scholarly article | Q13442814 |
P819 | ADS bibcode | 2019NatCo..10..466G |
P6179 | Dimensions Publication ID | 1111673601 |
P356 | DOI | 10.1038/S41467-019-08357-0 |
P932 | PMC publication ID | 6349899 |
P698 | PubMed publication ID | 30692536 |
P50 | author | Francis Albarède | Q3081274 |
Naohiro Yoshida | Q47297390 | ||
Elsa Gautier | Q61469300 | ||
Shohei Hattori | Q59846928 | ||
P2093 | author name string | J Hoek | |
J Savarino | |||
J Farquhar | |||
N Caillon | |||
E Albalat | |||
J Erbland | |||
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SO2 Oxidation Kinetics Leave a Consistent Isotopic Imprint on Volcanic Ice Core Sulfate | Q103814635 | ||
Seasonal variations of triple oxygen isotopic compositions of atmospheric sulfate, nitrate, and ozone at Dumont d'Urville, coastal Antarctica | Q103814642 | ||
Simulation of the diurnal variations of the oxygen isotope anomaly (Δ17O) of reactive atmospheric species | Q103814678 | ||
Anomalous sulfur isotope compositions of volcanic sulfate over the last millennium in Antarctic ice cores | Q103814684 | ||
Evidence from sulfate mass independent oxygen isotopic compositions of dramatic changes in atmospheric oxidation following massive volcanic eruptions | Q103814693 | ||
UV induced mass-independent sulfur isotope fractionation in stratospheric volcanic sulfate | Q103814695 | ||
Observation of wavelength-sensitive mass-independent sulfur isotope effects during SO2photolysis: Implications for the early atmosphere | Q103814701 | ||
Analytical procedure to determine both δ18O and δ17O of H2O2 in natural water and first measurements | Q103814705 | ||
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Cooling and societal change during the Late Antique Little Ice Age from 536 to around 660 AD | Q56209574 | ||
Climatic and societal impacts of a volcanic double event at the dawn of the Middle Ages | Q56656824 | ||
Robust global ocean cooling trend for the pre-industrial Common Era | Q56680688 | ||
Evolution of the oceanic sulfur cycle at the end of the Paleoproterozoic | Q56836611 | ||
Volcanic cooling signal in tree ring temperature records for the past millennium | Q56864233 | ||
Tree ring effects and ice core acidities clarify the volcanic record of the first millennium | Q56864240 | ||
Oxygen and sulfur isotopic composition of volcanic sulfate aerosol at the point of emission | Q57677142 | ||
Variability of sulfate signal in ice core records based on five replicate cores | Q57890952 | ||
Millennia-long tree-ring records from Tasmania and New Zealand: a basis for modelling climate variability and forcing, past, present and future | Q58063478 | ||
Insights from Antarctica on volcanic forcing during the Common Era | Q58083523 | ||
Volcanic forcing of climate over the past 1500 years: An improved ice core-based index for climate models | Q58262332 | ||
Modeling the distribution of the volcanic aerosol cloud from the 1783–1784 Laki eruption | Q58262370 | ||
Climatic response to high-latitude volcanic eruptions | Q58262384 | ||
A new bipolar ice core record of volcanism from WAIS Divide and NEEM and implications for climate forcing of the last 2000 years | Q58390757 | ||
Sulfur isotope measurement of sulfate and sulfide by high-resolution MC-ICP-MS | Q58391468 | ||
P275 | copyright license | Creative Commons Attribution 4.0 International | Q20007257 |
P6216 | copyright status | copyrighted | Q50423863 |
P2507 | corrigendum / erratum | Author Correction: 2600-years of stratospheric volcanism through sulfate isotopes | Q92825603 |
P433 | issue | 1 | |
P407 | language of work or name | English | Q1860 |
P921 | main subject | stratosphere | Q108376 |
P304 | page(s) | 466 | |
P577 | publication date | 2019-01-28 | |
P1433 | published in | Nature Communications | Q573880 |
P1476 | title | 2600-years of stratospheric volcanism through sulfate isotopes | |
P478 | volume | 10 |
Q107964022 | Bipolar volcanic synchronization of abrupt climate change in Greenland and Antarctic ice cores during the last glacial period |
Q94569899 | Large mass-independent sulphur isotope anomalies link stratospheric volcanism to the Late Ordovician mass extinction |
Q117157002 | Volcanism and the Greenland ice cores: A new tephrochronological framework for the last glacial-interglacial transition (LGIT) based on cryptotephra deposits in three ice cores |
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