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      Proteome degradation in fossils: investigating the longevity of protein survival in ancient bone

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      Rapid Communications in Mass Spectrometry
      BlackWell Publishing Ltd

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          Abstract

          RATIONALE

          We report the use of proteomics techniques to study how the fossil bone proteome changes in complexity over one million years.

          METHODS

          We include the attempted use of a previously unreported methodology in proteome research, to remove the dominant bone collagens using bacterial collagenase as well as conventional shotgun proteomics methodology following digestion with the protease trypsin. In this study we expand upon a set of 19 bovine sub-fossil specimens ranging over one and a half million years that had previously been shown to possess collagen, using a total of 46 LTQ-Orbitrap liquid chromatography/tandem mass spectrometry (LC/MS/MS) analyses containing 462,186 precursor ion analyses.

          RESULTS

          Although many types of proteins can typically be identified in recent bone, in degraded bone we observe a rapid loss of lower abundance proteins. Abundant serum proteins such as serum albumin and alpha-2-HS-glycoprotein appear to be more easily recovered in ancient bone, both being identified in specimens dating to the Early Pleistocene, the earliest period tested in this study. Proteins belonging to the leucine-rich repeat family such as lumican, biglycan and chondroadherin also survive well, possibly because of their interactions with bone collagen.

          CONCLUSIONS

          Of these 'survivor proteins' A2HSG shows a remarkable amount of sequence variation, making it potentially one of the most useful proteins to study for species identification and phylogenetic inference in archaeological and palaeontological bone.

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          Most cited references45

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          Bone diagenesis: an overview of processes

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            Early Pleistocene human occupation at the edge of the boreal zone in northwest Europe.

            The dispersal of early humans from Africa by 1.75 Myr ago led to a marked expansion of their range, from the island of Flores in the east to the Iberian peninsula in the west. This range encompassed tropical forest, savannah and Mediterranean habitats, but has hitherto not been demonstrated beyond 45 degrees N. Until recently, early colonization in Europe was thought to be confined to the area south of the Pyrenees and Alps. However, evidence from Pakefield (Suffolk, UK) at approximately 0.7 Myr indicated that humans occupied northern European latitudes when a Mediterranean-type climate prevailed. This provided the basis for an 'ebb and flow' model, where human populations were thought to survive in southern refugia during cold stages, only expanding northwards during fully temperate climates. Here we present new evidence from Happisburgh (Norfolk, UK) demonstrating that Early Pleistocene hominins were present in northern Europe >0.78 Myr ago when they were able to survive at the southern edge of the boreal zone. This has significant implications for our understanding of early human behaviour, adaptation and survival, as well as the tempo and mode of colonization after their first dispersal out of Africa.
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              The thermal history of human fossils and the likelihood of successful DNA amplification.

              Recent success in the amplification of ancient DNA (aDNA) from fossil humans has led to calls for further tests to be carried out on similar material. However, there has been little systematic research on the survival of DNA in the fossil record, even though the environment of the fossil is known to be of paramount importance for the survival of biomolecules over archaeological and geological timescales. A better understanding of aDNA survival would enable research to focus on material with greater chances of successful amplification, thus preventing the unnecessary loss of material and valuable researcher time. We argue that the thermal history of a fossil is a key parameter for the survival of biomolecules. The thermal history of a number of northwest European Neanderthal cave sites is reconstructed here and they are ranked in terms of the relative likelihood of aDNA survival at the sites, under the assumption that DNA depurination is the principal mechanism of degradation. The claims of aDNA amplification from material found at Lake Mungo, Australia, are also considered in the light of the thermal history of this site.
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                Author and article information

                Journal
                Rapid Commun Mass Spectrom
                Rapid Commun. Mass Spectrom
                rcm
                Rapid Communications in Mass Spectrometry
                BlackWell Publishing Ltd (Oxford, UK )
                0951-4198
                1097-0231
                30 March 2014
                12 February 2014
                : 28
                : 6
                : 605-615
                Affiliations
                Faculty of Life Sciences, Manchester Institute of Biotechnology 131 Princess Street, Manchester, M1 7DN, UK
                Author notes
                *Correspondence to: M. Buckley, Faculty of Life Sciences, Manchester Institute of Biotechnology, 131 Princess Street, Manchester M1 7DN, UK., E-mail: m.buckley@ 123456manchester.ac.uk
                Article
                10.1002/rcm.6821
                4282581
                24519823
                7bd8c23f-a6f1-4881-9c81-a60c3cde435a
                © 2014 The Authors. Rapid Communications in Mass Spectrometry published by John Wiley & Sons Ltd.

                This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited.

                History
                : 14 October 2013
                : 23 December 2013
                : 30 December 2013
                Categories
                Research Articles

                Analytical chemistry
                Analytical chemistry

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