This paper presents new U-Th ages obtained by LA-MC-CP-MS (laser ablation -multicollector -inductively coupled plasma -mass spectrometry) on coral samples from a sedimentary core of the Tunis lagoon. The ages and calculated ( 234 U/ 238 U) 0 initial ratios, similar to the seawater value for most corals demonstrate that they behaved as closed systems, or with only a very limited loss of 234 U and 230 Th. The ages (from 196 to 182 ka) show that the coral-rich sediments were deposited near the end of isotope stage 7. The precision on the dates is comparable to those of alpha-spectrometry (around 7.6% on average), but the possibility of multiple in-situ analyses offers other advantages. An example is provided by the very unusual open-system behaviour found in the outer Mg-calcite border of a coral branch, formed by a coralline red alga. The very high ( 234 U/ 238 U) and ( 230 Th/ 238 U) activity ratios (1.41 and 2.04, respectively) are tentatively explained using the model proposed by Thompson et al. [2003], that involves continuous enrichment of 234 Th ( 234 U) and 230 Th recoil nuclei provided by an U-enriched source. We suggest that this source might come from the bio-mineral itself, in the form of organic matter originally involved in the encrusting algal activity, and eventually degraded with an almost complete U-loss.