With mammography, breast microcalcifications can be classified according to their distribution, size and morphology. Chemically, these can be divided into 2 subtypes: type I, which are mostly associated with benign breast conditions, and type II, which are found in both malignant and benign lesions, including DCIS. Type II calcifications consist mainly of a calcium phosphate called hydroxyapatite (HAP), although other calcium phosphate phases have been linked to malignant breast cancer, including octacalcium phosphate (OCP).
By combining multiple analytic techniques – X-ray diffraction, scanning electron microscopy, and Raman and Fourier-transform infrared spectroscopy – we were able to capture unique additional information about these minerals, including their different crystallographic and chemical properties, and their importance in breast cancer progression.
For example, the spatial distribution of the different mineral phases of calcium phosphate in DCIS had not previously been investigated. In our study, we found a general distribution pattern of these phases across the DCIS calcification, suggesting the mineralisation process advances inwards – beginning with OCP at the calcification edge and progressing to crystalline, low-carbon content HAP as the dominant mineral in the core. This finding prompts questions regarding the role of calcium phosphate precursors that form during this process.
Interestingly, when vibrational spectroscopy is used to study the interaction of minerals and proteins across the microcalcification and into the surrounding tissue, we saw a similar differential pattern of distribution. This was important to explore, because the expression of collagen and proteins linked to bone formation has been shown to influence the size and shape of breast calcifications, promote or inhibit the nucleation and growth of minerals, and potentially influence DCIS progression. Lower amounts of protein within the calcification core support our hypothesis of more mature mineralization in this region, whereas at the edges we saw higher levels of interaction between OCP and collagen, with the collagen’s structure becoming dysregulated further into the connective tissue surrounding the calcification. Our findings highlight numerous changes in the density, stiffness and mechanical properties of the matrix surrounding microcalcifications, which may potentially contribute to the development and progression of cancer.
Collectively, our findings pinpoint novel features within DCIS breast calcifications, such as the gradient of mineralisation and collagen formation, which may be indicative of the DCIS state and overall risk of progression to invasive breast cancer. These features will be further examined in cases of DCIS that progressed to invasive cancer compared with DCIS that remained relatively harmless.