA DE POPULAÇÕESanthropologyIndis de l'Amèrica CentralDNA AncientTransecteducationHistory Ancient0105 earth and related environmental scienceseducation.field_of_studypopulation geneticGenomeGenome HumanHuman Genomepopulation geneticsarchaeologyCentral AmericaDNABiological SciencesSouth AmericaModels TheoreticalArchaeologyMitochondrial030104 developmental biologyAncient DNAGenetics PopulationDevelopmental BiologyHuman
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Intra- and inter-annual uranium concentration variability in a Belizean stalagmite controlled by prior aragonite precipitation: A new tool for recons…

2016

Aragonitic speleothems are increasingly utilised as palaeoclimate archives due to their amenability to high precision U–Th dating. Proxy records from fast-growing aragonitic stalagmites, precisely dated to annual timescales, can allow investigation of climatic events occurring on annual or even sub-annual timescales with minimal chronological uncertainty. However, the behaviour of many trace elements, such as uranium, in aragonitic speleothems has not thus far been as well constrained as in calcitic speleothems. Here, we use uranium concentration shifts measured across primary calcite-to-aragonite mineralogical transitions in speleothems to calculate the distribution coefficient of uranium …

010504 meteorology & atmospheric sciencesGeochemistryF700MineralogySpeleothemF800StalagmiteF600engineering.material010502 geochemistry & geophysics01 natural sciencesF900Geochemistry and PetrologymedicinePrecipitation0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryδ13CStable isotope ratioAragoniteTrace element15. Life on landSeasonalitymedicine.disease13. Climate actionengineeringGeologyGeochimica et Cosmochimica Acta
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