Isolated domains in apparently pristine speleothems can show open system behavior.
“Cryptic” diagenesis with very localized U-loss is observed in a Holocene speleothem.
Misinterpretation of U-Th age estimates in such samples can only be eliminated based on multi-aliquot age determinations.
Micro-CT scans recorded a limited number of voids in otherwise dense speleothem.