

Author: Heusser L. Heusser C. Kleczkowski A. Crowhurst S.
Publisher: Academic Press
ISSN: 0033-5894
Source: Quaternary Research, Vol.52, Iss.2, 1999-09, pp. : 154-158
Disclaimer: Any content in publications that violate the sovereignty, the constitution or regulations of the PRC is not accepted or approved by CNPIEC.
Abstract
High-resolution (∼≤100 yr sampling interval) Chilean pollen data between ∼10,000 and 60,000 cal yr B.P. exhibit systematic fluctuations in Subantarctic Parkland development. These variations are dominated by a 30,000–40,000-yr cycle similar to that in the Northern Hemisphere GISP2 δ18O data and other climatic records. Both Chilean and GISP2 data show oscillations in the 5000–12,000 and 1000–3000-yr period bands. The coherence is, however, generally low, and distribution of power spectra differs, with the dynamics of the pollen assemblage dominated by a combination of 12,000- and 5000-yr cycles. We suggest a preferential nonlinear response of Chilean vegetation to climatic forcing and interhemispheric differences as possible mechanisms underlying the resemblances and dissimilarities between both records.
Related content










By Roucoux K.H. Shackleton N.J. de Abreu L. Schönfeld J. Tzedakis P.C.
Quaternary Research, Vol. 56, Iss. 1, 2001-07 ,pp. :