Rapid phytolith extraction for analysis of phytolith concentrations and assemblages during an excavation: an application at Tell es-Safi/Gath,Israel

A rapid phytolith extraction procedure is described, that allows phytolith concentrations and morphotype assemblages to be analyzed within hours. This procedure enables the results of these analyses to be used during an archaeological excavation, in order to better understand how plants were used. The new procedure was tested using a standard phytolith extract and two experimental phytolith-sediment blends and found to be both accurate and precise. The reliability of partial slide counting was evaluated and found to be as accurate and precise as existing phytolith quantification methods. The new extraction and counting procedures were applied to an archaeological site, Tell es-Safi/Gath, Israel. The results demonstrate how information on phytolith concentrations in sediments that are available from one day to the next, can be used during an excavation to more effectively document the local features of interest and obtain better information.     

Iron Age hydraulic plaster from Tell es-Safi/Gath,Israel

Hydraulic plasters or mortars prior to the Roman period are rare. Here, we report the identification and characterization of 3000 year old (Iron Age) hydraulic plaster surfaces from the site of Tell es-Safi/Gath. This site, located in central Israel, was occupied almost continuously from prehistoric through modern times, and is identified as the Canaanite and Philistine city of Gath. A survey using an on-site Fourier transform infrared spectrometer (FTIR) identified the presence of amorphous silicates, in addition to calcite, in each of two superimposed plaster layers. This suite of minerals is characteristic of hydraulic plaster. An in-depth characterization of the plasters using FTIR, acid dissolution, X-ray fluorescence (XRF), X-ray powder diffractometry (pXRD), heating experiments and scanning electron microscopy (SEM) coupled with energy dispersive spectroscopy (SEM–EDS), shows that special silicate-containing minerals were brought from some distance to the site in order to produce these plaster surfaces. We therefore conclude that the plasters were deliberately produced, and were not the result of a fortuitous addition of local silicate minerals. A layer of around 150 μm thick enriched in carbonate hydroxylapatite was found in both plaster surfaces, and the same mineral was identified by infrared spectrometry in the surrounding sediments. This suggests that organic materials were used on these surfaces. These surfaces are among the oldest hydraulic plasters known.     

The Early Bronze Age Fortifications At Tell Es-Safi/Gath,Israel

Tell es-Safi/Gath is a multi-period site located on the border between the Judean foothills (Shephelah) and the southern coastal plain in central Israel, which has been subject to survey and excavations over the last two decades. Excavations by Bliss and Macalister in 1899 exposed a fortification system which was dated to the “Jewish period”. In this paper, we present updated data on these fortifications which have led to fresh insights. In two separate excavation areas, we excavated portions of the fortification system that surrounded the site which can now be dated to the EB III of the southern Levant. The EB fortification system influenced the location of later fortifications at the site. The nature of the construction techniques of these fortifications and the character of the settlement which they surrounded suggest that Tell es-Safi/Gath was a major regional urban centre during the EB III and was governed by a centralised administrative hierarchy.     

Geographical and Historical Realities behind the Earliest Layer in the David Story

ABSTRACT

The article attempts to identify an early Judahite layer in the David narrative in 1-2 Samuel and dates the reality behind it to the period prior to Judah expansion into the southern Hebron Highlands and the Beer-sheba Valley in the second half of the 9th century BCE. This helps to clarify the territorial and historical situation in the south in the 10th and early 9th centuries BCE. The article delineates the southern extent of the early north Israelite highlands polity, whose hub was in the area of Gibeon-Gibeah, and the territories of the Philistine kingdom of Gath and the desert polity that emerged at that time in the Beer-sheba Valley. It also deals with the role of Sheshonq I in shaping the long-term territorio-political order in southern Canaan.     

A Fresh Look at the Egyptian Environment of the Pharaonic Period

Abstract

The article deals with the territorial history of the southern steppe areas of the Levant in the period between ca. 1050–750 BCE. In the early days of the Iron Age, until the mid-9^th century BCE, parts of them, were ruled by local desert entities: in the late Iron I a Moabite polity and in the early Iron IIA and the early years of the late Iron IIA the Tel Masos-Beer-Sheba-Negev Highlands Highlands entity. This situation changed in the later years of the Iron IIA as a result of Damascus' rise to hegemony in the Levant. In the second half of the 9^th century BCE Judah, under Damascene domination, expanded for the first time into the Beer-Sheba Valley. In the first half of the eighth century BCE, with the revival of Assyrian power in the days of Adad-nirari III, Damascene authority was replaced by north Israelite domination in the south.