Abstract
Calcification of aortic valve leaflets is a growing mortality threat for the 18 million human lives claimed globally each year by heart disease. Extensive research has focused on the cellular and molecular pathophysiology associated with calcification, yet the detailed composition, structure, distribution and etiological history of mineral deposition remains unknown. Here transdisciplinary geology, biology and medicine (GeoBioMed) approaches prove that leaflet calcification is driven by amorphous calcium phosphate (ACP), ACP at the threshold of transformation toward hydroxyapatite (HAP) and cholesterol biomineralization. A paragenetic sequence of events is observed that includes: (1) original formation of unaltered leaflet tissues: (2) individual and coalescing 100’s nm- to 1 μm-scale ACP spherules and cholesterol crystals biomineralizing collagen fibers and smooth muscle cell myofilaments; (3) osteopontin coatings that stabilize ACP and collagen containment of nodules preventing exposure to the solution chemistry and water content of pumping blood, which combine to slow transformation to HAP; (4) mm-scale nodule growth via ACP spherule coalescence, diagenetic incorporation of altered collagen and aggregation with other ACP nodules; and (5) leaflet diastole and systole flexure causing nodules to twist, fold their encasing collagen fibers and increase stiffness. These in vivo mechanisms combine to slow leaflet calcification and establish previously unexplored hypotheses for testing novel drug therapies and clinical interventions as viable alternatives to current reliance on surgical/percutaneous valve implants.
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Introduction
The evolutionary success of invertebrate and vertebrate organisms through geological time has relied on their ability to harness the precipitation of thermodynamically unstable amorphous calcium phosphate (ACP) before it spontaneously transforms into crystalline hydroxyapatite (HAP)1,2. While ACP calcification is fundamental to an organism’s ability to precipitate essential hard parts such as bone and teeth, the capacity of ACP to morphologically shape-shift and atomically rearrange also results in various soft tissue pathologies3. This affinity for compositional flexibility reflects the dynamic nature of transient calcium phosphate compounds that lead to ACP biomineralization and eventual transformation toward HAP, a process in which nanometer-scale particles with short-range ionic order4,5 aggregate and undergo repeated events of precipitation, dissolution and reprecipitation (diagenetic phase transitions6). The complex physical, chemical and biological interactions controlling ACP (Cax(PO4)z·nH2O, n = 3–4.5; 15–20 wt% H2O)3,4 calcification are strongly influenced by solution chemistry (pH, saturation state and calcium/phosphate [Ca/P] concentrations), availability of H2O4 and activity of extracellular matrix proteins and peptides that stabilize ACP and prevent its transformation into crystalline HAP7,8,9,10.
There is mounting unmet need to discover new clinical therapies for the prevention and treatment of calcification in the human circulatory system11,12,13,14,15,16. This process of cardiovascular calcification is a significant factor in the more than 18 million lives claimed globally each year by heart disease12. Stenosis of vasculature associated with blood flow restriction and heart valve calcification that leads to cardiac dysfunction has long afflicted humankind. Hardening of the arteries (atherosclerosis) has been observed in 4000 year-old human mummies from ancient cultures around the world17. Leonardo Da Vinci in 1513-14 AD confirmed the narrowing of arteries as “the thickening of coats of these veins” in his studies of the human heart18. In modern society, cardiovascular calcification continues to be a common health disorder in people of all ages, genders and ethnic backgrounds, is associated with other comorbidities19,20, and is the most prevalent form of heart disease in patients 65 and older12,21. Yet beyond invasive valve implants, there are no viable alternative drug therapies or clinical treatment options available12,22.
Previous research on aortic valve calcification (also called calcific aortic valve disease; CAVD23) has primarily focused on cellular and molecular pathophysiology processes, including extracellular matrix biochemistry and biomechanics, but has not specifically targeted the etiological processes recorded by the calcification deposits themselves7,11,12,13,14,15,23,24. This is because standard microscopy techniques for pathological screening include stains that dissolve ACP and/or transform ACP to HAP in tissue sections, while x-ray diffraction cannot resolve the short-range ordering of ACP. Since 1975, several comprehensive reviews12,13,15,25 refer to four basic research studies26,27,28,29 that have identified ACP as the primary agent of aortic valve and arterial calcification by combining electron diffraction, standard microscopy and microprobe analyses with optical microscopy on unstained histological cryosections. Now, a half century later, rigorous examination specifically targeting the role of ACP in cardiovascular calcification remains to be completed12,14,25,29. This is in sharp contrast to long-running recognition of the fundamental importance of ACP biomineralization in bone, teeth and kidney stones4,30,31,32, as well as a wide variety of other bioengineering applications that have used multiple nano- and micro-scale analytical techniques to characterize ACP3,32,33,34.
GeoBioMed approach
The present study specifically targets calcification deposits formed in aortic valve leaflet tissues utilizing a transdisciplinary approach called GeoBioMed that combines concepts and techniques from the fields of geology, biology, and medicine6. These analyses of original unaltered and calcified (diagenetically altered6) aortic valve leaflet tissues reveal the distribution, composition and developmental record (paragenetic sequence6) of ACP, ACP at the initial stages of transformation toward hydroxyapatite (HAP), and cholesterol biomineralization within the context of tissue structure, cellular function, biomolecular activity and patient medical history. Collectively, this GeoBioMed evidence establishes a detailed history of soft tissue pathological calcification events, each stage of which occurs sequentially and/or simultaneously and to differing extents of reaction35 throughout each aortic valve leaflet. The paragenetic sequence spans from initial unaltered tissues through advanced calcified stages of collagen fiber and smooth muscle cell (SMC) myofilament calcification, stabilization by osteopontin (OPN), nodule formation and containment mechanisms and rotation during flexure that results in stiffening. The result is a previously unexplored roadmap for future development of untested GeoBioMed clinical therapies for the prevention and treatment of aortic valve leaflet calcification.
For the purposes of the present study, the term ACP is used to collectively refer to: (1) the transient amorphous phases of calcium phosphate that include dicalcium phosphate dihydrate (DCHD), dicalcium phosphate anhydrous (DCPA), octacalcium phosphate (OCP), α and β tricalcium phosphate (TCP) and ACP itself3,4; and (2) ACP deposits that, while still amorphous and non-birefringent, exhibit low order transformations toward HAP that begin to exhibit geometric (euhedral) forms36 (Fig. 1). Multiple previous medical and engineering studies3,4,26,27,28,29,30,32,33,34,36 have established an extensive analytical data base with which to consistently and accurately identify ACP and cholesterol biomineralization deposits in histological cryosections and petrographic epoxy impregnated sections. Optical, electron, laser and x-ray microscopy and spectroscopy evidence collected in the present study utilize this literature base as a comparative standard to confirm that the biomineralization deposits formed in the aortic valve leaflet tissues are predominantly composed of ACP and a minor component of crystalline cholesterol (Fig. 1). Internal controls for characterizing calcified tissues are provided by analyzing pristine non-calcified portions of the aortic valve leaflet tissues that are common throughout each histological cryosection and petrographic section.
Several lines of evidence collected in the present study indicate that the biominerals responsible for aortic valve calcification and resulting leaflet stenosis are composed of multiple transient forms of ACP, ACP at the threshold of transformation to HAP and cholesterol. These analyses include (Table 1; Figs. 1, 2): (1) energy dispersive elemental analyses (EDAX)4 indicating calcium (Ca) to phosphate (P) atomic % compositions (Ca/P) of 1.17 to 2.49; (2) Raman spectroscopy42,43 exhibiting broad peak overlap ranges of 400–500, 550–700 and 925–985 cm−1; and (3) absent (extinct) to extremely low birefringence under high resolution circular polarization (CPOL)6,36, while simultaneously exhibiting geometric (euhedral) forms under bright-field (BF) and CPOL microscopy. The aortic valve leaflet biomineralization deposits also exhibit characteristic mottled and generally poorly defined diffuse and shapeless textures of ACP. This is confirmed with the integration of micro-computed tomography (Micro-CT) imaging, high resolution BF, CPOL6 and transmitted light photomultiplier tube (TPMT)6 microscopy, and environmental scanning electron microscopy (ESEM)6 (Table 1). In addition, organic molecules coating biomineral individual layers are entrapped by each ensuing layer of ACP deposition, creating a high fidelity nm-scale microstratigraphy record of calcification6. These processes are documented with confocal autofluorescence (CAF)6, widefield fluorescence (WF)6, super resolution auto fluorescence (SRAF)6, and super resolution induced fluorescence (SRIF) microscopy6 using the Alexa 647 antibody against osteopontin (OPN)8,10. While OPN is a catalyst of HAP precipitation in non-phosphorylated form, it has also been shown that phosphorylated OPN acts as a strong inhibitor of ACP deposition8,9,10,44,45. Furthermore, Oil Red O (ORO) stain under BF is used to identify the presence of lipids and Alizarin Red S (ALZ) stain under BF to identify calcium in ACP. In addition, the well-defined acicular to lathe-shape crystalline structure of cholesterol under BF exhibits strong birefringence under CPOL46, which is further substantiated with the comprehensive suite of analyses presented in Table 1.
Materials and methods
Human aortic valve leaflet samples
All methods in this study were carried out in accordance with guidelines and regulations in a basic medical research study plan that was reviewed and approved by the UCLA Health Institutional Review Board (IRB 19-000624). Three human cadaveric (deceased patient) hearts were analyzed from a cohort of 26 hearts reposited at the Cardiac Arrhythmia Center and Neurocardiology Research Program of Excellence at UCLA Health. Written informed consent was obtained from all UCLA health patient participants as part of the OneLegacy Foundation and the NIH SPARC Program, which formed the basis for obtaining cadaveric donor hearts for research and for funding this effort. These cadaveric hearts were chosen based on their differential extent of calcification as described below. After 24 h pressure perfusion and fixation with 4% paraformaldehyde, samples were stored in 1 × PBS and 0.02% Sodium Azide at 4 °C until analysis. The heart donor population was 54 ± 10 years old, 65% male, and exhibited 31 ± 12% aortic calcification, 15 ± 4% aortic valve calcification, and 62 ± 7% coronary arterial calcification as calculated from CT scans.
Leaflet dissections and preparation of histological cryosections and petrographic sections
Legacy hearts chosen for analysis were first thoroughly documented with high-resolution photography using a Nikon D850 camera at UCLA Health. The three-dimensional (3D) distribution of calcification within each whole legacy heart prior to dissection was determined with: (1) 3D CT scans at a resolution of 600 μm on an CT (SOMATOM Definition AS, Siemens Healthcare, Forchheim, Germany) at UCLA Health; and (2) 3D micro-computed tomography (Micro-CT) scans at a resolution of 3 μm on a North Star X 5000 at the Roy J. Carver Biotechnology Center (CBC) and Carl R. Woese Institute for Genomic Biology (IGB) at the University of Illinois Urbana-Champaign (Illinois). CT and Micro-CT 3D x-ray scan data sets were then rendered and evaluated on a Hewlett Packard-Z-10 Workstation. These coupled CT and Micro-CT scans were used to guide dissections of each of the three aortic valve leaflets (left coronary, right coronary and non-coronary) and precisely record their 3D spatial orientation and positioning within the aortic valve. Dissections were completed at UCLA Health (which included additional high-resolution photography) with minor follow-up dissections in the Illinois CMtO CBC laboratory. All dissected samples were fixed in 10% formalin, gently washed in deionized water and transferred to 50 mL falcon tubes containing 1 × PBS and 0.1% Sodium Azide and stored at 4 °C until analysis. Prior to sectioning, dissected leaflets were scanned again on a North Star X-5000 Micro-CT at the CBC and IGB, as well as on a Rigaku HX130 Micro-CT at the Illinois Beckman Institute for Advanced Science and Technology. Individual leaflets were then further dissected, frozen in liquid nitrogen-cooled Isopentane, embedded in optimum cutting temperature (OCT; Tissue Tek, Sakura Fine Tek, USA) cryopreservation medium (non-coronary leaflets) and kept at − 80 °C until sectioning. From which a total of 30 serial histology crysections for tissue analysis were made at the Histology Laboratory at the Illinois College of Veterinary Medicine. Histology sections were glass mounted on an Epredia NX 70 cryostat at − 20 °C, after which the sections were stored at − 80 °C until analysis (uncovered, 20–30 μm-thick for three-dimensional [3D] analysis). An intact aortic valve leaflet (right) was air dried at 37 °C for 24 to 48 h in an Epredia warm air oven. From which, two petrographic glass-mounted thin Sects. (25 μm-thick, doubly polished) for mineralogical analyses were prepared at Wagner Petrographic Ltd. (Lindon, UT) using low viscosity cathodoluminescence-resistant epoxy and precise cutting angles to contextually capture the progression of nodule calcification within the leaflet tissue.
Immunofluorescence labeling of osteopontin (OPN) protein
The sequentially made histological cryosections were segregated into cohorts, which included: (1) unstained sections; (2) sections stained with Alizarin Red (ALZ) for calcium in ACP, Oil Red O (ORO) for lipids (both are contrasting stains for bright field microscopy) and a fluorescence 4′,6-diamidino-2-phenylindole stain (DAPI) for DNA (for fluorescence, confocal and super resolution microscopy); and (3) sections for immunohistochemical fluorescence labeling for the osteopontin (OPN) protein (fluorescence, confocal and super resolution microscopy). For immunohistochemical labeling, sections were removed from storage at -80 °C and placed on a slide holder in a C1000 Touch Bio-Rad thermal cycler set at 37 °C for one minute, then incubated with prechilled HPLC grade methanol for 30 min at − 20 °C. Sections were then immediately removed and hydrated in phosphate buffered saline containing 2% Triton-X-100 (PBST) for 30 min. Sections were blocked with IT Signal FX (I36933-ThermoFisher, Carlsbad, CA) for 30 min in a dark room to remove any unspecific binding of antibodies followed by incubation with an OPN antibody (CoraLite Plus 647 conjugated Osteopontin Rabbit polyclonal antibody (CL647-22952, Proteintech, Rosemont, IL) at 1:100 dilution with PBST and IT Signal FX (10%) for overnight incubation in a humid chamber. Sections were then washed three times in PBST, mounted in Prolong Gold (P36935-ThermoFisher, Carlsbad, CA), an antifade mounting medium containing DAPI. After wicking away excess mounting medium, sections were sealed with a cover glass and kept in the dark overnight for curing until reaching a higher refractive index (~ 1.4) to enable index matching high-resolution imaging with oil immersion objectives. These covered sections were then sealed with quick dry nail polish and stored at 4 °C, until analysis.
High-resolution imaging of aortic valve leaflets using multiple modalities
Petrographic epoxy impregnated sections were imaged unstained. However, the other consecutive histological cryosections of aortic valve leaflets were labeled with multiple visible contrast stains (for bright field microscopy) such as Alizarin Red S (ALZ) for Ca in ACP, Hematoxylin and Eosin stains for cellular morphology and Oil Red O (ORO) for lipids. The intermittent serial sections, not labeled with visible stains, were mounted with Prolong Gold antifade reagent containing DAPI (ThermoFisher Scientific, Carlsbad, CA), which labels nuclei/double stranded DNA in the sectioned samples and cured for 24–48 h to reach a refractive index of ~ 1.4 and mounted with a 170 μm-thick cover glass to improve the index matching, signal integrity and image quality, when especially using oil immersion objectives as described above.
The present study utilizes multiple optical modalities (Table 1) as described previously26, which include BF, TPMT, CPOL, CAF, WF, SRAF and SRIF modalities that were completed on a custom built Carl Zeiss LSM 980 Spectral NLO Airyscan II Super resolution system (Carl Zeiss, Oberkochen, Germany) housed in the CBC. This microscope system is mounted with a Carl Zeiss Axiocam 712 color camera for brightfield and polarization optical modalities and a Hamamatsu Orca-Flash4.0 digital CMOS camera for fluorescence images excited by Excelitas, Xylis broad spectrum LED illumination light source. This suite of optical hardware uniquely enabled multimodal images (BF, POL, CPOL, TPMT, WF, CAF, SRAF and SRIF), at precisely the same locations of interest under multiple magnification. Large areas of samples are also tiled (using a factory-built Zeiss automated XY stage) to capture contextual visualization of the whole section, as well as 3D images using Z-stack functionalities across a broad range of magnifications (10 × Plan Neofluar:0.45 NA; 20 × Plan Apochromat: 0.75 NA and 0.8 NA; 40 × Plan Apochromat Oil immersion: 1.4 NA; 100 × Plan Apochromat Oil immersion: 1.49 NA). Compared to conventional crossed Nicol polarization, the current utilization of CPOL quarter-wave plate (λ/4 wide spectrum compensator covering 0–30 λ together with a 570 nm retardation plate), which enhanced the birefringence of all crystals without depending on their extinction axis and added another order of birefringence color spectrum as per Zeiss Michel-Levy’s interference chart (2015; Supplementary Fig. 7). Under the CAF and SRAF/SRIF modalities, we used 405 nm (emission collected between 410–460), 488 nm (emission collected between 500–550) and 561 nm excitations (emission collected between 570–615) to collect the entire visible emission spectrum of autofluorescence signatures from both organic and inorganic crystalline architecture. Since the tissue is already autofluorescent, the OPN antibody conjugated dye was selected specifically to be distinct at 647 nm excitation to avoid any overlap with the autofluorescence (excitation 647 nm and emission collected between 650–720 nm). In some instances, a few SRAF and SRIF channels were merged after appropriate pseudo-coloring of the individual channels. While CAF provided a diffraction limited resolution of ~ 250 nm, the SRAF and SRIF images yielded 140 nm super resolution images. The pixel resolutions of the images were between 20 to 300 nm for most images under these two modalities. The TPMT images are obtained using the shortest wavelength available for retrieving highest optical resolution (405 nm laser) and the corresponding resolutions were ~ 180–200 nm under the 100 × 1.49 NA oil immersion objective. The tiles and Z-stack were optimized with multiple supporting focal points, stitched using the Carl Zeiss Zen (Carl Zeiss, Oberkochen, Germany) stitching module and the Z-stack slices were around 130 nm per slice and a range of 5–15-micron depth images were 3D projected using the 3D Surpass algorithm in the 3D visualization and rendering program Imaris (version 10.0, Oxford Instruments, Carteret, NJ).
Environmental scanning electron microscopy (ESEM) and energy dispersive elemental analysis (EDAX)
ESEM of both intact human aortic valve leaflets containing nodules and consecutive sections from the same blocks of tissue. Leaflet samples used for standard histological cryosectioning were critical point dried using hexamethyldisilazane (HMDS) followed by sputter coating with gold palladium (Au/Pd) target (Denton DESK II TSC, Moorstown, NJ). Samples were then imaged under vacuum in a FEI Quanta FEG 450 FESEM (Hillsboro, OR), housed in the Illinois Beckman Institute for Advanced Science and Technology, under multiple magnifications on cryosectioned samples as well as undisturbed intact aortic valve leaflets after mounting a chuck with carbon tape. As described previously6,47, ESEM imaging was done under the default setting of an ~ 10 mm working distance, 20 kV beam with a spot size of 4.0 nm, and multiple magnifications with a dwell time of 300 ns. On histological cryosections and petrographic sections, elemental maps and energy dispersive elemental analyses (EDAX; n = 9) with a spot size of 3 μm at each sample location (Supplementary Data Fig. 2) to specifically analyze Ca, P and Mg, the elements that are indicative of ACP calcification. Spot analysis locations included unaltered collagen, and individual ACP spherules and crusts on diagenetically unaltered collagen. The EDAX Ca/P atomic ratios were calculated and graphed in Microsoft Excel.
Raman spectroscopy of calcified leaflets
Calcification mineralogy was assessed with a WiTec Alpha300 RSA Raman imaging microscope system (WiTec, Nashville, TN) housed in the IGB with a 532 nm-wavelength laser. A 100 × air objective (LU Plan Fluor 0.8 NA) capable of providing submicron spatial resolution was used to record Raman spectra from 5 μm-thick histology cryosections mounted in ultrapure water of the aortic valve leaflets. Spectra were collected with a 1–10 mW laser power and a 1 s exposure time. An optical fiber, providing an effective pinhole of 50 μm, was used to transmit the optical signal to a WiTec UHTS400 spectrometer and WiTec Peltier cooled CCD camera. Peak fitting analysis was performed by assuming a Gaussian line profile (Type: Gauss (position cm-1, FWHM ∆ cm-1); position 431, FWHM = 16.2; position 442, FWHM = 48.0; position 454, FWHM = 14.4; position 581, FWHM = 14.3; position 586, FWHM = 60.0 cm−1; position 592, FWHM = 11.8; position 611, FWHM = 14.2; position 952, FWHM = 25.0; position 961, FWHM = 16.7). This analysis reveals all expected phosphate (PO4–3; Td point group) Raman bands corresponding to symmetric stretch (v1) at 961 cm−1, bending (v2) at 431 & 454 cm−1, and bending (V4) at 581, 592 & 611 cm−1.
Image adjustments, analysis, and presentation
Image processing and analysis were mostly performed in the native Carl Zeiss Zen (version 3.5) program used to acquire the images in the same system computer. Where needed the gamma of 0.45 or 0.75 was used under a spline mode where necessary to enhance the color and image fidelity for easy observation. Image enhancements were also made in the 3D rendering program Imaris, Canvas, Adobe Photoshop, Microsoft PowerPoint, when the final plates are cropped, resized and assembled.
Ethics approval and consent to participate
This basic medical research study was reviewed and approved by the institutional review board of University of California at Los Angeles (IRB#19-000624).
Results
Aortic valve leaflets
Aortic valves contain left coronary, right coronary and non-coronary leaflets that develop large mm-scale calcified nodules within the leaflet tissues (Fig. 3a–c). Rather than passive structures involved in aortic valve function, each thin aortic valve leaflet (Fig. 3a) is instead a dynamic, innervated, muscled and vascularized organ with the capacity to adapt to complex cardiac environmental conditions and stresses23,48,49. Common examples of leaflet function include activation of myocyte and fibroblast differentiation during inflammatory response to calcification50, as well as ongoing adjustment of biomechanical properties through fibroblast-driven tissue remodeling in response to the hemodynamic forces constantly imparted over the three billion repetitive systole and diastole cycles of a human lifespan23,48,49. These adaptive structural and functional responses are made possible by communication between valvular endothelial cells (VECs) and valvular interstitial cells (VICs), which results in tissue remodeling and the synthesis of a valvular extracellular matrix (VECM), collagen and elastin7,11,12,14,23,24,48,49,51,52,53.
The outermost monolayer of VECs overlying and encasing each leaflet is central to aortic valve function, with individual cells oriented relative to blood flow direction, leaflet sheer stress and cytoskeletal structure48. VICs within leaflets contain a mixed population of cells dominated by interacting smooth muscle cells and fibroblasts11,48,54. The thin (300–700 μm-thick) yet extremely strong 3-layered structure of each leaflet, which have no initial calcification when healthy23,48,49, consists of (Fig. 3d): (1) a fibrosa layer on the aortic side (45% of leaflet thickness) that contains a mixed population of VICs and Type I collagen fibers55,56,57 for support against circumferential hemodynamic stresses and tensile forces imparted by aortic backflow during diastole; (2) a middle spongiosa layer (35% of leaflet thickness) with a microvascular system that permits interstitial cells to absorb shear forces during the cardiac cycle, an extracellular matrix that produces high concentrations of proteoglycan and glycosaminoglycan (GAG) and a high hydrous content for gliding of the layers during the cardiac cycles; and (3) a lowermost ventricularis layer (20% of leaflet thickness) that contains densely laminated and radially aligned elastin fibers that provide tissue structural flexibility, enhanced radial stretch and elastic recoil during systole. However, upon calcification and initiation of inflammatory responses, leaflets undergo complex modifications and remodeling14.
Paragenetic sequence of aortic valve leaflet calcification events
Multiple independent lines of microscopy and spectroscopy evidence (Table 1) are combined here to establish a paragenetic sequence of ACP and cholesterol biomineralization events (Fig. 4) that result in the calcification of aortic valve leaflet tissues. All paragenetic sequence events (PSE 1–5; Fig. 4) are present simultaneously at different locations and at differential extents of development throughout each leaflet across a broad 107 range of length scales. This is caused by the highly variable extents of reaction that occur at any one location35 as calcifying fluids permeate through the aortic valve leaflet tissues. CPOL extinction and birefringence are especially valuable tools for identifying and mapping calcification in unstained histological cryosections and petrographic sections (Fig. 3d). However, small changes in histological cryosection and petrographic section thickness and the axial orientation of collagen fibers can also influence CPOL birefringence58. As a result, confirmation of the presence and extent of collagen calcification (PSE 2; Fig. 4) implied by CPOL birefringence is substantiated in the present study with integrated multimodal analyses (Table 1). In original leaflet tissues (PSE 1; Fig. 4) the uppermost layers of the fibrosa layer are composed of unaltered collagen fibers (Fig. 3d) that contain no evidence of either ACP or cholesterol deposits as follows. Each unaltered collagen fiber exhibits low concentrations of lipid droplets in BF (Fig. 5b; SI Fig. 3a), blue CPOL birefringence (Figs. 3d, 5c; SI Fig. 4a,c), green SRAF emissions (Figs. 5d; SI Fig. 4a–c) and has no detectable Ca or P concentrations with EDAX analyses of serial cryosections (Table 1; Fig. 1; SI Fig. 1). These characteristics are consistent with previous reports of unaltered collagen birefringence created by its anisotropic fibrous structure58,59 and emissions from intrinsic biomolecules such as proteoglycans and glycosaminoglycans (GAG)60,61.
Medial and lower portions of the fibrosa tissue layer (Fig. 3d) exhibit variable extents of ACP and cholesterol diagenetic alteration of collagen fibers and smooth muscle cell (SMC) myofilaments (PSE 2; Fig. 4). This is indicated by their Raman spectra (Table 1; Fig. 2; SI Fig. 1), the presence of individual 100’s nm- to 1 μm-scale ACP spherules and crusts formed by coalescing ACP spherules in ESEM (Figs. 5e, f; SI Fig. 2d), EDAX compositional Ca/P atomic ratios of 1.17–2.49 ± 0.38 (Table 1; Fig. 1; SI Fig. 1), red to green to yellow CPOL birefringence (Figs. 3d, 5g; SI Fig. 3), yellow SRAF emissions (Fig. 5h; SI Fig. 4b), and low-contrast diffuse gray Micro-CT (Fig. 3c). 100’s nm-scale ACP spherules precipitate within the ultrastructure of crimped collagen fibers57,62 (Fig. 5i,j; SI Fig. 4e,f) and within the banded ultrastructure of SMC myofilaments on thick phosphorylated myosin bands, which are separated by thinner actin bands with less ACP precipitation (Fig. 5k,l)50,63. This combination of optical and electron microscopy and Raman spectroscopy evidence indicates the presence of multiple transient ACP diagenetic calcium phosphate phases based on their Ca/P atomic %4,43 (Table 1; Fig. 1). The poorly ordered transient composition3 of ACP spherules and nodules (Fig. 1) result in extinct black to 1st order dark gray lavender birefringence in CPOL (Table 1, Fig. 5g; SI Fig. 3c).
ACP diagenetic alteration (PSE 2; Fig. 4) accentuates the CPOL blue birefringence of original collagen and SMC myofilament proteoglycans (SI Fig. 5) to create higher birefringence in areas of partial or complete calcification (Fig. 3d; SI Fig. 4a,c, 6b,f–h). Concentrated coatings of OPN observed on lipids, ACP and cholesterol (PSE 3; Figs. 4, 5j, 6d; SI Fig. 5) serve to chemically stabilize the ACP and prevent spontaneous transition to HAP7,8,10,41. In addition, the combination of Alizarin Red S staining and OPN coatings (analyzed on sequential histological cryosections) provide the contrast required to resolve: (1) Type I collagen fiber crimping (Fig. 5i,j; SI Fig. 4e,f) that is common in soft tissues and stores biomechanical energy during leaflet flexure62; and (2) ACP precipitation within the 1 μm-thick striated banding ultrastructure of SMC myofilaments (Fig. 5k,l; SI Fig. 5e,f)64. Cholesterol precipitates as parallel bundles of euhedral acicular crystals aligned between diagenetically altered collagen fibers and SMC myofilaments, as identified by their white CPOL birefringence (Fig. 5g; SI Fig. 3c), no SRAF emissions (Fig. 5h; SI Fig. 4c) and no detectable Ca or P concentrations with EDAX (Table 1). Furthermore, cholesterol crystals have previously been observed to enhance precipitation of 100’s nm-scale ACP spherules from synthetic cardiovascular fluids under controlled experimental conditions37.
The presence of nodules (PSE 4; Fig. 4) is an emblematic feature of calcified aortic valve leaflet tissues23,28,65 (Fig. 6; SI Figs. 6–9). Evidence indicating that these nodules are primarily composed of ACP includes Raman spectra (Table 1; Fig. 2; SI Fig. 1), low contrast diffuse gray Micro-CT (Fig. 3c), extinct black to dark gray lavender CPOL birefringence (Figs. 3d, 6a, c, h), yellow to red to indigo SRAF (Fig. 6e, i, j; SI Figs. 6–9), and EDAX Ca/P atomic ratios of 1.47–1.91 (Table 1; Fig. 1; SI Fig. 1). In addition, ACP and cholesterol nodules of all sizes are coated with OPN (Figs. 6b, d; SI Fig. 6b, c, f–h). The cores of nodules formed by coalescing ACP spherules commonly exhibit rudimentary euhedral geometric forms11 (Figs. 6f-i) that are similar to transformations observed in human kidney stones and natural hot springs6. Simultaneously, the outermost nodule margins diagenetically incorporate surrounding ACP altered collagen fibers via Ångstrom-scale fabric preserving (mimetic) dissolution and reprecipitation replacement6 (Fig. 6i; SI Movies 1–3). Importantly, all diagenetic paragenetic sequence events (PSE 2–5; Fig. 4) are observed to occur exclusively within, and not on the VECs and outermost surface of the aortic side of the fibrosa tissue layer (Fig. 3d; SI Figs. 8, 9). Nodules range from small 10’s μm-diameter single deposits growing between collagen fibers (Figs. 6a, b; SI Fig. 6) to large well-developed mm-sized aggregate nodules (Figs. 3d, 6i; SI Figs. 7–9). Initially, small nodules are composed of approximately equivalent amounts of ACP and acicular cholesterol crystals (Figs. 6a, b). Conversely, as nodule enlargement progresses through intermediate and advanced stages of calcification (PSE 4; Fig. 4), nodules become predominantly composed of ACP with significantly lower amounts of cholesterol (Figs. 6c–i, 7; SI Figs. 7–9).
Nodule twists, stenosis and containment
Calcification nodules (PSE 4; Fig. 4) form everywhere from deep within the leaflet fibrosa tissue layer to near the aortic margin and are overlain by 10’s μm-thick continuous layers of unaltered and unbroken collagen fibers (Figs. 3d, 6c,i, 7; SI Figs. 6–9). The interior underside of these collagen bundles, which are in direct proximity with each nodule, stretch during leaflet flexure and become increasingly more altered until becoming diagenetically incorporated into the nodule outer surfaces, allowing nodules to grow, expand and accrete (Figs. 6i, 7; SI Figs. 8, 9). However, an outermost containment barrier of unaltered and unbroken collagen is simultaneously maintained that prevents nodules from rupturing and penetrating the outermost VECs and fibrosa tissues (Fig. 7; SI Figs. 7–9). This containment mechanism prevents the ACP-dominated nodules from being directly exposed to blood solution chemistry (pH, saturation state, and availability of H2O). Exposure and direct contact with ACP-saturated and H2O-rich blood serum would quickly drive transformation of ACP into HAP and rapidly increase the extent and distribution of calcification4,66. A similar type of Type 1 collagen containment process encapsulates, restrains and decelerates the progression of pancreatic ductal adenocarcinoma cancer tumors67.
Stress and strain forces during each diastole and systole cycle induce leaflet tissue flexure68, which in turn causes the hard calcified nodules to continually rotate back-and-forth (twist) as they are forming (PSE 5; Fig. 4). This process is recorded by asymmetrically folded and overfolded69 unaltered collagen fibers that surround and contain small-to-large single and aggregated nodules (Figs. 6i, 7b, c, 8a; SI Figs. 8, 9). These folds store, transmit and dissipate elastic energy56 as surrounding collagen axially extends and contracts to prevent the fibers from tearing and breaking during twisting rotational motions of the nodules during leaflet flexure70. As additional nodules form in the fibrosa layer with increasing extents of calcification, nodules further twist and turn, physically contact each other, and eventually aggregate, which dramatically increases the elastic modulus of the tissue to cause stiffening and further reduce leaflet structural flexibility and function. A similar mechanism occurs during water motion-induced flexure of pliable connective tissues in marine benthic invertebrates such as sponges and soft corals, which causes spatially isolated mm-scale tissue hard parts (spicules) to contact each other, amplify strain, resist compression and increase elastic modulus and stiffness71.
Spongiosa and ventricularis ACP and cholesterol biomineralization
Unlike the dominance of fibrosa tissue layer ACP diagenetic alteration in the form of altered collagen, altered SMC myofilaments, and nodules, the lipid-rich spongiosa layer (Fig. 8a) is predominantly altered by acicular cholesterol crystals that form in cell cytoplasm. These clusters of acicular cholesterol crystals exhibit white to blue CPOL birefringence (Fig. 8b) and highly concentrated coatings of OPN (Fig. 8c). ACP biomineralization is minimal in the spongiosa, forming rare individual spherules at peripheral cell cytoplasm and membrane interfaces that exhibit a dark lavender gray CPOL, yellow SRAF emissions and have pervasive OPN coatings (Fig. 8c). In contrast, elastin-dense ventricularis tissues contain no cholesterol crystals (Fig. 8d) and exhibit only rare occurrences of ACP spherules (dark gray lavender CPOL and yellow SRAF emissions) within cell cytoplasm (Fig. 8e). The heterogeneously distributed moderate to high concentrations of OPN observed throughout the ventricularis layer (Figs. 8e) is consistent with previous observations72. Despite extensive cholesterol crystallization, some ACP spherules and moderate to high concentrations of lipids and OPN, there is no evidence of ACP nodule formation in the spongiosa and ventricularis cell layers as there is in the fibrosa layer.
Discussion
Implications for translational medicine
The paragenetic sequence of ACP and cholesterol biomineralization observed here (PSE 2–5; Fig. 4), which has been tracked across 10’s nm to 10’s cm length-scales within dissected samples and tissue sections, provides independent evidence to test current assumptions regarding mechanisms of aortic valve leaflet calcification. Previous cellular and molecular pathophysiology studies propose that calcification is initiated by external damage and scarring of the VEC and outermost fibrosa layer due to oxidative and biomechanical stress7,11,12,13,14,15,23,24. In this widely held scenario, ACP-saturated and water-rich blood serum solutions containing lipoproteins and immune cells would infiltrate through these damaged breeches, in a manner similar to that of saturated urine in the thin loops of Henle during human kidney stone formation73. Resulting inflammation would activate reactive oxygen species, monocytes and macrophages (multinucleated giant cells) and cause VICs to differentiate into fibroblast, osteoblast-like and SMC myofilament phenotypes that promote fibrosis, calcification, matrix remodeling and leaflet stenosis. Ensuing chronic inflammation would then activate macrophage and VIC apoptosis, with the release of Ca, P and extracellular vesicles further promoting a self-perpetuating cycle of calcification primarily at locations near aortic side breeches of the fibrosa layer of the leaflet tissues.
However, ACP and cholesterol biomineralization observed in the present study exhibits no evidence of calcification on the outer surface of the leaflets and no evidence of damage or breech of the VEC or outermost fibrosa tissues (Fig. 7; SI Figs. 8, 9). Instead, all diagenetic stages of the paragenetic sequence (PSE 2–5; Fig. 4) and small-to-large nodules that occur throughout the fibrosa tissues, with nodules surrounded and contained by continuous, tightly stretched, and unbroken outermost layers of non-calcified collagen fibers (Figs. 3d, 7; SI Figs. 8, 9). These in vivo mechanisms create the commonly observed bulbous appearance of calcified aortic valve leaflets23,65 (Fig. 3a; SI Fig. 2a, b; 7–9). The GeoBioMed evidence collected in the present study implies that calcification can take place without obvious damage of the outermost VEC and fibrosa tissues. As a result, original leaflet tissue permeability may be sufficient to permit the ongoing normally occurring infiltration of saturated lipid-rich serum-derived solutions that are capable of in vivo calcification. In addition to these permeating fluids, ACP-rich vesicles and lipids may also be delivered inside the leaflet tissues via microvasculature14.
Future GeoBioMed research will focus on the mechanisms of OPN stabilization and collagen containment to slow, prevent and disrupt key calcification events of the paragenetic sequence within aortic valve leaflet fibrosa tissues (Fig. 4). Targets include nm-scale ACP spherule precipitation, Ostwald ripening and coalescence of spherules into planar forms, and diagenetic recrystallization and incorporation of altered collagen at the margin of nodules. This will require further strategic multimodal analyses of calcified aortic valve leaflets from patients with replaced aortic valves and prosthetic implants10. The banding-specific deposition of ACP spherules within collagen crimps (Figs. 5i, j; SI Figs. 4e, f) and SMC myofilaments (Figs. 5k, l; SI Figs. 5e, f), suggests that ACP precipitation is substrate controlled by long-axis parallel and perpendicular ultrastructure and compositional changes within collagen fibers57,74,75 and SMC myofilaments76. These types of individual and combined mechanisms controlling the paragenetic sequence of calcification events (Fig. 4), which combine to prevent reliable thermodynamic predictions, can now be systematically tested in future studies using controlled microfluidic experimentation77. Previous experimental studies using blood serum and other fluids indicate that the initiation and thermodynamic stabilization of ACP is primarily controlled by8,10: (1) solution organic and inorganic chemistry and flow regime (e.g., pH; temperature; alkalinity; concentrations of Ca, P, Mg, Zn; organic molecule concentrations such as ATP, poly-l-lysine/citrate and poly-Asp, and boundary layer diffusion); (2) availability, concentration and distribution of proteins, phosphopeptides and other complexes that stabilize ACP and prevent or promote transition to HAP (e.g., phosphorylated OPN, casein, Mg); and (3) structure and composition of the substrate of precipitation. As each of these influences on ACP precipitation are systematically varied, the resulting composition, distribution and rate of ACP and cholesterol biomineralization can be tracked spatially and temporally in real time within microfluidic test beds such as the GeoBioCell78. These processes can be quantitatively tracked during systematic changes in aortic valve hydrology47 and ACP distribution and composition (e.g., elemental, isotopic, structural, trapped biomolecules) in the presence of hydrogels embedded with living VICs, collagen and SMC myofilaments77. Another complimentary and closely coordinated approach would be to experimentally track the precipitation of 100’s nm- to 1 μm-diameter ACP spherules within collagen crimps (Fig. 5i, j; SI Figs.4e, f) and SMC myofilaments (Figs. 5k, l; SI Figs. 5e, f). Controlled microfluidic experimentation would also permit testing of potential dosing effects of proteins such as OPN and nutraceuticals including Mg, Zn, Fe, vitamin K, phytate and natural plant derived compounds such as curcumin79. Collectively, these types GeoBioMed analytical approaches and experimentation, guided by the paragenetic sequence (Fig. 4), will permit discovery of fundamentally new approaches for the development of clinical therapies targeting the prevention and treatment of aortic valve leaflet calcification.
Data availability
Raw microscope images and processed images are available for download from the following link: https://figshare.com/s/c8ab95abe42b4d65d971
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Acknowledgements
We are sincerely thankful to those individuals who have donated their bodies and tissues for the advancement of education and research. We thank OneLegacy Foundation and the NIH SPARC Program, which formed the basis for obtaining donor hearts for research and for funding this effort. We are thankful to Anthony A. Smithson and Arvin Roque-Verdeflor with the Translational Research Imaging Center at UCLA for their support in computed tomographic data acquisition. We are grateful to our Research Operations Manager, Amiksha S. Gandhi, for her dedication to support our projects. We are also genuinely appreciative for invaluable discussions about this study with Issam Moussa (Carle Illinois College of Medicine), Charles Werth (Civil, Architectural and Environmental Engineering, UT Austin) and Marcelo Garcia (Civil and Environmental Engineering, Illinois). Rachel Chaffee (Integrated Biology, Illinois) provided research support and scientific discussions throughout the project. We sincerely thank Richard Reeder (Geosciences, Stony Brook) and John Rakovan *NM Bureau of Geology and mineral Resources) for invaluable discussions and literature on apatite mineral precipitation dynamics. We also gratefully acknowledge the analytical analyses provided by Kerishnee Naicker (Cytometry and Microscopy to Omics, Illinois), Karen Doty (Veterinary Medicine, Illinois), and Cate Wallace and Joshua Gibson (Beckman Institute, Illinois). We also sincerely thank Kurt Wagner and his team at Wagner Petrographic, Lindon, UT, for providing expert assistance, consultation and technical expertise in preparing petrographic sections.
Funding
This research was supported by a Barbara and Ed Weil Foundation grant to B.W.F., as well as NIH grant OT2OD023848 to K.S. and the UCLA Amara-Yad Project.
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K.S., O.A., and S.M. provided access to reposited legacy hearts that they thoughtfully chose and carefully prepared for analysis. S.M. was assisted by M.S and B.W.F. to conduct dissections, complete detailed photography and assemble contextual data. M.S., K.W.F. and B.WF. completed multimodal microscopy. R.B. and A.Z.S completed Raman spectroscopy analyses of histologic cryosections, as well as data modeling and drafting of figures. K.S., O.A., and S.M. provided in-depth discussions throughout the project and thoroughly edited text and figure drafts. M.S., K.W.F., S.M., O.A., S.K. and B.W.F. provided expertise throughout the study leading up to the final submission from their respective fields of neurocardiology and geobiology. R.B. and A.Z.S provided invaluable expertise in interpreting Raman spectroscopy of human tissues. All authors read and approved the final manuscript.
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Sivaguru, M., Mori, S., Fouke, K.W. et al. Osteopontin stabilization and collagen containment slows amorphous calcium phosphate transformation during human aortic valve leaflet calcification. Sci Rep 14, 12222 (2024). https://doi.org/10.1038/s41598-024-62962-8
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DOI: https://doi.org/10.1038/s41598-024-62962-8