The idea that original soft tissue structures and the native structural proteins comprising them can persist across geological time is controversial, in part because rigorous and testable mechanisms that can occur under natural conditions, resulting in such preservation, have not been well defined. Here, we evaluate two non-enzymatic structural protein crosslinking mechanisms, Fenton chemistry and glycation, for their possible contribution to the preservation of blood vessel structures recovered from the cortical bone of a Tyrannosaurus rex (USNM 555000 [formerly, MOR 555]). We demonstrate the endogeneity of the fossil vessel tissues, as well as the presence of type I collagen in the outermost vessel layers, using imaging, diffraction, spectroscopy, and immunohistochemistry. Then, we use data derived from synchrotron FTIR studies of the T. rex vessels to analyse their crosslink character, with comparison against two non-enzymatic Fenton chemistry- and glycation-treated extant chicken samples. We also provide supporting X-ray microprobe analyses of the chemical state of these fossil tissues to support our conclusion that non-enzymatic crosslinking pathways likely contributed to stabilizing, and thus preserving, these T. rex vessels. Finally, we propose that these stabilizing crosslinks could play a crucial role in the preservation of other microvascular tissues in skeletal elements from the Mesozoic.
Hollow, pliable, and transparent vessel-like structures have been recovered from skeletal elements of multiple fossil vertebrates, including non-avian dinosaurs1,2. Their vascular affinities have been supported through the application of varied independent methods to identify endogenous component proteins3,4, including collagen, which is not produced by microbes5, and elastin, which is vertebrate-specific6. Mass spectrometry sequencing of isolated vessels recovered from the cortical bone of a non-avian dinosaur further supported the presence of vertebrate-specific vascular proteins in isolated dinosaurian vessels7. The hallmark 67-nm-banding pattern typical of type I collagen has been documented in fossil tissues, following liberation by demineralisation8, and the presence of type I collagen in the vascular canals of a ~190 Mya sauropod dinosaur rib was suggested by synchrotron Fourier-transform infrared spectroscopy and Raman analyses9.
Various mechanisms, including transition metal-catalysed intermolecular crosslinking of structural proteins2,10, have been proposed to explain this unexpected preservation, but experimental testing of these proposed mechanisms has not been widely conducted. Therefore, in this work, our goal was to identify and test for the possible contribution of an explicit set of transition metal-catalysed crosslinking mechanisms to the preservation of vessel-like structures recovered from the compact bone of a Tyrannosaurus rex (USNM 555000 [formerly, MOR 555]), to lay a possible foundation for additional studies of preservation mechanisms for other soft tissues recovered from Mesozoic or more recent fossils.
The walls of vertebrate blood vessels are comprised of three distinct layers, the tunica intima (innermost, also identified as the tunica interna), tunica media, and tunica externa (outermost)11. These layers can be differentiated morphologically and chemically because of their unique molecular composition. Homotypic type I and heterotypic type I/III fibrillar collagen molecules, both of which exhibit 67-nm-banding character and are vertebrate-specific5,12,13,14,15, constitute the predominant collagen fraction of blood vessels (as much as 90%), primarily localizing to the tunica media and tunica externa to serve as the structural foundation of the vessel11,12,16. Elastin, a helical protein also specific to vertebrates6, confers resistance to pressure changes in vascular walls11 and is localized primarily to the tunica media and the basement membrane, which separates the tunica intima from the tunica media17. Thus, we proposed that these proteins could be detectable in some form if the structures investigated in this work were remnant dinosaur vessels, with chemical signatures diagnostic of their current preservation state.
Both elastin and collagen are identifiable by certain hallmark features constrained by their structure and molecular composition. For example, collagen is a repetitive helical protein with every third residue occupied by glycine12, which demonstrates unusual hydroxylation patterns on proline and lysine residues18. The 67-nm-banding motif of fibrillar collagen results from a characteristic head-to-toe stacking pattern and offset of adjacent molecule stacks that results from chemical composition and is critical to mechanical performance12,13,14,15. Elastin is also a highly repetitive helical protein capable of self-assembly, and is comprised of high levels of glycine, proline, and valine19. The tertiary structure of both fibrillar collagens and elastin arises from intramolecular crosslinks formed between lysine residues on adjacent tropocollagen and tropoelastin molecules, respectively, and in living organisms, these pathways are mediated by similar lysyl oxidase (enzymatic) mechanisms (Fig. S1)20,21.
However, intramolecular (and ultimately, intermolecular) crosslinks can also form by non-enzymatic, and hence unregulated, pathways, particularly as tissues age12,22,23. Such pathways have also been studied in association with atherosclerotic plaque formation, changes in hormones, and glucose regulation, among others22,23,24. The presence of reducing sugars contributes to the formation of carbonyl-containing glycation products (see Fig. S1), which then mature into advanced glycation end products via subsequent reaction mechanisms (i.e., AGEs or Maillard reaction products)24,25. Because these pathways are non-enzymatically driven, they can continue after death. These post mortem reactions may contribute significantly to tissue preservation by conferring resistance to degradation to the structural proteins that form the basis for the vessel structure. The existing biomedical and materials engineering literature shows that the accumulation of these non-enzymatic crosslinks between or within structural proteins significantly reduces their susceptibility to common degradation pathways, because as these crosslinks accumulate, vessel walls increase in stiffness12,17,26 and become more resistant to biological turn-over12 and/or enzymatic degradation27.
The involvement of structural proteins in Fenton chemistry and glycation crosslinking pathways yields a suite of diagnostic characters that can be detected, targeted, and characterized using a variety of techniques. For example, the metal-oxide precipitates9 and carbonyl (C=O)-containing crosslinks resulting from these processes (see Fig. S1), together with the formation of end product AGEs, contribute to changes in the spectroscopic properties of tissues24. In particular, finely crystalline iron oxide, which appears reddish-brown in colour depending on oxidation state, has been observed in the walls of ancient vessel tissues recovered from multiple specimens9,10, and the typical brownish hue of fossilised organic tissues has been attributed as much to AGE formation as to the presence of metal-oxide precipitates28.
To test our hypothesis that these early diagenetic processes could have contributed to the survival of these T. rex microvascular structures from deep time, we conducted an actualistic experiment in which non-enzymatic crosslinks of known character were induced in extant chicken type I collagen (recovered from the cortical bone of a chicken tibia) through Fenton and glycation pathways, using reactant concentrations relevant to known vertebrate systems (see Methods). We targeted type I collagen because it is the dominant protein in vertebrate tissues, and we derived our reference tissues from chicken because this species is phylogenetically close to non-avian dinosaurs. Moreover, this protein has been widely characterized and is readily available. Crosslink characteristics in the treated chicken tissues were directly compared with untreated tissues using synchrotron radiation Fourier-transform infrared spectroscopy (SR-FTIR) conducted in transmission mode. Then, we compared both treated and untreated states to our observations of the microvascular tissues recovered from the compact/cortical bone of the T. rex specimen (USNM 555000). Prior to SR-FTIR analysis, we employed optical and electron microscopy methods, small angle X-ray scattering (SAXS), and in situ immunohistochemistry (IHC) to test the endogeneity of these tissues. Finally, micro-focused X-ray fluorescence (µ-XRF) and extended X-ray absorption near-edge structure spectroscopy (µ-XANES) were utilized to document the presence of transition metals in the T. rex tissues and then to determine their chemical speciation, for iron compounds in particular, as further supporting evidence of the likely contribution of these crosslinking mechanisms to vessel tissue preservation.
SR-FTIR analysis of crosslink character in chicken type I collagen
We induced crosslinks in fresh, extant chicken type I collagen using either the Fenton reagent or iron-catalysed glycation29,30, and then used transmission SR-FTIR to analyse each tissue. Curve fitting and second derivative analysis identified locations and relative absorption intensities of key sub-bands of the protein Amide I band, which is consistent with, but not exclusive to, protein secondary structure. The Amide I band of untreated immature type I collagen was observed at ~1633 cm−1 (Fig. 1a), consistent with un-crosslinked (immature) type I collagen30,31,32.
Post-treatment SR-FTIR analysis (Fig. 1b,c) revealed three significant changes to chicken fibrillar collagen profiles when compared to untreated samples. First, treatment with the Fenton reagent (1657 cm−1) and iron-catalysed glycation (1660 cm−1) caused an apparent blue shift in the Amide I band (Fig. 1), as the absorption of the triple-helix (~1658–1660 cm−1)31,33 and intermolecular sub-bands (~1683–1690 cm−1)30,34 increasingly dominated, consistent with changes in the secondary structure of mature collagen due to increased intramolecular crosslinking31,32,33. Second, both glycation and Fenton treatments gave rise to a non-peptide carbonyl band at ~1739 cm−1 (Fig. 1b,c). Prior studies on aged collagenous tissues35, glycated fibrillar collagens25,34,35,36, and demineralised tissues of Mesozoic fossils4,9 all reported this same spectral feature to varying relative intensities, which can result from Fenton-type reactions in the immediate vicinity of peptide sequences36, leading to peptide crosslinking and the subsequent formation of aldehydic carbonyls37, or immature, intramolecular crosslinks (see Fig. S1). Third, a carbohydrate band (~900–1100 cm−1, Fig. S2)25,34 developed in extant tissues after glycation. We report this latter observation simply as evidence of crosslink introduction, but explore the feature no further because the shape of this band is highly dependent on the nature and amount of different sugar molecules present during crosslinking38 (i.e., in this work, we only carried out glycation analyses with D-glucose as a reagent), and because in these chicken tissues, the intramolecular crosslinks that have formed are of the immature variety, lacking exposure to the necessary subsequent pathways to mature into intermolecular crosslinks, or AGEs24,25.
Characterisation of T. rex vessel structures and evidence for endogenous structural proteins
Three types of vessels were liberated from demineralised (see Methods) T. rex cortical bone (Fig. S3), characterised as: (1) extensive, brown-hued, pliable vessel networks (Fig. 2a), (2) fragmented, opaque structures (Fig. S4a), and (3) fragmented, semi-translucent structures (Fig. S4a) under visible light microscopy (VLM). The pliable vessels (1) were hollow, ranged from 10–40 µm in width, and demonstrated branching networks consistent in size and morphology with microvascular tissues in extant bone39. Energy-dispersive X-ray spectroscopy (EDS; Fig. S4c–e) coupled with scanning electron microscopy (SEM) and, separately, µ-XRF spectroscopy (Fig. S5) confirmed that the differences observed in VLM between the soft, transparent (1) and opaque (2) and/or semi-translucent (3) vessels arose from compositional variation between these samples. The opaque (2) vessels were dominated by iron oxide, while the semi-translucent fragments (3) were composed of barium, sulphur, and oxygen. We focused all further analyses on the pliable (1) vessel networks, because they appeared most similar to those observed in extant bone tissue, and thus were presumably less altered.
When analysed by SEM, the pliable T. rex vessels (Fig. 2b) exhibited ordered fibrous structures across their outermost surface. At higher magnification (Fig. 2c), the vessel exteriors were roughly textured and finely striated, exhibiting features morphologically consistent with fibrillar collagen13. These same striated, fibrous features were also observed (Fig. 2d) in longitudinal sections of vessels imaged by transmission electron microscopy (TEM; see Methods). The average structural features included a fibril width of 110 nm, fibre bundle width of 1.0 µm, and ~74-nm periodicity (d-spacing) of fine striations as recorded in SEM (Fig. 2e) and 56 nm, in TEM (Fig. 2f). We used SAXS to determine the periodicity of T. rex fibrillar structures more precisely, calculating a d-spacing of 66.5 nm (Fig. S6).
These combined features are consistent with those seen in extant vessels liberated from cortical bone (see Fig. 3 of reference1), and with fibrillar collagen (predominantly type I in the tunica media and tunica externa of blood vessels11,12,16), which shows striations with an accepted d-spacing of 67 nm40. Similar features have been observed in vessels1 and mineralised fibrils8 recovered from other fossil specimens. Importantly, these vessel networks are too large, and not consistent in morphology, with fungal hyphae41.
The SR-FTIR spectrum of the T. rex vessels was dominated by Amide I and Amide II bands, at values consistent with the absorption bands of extant chicken type I collagen (Fig. 3)36,42,43. The maximum absorption intensity of the Amide I band, corresponding to carbonyl (C=O) stretching, was located at ~1657 cm−1; the Amide II band (N-H bending), at ~1541 cm−1; the CH2 bending vibration also seen in collagen, at ~1458 cm−1; and the C-OH stretching vibrations of carbohydrate moieties (associated with AGE formation)25,34 at ~1036 and ~1066 cm−1 were observed in both the treated extant and ancient tissues. Specifically, the location of the Amide I band for the dinosaur tissue is indicative of a predominant α-helix structure31, consistent with the triple α-helix structure of mature (crosslinked) fibrillar collagen. The C-H stretch (2852 and 2922 cm−1) and non-peptide carbonyl (1739 cm−1) bands can be associated with the presence of lipids and/or proteins25 and are discussed in more detail below. Because this analysis was carried out in transmission mode, all layers of the vessel structures (including the layers exhibiting morphological characters consistent with fibrillar collagen; see Fig. 2b,c) were probed during analysis.
Immunohistochemistry (IHC) of T. rex vessels
The above results indicate that these T. rex tissues are composed of a significant fraction of protein-derived compounds, and possess a degree of structural character consistent with fibrillar collagen. As a corroborating line of evidence, we also conducted in situ IHC analyses to identify and localise to the micron-scale protein-specific epitopes of the structural proteins elastin and type I collagen, and other proteins associated with extant microvascular tissue (actin, tropomyosin, haemoglobin). IHC was selected for identification of protein constituents because of the specificity of the vertebrate immune response, which can be employed to differentiate endogenous proteins associated with blood vessels44 from those arising due to exogenous contaminates45. Specifically, actin proteins constitute the cytoskeleton of blood vessel endothelial cells46 and contribute to the functionality of the thin filaments, along with tropomyosin, in smooth muscle cells47. Tropomyosin is a component of muscle tissues and is localised within the tunica media of vessel walls, where smooth muscle cells reside48. Thus, tropomyosin, actin, and collagen often co-localise in extant vessels at the lower magnifications represented herein. Elastin is a major component of the basement membrane that forms the boundary (i.e., internal elastic lamina) between the endothelial cells of the tunica intima and the collagen and smooth muscle cells forming the tunica media48. Haemoglobin, the major protein within vertebrate erythrocytes (red blood cells), is abundant in highly vascularised bone. When released during post mortem haemolysis, haemoglobin protein can interact with and adsorb onto surrounding tissues; in modern vertebrates, haemoglobin imparts a red hue to bone and the walls of blood vessels10. Thus, these proteins constitute a reasonable suite of targets for IHC techniques, and their in situ identification in fossil blood vessels supports their endogeneity. Concurrently, we tested for reactivity of these vessels to antibodies raised against peptidoglycan, a component of bacterial biofilms, and employed established negative controls to account for non-specific reactivity.
As shown in Fig. 4, antibodies raised against all of the components of extant vasculature that we tested exhibited positive binding to the dinosaur vessel walls. Composite images (Fig. 4a,c,e,g,i,k,m,o) were created by overlaying fluorescence images corresponding to antibody-antigen complexes upon VLM images of vessel sections. A fluorescent filter was used during capture of the adjacent images (Fig. 4b,d,f,h,j,l,n,p), which show the localisation and distribution of antibody-antigen complexes (green fluorescence). Negative controls to account for non-specific binding (Fig. 4a–d) were conducted by exposing vessels to secondary antibodies raised against mouse (a,b) and rabbit (c,d), the host species for antibodies employed. No signal was observed, indicating that spurious binding of the secondary antibodies to the tissues was not responsible for positive signal in the images. The response of these dinosaur vessels to actin antibodies (Fig. 4e,f) was observed as a thin and evenly distributed layer, whereas antibodies raised against the muscle protein tropomyosin (Fig. 4g,h) were bound with greater intensity over a broader portion of the vessel walls, consistent with the distribution of these proteins in extant vessels46,47. The dinosaur vessels also reacted to type I collagen antibodies (Fig. 4i,j), although elastin antibodies were bound with greater intensity (see Fig. 4k,l). These two proteins are highly evolutionarily conserved in certain regions of their respective sequences49,50, making them good targets for fossil studies. Antibodies raised against ostrich haemoglobin10 also showed positive binding, although at comparatively lower intensity (Fig. 4m,n). No reactivity was seen for vessels exposed to antibodies against bacterial peptidoglycan (Fig. 4o,p), eliminating the possibility that these structures arose from microbial contamination45.
Investigation of possible crosslinking mechanisms in T. rex vessel structures
We previously demonstrated that the treatment of extant microvascular tissue with haemoglobin, an Fe-coordinating protein, can significantly enhance stability over multi-year time frames10, in effect acting as a preserving agent. Here, we extend this experimental observation to propose that enhanced resistance to degradation is due in part to Fe-catalysed non-enzymatic crosslinking of molecules comprising structural tissues, with haemoglobin suggested as the primary source of such Fe in vessels undergoing diagenesis.
To test whether post mortem structural protein crosslinking (specifically, on type I collagen) could have enhanced the resistance of these T. rex vessel structures to degradation/diagenetic alteration processes, we employed two experimental approaches: for our first approach, we analysed the spectral features of the dinosaur tissues with the same approach applied to chicken type I collagen, and found that all three significant changes observed in the treated (crosslink-induced) chicken tissues were, to some degree, identifiable in the dinosaur vessel structures. In this work, our focus was specifically on fibrillar collagen (predominantly type I collagen in extant vessel tissues), for several reasons: (1) this structural protein type imparts structural integrity to modern vessels, (2) fibrillar collagen is most abundant in the tunica media and tunica externa, with the potential to encapsulate and protect the innermost contents of fossil vessel networks, and (3) our SEM and TEM imaging studies of these T. rex vessels clearly demonstrated extensive fibrillar surface features on the outermost preserved layers of the vessels as well as in their longitudinal sections.
Using transmission SR-FTIR, the maximum absorption intensity of the Amide I band of the T. rex tissue was observed at 1657 cm−1 (Fig. 5a). Sub-band analysis (Fig. 5a) indicated that this band location was due to increased relative intensities of the triple-helix (~1658–1660 cm−1)31,33 and intermolecular (~1683–1690 cm−1)33,34 sub-bands, as observed in both samples of crosslinked chicken vessels. The maximum absorption intensity of the T. rex Amide I band fell between the Amide I bands recorded for chicken type I collagen crosslinked using Fenton chemistry (1657 cm−1) and Fe-catalysed glycation (1660 cm−1), suggesting that both mechanisms could have contributed to post mortem crosslinking in this tissue.
The prominent non-peptide carbonyl band (Fig. 5b) observed in the dinosaur tissues (1739 cm−1) also developed in the chicken type I collagen tissues treated by both crosslinking mechanisms, because non-peptide carbonyls were introduced within immature, intramolecular crosslink structures25,34,35,36. This same spectral feature has been recorded, but not discussed, in two other works on ancient fossil soft tissues4,9. Concurrently, crosslinking of the chicken tissues enhanced the absorption intensity and prominence of C-H stretch bands, representing aliphatic protein groups at 2850 and 2930 cm−1 (Fig. 1). These same bands exhibited strong absorption in the dinosaur tissues (Fig. 3). Although C-H stretch and non-peptide carbonyl (C=O) bands can also be associated with lipids, the presence of lipids is only supported if strong and sharp (cusp-like) absorption bands associated with C-H bending modes are present in the fingerprint region (~1450 cm−1) and the absorption feature of olefins51 is present at ~3010 cm−1. In contrast, protein methyl group absorption in the region of (1500–1300 cm−1) exhibits a broader, more-rounded character (e.g., chicken spectrum in Fig. 3). Because the spectrum for the T. rex tissue exhibits neither strong, sharp C-H bending modes nor strong olefin absorption, we associated the C-H stretch and non-peptide carbonyl bands observed in the dinosaur tissue with the presence of protein structures.
The T. rex SR-FTIR spectrum also exhibits increased absorption in the carbohydrate region. The shape of the absorption band in this region is dependent on the nature and amount of different sugar molecules present during crosslinking38. In this specimen, the doublet presenting at ~1036 and ~1066 cm−1 (Fig. 3) is highly consistent in energy position, absorption intensity, and overall feature shape with observations of AGE ‘hotspots’ formed in the cardiac tissue of mice fed high-glycemic-index diets (specifically, amylopectin, which is a glucose starch)25. Increased absorption intensity in this same region was observed in both the Fenton chemistry- and glycation-treated chicken type I collagen samples, suggesting that the absorption band in the T. rex tissue could be due to multiple effects. Although a degree of contribution from enzymatic glycosylation52 cannot be ruled out, the combination of features present, in coordination with the carbohydrate band absorption shape, strongly indicate that this feature arises from non-enzymatic crosslinking mechanisms. Furthermore, the differences between the carbohydrate band of T. rex and that of either crosslinked chicken sample are likely due to a difference in crosslink state: the immature, intramolecular crosslinks induced in the chicken tissues lacked exposure to the subsequent pathways necessary for maturation into mature, intermolecular crosslinks (AGEs).
For our second experimental approach, we treated bulk T. rex tissue (Fig. 5c) with NaBH4. This compound reduces the carbonyl group within immature crosslinks, thereby decreasing the non-peptide carbonyl band absorption intensity (see Fig. S1)53. After treatment, we observed significantly lower intensity of the non-peptide carbonyl band at ~1739 cm−1 in the T. rex tissues, suggesting that a significant fraction of the crosslinks in this tissue are immature. The data suggest that this T. rex tissue possesses both intramolecular and intermolecular crosslink types.
Elemental mapping using µ-XRF (Fig. 6a,b,e) revealed that Fe was the only metal concentrated within the dinosaur vessel tissues (Figs. 6c,d,f and S5). Extended µ-XANES at the Fe K-edge on seven tissue locations (Fig. 6g) showed Fe3+ embedded in the vessel walls. These spectra, which were recorded up to 300 eV past the K-edge into the extended X-ray absorption fine structure (EXAFS) region, were used to identify the nature of Fe oxides present by simultaneously fitting several of the distinctive EXAFS features (see Fig. S7). Least-square linear combination fitting of the Fe K-edge XANES spectra, using a published spectral database of >90 Fe standard compounds, showed that these vessels contained finely crystalline goethite (α-FeO(OH)), a mineral we previously observed in vascular tissues recovered from two different dinosaur specimens10.
The identification of still-soft tissues and cellular structures in a suite of Mesozoic fossils1,2,3,4,5,8,10, and claims of endogenous proteins preserved within these materials3,4,8,9,10,28, is controversial because it challenges both conventional wisdom and theoretical kinetics, which preclude the persistence of proteins over geological time scales54,55. Data supporting endogeneity have been viewed with scepticism, in part because no mechanisms have been identified that could reasonably contribute to such preservation.
Our data support the presence of vertebrate-specific endogenous proteins, localized to these soft tissue dinosaur structures, including the presence of a significant quantity of type I collagen, consistent in location and chemistry with the vasculature of extant vertebrates11,12,16. Furthermore, we provide data to support a two-step mechanism that stabilises biomolecules and vessel structures shortly after organismal death, promoting their persistence within densely mineralised skeletal elements.
When biological iron, which exists in the thermodynamically unstable Fe2+ state, is released from complexing molecules, it oxidises rapidly, generating free radicals10,56,57,58 in the conversion from Fe2+ to the more stable and insoluble Fe3+ form. We hypothesise that early in diagenesis, perhaps immediately post mortem, iron-mediated Fenton and glycation pathways contributed to enhanced T. rex tissue longevity by rapidly crosslinking arginine and lysine residues of elastin and fibrillar collagen (and other vascular proteins) within and surrounding the blood vessels. This Fenton-type reaction would have been heavily favoured by conditions of oxidative stress as Fe-containing haemoglobin was liberated into and degraded within the vessel lumen during haemolysis56,57,58,59. The iron would have first bound to a metal-binding site on collagen, normally occupied by Ca, producing hydroxyl radicals that would then have instantaneously reacted with local amine groups10, leading to aldol condensation and crosslinking among adjacent protein molecules. Alternatively, or perhaps simultaneously, autoxidised carbohydrates in non-enzymatic glycation would have undergone condensation with the terminal amine groups of lysine, leading to ketoaldehyde formation and protein crosslinking. Both processes are catalysed by transition metal species, including iron60, and hence would have driven crosslinking in the immediate vicinity of the Fe catalyst10. Hence, the central role of Fe in structural protein crosslinking also provides a causal mechanism to explain the observations of intimately associated and distributed iron oxyhydroxides within the dinosaur tissues reported here. This idea is fully supported by the formation of iron oxyhydroxide precipitates observed in the walls of extant vascular tissues incubated in haemoglobin, and ancient vascular tissues recovered from other dinosaur specimens10.
Overall, the role of iron in generating free radicals is central to both the Fenton reaction and transition metal-catalysed glycation, and the immature, intramolecular crosslinks resulting from both pathways exhibit non-peptide carbonyl functional groups, which have been recorded, although not commented on, in other spectral analyses of ancient tissues4,9. We show that the chemical complexity of crosslinks in the dinosaur structural proteins varies widely, with the presence of both mature, intermolecular crosslinks identifiable via SR-FTIR Amide I sub-band analysis31,32,33 and based on the shape of the carbohydrate absorption band in the T. rex tissue (consistent with AGEs)25 and immature crosslinks verified by treatment with the reducing agent NaBH453. Although lipid peroxidation can also give rise to a carbonyl band at the same energy as the non-peptide carbonyl band resulting from intramolecular crosslinking, the full FTIR profile of a lipid is distinct from that of a protein. The T. rex tissues were found to exhibit a predominantly proteinaceous character, strongly indicating that the majority of the carbonyl groups in this sample derive from crosslinks associated with protein compounds. Molecular crosslinks (essentially, hyper-crosslinking) would have afforded exceptional resistance to mechanical, biological, and thermal degradation12,17,26,27,61,62,63,64. Moreover, post mortem lipid peroxidation events would have resulted in cell membrane degradation65, contributing to increased diffusion of serum proteins (e.g., haemoglobin) and myoglobin-containing Fe in smooth muscle cells to the structural components of vessel walls during short-term diagenesis. In contrast, lipoprotein oxidation events associated with ROS-mediated mechanisms could lead to the uptake of these compounds into vessel walls; therefore, it would not be unreasonable to expect the observation of lipoprotein plaque deposition in other fossil soft tissues, similar to atherosclerotic plaque formation in living systems65.
The extensive presence of finely crystalline goethite (α-FeO(OH)) in these fossil vessels suggests that conditions favoured thermodynamically-driven nucleation over kinetically-driven growth, and that this mineral formed on a large number of distributed nucleation sites (i.e., Ca-binding sites), as previously demonstrated9. In accordance with the fundamentals of mass transfer phenomena, diffusion mechanisms are aided by factors such as small crystallite size (large surface area), elevated temperature, solubility (Ksp), pH, and/or long time periods. Ultimately, growth within the sub-microscopic features of the microvascular walls would have intrinsically restricted crystallite size.
Goethite formation from aqueous ferrihydrite (Fe3+) significantly predominates over haematite in the range from pH 4 (>95% goethite) to pH 5 (>80% goethite)66, with the highest crystallinity of goethite exhibited at pH 466. Goethite solubility at neutral pH is extraordinarily low66. In this work and in our previous study10, we observed the presence of finely crystalline goethite throughout the fossil blood vessels investigated, suggesting that the mineral formed under acidic pH, which is consistent with the development of a hypoxic post mortem environment67. Over time, the vessel cavity pH would have been regulated primarily by ground water and the strong buffering capacity of bone mineral67,68, maintaining values near neutral pH and, as a result, preventing goethite dissolution. Micromobilisation of apatite crystals from the encapsulating bone onto the vessel walls could have provided a secondary form of stabilisation via encapsulation (note that such crystals would have been removed by the demineralisation process used to liberate the T. rex vessels in this work, and hence would not have been observed during microscopy studies). Therefore, we argue that such formation conditions are consistent with the Fe-catalysed crosslinking mechanisms tested in this work, and not of exogenous, geological origin.
We provide additional support for our hypothesis by demonstrating that both chemical pathways tested herein were capable of inducing crosslink formation in chicken type I collagen tissues within 48 h at reactant concentrations consistent with anticipated values in dinosaur blood systems (see Methods). Such observations reinforce the likely role of Fenton- and glycation-type transition metal (Fe)-catalysed pathways in the early and rapid diagenetic stabilisation of microvascular tissues in the burial environment. As we have previously shown, Fe in haemoglobin compounds can significantly enhance microvascular tissue stability over multi-year time frames10.
These data represent the first comprehensive chemical and molecular characterisation of vascular tissues recovered from this T. rex specimen (USNM 555000). By combining synchrotron and laboratory techniques with verified and well-understood immunological, diffraction, and microscope imaging methods, we provide the first identification of reducible, intramolecular (immature) and irreducible, intermolecular (mature) crosslinks in preserved, ancient vessel tissues. These data strongly support the previous hypothesis10 invoking transition metal (Fe)-mediated mechanisms as an agent of vessel preservation. Exposure of extant chicken type I collagen tissues to Fenton chemistry and transition metal-catalysed glycation rapidly induces chemical modifications also observed in the dinosaur tissues studied here.
In addition to these inherent molecular features conferring resistance to degradation in tissues that possess them, the sequestration of proteinaceous components within mineralised tissue has also been demonstrated to promote longevity, by restricting degradative pathways in the immediate and long-term post mortem environment69,70. We hypothesize that the enzymatic and non-enzymatic pathways described herein, coupled with adsorbance to the mineralized components of bone, can result in exceptional preservation of the original organic components of dinosaurian vascular tissues.
We have shown that actualistic taphonomy provides mechanisms for preserving endogenous soft tissues previously considered impossible, that these mechanisms provide a means for preserving constituent molecules to the degree that they may shed light on evolutionary relationships, and that certain aspects of the immediate microenvironments of degradation can be deduced by examining the chemistry of preservation. These results confirm earlier findings1,2,3,7, and those reported in other studies4,8, and shed light on the possible suite of processes involved in fossilisation at the molecular level. The ability to localize structural proteins within vascular tissues and correlate these observations to chemical and structural alterations in fossil soft tissues will contribute to the development of a comprehensive model of mechanisms that contribute to vascular tissue survival from deep time.
For a detailed description of the methods and techniques used, please see the Supplementary Information.
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The authors acknowledge the supporting contributions, both technical and material, of Dr. Ping Hu (LBNL) toward the preparation of chicken tissues for FTIR, of Eric Schaible (LBNL), Dr. Robert Ritchie (UC-Berkeley/LBNL), and Dr. Claire Acevedo (LBNL) toward the SAXS analyses, and of Dr. John R. Horner (Museum of the Rockies) toward the T. rex specimen tissues. All synchrotron work was performed at the Advanced Light Source, Lawrence Berkeley National Laboratory, which is supported by the U.S. Department of Energy, Office of Science, Office of Basic Energy Sciences. The Berkeley Synchrotron Infrared Structural Biology (BSISB) program is funded by the U.S. Department of Energy, Office of Science, Office of Biological and Environmental Research. Both were through Contract No. DE-AC02-05CH11231.
The authors declare no competing interests.
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Boatman, E.M., Goodwin, M.B., Holman, H.N. et al. Mechanisms of soft tissue and protein preservation in Tyrannosaurus rex. Sci Rep 9, 15678 (2019) doi:10.1038/s41598-019-51680-1
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