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The work profited from discussions at the CVAS working group of the Past Global Changes (PAGES) programme.
We acknowledge PALSEA, a working group of the International Union for Quaternary Sciences (INQUA) and Past Global Changes (PAGES), which in turn received support from the Swiss Academy of Sciences and the Chinese Academy of Sciences.
The authors acknowledge the collaborative research opportunities created by PALSEA, a working group of the International Union for Quaternary Sciences (INQUA) and Past Global Changes (PAGES), which in turn received support from the Swiss Academy of Sciences and the Chinese Academy of Sciences.
SJH, AMD and JCT were supported by the European Geoscience Union Galileo Conference fund (PlioMioVAR workshop, Leeds, UK, and online, 24–26 August 2022).
This manuscript was realized in the framework of the PAGES working group CVAS.
The authors acknowledge PALSEA (Palaeo-Constraints on Sea-Level Rise), a working group of the International Union for Quaternary Sciences (INQUA) and Past Global Changes (PAGES).
The PAGES Data Stewardship Scholarship (DSS_108) also supported this work. We thank SISAL members who contributed their published data to the database and provided additional information when necessary. Authors also thank the IT team of the RCAES, namely Evelin Bányai for installing the app on servers. We are also grateful to the SISAL Phase 2 Steering Committee for help in debugging the app. This is contribution No. 85 of the 2ka Palæoclimatology Research Group. The first author dedicates this paper to the memory of his beloved grandmother, Marta Chiovini (1928–2023).
This study includes data compiled by SISAL, a working group of the Past Global Changes (PAGES) project and is in part inspired by discussions at a SISAL workshop in Xi'an (China) in 2019.
This study was also undertaken by PEOPLE 3000, a working group of the Past Global Changes (PAGES) project, which in turn received support from the Swiss Academy of Sciences and the Chinese Academy of Sciences.
The Iso2k database is a contribution to Phases 3 and 4 of the PAGES 2k Network.