FN Archimer Export Format
PT J
TI The δ18O stratigraphy of the Hoxnian lacustrine sequence at Marks Tey, Essex, UK: implications for the climatic structure of MIS 11 in Britain
BT 
AF TYE, G. J.
   SHERRIFF, J.
   CANDY, I.
   COXON, P.
   PALMER, A.
   MCCLYMONT, E. L.
   SCHREVE, D. C.
AS 1:1;2:1;3:1;4:2;5:1;6:3;7:1;
FF 1:;2:;3:;4:;5:;6:;7:;
C1 Royal Holloway Univ London, Dept Geog, Egham TW20 0EX, Surrey, England.
   Trinity Coll Dublin, Dept Geog, Museum Bldg, Dublin, Ireland.
   Univ Durham, Dept Geog, S Rd, Durham DH1 3LE, England.
C2 UNIV LONDON, ENGLAND
   UNIV DUBLIN, IRELAND
   UNIV DURHAM, ENGLAND
IF 2.469
TC 23
UR https://archimer.ifremer.fr/doc/00421/53267/54669.pdf
   https://archimer.ifremer.fr/doc/00421/53267/54670.pdf
   https://archimer.ifremer.fr/doc/00421/53267/54671.xlsx
LA English
DT Article
CR MD 123 / GEOSCIENCES 1
   MD 134 / PICABIA
BO Marion Dufresne
DE ;abrupt event;Hoxnian;Interglacial;Marine Isotope Stage 11;delta O-18 and delta C-13
AB Marine Isotope Stage 11 (MIS 11) is considered one of the best analogues for the Holocene. In the UK the long lacustrine sequence at Marks Tey, Essex, spans the entirety of the Hoxnian interglacial, the British correlative of MIS 11c. We present multiproxy evidence from a new 18.5-m core from this sequence. Lithostratigraphy, pollen stratigraphy and biomarker evidence indicate that these sediments span the pre-, early and late temperate intervals of this interglacial as well as cold climate sediments that post-date the Hoxnian. The O-18 signal of endogenic carbonate from this sequence produces several clear patterns that are interpreted as reflecting the climatic structure of the interglacial. As well as providing evidence for long-term climate stability during the interglacial and a major post-Hoxnian stadial/interstadial oscillation the O-18 signal provides strong evidence for abrupt cooling events during the interglacial itself. One of these isotopic events occurs in association with a short-lived increase in non-arboreal pollen (the NAP phase). The results presented here are discussed in the context of other MIS 11 records from Europe and the North Atlantic, particularly with respect to our understanding of the occurrence of abrupt climatic events in pre-Holocene interglacials. Copyright 
PY 2016
PD FEB
SO Journal Of Quaternary Science
SN 0267-8179
PU Wiley
VL 31
IS 2
UT 000374767200002
BP 75
EP 92
DI 10.1002/jqs.2840
ID 53267
ER

EF