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Authigenic 10Be/9Be ratios and 10Be-fluxes (230Thxs-normalized) in central Baffin Bay sediments during the last glacial cycle: Paleoenvironmental implications
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10Be/9Be ratios and 10Be-fluxes yield equivalent results from glaciomarine sediments.

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10Be-systematic variability mainly obeys to glacio-climatic condition changes.

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10Be production proxies do not allow to characterize the geomagnetic features in PC16.

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Denudation rates are steady except for brief ice surging episodes coeval to H-events.

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10Be concentration is controlled by freshwater inputs from regional Ice Sheets.

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