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Funding Information: We are grateful to the editor Richard Jordan and two anonymous reviewers for their comments that greatly improved the early version of the paper. G.R was funded by a NERC studentship through the ACCE (Adapting to the Challenges of a Changing Environment) Doctoral Training Partnership (Grant No. 2210800). The modern Ythan samples were collected, prepared and counted as part of P.M's University of York BSc thesis: ?Surface distributions of salt-marsh foraminifera for the Ythan estuary, NE Scoltand: an unprecedented modern analogue for Holocene sea-level studies?, 2018. We thank W McKay and the Scottish Natural Heritage for providing support and access to the field site. RE, YM and RG worked on and provided the previously published data. We thank the technicians at the Department of Environment and Geography, University of York, particularly Maria Gehrels for her assistance with laboratory work on the Ythan samples, and the countless other people who contributed to the collection and collation of the foraminifera data from the existing sites. We also 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. Funding Information: We are grateful to the editor Richard Jordan and two anonymous reviewers for their comments that greatly improved the early version of the paper. G.R was funded by a NERC studentship through the ACCE (Adapting to the Challenges of a Changing Environment) Doctoral Training Partnership (Grant No. 2210800 ). The modern Ythan samples were collected, prepared and counted as part of P.M's University of York BSc thesis: ‘Surface distributions of salt-marsh foraminifera for the Ythan estuary, NE Scoltand: an unprecedented modern analogue for Holocene sea-level studies’, 2018. We thank W McKay and the Scottish Natural Heritage for providing support and access to the field site. RE, YM and RG worked on and provided the previously published data. We thank the technicians at the Department of Environment and Geography, University of York, particularly Maria Gehrels for her assistance with laboratory work on the Ythan samples, and the countless other people who contributed to the collection and collation of the foraminifera data from the existing sites. We also 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. Publisher Copyright: © 2021 |
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CORE (COnnecting REpositories)