What do Δ14C changes across the Gerzensee oscillation/GI-1b event imply for deglacial oscillations?

Journal of Quaternary Science

Volumn 15, Issue 3, 2000, Pages 203-214

  Andresen, C S A ^a   Bjorck S ^a   Bennike, O ^b   Heinemeier, J ^c   Kromer, B ^d  

^a UNIVERSITY OF COPENHAGEN   (Denmark)

^b GEUS ^*  (Denmark)

^c AARHUS UNIVERSITY   (Denmark)

^d HEIDELBERG ACADEMY OF SCIENCES AND HUMANITIES   (Germany)

Author keywords

14C changes; 14C dating; Allerod; Denmark; GI 1b; Lacustrine sediments; Pollen analysis; Solar forcing; Stable isotopes; Thermohaline circulation

Indexed keywords

ALLEROD; DEGLACIATION; LACUSTRINE DEPOSIT; PALYNOLOGY; RADIATIVE FORCING; RADIOCARBON DATING; STABLE ISOTOPE; THERMOHALINE CIRCULATION;

DENMARK;

EID: 0343673986     PISSN: 02678179     EISSN: None     Source Type: Journal    
DOI: 10.1002/(SICI)1099-1417(200003)15:3<203::AID-JQS514>3.0.CO;2-8     Document Type: Article

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