Journal articles
The study is also a contribution to the Past Global Change (PAGES) project and its working group LandCover6k that in turn received support from the Swiss National Science Foundation, the Swiss Academy of Sciences, the U.S. National Science Foundation, and the Chinese Academy of Sciences.
This is a contribution to the strategic research areas MERGE (ModElling the Regional and Global Earth system), the Bolin Centre for Climate Research, and the PAGES LandCover6k working group that, in turn, received support from the Swiss National Science Foundation, US National Science Foundation, Swiss Academy of Sciences, and Chinese Academy of Sciences.
We acknowledge support through the Past Global Change (PAGES) project and its working group LandCover6k (http://pastglobalchanges.org/landcover6k, last access: 25 July 2023).
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.
We acknowledge PALSEA, a working group of the International Union for Quaternary Sciences (INQUA) and Past Global Changes (PAGES).
This publication is a contribution from CLIVASH2k (Phase 3) of the PAGES 2k Network working group. CLIVASH2k is a contribution of Phase 3 of the PAGES 2k Network. Dieter Tetzner has been funded as part of the PAGES Data Stewardship scholarship awarded to Elizabeth R. Thomas. This financial support comes from the Chinese Academy of Sciences (CAS) and the Swiss Academy of Sciences (SCNAT). We thank the PAGES office for their support and the temporary data storage during the compilation of this database.
This paper was co-authored with PAGES Executive Director, Marie-France Loutre.
Some of the collaborations in this study were initiated through the PAGES QUIGS workshop 2020. We acknowledge the World Climate Research Programme, which, through its Working Group on Coupled Modelling, coordinated and promoted CMIP6, as well as the Working Group on Climate Models (WGCM) and Past Global Changes (PAGES) for their support of the Paleoclimate Modelling Intercomparison Project.
We thank the Past Global Changes (PAGES) programme for their financial and logistical support of the working group on Pliocene Climate Variability over glacial-interglacial timescales (PlioVAR), and we thank all workshop participants and members of the PlioVAR steering committee for their discussions.
This publication is a contribution towards PALSEA (Palaeo-Constraints on Sea-Level Rise), a working group of the International Union for Quaternary Sciences (INQUA) and Past Global Changes (PAGES), HOLSEA (Geographic variability of Holocene sea level) and International Geoscience Program (IGCP) Project 725, “Forecasting Coastal Change”.