Nicolas Caillon researcher ORCID ID = 0000-0002-6318-6194
Caillon, Nicolas
VIAF ID: 198796053 ( Personal )
Permalink: http://viaf.org/viaf/198796053
Preferred Forms
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Works
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Age of Himalayan bottom ice cores |
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Analyse isotopique de l'air piégé dans la glace pour quantifier les variations de température |
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Atmospheric nitrate export in streams along a montane to urban gradient |
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Automated system measuring triple oxygen and nitrogen isotope ratios in nitrate using the bacterial method and N2 O decomposition by microwave discharge. |
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Composition isotopique de l'air piégé dans les glaces polaires : outil de paléothermométrie |
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Evidence for stratigraphic distortion in the Greenland Ice Core Project (GRIP) ice core during Event 5e1 (120 kyr BP) from gas isotopes |
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Foliar uptake of atmospheric nitrate by two dominant subalpine plants: insights from in situ triple-isotope analysis |
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High-resolution record of Northern Hemisphere climate extending into the last interglacial period |
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Interlaboratory study for coral Sr/Ca and other element/Ca ratio measurements |
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Isotopic composition of trapped air in polar ice : cores used as a paleothermometer. |
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Large temperature variations over rapid climatic events in Greenland: a method based on air isotopic measurements |
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Mg/Ca thermometry in planktic foraminifera: Improving paleotemperature estimations forG. bulloidesandN. pachydermaleft |
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The monsoon imprint during the ‘atypical’ MIS 13 as seen through north and equatorial Indian Ocean records |
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Rapid climate variability during warm and cold periods in polar regions and Europe |
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Seasonal variations of triple oxygen isotopic compositions of atmospheric sulfate, nitrate, and ozone at Dumont d'Urville, coastal Antarctica |
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A simple and reliable method reducing sulfate to sulfide for multiple sulfur isotope analysis. |
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Summer variability of the atmospheric NO<sub>2</sub> : NO ratio at Dome C on the East Antarctic Plateau |
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Timing of atmospheric CO2 and Antarctic temperature changes across termination III |
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Tracing the Fate of Atmospheric Nitrate in a Subalpine Watershed Using ΔO |
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