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University of St Andrews. School of Earth & Environmental Sciences
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Cambrian-Eocene pre-rift, pulsed rift, passive margin and emplacement processes...
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Decline of anthropogenic lead in South Atlantic Ocean surface waters from 1990 t...
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Benthic foraminiferal turnover across the Dan-C2 event in the eastern South Atla...
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Importance of the Antarctic Slope Current in the Southern Ocean response to ice...
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Lithium elemental and isotope systematics of modern and cultured brachiopods : i...
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Boron isotope systematics of cultured brachiopods : Response to acidification, v...
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A high‐fidelity benthic stable isotope record of Late Cretaceous–Early Eocene cl...
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Variation in brachiopod microstructure and isotope geochemistry under low-pH-oce...
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Geological evolution of the Hampshire Basin (southern England) during a global c...
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Unravelling the complex geological evolution of one of Earth's final remaining f...
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The last forests on Antarctica : reconstructing flora and temperature from the N...
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Assessing the utility of barium isotopes to trace Eurasian riverine freshwater i...
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Mesoarchean partial melting of mafic crust and tonalite production during high-T...
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Stirred not shaken; critical evaluation of a proposed Archean meteorite impact i...
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Building Mesoarchaean crust upon Eoarchaean roots : the Akia Terrane, West Green...
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North Atlantic Craton architecture revealed by kimberlite-hosted crustal zircons
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Geodynamic implications of synchronous Norite and TTG formation in the 3 Ga Mani...
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Apatite : a U-Pb thermochronometer or geochronometer?
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Regional zircon U-Pb geochronology for the Maniitsoq region, southwest Greenland
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Demons in the North Atlantic : variability of deep ocean ventilation
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