Ancient harbour infrastructure in the Levant: tracking the birth and rise of new forms of anthropogenic pressure

Beirut, Sidon and Tyre were major centres of maritime trade from the Bronze Age onwards. This economic prosperity generated increased pressures on the local environment, through urbanization and harbour development. Until now, however, the impact of expanding seaport infrastructure has largely been neglected and there is a paucity of data concerning the environmental stresses caused by these new forms of anthropogenic impacts. Sediment archives from Beirut, Sidon and Tyre are key to understanding human impacts in harbour areas because: (i) they lie at the heart of ancient trade networks; (ii) they encompass the emergence of early maritime infrastructure; and (iii) they enable human alterations of coastal areas to be characterized over long timescales. Here we report multivariate analyses of litho- and biostratigraphic data to probe human stressors in the context of their evolving seaport technologies. The statistical outcomes show a notable break between natural and artificial sedimentation that began during the Iron Age. Three anchorage phases can be distinguished: (i) Bronze Age proto-harbours that correspond to natural anchorages, with minor human impacts; (ii) semi-artificial Iron Age harbours, with stratigraphic evidence for artificial reinforcement of the natural endowments; and (iii) heavy human impacts leading to completely artificial Roman and Byzantine harbours

The lagoonal harbour of Portus Pisanus (N Tyrrhen- ian Sea, Italy): a long history of human adaptation to changing coastline

During the last millennia human and natural processes have become increasingly intertwined, especially in the Mediterranean coastal and alluvial plains where major urban and trade centres developed since protohistoric times. The construction of ports represents one of the human activities that have mostly contributed to modify coastal environments, inducing a variety of hydrodynamic and hydrochemical changes especially since Roman times (Marriner et al., 2014). Exceptions in this common manner to plan harbours have been recognised along the N Tyrrhenian coast, where no high-impact defense works are explicitly documented by either historical sources or archaeological excavations for three main harbours developed during Etruscan-Roman times (IV-I century BC): Portus Lunae (Bini et al., 2012), Portus Pisanus and Vada Volterrana. Roman literary sources (i.e., Itinerarium Maritimum 501; Rutilio Namaziano) mentioned Portus Pisanus as a flourishing commercial site within a natural protected area (called Sinus Pisanus by Tacito) characterized by Posidonia meadows and located at the foot of Leghorn hills, ca. 18.5 km south of the Pisa city. Accordingly, recent excavations undertaken close to the hills slope, 3 km inland from modern coastline, unearthed a wooden palisade, stone piers and a warehouse dated to the Roman period (Pasquinucci, 2013; Morhange et al., 2015). However, the precise location of the lagoonal harbour basin is still controversial. This study aims to contribute to fill this knowledge gap and shed new light on the main stages of harbour history in the framework of the mid-late Holocene palaeogeographic evolution of the Pisa Plain. The application of a multidisciplinary approach (sedimentological and micropalaeontological core analyses, radiocarbon dating, geomorphological field survey, remote sensing and historical cartography) has revealed that a wide lagoonal basin formed in the study area during the marine transgression peak (ca. 8000 cal yr BP). This basin, recorded by a m-thick subsurface succession of soft grey clays with brackish meiofauna, persisted for several millennia and corresponds to Sinus Pisanus. The available stratigraphic data document that during Roman times the lagoon became progressively less connected to the sea and turned into a coastal lake/pond. Filling processes started two-three millennia later respect to the lagoon occupying the Pisa city area during the Holocene (Rossi et al., 2011). This seaward facies shift forced the westward transferring of the Middle Ages harbour. These results show that natural sheltered conditions along with the distance from coeval Arno River made more advantageous for humans following the shoreline changes, rather than making high-impact interventions. 2012, Bini M., Bruckner H., Chelli A., Da Prato S., Gervasini L., Palaeogeographies of the Magra Valley coastal plain to costrain the location of the Roman harbour of Luna (NW Italy), Palaeogeography, Palaeoclimatology, Palaeoecology, 337-338, 37–51. 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. 2015, Morhange C., Marriner N., Baralis A., Blot M.L., Bony G., Carayon N., Carmona P., Flaux C., Giaime M., Goiran J.-P., Kouka M., Lena A., Oueslati A., Pasquinucci M., Porotov A., Dynamiques géomorphologiques et typologie géoarcheologique des ports antiques en contextes lagunaires, Quaternaire, 26, (2), 117–139. 2013, Pasquinucci M., Guida all’archeologia delle coste livornesi. Nardini Editore. Provincia di Livorno. 271 pp. 2011, Rossi V., Amorosi A., Sarti G., Potenza M., Influence of inherited topography on the Holocene sedimentary evolution of coastal systems: An example from Arno coastal plain (Tuscany, Italy), Geomorphology, 135 (1-2), 117–128

Resonant Excitonic Optical Stark Effect In Gase

The time-resolved nonlinear transmission of bulk ε-GaSe has been studied in the femtosecond regime when resonantly exciting the material in the vicinity of the exciton at room temperature. Two regimes are evidenced. At early time delay, a blue shift of the exciton with no linewidth broadening can be related to optical Stark effect, while at longer time delay the usual exciton screening and band-gap renormalization due to real electronic transitions is observed. At resonance, a dependence of the Stark shift with the amplitude of the exciting field is obtained, as predicted by a simple "dressed- atom" model.55222307230

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

History and influence of the Danube delta lobes on the evolution of the ancient harbour of Orgame (Dobrogea, Romania)

On the coast of Northern Dobrogea, south of the Danube delta, the Greek settlement of Orgame was founded in the mid 7th c. BC, probably by Milesian colonists. The ancient city was located on the Cape Dolojman which today overlooks a large lagoon complex. We undertook a chronostratigraphic study to:(i) understand coastal changes around Cape Dolojman since ca. 5000 years BP in connection with the construction of the Danube delta lobes, and (ii) identify potential sediment impacts related to human occupation of the site. Three cores were extracted from the lagoon area. Sedimentological and biological analyses were undertaken to reconstruct the evolution of the coastal palaeoenvironments. The results show a closure of the marine bay around 3500 cal. BP and its transformation into a lagoon environment. The first major environmental change was due to the construction of the lobe St. George I and the formation of the barrier Lupilor. Around 2000 cal. BP, the formation of an intra-lagoonal lobe, the Dunavatz, led to the gradual transformation of the lagoon into a fluvial-dominated system. Paradoxically, lagoon waters today still wash the ancient Greek harbour environment, which has not been totally infilled by alluvial sediments. To understand this paradox, in a context of coastal progradation, we compared and contrasted the geomorphological data with the nearby city of Istros/Histria, which was already landlocked at this time. The location of these two Greek colonies relative to the coastal sediment cell and barriers partly explains their contrasting palaeoenvironmental evolution. Until 2650 cal. BP, the increase in charcoal and organic matter in sedimentary archives is interpreted as an anthropogenic signal for a more extensive use of the vegetation cover following the foundation of the city of Orgame (e.g. for domestic use and funeral rites)

Tsunamis in the geological record: Making waves with a cautionary tale from the Mediterranean

This is the final version of the article. Available from AAAS via the DOI in this record.From 2000 to 2015, tsunamis and storms killed more than 430,000 people worldwide and affected a further >530 million, with total damages exceeding US$970 billion. These alarming trends, underscored by the tragic events of the 2004 Indian Ocean catastrophe, have fueled increased worldwide demands for assessments of past, present, and future coastal risks. Nonetheless, despite its importance for hazard mitigation, discriminating between storm and tsunami deposits in the geological record is one of the most challenging and hotly contended topics in coastal geoscience. To probe this knowledge gap, we present a 4500-year reconstruction of "tsunami" variability from the Mediterranean based on stratigraphic but not historical archives and assess it in relation to climate records and reconstructions of storminess. We elucidate evidence for previously unrecognized "tsunami megacycles" with three peaks centered on the Little Ice Age, 1600, and 3100 cal. yr B.P. (calibrated years before present). These ~1500-year cycles, strongly correlated with climate deterioration in the Mediterranean/North Atlantic, challenge up to 90% of the original tsunami attributions and suggest, by contrast, that most events are better ascribed to periods of heightened storminess. This timely and provocative finding is crucial in providing appropriately tailored assessments of coastal hazard risk in the Mediterranean and beyond.Financial support for this work was provided by Labex OT-Med (ANR-11-LABX-0061). Additional assistance was provided by the Institut Universitaire de France (CLIMSORIENT project), ANR Geomar (ANR-12-SENV- 0008-01), A*MIDEX (ANR-11-IDEX-0001-02), and Partenariat Hubert Curien PROCOPE (33361WG). J.G. benefited from a research fellowship at Chrono-environnement funded by the Région Bourgogne-Franche-Comté

Chapitre 3. Étude géomorphologique des rivages d’Apollonia

Dans le cadre des fouilles archéologiques de la nécropole classique et hellénistique d’Apollonia, au lieu-dit Kalfata, nous avons eu l’opportunité de travailler sur la mobilité des paysages littoraux depuis environ 6000 ans. Nous avions plusieurs objectifs géomorphologiques à l’échelle de la région de Sozopol : Préciser la mobilité du niveau relatif de la mer ; Mesurer les variations des lignes de rivage par rapport aux sites d’occupation humaine ; Estimer les potentialités et la vulnérabilit..