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Late Pleistocene δ¹¹B based carbon dioxide levels from ODP Site 154-926
Earth's climate cooled markedly during the Late Miocene from 12 to 5 million years ago, with far-reaching consequences for global ecosystems. However, the driving forces of... -
Geochemical and isotope data from shallow aquifers in the Bas-Saint-Laurent a...
In this study, we combined radon in water activity (222Rn), stable isotopes of inorganic carbon (δ13CDIC), water stable isotopes (δ18O; δ2H) as well as major and trace ions...
