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Volumn 110, Issue 3, 1999, Pages 233-239

Amino acid dating of a molluscan fauna from Bassingham Fen, Lincolnshire: Implications for the chronology of the Trent Terraces

Author keywords

[No Author keywords available]

Indexed keywords

AMINO ACID; DATING METHOD; FEN; GEOCHRONOLOGY; MOLLUSC; SAND AND GRAVEL;

EID: 0032702482     PISSN: 00167878     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0016-7878(99)80073-X     Document Type: Article
Times cited : (8)

References (24)
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  • 2
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    • BOWEN, D. Q., HUGES, S., SYKES, G. A. & MILLER, G. H. 1989. Land-sea correlations in the Pleistocene based on isoleucine epimerization in non-marine molluscs. Nature, 340, 49-51.
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  • 3
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    • BRANDON, A. & SUMBLER, M. G. 1988. An Ipswichian fluvial deposit at Fulbeck, Lincolnshire and the chronology of the Trent terraces. Journal of Quaternary Science, 3, 127-133.
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    • Brandon, A.1    Sumbler, M.G.2
  • 4
    • 0026281501 scopus 로고
    • The Balderton Sand and Gravel: PreIpswichian cold stage fluvial deposits near Lincoln, England
    • 1991. The Balderton Sand and Gravel: preIpswichian cold stage fluvial deposits near Lincoln, England. Journal of Quaternary Science, 6, 117-138.
    • (1991) Journal of Quaternary Science , vol.6 , pp. 117-138
  • 6
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    • The utilization of Arctic river analogue studies in the interpretation of periglacial river sediments from southern Britain
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    • (1983) Background to Palaeohydrology , pp. 413-1131
    • Bryant, I.D.1
  • 8
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    • Holyoak, D.T.1
  • 12
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    • Non-marine molluscan faunas of periglacial deposits in Britain
    • Boardman, J.; ed. Cambridge University Press, Cambridge
    • KEEN, D. H. 1987. Non-marine molluscan faunas of periglacial deposits in Britain. In (Boardman, J.; ed.) Periglacial landfonns in Britain and Ireland. Cambridge University Press, Cambridge, 257-263.
    • (1987) Periglacial Landfonns in Britain and Ireland , pp. 257-263
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    • MARTINSON, D. G., PISIAS, N. G., HAYS, J. D., IMBRIE, J., MOORE, T. C. & SHACKLETON, N. J. 1987. Age dating and the orbital theory of the Ice Ages: development of a highresolution 0 to 300,000-year chronostratigraphy. Quaternary Research, 27, 1-29.
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