Using archaeological data for the understanding of Late-Holocene Sea of Galilee's level fluctuations

Unidad de excelencia María de Maeztu CEX2019-000940-MIn the Jordan Valley, reconstructed changes of the Sea of Galilee level have shown sharp fluctuations of the water elevation during the Holocene. In this paper, we provide new data originating from the excavations of Kursi Beach archaeological site located on the eastern shore of the Sea of Galilee and compare them with other data gathered from the archaeological site of Magdala, located on its western shore. Our data yield to constrain Sea of Galilee level changes between the Iron Age II (10th-9th centuries BCE) and the Crusader period (11th-12th centuries CE), a period of high interest for the archaeological community. We demonstrate that water level was around -212 to -210 m mean sea level (msl) for the Iron Age II period. Lake level rose to -208/-209 m msl during the Late Hellenistic/Early Roman period. Water level remained low (<-213/-214 m msl) from the Byzantine to the Crusader period (from 5th to 12th centuries CE). Our data provide new knowledge for the understanding of variations in the Sea of Galilee level in antiquity. We highlight that water level fluctuations must have been key factors taken into account in the habitation pattern

Geoarchaeology of Magdala harbour and Tel Akko (Israel)

With the support of the MISTRALS-ENVIMED-GEOSISRAEL program and A*MIDEX GEOMED project, we have been able to reconstruct the palaeo-environmental evolution of two ancient harbours in Israel. Harbour geoarchaeology was mainly developed in Israel by the late Avner Raban, founding member of the RIMS multidisciplinary research unit in 1972 at Haifa University. Since these pionneering years, a series of geoarchaeological projects have focused on different ancient harbours, mainly at Caesarea, Dor, and Atlit. Paradoxically, landscape evolution of the major harbour sites of Magdala and Tel Akko have been neglected until two comprehensive multidisciplinary archaeological projects were recently started. Recent excavations undertaken in the ancient city of Magdala, located on the western shore of the Sea of Galilee, have unearthed a harbour structure extending for more than 100 m, dating from the late Hellenistic (167-63 BC) to the middle Roman (70-270 AD) periods, with well-preserved quays and mooring stones. An integrated (geomorphological, sedimentological, micropalaeontological and archaeological) study of the sedimentary succession buried beneath the ancient harbour area reveals the harbour’s main evolutionary stages, shedding new light on the natural versus anthropogenic controls on sedimentation. Three sedimentary sequences reflect the recent palaeoenvironmental evolution of Magdala. These include: 1) a pre-harbour foundation sequence; 2) a harbour sequence from the 3rd-2nd centuries BC to the first half of the 1st century AD. The substantial increase of ostracod species (Pseudocandona albicans) preferring calm waters and fine-grained facies point to the establishment of a protected, shallow and organic-rich setting. The increase in sodium and potassium concentrations is accompanied by the sudden appearance of Heterocypris salina, a brackish-tolerant species, and by the dominance of noded valves of Cyprideis torosa ; and 3) a harbour abandonment sequence dated ca. 270-350 years AD. Archaeological excavations at Tel Akko, east of the present city, revealed imported artifacts and evidence for maritime trade from the Middle Bronze Age (2200–1500 years BC) onwards. The findings strongly indicated that a harbour had been developed on this site even though its exact location and associated facilities were still to be determined. Sedimentological and paleontological analyses together with 14C dating of cores provide new palaeo-environmental information allowing for the reconstruction of shoreline changes over the last 4000 years. Firstly, we propose that the southern face of the tell constituted the harbor environment,with lagoonal-marine characteristics until ca. 2800 years BP; and that the site was protected by a natural rocky breakwater and a spit which were eventually silted up and transformed into a continental marsh. This environment might have been used as a harbour by inhabitants before the archaic period. Secondly, it seems that the west side of the tell was lined by a sandy coast that had prograded offering an open anchorage until the Persian period. These results must be cross-validated by future archaeological excavations aimed at more accurately locating the ancient harbour structures. 2013, Kaniewski D., Van Campo E., Morhange C., Guiot J., Zviely D., Shaked I., Otto T., Artzy M., Early urban impact on Mediterranean coastal environments, Nature Scientific Reports, 3. 2013, Sarti G., Rossi V., Amorosi A., De Luca S., Lena A., Morhange C., Ribolini A., Sammartino I., Bertoni D., Zanchetta G., Magdala harbour sedimentation (sea of Galilee, Israel), from natural to anthropogenic control, Quaternary International, 303, pp. 120-131. 2014, Anthony E. J., Marriner N., Morhange C., Human influence and the changing geomorphology of Mediterranean deltas and coasts over the last 6000 years: from progradation to destruction phase? Earth Science Reviews, 139, pp. 336–361. 2014, Kaniewski D., Van Campo E., Morhange C., Guiot J., Zviely D., Le Burel S., Otto T., Artzy M., Vulnerability of ecosystems facing long-term changes along the Mediterranean coast of Israel, PLoS ONE, 9, 7. 2014, Marriner N., Morhange C., Kaniewski D., Carayon N., Ancient harbour infrastructure in the Levant: tracking the birth and rise of new forms of anthropogenic pressure, Nature Scientific Reports, 4, 5554. 2014, Morhange C., Salamon A., Bony G., Flaux C., Galili E., Goiran J.-P., Zviely D., Geoarchaeology of tsunamis and the revival of neo-catastrophism in the Eastern Mediterranean, in Rome "La Sapienza" Studies on the Archaeology of Palestine & Transjordan (ROSAPAT 11), Overcoming catastrophes, pp. 31-51. 2015, Morhange C., Marriner N., Carayon N., The geoarchaeology of ancient Mediterranean harbours, in French geoarchaeology in the 21st century, G. Arnaud-Fassetta and N. Carcaud eds., CNRS editions, Alpha, Paris, pp. 281-289. 2015, Rossi V., Sammartino I., Amorosi A., Sarti G., De Luca S., Lena A., Morhange C., New insights into the palaeoenvironmental evolution of Magdala ancient harbour (Sea of Galilee, Israel) from ostracod assemblages, geochemistry and sedimentology, Journal of Archaeological Science, 54, pp. 356-373

Fast quantitative analysis of n-alkanes, PAHs and alkenones in sediments

Altres ajuts: acord transformatiu CRUE-CSICUnidad de excelencia María de Maeztu CEX2019-000940-MThe study of different organic biomarker classes is essential to elucidate global Earth dynamics since different biogeochemical processes play a role in regulating environmental and climatic conditions. However, multiproxy analysis generally consists of labor-intensive and time-consuming methodologies, which hamper the study of a large number of samples. Here, we develop and validate a fast analytical method to quantify different classes of organic biomarkers (PAHs, n-alkanes and alkenones) in sediments. This new method sequentally extracts and fractionates the target compounds using a pressure liquid extraction (PLE) system, which allows us to selectively obtain the analytes by reducing the time of analysis, sample handling and solvent usage. We show that our method provides reproducible results and high recoveries (>70%), and can be applied to a wide range of sedimentary environments, such as oceanic basins, continental slope and shelf, and lakes. Moreover, the method provides reproducible estimates of paleoclimatic indices, such as the carbon preference index (CPI), the average chain length (ACL) and the U37K'-derived sea-surface temperature (SST). Therefore, this new method enables fast quantitative multiproxy analysis of oceanic, coastal and lake sediments

Refining Late-Holocene environmental changes of the Akko coastal plain and its impacts on the settlement and anchorage patterns of Tel Akko (Israel)

Acord transformatiu CRUE-CSICAltres ajuts: United States-Israel Binational Science Foundation (Project number: 2016080)Akko/Acre, a UNESCO World Heritage site since 2001, is one of the oldest continuously inhabited sites in the eastern Mediterranean. Tel Akko was a major maritime centre of the southern Levant from the Middle Bronze to the Late Persian period. The city was then moved 1500 m to the west on the Akko promontory where the 'Old City' of Saint-Jean d'Acre is located. The natural and anthropogenic evolution of Tel Akko area is reflected by persistent geographical and habitation pattern changes. We combine sedimentological and faunal analyses of radiocarbon dated cores as well as identification of ceramic sherds found in the cores with ground penetrating radar investigations to propose an up-to-date palaeogeographical reconstruction of landscape/environmental changes of the Akko coastal plain in order to understand the extent to which environmental pressures have played a role on the position of anchorage and habitation patterns. We highlight how the local population make use of the natural advantages of the area and adapted to environmental pressures. Following a constant sedimentary input and simultaneous coastal progradation of the Akko coastal plain the main anchorage areas where forced to move. While the 2nd Millennium BCE anchorage was on the southern area of the tell, the late-1st Millennium BCE (Phoenician-Persian) anchorage was relocated on the western area. Vicissitudes in settlement pattern noted in archaeological excavations and surveys on Tel Akko have, most likely, been the consequence of the changes in the position of the coastline

The late Holocene record of Lake Mareotis, Nile Delta, Egypt

Lake Maryut (northwestern Nile Delta, Egypt) was a key feature of Alexandria's hinterland and economy during Greco-Roman times. Its shores accommodated major economic centers, and the lake acted as a gateway between the Nile valley and the Mediterranean. It is suggested that lake-level changes, connections with the Nile and the sea, and possible high-energy events considerably shaped the human occupation history of the Maryut. To reconstruct Lake Maryut hydrology in historical times, we used faunal remains, geochemistry (Sr isotopic signature of ostracods) and geoarcheological indicators of relative lake-level changes. The data show both a rise in Nile inputs to the basin during the first millennia BCE and CE and a lake-level rise of ca. 1.5 m during the Roman period. A high-energy deposit, inferred from reworked radiocarbon dates, may explain an enigmatic sedimentary hiatus previously attested to in Maryut's chronostratigraphy

Using a multi-proxy approach to locate the elusive Phoenician/Persian anchorage of Tel Akko (Israel)

Unidad de excelencia María de Maeztu CEX2019-000940-MAltres ajuts: acords transformatius de la UABPrevious geoarchaeological research on the Akko coastal plain have contributed to the understanding of the ancient coastal interface and added evidence as to the location/shift of the ancient anchorages dating from the Middle Bronze Age (beginning of the 2nd Millennium BC) to the Early Hellenistic period (mid of the 2nd century BC) of the ancient site of Tel Akko. The present research provides new insights into the environmental changes and likely anchorage sites along the western edge of Tel Akko in the 1st Millennium BC (Iron Age II and III, periods associated with the Phoenician mariners and Persian army incursion). Our approach for locating the anchorage is based on a detailed investigation of subsurface sediments combining sedimentological and faunal analysis and radiocarbon dating of cores as well as identification of ceramic sherds found in the cores, and ground penetrating radar (GPR) and electrical resistivity tomography (ERT) surveys. Paleoenvironmental changes are compared and contrasted with the results of the archaeological investigations on the tell and in its vicinity. Our new data demonstrates that the Phoenician/Persian maritime interface of Tel Akko was mainly oriented toward the southwestern area of the tell where a natural anchorage was likely to have been located. At that time, the water depth in this area was ca. 2m, allowing for the anchorage of seagoing vessels. Increasing sediment deposition lead to the deterioration of direct, and eventual loss of access, to the sea. These conditions initiated the abandonment of the tell in the Early Hellenistic period as well as the westward shift to habitation on the peninsula, now the 'Old city of Akko', the Crusaders' Saint Jean d'Acre

Géoarchéologie des ports antiques en contextes deltaïques : Quelques exemples de Méditerranée et de mer Noire

Références de la thèseGiaime M. (2016). Géoarchéologie des ports antiques en contextes deltaïques : quelques exemples de Méditerranée et de mer Noire. Thèse de doctorat en géographie, Aix-Marseille Université. Évolution du trait de côte et localisation des zones d’ancrage de Tel Akko (Israël) au cours du temps Topographie adaptée à partir de la carte de Treidel (1925-1926) M. Giaime, 2016 Au cours de mon travail de doctorat, j’ai utilisé la démarche classique employée en géoarchéologie portu..

Geoarchaeology of ancient deltaic harbours : lessons from the Mediterranean and the Black Seas

Les deltas ont débuté leur édification il y a environ 7000 ans suite à la stabilisation du niveau de la mer. Ils offraient durant l’Antiquité une mosaïque d’environnements, plus ou moins protégés, favorables aux activités maritimes. Nous montrons que plusieurs types de ports deltaïques peuvent être identifiés en raison des différents contextes géomorphologiques offerts par les deltas. La mise en relation des résultats bio-sédimentologiques, avec les données archéologiques nous ont permis de détailler l’évolution des environnements portuaires de plusieurs sites antiques situés dans des deltas. La première étude a été menée à l’échelle du delta de la Kouban (Péninsule de Taman, Russie). Un carottage réalisé à l’extrémité orientale de la péninsule et sa comparaison avec d’autres études géoarchéologiques menées récemment dans le delta nous a permis de restituer l’évolution paléogéographique de la péninsule. Nous avons pu confirmer que cette dernière a constituée, suite à la remontée postglaciaire du niveau marin, un large archipel articulé autour de quatre îles. À Tel Akko (Baie de Haifa, Israël), notre étude nous a permis de restituer l’évolution côtière du site depuis l’Âge du Bronze. À Pollentia, cité romaine des Baléares, nous avons été en mesure de démontrer que le port était situé dans une lagune de faible profondeur située en marge distale d’un petit delta côtier. Enfin à Halmyris (Danube, Roumanie) nous avons été en mesure de démontrer que la forteresse romaine, installée sur un promontoire, était protégée des crues tout en bénéficiant d’un accès facilité au fleuve par l’intermédiaire d’un chenal secondaire au sein duquel son port aurait pu être installé.River deltas began forming around 7000 years BP because of the stabilisation of the mean sea-level. The natural variety of wetland environments on clastic coasts, in particular deltas, explains in major part the important disparities in harbour contexts. The combination of earth sciences with archaeological tools allows us to investigate the environmental evolution of four ancient sites located on deltas. We investigate 7000 years of environmental changes on the Kuban delta (Taman Peninsula, Russia). A coring, from the eastern limit of the peninsula, and its comparison with other geoarchaeological studies undertaken on the delta, allow us to confirm that the Holocene marine transgression created an archipelago of four islands around 6000 years ago in the area of the present-day Taman Peninsula. In Antiquity, natural factors such as delta progradation and the evolution of spits and sand bars have considerably affected the landscape evolution and therefore human occupation of the peninsula. At Tel Akko, (Haifa Bay, Israel), we reconstruct the evolution of the coastal zone of the site since the Bronze Age. We propose different harbour locations over time. At Pollentia, a Roman city of Mallorca, we have been able to demonstrate that the harbour was situated in a shallow lagoon, probably dredged at the time of its foundation. At Halymris (Danube delta, Romania), our research supports the presence of a secondary fluvial-channel located close to the fortress where the harbour may have been installed. The fortress, located at the foot of a promontory, was protected from floods and provided easy access to the main channel of the river