Publications des scientifiques de l'IRD

Soulet G., Maestrati P., Gofas S., Bayon G., Dewilde F., Labonne Maylis, Dennielou B., Ferraton F., Siani G. (2023). Marine reservoir ages for coastal West Africa. Geochronology, 5 (2), p. 345-359.

Titre du document
Marine reservoir ages for coastal West Africa
Année de publication
2023
Type de document
Article référencé dans le Web of Science WOS:001161796100001
Auteurs
Soulet G., Maestrati P., Gofas S., Bayon G., Dewilde F., Labonne Maylis, Dennielou B., Ferraton F., Siani G.
Source
Geochronology, 2023, 5 (2), p. 345-359
We measured the 14C age of pre-bomb suspension-feeding bivalves of known age from coastal West Africa across a latitudinal transect extending from 33 circle N to 15 circle S. The specimens are from collections belonging to the Museum National d'Histoire Naturelle (Paris, France). They were carefully chosen to ensure that the specimens were collected alive or that they died not long before collection. From the 14C dating of the known-age bivalves, we calculated the marine reservoir age (as Delta R and R values) for each specimen. Delta R values were calculated relative to the Marine20 calibration curve, and the R values were calculated relative to Intcal20 or SHcal20 calibration curves. Except for five outliers, the Delta R and R values were generally homogenous with weighted mean values of -72 +/- 42 14C years (1 SD, n=24) and 406 +/- 56 14C years (1 SD, n=24) respectively. These values are typical of low-latitude marine reservoir age values. Five suspension-feeding species living in five different ecological habitats were studied. For localities where several species were available, the results yielded similar results whatever the species considered, suggesting that, in these locations, the habitat has only a limited impact on marine reservoir age reconstruction. We show that our measured marine reservoir ages follow the declining trend of the global marine reservoir age starting ca. 1900 CE, suggesting that the marine reservoir age of coastal West Africa is driven, at least to the first order, by the atmospheric CO2 14C ageing due to fossil fuel burning rather than by local effects. Each outlier was discussed. Local upwelling conditions or sub-fossil specimens may explain the older 14C age and thus the larger marine reservoir ages for these samples. Bucardium ringens might not be the best choice for marine reservoir age reconstructions.
Plan de classement
Sciences du milieu [021] ; Limnologie physique / Océanographie physique [032] ; Géologie et formations superficielles [064]
Description Géographique
ATLANTIQUE ; MAURITANIE ; SENEGAL ; GUINEE ; SIERRA LEONE ; COTE D'IVOIRE ; BENIN ; GABON ; CONGO ; AFRIQUE DE L'OUEST
Localisation
Fonds IRD [F B010089560]
Identifiant IRD
fdi:010089560
Contact
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    IRD - Délégation régionale Île-de-France & Ouest
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