Rapid late-glacial atmospheric CO2 chang
β
David J. Beerling; Hilary H. Birks; F. Ian Woodward
π
Article
π
1995
π
John Wiley and Sons
π
English
β 672 KB
The Younger Dryas stadia1 (1 1 000-10000 yr BP) was an abrupt return to a glacial climate during the termination of the last glaciation. We have reconstructed atmospheric CO, concentrations from a high-resolution sequence of fossil Salix herbacea leaves through this climatic oscillation from Kriiken