A time-course Raman spectroscopic analysis of spontaneous in vitro microcalcifications in a breast cancer cell line
Laboratory Investigation (2021) 101:1267–1280
https://doi.org/10.1038/s41374-021-00619-0
ARTICLE
A time-course Raman spectroscopic analysis of spontaneous in vitro
microcalcifications in a breast cancer cell line
Pascaline Bouzy 1 Shane O’Grady2 Honey Madupalli3 Mary Tecklenburg3 Keith Rogers4
Francesca Palombo1 Maria P. Morgan 2 Nicholas Stone 1
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Received: 18 February 2021 / Revised: 17 May 2021 / Accepted: 17 May 2021 / Published online: 11 June 2021
© The Author(s) 2021. This article is published with open access
Abstract
Microcalcifications are early markers of breast cancer and can provide valuable prognostic information to support clinical
decision-making. Current detection of calcifications in breast tissue is based on X-ray mammography, which involves the use of
ionizing radiation with potentially detrimental effects, or MRI scans, which have limited spatial resolution. Additionally, these
techniques are not capable of discriminating between microcalcifications from benign and malignant lesions. Several studies show
that vibrational spectroscopic techniques are capable of discriminating and classifying breast lesions, with a pathology grade
based on the chemical composition of the microcalcifications. However, the occurrence of microcalcifications in the breast and
the underlying mineralization process are still not fully understood. Using a previously established model of in vitro
mineralization, the MDA-MB-231 human breast cancer cell line was induced using two osteogenic agents, inorganic phosphate
(Pi) and β-glycerophosphate (βG), and direct monitoring of the mineralization process was conducted using Raman microspectroscopy. MDA-MB-231 cells cultured in a medium supplemented with Pi presented more rapid mineralization (by day 3)
than cells exposed to βG (by day 11). A redshift of the phosphate stretching peak for cells supplemented with βG revealed the
presence of different precursor phases (octacalcium phosphate) during apatite crystal formation. These results demonstrate that
Raman micro-spectroscopy is a powerful tool for nondestructive analysis of mineral species and can provide valuable information
for evaluating mineralization dynamics and any associated breast cancer progression, if utilized in pathological samples.
Introduction
In 2018, breast cancer was one of the most commonly diagnosed types of cancer and the second cause of death from
Supplementary information The online version contains
supplementary material available at https://doi.org/10.1038/s41374021-00619-0.
* Nicholas Stone
1
School of Physics and Astronomy, University of Exeter,
Exeter, UK
2
School of Pharmacy and Biomolecular Science, Royal College of
Surgeons in Ireland, Dublin, 2, Ireland
3
Department of Chemistry and Biochemistry and Science of
Advanced Materials Program, Central Michigan University,
Mt. Pleasant, MI, USA
4
Cranfield Forensic Institute, Cranfield University,
Shrivenham, UK
cancer worldwide (after lung cancer) [1]. Around 2.1 million
women across the world were diagnosed with breast cancer in
2018 [1] with survival rates which are predicted to increase
over the next decades, mainly due to changes in detection
practice by screening individuals more often and earlier [2].
Early-stage diagnosis is important to improve the survival rate
and treatment response, and in this context microcalcifications
appear to be the most valuable marker of breast cancer [3]. Xray and vibrational spectroscopy techniques are widely used to
investigate the composition of these crystals [4–9]. For
instance, it has already been shown that type I microcalcifications are composed of calcium oxalate dihydrate and are
observed only in benign lesions, whilst type II microcalcifications are mainly composed of calcium hydroxyapatite (Hap)
and are associated with both proliferative benign lesions and
malignant lesions [10]. Moreover, in biological tissue, the Hap
crystal is not found in its stoichiometric form as the lattice
contains carbonates (CO32− ions) which reduce the stability of
the crystal and increase its solubility [11–13] with detrimental
effects. Two types of substitution are found in the Hap lattice:
type A, in which carbonate replaces a hydroxyl ion (OH−), and
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P. Bouzy et al.
Fig. 1 Experimental design
and specific Raman features of
mineralization. a Protocol used
for 14-days mineralization of
MDA-MB-231 cells (left panel).
Acronyms denote OC
osteogenic cocktail, Dex
dexamethasone, Pi inorganic
phosphate, DMEM Dulbecco’s
modified Eagle medium, βG βglycerophosphate, AA ascorbic
acid. Representative images of
MDA-MB-231 cells growing at
different time point of
mineralization (Day 3, 7, 11, and
14) (right panel). Scale bar: 20
µm and ×100 magnification. b
Raman spectra acquired from
mineral deposits in cell culture
after 3 days and c 11 days of
mineralization. Labels denote
Phe Phenylalanine, Cys
Cysteine, Tyr Tyrosine. Cells
were treated with Pi + Dex (blue
line) and OC + Dex (or βG)
(green line). Non-treated cells
were considered as control (red
line). Each spectrum is an
average of 40 spectra for each
condition.
type B, where carbonate replaces a phosphate ion (PO43−) [14].
Baker et al. have previously demonstrated using FTIR microspectroscopy that the extent of carbonate substitution within
breast microcalcifications directly correlates with the degree of
pathology [5], a finding that is in line with results of other
Raman studies [4, 5, 15]. However, further analysis shows that
the calcification’s chemical composition is more complex and
suggests the presence of a close interplay between microcalcifications and their microenvironments, potentially affecting
both formation and maturation of the crystals.
It is known that the regulation of tumor pH plays an
important role in cell proliferation and cancer progression.
Several studies have shown that cells within a tumor
experience hypoxia and upregulation of metabolic
A time-course Raman spectroscopic analysis of spontaneous in vitro microcalcifications in a breast. . .
processes. Changes in metabolic activity lead to an increase
of intracellular concentrations of H+ hydrogen ions and
carbon dioxide, which are then released (via different
transporters) into the microenvironment causing a decrease
of pH [16] and promoting breast cancer progression [17].
The acidic tumor microenvironment can give rise to different precursors in microcalcifications [18]. In addition,
recent studies suggest that microcalcifications may contain
other mineral phases such as magnesium-substituted β-tricalcium phosphate (β-TCP or whitlockite) [15, 19].
In this study, we hypothesized that, in addition to the calcium Hap, different phosphate species as mineral precursors
(e.g. octacalcium phosphate (OCP) or amorphous calcium
phosphate (ACP)) could be found in the calcium deposits [20].
To gain an insight into the crystal formation process, we
evaluated two different pathways of cell mineralization
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