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Sub-micron spongiform porosoity is the major ultra-structural alteration occurring in archaeological bone

Lookup NU author(s): Dr Gordon Turner-Walker, Dr Christina Nielsen-Marsh, Dr Matthew Collins

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Abstract

Total pore volume and pore size distribution are indicators of the degree of post-mortem modification of bone. Direct measurements of pore size distribution in archaeological bones using mercury intrusion porosimetry (HgIP) and back scattered scanning electron microscopy (BSE-SEM) reveal a common pattern int he changes seen in degraded bone as compared to modern samples. The estimates of pore size distribution from HgIP and direct measurement from the BSE-SEM images show remarkable correspondence. The coupling of these two independent approaches has allowed the diagenetic porosity changes in human archaeological bone in the >0.01 mum range to be directly imaged, and their relationship to pre-existing physiological pores to be explored. The increase in porosity in the archaeological bones is restricted to two discrete pore ranges. The smaller of these two rangers (0.007-0.1 mum) lies in the range of the collagen fibril (0.1 mum) diameter) and is presumably formed by the loss of collagen, whereas the large pore size distribution is evidence of direct microbial alteration of the bone. HgIP has great potential for the characterization of microbial and chemical alteration of bone.


Publication metadata

Author(s): Turner-Walker G, Nielsen-Marsh CM, Syversen U, Kars H, Collins MJ

Publication type: Article

Publication status: Published

Journal: International Journal of Osteoarchaeology

Year: 2002

Volume: 12

Issue: 6

Pages: 407-414

ISSN (print): 1047-482X

ISSN (electronic): 1099-1212

Publisher: John Wiley & Sons Ltd.

URL: http://dx.doi.org/10.1002/oa.642

DOI: 10.1002/oa.642


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