Because of their understanding of climate changes during the geological pas
t geoscientists can make important contributions to the evaluation of the c
urrent climate scenario. The climate factors that are actually decisive, su
ch as changes in solar energy, which have substantially characterized the t
emperatures prevailing on the earth and continue to determine them, cannot
be controlled by man. Impacts introduced by anthropogenic influences, such
as the input of climatically relevant gases into the atmosphere, represent
the only possibility of intervention even though the effects of countermeas
ures on the climate are bound to remain slight. In view of the relatively m
inor effects that anthropogenic carbon dioxide has had, and will presumably
continue to have, on the climate scenario it must be wondered whether the
considerable effort expended on countermeasures is always justifiable from
an economic point of view. In spite of this, the consumption of fossil fuel
s, and thus the emission of carbon dioxide, must be kept as low as possible
for reasons of environmental protection and the preservation of raze mater
ials. The BGR (Federal Institute for Geosciences and Raw Materials) suggest
s that these findings should be incorporated in the arguments put forward b
y policy makers when decisions on industrial development and global warming
prevention are made, so that the dialogue between economic and ecological
interests can yield sensible and environmentally compatible solutions at re
asonable cost. The inclusion of, and even closer cooperation between, neo-c
limatology, which focuses on the more recent past, and palaeo-climate resea
rch, which applies geoscience to reconstruct climatological data, is creati
ng an enhanced basis for future climate forecasts. Sudden and severe climat
e changes, the reasons for which have not been determined to date, are know
n to have occurred within one decade in prehistoric times. The justified qu
estion about forecasting short- and medium-term climate changes cannot yet
be answered by reliable model predictions. In the long run, however, astron
omic and geoscientific findings suggest a temperature drop over the next 10
000 years.