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- W1963846006 abstract "Abstract Foraminiferal assemblages preserved within salt-marsh sediment can provide an accurate and precise means to reconstruct relative sea level due to a strong relationship with elevation, which can be quantified using a transfer function. We collected a set of surface samples from two salt marshes in the Morbihan Golfe, France to determine foraminiferal distribution patterns. Dominant taxa included Jadammina macrescens , Trochammina inflata , Haplophragmoides spp. and Miliammina fusca . We developed a foraminifera-based transfer function using a modern training set of 36 samples and 23 species. The strong relationship between observed and predicted values (r 2 jack = 0.7) indicated that foraminiferal distribution is primarily controlled by elevation with respect to the tidal frame and precise reconstructions of former sea level are possible (RMSEP jack = 0.07 m). The application of the transfer function to a short salt-marsh core (0.32 m) allowed the reconstruction of former sea levels, which were placed in a chronological framework using short-lived radionuclides ( 210 Pb and 137 Cs). The agreement between the foraminifera-based sea level curve and the Brest tide-gauge record confirms the reliability of transfer function estimates and the validity of this methodology to extend sea level reconstructions back into the pre-instrumental period. Both instrumental and microfossil records suggest an acceleration of sea level rise during the 20th century." @default.
- W1963846006 created "2016-06-24" @default.
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- W1963846006 date "2011-01-01" @default.
- W1963846006 modified "2023-09-27" @default.
- W1963846006 title "The application of foraminifera to reconstruct the rate of 20th century sea level rise, Morbihan Golfe, Brittany, France" @default.
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- W1963846006 doi "https://doi.org/10.1016/j.yqres.2010.07.017" @default.
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