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International audience; The Sasanian period (224–651 CE) marked an era of large-scale urban projects in southwest Asia, including Iran's semi-arid highlands, with particular efforts to manipulate water bodies. This study presents a recent interdisciplinary investigation of a spring-fed pond at the entrance of the Palace of Ardashir (Firuzabad plain, southwest Iran), part of a recently registered World Heritage site. Historical accounts suggest that the entire water system of the plain, including the pond, underwent a hydraulic re-organization at the beginning of the Sasanian period, a fact that has never been investigated geoarchaeologically. A series of sediment cores were retrieved from the pond to probe its evolution and examine the extent of its landscape modification. The cores were sedimentologically described and radiocarbon-dated with age–depth models established based on 57 AMS (accelerator mass spectrometry) 14C dates to understand the basin's depositional history. The results indicate that (i) Ardashir Pond has existed as part of a larger wetland complex since at least 4500 years ago, (ii) it was substantially enlarged at the beginning of the Sasanian era, and (iii) it was abandoned at the end of the Sasanian period. The Ardashir Pond is one of the first geoarchaeologically investigated case studies to demonstrate the Sasanian landscape in the framework of the “Iranshahr” sociopolitical concept.

International audience; Successful heritage management requires a robust comprehension of the threats facing archaeological sites, at both current and future timescales. Siraf, on the Persian Gulf of Iran, is a site of national and international importance whose history stretches back to the Sassanid period (224-652 AD). In the present context of global change (drought and relative sea-level rise) and anthropogenic impacts (coastal artificialization and reduced sediment supply), the city's waterfront archaeology is undergoing significant erosion. Nonetheless, at present, the processes leading to the loss of Siraf's in situ archaeological remains are still poorly understood, including the rates, timing and drivers of coastal erosion. Here we use Landsat images to monitor shoreline changes along the Siraf coastline between 1973 and 2016. We spatially quantify the causes and impacts of surface changes along 244 transects. The results demonstrate that coastal erosion is responsible for widespread and archaeologically significant damage, with 48% of the studied transects showing erosion during the period 1973-2016. We elucidate significant temporal variations in the data and, most notably, demonstrate that continued drought since the early 2000s has impacted upon sediment supply to coastal areas, severely accentuating erosion. For instance, between 2003 and 2016, 70% of transects recorded shoreline retreat with worrying implications for the waterfront archaeology of Siraf. These quantitative results provide invaluable spatial information regarding the causes and impacts of erosion upon Siraf's waterfront heritage, in addition to furnishing a template for the protection of the city's internationally important cultural heritage.

The scarcity of high-resolution palaeoclimate records from the interior of West Asia has limited our understanding of the mechanisms of past climate change and their potential impacts on early human societies of the Eastern Fertile Crescent. Here, we present a multiproxy sedimentological, geochemical and palynological record from the Hashilan Wetland in the central Zagros Mountains, spanning the time interval from 22 to 2.2 kcal bp. Our results indicate a cold, dry climate for the last deglaciation (22 to 10 kcal bp) with amplified aridity during the Last Glacial Maximum, Heinrich Stadial 1, the Younger Dryas and the 8.2 and 3.2 ka events. The Early Holocene (11.6 to 7.8 kcal bp) is characterised by prolonged dry summers, frequent spring/summer dust storms and restricted oak woodlands that gradually expanded as summers shortened toward the second half of the Holocene (

International audience; Dinoflagellate cyst assemblages were analysed in four short sediment cores collected in the south Basin of the Caspian Sea for assessing environmental changes over the last few millennia. Two of these cores were dated by radionuclides. The sedimentation rate of one of them was very high, in the order of 20 mm per year. The interpretation of the four sequences is supported by a collection of 27 lagoonal or marine surface sediment samples. A sharp increase in the concentration of the dinocyst occurs after 1967, especially owing to Lingulodinium machaerophorum. Considering nine other cores covering parts or the whole of Holocene, it became clear that this species started to develop in the Caspian Sea only during the last three millennia. By analysing instrumental data and collating existing reconstructions of sea level changes over the last decades, we show that the main forcing for the recent increase of L. machaerophorum percentages and concentration is global climate change, especially sea surface temperature increase. Sea level fluctuations likely only have a minor impact. We argue that the recent increase in L. machaerophorum indicates that the Caspian Sea clearly is in the Anthropocene.

International audience; During the last two decades, the number of tropical cyclone (TC) events in the Arabian Sea has increased dramatically, causing severe human and economic damage in Oman, Iran and Pakistan. Within this context, Gonu, Phet and Shaheen were the Arabian Sea's most destructive TCs on record, leading to a total of 6.07 billion USD in damages and 159 fatalities. Previous studies have mainly focused on atmospheric, sea surface temperature (SST) and anthropogenic impacts of TC generation and intensification. By contrast, oceanographic currents, Persian Gulf water outflow and the role of ocean-atmospheric interactions on the distribution of outflow water into the Arabian Sea, and their impacts on the TC intensification, are poorly understood. In order to address this issue, we use historical TC records, satellite data, atmospheric and oceanographic models to shed new light on the relationship between Persian Gulf water outflow and ocean currents on TC intensification in the Arabian Sea. The results demonstrate that water outflow depths are controlled by wind stress and upwelling intensity. Increased upwelling events due to the poleward movement of the monsoon belt have led to an increase in upper ocean salinity and heat content. Rapid TC intensification has increased noticeably since 2007 and more than 72% of cyclones have reached category 3 or more. We find that TC intensity is controlled by warm and saline (> 36.6 PSU) water distribution patterns, mediated by eddy and jet currents. Rapid intensification of pre-monsoon TCs occurred by tracking to the north and northwest, with most landfalls occurring during this period. Post-monsoon TCs generally affect the center and the southwest of the Arabian Sea. The TC risk manifests an increasing trend since 2007, therefore education programs via international platforms such as the International Ocean Institute (IOI) and UNESCO are required for the countries most at risk.

International audience; The olive tree (Olea europaea L.) is one of the species best adapted to a Mediterranean-type climate. Nonetheless, the Mediterranean Basin is deemed to be a climate change ‘hotspot’ by the Intergovernmental Panel on Climate Change because future model projections suggest considerable warming and drying. Within this context, new environmental challenges will arise in the coming decades, which will both weaken and threaten olive-growing areas, leading to a loss of productivity and changes in fruit and oil quality. Olive growing, a core of the Mediterranean economy, might soon be under stress. To probe the link between climate and olive trees, we here report 5,400 years of olive tree dynamics from the ancient city of Tyre, Lebanon. We show that optimal fruiting scales closely with temperature. Present-day and palaeo data define an optimal annual average temperature of 16.9 ± 0.3 °C for olive flowering that has existed at least since the Neolithic period. According to our projections, during the second half of the twenty-first century, temperature increases in Lebanon will have detrimental consequences on olive tree growth and olive oil production, especially in the country’s southern regions, which will become too hot for optimal flowering and fruiting. These data provide a template to understand present and future thresholds of olive production under climate change.

International audience; A revision of the data used to build the Caspian Sea level curve over the last 2200 years BP has been made based on a combination of geological and archaeo-historical data, using only those for which sufficient metadata were available. This compilation is completed by new sedimentological and palynological data from the south-east corner of the Caspian Sea, especially close to the known termini of the Sasanian Gorgan and Tammisheh Walls. A new calibration of the radiocarbon dates was used, i.e. with a freshwater offset reservoir of 351 ± 33 years. A literature survey of the Derbent lowstand indicated that this term has different definitions, depending on authors; it is thus to be used with caution. Here we therefore prefer to distinguish the mid-Sasanian lowstand and the later Medieval moderate lowstand. The “2600 years BP highstand” has not been found, mostly due to the calibration or recalibration of the datapoints used; data are indeed lacking at that time. Instead, a younger Parthian highstand (around 50 BC–50 AD) is clearly defined. The maximal amplitude and speed of change of the Caspian Sea level were respectively of >15 m and 14 cm per year. Compared to last century, the latter rate is 25% higher, but the amplitude is more than five times larger. The climatic causes of the Caspian Sea level changes are discussed. It is far from a simple case of temperature forcing; temperature forcing may result in several effects, that may impact the Caspian Sea level variations in opposite ways. Moreover, human intervention on river diversion and natural hazards were likely, for several time periods.

International audience; The western Makran subduction zone is capable of producing considerable tsunami run-up heights that penetrate up to 5 km inland. In this study, we show how climate change has affected urbanization along the tsunami-prone Makran coastline during the past 35 years. To address this issue, we have employed climate data, satellite altimeter radar, geomorphology and historical shoreline changes in order to shed light on the factors leading to a decline in access to freshwater resources and also rapid urbanization. We furthermore consider the interactions between environmental changes and human-induced coastal and catchment modifications in increasing socioeconomic vulnerabilities of littoral areas. The results of this study show that agricultural and freshwater management methods along the Chabahar coastal plain date back to at least 1808 CE, when wetter climate conditions characterized the area. Severe climate changes have been pronounced since 2000. Within this context, the majority of agricultural lands have been abandoned due to increasing drought intensity and duration. Decreasing cultivation and limited access to freshwater resources have led to extensive urbanization particularly for the two cities of Konarak and Chabahar. Enhanced soil erosion, increasing summer monsoon wind speed, sea-level rise and the growing number of strong storm events are some of the climate change-related hazards for high to very high socially vulnerable zones. In addition to environmental risks, poor urban planning has increased damage to coastal infrastructures such as ports and desalination plants. Furthermore, industrial and urban growth in the northwest of the Makran could further enhance socioeconomic damage by earthquakes and tsunamis.

International audience; The fluvial harbour of Aquileia (Italy), one of the most important Roman trading centres in the Mediterranean, was abandoned after the city's destruction in 452 AD. The deserted harbour evolved into a swamp surrounded by a floodplain that has recorded the anthropogenic, environmental and climatic pressures that have occurred during the last 1500 years in the northern Adriatic. Focusing on the period since 500 AD, we here reconstruct the area's long-term ecosystem dynamics. We show that ecosystem dynamics mainly mirror the climate phases of the pre-industrial era. After the Roman era, anthropogenic activities (agriculture, pasture and fire activity) declined in scope and amplitude and are chronologically limited (from the late 7th to the early 13th centuries AD), acting as a background pressure on ecosystems. The main non-human impacts recorded by ecosystems correspond to the Late Antique Little Ice Age, defined by an average temperature anomaly of −2.04 ± 0.17 °C, exceeding the Pre-industrial Little Ice Age by −1.26 ± 0.16 °C in severity. The temperatures reconstructed for the Medieval Climate Anomaly are close to those recorded for the 20th century AD (average anomaly of 0.08 ± 0.15 °C) but they differ from the 21st century AD, according to the CRUTEM4 data. Aquileia shows that ancient harbours are key areas to understand how climate and human societies have shaped northern Adriatic environments since the post-Roman period.

The Achaemenids and Sasanian ‘Persian’ Empires were significant political, economic, and social forces in the Late Bronze Age and Late Antiquity Eurasia, respectively, which have left marks on the heritage of the Mediterranean and Middle Eastern world. While attention is often focused on military and political conditions when discussing the prosperity and decline of these imperial powers, their realms, which crossed a variety of environmental settings, were highly dependent on the predictability of rainfall that drove agriculture and effective provisioning. Here, we present a multi-proxy sedimentological, geochemical, and palynological record from a 2.5-m long peat deposit near the excavation site in Konar Sandal near Jiroft in southeastern Iran, covering 4000-850 cal yr BP. Around 3950 cal yr BP a wet period prevailed based on elemental ratios, stable C isotope, pollen, and diagnostic lipids. Between 3900 and 3300 cal yr BP, wet/semi-wet conditions developed with the appearance of Cerealia-type pollen. Dry and windy conditions followed (ca. 3300-2900 cal yr BP), which coincided with the Siberian anticyclones and climatic shifts developing in the Eastern Mediterranean region. Consequently, the Bronze Age settlements around Jiroft, dependent on agriculture, underwent a steady decline. A prolonged wet period followed (ca. 2900-2300 cal yr BP) with the abundance of Sparganium-type pollen and the aquatic lipid proxy (Paq). This change coincided with intensive agricultural practices and the flourishing of the powerful Median and Achaemenid empires. The shift to high Ti/Al ratios coeval with the lowest δ13COM values suggests an increase in aeolian activity and dry conditions ca. 2100-1650 cal yr BP. The Jiroft valley again experienced wet conditions between 1550 and 1300 cal yr BP, which overlapped with the economic prosperity of the middle to late Sasanian empire. The paleoenvironmental reconstruction indicates that wet periods and intensive agriculture coincide with the Persian empires' zenith, political influence, and economic affluence. Therefore, contextualized and detailed paleoenvironmental records are desirable to explore the interplay of political and climatic factors in the development and fragmentation of the ancient settlements and imperial powers in Eurasian history. 1. Introduction 2. Geographical setting 3. Materials and methods 3.1. Sampling, magnetic susceptibility, and grain size analysis 3.2. Radiocarbon analyses 3.3. Elemental and mineralogical analyses 3.4. C/N and stable isotope analyses 3.4.1. Lipid extraction 3.5. Pollen analysis 4. Results 4.1. Age-depth model and chronology 4.2. Units 4.2.1. Unit 1 (U 1; 250-189 cm; ca. 4000-3550 cal yr BP) 4.2.2. Unit 2 (U 2; 189-164 cm; ca. 3550-3300 cal yr BP) 4.2.3. Unit 3 (U 3; 164-134 cm; ca. 3300-2900 cal yr BP) 4.2.4. Unit 4 (U 4; 134-106 cm; ca. 2900-2300 cal yr BP) 4.2.5. Unit 5 (U 5; 106-61 cm; ca. 2300-1550 cal yr BP) 4.2.6. Unit 6 (U 6; 61-10 cm; ca. 1550-850 cal yr BP) 5. Discussion 5.1. Paleoclimate preceding the decline of the Jiroft civilization 5.2. The Late Bronze Age decline in Jiroft 5.3. Rise and fall of the Persian Empire 5.3.1. The pre-Islamic period and recent times 6. Conclusions

International audience; Palaeoecology is increasingly contributing to conservation biology and restoration ecology by extending the recent annual to decennial records of ecological observations to centennial and millennial time scales. One of the almost neglected potential applications of palaeoecological investigations in conservation biology is the discovering of hidden species in subrecent fossil records. Such discoveries can be common in biodiversity hotspots in which the fauna and flora are not still fully known. In this study, we present the case of the liverwort Riella in continental southwest Asia (Iranian plateau), a very vulnerable taxon growing and reproducing under very special ecological circumstances. Our study adds two new species of Riella (R. echinata and R. helicophylla) in addition to the formerly reported R. cossoniana, to the subfossil bryophyte flora of Iran. We demonstrate the important contribution that the genus has played in the history of wetland flora of the semi-arid to arid areas of Iran during the late Quaternary. We further demonstrate the possibility that it is still thriving in many wetland systems and may need to be discovered and then protected in its potential habitats. We suggest that in the biodiversity hotspots of lower latitudes, more attention has to be paid to taxonomic identification of species to reveal the hidden part of the biodiversity for defining better conservation strategies for vulnerable aquatic ecosystems such as the seasonal wetland systems.

International audience

International audience; The impacts of relative sea‐level (RSL) variations and crust mobility on the development of ancient harbours in the northern Persian Gulf are poorly understood. Many unanswered questions remain with regard to the main reasons for a shift in the location of the most important ancient harbours in the northern part of the Persian Gulf coastal since 50 BC. Furthermore, some important early Islamic harbours, such as Siraf, have ancient city quarters that are today below the present sea level. The aim of this study is to evaluate the relationship between halokinesis and RSL changes using geophysical models and multidisciplinary geoarchaeological methods at the ancient Sassanid–Islamic site of Bataneh (presently known as Najirum) located at the foothill of an active Darang salt diapir. The results reveal that after the mid‐Holocene highstand, RSL regression was not continuous. The studied facies have recorded three RSL oscillations. The oscillations are correlated with the eustatic sea‐level position. During the first lowstand, important Sassanid harbours shifted from Rishar to Apologus. The second lowstand is consistent with the transition of maritime trade from Apologus to Siraf, during the Abbasid dynasty. Uplift of the Bataneh coastal zone exposed the city to risks from flooding and fluvial debris flows. With a modification of the local watershed, runoff water originating from the salt anticlinal was controlled and used for the extraction of gypsum in evaporation ponds. The economic expansion of Siraf led to Bataneh being abandoned with a shift in trade to Kish Island

This paper presents results of a multidisciplinary research initiative examining human responses to environmental change at the intersection of the southern coastal plain of the Caspian Sea and the foothills of the Alborz Mountains during the terminal Pleistocene and early Holocene. Our palaeo-environmental analysis of two sedimentary cores obtained from a lagoon in close proximity to four caves, occupied by human groups during the transition from hunting and gathering to food-producing ways of life in this region, confirms Charles McBurney's 1968 hypothesis that when Caspian Sea levels were high, Mesolithic hunters were reliant on seal and deer, but as water levels receded and a wide coastal plain emerged, hunters consumed a different range of herbivorous mammalian species. Palynological evidence obtained from these two cores also demonstrates that the cool and dry climatic conditions often associated with the Younger Dryas stadial do not appear to have been extreme in this region. Thus, increasingly sedentary hunting and gathering groups could have drawn on plant and animal resources from multiple ecological niches without suffering significant resource stress or reduced population levels that may have been encountered in neighbouring regions. Our analyses of botanical, faunal and archaeological remains from a recently-discovered open-air Mesolithic and aceramic Neolithic site also shows an early process of Neolithization in the southern Caspian basin, which was a very gradual, low-cost adaptation to new ways of life, with neither the abandonment of hunting and gathering, nor a climatic trigger event for the emergence of a low-level, food-producing society.

International audience; The late glacial-early Holocene transition is a key period in the earth's history. However, although this transition is well studied in Europe, it is not well constrained in the Middle East and palaeohydrological records with robust chronologies remain scarce from this region. Here we present an interesting hydrobiological record showing a major environmental change occurring in the Dasht-e Arjan Wetland (southwestern Iran, near to Persepolis) during the late glacial-early Holocene transition (ca. 11 650 years cal BP). We use subfossil chironomids (Insecta: Diptera) as a proxy for hydrological changes and to reconstruct lake-level fluctuations. The Arjan wetland was a deep lake during the Younger Dryas marked by a dominance of Chironomus plumosus/anthracinus-type, taxa adapted to anoxic conditions of deep waters. At the beginning of the Holocene, a drastic decrease (more than 80% to less than 10%) of Chironomus plumosus/anthracinus-type, combined with diversification of littoral taxa such as Polypedilum nubeculosum-type, Dicrotendipes nervosus-type, and Glyptotendipes pallens-type, suggests a lake-level decrease and a more vegetalized aquatic environment. We compare and contrast the chironomid record of Arjan with a similar record from northwestern Iran. The palaeoclimatic significance of the record, at a local and regional scale, is subsequently discussed. The increase in Northern Hemisphere temperatures, inferred by geochemical data from NGRIP, at the beginning of the Holocene best explains the change from the Younger Dryas highstand to early Holocene lowstand conditions in the Dasht-e Arjan wetland. However, a contribution of the meltwater inflow from small local glaciers in the catchment basin is not excluded.; La transition tardiglaciaire-Holocène précoce représente une période clé de l'histoire de la terre. Si cette transition est bien étudiée en Europe, ce n'est toutefois pas le cas au Moyen-Orient, et les profils paléohydrologiques associés à des chronologies robustes demeurent rares pour cette région. Nous présentons un profil hydrobiologique intéressant qui montre un important changement environnemental s'étant produit dans la zone humide de Dasht-e Arjan (sud-ouest de l'Iran, près de Persépolis) durant la transition tardiglaciaire-Holocène précoce (vers 11 650 ans cal BP). Nous utilisons des subfossiles de chi-ronomidés (insectes : diptères) comme indicateurs de changements hydrologiques et pour reconstituer les fluctuations du niveau de lacs. Le milieu humide d'Arjan était un lac profond durant le Dryas récent, caractérisé par une prépondérance de taxons de type Chironomus plumosus/anthracinus adaptés aux conditions anoxiques des eaux profondes. Une baisse drastique (de plus de 80 % à moins de 10 %) de ces taxons au début de l'Holocène, combinée à la diversification de taxons littoraux de types Polypedilum nubeculosum, Dicrotendipes nervosus et Glyptotendipes pallens, indiquerait une baisse du niveau du lac et un milieu aquatique plus végétalisé. Nous comparons le profil des chironomidés d'Arjan à un profil semblable du nord-ouest de l'Iran. La signification paléoclimatique du profil, aux échelles locales et régionales, est ensuite abordée. L'augmentation des températures dans l'hémisphère nord au début de l'Holocène, inférée à partir de données géochimiques du NGRIP, est ce qui explique le mieux le passage de conditions de haut niveau du Dryas récent aux conditions de bas niveau de l'Holocène précoce dans la zone humide de Dasht-e Arjan. Un effet de l'apport d'eau de fonte de petits glaciers locaux dans le bassin versant n'est toutefois pas exclu. [Traduit par la Rédaction] Mots-clés : Dryas récent, changement climatique, karst, changement du niveau des lacs, Zagros.

International audience; Despite frequent historical documents on shipping and trade routes in the Caspian Sea since early historical dates, the maritime archaeological evidence remains largely undiscovered. Exposing a shipwreck in southwest corner of the Caspian Sea at the shoreline of Qoroq village in Guilan Province of Iran provides an opportunity to study some frames of historical maritime activities in southern Caspian coasts. Sedimentological and geophysical, archaeological, and historical investigations were conducted to detect the age of the shipwreck, its probable origin and the impacts of environmental changes on preservation, exposing and damaging the ship. The results showed that the ship was broken down along its longitudinal axis and the remains were distributed along the shore where they are buried by coastal sediments. Pinus sylvestris is the tree species used in building the ship and the Caucasus Mountains was considered as a timber supply area. A combination of radiocarbon data and historical evidence showed that the ship's construction date is mostly back to mid-18th century. It seems that the ship sunk in a high energy environment. Deposition of various types of sediments inside and around of the shipwreck suggests that the ship was dragged from the high energy environment to the current location. The hydrodynamics of the coastal area along with rapid Caspian sea-level changes were mostly responsible for preservation as well as exposing the ship.

International audience; Historical texts and archaeological studies attest to the maritime and trade importance of the Persian Gulf since the Sassanid Empires. Nonetheless, there is a paucity of data regarding ancient navigation and the reasons for a shift in m aritim e trade from the western (e.g. Shatt-al-Arab) to eastern (Siraf) Persian Gulf by the Abbasid dynasty. For som e scholars, Siraf was occupied between 360 and 977 CE, after which tim e an earthquake en-trained the dem ise of the city. However, it is unclear when Siraf was founded and how natural navigation conditions changed for ocean-going vessels in harbours of the NW Persian Gulf. To address this knowledge gap, we here present new geoarchaeological data from Siraf. Two anthropogenic facies were detected in drilled cores. They suggest that Siraf dates back to 2 BC-317 CE. After a hiatus, a second occupation phase began during the reign of Shapur II. Relative Sea-Level (RSL) fluctuations, climate change and Persian Gulf bathymetry all affected the possible nautical accessibility of this ancient Persian harbour. A fall in RSL, leading to a shortening of navigable water columns and amplified summertime Shamal wind from 550 CE onwards possibly led to a loss in the im portance of Shatt-al-Arab and other ports in the western Persian Gulf. It appears to have m ade Siraf the best alternative for seafarers. According to the wind regimes, the best time for arrival and departure from Siraf was August and October, respectively. RSL rise and increasing coastal erosion during the winter-tim e Shamal winds led to the degradation of harbour potentialities and was possibly at the origin of econom ic decline and poorly adapted harbour works at Siraf during a 150-year period between 850 and 1000 CE.

We present the entomological results of a geological and biological exploration in the Lutdesert, performed in 2014 by the Iranian National Institute for Oceanography and AtmosphericSciences (INIOAS) and the University of Tehran. Five localities were sampled, including theone considered as the the hottest spot on Earth. They yielded 15 insect taxa belonging to Blat-todea, Orthoptera, Coleoptera, Heteroptera, suggesting that in spite of being originally de-scribed as “abiotic” or “aphytic”, the Lut desert shelters a diverse insect fauna with someremarkable elements such as the endemic desert cockroache Leiopteroblatta monodi. Compar-ison with results obtained by Franco-Iranian expeditions in the sixties and seventies revealsseveral taxa in common, but also striking differences in the composition of the insect assem-blages, suggesting that the insect fauna in the Lut desert is potentially much more diverse thanpreviously expected., info:eu-repo/semantics/published

Ongoing global change and its direct environmental impacts, in addition to securing economic transition to the post-oil era, could trigger complex socio-economic and political crises in oil-dependent economies of the Persian Gulf Region (PGR). To evaluate the role of climate change and related policies in degrading the environment and its socio-economic impacts in the PGR, we have used a variety of available global datasets and published data. The results show that the countries of the PGR pursue some types of socio-economic reforms to alleviate the impacts of climate change. However, it seems that these attempts are not compatible with the environment's capacity. The main problem stems from the fact that political differences between the PGR nations prevent them from managing the Persian Gulf environment as an integrated natural system and consequently they have to limit their efforts within their borders, regardless of what happens in other parts of the system. The shift to alternative revenue sources by the countries needs socioeconomic preparedness while there are environmental obstacles, political tensions and geopolitical rivalries. Unless there is a cooperative approach to mitigate the effects of climate change, accompanied by a reorientation of PGR economies, the situation is likely to worsen rather than improve. To address the challenges of climate change, integrated regional collaborations are needed. Collective action, such as more investment in regional research and development and education, is required if the PGR is to successfully transition from a commodity-based to a knowledge-based economy., Persian Gulf, Climate Change, Economy, Environment, Water Scarcity.

International audience; The striped hyena is the largest living omnivorous scavenger in SW Asia. It generally lives in semi-arid desert steppe regions, often denning in small caves, rock shelters, and burrows close to human settlements. Bone fragments of wild and domestic animals and desiccated scats are frequently found in the hyena dens. In this study, eight striped hyena desiccated scats were subjected to pollen analysis. All scats were rich in pollen and the exine was well-preserved with no visible sign of corrosion. Pollen spectra revealed interesting information on the regional and local vegetation, as well as the foraging behavior and diet of the animal. They reflected an array of different landscapes ranging from natural/semi-natural xerophytic desert steppes, agricultural fields, and grazing pastures. Some scats contained certain pollen taxa very rarely observed in wetland sediments, indicating the high potential of hyena "copropalynology"in providing detailed information on the past floristic composition of the landscape. When comparing with archeobotanical data from the area, the hyena scat assemblages show that the general physiognomy of the landscape has remained almost unchanged since the 6th millennium B.C., with only minor changes in the composition or density of the woody components of the desert steppe. As most of the Holocene fossil coprolites in archeological and paleontological sites of SW Asia would have been left by striped hyena, the study of the modern analogs of such accumulations in extant hyena dens is helpful to correctly interpret the fossil faunal assemblages to reconstruct the paleolandscapes, land-use change, and animal paleoethology.

International audience; South Caspian Sea sub-basin, as the deepest part of the Caspian Sea (CS) remained as land-locked basin even during extreme sea level fall that most part of the CS desiccated. Therefore, bottom sediments of the south CS continuously recorded many past intra-basinal and extra-basinal events. In the current research we have used four short cores (

International audience; Palustrine carbonates are frequently found with active and dried karstic springs in the foothills of the mountains bordering the Persepolis Basin, southwest Iran. A combination of geological conditions favours their formation, including (i) the presence of karstic limestone aquifers in the limbs of anticlines cut through by fault systems; (ii) very gentle slopes from the spring resurgence point towards the centre of the alluvial plain, creating a flat waterlogged area; and (iii) a semiarid climate with marked precipitation seasonality or significant fluctuations in water discharge and wetland water table. We suggest the term "anastomosing wetlands" or "anastomosing palustrine environments" to denote the studied karstic spring-fed carbonate wetlands, because of similarities with anastomosing river systems in aerial view. The common presence of extended anasto-mosing wetland carbonates in the Persepolis Basin and adjacent basins in the central and southern Zagros suggests that they can play an important role in the geological records of collision-related basin-and-range settings dominated by karstic limestones. Karstic spring wetlands are a main source of fresh water hosting a rich biodiversity, which attracts human communities, whose impact is visible in the archaeological material imbedded in the wetland stratigraphy. Fresh water availability, through these spring wetlands, partly explains why the semiarid Persepolis region was selected by successive civilizations, from Elamites to Persians until early Islamic entities, to establish regional centres throughout the period from the third millennium B.C. to the first millennium A.D. Only a few of these ecosystems have survived the intensive human activities of recent decades.; Des carbonates palustres sont fréquemment associés à des sources karstiques actives et asséchées dans le contrefort des montagnes bordant le bassin de Persépolis, dans le sud-ouest de l'Iran. Une combinaison de conditions géologiques favorise leur formation, à savoir : i) la présence d'aquifères de calcaires karstiques dans les flans d'anticlinaux découpés par des systèmes de failles, ii) les pentes très douces des points de résurgence de sources vers le centre de la plaine alluviale, créant une zone plane saturée et iii) un climat semi-aride caractérisé par une saisonnalité marquée des précipitations ou d'importantes fluctuations de l'écoulement de l'eau et de la nappe phréatique dans les zones humides. Nous proposons le terme « zones humides anastomosées » ou « milieux palustres anastomosés » pour désigner les zones humides à carbonates karstiques alimentées par des sources en raison de similitudes qu'elles présentent en vue aérienne avec des réseaux hydrographiques anastomosés. La présence répandue de carbonates dans les zones humides anastomosées du bassin de Persépolis et des bassins voisins des parties centrales et sud des monts Zagros indiquerait qu'ils peuvent jouer un rôle important dans les profils géologiques des milieux de bassins et montagnes. Ces milieux sont associés à des collisions tectoniques dans lesquels prédominent des calcaires karstiques. Les zones humides karstiques alimentées par des sources constituent une source d'eau douce majeure abritant une grande diversité). biologique qui attire les collectivités humaines, dont l'impact est visible dans le matériel archéologique présent dans la stratigraphie des zones humides. La disponibilité d'eau douce qu'offrent ces zones humides alimentées par des sources explique en partie pourquoi la région semi-aride de Persépolis a été retenue par des civilisations successives, des Élamites aux Perses jusqu'aux premières entités islamiques, pour y établir des centres régionaux durant toute la période allant du 3 e millénaire avant notre ère au 1er millénaire de notre ère. Seuls quelques-uns de ces écosystèmes ont survécu à l'intense activité humaine des récentes décennies.

International audience

International audience; Production, transport and deposition of mineral dust have significant impacts on different components of the Earth systems through time and space. In modern times, dust plumes are associated with their source region(s) using satellite and land-based measurements and trajectory analysis of air masses through time. Reconstruction of past changes in the sources of mineral dust as related to changes in climate, however, must rely on the knowledge of the geochemical and mineralogical composition of modern and paleo-dust, and that of their potential source origins. In this contribution, we present a 13,000-yr record of variations in radiogenic Sr–Nd–Hf isotopes and Rare Earth Element (REE) anomalies as well as dust grain size from an ombrotrophic (rain fed) peat core in NW Iran as proxies of past changes in the sources of dust over the interior of West Asia. Our data shows that although the grain size of dust varies in a narrow range through the entire record, the geochemical fingerprint of dust particles deposited during the low-flux, early Holocene period (11,700–6,000 yr BP) is distinctly different from aerosols deposited during high dust flux periods of the Younger Dryas and the mid-late Holocene (6,000–present). Our findings indicate that the composition of mineral dust deposited at the study site changed as a function of prevailing atmospheric circulation regimes and land exposure throughout the last deglacial period and the Holocene. Simulations of atmospheric circulation over the region show the Northern Hemisphere Summer Westerly Jet was displaced poleward across the study area during the early Holocene when Northern Hemisphere insolation was higher due to the Earth's orbital configuration. This shift, coupled with lower dust emissions simulated based on greening of the Afro-Asian Dust Belt during the early Holocene likely led to potential sources in Central Asia dominating dust export to West Asia during this period. In contrast, the dominant western and southwest Asian and Eastern African sources have prevailed during the mid-Holocene to modern times.

The Jiroft valley, situated on banks of the Halil Rud developed as an important agricultural and trading center during the Early Bronze Age. Known for its famous steatite sculptures and clay pottery, the first settlement in Konar Sandal collapsed around 3rd millennium BCE. A second shorter, but major phase of occupation in the settlement occurred towards the end of 2nd millennium BCE. A 250-cm long peat sequence near the archaeological complex at Konar Sandal was investigated to reconstruct the human environment history using palynological, sedimentological and geochemical data. With a basal age of 4 ka, the core traces the hydroclimatic changes and human activities that started just after large scale abandonment of Konar Sandal and extends from the late Bronze Age to the Mongol invasion. The results show that Jiroft had an arid dry climate dominated by the Saharo-Sindian open pseudo-savanna vegetation. However, due to human clearance and intensified agro-sylvo-pastoral activities, and climatic factors, the land-cover shifted from open xeric scrublands to a more open degraded landscape. The principal human occupation was cereal cultivation and herding. However, it is likely that during the more arid periods, communities retreated and abandoned agriculture, facilitating successional processes. Such droughts occurred around 4.0-3.8 ka and 3.4-2.8 ka and are related to the Siberian Anticyclonic system. Declining Artemisia and shrubs indicate milder climates ca. 3.8-3.4 ka and 2.8-0.6 ka. The latter period that started with the rule of the Persian empires (550-650 BCE), and continued through the Islamic era, coincides with intensive human activities, and the highest degradation of vegetation. (C) 2018 Elsevier Ltd. All rights reserved.

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The coastal area extending east of the city of Martigues, between the bays of Bonnieu and that of Chariot, is characterized by an alternation of gently sloping rocky coast and 5 m high cliffs composed of Miocene limestone. The foot of the cliff is marked by a well developed notch and a discontinuous wave-cut platform; at its base, the sea bottom reaches a maximum depth of about 4.5–6 m. The emerged area shows boulders placed up to 10 m inland of the coastline at around 2 m above s.l. and, weighing as much as 35 tonnes. A geomorphological survey was conducted by means of a Terrestrial Laser Scanner to estimate boulder sizes. The particular focus of the proposed study was to estimate the minimum wave height required to detach and transport two boulders, originally joined together as one bigger one and weighing approximately 25 tonnes, from the wave-cut platform onto the surf bench. Hydrodynamic models developed by various authors were used to calculate the minimum wave height necessary to move them. The data obtained from the resulting hydrodynamic equations were compared to wave-climate data collected over the last 15 years by the buoy off the coast of Marseille, in the Gulf of Lion. The present study seems to confirm that it would not have been necessary to have a tsunami impact (among other things, never recorded in the last 20 years) to move a 25 tonnes boulder. Indeed, hydrodynamic equations suggest that the boulder might have been broken and only subsequently moved due to the impact of waves generated by an extreme storm which would have occurred prior to December 2003. This hypothesis seems to be in agreement with the morphology of the sea bottom, hydrodynamic features of the area as well as eyewitnesses.

The establishment of Regional Education and Research Centre on Oceanography for West Asia (RCOWA) was approved by 37th UNESCO General Conference as a Category 2 under the Auspices of UNESCO in the Iranian National Institute for Oceanography and Atmospheric Science (INIOAS) in November 2013 (37 C/18 Part XVII) and the agreement was signed in 2015. The center aims to achieve the objectives of the agreement which are as follows: (a)ensure the harmonious and mutually reinforcing involvement of the members of the region in Ocean studies by organizing joint projects, conferences and training/educational courses; (b)define regional problems, the solution of which requires regional and international cooperation, assist in the identification of training, education, and mutual assistance needs, particularly those related to the Centre programs; (c)assist in identification and meeting national and regional priorities by sharing knowledge and experience through organizing training courses and symposiums; (d)engage the academic and research community, experts from governmental and non-governmental organizations, industry, and decision-makers from the region and abroad in finding ways to solve the challenging economic and social problems facing the region by organizing exchange visits, consultations, etc. This objective will be achieved through the organization of regional forum/network to address the challenges, explore scientific understanding of the impacts and to discuss policies on the use and protection of the sea and coasts in supporting economic development of each country of the region, and the region as the whole;(e)supervise and coordinate the implementation of joint projects in consultation with national and international institutions of the Member States concerned in order to avoid duplication and overlap of efforts by organizing regular meetings with regional partners; (f)promote the standardization of data collection and data analysis methods based on existing protocols and agreements. Advocate open access and free exchange of oceanographic data along the guidelines specified in the IOC/IODE data exchange policy to facilitate scientific progress and improve education and training results. Reanimate IOC/IODE ODIN type program for the region; (g)advice on the application of new knowledge on science and technology to various priority areas at the local/national/regional levels by organizing workshops and briefings; (h)provide general guidance and recommendations, as well as serve as a mechanism for Member States, to formulate, evaluate, and follow-up on proposals for projects aimed at strengthening national and regional capabilities in marine scientific research, education and the establishment of common services and facilities; (i)make the operations of the Centre open and transparent by producing regular newsletters/bulletins to describe the progress of the Canter’s operations, developing the Centre’s web-site and increasing communication flow/exchange of information on activities, in order to discuss common issues and explore opportunities for further collaboration; (j)promote activities of the Centre and UNESCO as well as UNESCO/IOC role in marine and coastal matters; raise public awareness concerning the need for the sustainable management of the sea and coastal areas; and introduce the benefits of national and regional cooperation approach and of the importance of the operation of the sea and coasts by supporting establishment of Marine Protected Areas, through active participation in World Ocean Day and other awareness raising efforts; (k)collect information on the state of the art technology required for the implementation of the maritime program activities, develop an inventory of regional institutions and experts working on marine related issues, as well as catalogues of regional oceanographic data and make this information available to decision-makers and regional/international partners; (l)organize assistance in mobilizing human, financial, and material resources to respond to the needs of the coastal countries of the region in dealing with emergency situations triggered by marine natural disasters; and, (m)make recommendations to the governing bodies of the region on policy matters, and submit proposals on the budgetary and other forms of support required for the successful work of the Centre. Geographical Coverage of the Centre17 countries of the West Asia region are covered by the Centre activities: (Pakistan, Iraq, Oman, Turkey, India, Qatar, Lebanon, Egypt, United Arab Emirates, Kuwait, Yemen, Bahrain, Saudi Arabia, Syria, Palestine, Jordan and Iran). On case to case basis, neighboring countries to the region are invited to take part in the activities of the Centre. OpenASFA input Published Non Refereed

International audience; Environmental changes since the late deglaciation are reconstructed from the sediment of Lake Hamoun. Lake Hamoun is located at the border of Iran and Afghanistan where inflowing rivers originate from the drainage basins of SW Hindu Kush Mountains and westernmost Himalaya. The lake has experienced a complex hydrological history during the late Quaternary due to climatic changes. Geochemical, sedimentological, and paleontological proxies as well as geomorphological data were used to investigate environmental changes of the lake. The results demonstrate that since the late glacial, the basin has directly and/or indirectly received its moisture from various climatic systems. During the early Holocene, both the Indian summer monsoon (ISM) and the mid-latitude westerlies (MLW) intensified and consequently the basin received higher precipitation. This interpretation is supported by higher content of total organic matter (mean: 8.2%), finer-grained sediments with low delta O-18 values (mean: -3.5%), as well as rich fossil content. Lower organic matter content (,\textless 5%), higher magnetic susceptibility values (5.8-10x10(-4) SI unit), and coarser-grained sediments with no shell fragments support the dominance of an arid environment during the early-mid Holocene. The results of stable isotopes suggest weakening of ISM and intensification of MLW during the mid-late Holocene in the study area, when Bronze Age civilizations emerged in the Sistan Basin. In the late Holocene, lake levels experienced more severe fluctuations due to variations in the MLW. Shifts in settlement areas seen in the archaeological record may thus have been a response to climatic changes.

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This article is made available through the Brunel Open Access Publishing Fund. Copyright @ Author(s) 2013. This work is distributed under the Creative Commons Attribution 3.0 License. Historical literature may constitute a valuable source of information to reconstruct sea-level changes. Here, historical documents and geological records have been combined to reconstruct Caspian sea-level (CSL) changes during the last millennium. In addition to a comprehensive literature review, new data from two short sediment cores were obtained from the south-eastern Caspian coast to identify coastal change driven by water-level changes and to compare the results with other geological and historical findings. The overall results indicate a high-stand during the Little Ice Age, up to −21m (and extra rises due to manmade river avulsion), with a −28m low-stand during the Medieval Climate Anomaly, while presently the CSL stands at −26.5 m. A comparison of the CSL curve with other lake systems and proxy records suggests that the main sea-level oscillations are essentially paced by solar irradiance. Although the major controller of the long-term CSL changes is driven by climatological factors, the seismicity of the basin creates local changes in base level. These local base-level changes should be considered in any CSL reconstruction.

International audience; Core sediments from the dry lake bed of Hamoun were subdivided into 3 main sedimentary units using a multi-proxy approach (e.g. petrography, grain size analysis, total organic matter % and CaCO3% determination) to reconstruct the palaeoenvironment of the Sistan Basin (SE Iran) as a transition zone between the monsoon summer precipitation zone of south Asia and the Mediterranean winter precipitation zone of the Iranian plateau during the Holocene. Data revealed that during the late-glacial to early Holocene, the lake and its catchment area, western Hindu Kush, were under a more prominent influence of the Indian Ocean monsoon and formed a moist and productive environment with less wind action, as shown by the provenance of high organic matter lacustrine sediments together with the lack of an aeolian fraction. Due to southward migration of the Inter Tropical Convergence Zone during the mid Holocene, arid climate manifested by an interplay of seasonal aeolian and fluvial deposition became dominant. These conditions were due to reinforcement of subtropical anticyclones on the Iranian plateau. The presence of green to brownish green moderate organic matter lacustrine sediments showed that during the late Holocene, Mediterranean-type winter precipitation dominated in the area. During the initial part of this period, the Shahr-iSukhteh civilization was close to the lake. The environment was relatively similar with that of today. Some palaeostorms can also be detected during this time interval, shown by occurrences of high aeolian inputs in the basin. (C) 2015 Elsevier Ltd and INQUA. All rights reserved.

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https://hal.archives-ouvertes.fr/hal-02567362; International audience

International audience; Ancient Persia witnessed one of its most prosperous cultural and socio-economic periods between 550 bc and ad 651, with the successive domination of the Achaemenid, Seleucid, Parthian and Sassanian Empires. During this period agricultural activities increased on the Iranian plateau, as demonstrated by a remarkable arboricultural expansion. However, available data are not very informative about the spatial organization of agricultural practices. The possible links between climate conditions and agricultural activities during this millennium of continuous imperial domination are also unclear, due to the lack of parallel human-independent palaeoclimatic proxies. This study presents a new late Holocene pollen-based vegetation record from Lake Parishan, SW Iran. This record provides invaluable information regarding anthropogenic activities before, during and after the empires and sheds light on (i) spatial patterning in agricultural activities and (ii) possible climate impacts on agro-sylvo-pastoral practices during this period. Results of this study indicate that arboriculture was the most prominent form of agricultural activity in SW Iran especially during the Achaemenid, Seleucid and Parthian periods. Contrary to the information provided by some Greco-Roman written sources, the record from Lake Parishan shows that olive cultivation was practiced during Achaemenid and Seleucid times, when olive cultivation was significant, at least in this basin located close to the capital area of the Achaemenid Empire. In addition, pollen from aquatic vegetation suggests that the period of the latter centuries of the first millennium bc was characterized by a higher lake level, which might have favoured cultural and socio-economic prosperity.

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International audience; Two short (100 and 175 cm-long) sediment cores from the southwestern corner of Lake Urmia provide a record of vegetation dynamics, lake-level changes and the role of climate and humans in shaping the landscape around Lake Urmia over the last 2550 years. Relatively low values of arboreal pollen (AP), and substantial values of Artemisia pollen from 2550 to 1500 cal BP indicate the prevalence of steppe vegetation and relatively arid climate in the area. However, a prominent peak of Riella spores may indicate a short-lived lake-level rise for the period 1900-2000 cal BP. The next period, 1500-550 cal BP, is characterized by substantial rise in AP, particularly Quercus, and a sharp decline of Artemisia, Chenopodiaceae/Amaranthaceae and wetland pollen types, suggesting the expansion of oak forests under a rather moist climate and/or a decline in agro-sylvo-pastoral practices in the area. Agricultural activity in the area can be inferred from sporadic occurrences of Vitis, Ricinus and Juglans pollen from the beginning of the record. The rise of saline habitat pollen types between 1100 and 800 cal BP, along with increased values of magnetic susceptibility and organic matter, suggest a lower water level and the subaerial exposure of saline mud flats, which could favour the re-colonization of chenopods and other halophytes around the margins of the lake. Thus, the Medieval Climatic Anomaly seems to be warmer-than-present in the Lake Urmia region. From 450 to 150 cal BP, the decline in Quercus and high values of Artemisia, along with higher lake levels and high magnetic susceptibility values, could be associated with the Little Ice Age. Since 500 cal BP, Quercus and Riella steadily decline and fade out towards the surface of the core, whereas pollen types attributable to steppe and desert vegetation increase. A prominent increase in organic matter in the uppermost part of the record could be associated with a lower lake level and the expansion of wetland vegetation in the recent past. Our findings suggest that the regional forest coverage in the highlands of Zagros and Azerbaijan has reached its minimum during recent decades, while Urmia's lake level dropped dramatically (increasing its water salinity) most likely as a function of extensive anthropogenic activities and general climate aridification. (C) 2015 Elsevier Ltd and INQUA. All rights reserved.

International audience; With ongoing climate change, coral susceptibility to thermal stress constitutes a central concern in reefconservation. In the Persian Gulf, coral reefs are confronted with a high seasonal variability in water temperature, and both hot and cold extremes have been associated with episodes of coral bleaching and mortality. Using physiological performance as a measure of coral health, we investigated the thermal susceptibility of the common acroporid, Acropora downingi, near Hengam Island where the temperature oscillates seasonally in the range 20.2-34.2 °C. In a series of two short-term experiments comparing coral response in summer versus winter conditions, we exposed corals during each season (1) to the corresponding seasonal average and extreme temperature levels in a static thermal environment, and (2) to a progressive temperature deviation from the annual mean toward the corresponding extreme seasonal value and beyond in a dynamic thermal environment. We monitored four indictors of coral physiological performance: net photosynthesis (Pn), dark respiration (R), autotrophic capability (Pn/R), and survival. Corals exposed to warming during summer showed a decrease in net photosynthesis and ultimately died, while corals exposed to cooling during winter were not affected in their photosynthetic performance and survival. Coral autotrophic capability Pn/R was lower at the warmer thermal level within eachseason, and during summer compared to winter. Corals exposed to the maximum temperature of summer displayed Pn/R < 1, inferring that photosynthetic performance could not support basal metabolic needs under this environment. Our results suggest that the autotrophic performance of the Persian Gulf A. downingi is sensitive to the extreme temperatures endured in summer, and therefore its populations may be impacted by future increases in water temperature.

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International audience; A short sediment core (300 cm) was retrieved from a peaty deposit in the northeastern corner of Lake Neor in NW Iran yielding a 6500-year-old sequence relatively rich in pollen and beetle remains. Beetle assemblages contained a significant amount of coprophagous and coprophilous species all along the core. Pollen spectra suggest an open steppe landscape typical of the modern Irano-Turanian highlands with pollen indicators of agro-pastoral activities and also the proximity of the mesic temperate Hyrcanian forest to the east. Together, insect and pollen evidence, in agreement with the archaeological evidence for NW Iran, suggest that pastoralism was practised in the high elevation surroundings of Neor in Talysch Mountains at least since ca. 6500 years ago. This preliminary study highlights the strong potential of palaeoentomological investigations in furthering our understanding of the history of pastoralism in the Middle East.