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.2016 Dec 12;11(12):e0168042.
doi: 10.1371/journal.pone.0168042. eCollection 2016.

Biomolecular Evidence of Silk from 8,500 Years Ago

Affiliations

Biomolecular Evidence of Silk from 8,500 Years Ago

Yuxuan Gong et al. PLoS One..

Abstract

Pottery, bone implements, and stone tools are routinely found at Neolithic sites. However, the integrity of textiles or silk is susceptible to degradation, and it is therefore very difficult for such materials to be preserved for 8,000 years. Although previous studies have provided important evidence of the emergence of weaving skills and tools, such as figuline spinning wheels and osseous lamellas with traces of filament winding, there is a lack of direct evidence proving the existence of silk. In this paper, we explored evidence of prehistoric silk fibroin through the analysis of soil samples collected from three tombs at the Neolithic site of Jiahu. Mass spectrometry was employed and integrated with proteomics to characterize the key peptides of silk fibroin. The direct biomolecular evidence reported here showed the existence of prehistoric silk fibroin, which was found in 8,500-year-old tombs. Rough weaving tools and bone needles were also excavated, indicating the possibility that the Jiahu residents may possess the basic weaving and sewing skills in making textile. This finding may advance the study of the history of silk, and the civilization of the Neolithic Age.

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Conflict of interest statement

The authors have declared that no competing interests exist.

Figures

Fig 1
Fig 1. Tombs M436 (a), M451 (b), and M466 (c).
The positions where the relic body soil samples were collected are indicated by the arrows and shown in the separate images. The four black dots indicate the locations where the control samples were collected.
Fig 2
Fig 2. MS/MS results of PeptideGAGAGAGY.
This figure shows data-dependent acquisition using the LTQ-Orbitrap XL for the peptide at m/z 623.27698 (GAGAGAGY) in Table 2 (M436 no. 1). The b- and y-type ion fragments of the peptide after CID in MS/MS.
Fig 3
Fig 3. MS/MS results of PeptideGAGAGSGAGSGAGAGSGAGAGY.
This figure shows data-dependent acquisition using the LTQ-Orbitrap XL for the peptide at m/z 784.34058 (GAGAGSGAGSGAGAGSGAGAGY) in Table 2 (M436 no. 2). The b- and y-type ion fragments of the peptide after CID in MS/MS.
Fig 4
Fig 4. MS/MS results of PeptideGAGVGAGY.
This figure shows data-dependent acquisition using the LTQ-Orbitrap XL for the peptide at m/z 651.30884 (GAGVGAGY) in Table 2 (M436 no. 3). The b- and y-type ion fragments of the peptide after CID in MS/MS.
Fig 5
Fig 5. MS/MS results of PeptideGAGAGSGAGSGAGAGSGAGAGY.
This figure shows data-dependent acquisition using the LTQ-Orbitrap XL for the peptide at m/z 784.34003 (GAGAGSGAGSGAGAGSGAGAGY) in Table 2 (M451 no. 4). The b- and y-type ion fragments of the peptide after CID in MS/MS.
Fig 6
Fig 6. MS/MS results of PeptideGAGAGAGY.
This figure shows data-dependent acquisition using the LTQ-Orbitrap XL for the peptide at m/z 623.27789 (GAGAGAGY) in Table 2 (M451 no. 5). The b- and y-type ion fragments of the peptide after CID in MS/MS.
Fig 7
Fig 7. MS/MS results of PeptideGAGAGSGAASGAGAGAGAGAGTGSSGF.
This figure shows data-dependent acquisition using the LTQ-Orbitrap XL for the peptide at m/z 969.93207 (GAGAGSGAASGAGAGAGAGAGTGSSGF) in Table 2 (M451 no. 6). The b- and y-type ion fragments of the peptide after CID in MS/MS.
See this image and copyright information in PMC

References

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