Tarsus

Author(s):  
Clyde E. Fant ◽  
Mitchell G. Reddish

Tarsus, best known as the home of the Apostle Paul, was the principal city of the eastern Cilician plain. A city renowned in antiquity as a center of culture and learning, Tarsus was visited by such figures as Julius Caesar, Mark Antony, and Cleopatra. Recent excavations have uncovered more remains of the city from Hellenistic and Roman times, including a paved, colonnaded street. Tarsus, the capital of the ancient province of Cilicia, is located near the eastern Mediterranean coast of Turkey. Situated today 10 miles inland from the sea, Tarsus served as a port city because the Cydnus River (today the Tarsus Çayï) passed through Tarsus on its way to the sea. The river was navigable by ships from the Mediterranean coast to Tarsus. Lake Rhegma, a lagoon near the Mediterranean coast into which the river flowed, served as the harbor for Tarsus. During the 6th century C.E., Emperor Justinian moved the course of the Cydnus River to the east of Tarsus, while leaving several minor branches of the river to flow through the city. The city of Tarsus belonged to the region of Asia Minor known as Cilicia. Ancient Cilicia was composed of two parts, Cilicia Pedias (“flat” or “smooth” Cilicia) and Cilicia Trachaei (“rough” Cilicia). Cilicia Pedias was a fertile plain in the eastern part of the region, whereas Cilicia Trachaei was a rugged, heavily forested mountainous region in the western part, dominated by the Taurus Mountains. Tarsus, the major city of Cilicia Pedias, was located just south of the Cilician Gates, the main pass through the Taurus Mountains. Through this pass ran the major road connecting Syria to Asia Minor, thus providing Tarsus access to trade and travel over land as well as over the Mediterranean. The earliest settlement at Tarsus was likely at Gözlü Kule, a tumulus on the southeast side of modern Tarsus. Excavations under the direction of Hetty Goldman of Princeton University before and immediately after World War II at the tumulus discovered evidence that the site was occupied from Neolithic to Islamic times. At least as early as the 3rd millennium B.C.E., a fortified town existed at the site of Tarsus.

Check List ◽  
2015 ◽  
Vol 11 (2) ◽  
pp. 1588 ◽  
Author(s):  
Saadet Yağmur Bulguroğlu ◽  
Jale Korun ◽  
Mehmet Gökoğlu

New information on distribution of marine leech, Pontobdella muricata (Linnaeus, 1758) is given here. One leech was observed on the dorsal surface of Thornback Ray, Raja clavata (Linnaeus, 1758) that was caught in 2013 in the Antalya, Turkey. This is a new record for the eastern Mediterranean coast of Turkey.


Author(s):  
Clyde E. Fant ◽  
Mitchell G. Reddish

Antalya, the modern name for ancient Attalia, is a delightful city perched on the Mediterranean coast of southern Turkey. The eleventh largest city in modern Turkey, Antalya is a thriving tourist center. Although many visitors to the city use it as a base for visiting beaches along Turkey’s Mediterranean coast or archaeological sites in nearby locations, Antalya has plenty of charm and interest of its own. Attalia was a city in the region known as Pamphylia, an area bounded by the Taurus Mountains on the north and the Mediterranean Sea on the south. Situated on what is now called the Gulf of Antalya, the city served as the major port in Pamphylia during Hellenistic, Roman, and Byzantine times. Attalus II, who was king of Pergamum from 159 to 138 B.C.E., founded the city and named it after himself. When Attalus III (r. 138–133 B.C.E.) bequeathed the Pergamum kingdom to Rome in his will, Attalia was one of the areas excluded and thus became a free city for a while. In 77 B.C.E. Attalia was annexed by the Romans. During the 2nd century C.E. Emperor Hadrian conferred the status of colony on the city and visited Attalia in 130 C.E. The Hadrian Gate was built to commemorate this visit. Dedicated to the emperor, the triple-arched gate was made of marble and contained a dedicatory inscription in bronze letters. During the Byzantine era the city was known as Adalia and continued to serve as an important port city. Used by the Crusaders as a harbor on their way to the Holy Land, the city was conquered by the Seljuk Turks in 1207. The Seljuks left their mark upon the city by means of several buildings, some of which still decorate the city’s landscape. Around the end of the 14th century, the Ottomans gained control of the city. During this period Antalya continued to flourish and serve as an important harbor on the Mediterranean. When the Allies dismantled the Ottoman Empire at the end of World War I, Antalya was given to Italy, only to be retaken by the Turkish army in 1921.


2018 ◽  
Vol 90 (1) ◽  
pp. 10-25 ◽  
Author(s):  
Carole Nehme ◽  
Sophie Verheyden ◽  
Sebastian F.M. Breitenbach ◽  
David P. Gillikin ◽  
Anouk Verheyden ◽  
...  

AbstractLittle is known about terrestrial climate dynamics in the Levant during the penultimate interglacial-glacial period. To decipher the palaeoclimatic history of the Marine Oxygen Isotope Stage (MIS) 6 glacial period, a well-dated stalagmite (~194 to ~154 ka) from Kanaan Cave on the Mediterranean coast in Lebanon was analyzed for its petrography, growth history, and stable isotope geochemistry. A resolved climate record has been recovered from this precisely U–Th dated speleothem, spanning the late MIS 7 and early MIS 6 at low resolution and the mid–MIS 6 at higher resolution. The stalagmite grew discontinuously from ~194 to ~163 ka. More consistent growth and higher growth rates between ~163 and ~154 ka are most probably linked to increased water recharge and thus more humid conditions. More distinct layering in the upper part of the speleothem suggests strong seasonality from ~163 ka to ~154 ka. Short-term oxygen and carbon isotope excursions were found between ~155 and ~163 ka. The inferred Kanaan Cave humid intervals during the mid–MIS 6 follow variations of pollen records in the Mediterranean basins and correlate well with the synthetic Greenland record and East Asian summer monsoon interstadial periods, indicating short warm/wet periods similar to the Dansgaard-Oeschger events during MIS 4–3 in the eastern Mediterranean region.


2013 ◽  
Vol 13 (7) ◽  
pp. 1707-1722 ◽  
Author(s):  
M. Reale ◽  
P. Lionello

Abstract. The link between winter (December-January-February) precipitation events at 15 Mediterranean coastal locations and synoptic features (cyclones and Northern Hemisphere teleconnection patterns) is analyzed. A list of precipitation events has been produced; q percentile thresholds (Thq) and corresponding frequency Nq (for q equal to 25, 50, 90 and 98) have been considered. A negative trend has been detected in total precipitation and N50 at many locations, while no significant trend in N25, N90 and N98 has been found. The negative phase of the North Atlantic Oscillation (NAO) and the East Atlantic/West Russia pattern (EAWR) compete for exerting the largest influence on the frequency of the 25th, 50th and 90th percentiles, with EAWR and NAO exerting their largest influence in the central and western Mediterranean areas, respectively. All percentiles show a similar behavior except for the 98th percentile, which shows no convincing link to any teleconnection pattern. The cyclone tracks that are associated with precipitation events have been selected using the ERA-40 reanalysis data, and a strong link between intense precipitation and cyclones is shown for all stations. In general, the probability of detecting a cyclone within a distance of 20° from each station increases with the intensity of the precipitation event and decreases with the duration of a dry period. The origin and track of cyclones producing intense precipitation differ among different areas. When precipitation occurs in the northwestern Mediterranean, cyclones are generally either of Atlantic origin or secondary cyclones associated with the passage of major cyclones north of the Mediterranean Basin, while they are mostly generated inside the region itself for events at the eastern Mediterranean coast. An important fraction of intense events in the southern areas is produced by cyclones that are generated over northern Africa. The analysis of sea level pressure and geopotential height at 500 hPa highlights the important role of cyclone depth, circulation strength, surrounding synoptic condition, and of slow speed of the cyclone center for producing intense precipitation events.


2019 ◽  
Vol 20 (9) ◽  
Author(s):  
ABDEL FATTAH N. ABD RABOU

Abstract. Abd Rabou AFN. 2019. On the occurrence and health risks of the Silver-cheeked Toadfish (Lagocephalus sceleratus Gmelin, 1789) in the marine ecosystem of the Gaza Strip, Palestine. Biodiversitas 20: 2620-2627. The Silver-cheeked Toadfish (Lagocephalus sceleratus Gmelin, 1789) is one of the most recent invaders into the Mediterranean Sea. It represents a serious ecological risk to Mediterranean biodiversity and fisheries resources and a health risk to public health. The current study comes to handle the occurrence and health risks of the species in the Eastern Mediterranean of the Gaza Strip, Palestine. Frequent visits to local fish markets, meetings, and discussions with stakeholders, and chasing of local media reports were the main tools involved to satisfy the goals of the study, which extended from 2010 to 2019. The first record of the Silver-cheeked Toadfish in the Mediterranean coast of the Gaza Strip was in 2006 as claimed by fisheries parties. The by-catch of the species by fishing gear extended over the entire length of the Mediterranean coast of the Gaza Strip (42 km). The species was said to damage fishing nets, lines and hooks by its strong teeth. Prior to its banning in early 2010s, all pufferfishes including the species in question were sold freely in Gaza fish markets. Several cases of hospitalization have been reported in the Gaza Strip after consumption of the Silver-cheeked Toadfish. The symptoms of TTX intoxication included nausea and vomiting, dizziness, headache, abdominal pain, perioral paraesthesia, and tingling over the entire body. No death cases were reported locally. Many awareness campaigns have been conducted by fisheries parties to warn both fishermen and local people from the ecological and health risks associated with the Silver-cheeked Toadfish and TTX intoxication. Finally, the threats imposed by the Silver-cheeked Toadfish on the Eastern Mediterranean countries including Palestine indicate that potential solutions to the problem should be explored.


2016 ◽  
Vol 17 (2) ◽  
pp. 440 ◽  
Author(s):  
N. SOKOLOVER ◽  
P. D. TAYLOR ◽  
M. ILAN

The impact of global warming on the composition of marine biotas is increasing, underscoring the need for better baseline information on the species currently present in given areas. Little is known about the bryozoan fauna of Israel; the most recent publication concerning species from the Mediterranean coast was based on samples collected in the 1960s and 1970s. Since that time, not only have the species present in this region changed, but so too has our understanding of bryozoan taxonomy. Here we use samples collected during the last decade to identify 47 bryozoan species, of which 15 are first records for the Levantine basin. These include one new genus and species (Crenulatella levantinensis gen. et. sp. nov.), two new species (Licornia vieirai sp. nov. and Trematooecia mikeli sp. nov.), and two species that may be new but for which available material is inadequate for formal description (Reteporella sp. and Thalamoporella sp.). In addition, Conopeum ponticum is recorded for the first time from the Mediterranean Sea. Non-indigenous species make up almost one-quarter of the 47 species identified. All of the non-indigenous species are native to tropical and subtropical regions, implying a change of the Levant bryozoan biota from a temperate to a more tropical state, probably related to both higher temperature and salinity and to the opening of the Suez Canal connecting the Red Sea and the Eastern Mediterranean.  


2019 ◽  
Vol 88 (3) ◽  
pp. 285-300
Author(s):  
Khaled Mahmoud Abdelsalam

Abstract Sampling of fouling organisms carried out during January 2019 at Al-Max (west of the city of Alexandria) on the Mediterranean coast of Egypt revealed the presence of larval populations belonging to the genus Telmatogeton (Chironomidae), which is reported for the first time from the Mediterranean coast of Egypt. The larvae were found among clumps of fine filamentous green algae (Enteromorpha compressa). A description of the larva with taxonomic remarks and comments on its ecology and geographical distribution are given.


2020 ◽  
Vol 8 ◽  
Author(s):  
Sabrina Lo Brutto ◽  
Davide Iaciofano

A survey has been carried out at four Israeli rocky sites to evaluate the diversity of the amphipod fauna on various hard substrates, still scarcely monitored, as potential pabulum for amphipod crustacean species. A survey of shallow rocky reefs along the Mediterranean coast of Israel recovered 28 species and integrated the Amphipoda checklist for the country ofIsrael with 12 newly-recorded species. Such renewed national list includes Maera schieckei Karaman & Ruffo, 1971, a rare species endemic to the Mediterranean Sea, recorded here for the first time from the southern Levant Basin. The species, described from specimens collected in the Tyrrhenian Sea in 1970, has been only recorded eight times within the whole Mediterranean Sea. A revision of the bibliography on the distribution and ecology of M. schieckei showed that, although mentioned only for the western Mediterranean basin by some authors, it is listed in the checklist of amphipods of the Aegean Sea and neighbouring seas and has been found in the eastern Mediterranean basin since 1978. Maera schieckei was rarely found in the Mediterranean, one of the most studied marine biogeographic region as concerns the amphipod fauna; and the species seems to prefer bays or gulf areas. The role of updating and monitoring faunal composition should be re-evaluated.


X ◽  
2020 ◽  
Author(s):  
Julio Navarro Palazón ◽  
Luis José García-Pulido

FORTMED 2020 is the fifth edition of the International Conference on Fortifications of the Mediterranean Coast. The Conference has been held in March 26th, 27th and 28th 2020 in Granada (Spain), at the Laboratory of Archaeology and Architecture of the City (Laboratorio de Arqueología y Arquitectura de la Ciudad, LAAC) of the School of Arabic Studies (Escuela de Estudios Árabes, EEA), a research centre that belongs to the Spanish National Research Council (Consejo Superior de Investigaciones Científicas, CSIC). The main objective of FORTMED conferences is to exchange and share knowledge for a better understanding, assessment, management and exploitation of the built Cultural Heritage. The focus is on defensive architecture in the Mediterranean area, from the Antiquity to the present day, although it does not exclude other fortifications built overseas but high influenced by those on the Mediterranean.


Author(s):  
David Abulafia

While the Ragusans benefited from their special relationship with the Turks, the Genoese and Venetians were more cautious in building ties to the Ottoman court. The sultan was anxious not to turn them away, but they viewed the eastern Mediterranean as increasingly dangerous. Difficulties were compounded by occasional arguments between the Venetians and the Mamluk sultans of Egypt, who required ever larger amounts in taxes in order to prop up their regime. The Mamluks were also a regional threat. In 1424–6 they invaded Cyprus and carried away its king, Janus, along with 6,000 captives; a ransom of 200,000 ducats had to be paid before Janus was restored to the throne, and it is said that he never laughed again. In 1444 they besieged Rhodes. In 1460 they supported a claimant to the throne of Cyprus, sending eighty ships against the island, to the horror of Christendom, for no one could understand why James of Lusignan, a bastard, would wish to enlist Egyptian aid in a bid for a throne to which he was not entitled. As Ottoman and Mamluk pressure on these areas became intolerable, the Genoese and their rivals increasingly turned their attention towards the West, buying sugar in Sicily and Spain and grain in Sicily and Morocco. The mid-fifteenth century saw a veritable economic renaissance in Genoa, at first sight against all the odds: the city was still consumed by internal strife, but large segments of the population were able to benefit from trade and investment, and the city boomed. Especially attractive were shares in the new public bank, the Banco di San Giorgio, which eventually acquired dominion over Corsica. The loss of easy access by the Genoese to the alum mines of Phokaia in Asia Minor was compensated by the discovery in 1464 of alum mines on the doorstep of Rome itself, at Tolfa; Pope Pius II described the discovery as ‘our greatest victory against the Turk’. It reduced dependence on ‘the Turk’, and yet it did not reduce dependence on the Genoese, who switched their attention to central Italy, and built a new alum monopoly there.


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