Caves in caves: Evolution of post-depositional macroholes in stalagmites

In a previous paper (Shtober-Zisu et al., 2012) we described millimeter to centimetersized fluid-free holes within the interiors of stalagmites of widely varying origin. We present here further observations of this phenomenon, using X-ray tomography, macroscopic and microscopic observation of sections of twenty-six stalagmites from various sites in North America and the Caribbean region. We can distinguish three types of cavities in speleothems: primary μm-sized fluid inclusions; mm to cm sized holes, aligned along the stalagmite growth axis which are clearly syngenetic; and μm to cm-sized holes away from the growth axis ("offaxis holes or OAHs") deeply buried inside their host stalagmites, and cutting primary growth layers. Neither axial nor off axis holes contain fluid today. Off-axis holes appear to have been formed by internal corrosion of the calcite host, possibly enhanced by the action of bacteria which were sustained by permeation of through the body of the stalagmite of water containing dissolved organic species. A modern stalagmite from Israel is shown to contain bacteria associated with active hole formation.