isoprobe-t multicollector thermal ionization mass spectrometer (IsotopX Ltd)
90
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IsotopX Ltd
isoprobe-t multicollector thermal ionization mass spectrometer
Isoprobe T Multicollector Thermal Ionization Mass Spectrometer, supplied by IsotopX Ltd, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/product/isoprobe+t+thermal+ionization+mass+spectrometer/isoprobe+t+thermal+ionization+mass+spectrometer/pmc10372641__pnas__2301478120__sapp-46-15-14
Average 90 stars, based on 1 article reviews
Isoprobe T Multicollector Thermal Ionization Mass Spectrometer, supplied by IsotopX Ltd, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/product/isoprobe+t+thermal+ionization+mass+spectrometer/isoprobe+t+thermal+ionization+mass+spectrometer/pmc10372641__pnas__2301478120__sapp-46-15-14
Average 90 stars, based on 1 article reviews
isoprobe-t multicollector thermal ionization mass spectrometer - by Bioz Stars,
2026-10
90/100 stars
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Targeted Proteomics:Article Title: Fluctuations in Precambrian atmospheric oxygenation recorded by chromium isotopes. Article Snippet: Geochemical data suggest that oxygenation of the Earth’s atmosphere occurred in two broad steps.. The first rise in atmospheric oxygen is thought to have occurred between 2.45 and 2.2 Gyr ago, leading to a significant increase in atmospheric oxygen concentrations and concomitant oxygenation of the shallow surface ocean.. The second increase in atmospheric oxygen appears to have taken place in distinct stages during the late Neoproterozoic era ( 800–542 Myr ago), ultimately leading to oxygenation of the deep ocean 580 Myr ago, but details of the evolution of atmospheric oxygenation remain uncertain. Mass Spectrometry:Article Title: Fluctuations in Precambrian atmospheric oxygenation recorded by chromium isotopes. Article Snippet: Geochemical data suggest that oxygenation of the Earth’s atmosphere occurred in two broad steps.. The first rise in atmospheric oxygen is thought to have occurred between 2.45 and 2.2 Gyr ago, leading to a significant increase in atmospheric oxygen concentrations and concomitant oxygenation of the shallow surface ocean.. The second increase in atmospheric oxygen appears to have taken place in distinct stages during the late Neoproterozoic era ( 800–542 Myr ago), ultimately leading to oxygenation of the deep ocean 580 Myr ago, but details of the evolution of atmospheric oxygenation remain uncertain. Article Title: The Cr-isotope signature of surface seawater — A global perspective Article Snippet: This study presents chromium-isotope data (expressed as δ 53 Cr) and chromium concentrations (Cr) of surface seawater (0–2 m depth) from a variety of locations worldwide.. In addition to samples from the open ocean (Arctic, Southern, Pacific, and Atlantic Oceans), samples were analysed from areas with more restricted water exchange rates (the Mediterranean Sea, Øresund, and Baltic Sea).. The data indicate a heterogeneous distribution of δ 53 Cr in seawater with a total range from +0.13‰ to +1.24‰. Article Title: Highly fractionated chromium isotopes in Mesoproterozoic-aged shales and atmospheric oxygen Article Snippet: .. The Cr isotope measurements were performed on an IsotopX, Ltd. |
