about
Sulfur isotopes of organic matter preserved in 3.45-billion-year-old stromatolites reveal microbial metabolismHigh-temperature environments of human evolution in East Africa based on bond ordering in paleosol carbonates“Clumped-isotope” geochemistry—The study of naturally-occurring, multiply-substituted isotopologuesLarge and unexpected enrichment in stratospheric 16O13C18O and its meridional variation.The magnitude and duration of Late Ordovician-Early Silurian glaciation.Potential environmental impact of a hydrogen economy on the stratosphere.Isotopic ordering in eggshells reflects body temperatures and suggests differing thermophysiology in two Cretaceous dinosaurs.Coupling of surface temperatures and atmospheric CO2 concentrations during the Palaeozoic era.Impact-induced shock and the formation of natural quasicrystals in the early solar system.Carbonates in the Martian meteorite Allan Hills 84001 formed at 18 +/- 4 degrees C in a near-surface aqueous environmentEvidence for the extraterrestrial origin of a natural quasicrystalThe chlorine isotope fingerprint of the lunar magma ocean.SQUID-SIMS is a useful approach to uncover primary signals in the Archean sulfur cycle.Lunar apatite with terrestrial volatile abundances.Low-temperature carbonate concretions in the Martian meteorite ALH84001: evidence from stable isotopes and mineralogy.Oxygen-isotope evidence for recycled crust in the sources of mid-ocean-ridge basaltsRedox variations in Mauna Kea lavas, the oxygen fugacity of the Hawaiian plume, and the role of volcanic gases in Earth's oxygenation.Dinosaur body temperatures determined from isotopic (¹³C-¹⁸O) ordering in fossil biominerals.Secondary ion mass spectrometry of vapor-liquid-solid grown, Au-catalyzed, Si wires.Rapid uplift of the Altiplano revealed through 13C-18O bonds in paleosol carbonates.Abrupt pre-Bølling-Allerød warming and circulation changes in the deep ocean.Extreme deuterium enrichment in stratospheric hydrogen and the global atmospheric budget of H2.A hydrothermal origin for isotopically anomalous cap dolostone cements from south China.Geology. On the origins of granites.Gas formation. Formation temperatures of thermogenic and biogenic methane.Geochemistry. The oldest fossil or just another rock?Measurement of rare isotopologues of nitrous oxide by high-resolution multi-collector mass spectrometry.Carbon isotope evidence for early life.Combined 13C–D and D–D clumping in methane: Methods and preliminary resultsA high-resolution gas-source isotope ratio mass spectrometerOxygen isotope composition of the Phanerozoic ocean and a possible solution to the dolomite problemThe utility of methane clumped isotopes to constrain the origins of methane in natural gas accumulationsMethane clumped isotopes: Progress and potential for a new isotopic tracerPrediction of equilibrium distributions of isotopologues for methane, ethane and propane using density functional theoryDistinguishing and understanding thermogenic and biogenic sources of methane using multiply substituted isotopologuesDiverse origins of Arctic and Subarctic methane point source emissions identified with multiply-substituted isotopologuesEquilibrium and non-equilibrium controls on the abundances of clumped isotopologues of methane during thermogenic formation in laboratory experiments: Implications for the chemistry of pyrolysis and the origins of natural gasesMethane clumped isotopes in the Songliao Basin (China): New insights into abiotic vs. biotic hydrocarbon formation18O13C16O in Earth’s atmosphereEquilibrium thermodynamics of multiply substituted isotopologues of molecular gases
P50
Q28727466-ABC1B378-E8EC-4A98-A9B1-CAFAD2E8B3CFQ28750663-C209EFAC-C884-4C44-9B3C-16A1225EC03BQ29396094-FB2C7B2E-E962-4FFF-BAE1-FFB9D281BB2EQ33476092-39B0AEC6-4020-47E7-86C6-12901D604B19Q34161124-098B428D-9DC3-49FF-968B-7C85D87C2BE2Q34205784-BC2A6C64-132E-4E2A-81D3-7A93FA407D08Q34497826-26A85655-F023-4ACC-A663-09DB602DD562Q34686607-8AA75ADD-56E1-43AB-B969-D203DB52E39EQ35187402-343F042B-B2C3-48CC-B08B-17883A4A914FQ35345809-E5D44978-AB84-475C-8BA5-FA59FB0F77DDQ35749759-2A1FC935-CC4B-48D9-9695-9E61282FBB6BQ35851165-44B672A0-F809-4F8D-B02A-73FDE8312999Q37711998-B5066160-4217-4D72-8392-3C728457481DQ38483242-186FDBB2-AB81-42F3-AEEC-6725A4F0E4A3Q38502805-E445EF0C-A9B8-479D-966D-BF50DAE29AC5Q41719678-D44489B0-EC56-4E6C-B380-C5634675C531Q41927313-01656A7C-2FC6-4958-83A7-ACCC2666C889Q43940264-2702797E-A026-4353-B581-7E3DD8FDEB2BQ45933721-4D082870-BFF5-4562-9961-DB034511D1A3Q45952382-84D02322-3666-4B2B-8F03-51E4D9225E06Q46131312-6004020C-7702-4C75-988E-69EE7653BD43Q46181628-7ED093AD-93E2-4B27-9064-473739BF32B3Q46186502-02B5386E-A585-43DF-B2E0-DA911412A444Q46523908-FDD49D8B-26E6-46B8-A7DB-54797933D34FQ46753793-C22B2F70-347C-4CCC-84D0-EE75B1DF048FQ46843855-5553A885-BE39-4821-8426-5450EB455356Q46942350-613A3C25-41DE-4C9D-A47F-08BE47C8B611Q52267009-76FAB758-A063-4383-9F19-6CB21FB0AC73Q55881624-9FE0924B-CB63-40EE-9AEA-04000B0563D0Q55881625-DDDB8C53-1536-4F5C-A5BE-FEEFA66B99BEQ56520792-34B0D3E5-B5A8-4526-B833-5A8D38E68FE4Q56600982-57B4E1A7-C80D-4ECD-884A-BA80AC3F4DD6Q56600983-0CF1D135-DDA3-4172-B512-5AE7591641F0Q56600985-13FDEE55-F212-4B99-958C-57F9EE36A900Q56600987-C5BC9FBA-9102-48D1-9F3D-A0489F91ED3EQ56600988-D2F74AE5-0E1D-4F1C-8F13-506519CB9B5AQ56600989-B46A6F06-1CF3-4343-91BC-9FE3BD416A71Q56600991-D326EB14-215B-4FF0-BE22-559F4993F42EQ56673996-FAD9AB09-C91D-48E0-A1D8-6A317854C809Q56673997-E65C0A6B-0BB0-432C-A4A9-0A58673AC58F
P50
description
professor, geologist at Caltech
@en
name
John M. Eiler
@ast
John M. Eiler
@en
John M. Eiler
@es
John M. Eiler
@nl
type
label
John M. Eiler
@ast
John M. Eiler
@en
John M. Eiler
@es
John M. Eiler
@nl
altLabel
J. M. Eiler
@en
J.M. Eiler
@en
John Eiler
@en
John M Eiler
@en
prefLabel
John M. Eiler
@ast
John M. Eiler
@en
John M. Eiler
@es
John M. Eiler
@nl
P1960
U6nxFFsAAAAJ