Speleothems are usually considered to be closed systems, as there is limited exchange of uranium and thorium with the cave environment. In some cases, speleothems may act as a more open system (introducing uncertainty into U-Th dating) when the speleothems have undergone dissolution or if the cave environment is in constant flux. It’s best to choose speleothem samples from deeper within the cave where the environment is more stable, as well as speleothems with a pristine structure that does not show any signs of dissolution.
Corals represent closed systems in most cases. Uranium is integrated into the coral structure from the seawater during coral growth and further uranium exchange with the seawater does not generally occur after growth. Coral surfaces do not contain thorium, thus any Th measured would be a result of decay. The stability of both uranium and thorium in coral structures demonstrate that living corals exist within an essentially closed system.
However, deep in time, recrystallization (regrowth) can occur during periods of low sea-level, which leads to potential uranium loss from the coral structure and age biases in the U-Th date. Any potential recrystallization should be analysed and considered prior to U-Th dating (and completed via XRD). Broadly, a comparison of uranium content between fossil coral and modern counterpart corals (nearest living relative) can provide some information as to whether the fossil existed in a closed or open system.
Lakes have high quantities of carbonates available in sediment cores, however U-Th dating remains difficult in these environments due to the introduction of thorium into the partially open system (usually via detrital material). This can potentially be corrected for by measuring 230Th/232Th to estimate the quantity of detrital material (see Chen et al. 2020 for details). Furthermore, mollusc shells and foraminifera found within sediment cores have been shown to exchange uranium after deposition, challenging the use of U-Th dating in this context.
Bones represent open systems, which means that any U-Th age that is calculated will always provide a minimum age possible for the bone (terminus post quem). The age could be similar to the age of the death of the fossil if the uptake occurred very soon after the death of the organism. However, in the case of a delayed uptake, the fossil will be older than the calculated U-Th date. While it is difficult to assess the level of openness of a bone sample, there are techniques which may be used to approximate the level of potential date offset. For example, you may sample the bone at various points to provide evidence as to how the U-Th ratio varies from a point of high contact (bone edges) to points of low contact (bone interiors) with the exterior environment (Grün et al. 2014).
Optimal samples for U-Th dating
The most optimal samples for accurate U-Th dating are those that exist in closed systems, including speleothems and corals. In some cases, bones and lake sediments may also be used, but the state of your samples should be carefully considered prior to planning your analysis and interpreting U-Th dating results. We recommend contacting the lab directly before sending your samples for analysis.
Chen, C.Y., McGee, D., Woods, A., Pérez, L., Hatfield, R.G., Edwards, R.L., Cheng, H., Valero-Garcés, B.L., Lehmann, S.B., Stoner, J.S. and Schwalb, A., 2020. U-Th dating of lake sediments: Lessons from the 700 ka sediment record of Lake Junín, Peru. Quaternary Science Reviews, 244, p.106422.
Grün, R., Eggins, S., Kinsley, L., Moseley, H. and Sambridge, M., 2014. Laser ablation U-series analysis of fossil bones and teeth. Palaeogeography, Palaeoclimatology, Palaeoecology, 416, pp.150-167.