『Abstract
　Calcitic speleothems from a cave located on the north central coast of Grand Cayman commonly include corrosion surfaces that developed when calcite precipitation ceased and corrosion mediated by condensates became the operative process. Dissolution features associated with these surfaces, including etched crystal surfaces, microcavities, and solution-widended boundaries between crystals, are commonly occupied by microbes and microbial mats that have been replaced by calcium phosphate and/or coated with calcium phosphate. No mineralized microbes were found in the calcite crystals that form the speleothems. The morphology of the mineralized hyphae (eight morphotypes) and spores (nine morphotypes) are indicative of actinomycetes, a group of microbes that are ideally adapted to life in oligotrophic cave environs. Superb preservation of the delicate hyphae, aerial hyphae, and delicate ornamentation on the hyphae and spores indicate that the microbes underwent rapid mineralized while close to their original life positions. Although these actinomycetes were extremely susceptible to replacement by calcium phosphate, there is no evidence that they directly or indirectly controlled precipitation. Nevertheless, the association between the P-rich precipitates and microbes shows that the use of phosphorus as a proxy for seasonal climate change in paleoclimate analyses must be treated with caution.

Keywords: Actinomycetes; Phosphates; Speleothems; Microbes』

1. Introduction
2. Setting
3. Methodology
4. Results
　4.1. General features of the speleothems
　4.2. Microbes
　　4.2.1. Preservation
　　4.2.2. Morphotypes
　　4.2.3. Taxonomic affinities
　4.3. Phosphorus-rich precipitates
　　4.3.1. Distribution
　　4.3.2. Composition
　　4.3.3. Distribution
5. Discussion
6. Conclusions
Acknowledgements
References