Abstract
We use authentication tests developed for ancient DNA to evaluate claims by Asara et al. of collagen peptide sequences recovered from mastodon and Tyrannosaurus rex fossils. Although the mastodon passes, absence of amino acid composition data, lack of evidence for peptide deamidation, and association of the α1(I) peptide sequences with amphibians not birds, suggests that T. rex does not.
Comment
Early reports of DNA preservation in multi-million year old bones (i.e. dinosaurs) have been largely dismissed (see 1 and SOM T1, 2) but reports of protein recovery are persistent (see 3 for review). Most of these studies used secondary methods of detection, but protein sequence, arguably the gold standard for molecular palaeontology, has now been claimed for the first time (2). Following initial optimism generated by reports of dinosaur DNA, there arose a gradual awareness of the problems and pitfalls which bedevil analysis of ancient samples (1), leading to a series of recommendations for future analysis (1, 4). As yet, there are no equivalent standards for fossil protein, so here we apply the recommended tests for DNA (4) to the authentication of the reported protein sequences (2) (Table 1).
Table 1.
Test | Sample | Pass | Observation |
---|---|---|---|
Does the age, environmental history and preservation of the sample suggest collagen survival? | Mastodon 300-600 ka | Collagen t½ @ 7.5 °C = 130 ka | |
T. rex 65 Ma | Collagen t½ @ 20 °C = 2 ka | ||
Does the biomolecular and/or macromolecular preservation of the sample, the molecular target, the innate nature of the sample and its handling history suggest that contamination is a risk? | Biomolecular preservation | ? | Range of evidence presented (8) but no amino acid compositional data. |
Macromolecular preservation | ...but macromolecular ≠ biomolecular preservation (9). | ||
Molecular target | |||
Handling history | ...but large (2.5 g) samples processed | ||
Do the data suggest that the sequence is authentic, rather than the result of damage, and contamination? | Errors in interpretation of spectra (see SOM Table 1 and 13)? Damage induced errors in sequence. | ||
Do the results make sense, and are there enough data to make the study useful and/or support the conclusions? | Mastodon | Weak affinity to mammals | |
T. rex | Affinity of α1(I) peptides amphibians, not birds or reptiles |
Likelihood of collagen survival
The extremely hierarchical structure of collagen results in unusual, catastrophic degradation (5) as a consequence of fibril collapse. The rate of collagen degradation in bone is slow because the mineral ‘locks’ the components of the matrix together, preventing helical expansion which is a pre-requisite of fibril collapse (6). The packing which stabilises collagen fibrils (6) also increases the temperature sensitivity of degradation (Ea 173 kJ mol-1; Fig. 1). Collagen decomposition would be much faster in the T. rex buried in the then megathermal (>20 °C) (7) environment of the Hell Creek formation (collagen t ½ ~ 2 ka) than it would have been in the mastodon lying within the Doeden Gravel Beds (present day mean temperature 7.5 °C; collagen t ½ 130 ka; Fig. 1).
Risk of contamination
The molecular target (collagen) is ideal for this investigation; the protein has a highly characteristic motif and yet also is sufficiently variable to enable meaningful comparison between distant taxa if sufficient sequence is obtained (Fig. 2). In comparison with ancient DNA amplification, contamination by collagen is inherently less likely. Furthermore because the bones were excavated by the authors, obvious contamination sources such as animal glue (used in conservation) can be excluded. Concentrating protein from the large amounts of bone used (2.5 g) may have heightened the risk of extraneous proteins entering the sample during extraction, but there have been no systematic studies of this phenomenon. Independent extraction and analyses would have strengthened claims for the authenticity of the origin of the peptides (and potentially ameliorated the original problems of data interpretation) (4).
The remarkable soft-tissue preservation of the investigated T. rex specimen (MOR 1125) has been documented (8); however microscopic preservation does not equal molecular preservation (9). Immunohistochemistry provides support for collagen preservation, although no data regarding inhibition assays with collagen from different species or cross-reactivity with likely contaminants (e.g. fungi 10) are presented. Curiously no amino acid compositional analysis was conducted (c.f. 11) although immonium ions were identified (by TOF-SIMS). In our experience, collagen-like amino acid profiles have been obtained in all bones from which we could obtain collagen sequence (Fig. 1, inset).
Proof of sequence authenticity
The spectra (12) (SOM of 12) are inconsistent with many of the original sequence assignments (13, 14) (SOM Table 1 and 13). A common diagenetic modification, deamidation, not considered in the original publication, may shed light on authenticity. The facile succinimide mediated deamidation of N1156G (14) occurred in peptide Ost 5 (see Table 1 of 13 for nomenclature) from ostrich, presumably during sample preparation. Direct hydrolytic deamidation is slower (14) and an expectation of elevated levels of such products is reasonable for old samples. We agree with the new interpretation (13) of the spectrum illustrated in Fig. 2b of 3 as α1(I) G362SEGPEGVR370, the deamidated (Q→E367) form of the sequence found in most mammals (12). By way of contrast, none of the three glutamine residues in “T. rex” peptides are deamidated (Table S1 SOM). Only time will tell if Q→E is a useful marker for authentically old collagen, but from the evidence presented the mastodon sequence looks more diagenetically altered than T. rex.
The unusual, fragmented nature of the reported T. rex sequence does not make it amenable to standard, model-based phylogenetic analysis. Instead, we examined the phylogenetic signal of the α1(I) fragments of mastodon and T. rex using Neighbor-Net analysis and uncorrected genetic distances. Using the originally reported sequences (2), both the T. rex and mastodon signal displayed an affinity with amphibians (Fig. 2a) (12). Our re-interpretation of the spectra changes the affinity of mastodon but not of T. rex (Fig. 2b). Two other peptides are reported from T. rex (3); we question the interpretation of the (frog) α1(II) spectrum, but not the α2(I) assignment which is identical to chicken.
We require more data to be convinced of the authenticity of the T. rex collagen. Nevertheless, the handful of spectra reported for the temperate Pleistocene mastodon fail neither phylogenetic nor diagenetic tests, highlighting the potential of protein mass spectrometry to bridge the present gulf in our understanding between the fate of archaeological and fossil proteins (Fig 1.). In order to avoid past mistakes of ancient DNA research(1), we would recommend that future fossil protein claims are considered in the light of tests for authenticity such as those we have used.
Supplementary Material
Acknowledgments
This work was supported by NSF (EAR-0309467), NERC (NE511148, GR9/01656), NCRR (P41-18627), EU (MEST-CT-2004-007909, MEST-CT-2005-020601), Wellcome Trust Bioarchaeology Fellowships (KP, HK) Analytical Chemistry Trust Fund, the RSC Analytical Division, EPSRC, and the Michigan Proteome Consortium.
References
- 1.Willerslev E, Cooper A. Proceedings of the Royal Society of London Series B-Biological Sciences. 2005 Jan 7;272:3. [Google Scholar]
- 2.Asara JM, Schweitzer MH, Freimark LM, Phillips M, Cantley LC. Science. 2007 Apr 13;316:280. doi: 10.1126/science.1137614. 2007. [DOI] [PubMed] [Google Scholar]
- 3.Schweitzer MH. Palaeontologia Electronica. 2002;5 [Google Scholar]
- 4.Gilbert MTP, Bandelt H-J, Hofreiter M, Barnes I. Trends in Ecology and Evolution. 2005 Oct;20:541. doi: 10.1016/j.tree.2005.07.005. 2005. [DOI] [PubMed] [Google Scholar]
- 5.Collins MJ, Riley MS, Child AM, Turner-Walker G. Journal of Archaeological Science. 1995;22:175. [Google Scholar]
- 6.Miles CA, Ghelashvili M. Biophysical Journal. 1999;76:3243. doi: 10.1016/S0006-3495(99)77476-X. [DOI] [PMC free article] [PubMed] [Google Scholar]
- 7.Johnson KR, Nichols DJ, Hartman JH. The Hell Creek Formation and the Cretaceous-Tertiary Boundary in the northern Great Plains: Geological Society of America Special Paper. 2002;361:503–510. [Google Scholar]
- 8.Schweitzer MH, et al. Science. 2007 Apr 13;316:277. 2007. [Google Scholar]
- 9.Gupta NS, Briggs DEG, Pancost RD. Journal of the Geological Society. 2006 Nov;163:897. [Google Scholar]
- 10.Sepulveda P, et al. Infect. Immun. 1995 Jun 1;63:2173. doi: 10.1128/iai.63.6.2173-2179.1995. [DOI] [PMC free article] [PubMed] [Google Scholar]
- 11.Schweitzer M, Hill CL, Asara JM, Lane WS, Pincus SH. Journal of Molecular Evolution. 2002 Dec 01;55:696. doi: 10.1007/s00239-002-2365-6. 2002. [DOI] [PubMed] [Google Scholar]
- 12.Supplementary, Material.
- 13.Asara JM, et al. Science. 2007 Sep 7;317:1324. doi: 10.1126/science.317.5843.1324. [DOI] [PubMed] [Google Scholar]
- 14.Robinson NE, et al. Journal of Peptide Research. 2004;63:426. doi: 10.1111/j.1399-3011.2004.00151.x. [DOI] [PubMed] [Google Scholar]
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