Revised open system U-series/ESR age calculations for teeth from Stratum C at the Hoxnian Interglacial type locality, England

Rainer Grün; Henry P. Schwarcz

doi:10.1016/S0277-3791(00)00085-8

Revised open system U-series/ESR age calculations for teeth from Stratum C at the Hoxnian Interglacial type locality, England

Rainer Grün^*, Henry P. Schwarcz

^*Corresponding author for this work

Research output: Contribution to journal › Article › peer-review

74 Citations (Scopus)

Abstract

Re-calculation of previously published U-series/ESR age results in two teeth from Layer C of the type locality of the Hoxnian Interglacial resulted in a mean age of 404_-42/⁺³³ ka. This age indicates that the deposition of this layer took place during Oxygen Isotope Stage (OIS) 11, possibly at the boundary to OIS 10. (C) 2000 Elsevier Science Ltd.

Original language	English
Pages (from-to)	1151-1154
Number of pages	4
Journal	Quaternary Science Reviews
Volume	19
Issue number	12
DOIs	https://doi.org/10.1016/S0277-3791(00)00085-8
Publication status	Published - Jul 2000

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10.1016/S0277-3791(00)00085-8

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title = "Revised open system U-series/ESR age calculations for teeth from Stratum C at the Hoxnian Interglacial type locality, England",

abstract = "Re-calculation of previously published U-series/ESR age results in two teeth from Layer C of the type locality of the Hoxnian Interglacial resulted in a mean age of 404-42/+33 ka. This age indicates that the deposition of this layer took place during Oxygen Isotope Stage (OIS) 11, possibly at the boundary to OIS 10. (C) 2000 Elsevier Science Ltd.",

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AB - Re-calculation of previously published U-series/ESR age results in two teeth from Layer C of the type locality of the Hoxnian Interglacial resulted in a mean age of 404-42/+33 ka. This age indicates that the deposition of this layer took place during Oxygen Isotope Stage (OIS) 11, possibly at the boundary to OIS 10. (C) 2000 Elsevier Science Ltd.

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Revised open system U-series/ESR age calculations for teeth from Stratum C at the Hoxnian Interglacial type locality, England

Abstract

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