Ancient harbors and Holocene morphogenesis of the Ras Ibn Hani peninsula (Syria)

2012 ◽  
Vol 78 (1) ◽  
pp. 35-49 ◽  
Author(s):  
Nick Marriner ◽  
Jean-Philippe Goiran ◽  
Bernard Geyer ◽  
Valérie Matoïan ◽  
Michel al-Maqdissi ◽  
...  

AbstractRas Ibn Hani peninsula, a wave-dominated tombolo (800 × 1000 m) on the Syrian coast, provides evidence for significant Holocene changes that can be linked to geological inheritance, rising post-glacial sea level, sediment supply and human impacts. Initial development of Ras Ibn Hani's coastal system began ~ 8000 years ago when shallow marine environments formed in a context of rising post-glacial sea level. Following relative sea-level stabilization ~ 6000 cal yr BP, beach facies trace the gradual formation of a wave-dominated sandbank fronted by a ~ 2300 × ~ 500 m palaeo-island whose environmental potentiality was attractive to Bronze Age societies. A particularly rapid phase of tombolo accretion is observed after ~ 3500 cal yr BP characterised by a two- to fourfold increase in sedimentation rates. This is consistent with (i) a pulse in sediment supply probably driven by Bronze Age/Iron Age soil erosion in local catchments, and (ii) positive feedback mechanisms linked to regionally attested neotectonics. Archaeological remains and radiocarbon datings confirm that the subaerial tombolo was probably in place by the Late Bronze Age. These data fit tightly with other eastern Mediterranean tombolo systems suggesting that there is a great deal of predictability to their geology and stratigraphy at the regional scale.

PLoS ONE ◽  
2021 ◽  
Vol 16 (6) ◽  
pp. e0251870
Author(s):  
Assaf Yasur-Landau ◽  
Gilad Shtienberg ◽  
Gil Gambash ◽  
Giorgio Spada ◽  
Daniele Melini ◽  
...  

This article presents new archaeological observations and multidisciplinary research from Dor, Israel to establish a more reliable relative sea level for the Carmel Coast and Southern Levant between the Middle Bronze Age and the Roman period (ca. 3500–1800 y BP). Our record indicates a period of low relative sea level, around -2.5 m below present, from the Middle Bronze Age to the Hellenistic period (ca. 3500–2200 y BP). This was followed by a rapid rise to present levels, starting in the Hellenistic period and concluding during the Roman period (ca. 2200–1800 y BP). These Roman levels agree with other relative sea-level indications from Israel and other tectonically stable areas in the Mediterranean. Several relative sea-level reconstruction models carried out in the current study provide different predictions due to their parameters and do not model the changes observed from field data which points to a non-isostatic origin for the changes. Long-term low stable Iron Age relative sea level can be seen in Dor, where Iron Age harbor structures remain around the same elevation between ca. 3100–2700 y BP. A similar pattern occurs at Atlit, the Iron Age harbor to the north used continuously from ca. 2900 y BP to the beginning of the Hellenistic period (ca. 2200 y BP). An examination of historical and archaeological sources reveals decline and occasional disappearance of Hellenistic sites along the coast of Israel at ca. 2200 y BP (2nd century BCE), as in the case of Yavneh Yam, Ashdod Yam, Straton’s Tower, and tel Taninim. In Akko-Ptolemais, the large harbor installations built in the Hellenistic period were never replaced by a substantial Roman harbor. The conclusions of this research are thus relevant for the sea-level research community and for the historical analyses of the Israeli and South Levantine coastline.


2021 ◽  
Vol 33 (2) ◽  
pp. 185-210
Author(s):  
Bartłomiej Lis ◽  
Trevor Van Damme

While handwashing is attested in the Bronze Age cultures of the eastern Mediterranean and appears in both Linear B records and Homeric epics, the custom has not been discussed with regard to the material culture of Mycenaean Greece. On analogy with Egyptian handwashing equipment, we explore the possibility that a conical bowl made of bronze and copied in clay was introduced in Greece early in the Late Bronze Age for this specific use. We integrate epigraphic, iconographic and formal analyses to support this claim, but in order to interrogate the quotidian function of ceramic lekanes, we present the results of use-wear analysis performed on 130 examples. As use-wear develops from repeated use over a long time, it is a good indicator of normative behaviour, particularly when large datasets are amassed and contrasted with other shapes. While not conclusive, our results allow us to rule out a function as tableware for food consumption, and in combination with all other analyses support the interpretation of lekanes as handwashing basins. We then trace the development of this custom from its initial adoption by elite groups to its spread among new social classes and venues after the collapse of the palace system: at home, as part of communal feasting and sacrifice or as an element of funerary rites. The widespread distribution of handwashing equipment after 1200 bc closely mirrors the situation in our earliest surviving Greek Iron Age texts and joins a growing body of evidence pointing to strong continuity in social practices between the Postpalatial period and the early Iron Age in Greece.


2010 ◽  
Vol 74 (2) ◽  
pp. 207-215 ◽  
Author(s):  
D. Kaniewski ◽  
E. Paulissen ◽  
E. Van Campo ◽  
H. Weiss ◽  
T. Otto ◽  
...  

AbstractThe alluvial deposits near Gibala-Tell Tweini provide a unique record of environmental history and food availability estimates covering the Late Bronze Age and the Early Iron Age. The refined pollen-derived climatic proxy suggests that drier climatic conditions occurred in the Mediterranean belt of Syria from the late 13th/early 12th centuries BC to the 9th century BC. This period corresponds with the time frame of the Late Bronze Age collapse and the subsequent Dark Age. The abrupt climate change at the end of the Late Bronze Age caused region-wide crop failures, leading towards socio-economic crises and unsustainability, forcing regional habitat-tracking. Archaeological data show that the first conflagration of Gibala occurred simultaneously with the destruction of the capital city Ugarit currently dated between 1194 and 1175 BC. Gibala redeveloped shortly after this destruction, with large-scale urbanization visible in two main architectural phases during the Early Iron Age I. The later Iron Age I city was destroyed during a second conflagration, which is radiocarbon-dated at circa 2950 cal yr BP. The data from Gibala-Tell Tweini provide evidence in support of the drought hypothesis as a triggering factor behind the Late Bronze Age collapse in the Eastern Mediterranean.


2018 ◽  
Vol 5 (2) ◽  
pp. 177-201 ◽  
Author(s):  
Michael Wagreich ◽  
Erich Draganits

This article reviews possible lower boundaries for an early Anthropocene period. Although a noticeable environmental impact of humans, caused by hunting, the use of fire, forest clearance, animal domestication and agriculture had already occurred in the Neolithic, these early signals are strongly diachronous and localised. Here, we examine early significant, synchronous and regional stratigraphic signals indicating an anthropogenic influence as consequences of mining and smelting-related trace metal contamination. A first regional lead contamination event in the Northern Hemisphere is recognized during the (Eastern Mediterranean) Late Bronze Age to Early Iron Age, between 3500 and 2800 BP, with a peak at around 3000 BP. Another pronounced anthropogenic lead peak is recorded around 2000 BP, during the Roman period. These events, as defined by lead enrichment and changes in lead isotope ratios, accompanied by other trace metal enrichments, are found in several types of archives, such as Arctic ice-cores and European peat-bogs, speleothems as well as fluvial, lake and marine records. Potential stratigraphic correlations and secondary markers may be present using tephrochronology, climate events, and magnetostratigraphy. Such a definition of the base of a formally defined (early) Anthropocene stage/period allows the application of the GSSP (Global Stratotype Section and Point) concept by using a point in a physical archive, and, in contrast to the late Anthropocene, includes a significant quantity of anthropogenic strata as evidence for an Anthropocene chronostratigraphic unit.


2017 ◽  
Vol 25 ◽  
pp. 487-510 ◽  
Author(s):  
Monika Badura ◽  
Ewelina Rzeźnicka ◽  
Urszula Wicenciak ◽  
Tomasz Waliszewski

The seaside settlement of Jiyeh in Lebanon, now identified with the ancient Porphyreon, boasts a history dating back to the Late Bronze Age and Iron Age when Phoenicia occupied part of the Levantine coast (eastern Mediterranean). Extensive archaeological excavations by a team from the Polish Centre of Mediterranean Archaeology University of Warsaw have focused on the urban residential quarter, which consists of numerous houses and buildings separated by passages, containing material that has provided important insights into the lives of its inhabitants over time. However, as archaeobotanical studies had not been conducted there before, the question of plant use remains an important and largely unknown area of research. This article presents the first botanical results from Jiyeh (seasons 2009–2014) and considers their implications for future cooperation between archaeologists and natural scientists.


2017 ◽  
Vol 17 (3) ◽  
pp. 449-466 ◽  
Author(s):  
Isavela N. Monioudi ◽  
Adonis F. Velegrakis ◽  
Antonis E. Chatzipavlis ◽  
Anastasios Rigos ◽  
Theophanis Karambas ◽  
...  

Abstract. The present contribution constitutes the first comprehensive attempt to (a) record the spatial characteristics of the beaches of the Aegean archipelago (Greece), a critical resource for both the local and national economy, and (b) provide a rapid assessment of the impacts of the long-term and episodic sea level rise (SLR) under different scenarios. Spatial information and other attributes (e.g., presence of coastal protection works and backshore development) of the beaches of the 58 largest islands of the archipelago were obtained on the basis of remote-sensed images available on the web. Ranges of SLR-induced beach retreats under different morphological, sedimentological and hydrodynamic forcing, and SLR scenarios were estimated using suitable ensembles of cross-shore (1-D) morphodynamic models. These ranges, combined with empirically derived estimations of wave run-up induced flooding, were then compared with the recorded maximum beach widths to provide ranges of retreat/erosion and flooding at the archipelago scale. The spatial information shows that the Aegean pocket beaches may be particularly vulnerable to mean sea level rise (MSLR) and episodic SLRs due to (i) their narrow widths (about 59 % of the beaches have maximum widths < 20 m), (ii) their limited terrestrial sediment supply, (iii) the substantial coastal development and (iv) the limited existing coastal protection. Modeling results indeed project severe impacts under mean and episodic SLRs, which by 2100 could be devastating. For example, under MSLR of 0.5 m – representative concentration pathway (RCP) 4.5 of the Fifth Assessment Report (AR5) of the Intergovernmental Panel on Climate change (IPCC) – a storm-induced sea level rise of 0.6 m is projected to result in a complete erosion of between 31 and 88 % of all beaches (29–87 % of beaches are currently fronting coastal infrastructure and assets), at least temporarily. Our results suggest a very considerable risk which will require significant effort, financial resources and policies/regulation in order to protect/maintain the critical economic resource of the Aegean archipelago.


Complutum ◽  
2021 ◽  
Vol 32 (1) ◽  
pp. 29-47
Author(s):  
Francisco B. Gomes

 First highlighted as possible markers for early, 2nd millennium BCE contacts between the Iberian Peninsula and the Eastern Mediterranean, phytomorphic carnelian pendants have become a significant part of the discussion on that subject. However, a number of new finds which have taken place in recent years have transformed the available image regarding both the geographic distribution and the chronological setting of these pieces. An updated overview is presented here, which suggests they should now preferably be considered as part of the array of prestige goods introduced in the Far West by Phoenician trade between the later stages of the Late Bronze Age and the Early Iron Age


Author(s):  
Roger B. Ulrich

The inherent strengths, weaknesses, and availability of diverse Roman building materials governed the techniques used in construction and greatly influenced the final appearance of Roman architecture. Trace archaeological evidence exists of buildings and burials in Rome from the Italian Bronze Age (second millennium bce) or earlier, and substantial physical remains, in the form of Iron-Age huts and grave goods, roughly correspond to the Romans’ own belief of the foundation date of their city (traditionally 753 bce). Rome’s earliest builders sourced materials obtainable from the immediate environment and transformed them using practical knowledge. Within the span of a couple centuries, architectural design, implementation, and decoration reflect a broad interaction between Roman builders and their counterparts in the regions around central Italy (particularly Etruria to the north and Campania to the south) and also the wider Mediterranean world, particularly those areas where Greeks traditionally lived or had placed colonies. While southern Italy and Sicily represent the closest areas for the transmission of Greek ideas, Greek building practices on the Greek mainland and in Asia Minor also influenced Roman projects from the Archaic period onwards. As Rome grew wealthier and expanded abroad, patrons and builders imported marble to the capital from the Aegean, well before the discovery of more local, Italian sources. The importation of exotic stones grew exponentially over the period of the late Republic and the first two centuries of empire. The coloured marbles that embellished the buildings of Rome served as physical testimony to Rome’s control over the eastern Mediterranean. Nothing, however, was as transformative as the adoption of concrete in the late 3rd century bce, the mass production of fired brick, and the ensuing experimentation that resulted in the vaulted structures that have become the hallmark of Roman architecture.


Sign in / Sign up

Export Citation Format

Share Document