The study of environmental change during the Anthropogene is becoming
increasingly important, as societies develop a growing awareness of
future climatic changes and possible human impacts on the
environment. Obviously, no proper predictions of future geomorphologic
reaction to environmental changes can be made without a clear
understanding of past environmental changes, and particularly during
the Holocene. In this context, coordinated and integrated efforts may
lead to a more complete understanding of past and future environmental
change. Integrated studies of human influence on environmental change
and geomorphology have led to the formation of geoarchaeological
projects with interdisciplinary research, in which geomorphology plays
an important part. The 26th Annual Geomorphology Conference in Trier,
Germany, on Geomorpology and the History of the Environment,
convened by ROLAND BAUMHAUER and BRTGITTA SCHUTT, focused on past
human influence on the environment.
In 13 contributions, all but one written in English, 31 scientists
from Germany (30) and Austria (1) present their recent results. -
High-resolution dating in combination with geochemical investigations
leads to a record of sedimentary yield for the last 14,000 years for a
crater lake and its catchment in western Germany; on the basis of
paleolimnological data B.ZOLITSCHKA discusses natural versus human
forcing. Since the lst millennium BC, periods of human-induced
environmental change are documented. - A data bank of archaeological
sites for a mountainous region in western Germany is used by H. LOHR,
B. SCHUTT and R. BAUMHAUER to reconstruct location factors (elevation
a. s. 1., soils, geology) of prehistoric sites. - R. MARKET,
R. SCHNEIDER, A. FRTEDMANN and J. SEIDEE present a detailed study on
environmental change and human impact on relief development in the
Upper Rhine valley and Black Forest durin`, the Atlantic, related to
the first Neolithic settlements, and from the late Bronze Age to the
end of the Roman Empire. The human influence on geomorphologic
processes was most pronounced during the Latene and Roman
periods. -The geomorphological setting of the important late Iron Age
oppidum (settlement) of Manching at the Danube River is described by
J. VÖLKEL, M. LEOPOLD and B. WEBER, as well as the late Iron Age
soil erosion in the vicinity of a Celtic square enclosure near the
Danube valley in southeast Bavaria. For the first time, a detailed
quantitative and precision-dated reconstruction of soil erosion and
collovial sedimentation is presented for a prehistoric landscape. -
Geomorphologic-sedimentological investigations next to a 7250 cal yr
BP settlement in southwestern Germany, carried out by A. SCHULTE and
T. HECKMANN, show that human farming activities had a substantial
influence on environmental change only during the Bronze Age, but not
earlier. - The colluvial sequences on till plains in Vorpommern
(north-east Germany) are investigated and discussed by H. HELBIG,
P. de KLERK, P. KÜHN and J. KWASNIOWSKI. The authors emphasize that
it is still difficult to correlate certain phases of accelerated soil
erosion with periods of Slavonic and German colonisation, especially
where the homogeneity of the colluvial soils on present-day
agricultural fields do not allow a high resolution in time. - A
reconstruction of the lateglacial and early: Holocene landscape
evolution of the Upper Rhine River floodplain with the tributary
Neckar River between Frankfurt/Main and Heidelberg reveals the
influence of climatic changes and oscillations on floodplain
sedimentation, peat growth, dune formation etc. (R. DAMBECK and
J. A. A. Bos). Rhine and Neckar show a different geomorphologic
pattern during the Allerod and Younger Dryas. - A number of models are
used by L. SCHROTT and T. ADAMS to quantify postglacial sediment
volumes and denudation in an alpine basin of the Italian
Dolomites. Debris flows are most important among the geomorphic
processes of denudation and sedimentation. - In the east Austrian
alpine foreland, H. EICHER shows how special farming methods (since
Roman times) and the political border between the Holy Roman Empire of
German Nation and the Kingdom of Hungary (AD 1043-AD 1918) are
reflected by alluvial clay sedimentation in the cut-and-fill terrace
landforms. - During the Holocene, four sediment and three soil
formation cycles are distinguished by D. FAUST and C. ZIELHOFER in the
Qued Medjerba valley in northern Tunesia. The sediment-soil-sequence
of the floodplain records water level amplitude changes, which are
correlated with environmental and cultural changes. During the last
ca. 440 years BP extreme flood events occurred. - In a case study of
the Gongola Basin in northeast Nigeria, K.-M. MOLDENHAUER shows that
river incision is caused by severe ecological degradation processes,
which are not the result of climate change but of over-utilization of
fragile ecosystems. - Case studies from southwest Germany of
IR-OSL-dated colluvial archives as evidence for the Holocene landscape
history are presented by A. KADEREIT, A. LANG, S. HÖNSCHEIDT, J. MÜTH
and G. WAGNER. Their results corroborate the results of other studies:
Although small scale Neolithic colluvium formation is detected, the
relief-forming deposition of thick footslope covering colluvia only
started in the Bronze Age; pre-modern colluvial sedimentation was
significantly accelerated in the Iron/Roman period and reached its
most pronounced phases during the Middle Ages. Older sediments from
interim storages on the slope are reworked successively. - By
analysing more than 1,000 drill cores, T. SCHNEIDER reconstructs the
postglacial development of alluvial cones and bogs along the northern
border of the German Alps. A number of phases of enhanced fluvial
accumulation and peat growth IS documented. The development of the
cones occurred mainly during the lategla- clal period. However, human
influence through intense forest grazing and forest degradation since
medieval times is recorded in sedimentation and erosion processes.
The main focus of the contributions has been the impact of human
activities on the natural environment. Environmental change and
geomorphology is a scientifically sound and well-written book giving a
comprehensive overview of recent German research. Most of the research
work reported here was funded by the German Research Foundation
(DFG). Especially interesting is the main theme, i. e. the
observation that anthropogenic factors are the main causes for
geomorphological processes and environmental changes since the Bronze
Age, a fact often overlooked in geomorphology textbooks. The volume
offers an excellent approach by considering an impressive variety of
methods, which include geomorphological, geomorphometrical and
geophysical methods (seismic refraction, geoelectrical sounding,
ground penetrating radar), GIS techniques, pedological analyses,
modelling, drilling, dating by 14CC, IRSL, OSL, TL, archaeological
methods and dating by artifacts, pollen analyses, examination of
historic maps and written archives, etc. This volume should have a
wide readership not only within the geoarchaeology community but also
within the geomorphology community. After all, during the past
millennium humans influenced the environment more decisively and irre-
versibly in a global scale than during the preceding more than 2.5
million years since the species Homo existed (quoted from the
preface).
KLAUS HEINE, Regensburg