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 during the mid-late Holocene appears to have been located nearby some of the largest human settlements existing during this period. By documenting the conditions of the lake in time, using classical and modern approaches, the climate and geomorphology of the basin may be reconstructed. Synchrotron X-ray fluorescence measurements were performed on sections of a sedimentary core from the lake, representing an estimated 7500yr of history. Analysis yielded 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 geomorphology, climate and human activities.