SENSITIVITY OF VARIOUS METHODS OF MEASURING THECA VOLUME IN BLASTOIDS
Simple displacement of water by the specimen in a graduated cylinder was fast and inexpensive, but had low precision and repeatability. This method was particularly poor at measuring small volumes. Calculating volume by dividing the mass of specimens by the density of calcite was fast, extremely precise, very repeatable, but has moderate up front costs of an analytical balance. This method was particularly effective when measuring extremely small specimens but concerns arise where potentially incomplete infilling of the theca by calcite, or other minerals of different densities, may become problematic. Estimating volume by measuring the mass of water displaced by immersed specimens was somewhat time consuming, reasonably precise, very repeatable, but has moderate up front costs of an analytical balance. This method works well on large specimens even if they are incompletely in filled or of mixed mineralogy, but becomes less repeatable at small sizes because of the nature of the apparatus and the potential of surface bubbles on all specimens. Measuring volume with a 3-D laser scanner was very time consuming, but had high precision and repeatability at large sizes, but was poor at measuring small volumes because of the limitations of the scanner resolution. This method has very high up front costs because of price of the scanner and associated desktop computer.