This book deals with all parts of cave science. One of the eight chapters is "Behavior and Products of Cave Microorganisms." It covers the microbial aspects of cave manganese and iron minerals, saltpeter, and moonmilk. The biogeochemistry of iron and manganese layers in Cave of the Winds, Colorado, is elucidated by nearby iron- and manganese-depositing surface springs. The spring deposits are covered by Leptothrix slime. The heavy metals are said to be derived from granite beneath the cave's limestone. When the land surface lowered, conditions in the cave changed sequentially, so that bacterial goethite (Fe) was laid down first, then birnessite (Mn), then nonmineralized clay and silt, and finally the cave was drained. A sample of moist moonmilk from Mondmilchloch, Switzerland (type locality for the substance), grew brown, gray, and green spots, presumably from microbial contamination. The authors say that this means that the moonmilk contained soluble organic compounds derived from percolating water that provided energy for organisms such as actinomycetes that produced the moonmilk. The book proposes a new mechanism for the origin of the small size of moonmilk grains. A transmission electron micrograph from Caverns of Sonora, Texas, shows a cell at the end of one of the smallest rod-shaped grains. The authors suggest that such cells control the mineral growth, and incidentally cause the strange diagonal crystal orientation of moonmilk calcite. When the cell divides, mineral growth ceases, and subsequent enlargement is by inorganic overgrowth. The chemoautotrophic hydrogen sulfide environment at Movile Cave, Romania, is dealt with in the chapter on Habits of Cave Animals. Energy for the surprising array of troglobites in that cave is processed by Beggiatoa in floating mats and by probable Thiobacillus in the water column. The authors offer a speculative equation for energy conversion in which hydrogen sulfide combines with carbon dioxide and oxygen to produce sulfuric acid and carbohydrate. This 176-page book, illustrated with splendid etchings by John Schoenherr (himself a speleologist) is an exemplary introduction.