NOAA/WDS Paleoclimatology - Schaub - Gaenziloo/Landikon subfossil ~14500BP - PISY - ITRDB SWIT240

Fossil wood finds reveal a high resolution paleoclimatic proxy record of Lateglacial and Early Holocene. Eighty-one buried fossil pine stumps have been excavated on the construction site (Gaenziloo) of the A4-highway tunnel through Uetliberg near Zurich (Switzerland). The trees were buried during their lifetime by loamy alluvia washed down from the upper part of the slopes. The stumps have remained well preserved for more than 13,500 years. The cross sections of the trunks were analyzed dendrochronologically. The sections were dated by 14C, and 14C age vs. ring number were obtained from decadal sample segments.

Three floating chronologies were built. They cover a time span of 428 years in the Mid-Allerød (GAEALLCH_A), 561 years in the Late-Allerød (GAEALLCH_D) and 212 years in the Younger Dryas (GAEYD_A). Visual synchronization, t-values, percentages of parallel variation ('Gleichlaeufigkeit') and radiocarbon wiggle matching (14C age determinations on a decadal scale) as well as a check by the program Cofecha support the validity of the resulting chronologies.

The two Allerød-chronologies from Gaenziloo were linked with two chronologies from Daettnau (DAEALCH_1 and DAEALCH_2) published by Kaiser, K.F. (1993. Beiträge zur Klimageschichte vom Hochglazial bis ins frühe Holozän, rekonstruiert mit Jahrringen und Molluskenschalen aus verschiedenen Vereisungsgebieten. Ziegler Druck- und Verlags-AG, Winterthur. 206pp). They extend the existing floating Swiss chronology in the Late-Allerød by a total of 186 years. Unfortunately independent chronology GAEYD_A does not overlap with the actual absolute chronology developed by the tree-ring laboratory of the University of Hohenheim (Friedrich, M. et al., 2004. The 12,460 year Hohenheim oak and pine tree-ring chronology from Central Europe - A unique annual record for radiocarbon calibration and paleo-environment reconstructions. Radiocarbon 46(3), 1111-22.).