Foraminifera are single-celled protists with shells, found in all marine environments, where they may be planktic or benthic in mode of life. Although a species (Syringammina fragilissima), is known to form a structure of up to 20 cm across, most foraminifera are actually small and microscopic.
Their shells are also referred to as tests because in some forms the protoplasm covers the exterior of the shell. The shells are commonly divided into chambers which are added during growth, though the simplest forms are open tubes or hollow spheres. Depending on the species, the shell may be made of organic compounds, sand grains and other particles cemented together, or crystalline calcite.
Foraminifera have a geological range from the earliest Cambrian to the present day. So they have been utilized for biostratigraphy for many years, and they have also proven invaluable in palaeoenvironmental reconstructions, and most recently for palaeoceanographical and palaeoclimatological purposes.
Photo credit: ©Frederic Labaune | Locality: unknown