2018
DOI: 10.1017/rdc.2017.118
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Reservoir Ages in the Western Tropical North Atlantic from One Coral off Martinique Island (Lesser Antilles)

Abstract: Sea surface reservoir ages (R) are reported from radiocarbon (14C) measurements of the annual growth bands of coral Siderastrea siderea collected on the Atlantic coast off Martinique Island, in the Lesser Antilles volcanic arc. Mean values of R are similar between 1835 and 1845 during pre-anthropogenic times at 385±30 yr and between 1895 and 1905 at 382±20 yr when there was a huge eruption from the Montagne Pelée volcano in 1902–1903. Limited 14C aging of sea surface (~40 yr) may be due to enhanced volcanic ac… Show more

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Cited by 4 publications
(7 citation statements)
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“… Age model established for event deposits free core (hemipelagic section depleted from event deposits) with Oxcal 4.4 program (Bronk Ramsey, 2009) by using the Marine 20 calibration curve (Heaton et al., 2020), the recalculated reservoir age Δ R value recalculated from Paterne et al. (2018) and a k parameter of 1. Modeled radiocarbon ages are indicated in red and the turbidite age distributions are in black, both with the mean and standard deviation, Dark gray interpolated interval: 1‐sigma probability (68.3%), light gray interpolated interval: 2‐sigma (95.4%).…”
Section: Resultsmentioning
confidence: 99%
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“… Age model established for event deposits free core (hemipelagic section depleted from event deposits) with Oxcal 4.4 program (Bronk Ramsey, 2009) by using the Marine 20 calibration curve (Heaton et al., 2020), the recalculated reservoir age Δ R value recalculated from Paterne et al. (2018) and a k parameter of 1. Modeled radiocarbon ages are indicated in red and the turbidite age distributions are in black, both with the mean and standard deviation, Dark gray interpolated interval: 1‐sigma probability (68.3%), light gray interpolated interval: 2‐sigma (95.4%).…”
Section: Resultsmentioning
confidence: 99%
“…The radiocarbon ages were calibrated with the OxCal 4.4 software (Bronk Ramsey, 2009) using the IntCal Marine20 calibration curve (Heaton et al., 2020), and the regional offset Δ R value of −156 ± 32 years, recalculated from Paterne et al. (2018) for the MARINE20 curve (with CALIB REV8.2 software, Stuiver et al., 2021). Then, we used a Bayesian model with a P‐sequence deposition model in OxCal (Poisson distribution, Bronk Ramsey, 2008; Bronk Ramsey & Lee, 2013) to construct an age‐depth model of event‐free sediment sections, which we built for each core by removing all instantaneous event deposits.…”
Section: Methodsmentioning
confidence: 99%
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