diglyceridit

Diglyceridit is a hypothetical mineral species described in some mineralogical discussions as an organic–inorganic hybrid. The name is derived from diglyceride, reflecting proposed organic ligands that, in these descriptions, might accompany an inorganic framework. Because no authenticated specimens are publicly documented, diglyceridit remains a speculative entry rather than a confirmed mineral.

Composition and structure are described in provisional terms. In these accounts, diglyceridit is envisioned as consisting of layers of metal cations coordinated to inorganic anions, with interlayer organic diglyceride‑like ligands occupying space between sheets. The exact formula and crystal structure are not established, and suggested models emphasize variability and dependence on environmental conditions during hypothetical formation.

Occurrence and geology are likewise speculative. Proposals place diglyceridit in environments where organic-rich fluids interact with minerals containing metal cations, such as sedimentary or hydrothermal settings. However, there are no verified field localities or sample collections associated with the mineral in current, publicly accessible records.

Physical properties and identification are described in broad terms. If diglyceridit existed, it might be relatively soft and could exhibit a sheet‑like habit with a color range from colorless to pale hues, influenced by the organic content. Optical properties, hardness, and density are not established due to the absence of verified material.

Etymology and taxonomy reflect its proposed organic–inorganic character. The name points to a conceptual link with diglycerides, while its taxonomic status would depend on future verification and acceptance by the mineralogical community. At present, diglyceridit is regarded as hypothetical and not part of an established mineral catalog.