2019
DOI: 10.1016/j.quageo.2018.12.002
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Marine radiocarbon reservoir age of the coralline intertidal alga Lithophyllum byssoides in the Mediterranean

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Cited by 10 publications
(12 citation statements)
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“…Consequently, the analysed data were corrected for MRE by means of the study of samples of known age from museum collections. Samples of pre-bomb intertidal alga L. byssoides from the Adriatic revealed a mean reservoir age of R(t) 318 ± 35 14 C yr and a DR (weighted mean) value of À47 ± 35 14 C yr (Faivre et al, 2019) while shells in the Adriatic reveal larger variations. Here we calibrated shell data using the Adriatic mean, i.e.…”
Section: Reservoir Agesmentioning
confidence: 98%
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“…Consequently, the analysed data were corrected for MRE by means of the study of samples of known age from museum collections. Samples of pre-bomb intertidal alga L. byssoides from the Adriatic revealed a mean reservoir age of R(t) 318 ± 35 14 C yr and a DR (weighted mean) value of À47 ± 35 14 C yr (Faivre et al, 2019) while shells in the Adriatic reveal larger variations. Here we calibrated shell data using the Adriatic mean, i.e.…”
Section: Reservoir Agesmentioning
confidence: 98%
“…The ages were calibrated with the standard MARINE13 calibration curve (Reimer et al, 2013) and the regional average marine reservoir correction (DR) for the Adriatic Sea (Faivre et al, 2015(Faivre et al, , 2019.…”
Section: Radiocarbon and Stable Isotope Analysesmentioning
confidence: 99%
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“…We employed the IntCal20 and Marine20 datasets for terrestrial and marine samples, respectively ). The regional average marine reservoir correction (ΔR) was applied for L. byssoides (ΔR of -209 ± 35 14 C yr;Faivre et al, 2019b) and for shells from the Adriatic (ΔR of -59± 117 14 C yr; Faivre et al, 2015) recalculated with Marine20 (Heaton et al, 2020). The indicative range (i.e.…”
Section: Rsl In North-eastern Adriaticmentioning
confidence: 99%
“…The first method is the most reliable for reasons stated below. It is important to emphasize, however, that it is not known if the DCP established in this manner is constant through time, as is the case with the marine reservoir effect (MRE [28,29], and references therein, [30]), although the MRE and DCP have different origins. The DCP is often used in discussion of speleothem 14 C ages [31][32][33].…”
Section: Introductionmentioning
confidence: 99%