Abstract. The ongoing ecological conversion of mountain forests in central Europe from
widespread Picea monocultures to mixed stands conceptually also requires a
historical perspective on the very long-term, i.e. Holocene, vegetation and
land-use dynamics. Detailed sources of information for this are
palynological data. The Erzgebirge in focus here, with a maximum
height of 1244 m a.s.l., represents an extreme case of extensive historical
deforestation since the Middle Ages due to mining, metallurgy, and other
industrial activities, as well as rural and urban colonisation. For this
regional review we collected and evaluated 121 pollen diagrams of different
stratigraphic, taxonomic, and chronological resolution. This number makes
this region an upland area in central Europe with an exceptionally high
density of palynological data. Using well-dated diagrams going back to the
early Holocene, main regional vegetation phases were derived: the Betula–Pinus phase (ca.
11 600–10 200 cal yr BP), the Corylus phase (ca. 10 200–9000 cal yr BP), the Picea phase
(ca. 9000–6000 cal yr BP), the Fagus–Picea phase (ca. 6000–4500 cal yr BP), the
Abies–Fagus–Picea phase (ca. 4000–1000 cal yr BP), and the anthropogenic vegetation phase (ca.
1000–0 cal yr BP). Some diagrams show the presence or even continuous curves
of potential pasture and meadow indicators from around 2000 cal BCE at the
earliest. Even cereal pollen grains occur sporadically already before the
High Medieval. These palynological indications of a local prehistoric human
impact also in the higher altitudes find parallels in the
(geo-)archaeologically proven Bronze Age tin placer mining and in the
geochemically proven Iron Age metallurgy in the Erzgebirge. The pollen data
show that immediately before the medieval clearing, i.e. beginning at the
end of the 12th century CE, forests were mainly dominated by Fagus and Abies and
complemented by Picea with increasing share towards the highest altitudes.
According to historical data, the minimum of the regional forest cover was
reached during the 17th–18th centuries CE. The dominance of Picea in modern
pollen spectra is caused by anthropogenic afforestation in the form of
monocultures since that time. Future palynological investigations,
preferably within the framework of altitudinal transect studies, should aim
for chronologically and taxonomically high-resolution and radiometrically
well-dated pollen diagrams from the larger peatlands.