Reply to comment by E. Bard et al. on “Younger Dryas sea level and meltwater pulse 1B recorded in Barbados reef crest coralAcropora palmata” by N. A. Abdul et al.

Final deglaciation of the Scandinavian Ice Sheet and implications for the Holocene global sea-level budget

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Younger Dryas sea level and meltwater pulse 1B recorded in Barbados reef crest coralAcropora palmata

(2016) N. A. Abdul et al.   PALEOCEANOGRAPHY

Comment on “Younger Dryas sea level and meltwater pulse 1B recorded in Barbados reefal crest coralAcropora palmata” by N. A. Abdul et al.

(2016) Edouard Bard et al.   PALEOCEANOGRAPHY

Deglaciation of Fennoscandia

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Sea level and global ice volumes from the Last Glacial Maximum to the Holocene

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Barbados-based estimate of ice volume at Last Glacial Maximum affected by subducted plate

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Ice-sheet collapse and sea-level rise at the Bølling warming 14,600 years ago

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Ice sheet sources of sea level rise and freshwater discharge during the last deglaciation

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Evidence for a slow subsidence of the Tahiti Island from GPS, DORIS, and combined satellite altimetry and tide gauge sea level records

(2011) Abdelali Fadil et al.   COMPTES RENDUS GEOSCIENCE

Assessing subsidence rates and paleo water-depths for Tahiti reefs using U–Th chronology of altered corals

(2011) Alexander L. Thomas et al.   MARINE GEOLOGY

Deglacial Meltwater Pulse 1B and Younger Dryas Sea Levels Revisited with Boreholes at Tahiti

(2010) E. Bard et al.   SCIENCE

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