The δ18O stratigraphy of the Hoxnian lacustrine sequence at Marks Tey, Essex, UK: Implications for the climatic structure of MIS 11 in Britain

Journal of Quaternary Science

Volumn 31, Issue 2, 2016, Pages 75-92

  Tye, G J ^a   Sherriff, J ^a   Candy, I ^a   Coxon, P ^b   Palmer, A ^a   Mcclymont, E L ^c   Schreve, D C ^a  

^a UNIVERSITY OF LONDON   (United Kingdom)

^b TRINITY COLLEGE DUBLIN   (Ireland)

^c DURHAM UNIVERSITY   (United Kingdom)

Author keywords

Abrupt event; Hoxnian; Interglacial; Marine Isotope Stage 11; 18O and 13C

Indexed keywords

HOLOCENE; HOXNIAN; INTERGLACIAL; LACUSTRINE DEPOSIT; LITHOSTRATIGRAPHY; MARINE ISOTOPE STAGE; OXYGEN ISOTOPE; PALEOCLIMATE; SEDIMENT CORE; SEQUENCE STRATIGRAPHY;

ENGLAND; ESSEX [ENGLAND]; UNITED KINGDOM;

EID: 84961279096     PISSN: 02678179     EISSN: 10991417     Source Type: Journal    
DOI: 10.1002/jqs.2840     Document Type: Article

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