Earliest evidence for the use of pottery



Pottery was a hunter-gatherer innovation that first emerged in East Asia between 20,000 and 12,000 calibrated years before present1,2 (cal bp), towards the end of the Late Pleistocene epoch, a period of time when humans were adjusting to changing climates and new environments. Ceramic container technologies were one of a range of late glacial adaptations that were pivotal to structuring subsequent cultural trajectories in different regions of the world, but the reasons for their emergence and widespread uptake are poorly understood. The first ceramic containers must have provided prehistoric hunter-gatherers with attractive new strategies for processing and consuming foodstuffs, but virtually nothing is known of how early pots were used. Here we report the chemical analysis of food residues associated with Late Pleistocene pottery, focusing on one of the best-studied prehistoric ceramic sequences in the world, the Japanese Jōmon. We demonstrate that lipids can be recovered reliably from charred surface deposits adhering to pottery dating from about 15,000 to 11,800 cal bp (the Incipient Jōmon period), the oldest pottery so far investigated, and that in most cases these organic compounds are unequivocally derived from processing freshwater and marine organisms. Stable isotope data support the lipid evidence and suggest that most of the 101 charred deposits analysed, from across the major islands of Japan, were derived from high-trophic-level aquatic food. Productive aquatic ecotones were heavily exploited by late glacial foragers3, perhaps providing an initial impetus for investment in ceramic container technology, and paving the way for further intensification of pottery use by hunter-gatherers in the early Holocene epoch. Now that we have shown that it is possible to analyse organic residues from some of the world’s earliest ceramic vessels, the subsequent development of this critical technology can be clarified through further widespread testing of hunter-gatherer pottery from later periods.

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Figure 1: Locations of sites sampled and temporal changes in early pottery production against Greenland ice-core oxygen isotope record.
Figure 2: Bulk carbon and nitrogen stable isotope ratios and fatty acid stable carbon isotope ratios from Incipient Jōmon pottery.
Figure 3: Partial gas chromatograms of a lipid extract from a charred deposit adhering to a Torihama potsherd (12,000 cal bp).


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We thank the Leverhulme trust (F/00 152/AM) and the Japanese Society for the Promotion of Science (PE 11560) for their support. We are grateful to K. Adachi, K. Higashi, Y. Kasai, H. Kato, K. Nagahama, H. Oguma, T. Tsuchiya, T. Watanabe and T. Yamahara for providing access to samples.

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O.E.C., H.S., Y.N., S.I. and P.J. planned the project. O.E.C. wrote the paper with assistance from all other authors. P.J., H.S., Y.N. and K.G. carried out sampling with assistance of M.A. and J.U., who provided contextual data. O.E.C., H.S., A.L., K.T., D.A. and A.T. carried out the lipid analysis. C.P.H. and L.C. carried out the bulk stable isotope analyses. All authors commented on the manuscript.

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Correspondence to O. E. Craig.

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The authors declare no competing financial interests.

Supplementary information

Supplementary Information

This file contains Supplementary Tables 1-4 and Supplementary References. Tables 1-4 contain contextual details (including radiocarbon dates) of each of the sites investigated, a summary of the lipid residue analysis results, bulk isotope characteristics of each sample analysed and a summary of the reference isotope values used to derive the fields in Figure 2B. (PDF 280 kb)

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Craig, O., Saul, H., Lucquin, A. et al. Earliest evidence for the use of pottery. Nature 496, 351–354 (2013). https://doi.org/10.1038/nature12109

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