The oxygen and carbon isotopic signatures of biogenic carbonates in Gerzensee, Switzerland, during the rapid warming around 14,685 years BP and the following interstadial

Palaeogeography, Palaeoclimatology, Palaeoecology

Volumn 391, Issue , 2013, Pages 25-32

  Von Grafenstein, Ulrich ^a   Belmecheri, Soumaya ^a   Eicher, Ueli ^b   van Raden, Ulrike J ^c   Erlenkeuser, Helmut ^d   Andersen, Nils ^d   Ammann, Brigitta ^b  

^a CNRS   (France)

^b UNIVERSITY OF BERN   (Switzerland)

^c GEOLOGICAL INSTITUTE   (Switzerland)

^d UNIVERSITY OF KIEL   (Germany)

Author keywords

Late glacial; Ostracods; Stable isotopes; Temperature; Termination 1a

Indexed keywords

CARBON; CARBONATE; ESTIMATION METHOD; GLACIAL DEPOSIT; INTERSTADIAL; ISOTOPIC ANALYSIS; OXYGEN; QUANTITATIVE ANALYSIS; SEASONAL VARIATION; SEDIMENT-WATER INTERFACE; STABLE ISOTOPE; WATER LEVEL;

ARCTIC; GREENLAND; GREENLAND ICE SHEET; SWITZERLAND;

CHARALES; MOLLUSCA; OSTRACODA;

EID: 84890210879     PISSN: 00310182     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.palaeo.2013.08.018     Document Type: Article

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