Pascaline
Bouzy
a,
Iain D.
Lyburn
bc,
Sarah E.
Pinder
d,
Robert
Scott
b,
Jessica
Mansfield
a,
Julian
Moger
a,
Charlene
Greenwood
e,
Ihssane
Bouybayoune
d,
Eleanor
Cornford
c,
Keith
Rogers
b and
Nick
Stone
*ac
aSchool of Physics and Astronomy, University of Exeter, Exeter, UK. E-mail: N.Stone@exeter.ac.uk
bCranfield Forensic Institute, Cranfield University, Shrivenham, UK
cGloucestershire Hospitals NHS Foundation Trust, UK
dKing's College London, Comprehensive Cancer Centre at Guy's Hospital, London, UK
eSchool of Chemical and Physical Sciences, Keele University, Keele, Staffordshire, UK
First published on 21st February 2023
Microcalcifications play an important role in cancer detection. They are evaluated by their radiological and histological characteristics but it is challenging to find a link between their morphology, their composition and the nature of a specific type of breast lesion. Whilst there are some mammographic features that are either typically benign or typically malignant often the appearances are indeterminate. Here, we explore a large range of vibrational spectroscopic and multiphoton imaging techniques in order to gain more information about the composition of the microcalcifications. For the first time, we validated the presence of carbonate ions in the microcalcifications by O-PTIR and Raman spectroscopy at the same time, the same location and the same high resolution (0.5 μm). Furthermore, the use of multiphoton imaging allowed us to create stimulated Raman histology (SRH) images which mimic histological images with all chemical information. In conclusion, we established a protocol for efficiently analysing the microcalcifications by iteratively refining the area of interest.
However, the formation of BMCs and their possible role in cancer are still not fully understood even if many theories are found in the literature.17–21 Furthermore, there is a lack of information about their chemical composition, distribution, morphology, and relationship with surrounding soft tissues.
Scanning electron microscopy (SEM) has highlighted a range of different morphologies but also a heterogeneity within the structure of BMCs.8,22 For instance, several studies have shown that some pathological calcifications exhibited concentric ring structures. Gaining chemical information about these structures could help to understand the formation of the pathological calcifications. In this context, it is fundamental to use different microscopic techniques in order to correlate the morphology, the chemical composition and the breast pathology.22,23
Vibrational spectroscopy (Fourier Transform Infrared (FTIR) and Raman spectroscopy) has been used for biological and clinical evaluation for several decades, applied to cells, biofluids and tissue sections.24–27 It has also been recognised as a powerful tool for identifying BMCs in breast tissues as well as their biochemical composition.4,13,28–32
These vibrational spectroscopic tools offer many advantages but also some challenges when applied to breast tissue sections. The traditional FTIR systems have a Mercury Cadmium Telluride (MCT) detector, which covers a large spectral range (∼3900–800 cm−1), collecting the information regarding lipids, proteins, and mineral content. Unfortunately, these FTIR systems have a very low spatial resolution, due to the diffraction limit of the technique, 1000 cm−1 being equivalent to a wavelength of 10 μm.
There are some alternatives to improve the spatial resolution of IR such attenuated total reflectance (ATR) FTIR spectroscopy. However, this approach needs a close contact between the sample and an ATR crystal, which has potential to cause sample damage. It can result in a resolution improvement, dependent on the refractive index of the crystal, e.g. 4 for germanium, reducing the spectral resolution achievable from 5–12 μm to 1.2–3 μm for mid-IR.
In FTIR, the signal-to-noise ratio of the data in the long wavelength region can be impacted by the attenuation from substrates, system optics and the calcification itself, which is highly absorbing compared to biological tissues of the same thickness. Sometimes, the microcalcification size is smaller than the FTIR system can resolve.33 In addition, the quality of the data is dependent on the sample preparation i.e., a saturation of the IR signal can be caused by a thickness of only a few microns of highly absorbing phosphate rich mineral.
Raman spectroscopy provides more flexibility in terms of sample preparation and analysis, i.e., liquid or powder samples, or thick tissue samples, as well as an order of magnitude improvement in spatial resolution, with diffraction limited resolution of between 500 and 1000 nm. However, Raman scattering cross-sections are relatively low and intense laser light is required to provide sufficient signals in reasonable timescales. This can lead to the risk that the laser can induce burning due to paraffin residues, ink or the calcifications themselves. This phenomenon is not generally observed with NIR excitation wavelengths in the majority of biological tissues,34,35 but appears to be feasible, particularly with 785 nm laser.
In addition to the traditional FTIR and Raman spectroscopy techniques, a new technique has emerged in the literature, which is Photothermal Infrared (PTIR) spectroscopy.36,37 This technique is based on utilising the photothermal effect, induced by a tuneable mid-IR laser, and allows the user to achieve as small as nanoscale resolution. This was first demonstrated with the use of atomic force microscopic (AFM) tips being used to measure the thermoelastic expansion of the sample when a tuneable IR laser source matches the absorption frequency/wavelength of the material. Note that while, the lateral resolution of an O-PTIR microscope is equal to 500 nm, the lateral resolution of an AFM-IR microscope is around 50 nm.38,39
More recently the technique of optical photothermal infrared (O-PTIR) spectroscopy has been developed, which measures the photothermal response of the sample to pulses of single frequency mid-IR radiation.40 The thermoelastic expansion following the resonant absorption leads to a change in the local refractive index of the sample. The photothermal response is detected by a non-destructive visible or NIR laser probe which determines the spatial resolution of the measurement. This results in a submicron spatial resolution (around 500 nm vs. 5–12 μm of FTIR)41,42 without requiring any contact with the sample, reducing the potentially for sample damage.43
The photothermal system offers other advantages; using a series of quantum cascade lasers (QCL), which are significantly brighter sources than a Globar thermal source, to cover the entire fingerprint region (1800–800 cm−1). QCLs are also rapidly tuneable to a specific wavelength of interest, enabling relatively fast discrete frequency mapping to be achieved. Vibrational spectroscopy associated with QCL has emerged during the past decades and provides a rapid and highly sensitive approach.44,45 The past few years have seen several demonstrations of mid-IR imaging using QCL sources that have been applied in several studies investigating, for example, colorectal disease45 and breast cancer.46
For the first time a system is available which combines all the advantages of the previous techniques described above with a rapid and sensitive approach and a high resolution. In brief, within our system, the sample is illuminated by a pulsed mid-IR laser. When this IR laser is tuned for a specific wavenumber for a specific IR absorption, a photothermal expansion is created in the sample. These changes are detected a visible or NIR laser probe. Importantly for multi-modal analytical validation, this laser probe enables the simultaneous collection of Raman and IR spectra, at the same location and the same resolution.41,42,47
In parallel, a multimodal approach that offer a submicron resolution has been performed. First, the second harmonic generation (SHG) technique has been applied, which is well-known for imaging collagen in biological samples.48 Its application to the analysis of BMCs provides new perspectives, as the collagen seems to play a role to discriminate BMCs in different breast pathologies. In fact, as suggest by Shin et al., the level of collagen is higher in fibroadenoma rather than invasive ductal carcinoma, which both have similar carbonate level.49 Moreover, two photon fluorescence (TPF), widely used to identify mineral tissues,50,51 could help by identifying the BMCs in the breast tissue sections. Finally, stimulated Raman scattering (SRS), a non-linear optical technique, offers the ability to obtain complementary information to Raman spectroscopy as it allows imaging of biological tissues and exploration of their chemical composition with a submicron resolution.49,51 Likewise, this multimodal approach generates stimulated Raman histology (SRH) images based on the SRS images for the CH2 and CH3 bonds (2845 and 2930 cm−1, respectively) in good agreement with the H&E images.52,53 These images are created based on label-free and non-destructive techniques and could provide faster histological information when standards H&E images are not available.
The objective of this study was to investigate the potential of combined O-PTIR and Raman spectroscopy for analysing breast BMCs, their composition, and the surrounding tissues and to ascertain when this instrument adds additional value over routine vibrational spectroscopic imaging approaches. Furthermore, the complementary nature of stimulated Raman scattering (SRS) and second harmonic generation (SHG) microscopy techniques allow visualisation of the collagen network and the protein distribution in the tissue50,51 as well as within the BMC with a very good resolution.54,55 By integrating all these techniques, we aim to gain more information about BMCs in different breast pathologies.
Fig. 1 Experimental protocol used to analyse the breast tissue sections using FTIR, O-PTIR and Raman spectroscopy and multiphoton imaging. |
Prior to the spectroscopic analysis, all samples were deparaffinised using the following protocol: 3 baths of Histoclear (National Diagnostics, USA) for 5 min, following by 15 dips in isopropanol (IPA) 100% (Fisher Scientific, UK), repeated twice, then 15 dips in IPA 90%, 15 dips in IPA 70% and 15 dips in distilled water. The samples were air dried at room temperature before analysis.
Micro-Raman measurements were acquired using a Renishaw InVia confocal Raman microscope, comprising a 50× long working distance objective (N.A. 0.5) for illumination and for collection of the backscattered light, xyz motorized stage, 600 lines per mm grating and CCD camera. The excitation beam was from a diode laser source with 785 nm wavelength. Before each set of measurements, a system calibration was performed using three standards: silicon wafer, polytetrafluoroethylene (PTFE) and green glass.
Simultaneous O-PTIR and Raman measurements were carried out using a mIRage IR microscope (Photothermal Spectroscopy Corp, Santa Barbara, USA) equipped with a 40× objective (N.A. 0.78), a 4-module-pulsed QCL with a tuneable range from 1799–785 cm−1. The system is coupled with a Horiba Scientific iHR-320 spectrometer, 600 lines per mm grating and deep depletion CCD camera. The probe beam and Raman excitation light was from a diode laser source with 785 nm wavelength.
For the SRS images the tuneable beam is set to 802 nm and the delay is adjusted to excite the 2930 cm−1 vibrations, for TPF and SHG images the tuneable beam was set at 810 nm, with a 0.207 μm pixel size. All the data are collected using the Olympus Fluoview FV3000 software.
A micro-Raman map of each microcalcification in the breast tissue sections was recorded using Renishaw Streamline® mode.59 The acquisition time was 15 seconds with a step size of 1.4 μm from 350–1800 cm−1 spectral range at 1500 cm−1 centre. Raman maps were recorded using WiRE software (Renishaw PLC).
O-PTIR and Raman single spectra were acquired simultaneously at the same locations with the same spatial resolutions (∼0.5 μm). O-PTIR spectra were collected from 1796–786 cm−1, with a spectral resolution of 6.6 cm−1 at each spectral step, using 43% of the QCL power, 59% of the probe power and 16 scans per spectrum. A background spectrum was measured using a Kevley low-E substrate prior the sample acquisition. Raman spectra were collected from a 200–2055 cm−1 spectral range with the grating centred at 1200 cm−1. Before each measurement, a system calibration was performed using three standards: silicon wafer, PTFE and aspirin.
The single IR frequency images were collected in reflective mode over with a spatial resolution of around 0.5 μm for specific frequencies of interest by tuning the QCL system at 1656, 1524, 1044 and 872 cm−1 for the amide I and II, phosphate and carbonate bands.
All data was collected using the PTIR Studio 4.3 software (Spectroscopy Corp., Santa Barbara, USA).
The main advantage of the FTIR imaging system is that it consists of a large field of view (704 × 704 μm) allowing the analysis of very large images within a reasonable amount of time. In that way, it is possible to verify the presence of BMCs (based on the phosphate peak intensity) in this section, which is often very difficult to do visually as the sections are not stained. The IR image in Fig. 2b is based on the phosphate (PO42−) peak intensity (1030 cm−1) showing a good correlation with the H&E section. An example of a mean IR spectrum in Fig. 2d gives information about the composition of the BMC in terms of proteins (1656 cm−1, amide I) and mineral content (1060 cm−1, phosphate band). Unfortunately, the Agilent system does not cover the long wavelength region corresponding to the carbonate (CO32−) band at around 872 cm−1, when using the MCT focal plane array detector. The carbonate bands (1450–1415 cm−1) could be used to measure the amount of carbonate ions in the BMC but, due to possible residue of paraffin signal in this region, they should not be used alone, but in addition to those at 872 cm−1 for more accuracy. Furthermore, a saturation of the signal of the PO42− band (1060–1020 cm−1) is observed which is directly related to the sample thickness (as well as the inherent vibrational absorption cross-section).
In parallel, based on the IR and histological images, Raman maps have been acquired (Fig. 2c). This system has a greater spatial resolution than the FTIR system and allows selection of specific areas in the BMCs. It has been apparent for a few years that using Raman spectroscopy, the identification of minerals is relatively simple61–64 with the presence of the most distinct phosphate peak at 960 cm−1. The mean Raman spectrum illustrated in the Fig. 2e shows several phosphate bands at 961, 583 and 449 cm−1 corresponding to the ν1 PO42−, ν4 PO42− and ν2 PO42− bands, respectively65 and are specific for mineral species. The Raman spectrum also exhibits a ν1 CO32− band at 1072 cm−1.65 Unfortunately, the CO32− peak is a low intensity shoulder in the ν3 PO42− band. It is difficult to determine accurately the amount of carbonate in the BMCs and validate the results obtained from the FTIR spectroscopy.
The recently developed, and now commercially available, O-PTIR system (Photothermal Corp.), as outlined above, enables the simultaneous collection of IR and Raman spectra, from the same spot and same resolution.47,66,67 As illustrated in Fig. 3, O-PTIR and Raman spectra were collected in the centre of a solid BMC (Fig. 3a). The single O-PTIR spectrum (Fig. 3c) exhibits a phosphate peak at 1046 cm−1, without any saturation issues, and the carbonate band at 873 cm−1. In parallel, the Raman spectrum also shows phosphate and carbonate bands at 962 and 1072 cm−1, respectively. For the first time, we can assess and cross-validate the presence of carbonate ions in the BMCs, precisely, with both techniques.
In addition, the photothermal system, with a tuneable QCL, allows selection and acquisition of discrete wavelengths of interest with a high spatial resolution (0.5 μm per pixel). These single IR frequency images allow visualisation of the spatial distribution of proteins and lipids.
The Fig. 4a illustrates an example of an unstained breast tissue section image containing a BMC (red box). Fig. 4b–d show spatial distribution of proteins at 1656 cm−1 (amide I band), 1044 cm−1 (phosphate band) and 873 cm−1 (carbonate band). The disadvantage of these discrete frequency images is that the variation of intensity across the images could reflect a difference of thickness between the BMC and the soft tissue. In order to confirm the presence of these components (i.e. carbonate and phosphate ions) within the BMC and the spectral features at 872 and 1044 cm−1, respectively, different image ratios have been performed (Fig. 4e and f) and full O-PTIR spectra were collected at specific points in the tissue and the BMC (black squares, Fig. 4g and h). The presence of the amide I, II bands (1656–1660 cm−1 and 1544–1529 cm−1) but also phosphate peak at 1044 cm−1 and carbonate peak 872 cm−1 in the O-PTIR spectra evidences the spatial distribution of these components observed in the IR single wavelength images.
Fig. 5 is an example of a sample where the BMC is missing in the histological section. Based on the visible image (Fig. 5a), an IR image is recorded, highlighting two BMCs in the tissue (red arrows, Fig. 5b). Fig. 5b is a single-wavenumber image at 1030 cm−1 extracted from an FTIR hyperspectral data cube. A large-scale image (2.6 × 1.4 mm) is analysed in only 40 minutes. A Raman map (Fig. 5c) and an image at a single IR wavelength (1044 cm−1, phosphate band) (Fig. 5d) are acquired from the red square in Fig. 5a. This single frequency O-PTIR image is analysed in 20 minutes (188 × 130 μm) and illustrates a well-defined BMC using the 0.5 μm resolution. However, the acquisition time for each image depends on the size of the tissue section and the spatial resolution, which can be more important than the FTIR and Raman systems. A refinement of the area is necessary before using the photothermal system. In this process, a Raman spectroscopic analysis seems to be appropriate, by collecting a considerable image size with a satisfactory spatial resolution. In fact, the Raman map collected in Fig. 5c shows the BMC but also the soft tissue (8 hours of acquisition time for 354 × 316 μm). The Raman maps at the phosphate peak intensity (961 cm−1) shows several tiny BMCs surrounding the main focus of BMC in the tissue that were not visible in the IR image.
A multivariate analysis was performed on the Raman maps and illustrated in Fig. 6a and c in order to gain more information about the tissue surrounding the BMC. The K-means cluster analysis (Fig. 6c) shows different clusters exhibiting spectral features related to the tissue (dark blue and cyan clusters) and unexpectedly, two distinct clusters for the BMCs (orange and yellow clusters). In this figure, the centroids related to the tissue clusters have been removed for clarity. A comparison between the Raman map at the phosphate peak intensity and the cluster analysis evidences a good agreement. In fact, the BMCs are highlighted by the red arrows in Fig. 6a and the orange cluster in Fig. 6c. However, the multivariate analysis shows another cluster related to the BMCs represented in yellow in the Fig. 6c, diffuse in the surrounding tissue, which was not visible in the IR image in Fig. 5b. The mean spectra obtained for these two clusters illustrate different types of minerals (Fig. 6d). The orange spectrum related to the orange cluster (Fig. 6c) shows specific features for carbonated Hap with the phosphate band at 959 cm−1 and the carbonate band at 1070 cm−1, whereas the yellow spectrum exhibits two phosphate bands at 969 cm−1 and 1081 cm−1. By comparing this spectrum to our database of different standards, these BMCs are shown to be made of β-tricalcium phosphate (β-TCP). In fact, the spectrum shows the same features as the pure β-TCP component illustrated in Fig. 6b. This reflects the heterogeneity of different minerals in BMCs in the breast.
Based on the K-means image, a small area has been analysed using the Photothermal system defined in red square in Fig. 6c. Simultaneous IR and Raman hyperspectral images were recorded (16 × 21 μm for 19 hours) and illustrated in Fig. 6e and f. Regarding the acquisition time of these images, the K-means cluster analysis of the Raman maps enables targeting smaller areas of interest for the photothermal system, which are impossible to find using only the visible image, although the FTIR could also be used alone in some circumstances. The spectra extracted from the hyperspectral images at the same position show for the first time, IR and Raman spectra with characteristics of β-TCP (Fig. 6g and h). The IR spectra of different phosphate species are difficult to discriminate as they exhibit a very important ν3PO43− peak at around 1030 cm−1 combined with the organic matrix. For the first time, simultaneous IR and Raman spectra, from the same location, show specific features for the phosphate bands at 1084, 1034, 960 cm−1 and 969 and 1088 cm−1, respectively related to the β-TCP.
This study demonstrates that the combination of different vibrational spectroscopic techniques at very different spatial resolutions and imaging speeds is necessary to refine the analysis of a very specific area of interest.
Fig. 7 illustrates the different techniques applied to the same BMC in different tissue sections. In this example, where the BMC is missing in the H&E section (red arrow, Fig. 7e). Fig. 7a shows composite SRS (in green), TPF (in blue) and SHG (in red) images on a large field of view. This multimodal approach gives the chemical distribution of the proteins (in green) at 2930 cm−1 and collagen fibres in the connective tissue (in red). However, it is not possible to discriminate the different collagen types. A zoomed image of the area of interest (red square, Fig. 7a) was taken and illustrated in Fig. 7b. It demonstrates, in this tissue section that the BMC is a combination of Hap (in blue) and proteins (in green), which was confirmed by Raman spectroscopy. In order to generate the SRH image, SRS images were taken at 2930 cm−1 and 2485 cm−1 (Fig. 7c) following the protocol in different studies.52,53 A difference of the SRS signals (SRS2930 cm−1 − SRS2845 cm−1) was overlaid on the SRS2845cm−1 image. False colours were applied to mimic the H&E images, based on the known vibrational modes of the molecules of interest selected in the SRS. The SRS2845cm−1 image in pink representing the cytoplasm and the SRS2930 cm−1 − SRS2845 cm−1 image in purple representing the cell nuclei as illustrated in Fig. 7d. There is a good agreement between the SRH image and the traditional H&E images (Fig. 7e) even though the images are two different but adjacent tissue sections. This method allows the generation of digitally stained images by using a label-free and non-destructive technique, whilst also allowing in parallel a vibrational spectroscopic approach to gain complete information about the BMCs.
However, there are several challenges with using the O-PTIR approach: the area of the visible image is limited by the field of view of the system (125 × 626 μm), restricting visualisation of larger tissue samples. Additionally, by increasing the spatial resolution, the acquisition time increases accordingly, which limits the ability to select large areas of interest in contrast to standard FTIR systems.
Furthermore, for some minerals, artefacts in O-PTIR spectra or a shift in the peak positions are observed e.g. Calcium oxalate monohydrate, cHap. This has also been shown in a study from Bazin et al., suggesting that at a nanoscale analysis (AFM-IR or O-PTIR spectroscopy) there is some differences between AFM-IR and FTIR data, depending on the type of mineral analysed.68
Other points are noticed, for a probe at 785 nm, a sample thickness of 2, 5 or 10 μm is suitable for the O-PTIR spectroscopy analysis. However, thicker samples are recommended, in order to get an improved Raman signal. BaF2 or CaF2 slides can be used for the system, but a stainless-steel substrate is more challenging; the QCL IR source tended to heat the slide, which subsequently damaged the tissue sample. By using the stainless-steel substrate, some artefacts were observed in the O-PTIR spectra for different thicknesses of tissue sections. One hypothesis could be that this substrate reflects more than a transparent substrate, which create these artefacts. It is also possible to use glass slides, although thicker (more than 10 μm) samples are necessary to avoid the contribution of the substrate in the spectra. In the samples measured, this appears to result in BMCs more prone to burning.
The SRS and SHG techniques play an important role in the analysis for investigating the collagen content in the BMCs and further analyses are necessary to validate the results and to understand the involvement of the collagen matrix in the BMC formation. However, the presence of proteins within the calcifications tends to evidence the heterogeneous nucleation process as observed in many pathological calcifications.70,71 In our case, the crystal growth is embedded in the organic scaffold of proteins, DNA and collagen fibres.70 Moreover, this multimodal approach allows the reconstruction of SRS images to accurately mimic H&E sections. This method opens new perspectives in our scientific study to obtain faster H&E images (compare to the traditional H&E staining protocol). Furthermore, as we usually work on adjacent sections, some BMCs could be missing in the H&E sections and are hardly noticeable in unstained sections and tends to be a challenge for the vibrational spectroscopic analysis. In this case, SRS images can guide us when a BMC is missing in adjacent sections.
In conclusion, by combining a range of key complementary analytical techniques, it is possible to gain improved information regarding the spatial distribution of the mineral and organic components and the validation of the specific compositions found within BMCs.
All the other authors contributed to the interpretation of the results, the writing and/or the critical revision of the manuscript and approved the final version.
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