Geological evidence of a palynologically defined cooling in southeastern Canada at 10 000-8000 14C yr BP

• Published in: Géographie physique et Quaternaire
• Main Authors: Brookes, Ian A., Grant, Douglas R.
• Format: Text
• Language: English
• Published: Les Presses de l'Université de Montréal 2007
• Subjects: Canada; Glacial Lake; Goldthwait; Sea ice
• Online Access: http://id.erudit.org/iderudit/038994ar; https://doi.org/10.7202/038994ar

Post-glacial pollen spectra over a wide area of southeastern Canada have been interpreted as showing that the general warmth-adapted trend of regional vegetation change was interrupted between 10 000 and 8000 14C yr BP, reverting to conditions associated with a markedly cooler climate. This biotic r...