CAVES IN CAVES: POST-DEPOSITIONAL HOLES IN SPELEOTHEMS

Calcitic stalagmites when viewed in lengthwise axial section, show two kinds of holes. Some (“axial holes”) were formed syngenetically as is shown by the depression of growth layers into the holes and the persistence of the axial hole over many cm of the growth history. Some cut the active growth surface of the stalagmite. “Off-axis holes” are seen in many stalagmites (as well as stalactites); they cut discordantly through growth layers, and never terminate at a growth surface. They range in size from a few mm to several cm in maximum dimension, and may not be coaxially oriented. They are lined with micron-sized, randomly oriented calcite crystals and under which lies an organic-rich coating. Computerized tomographic X-ray (CT) scans reveal abundant off-axis holes in some speleothems, while most display at least a few holes. Magnetic resonance imaging shows that, in uncut speleothems, these holes never contain water (although Genty et al. [2002] found water-filled holes in some stalagmites). Off-axis holes may be a result of bioerosion, possibly bacterial, followed by partial refilling of the hole with calcite which is prevented from growing epitaxially on the host calcite.