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Funding statement
This paper has been written in the framework of PALSEA, the PALeo constraints on SEA level rise project, sponsored by PAGES and INQUA. This publication was planned at the PALSEA workshop in Lochinver, Scotland, organised by Antony Long and Natasha Barlow (Durham University). Publication costs were covered by Tulane's Vokes Geology Fund (Torbjorn E. Tornqvist). The authors wish to thank the following funding sources: Natural Environmental Research Council under the numbers NE/I008365/1 (Andre Dusterhus) and NE/I008624/1 (W. Roland Gehrels); Institutional Strategy of the University of Bremen (German Excellence Initiative, Alessio Rovere); the US National Science Foundation (NSF) grant OCE1458904 (Benjamin P. Horton, Robert E. Kopp), grant OCE-1502588 (Torbjorn Tornqvist) and award no. 1443037 (Andrea Dutton); Global Change Program (EAR 1304909, Jorie Clark); and the German Climate Modeling Initiative (PALMOD, Volker Klemann).
Remove constraint Funding statement: This paper has been written in the framework of PALSEA, the PALeo constraints on SEA level rise project, sponsored by PAGES and INQUA. This publication was planned at the PALSEA workshop in Lochinver, Scotland, organised by Antony Long and Natasha Barlow (Durham University). Publication costs were covered by Tulane's Vokes Geology Fund (Torbjorn E. Tornqvist). The authors wish to thank the following funding sources: Natural Environmental Research Council under the numbers NE/I008365/1 (Andre Dusterhus) and NE/I008624/1 (W. Roland Gehrels); Institutional Strategy of the University of Bremen (German Excellence Initiative, Alessio Rovere); the US National Science Foundation (NSF) grant OCE1458904 (Benjamin P. Horton, Robert E. Kopp), grant OCE-1502588 (Torbjorn Tornqvist) and award no. 1443037 (Andrea Dutton); Global Change Program (EAR 1304909, Jorie Clark); and the German Climate Modeling Initiative (PALMOD, Volker Klemann).