Search

Objective To determine the species of intestinal parasites present in 7th century BC high-status residents of Jerusalem and to expose the history of regional health and sanitary conditions. Materials Fifteen sediment samples were collected from the cesspit below a stone toilet seat found at the site of Armon Hanatziv, southern Jerusalem. The toilet installation was located in a garden adjacent to a monumental structure with extraordinary architectural elements. Methods A light microscope was used to identify and measure the eggs. Results The presence of four intestinal parasite egg taxa was detected: Trichuris trichiura (whipworm), Taenia sp. (beef/pork tapeworm), Ascaris lumbricoides (roundworm), and Enterobius vermicularis (pinworm). This is the earliest appearance of roundworm and pinworm in the ancient Israel parasitological record. Conclusions Findings reveal that intestinal parasitic diseases most likely caused by poor sanitary conditions were a human problem in the Late Iron Age of Israel, affecting even high-status groups. Significance The study demonstrates the potential of archaeoparasitological investigations to expand our knowledge of the origin and history of regional infections. Moreover, parasitological evidence enabled us to determine the purpose of the cubical perforated stone artifacts (stone toilet seats rather than cultic objects as currently debated). Limitations The eggs of some parasite taxa are less durable, so may theoretically be absent due to selective preservation. Suggestions for Further Research Future excavations of ancient Israel should include archaeoparasitological studies of rare toilet installations to prevent information loss of regional history of diseases and to better understand their archaeological context.

Global agro-biodiversity has resulted from processes of plant migration and agricultural adoption. Although critically affecting current diversity, crop diffusion from antiquity to the middle-ages is poorly researched, overshadowed by studies on that of prehistoric periods. A new archaeobotanical dataset from three Negev Highland desert sites demonstrates the first millennium CE’s significance for long-term agricultural change in southwest Asia. This enables evaluation of the “Islamic Green Revolution” (IGR) thesis compared to “Roman Agricultural Diffusion” (RAD), and both versus crop diffusion since the Neolithic. Among the finds, some of the earliestSolanum melongenaseeds in the Levant represent the proposed IGR. Several other identified economic plants, including two unprecedented in Levantine archaeobotany (Ziziphus jujuba, Lupinus albus), implicate RAD as the greater force for crop migrations. Altogether the evidence supports a gradualist model for Holocene-wide crop diffusion, within which the first millennium CE contributed more to global agro-diversity than any earlier period.

This study presents a comprehensive paleoenvironmental reconstruction of the Byzantine and Early Islamic western Negev Desert communities during the 4th-8th centuries CE. The study is based on 33 pollen samples and hundreds of charcoal remains that were recovered from the villages of Shivta and Nitzana. The results demonstrate that during the 5–6th centuries CE flourishing desert agricultural communities existed on the periphery of the Byzantine Empire (Eastern Roman Empire). The presence of diverse fruit-tree horticulture is revealed by both pollen and charcoal remains (grape, fig, olive, carob, almond/apricot, pomegranate, date palm and the exotic hazelnut). The rich botanical assemblages also provide evidence of the cultivation by irrigation of conifers and other Mediterranean trees common to the more humid Mediterranean vegetation zone, including the prestigious cedar of Lebanon. The palynological reconstruction of an ornamental garden at Shivta indicates the ability to invest water and labor, not only for horticultural and construction purposes, but also for ornamental greenery. We therefore suggest that the Byzantine Negev Desert community was a luxury society in contrast to societies living in a mode of survival in challenging desert environments. During the Early Islamic period (since the second half of the 7th century CE), our data show a dramatic decline in fruit-tree horticulture coupled with indicators signifying overexploitation for fuel of the nearby natural woody desert environment. Hence, we claim that in addition to previous possible explanations for the demise of the Negev Byzantine communities (plague pandemic, climate change, the Muslim conquest), overexploitation of the natural vegetation should also be taken into account. This study therefore helps address historical questions that are also pertinent to the modern era, regarding the existence of flourishing societies in challenging environments, overexploitation of the natural environment, and neglect of sustainability.

The geography of Judah is unique among the territorial kingdoms of the southern Levant, featuring four distinct regions with the potential for exploitation in different economic strategies. In the ...

The present study has two main goals. The first is to reconstruct the botanical components that grew in the impressive garden of Villa Arianna (Stabiae). The garden, which was extensively destroyed and covered by tephra ash in 79 CE, is considered the largest peristyle garden in the Vesuvian region. Its plants were revealed based on a unique palynological-archaeological method involving the extraction of pollen from plaster attached to structures that faced the garden. The second aim is to compare this prestigious garden with other early elite Roman gardens, located in the eastern part of the Empire, to trace the importation of plants, horticultural trends, etc. For this purpose, gardens of Herod the Great, the client king of Judaea, which the author recently studied palynologically (in Caesarea, Herodium and Jericho), were compared with the new pollen results of Villa Arianna. The comparison between the gardens’ botanical components and their different landscapes led to the following conclusions: (1) Plants were imported from both ends of the Empire as elite products (rather than cash crops). Hazelnut (Corylus) and cedar (Cedrus) were introduced from west to east, while the date palm (Phoenix dactylifera) was introduced along an east-west axis. (2) The gardening trend of tree dwarfism was observed both at Villa Arianna and Jericho. (3) The gardens flourished in challenging habitats. At Villa Arianna and Caesarea, efforts were devoted to sustaining splendid gardens in the relatively harsh, saline Mediterranean Sea environment; at Herodium and Jericho, special efforts were required for the success of Mediterranean plants in semi-arid climate. (4) Herod’s mausoleum garden in Herodium, whose dark evergreen trees on the whitish slopes of the artificial tumulus could be seen from the Temple in Jerusalem, may have been inspired by the architectural arrangement of the Pantheon and the Mausoleum of Augustus, the patron of Herod.

In this study we present the identification of several Early Roman (63 b.c.e.–70 c.e.) charred wood assemblages, collected from the “Lower City” of Jerusalem. The results outline elements in Jerusa...

A substantial amount of macro-botanical remains has been recorded at Tel Megiddo since the initiation of the renewed excavations in 1992. We constructed a database with 1,162 identified samples and...

We present here the earliest evidence for large-scale table olive production from the mid-7th millennium BP inundated site of Hishuley Carmel on the northern Mediterranean coast of Israel. Olive pit size and fragmentation patterns, pollen as well as the architecture of installations associated with pits from this site, were compared to finds from the nearby and slightly earlier submerged Kfar Samir site. Results indicate that at Kfar Samir olive oil was extracted, while at Hishuley Carmel the data showed that large quantities of table olives, the oldest reported to date, were prepared. This process was most probably facilitated by the site’s proximity to the Mediterranean Sea, which served as a source of both sea water and salt required for debittering/pickling/salting the fruit, as experimentally demonstrated in this study. Comparison of pit morphometry from modern cultivars, wild-growing trees and the archaeological sites, intimates that in pit morphology the ancient pits resemble wild olives, but we cannot totally exclude the possibility that they derive from early cultivated trees. Our findings demonstrate that in this region, olive oil production may have predated table olive preparation, with each development serving as a milestone in the early exploitation of the olive.

Significance Commercial production of luxury “Gaza wine” was long assumed to be the economic basis of Late Antique settlement in the Negev Desert. We present empirical evidence for local viticulture of scale and its connection to Mediterranean trade. Offering unprecedented testimony to the globalization of an ancient production economy in a marginal environment, our archaeobotanical and ceramic dataset illuminates the rise and fall of local viticulture in the fourth to sixth centuries of the common era (CE). Decline likely resulted from market contraction triggered by plague and climate change rather than Islamic conquest, exposing systemic vulnerabilities of Negev agricultural commercialization. In millennial-scale Negev history, the Late Antique commercial florescence is anomalous, lasting about two centuries before reverting to smaller settlement and survival–subsistence strategies., The international scope of the Mediterranean wine trade in Late Antiquity raises important questions concerning sustainability in an ancient international economy and offers a valuable historical precedent to modern globalization. Such questions involve the role of intercontinental commerce in maintaining sustainable production within important supply regions and the vulnerability of peripheral regions believed to have been especially sensitive to environmental and political disturbances. We provide archaeobotanical evidence from trash mounds at three sites in the central Negev Desert, Israel, unraveling the rise and fall of viticulture over the second to eighth centuries of the common era (CE). Using quantitative ceramic data obtained in the same archaeological contexts, we further investigate connections between Negev viticulture and circum-Mediterranean trade. Our findings demonstrate interrelated growth in viticulture and involvement in Mediterranean trade reaching what appears to be a commercial scale in the fourth to mid-sixth centuries. Following a mid-sixth century peak, decline of this system is evident in the mid- to late sixth century, nearly a century before the Islamic conquest. These findings closely correspond with other archaeological evidence for social, economic, and urban growth in the fourth century and decline centered on the mid-sixth century. Contracting markets were a likely proximate cause for the decline; possible triggers include climate change, plague, and wider sociopolitical developments. In long-term historical perspective, the unprecedented commercial florescence of the Late Antique Negev appears to have been unsustainable, reverting to an age-old pattern of smaller-scale settlement and survival–subsistence strategies within a time frame of about two centuries.

The 13 articles in this special issue of the journal Quaternary Science Reviews explore links and processes behind societal-cultural changes, environmental changes and climate changes during the Ho...

This study aims to trace changes in the River Nile flows over the Late Quaternary and is based on palynomorphs which were embedded in the sea floor of the Levantine Basin. The palynomorphs were extracted from two marine sediment cores, which cover the last 86 ka and are located at the two ends of the Levantine Basin: MD-9509, at the southern part of the Levantine Basin, and MD-9501, at its northern part. Core MD-9509 was taken from the Nile cone and is characterized by high sedimentation rates and a good state of palynomorph preservation. The assemblages included palynomorphs which were transported via the Nile headwaters and therefore enabled the reconstruction of the River Nile flows. The results demonstrate that the last glacial period (∼75–16 ka) was characterized by a decrease in Nile water discharge and an increase in sediment influx, while opposite trends were observed prior to the last glacial period as well as during the deglaciation and the Holocene. Based on the study of the spores, it is suggested that during the last glacial, the main contributors of freshwater and sediment load to the Eastern Mediterranean Sea were the Blue Nile and the Atbara and only during interglacials was there a more significant contribution of the White Nile. Within the northern core, MD-9501, pollen was preserved only during the formation of sapropels S3 and S1. The comparison of the sapropelic palynological spectra in both core sites clearly indicates that during sapropel deposition, climate conditions were more humid in the Northern Levant, reflecting the north-south regional Mediterranean climatic moisture gradient. Sapropel formation was a result of the intensification of the monsoonal climate system which was most probably related to the maximum insolation values at 65°N, while, currently, the Atlantic is the main influencing climate system in the region. One of the most interesting observations in this study is that during Heinrich Events H2-H6, which originated in the north Atlantic and were identified in MD-9509 based on minimum arboreal pollen percentages, pollen originating from tropical regions was not embedded in the Levantine Basin. These results lend support to the view that episodes of dryness in tropical/sub-tropical Eastern Africa were associated not only with low-latitude climate controls, but also with high-latitude glacial stress.

The Euphrates poplar (Populus euphratica), can be found in the arid regions of the Negev highlands, the Judean desert, and the northern Arava in a number of clustered populations located near permanent water sources. The trees' distribution in the desert regions is not continuous, being disconnected from its major area of distribution along the Jordan River, where its distribution is uninterrupted. It is unclear how and when this disjunctive distribution occurred, and what were the initial ecological conditions for this poplar's original establishment and success. In this article we present a study of the current distribution of these trees within an arid environment, and of their various traditional uses. A strong relationship is demonstrated between the present location of the trees and settlements from the Roman and Byzantine periods (between the 1st century BCE to 7th century CE). Euphrates poplars are abundant today near early Christian monasteries, which could have been the main factor responsible for their present-day distribution.

This study presents, for the first time, an environmental reconstruction of a sequence spanning nearly the entire Mediterranean Epipaleolithic (∼22.0–11.9 ka cal. BP). The study is based on a well-dated, high-resolution pollen record recovered from the waterlogged archaeological site Jordan River Dureijat (JRD), located on the banks of Paleolake Hula. JRD's continuous sequence enabled us to build a pollen-based paleoclimate model providing a solid background for the dramatic cultural changes that occurred in the region during this period. Taxonomic identification of the waterlogged wood assemblage collected from JRD was used to fine-tune the paleoenvironmental reconstruction. The chronological framework is based on radiocarbon dating and the typology of archaeological findings. The LGM (∼22–19 ka cal. BP) was found to be the coldest period of the sequence, marked by a distinct decrease in the reconstructed January temperatures of up to 5°C lower than today, while mean annual precipitation was only slightly lower than the present-day average (∼450 vs. 515 mm, respectively). The wettest and warmest period of the record was identified between ∼14.9 and 13.0 ka cal. BP, with maximum values of 545 mm mean annual precipitation reached at ∼14.5 ka cal. BP. This time interval is synchronized with the global warm and moist Bolling-Allerod interstadial as well as with the onset of the Natufian culture and the emergence of sedentism in the Levant. The Younger Dryas began around 12.9 ka cal. BP and was identified as an exceptional period by the JRD sequence with low temperatures and minimal climatic seasonality contrast: an increase in rain contribution during spring, summer, and autumn was documented concurrently with a significant decrease in winter precipitation. The detailed vegetation and climatological reconstruction presented in this study serves as backdrop to seminal events in human history: the transition from small nomadic groups of hunter-gatherers to the sedentary villages of the Natufian, eventually transitioning to the agricultural, complex communities of the Neolithic.

• Tel Yarmuth is one of the largest Early Bronze Age urban centers in the Land of Israel.

Various artillery and rigging artefacts were retrieved from the Megadim wreck-site, Israel. The present research is aimed at determining the composition, microstructure and manufacturing processes of the objects, as well as their dating. Therefore, a multidisciplinary testing approach was applied, based on typology, metallurgical criteria, archaeobotanical analysis and 14C radiocarbon dating. Based on their typology, the three cannons found off Megadim were of Venetian origin. Metallurgical analysis of the three cannons revealed they were made of cast bronze, with tin (Sn) composition of 3.2–6.5 wt%; and were most likely manufactured at the same European foundry. The chain links of the iron-bound deadeye were made of wrought-iron, manufactured by the bloomery process; and the forge-welding zone of the largest chain was located. Epi-illuminated and SEM analyses suggest that the deadeyes were made of Rhus coriaria, and the wads were made of Cupressus sempervirens and Pinus pinea. The largest breech chamber was made of cast leaded-bronze, probably manufactured of recycled alloys due to the low amount of tin. The other two chambers were made of wrought-iron, and based on their similar composition, were probably manufactured at the same workshop. Examination of the material extracted from the chambers suggests it was black powder. The bronze cannons were typologically dated to between the late 16th and the early 17th centuries. Based on the metallurgical criteria and the 14C analysis, it is suggested that all the objects were most likely manufactured before the middle of the 17th century. This research enhances our knowledge of the Megadim wreck-site, and provides better understanding of the manufacturing technologies of marine artillery and rigging elements in Europe between the late 16th and early 17th centuries.

Today, citrus orchards are a major component of the Mediterranean landscape and one of the most important cultivated fruits in the region; however, citrus is not native to the Mediterranean Basin, but originated in Southeast Asia. Here, the route of the spread and diversification of citrus is traced through the use of reliable historical information (ancient texts, art, and artifacts such as wall paintings and coins) and archaeobotanical remains such as fossil pollen grains, charcoals, seeds, and other fruit remains. These botanical remains are evaluated for their reliability (in terms of identification, archaeological context, and dating) and possible interpretations. Citrus medica (citron) was the first citrus to spread west, apparently through Persia and the Southern Levant (remains were found in a Persian royal garden near Jerusalem dated to the fifth and fourth centuries BC) and then to the western Mediterranean (early Roman period, ≈third and second centuries BC). In the latter region, seeds and pollen remains of citron were found in gardens owned by the affluent in the Vesuvius area and Rome. The earliest lemon (C. limon) botanical remains were found in the Forum Romanum (Rome) and are dated to the late first century BC/early first century AD. It seems, therefore, that lemon was the second citrus species introduced to the Mediterranean. The contexts of the botanical remains, in relation to elite gardens, show that in antiquity, both citrus and lemon were products representing high social status. Sour orange (C. aurantium), lime (C. aurantifolia), and pummelo (C. maxima) did not reach the Mediterranean until the 10th century AD, after the Islamic conquest. Sweet orange (C. sinesis) was introduced during the second half of the 15th century AD, probably via the trade route established by the Genoese, and later (16th century AD) by the Portuguese. The mandarin (C. reticulata) reached the Mediterranean only in the early 19th century. While citron and lemon arrived in the Mediterranean as elite products, all other citrus fruit most probably spread for economic reasons.

We are grateful to Ben-Yosefet al. (above) for their thorough critical evaluation of our recent paper. We identified a group of modified wooden shafts originating in two large complex caves with Late Chalcolithic (Ghassulian) burials in the Negev Desert (Israel) as the earliest Levantine wooden spinning implements (Langgutet al. 2016). Their detailed assessment culminated in the alternative hypothesis that the wooden objects functioned as sticks that carried metal maceheads during rituals. This raises several issues that merit serious consideration. Our response to Ben-Yosefet al.'s suggestions is divided into two sections, each concentrating on one of the two main technologies under discussion: spinning and metallurgy.

Using a biographic-like approach, this article presents the initial results of the study of an elite Iron Age house at Tel ‘Eton, from its conception, through its birth and life, to its death and d...

In this article we discuss four datasets that provide evidence for the expansion of grain growing in Canaan in the second half of the 13th century and the 12th century BCE: the faunal and flint records from Megiddo, the pollen diagram for the Sea of Galilee and the ancient DNA study of Bronze and Iron Age cattle in the Levant. Efforts to expand dry farming in Canaan were probably related to the dry climate event in the later phases of the Late Bronze Age, which has recently been detected in several pollen records from the Eastern Mediterranean. We discuss textual evidence related to drought and famine that struck the Near East at that time. We then suggest that the Egyptian administration in Canaan initiated the extension of dry farming in order to stabilise the situation in the southern and eastern fringe areas of the Levant and supply grain to areas in the northern Near East which, according to textual data, were badly afflicted by the climate crisis.

Significance Historians have long debated the role of climate in the rise and fall of empires of the 1st millennium CE. Drastic territorial contraction of the Byzantine Empire, societal decline, and beginning of the European Middle Ages have generally been linked to the Islamic conquests of the seventh century. This multidisciplinary archaeological investigation of trash mounds in the Negev Desert establishes the end date of organized trash management in the Byzantine-period city of Elusa and demonstrates urban collapse a century before the Islamic transition. Our findings, taken together with other evidence for Byzantine urban dysfunction, the Justinianic Plague, and recent research on the Late Antique Little Ice Age, flesh out the impact of the sixth century on broad historical trajectories., The historic event of the Late Antique Little Ice Age (LALIA) was recently identified in dozens of natural and geological climate proxies of the northern hemisphere. Although this climatic downturn was proposed as a major cause for pandemic and extensive societal upheavals in the sixth–seventh centuries CE, archaeological evidence for the magnitude of societal response to this event is sparse. This study uses ancient trash mounds as a type of proxy for identifying societal crisis in the urban domain, and employs multidisciplinary investigations to establish the terminal date of organized trash collection and high-level municipal functioning on a city-wide scale. Survey, excavation, sediment analysis, and geographic information system assessment of mound volume were conducted on a series of mounds surrounding the Byzantine urban settlement of Elusa in the Negev Desert. These reveal the massive collection and dumping of domestic and construction waste over time on the city edges. Carbon dating of charred seeds and charcoal fragments combined with ceramic analysis establish the end date of orchestrated trash removal near the mid-sixth century, coinciding closely with the beginning of the LALIA event and outbreak of the Justinian Plague in the year 541. This evidence for societal decline during the sixth century ties with other arguments for urban dysfunction across the Byzantine Levant at this time. We demonstrate the utility of trash mounds as sensitive proxies of social response and unravel the time–space dynamics of urban collapse, suggesting diminished resilience to rapid climate change in the frontier Negev region of the empire.

Olive (Olea europaea L.) was one of the most important fruit trees in the ancient Mediterranean region and a founder species of horticulture in the Mediterranean Basin. Different views have been expressed regarding the geographical origins and timing of olive cultivation. Since genetic studies and macro-botanical remains point in different directions, we turn to another proxy - the palynological evidence. This study uses pollen records to shed new light on the history of olive cultivation and large-scale olive management. We employ a fossil pollen dataset composed of high-resolution pollen records obtained across the Mediterranean Basin covering most of the Holocene. Human activity is indicated when Olea pollen percentages rise fairly suddenly, are not accompanied by an increase of other Mediterranean sclerophyllous trees, and when the rise occurs in combination with consistent archaeological and archaeobotanical evidence. Based on these criteria, our results show that the southern Levant served as the locus of primary olive cultivation as early as similar to 6500 years BP (yBP), and that a later, early/mid 6th millennium BP cultivation process occurred in the Aegean (Crete) - whether as an independent large-scale management event or as a result of knowledge and/or seedling transfer from the southern Levant. Thus, the early management of olive trees corresponds to the establishment of the Mediterranean village economy and the completion of the 'secondary products revolution', rather than urbanization or state formation. From these two areas of origin, the southern Levant and the Aegean olive cultivation spread across the Mediterranean, with the beginning of olive horticulture in the northern Levant dated to similar to 4800 yBP. In Anatolia, large-scale olive horticulture was palynologically recorded by similar to 3200 yBP, in mainland Italy at similar to 3400 yBP, and in the Iberian Peninsula at mid/late 3rd millennium BP.

International audience; This paper explores long-term trends in human population and vegetation change in the Levant from the early to the late Holocene in order to assess when and how human impact has shaped the region’s landscapes over the millennia. To do so, we employed multiple proxies and compared archaeological, pollen and palaeoclimate data within a multi-scalar approach in order to assess how Holocene landscape dynamics change at different geographical scales. We based our analysis on 14 fossil pollen sequences and applied a hierarchical agglomerative clustering and community classification in order to define groups of vegetation types (e.g. grassland, wetland, woodland, etc.). Human impact on the landscape has been assessed by the analysis of pollen indicator groups. Archaeological settlement data and Summed Probability Distribution (SPD) of radiocarbon dates have been used to reconstruct long-term demographic trends. In this study, for the first time, the evolution of the human population is estimated statistically and compared with environmental proxies for assessing the interplay of biotic and abiotic factors in shaping the Holocene landscapes in the Levant.

The genus Tamarix (tamarisk, salt cedar; family Tamaricaceae) includes some 60 taxa worldwide. The genus is native to the drier areas of Eurasia and Africa, Western Europe, and the south and east United States (Schmidt, Relationship of salinity and depth to the water table on Tamarix spp. (salt cedar) growth and water use. Thesis submitted toward the M.Sc. Texas A&M University, p 90, 2003). The genus is composed of evergreen or deciduous shrubs or trees, usually on saline soils and tolerant to salts and alkaline conditions. The pink or white flowers grow in dense masses on 5–10-cm-long spikes or panicles flowering during spring, summer, and autumn. Tamarix can spread both vegetatively and by seed that are plumose at tips and can be dispersed by wind and water (Waisel, Biology of halophytes. Academic Press, London, 1972)… More than 15 species of Tamarix are found in Israel (Baum, The genus Tamarix. The Israel Academy of Sciences and Humanities, Jerusalem, 1978). The taxonomy of this genus has long been subjected to general and regional revisions. There has always been vast disagreement between botanists as to the delimitation and the grouping of the species (Zohary, Flora Palaestina part II. The Israel Academy for Science and Humanities, Jerusalem, 1972). The aim of the present study was to revise the taxonomy of the genus Tamarix, based primarily on pollen characters.

This article presents a systematic methodological comparison of three archaeobotanical proxies (phytoliths, pollen and seeds) applied to an assemblage of dung pellets and corresponding archaeological refuse deposits from Early Islamic contexts at the site of Shivta. We set out with three main methodological questions: one, to evaluate the relative input of botanical remains from dung in refuse assemblages; two, to evaluate each archaeobotanical dataset and to test whether they are comparable, complementary or contradictory in their interpretations from dung; and three, infer herding practices at the site during the Early Islamic period. Our findings show that ovicaprine dung accumulated in Early Islamic Shivta during at least two periods: mid-7th–mid-8th centuries CE, and late-8th–mid-10th centuries CE. Methodologically, we see incomplete and incompatible reconstructions arise when each method is considered alone, with each proxy possessing its own advantages and limitations. Specifically, the amount of preserved seeds in dung pellets is low, which restricts statistical analysis and tends to emphasize small or hard-coated seeds and vegetation fruiting season; yet this method has the highest taxonomic power; pollen preserves only in uncharred pellets, emphasizes the flowering season and has an intermediate taxonomic value; phytoliths have the lowest taxonomic value yet complete the picture of livestock feeding habits by identifying leaf and stem remains, some from domestic cereals, which went unnoticed in both seed and pollen analyses. The combined archaeobotanical reconstruction from samples of the mid-7th–mid-8th centuries suggests that spring-time herding at Shivta was based on free-grazing of wild vegetation, supplemented by chaff and/or hay from domestic cereals. For the late-8th–mid-10th century samples, phytolith and pollen reconstruction indicates autumn-winter free-grazing with no evidence of foddering. Unlike the dung pellets, macrobotanical remains in the refuse deposits included domestic as well as wild taxa, the former mainly food plants that serve for human consumption. Plant remains in these refuse deposits originate primarily from domestic trash and are only partially composed of dung remains. The significance of this study is not only in its general methodological contribution to archaeobotany, but also to lasting discussions regarding the contribution of dung remains to archaeological deposits used for seed, pollen and phytolith analyses. We offer here a strong method for determining whether deposits derive from dung alone, are mixed, or absolutely do not contain dung. This has important ramifications for archaeological interpretation.

A flintlock musket and a brass case with two nails attached, were retrieved from the Akko 1 shipwreck, dated to the early 19th century, and studied using metallurgical analysis. Both artefacts were covered with encrustation and concretion. The iron musket barrel and the iron nails did not survive; only corrosion products and oxides were left of them. The brass case, the brass musket ramrod pipe, and the wood texture were well preserved. In both artefacts the iron was sacrificed to protect the brass. This information may assist in future conservation of similar objects.

A unique set of circumstances has preserved a group of rare wooden artefacts deep within burial caves in the southern Levant. Identified as spindles and distaffs, they are fashioned from tamarisk wood and date to the Late Chalcolithic period. Analysis suggests that these implements were used to spin flax fibres, and they provide the earliest evidence for two distinct spinning techniques, drop spinning and supported spinning (with rolling on the thigh). One wooden spindle with the whorl still in place is the oldest such tool to survive intact in the Near East. The lead forming the whorl may have originated in Anatolia, and it is evidence, perhaps, of early long-distance trade.

We report results of palynological investigation of a core of sediments extracted from the bottom of the Sea of Galilee. The core was sampled at high resolution for both palynological analysis (a sample was taken c. every 40 years) and radiocarbon dating. The article focuses on the Early Bronze and Intermediate Bronze Ages, c. 3600–1950 BC. The results enable reconstruction of the vegetation and thus climate in the lake's fluvial and alluvial catchment, which includes large parts of northern Israel and Lebanon and south-western Syria. The study sheds light on topics such as changes in olive cultivation through time and regions, processes of urbanization and collapse and settlement expansion and retraction in the arid zones.

The Armenian kites are the northernmost known kites in south-west Asia. In contrast to those in the deserts further south, their research has only recently begun. The Armenian kites are situated at high elevations, mostly between 900 and 1500 m above mean sea level, in steppic conditions where Artemisia is at present the dominant shrub on the landscape. In our ongoing project we excavated three V-shaped kites and one enclosure kite. The two kinds are similar in construction details, but they differ in size and location: the former run down into gullies, while the latter were placed on the plateau. Six OSL ages suggest terminal Late Bronze Age and Early Iron Age construction dates, while geomorphological considerations and surface artefacts suggest earlier dates. A preliminary palynological study suggests a gradual increase in grazing-resistant vegetation since the mid-Holocene, probably reflecting human impact on the natural vegetation through the herding of grazing animals.

A new high-resolution palynological record from the Sea of Galilee (Israel), roughly spanning the Last Glacial Maximum (LGM) obtained from a trench dug in the vicinity of the well-dated prehistoric site of Ohalo II (23–24 ka cal. BP) — combined with detailed litho-stratigraphic and magnetic susceptibility analyses — provides evidence of vegetation, lake levels and climate change in the northern Jordan Valley. The sequence begins with laminated marls of the last Lake Lisan high stand and ends with the near-shore deposits containing the prehistoric site. Palynologically, the early phase of the high stand (pollen zone 1) is characterised by high-AP (mainly Quercus ithaburensis), reflecting a relatively humid climate. During its later part (zone 2), the increase in Artemisia indicates a regional drying. Several fluctuations in lake levels and humidity are recorded (pollen zones 3–4) prior to human occupation at the prehistoric camp, during a renewed humid climate (pollen zone 5); in its early phase Quercus ca...

The identification of historical events by geological and archaeological evidence is often ambiguous and conflicting, undermining the enormous potential for sub-annual precision in dating. The ruin of one of the largest pottery factories in the Middle East during Byzantine times, recently excavated in Yavneh (central Israel), exemplifies this: aligned fallen walls and columns and a kiln that collapsed while still in operation, with dozens of ceramic storage jars in articulation. Archaeological dating, which limits the time of the collapse to the seventh century CE, cannot distinguish between two large documented earthquakes that occurred during this century. By using pollen grains trapped by the collapse, we were able to distinguish, for the first time, between the two candidate earthquakes: September 634 CE and early June 659 CE. The pollen was extracted from the dust captured on the floor of the kiln during the cooling process of the vessels. The dust was collected only from below in situ whole vessels,...

This article describes the earliest evidence for the growing of two prestigious fruit trees:Juglans regia(Persian walnut) andCitrus medica(citron) in ancient Israel. The study also tries to identify the origin of these trees as well as their influence on Jewish tradition and culture. The palynological information from the Southern Levant supports the hypothesis of the survival ofJ. regiaduring the Last Glacial period in some areas of Eurasia. Accumulating palynological information as well as archeobotanical evidence ofJ. regiaplant remains from northern Israel from ∼1800 years BCE suggests the beginning of horticulture of walnut in the Southern Levant. The growing of walnut within Israel probably started in the north, and nearly one millennium later, palynological evidence indicates thatJ. regiacultivation had spread also to the Judean Mountains. Walnut is mentioned only once in the Bible, in Song of Solomon (6:11). From the interpretation of this text as well other Jewish texts and the available palynological diagrams, it is clear that since the Persian period (fifth to fourth centuries BCE),J. regiawas well established in ancient Israel. Citron, although being one of the four species of the Jewish feast of Tabernacles (Sukkot), is not native to the flora of the Near East. The earliest archeobotanical evidence of the growing ofC. medicain Israel was recently discovered in a Royal Persian garden in Ramat Rahel near Jerusalem, dated to the fifth to fourth centuries BCE.C. medicaseems to have made its way to Ramat Rahel from India via Persia. From that point on, citron gradually penetrated the Jewish culture and tradition. The citron is not mentioned in the Bible, and the association between the citron and thePürî `ëc hädär(Leviticus 23:40), translated “fruit of the goodly tree,” was only made during the first century AD.

This study is the first to successfully address the identification of the botanical components of a garden in the 2000-year-old palatial courtyard of Herod the Great's Promontory Palace in Caesarea Maritima. Based on the extraction and identification of fossil pollen grains, we were able to reconstruct at least part of the garden's flora, which, we argue, could only have grown within the confines of a garden of this splendid seaside palace which was protected architecturally from salty sea spray. The palynological spectrum included, among other taxa, high percentages of Cupressaceae pollen (cypress) as well as pollen of the non-local tree Corylus sp. (hazelnut), which was most probably introduced as an ornamental from the northeast Mediterranean or from Italy. These trees appear to have been accompanied by other ornamental plants (e.g. Salvia and various Rosaceae plants). The choice of flora to be planted in the garden is consistent with our knowledge of prestige Roman gardens dated to Herod's time. This exceptional and magnificent palace, with its luxurious architectural features and its impressive, well-maintained garden, symbolized the power and the abilities of King Herod, the greatest builder in ancient Jewish history.

Professor Dani Zohary with “his beloved artichokes.” With his friend and partner Jehuda Basnizki, Dani Zohary developed seed propagation of the traditionally vegetatively propagated globe artichoke...

The history of lake-level changes at the Dead Sea during the Holocene was determined mainly by radiocarbon dating of terrestrial organic debris. This article reviews the various studies that have been devoted over the past 2 decades to defining the Dead Sea levels during the Bronze and Iron Ages (~5.5 to 2.5 ka cal BP) and adds new data and interpretation. In particular, we focus on research efforts devoted to refining the chronology of the sedimentary sequence in the Ze’elim Gully, a key site of paleoclimate investigation in the European Research Council project titled Reconstructing Ancient Israel. The Bronze and Iron Ages are characterized by significant changes in human culture, reflected in archaeological records in which sharp settlement oscillations over relatively short periods of time are evident. During the Early Bronze, Intermediate Bronze, Middle Bronze, and Late Bronze Ages, the Dead Sea saw significant level fluctuations, reaching in the Middle Bronze an elevation of ~370 m below mean sea level (bmsl), and declining in the Late Bronze to below 414 m bmsl. At the end of the Late Bronze Age and upon the transition to the Iron Age, the lake recovered slightly and rose to ~408 m bmsl. This recovery reflected the resumption of freshwater activity in the Judean Hills, which was likely accompanied by more favorable hydrological-environmental conditions that seem to have facilitated the wave of Iron Age settlement in the region. DOI: 10.2458/azu_rc.57.18560

This article presents the role of climate fluctuations in shaping southern Levantine human history from 3600 to 600 BCE (the Bronze and Iron Ages) as evidenced in palynological studies. This time interval is critical in the history of the region; it includes two phases of rise and decline of urban life, organization of the first territorial kingdoms, and domination of the area by great Ancient Near Eastern empires. The study is based on a comparison of several fossil pollen records that span a north-south transect of 220 km along the southern Levant: Birkat Ram in the northern Golan Heights, Sea of Galilee, and Ein Feshkha and Ze’elim Gully both on the western shore of the Dead Sea. The vegetation history and its climatic implications are as follows: during the Early Bronze Age I (~3600–3000 BCE) climate conditions were wet; a minor reduction in humidity was documented during the Early Bronze Age II–III (~3000–2500 BCE). The Intermediate Bronze Age (~2500–1950 BCE) was characterized by moderate climate conditions, however, since ~2000 BCE and during the Middle Bronze Age I (~1950–1750 BCE) drier climate conditions were prevalent, while the Middle Bronze Age II–III (~1750–1550 BCE) was comparably wet. Humid conditions continued in the early phases of the Late Bronze Age, while towards the end of the period and down to ~1100 BCE the area features the driest climate conditions in the timespan reported here; this observation is based on the dramatic decrease in arboreal vegetation. During the period of ~1100–750 BCE, which covers most of the Iron Age I (~1150–950 BCE) and the Iron Age IIA (~950–780 BCE), an increase in Mediterranean trees was documented, representing wetter climate conditions, which followed the severe dry phase of the end of the Late Bronze Age. The decrease in arboreal percentages, which characterize the Iron Age IIB (~780–680 BCE) and Iron Age IIC (~680–586 BCE), could have been caused by anthropogenic activity and/or might have derived from slightly drier climate conditions. Variations in the distribution of cultivated olive trees along the different periods resulted from human preference and/or changes in the available moisture. DOI: 10.2458/azu_rc.57.18555

A detailed pollen record for the time interval of ∼2500–500 BCE, which covers the time period of the Intermediate Bronze Age (Early Bronze Age IV) into the Iron Ages in the Levant, is presented. The study was conducted in the Ze’elim Gully, which drains the southern Judean Highlands into the Dead Sea. During the Bronze and Iron Ages, the Judean Highlands exhibited dramatic settlement fluctuations. To better understand these oscillations, high-resolution fossil pollen data were combined with a recent pollen data set, lithological features, radiocarbon dating and palaeohydrological information derived from the Dead Sea levels. Due to the occurrence of hiatuses in this fluvial environment, we used a composite profile which was based on two palynological-sedimentological profiles. This integrated information enabled us to reconstruct in great detail for the first time the environmental conditions in relation to the picture derived from archaeological field-work in the Judean Highlands. Evidence for drier clim...