The northernmost conifers in the world are located well above the Arctic Ci
rcle in the Taymir region of northern Siberia and have been recording the t
hermal environment for centuries to millennia. The trees respond to tempera
tures beyond the narrow season of actual cambial cell division by means of
root growth, photosynthesis, lignification of cell walls, and other biochem
ical processes. Data from annual tree-ring widths are used to reconstruct M
ay-September mean temperatures for the past four centuries. These warm-seas
on temperatures correlate with annual temperatures and indicate unusual war
ming in the 20th century. However, there is a loss of thermal response in r
ing widths since about 1970, Previously the warmer temperatures induced wid
er rings. Most major warming and cooling trends are in agreement with other
high-latitude temperature reconstructions based on tree-ring analyses with
some regional differences in timing of cooling in the late 18th century an
d of warming in the late 19th century. (C) 2000 University of Washington.