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In Oman, many coastal sites dated to the Neolithic have yielded material culture related to ornament manufacture. These sites are the remnants of fishermen occupations, developing an economy mainly based on maritime and mangrove resources. The Omani islands of Maṣīrah and Al‐Ḥallāniyah are both situated in the Arabian Sea. Today, Maṣīrah is located about 20 km from the continent, while Al‐Ḥallāniyah is part of the Khurīyā Murīyā archipelago off the southern coast of Oman. On Maṣīrah, workshops have been discovered in Neolithic shell middens, revealing the work of stone and Spondylus sp. shells for bead production, using lithic tools. Separated by approximately 400 km from Maṣīrah, Al‐Ḥallāniyah yielded several Neolithic sites with similar evidence for shell bead production. The main lithic tools discovered are micro‐drills, pièces esquillées (splintered pieces) made of local chert, and multitasking tools made of stone, used as anvils, hammerstone and/or polishing stone. Most of the micro‐drills are made from bladelets either with sharped edges or with steep edges and testify to predetermined knapping operations. However, others created on undifferentiated flakes appear to be more opportunistic (or expedient). Micro‐drills of the Maṣīrah and Al‐Ḥallāniyah types seem to be quite new to the Neolithic toolkit of coastal Oman. Pièces esquillées demonstrate the use of bipolar flaking (performed on an anvil) but functional questions remain. These could be cores, but also chisels used between a hammer and a material (shell) placed on an anvil. Stone tools show marks that are characteristic of use as hammers, anvils and as tools used to polish the beads after perforation. [ABSTRACT FROM AUTHOR]

For over a decade, the French mission 'Archaeology of the Arabian Seashores' has been exploring the evolution of the Omani coastline, from hunter–gatherers to the rise of complex societies during the crucial passages from the culmination of the Pleistocene to the Early Bronze Age, passing through the Neolithic. The team extensively surveyed the land spreading from the eastern head of Arabia, Ra's al‐Hadd and Ra's al‐Jinz, to the last villages of Dhofar, including Masirah Island and the Hallaniyyat archipelago, covering 1000 km. Most Final Palaeolithic, Neolithic and Early Bronze Age sites were tested or excavated. A multidisciplinary approach that involves the joint work of archaeologists and geologists was chosen to include the contribution of environmental factors to modifying the equilibriums between the natural environment and human communities through the study of climatic and eustatic fluctuations. The project provided a substantive perspective on the evolution of maritime communities between 10,000 and 2000 bce. Moreover, an interdisciplinary and multiscalar approach for describing and analysing the change in the material culture of this region made it possible to transcend the traditional typology and examine the role of human communities' interaction. [ABSTRACT FROM AUTHOR]

In southern and south-eastern Arabia, the Neolithic developed between 6500 and 3100 BCE. In the Sultanate of Oman, occupation occurred along wadi banks, around paleolakes, and at large shellmiddens accumulated on the shores of the Arabian Sea. Nevertheless, the origins and development of human occupation on the Arabian Sea islands are poorly known, if not totally undocumented. After exploring the archaeological potential of the large island of Masirah, we focused our research on the small Al-Hallaniyat archipelago (formerly known as the Kuria Muria islands). A preliminary archaeological survey led us to test several sites belonging to different occupational phases on the island, and we explored the largest shell-midden at the HLY-4 site in 2014 and 2019. Radiocarbon dating results, along with lithic analysis, demonstrate that at around 4200-4000 BCE, a Neolithic community settled the largest island (Al-Hallaniyah). While goats and dogs had been introduced as livestock, fish and dolphins were regularly fished and captured as a main food resource together with marine turtles and nesting birds. At HLY-4, not only lithic and bone artifacts characterize the assemblage, as standardized discoid marine-shell beads were also manufactured. The Neolithic conquest of Masirah Island occurred early in the Neolithic (at the beginning of the sixth millennium BCE), while the settlements on the Farasan islands (in the Red Sea) are dated to around 4500 BCE, and thus the ones on the Al-Hallaniyat archipelago to the end of the fifth millennium BCE. In Arabia, their chronological assessment marks the final conquest of the insular areas. [ABSTRACT FROM AUTHOR]

We successfully measured four radiocarbon dates on two specimens of a black geometric rock painting with a fragment in jeopardy of naturally spalling off in the wall of a rock shelter in the Ẓufār region, in the south of the Sultanate of Oman. Extraction of carbon dioxide (CO2) for radiocarbon dating of the binder in the black pigment of the rock painting specimen was conducted in the plasma oxidation laboratory at the Office of Archeological Studies in Santa Fe, NM. The radiocarbon content was measured on the Swiss ETH-Zürich accelerator mass spectrometer MICADAS. The dates obtained agreed with one another within the statistical uncertainty and the average date of the four samples was 1500 ± 35 radiocarbon years BP. The calendric equivalents of the average date results in calendric calibration date ranges that span the mid-fifth through mid-seventh centuries (440–453 CE, 478–496 CE, and 534–646 CE). This research demonstrates that it is possible to date the black paintings of the Jebel al-Qara' area of Oman; this is the first pictogram that was dated using radiocarbon dating in the region. [ABSTRACT FROM AUTHOR]

Here we describe a new elasmobranch assemblage consisting of isolated dental material from the Aquitanian near-shore marine deposits of the Shuwayr and Warak formations at Sharbithat, in eastern Sultanate of Oman. The faunal composition clearly indicates affinities to other early Miocene elasmobranch-bearing localities worldwide. This assemblage is predominantly composed of large and common pelagic sharks as well as teeth attributable to a new species of fantail stingray, Taeniurops tosii, as old as the oldest undisputable fossil records of Taeniurops. The study of this fossil assemblage presented here improves the knowledge of the ancient elasmobranchs that frequented the eastern Arabian coasts during the closure of the Neotethys and the birth of the Arabian Sea. [ABSTRACT FROM AUTHOR]

A mega‐tooth belonging to a Miocene fossil shark was discovered along the shores of the Arabian Sea inside one of the Neolithic domestic settlements at Sharbithat (SHA‐10) (Sultanate of Oman). Attributed to a representative of the extinct genus Otodus (Megaselachus), this tooth is the first ever discovered in the Arabian Peninsula. In the field, research permitted the localization and study, a few kilometres away, of the palaeontological deposit where this retrieval was made. The shark, traditionally extensively hunted on the shores of the Arabian Sea, is well attested in the region's Neolithic ichthyological assemblages. Moreover, during this period, some groups of seaborne hunters were specialized in this form of fishing, which was indeed quite dangerous. But why did an individual some 5,500 years ago collect this curio, an unusual fossil, but also one he could easily recognize? The fossils of large sharks sometimes played an important part in ancient societies. Could this also have been the case in South‐Eastern Arabia? [ABSTRACT FROM AUTHOR]

We present the results of the geomorphological mapping of a region of the Dhofar (Sultanate of Oman) including two contrasting physiographic units sharing a common drainage system into the Arabian Sea: the Jebel Qara limestone massif and the coastal plain of Salalah. Neogene to Quaternary tectonic activity controlled the formation of an extensive system of faults and caused the uplift of the Jebel Qara, forming structural escarpments. The massif underwent karstification and subsequent linear erosion. Today the Jebel is cut by a dendritic net of dry valleys, occasionally dammed by calcareous tufa dams. The transition between the southern escarpment of the Jebel and the plain below displays flat alluvial fans, bordered by a strip of beachrock, coastal dunes, and coastal lagoons, located in correspondence to estuaries. Dramatic soil erosion is evident, linked to intense human-triggered zoogeomorphological processes started in the Mid-Late Holocene after the introduction of pastoral land-use. [ABSTRACT FROM AUTHOR]

The study of the fish bones from the Neolithic shell midden of Suwayh 1, excavated in the 2000s, identified a total of 1060 identifiable fish bones, from 23 families, 33 genera and 28 different species. Radiocarbon dating demonstrates that the sites date to the early 6th to mid 5th millennium BC. The results follow an eight‐phase chronology highlighted by an earlier malacological study. The most important taxa were the Carcharhinidae (requiem shark), Rhinopteridae (cownose rays), Sparoidea (Sparidae and Lethrinidae: sea breams and emperors) and Ariidae (sea catfishes). The results of the fish study show that the Suwayh lagoon must have gradually opened up to the sea and been populated with mangroves. The unique presence of so many sharks at this site seems to indicate that the inhabitants had a special interest in shark fishing and that their location was ideal for this specialised activity. Two types of fishing nets and hooks have been discovered, which require the use of different fishing techniques. [ABSTRACT FROM AUTHOR]

For decades, so-called Fasad points have been discovered in Oman and the UAE. These lithic projectile points have been until now fossiles directeurs (or defining artefacts) for Early Holocene human occupation prior to the development of the Arabian Neolithic. It appears that many different types of points are described in the literature as Fasad points, but the actual variability of the archaeological discoveries leads to the necessity for reassessment and clarification of the very definition of this type of artefact. We propose here a new definition of the Fasad points with the creation of sub-types. We also discuss the trend of using this lithic type as a marker for the diffusion of PPNB technology towards the south-east from the Mediterranean Levantine Neolithic core area. [ABSTRACT FROM AUTHOR]

During the Neolithic and Early Bronze Age, many teeth of large sharks ( Carcharhinus leucas) and stingray spines were transformed into projectile points in south-eastern Arabia. These points were probably used for fishing. Deriving from dangerous and/or toxic animals, shark teeth and stingray spines were certainly markers of prestige. [ABSTRACT FROM AUTHOR]