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- W1990477265 abstract "Quantitative analyses of foraminiferal distributions along the coast of Maine are used to provide transfer functions for reconstruction of sea-level changes from fossil foraminiferal assemblages. The indicative meaning of fossil assemblages is most accurately predicted by a training set that incorporates live and dead foraminifera and that uses flooding duration, not height, as the predictor variable. Sea-level records are produced for two sites in Maine (USA): a middle marsh site in Scarboro and a high marsh site in Machiasport. These records offer temporal resolution of five to seven years and span the past century. They are compared with instrumental data from a nearby tidal station to assess their accuracy. Strong correlations are found between the geologic records and the observational data, in particular between the foraminiferal record from Machiasport and the tide-gauge record from Eastport (r 2 = 0.83, p = 0.005). Thus a foraminifera-based transfer-function approach offers great potential for resolving decadal-scale sea-level changes from the geologic record." @default.
- W1990477265 created "2016-06-24" @default.
- W1990477265 creator A5001929892 @default.
- W1990477265 date "2000-04-01" @default.
- W1990477265 modified "2023-10-16" @default.
- W1990477265 title "Using foraminiferal transfer functions to produce high-resolution sea-level records from salt-marsh deposits, Maine, USA" @default.
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- W1990477265 doi "https://doi.org/10.1191/095968300670746884" @default.
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