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NERC Radiocarbon Facility
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Validation of Radiocarbon Dates of Woolly Mammoth Remains from Northwestern Chuk...
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Tracking millennial-scale Holocene glacial advance and retreat using osmium isot...
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Sedimentology and chronology of the advance and retreat of the last British-Iris...
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Late Holocene sea-level change in Arctic Norway
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Predicting climate change impacts on maritime Antarctic soils: a space-for-time...
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Controls upon the Last Glacial Maximum deglaciation of the northern Uummannaq Ic...
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Early deglaciation of the British-Irish Ice Sheet on the Atlantic shelf northwes...
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Soil microbial respiration in arctic soil does not acclimate to temperature
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A passive sampling method for radiocarbon analysis of soil respiration using mol...
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The age of CO2 released from soils in contrasting ecosystems during the arctic w...
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The mixed-bed glacial landform imprint of the North Sea Lobe in the western Nort...
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Plant carbon allocation drives turnover of old soil organic matter in permafrost...
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Ice-stream demise dynamically conditioned by trough shape and bed strength
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Selectively bred oysters can alter their biomineralization pathways, promoting r...
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Erosion of organic carbon in the Artic as a geological carbon dioxide sink
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Erosion of organic carbon in the Artic as a geological carbon dioxide sink
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Erosion of organic carbon in the Artic as a geological carbon dioxide sink
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Erosion of organic carbon in the Artic as a geological carbon dioxide sink
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Erosion of organic carbon in the Artic as a geological carbon dioxide sink
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Erosion of organic carbon in the Artic as a geological carbon dioxide sink
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