The Amuq valley in southern Turkey is an important and interesting area in
the Near East forming a space-time bridge for archaeologists and scientists
to ancient and modern civilizations. The Lake of Antioch which evolved dur
ing the mid-late Holocene appears to have been located nearby some of the l
argest human settlements existing during this period. By documenting the co
nditions of the lake in time, using classical and modern approaches, the cl
imate and geomorphology of the basin may be reconstructed. Synchrotron X-ra
y fluorescence measurements were performed on sections of a sedimentary cor
e from the lake, representing an estimated 7500yr of history. Analysis yiel
ded the distribution of elemental masses spanning Ca to Mo as a function of
depth from the surface. We find that the elemental concentrations measured
follow a number of distinct patterns that may be related to local geomorph
ology, climate and human activities. (C) 2001 Elsevier Science B.V. All rig
hts reserved.