rings and other dendrochronological work with diffuse-porous species
more difficult than is work with ring-porous species such as oak.
The biological regularity of the ring series in trees of temperate
zones makes it possible to date wood by comparing the sequences of
undated wood with those of wood of known age. To establish comprehen-
sive continuous growth-ring curves for periods longer than a tree’s lifetime,
it is necessary to use an overlapping system of individual curves (Fig. 2).
An overlapping system is necessary for the establishment of these master
chronologies, because trees in Europe do not normally live more than two
or three centuries. Such standard curves exist, among others, for south
and west Germany, several regions of north Germany, several areas in the
Netherlands (partial), and the Baltic area, from which the wood for most
Flemish and Dutch paintings was obtained (Fig. 3) (Eckstein et al. 1986).
To determine the ring widths in wood, a magnifying glass with an inte-
grated scale may be used (Fig. 4a). This method is used if measurements
have to be taken without laboratory equipment at the site. It is more con-
venient and faster to take measurements in the laboratory using a station-
ary binocular and a traveling stage on which the sample is mounted. These
devices can be connected to a computer to record the data for immediate
use in subsequent steps of the analysis (Fig. 4b).
Cross dating in its simplest form is the comparison of two tree
ring sequences to determine if and to what degree they match, as well as
to determine their placement in time to each other (Fig. 5). If one of the
curves is attributed to a definite stretch of time, the positioning ofthe
Measurement and
Cross Dating
D A P P 41
Figure 2
Overlapping system for the establishment of
master chronologies.