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===Black Sea=== In 1976, [[Willard Bascom]] suggested that the deep, [[anoxic waters]] of the [[Black Sea]] might have preserved ships from antiquity because typical wood-devouring organisms could not survive there. At a depth of 150 m, it contains insufficient oxygen to support most familiar biological life forms.{{citation_needed|date=August 2019}} Originally a land-locked freshwater lake, the Black Sea was flooded with salt water from the [[Mediterranean Sea]] during the [[Holocene]]. The influx of salt water essentially smothered the freshwater below it because a lack of internal motion and mixing meant that no fresh oxygen reached the deep waters,<ref>OΔuz, T., Latun, V.S., Latif, M.A., Vladimirov, V. L., Sur, H. I., Markov, A. A., Ozsoy, E. Kotovschichkov, B. B., Eremeev, V.N., and Unluata, U., 1993, Circulation in the surface and intermediate layers, ''Deep-Sea Research'' 1.40: 1597–612.</ref> creating a [[meromictic]] body of water. The anoxic environment, which is hostile to many biological organisms that destroy wood in the oxygenated waters, provides an excellent testing site for deep-water archaeological surveys.{{citation_needed|date=August 2019}} In a series of expeditions, a team of marine archaeologists led by Ballard identified what appeared to be ancient shorelines, freshwater snail shells, and drowned river valleys in roughly 300 feet (100 m) of water off the Black Sea coast of modern [[Turkey]].<ref>{{cite web|url=http://www.theguardian.com/science/2000/sep/14/internationalnews.archaeology|title=Evidence found of Noah's ark flood victims|last=Radford|first=Tim|work=[[The Guardian]]|date=September 14, 2000|access-date=August 21, 2022|archive-date=August 21, 2022|archive-url=https://web.archive.org/web/20220821134355/https://www.theguardian.com/science/2000/sep/14/internationalnews.archaeology|url-status=live}}</ref><ref>{{cite web|url=https://www.nationalgeographic.com/ngnews/blacksea.html|title=Evidence of Human Habitation in the Black Sea @ nationalgeographic.com|publisher=[[National Geographic]]|access-date=August 21, 2022|archive-date=July 6, 2021|archive-url=https://web.archive.org/web/20210706010122/https://www.nationalgeographic.com/ngnews/blacksea.html|url-status=live}}</ref> [[Radiocarbon]] dating of freshwater mollusk remains indicated an age of about 7,000 years.{{citation_needed|date=August 2019}} The team discovered three ancient wrecks west of the town of [[Sinop, Turkey|Sinop]] at depths of 100 m. Wreck A and Wreck C probably date to the late Roman period (2ndβ4th century A.D.), while Wreck B probably dates to the Byzantine period (5th to 7th century A.D.).{{citation_needed|date=August 2019}} To the east of Sinop, the team discovered a remarkably well-preserved wreck at a 320 m depth, in the Black Sea's deep anoxic waters. The vessel's entire hull and cargo are intact, buried in sediments. Its deck structures are also intact, including a mast rising 11 m into the water column. Radiocarbon dating of wood from the wreck provides a date of 410β520 A.D. It has been named "Sinop D" by the Ballard team.{{citation_needed|date=August 2019}} In 2000, the team conducted an expedition that focused on exploration of the seabed about 15β30 km west of Sinop, and an additional deep-water survey east and north of the peninsula. Their project had several goals. They sought to discover whether human habitation sites could be identified on the ancient submerged landscape, they examined the sea-bed for shipwrecks (where they found Sinop A-D), to test the hypothesis that the anoxic waters below 200 m would protect shipwrecks from the expected biological attacks on organic components, and to seek data about an ancient trade route between Sinop and the [[Crimea]] indicated by terrestrial archaeological remains.{{citation_needed|date=August 2019}} Although Sinop served as a primary trade center in the Black Sea, the wrecks were located west of the trade route predicted by the prevalence of Sinopian ceramics on the Crimean peninsula. On wrecks A-C, mounds of distinctive carrot-shaped shipping jars, called [[amphorae]], were found. They were of a style associated with Sinop and retained much of their original stacking pattern on the sea floor. The jars may have carried a variety of archetypal Black Sea products such as olive oil, honey, wine, or fish sauce. The contents are unknown because no artifacts were recovered from these wreck sites in 2000.{{citation_needed|date=August 2019}} The wreck provided the team with vast information about the technological changes and trade in the Black Sea during political, social, and economic transition through their study of the ship's construction techniques. Studies show that in Sinop during the Byzantine era, they had developed long-distance trading as early as 4500 BC. Sea-trading on the Black Sea was most intense during the period of late antiquity, between the 2nd and 7th centuries AD.<ref>Hiebert, F., 2001, Black Sea coastal cultures: trade and interaction, ''Expedition'' 43: 11β20</ref> The examination of the four shipwrecks found by Ballard and his team provide the direct evidence for Black Sea maritime trade so well attested by the distribution of ceramics on land.{{citation_needed|date=August 2019}} The video images of Shipwreck A show a wall of shipping jars standing about 2 m above the seabed. The amphorae highest on the mound had fallen over without displacing those still standing in the rows beneath them, and, likely, the ship settled upright on the seabed gradually being both buried in and filled with sediment as exposed wood was devoured by the larva or the [[shipworm]].{{citation_needed|date=August 2019}} Shipwreck B also consisted of a large pile of amphorae but several types are visible, as are multiple timbers protruding from within the mound and on it. In addition to the Sinop-style jars, several amphorae similar to examples excavated on the [[Yassiada]] Byzantine shipwreck and dating from the 5th to late 6th century AD are present.<ref>van Doorninck, F. H. Jr., 2002, Byzantine shipwrecks, in A. Laiou (ed.), ''The Economic History of Byzantium from the Seventh through the Fifteenth Century'' I, 899β905. Dumbarton Oaks Studies 30, Washington, DC.</ref> Two discrete and mostly buried piles of carrot-shaped shipping jars comprise shipwreck C. The team's visit to the site was short and was intended primarily to test survey methodology for deep-water procedures.{{citation_needed|date=August 2019}} Shipwreck D provided the team with an unprecedented opportunity to document hull construction during a time of transition. When observing the sonar signature of Shipwreck D, a long, slender upright feature on the seabed, transformed itself into a wooden mast. Elements rarely present on shallower shipwreck sites are beautifully preserved 200 m below the surface. Disappointingly for ship scholars and historians of technology, there are few indications of how the planks of Sinop D are held together. There are no [[mortise and tenon]] fastenings and no sewing. Shipwreck D may be one of the earliest [[lateen]]-rigged ships to be studied by archaeologists. The angle of the mast and the lack of fittings on it suggest that a lateen sail is the most likely configuration for such a small vessel.{{citation_needed|date=August 2019}} The Institute for Exploration Black Sea expeditions relied on remote sensing with side-scan sonar in shallow and deep water to identify potential archaeological sites examined by [[Remotely operated underwater vehicle|ROV]]s. The hypothesis that the anoxic waters of the Black Sea would allow extraordinary organic preservation is borne out by the discovery of Sinop D, the 1,500-year-old shipwreck with excellent preservation of features above the sediment layer.<ref>Ballard, Robert D., and Ward, Cheryl, 2004, Deep-water Archaeological Survey in the Black Sea; 2000 Season, ''The International Journal of Nautical Archaeology'', 33.1: 2β13, ([http://www.coastal.edu/archaeology/cward/Ward%20publication%20files/Ward%20and%20Ballard%202004%20IJNA.pdf online] {{webarchive|url=https://web.archive.org/web/20130522033235/http://www.coastal.edu/archaeology/cward/Ward%20publication%20files/Ward%20and%20Ballard%202004%20IJNA.pdf |date=May 22, 2013 }}).</ref> According to a report in ''[[New Scientist]]'' magazine (May 4, 2002, p. 13), the researchers found an underwater delta south of the [[Bosporus]]. There was evidence of a strong flow of fresh water out of the Black Sea in the [[8th millennium BC]]. Ballard's research has contributed to the debate over the [[Black Sea deluge theory]].{{citation_needed|date=August 2019}}
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