Tiny (50-200 nm) spheroids were first discovered by Folk through SEM work on the hot springs of Viterbo Italy. He termed these small, spherical structures "nannobacteria, " and proposed that they may be important agents in precipitation of CaCO 3 , as needle-like crystals of the mineral aragonite, and as bundles of such needle-like crystals (termed "fuzzy dumbbells"), or as elongated crystals of the mineral calcite [1].During the past 15 years, nanometer-scale spheroids have been discovered in the geological, medical, and astronomical worlds. There can be no doubt as to their existence, but their significance and origin remain a subject of continuing controversy. Even the spelling ("nanno-"), which has been the standard in biology, geology, and paleontology going back to the 19 th century, has been questioned. Whether or not they are truly bacteria or any form of life has been a subject of heated debate. At one end of the spectrum are claims that they are a minute form of microbial life (bacteria or archaea) because they are culturable organisms with distinct cell walls/membranes that stain (+) for DNA. Other workers suggest that they are membrane vesicles blebbing off of the cell walls of "normal" bacteria. Another view is that they represent inchoate mineral nuclei formed either in the presence of bacterial slime (EPS) or in other organic-rich milieus. A key argument of opponents to the concept of very small bacteria is that a minimum volume of 200 nm 3 is thought to be needed to hold all the molecules essential for life functions [2]. These debates have motivated years of research. If nothing else, we have learned that when trying to answer questions at the nanometer scale, careful sample preparation is essential. Unfortunately, during preparation of samples for SEM, spherical nannobacteria-like artifacts can be produced by gold coating for more than 60 seconds. Therefore, we coat our samples for no more than 30 seconds to avoid creation of spherical artifacts [3]. Unfortunately, sub-spherical, nannobacteria-like features can also be produced by acid-etching of purely inorganic minerals [4]. Therefore, we strive to imageonly freshly broken surfaces and we use acid only to prepare samples when we can compare an acid-etched surface to a freshly broken surface. Trials of different dehydration methods (air drying, air drying under vacuum, sequential ethyl alcohol solutions, with HMDS, or critical point drying) also resulted in significant, visible differences in the appearance of the dehydrated biofilm, particularly at the nanometer scale, including tiny, spherical artifacts [5]. Dehydration in acetone produced the best-preserved biofilm structure for our TEM sections. Finally, experiments in which bacterial cultures were lysed and then air-dried resulted in formation of bacterial debris containing nanometer-scale textures [4].With the remains of lysed bacteria in mind, we established criteria for distinguishing nannobacteria from nanometer-scale textures in fine-scale organic debris. In SEM, nannobacteria appear...