(Supplement Table S2) Results of 230Th/U-dating
We compared the suitability of two skeletal materials of the Atlantic brain coral Diploria strigosa for 230Th/U-dating: the commonly used bulk material comprising all skeletal elements and the denser theca wall material. Eight fossil corals of presumably Last Interglacial age from Bonaire, southern Caribbean Sea, were investigated, and several sub-samples were dated from each coral. For four corals, both the ages and the activity ratios of the bulk material and theca wall agree within uncertainty. Three corals show significantly older ages for their bulk material than for their theca wall mate... Mehr ...
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Dokumenttyp: | Dataset |
Erscheinungsdatum: | 2016 |
Verlag/Hrsg.: |
PANGAEA
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Schlagwörter: | AGE / 230Th/U Thorium-Uranium / standard deviation / BON-12-A / BON-13-AI.1 / BON-17-AI / BON-24-AII.2 / BON-26-A / BON-28-AI / BON-33-BI.2 / BON-5-A / Bonaire / Caribbean Netherlands / Center for Marine Environmental Sciences / Comment / DRILL / Drilling/drill rig / Event label / Group / Hand drill / HDRILL / MARUM / Multi-collector inductively coupled plasma mass spectrometer (MC-ICP-MS) / Thorium-230/Uranium-238 activity ratio / Thorium-232 / Thorium-232/Uranium-238 activity ratio / Uranium-234/Uranium-238 activity ratio / Uranium-238 |
Sprache: | Englisch |
Permalink: | https://search.fid-benelux.de/Record/base-28770028 |
Datenquelle: | BASE; Originalkatalog |
Powered By: | BASE |
Link(s) : | https://doi.pangaea.de/10.1594/PANGAEA.858209 |
We compared the suitability of two skeletal materials of the Atlantic brain coral Diploria strigosa for 230Th/U-dating: the commonly used bulk material comprising all skeletal elements and the denser theca wall material. Eight fossil corals of presumably Last Interglacial age from Bonaire, southern Caribbean Sea, were investigated, and several sub-samples were dated from each coral. For four corals, both the ages and the activity ratios of the bulk material and theca wall agree within uncertainty. Three corals show significantly older ages for their bulk material than for their theca wall material as well as substantially elevated 232Th content and (230Th/238U) ratios. The bulk material samples of another coral show younger ages and lower (230Th/238U) ratios than the corresponding theca wall samples. This coral also contains a considerable amount of 232Th. The application of the available open-system models developed to account for post-depositional diagenetic effects in corals shows that none of the models can successfully be applied to the Bonaire corals. The most likely explanation for this observation is that the assumptions of the models are not fulfilled by our data set. Comparison of the theca wall and bulk material data enables us to obtain information about the open-system processes that affected the corals. The corals showing apparently older ages for their bulk material were probably affected by contamination with a secondary (detrital) phase. The most likely source of the detrital material is carbonate sand. The higher (230Th/232Th) ratio of this material implies that detrital contamination would have a much stronger impact on the ages than a contaminant with a bulk Earth (230Th/232Th) ratio and that the threshold for the commonly applied 232Th reliability criterion would be much lower than the generally used value of 1 ng g^-1. The coral showing apparently younger ages for its bulk material was probably influenced by more than one diagenetic process. A potential scenario is a combination of detrital ...