40 results on '"Djamali M"'
Search Results
2. Archaeology, history and symbolism.
- Author
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Spagnoli, F., primary, Shirazi, R., additional, Shirazi, Z., additional, Andam, S. Saeidi Ghavi, additional, and Djamali, M., additional
- Published
- 2021
- Full Text
- View/download PDF
3. Environmental and climate reconstruction of the late-glacial-Holocene transition from a lake sediment sequence in Aubrac, French Massif Central: Chironomid and diatom evidence
- Author
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Gandouin, E., Rioual, P., Pailles, C., Brooks, S.J., Ponel, P., Guiter, F., Djamali, M., Andrieu-Ponel, V., Birks, H.J.B., Leydet, M., Belkacem, D., Haas, J.N., Van der Putten, N., and de Beaulieu, J.L.
- Published
- 2016
- Full Text
- View/download PDF
4. Tappeh Qazānchi, a Settlement from the Early Neolithic to the Bronze Age in the Kermanshah Plain, Iran
- Author
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Mashkour, Marjan, Davoudi, H., Djamali, M., Shidrang, S., Tengberg, M., Mylona, Pantelitsa, Khormali, F., Morteza, R., Beizaee Doost, S., Moradi, B., Khazaeli, R., Fathi, H., Fathi, Z., Archéozoologie, archéobotanique : sociétés, pratiques et environnements (AASPE), Muséum national d'Histoire naturelle (MNHN)-Centre National de la Recherche Scientifique (CNRS), University of Tehran, Institut méditerranéen de biodiversité et d'écologie marine et continentale (IMBE), Avignon Université (AU)-Aix Marseille Université (AMU)-Institut de recherche pour le développement [IRD] : UMR237-Centre National de la Recherche Scientifique (CNRS), MUSEE NATIONAL IRAN, and Muséum national d'Histoire naturelle (MNHN)
- Subjects
[SDV.EE]Life Sciences [q-bio]/Ecology, environment ,Central Zagros ,[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory ,Lithic and pottery technologies ,Palaeoenvironment ,Micromorphology ,Bioarchaeology ,[SHS]Humanities and Social Sciences - Abstract
International audience; Tappeh Qazānchi, not far from the Razavar river, is located to the northwest of Kermanshah city at 1323 masl. Parts of the north and east sides of the mound have been damaged by agricultural activities. As a result, 100 m of the northern section has been exposed, and has been found to contain cultural sequences from throughout the Holocene. The site was sounded during the winter of 2019 to identify the cultural sequences, site formation and settlement patterns present. The extent of the core area was estimated to be ca. 2 hectares, following sounding results in test trenches that were excavated in order to define the core area and buffer zone. The first results from the stratigraphic excavation and the relative and absolute chronologies indicate that the upper levels of the site belong to the Middle Bronze Age and the Late Chalcolithic periods, and the lower levels contain a Pre-Pottery Neolithic sequence. The results of archaeobotanical, archaeozoological, micromorphological and palaeoclimatological studies point to a localised wet environment during the Holocene with periodically flooded zones around the site. Tappeh Qazānchi is comparable to the Middle Bronze Age of Chogha Maran (upper phase) and Godin Tepe (Period III), as well as the Late Chalcolithic of Siahbid (middle and late phases) and GodinTepe (Period IX), that are located in the same cultural range in Central Zagros. The Pre-Pottery Neolithic phases at Qazānchi are also contemporaneous to East Chia Sabz, Sheikh-e Abad, Kelek Asad Morad and Chogha Golan, and this is also one of the first settlements in the early Holocene in the east of the Fertile Crescent.
- Published
- 2023
5. Tappeh Qazanchi, an example of a pioneering farming community during the Pre-Pottery Neolithic in Central Zagros (Iran). In session: Uses and misuses of landscapes and resources: New perspectives on pioneer farming societies in the world
- Author
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Mashkour, M., Davoudi, H., Tengberg, M., Mylona, P., Shidrang, S., Djamali, M., Beizaee Doost, S., Khazaeli, R., Fathi, H., Archéozoologie, archéobotanique : sociétés, pratiques et environnements (AASPE), Muséum national d'Histoire naturelle (MNHN)-Centre National de la Recherche Scientifique (CNRS), Archaeozoological section, Bioarchaeological laboratory, University of Tehran, Muséum national d'Histoire naturelle (MNHN), National Museum of Iran, Institut méditerranéen de biodiversité et d'écologie marine et continentale (IMBE), Avignon Université (AU)-Aix Marseille Université (AMU)-Institut de recherche pour le développement [IRD] : UMR237-Centre National de la Recherche Scientifique (CNRS), University of Tehran, Central Laboratory, Bioarchaeology Laboratory, LIA-CNRS project HAOMA - Human and Environment Interaction on the Iranian Plateau. PIs Marjan Mashkour (CNRS-AASPE) & Morteza Djamali (CNRS-IMBE), and AFEQ-CNF INQUA https://q13.sciencesconf.org
- Subjects
[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory ,[SDE.BE]Environmental Sciences/Biodiversity and Ecology - Abstract
International audience; Recent archaeological investigations in the North West of Kermanshah have highlighted the importance of this region for documenting initial stages of the Neolithisation of Central Zagros. During winter 2019 we excavated Tappeh Qazānchi, near Kermanshah. The site was first reported by Robert J. Braidwood during the 60’s. It is unfortunately now heavily damaged by agricultural activities. Tappeh Qazānchi is a 2 hectares mound of 13 meters height, 160 meters long and 160 meters wide. Our preliminary surface collection on the site during 2012 indicated a multi-period occupation and the presence of lithic tools characteristic of the Early Neolithic period. The 2019 sounding confirmed these preliminary observations. We opened three trenches and found a Bronze Age deposit on the top of the mound and pre-pottery Neolithic ashy layers from eight to thirteen meters lower down. The Neolithic occupation of Tappeh Qazānchi is comparable to Chogha Golan, Sheikhi Abad and East Chia Sabz on the basis of radiocarbon dating and lithic analyses. This presentation will summarise the results of chronological, bioarchaeological, lithic and micromorphological studies with a particular emphasis on archaeobotanical, archaeozoological and micromorphologial results.
- Published
- 2022
6. Late Little Ice Age palaeoenvironmental records from the Anzali and Amirkola Lagoons (south Caspian Sea): Vegetation and sea level changes
- Author
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Leroy, S.A.G., Lahijani, H.A.K., Djamali, M., Naqinezhad, A., Moghadam, M.V., Arpe, K., Shah-Hosseini, M., Hosseindoust, M., Miller, Ch.S., Tavakoli, V., Habibi, P., and Naderi Beni, M.
- Published
- 2011
- Full Text
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7. The Eurasian Modern Pollen Database (EMPD), version 2
- Author
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Davis, B, Chevalier, M, Sommer, P, Carter, V, Finsinger, W, Mauri, A, Phelps, L, Zanon, M, Abegglen, R, Akesson, C, Alba-Sanchez, F, Scott Anderson, R, Antipina, T, Atanassova, J, Beer, R, Belyanina, N, Blyakharchuk, T, Borisova, O, Bozilova, E, Bukreeva, G, Jane Bunting, M, Clo, E, Colombaroli, D, Combourieu-Nebout, N, Desprat, S, Di Rita, F, Djamali, M, Edwards, K, Fall, P, Feurdean, A, Fletcher, W, Florenzano, A, Furlanetto, G, Gaceur, E, Galimov, A, Galka, M, Garcia-Moreiras, I, Giesecke, T, Grindean, R, Guido, M, Gvozdeva, I, Herzschuh, U, Hjelle, K, Ivanov, S, Jahns, S, Jankovska, V, Jimenez-Moreno, G, Karpinska-Kolaczek, M, Kitaba, I, Kolaczek, P, Lapteva, E, Latalowa, M, Lebreton, V, Leroy, S, Leydet, M, Lopatina, D, Lopez-Saez, J, Lotter, A, Magri, D, Marinova, E, Matthias, I, Mavridou, A, Mercuri, A, Mesa-Fernandez, J, Mikishin, Y, Milecka, K, Montanari, C, Morales-Molino, C, Mrotzek, A, Sobrino, C, Naidina, O, Nakagawa, T, Nielsen, A, Novenko, E, Panajiotidis, S, Panova, N, Papadopoulou, M, Pardoe, H, Pedziszewska, A, Petrenko, T, Ramos-Roman, M, Ravazzi, C, Rosch, M, Ryabogina, N, Ruiz, S, Sakari Salonen, J, Sapelko, T, Schofield, J, Seppa, H, Shumilovskikh, L, Stivrins, N, Stojakowits, P, Svitavska, H, Swieta-Musznicka, J, Tantau, I, Tinner, W, Tobolski, K, Tonkov, S, Tsakiridou, M, Valsecchi, V, Zanina, O, Zimny, M, Davis B. A. S., Chevalier M., Sommer P., Carter V. A., Finsinger W., Mauri A., Phelps L. N., Zanon M., Abegglen R., Akesson C. M., Alba-Sanchez F., Scott Anderson R., Antipina T. G., Atanassova J. R., Beer R., Belyanina N. I., Blyakharchuk T. A., Borisova O. K., Bozilova E., Bukreeva G., Jane Bunting M., Clo E., Colombaroli D., Combourieu-Nebout N., Desprat S., Di Rita F., Djamali M., Edwards K. J., Fall P. L., Feurdean A., Fletcher W., Florenzano A., Furlanetto G., Gaceur E., Galimov A. T., Galka M., Garcia-Moreiras I., Giesecke T., Grindean R., Guido M. A., Gvozdeva I. G., Herzschuh U., Hjelle K. L., Ivanov S., Jahns S., Jankovska V., Jimenez-Moreno G., Karpinska-Kolaczek M., Kitaba I., Kolaczek P., Lapteva E. G., Latalowa M., Lebreton V., Leroy S., Leydet M., Lopatina D. A., Lopez-Saez J. A., Lotter A. F., Magri D., Marinova E., Matthias I., Mavridou A., Mercuri A. M., Mesa-Fernandez J. M., Mikishin Y. A., Milecka K., Montanari C., Morales-Molino C., Mrotzek A., Sobrino C. M., Naidina O. D., Nakagawa T., Nielsen A. B., Novenko E. Y., Panajiotidis S., Panova N. K., Papadopoulou M., Pardoe H. S., Pedziszewska A., Petrenko T. I., Ramos-Roman M. J., Ravazzi C., Rosch M., Ryabogina N., Ruiz S. S., Sakari Salonen J., Sapelko T. V., Schofield J. E., Seppa H., Shumilovskikh L., Stivrins N., Stojakowits P., Svitavska H. S., Swieta-Musznicka J., Tantau I., Tinner W., Tobolski K., Tonkov S., Tsakiridou M., Valsecchi V., Zanina O. G., Zimny M., Davis, B, Chevalier, M, Sommer, P, Carter, V, Finsinger, W, Mauri, A, Phelps, L, Zanon, M, Abegglen, R, Akesson, C, Alba-Sanchez, F, Scott Anderson, R, Antipina, T, Atanassova, J, Beer, R, Belyanina, N, Blyakharchuk, T, Borisova, O, Bozilova, E, Bukreeva, G, Jane Bunting, M, Clo, E, Colombaroli, D, Combourieu-Nebout, N, Desprat, S, Di Rita, F, Djamali, M, Edwards, K, Fall, P, Feurdean, A, Fletcher, W, Florenzano, A, Furlanetto, G, Gaceur, E, Galimov, A, Galka, M, Garcia-Moreiras, I, Giesecke, T, Grindean, R, Guido, M, Gvozdeva, I, Herzschuh, U, Hjelle, K, Ivanov, S, Jahns, S, Jankovska, V, Jimenez-Moreno, G, Karpinska-Kolaczek, M, Kitaba, I, Kolaczek, P, Lapteva, E, Latalowa, M, Lebreton, V, Leroy, S, Leydet, M, Lopatina, D, Lopez-Saez, J, Lotter, A, Magri, D, Marinova, E, Matthias, I, Mavridou, A, Mercuri, A, Mesa-Fernandez, J, Mikishin, Y, Milecka, K, Montanari, C, Morales-Molino, C, Mrotzek, A, Sobrino, C, Naidina, O, Nakagawa, T, Nielsen, A, Novenko, E, Panajiotidis, S, Panova, N, Papadopoulou, M, Pardoe, H, Pedziszewska, A, Petrenko, T, Ramos-Roman, M, Ravazzi, C, Rosch, M, Ryabogina, N, Ruiz, S, Sakari Salonen, J, Sapelko, T, Schofield, J, Seppa, H, Shumilovskikh, L, Stivrins, N, Stojakowits, P, Svitavska, H, Swieta-Musznicka, J, Tantau, I, Tinner, W, Tobolski, K, Tonkov, S, Tsakiridou, M, Valsecchi, V, Zanina, O, Zimny, M, Davis B. A. S., Chevalier M., Sommer P., Carter V. A., Finsinger W., Mauri A., Phelps L. N., Zanon M., Abegglen R., Akesson C. M., Alba-Sanchez F., Scott Anderson R., Antipina T. G., Atanassova J. R., Beer R., Belyanina N. I., Blyakharchuk T. A., Borisova O. K., Bozilova E., Bukreeva G., Jane Bunting M., Clo E., Colombaroli D., Combourieu-Nebout N., Desprat S., Di Rita F., Djamali M., Edwards K. J., Fall P. L., Feurdean A., Fletcher W., Florenzano A., Furlanetto G., Gaceur E., Galimov A. T., Galka M., Garcia-Moreiras I., Giesecke T., Grindean R., Guido M. A., Gvozdeva I. G., Herzschuh U., Hjelle K. L., Ivanov S., Jahns S., Jankovska V., Jimenez-Moreno G., Karpinska-Kolaczek M., Kitaba I., Kolaczek P., Lapteva E. G., Latalowa M., Lebreton V., Leroy S., Leydet M., Lopatina D. A., Lopez-Saez J. A., Lotter A. F., Magri D., Marinova E., Matthias I., Mavridou A., Mercuri A. M., Mesa-Fernandez J. M., Mikishin Y. A., Milecka K., Montanari C., Morales-Molino C., Mrotzek A., Sobrino C. M., Naidina O. D., Nakagawa T., Nielsen A. B., Novenko E. Y., Panajiotidis S., Panova N. K., Papadopoulou M., Pardoe H. S., Pedziszewska A., Petrenko T. I., Ramos-Roman M. J., Ravazzi C., Rosch M., Ryabogina N., Ruiz S. S., Sakari Salonen J., Sapelko T. V., Schofield J. E., Seppa H., Shumilovskikh L., Stivrins N., Stojakowits P., Svitavska H. S., Swieta-Musznicka J., Tantau I., Tinner W., Tobolski K., Tonkov S., Tsakiridou M., Valsecchi V., Zanina O. G., and Zimny M.
- Abstract
The Eurasian (née European) Modern Pollen Database (EMPD) was established in 2013 to provide a public database of high-quality modern pollen surface samples to help support studies of past climate, land cover, and land use using fossil pollen. The EMPD is part of, and complementary to, the European Pollen Database (EPD) which contains data on fossil pollen found in Late Quaternary sedimentary archives throughout the Eurasian region. The EPD is in turn part of the rapidly growing Neotoma database, which is now the primary home for global palaeoecological data. This paper describes version 2 of the EMPD in which the number of samples held in the database has been increased by 60 % from 4826 to 8134. Much of the improvement in data coverage has come from northern Asia, and the database has consequently been renamed the Eurasian Modern Pollen Database to reflect this geographical enlargement. The EMPD can be viewed online using a dedicated map-based viewer at https://empd2.github.io and downloaded in a variety of file formats at https://doi.pangaea.de/10.1594/PANGAEA.909130 (Chevalier et al., 2019).
- Published
- 2020
8. Exploring Mathematical Concepts and Philosophical Values in Jember Batik
- Author
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Amalia, Devita, primary, Noviani, Dwi, additional, Djamali, M. Fadil, additional, and Rofiki, Imam, additional
- Published
- 2021
- Full Text
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9. Modern pollen rain–vegetation relationships along a forest–steppe transect in the Golestan National Park, NE Iran
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Djamali, M., de Beaulieu, J.-L., Campagne, P., Andrieu-Ponel, V., Ponel, P., Leroy, S.A.G., and Akhani, H.
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- 2009
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10. The first archaeological campaign at Tappeh Qazānchi, a new PPN site in the West Central Zagros
- Author
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Mashkour, Marjan, Davoudi, Hossein, Shidrang, S, Orange, M., Khoramli, F., Mylona, P, Djamali, M., Tengberg, Margareta, Rahmati, M., Beyzaei Doust, Sanaz, Moradi, B., Khazaeli, R., Fathi, Homa, Fathi, Z., Archéozoologie, archéobotanique : sociétés, pratiques et environnements (AASPE), Muséum national d'Histoire naturelle (MNHN)-Centre National de la Recherche Scientifique (CNRS), University of Tehran, Central Laboratory, Bioarchaeology Laboratory, Center for Paleolithic Research, National Museum of Iran, Institut méditerranéen de biodiversité et d'écologie marine et continentale (IMBE), Avignon Université (AU)-Aix Marseille Université (AMU)-Institut de recherche pour le développement [IRD] : UMR237-Centre National de la Recherche Scientifique (CNRS), Archaeozoological section, Bioarchaeological laboratory, University of Tehran, and Université de Copenhague
- Subjects
[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory - Abstract
International audience
- Published
- 2021
11. EKSPLORASI KONSEP DILATASI ETNOMATEMATIKA PADA BATIK TEMBAKAU JEMBER
- Author
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Sulisawati, Dwi Noviani, primary, Amalia, Devita, primary, and Djamali, M. Fadil, primary
- Published
- 2021
- Full Text
- View/download PDF
12. Réflexions sur la contribution des coprolithes de hyènes modernes comme référentiel pour les reconstitutions paléoenvironnementales
- Author
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Djamali, M., Mashkour, M, Institut méditerranéen de biodiversité et d'écologie marine et continentale (IMBE), Avignon Université (AU)-Aix Marseille Université (AMU)-Institut de recherche pour le développement [IRD] : UMR237-Centre National de la Recherche Scientifique (CNRS), Archéozoologie, archéobotanique : sociétés, pratiques et environnements (AASPE), Muséum national d'Histoire naturelle (MNHN)-Centre National de la Recherche Scientifique (CNRS), and Région Île-de-France en co-organisation avec le DIM « Matériaux anciens et patrimoniaux »
- Subjects
[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory ,[SDE.BE]Environmental Sciences/Biodiversity and Ecology - Abstract
International audience
- Published
- 2021
13. Palaeoenvironment of a Late Quaternary lacustrine–palustrine carbonate complex: Zarand Basin, Saveh, central Iran
- Author
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Djamali, M., Soulié-Märsche, I., Esu, D., Gliozzi, E., and Okhravi, R.
- Published
- 2006
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14. Fire as a motor of rapid environmental degradation during the earliest peopling of Malta 7500 years ago
- Author
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Marriner, N., Kaniewski, D., Gambin, T., Gambin, B., Vannière, B., Morhange, C., Djamali, M., Tachikawa, K., Robin, V., Rius, D., and Bard, E.
- Published
- 2019
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15. Dendrochronological studies of common cypress (Cupressus sempervirens L. var. horizontalis) to determine its annual diameter growth rate and identify the oldest trees in the Hyrcanian habitats, Iran.
- Author
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Eshkevari, T. Amini, Ejtehad, H., and Djamali, M.
- Abstract
In temperate regions, the one-year life cycle forms observable growth rings influenced by the genetic, physiological, climatic, and physiographic structures of trees that consider in dendrochronology. Common cypress (Cupressus sempervirens L. var. horizontalis) is a precious Mediterranean species that grows in the Hyrcanian regions, as the only native cypress in Iran. In order to determine the annual diameter growth of this species and to identify the oldest trees, a sample of 92 aging woods was selected in the Hyrcanian habitats of Iran. Samples were collected by an increment borer with a length of 50 cm and measured in the dendrochronology laboratory by Lintab 6 device, and the obtained data were automatically recorded for time matching in TSAP-Win software and time series analysis. After comparative dating and eliminating any measurement error, the mean values of the vegetative ring width of all specimens were calculated and the average growth of the cypress was obtained. The relationship between the width of growth rings in each cypress tree, and the difference in tree growth of the three provinces viz. Gilan, Mazandaran and Golestan was evaluated using R software. The results showed that a tree in Viaeyeh, Rudbar county is the oldest tree in existence reaching an age of 1519 years. The annual diameter growth of cypress is reported as 0.95 mm. The growth rate curve in Mazandaran province during the last 450 years showed milder characteristics in the arrangement, uniformity and slope of change compared to the other two provinces. This indicates the stability of climatic and habitat conditions in Hassanabad, Mazandaran province, compared with the two other areas and sufficient evidence that this area is very close to the Mediterranean climate. [ABSTRACT FROM AUTHOR]
- Published
- 2022
- Full Text
- View/download PDF
16. Pollen-derived biomes in the Eastern Mediterranean–Black Sea–Caspian-Corridor
- Author
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Marinova, E. Harrison, S.P. Bragg, F. Connor, S. de Laet, V. Leroy, S.A.G. Mudie, P. Atanassova, J. Bozilova, E. Caner, H. Cordova, C. Djamali, M. Filipova-Marinova, M. Gerasimenko, N. Jahns, S. Kouli, K. Kotthoff, U. Kvavadze, E. Lazarova, M. Novenko, E. Ramezani, E. Röpke, A. Shumilovskikh, L. Tanţǎu, I. Tonkov, S.
- Abstract
Aim: To evaluate the biomization technique for reconstructing past vegetation in the Eastern Mediterranean–Black Sea–Caspian-Corridor using an extensive modern pollen data set and comparing reconstructions to potential vegetation and observed land cover data. Location: The region between 28–48°N and 22–62°E. Methods: We apply the biomization technique to 1,387 modern pollen samples, representing 1,107 entities, to reconstruct the distribution of 13 broad vegetation categories (biomes). We assess the results using estimates of potential natural vegetation from the European Vegetation Map and the Physico-Geographic Atlas of the World. We test whether anthropogenic disturbance affects reconstruction quality using land use information from the Global Land Cover data set. Results: The biomization scheme successfully predicts the broadscale patterns of vegetation across the region, including changes with elevation. The technique discriminates deserts from shrublands, the prevalence of woodlands in moister lowland sites, and the presence of temperate and mixed forests at higher elevations. Quantitative assessment of the reconstructions is less satisfactory: the biome is predicted correctly at 44% of the sites in Europe and 33% of the sites overall. The low success rate is not a reflection of anthropogenic impacts: only 33% of the samples are correctly assigned after the removal of sites in anthropogenically altered environments. Open vegetation is less successfully predicted (33%) than forest types (73%), reflecting the under-representation of herbaceous taxa in pollen assemblages and the impact of long-distance pollen transport into open environments. Samples from small basins (
- Published
- 2018
17. (Organisat.rice.eur.) Human adaptation to environmental constraints on the Iranian Plateau since the Late Glacial: A view from the Zagros mountains in the past and present
- Author
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Mashkour, M., Djamali, M., Archéozoologie, archéobotanique : sociétés, pratiques et environnements (AASPE), Muséum national d'Histoire naturelle (MNHN)-Centre National de la Recherche Scientifique (CNRS), Institut méditerranéen de biodiversité et d'écologie marine et continentale (IMBE), Avignon Université (AU)-Aix Marseille Université (AMU)-Institut de recherche pour le développement [IRD] : UMR237-Centre National de la Recherche Scientifique (CNRS), and LABORATOIRE INTERNATIONAL ASSOCIÉ 'HAOMA'- INEE- CNRS
- Subjects
[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory ,[SDE.MCG]Environmental Sciences/Global Changes ,[SDE.BE]Environmental Sciences/Biodiversity and Ecology - Abstract
International audience
- Published
- 2017
18. Hydroclimatic changes in Iran, during the Lateglacial/Holocene transition, based on chironomid analysis: Comparison of records from Lake Neor (NW Iran) and Lake Arjan (SW Iran)
- Author
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Aubert, C, Djamali, M., Guibal, F., Lahijani, H., Naderi Beni, A., Beaulieu JL, de, Pourmand, A., Sharifi, A., Thiéry, A, Ponel, P., Gandouin, E., Institut méditerranéen de biodiversité et d'écologie marine et continentale (IMBE), Centre National de la Recherche Scientifique (CNRS)-Institut de recherche pour le développement [IRD] : UMR237-Aix Marseille Université (AMU)-Avignon Université (AU), Iranian National Institute for Oceanography, Ferdowsi University of Mashhad, Division of Marine Geology & Geophysics, University of Miami, University of Miami [Coral Gables], Avignon Université (AU)-Aix Marseille Université (AMU)-Institut de recherche pour le développement [IRD] : UMR237-Centre National de la Recherche Scientifique (CNRS), and Ferdowsi University of Mashhad (FUM)
- Subjects
[SDE]Environmental Sciences ,ComputingMilieux_MISCELLANEOUS - Abstract
International audience
- Published
- 2017
19. Pollen-derived biomes in the Eastern Mediterranean-Black Sea-Caspian-Corridor
- Author
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Marinova, E, Harrison, SP, Bragg, F, Connor, S, de Laet, V, Leroy, SAG, Mudie, P, Atanassova, J, Bozilova, E, Caner, H, Cordova, C, Djamali, M, Filipova-Marinova, M, Gerasimenko, N, Jahns, S, Kouli, K, Kotthoff, U, Kvavadze, E, Lazarova, M, Novenko, E, Ramezani, E, Roepke, A, Shumilovskikh, L, Tantau, I, Tonkov, S, Marinova, E, Harrison, SP, Bragg, F, Connor, S, de Laet, V, Leroy, SAG, Mudie, P, Atanassova, J, Bozilova, E, Caner, H, Cordova, C, Djamali, M, Filipova-Marinova, M, Gerasimenko, N, Jahns, S, Kouli, K, Kotthoff, U, Kvavadze, E, Lazarova, M, Novenko, E, Ramezani, E, Roepke, A, Shumilovskikh, L, Tantau, I, and Tonkov, S
- Abstract
AIM: To evaluate the biomization technique for reconstructing past vegetation in the Eastern Mediterranean–Black Sea–Caspian‐Corridor using an extensive modern pollen data set and comparing reconstructions to potential vegetation and observed land cover data. LOCATION: The region between 28–48°N and 22–62°E. METHODS: We apply the biomization technique to 1,387 modern pollen samples, representing 1,107 entities, to reconstruct the distribution of 13 broad vegetation categories (biomes). We assess the results using estimates of potential natural vegetation from the European Vegetation Map and the Physico‐Geographic Atlas of the World. We test whether anthropogenic disturbance affects reconstruction quality using land use information from the Global Land Cover data set. RESULTS: The biomization scheme successfully predicts the broadscale patterns of vegetation across the region, including changes with elevation. The technique discriminates deserts from shrublands, the prevalence of woodlands in moister lowland sites, and the presence of temperate and mixed forests at higher elevations. Quantitative assessment of the reconstructions is less satisfactory: the biome is predicted correctly at 44% of the sites in Europe and 33% of the sites overall. The low success rate is not a reflection of anthropogenic impacts: only 33% of the samples are correctly assigned after the removal of sites in anthropogenically altered environments. Open vegetation is less successfully predicted (33%) than forest types (73%), reflecting the under‐representation of herbaceous taxa in pollen assemblages and the impact of long‐distance pollen transport into open environments. Samples from small basins (<1 km²) are more likely to be reconstructed accurately, with 58% of the sites in Europe and 66% of all sites correctly predicted, probably because they sample an appropriate pollen source area to reflect regional vegetation patterns in relatively heterogeneous landscapes. While methodological biase
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- 2018
20. Palaeoenvironment and geological evolution of a late Quaternary lacustrine-palustrine carbonate complex: Zaranda Basin, Saveh, Central Iran
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DJAMALI M, ESU D, GLIOZZI E, OKHRAVI R, SOULIÉ-MÄRSCHE I, Djamali, M, Esu, D, Gliozzi, E, Okhravi, R, and SOULIÉ-MÄRSCHE, I
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palustrine ,Lacustrine carbonate ,Late Quaternary - Abstract
The continental carbonate deposits of the Zarand Basin were deposited within an intra-continental strike-slip basin situated in the northwestern corner of central Iran. They consist of distal alluvial mudstones to marlstones, carbonate pond deposits, carbonate and siliciclastic-infilled channels, and lacustrine carbonates deposited within a distal alluvial–lacustrine–palustrine complex. Both sedimentological and palaeontological evidence suggest that these sediments mostly formed within an open hydrological system. The common presence of root traces, greyish green mudstones, calcareous nodulisation, mottling, and desiccation breccias indicate a palustrine setting. The carbonate deposits of the Zarand Basin were formed under an overall semi-arid climate but periods of more aridity characterised by extensive calcretization can be distinguished in the stratigraphical sections. Both tectonics and climate have contributed in controlling the sedimentation of the Zarand Basin. Archaeological and geomorphological evidence provides a unique sub-recent analogue for ancient palustrine limestones developed within an intra-continental basin under a semi-arid climatic regime. The combination of geological and archaeological data and their comparison with historical documents show that the socalled historical lake of Saveh was the remnant of the more ancient wetland system which dominated the Zarand region during the late Quaternary.
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- 2006
21. 7300 years of vegetation history and climate for NW Malta: a Holocene perspective
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Gambin, B., primary, Andrieu-Ponel, V., additional, Médail, F., additional, Marriner, N., additional, Peyron, O., additional, Montade, V., additional, Gambin, T., additional, Morhange, C., additional, Belkacem, D., additional, and Djamali, M., additional
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- 2016
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22. 7300 years of vegetation history and climate for NW Malta: a Holocene perspective
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Gambin, B., primary, Andrieu-Ponel, V., additional, Médail, F., additional, Marriner, N., additional, Peyron, O., additional, Montade, V., additional, Gambin, T., additional, Morhange, C., additional, Belkacem, D., additional, and Djamali, M., additional
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- 2015
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23. A priori metrics to select best training dataset of top-oil temperature models of power transformers
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Djamali, M., primary and Tenbohlen, S., additional
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- 2014
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24. Caspian sea-level changes during the last millennium: historical and geological evidence from the south Caspian Sea
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Naderi Beni, A., primary, Lahijani, H., additional, Mousavi Harami, R., additional, Arpe, K., additional, Leroy, S. A. G., additional, Marriner, N., additional, Berberian, M., additional, Andrieu-Ponel, V., additional, Djamali, M., additional, Mahboubi, A., additional, and Reimer, P. J., additional
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- 2013
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25. Caspian sea-level changes during the last millennium: historical and geological evidence from the south Caspian Sea.
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Beni, A. Naderi, Lahijani, H., Harami, R. Mousavi, Arpe, K., Leroy, S. A. G., Marriner, N., Berberian, M., Andrieu-Ponel, V., Djamali, M., Mahboubi, A., and Reimer, P. J.
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GEOLOGY ,INFORMATION theory ,SEDIMENTS ,CLIMATOLOGY ,SEISMOLOGY - Abstract
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 -21 m (and extra rises due to manmade river avulsion), with a -28 m 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. [ABSTRACT FROM AUTHOR]
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- 2013
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26. Cyclosporin A-induced functional and morphological changes in pilocarpine treated rat submandibular glands
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Dehpour, A. R., Nouhnejad, P., Mousavizadeh, K., Ghafourifar, P., Djamali, M., and Borhanimoghadam, B.
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- 1996
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27. Synthese und Eigenschaften eines Celluloseaustauschers mit Diaminodibenzo-18-Krone-6 als Ankergruppe
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Djamali, M. G., primary, Burba, P., additional, and Lieser, K. H., additional
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- 1980
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28. Darstellung und eigenschaften eines ionenaustauschers mit einem 1,3-diketon als Ankergruppe auf der Basis von Polystyrol
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Djamali, M. G., primary and Lieser, K. H., additional
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- 1983
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29. Synthese und Eigenschaften eines chelatbildenden Austauschers mit N,N′-bis-(2-hydroxybenzyl)-ethylendiamin als Ankergruppe auf der Basis von Polystyrol
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Djamali, M. G., primary and Lieser, K. H., additional
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- 1983
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30. Endoplasmic Reticulum Stress-Induced Autophagy Provides Cytoprotection from Chemical Hypoxia and Oxidant Injury and Ameliorates Renal Ischemia-Reperfusion Injury.
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Bhavya B Chandrika, Cheng Yang, Yang Ou, Xiaoke Feng, Djamali Muhoza, Alexandrea F Holmes, Sue Theus, Sarika Deshmukh, Randy S Haun, and Gur P Kaushal
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Medicine ,Science - Abstract
We examined whether endoplasmic reticulum (ER) stress-induced autophagy provides cytoprotection from renal tubular epithelial cell injury due to oxidants and chemical hypoxia in vitro, as well as from ischemia-reperfusion (IR) injury in vivo. We demonstrate that the ER stress inducer tunicamycin triggers an unfolded protein response, upregulates ER chaperone Grp78, and activates the autophagy pathway in renal tubular epithelial cells in culture. Inhibition of ER stress-induced autophagy accelerated caspase-3 activation and cell death suggesting a pro-survival role of ER stress-induced autophagy. Compared to wild-type cells, autophagy-deficient MEFs subjected to ER stress had enhanced caspase-3 activation and cell death, a finding that further supports the cytoprotective role of ER stress-induced autophagy. Induction of autophagy by ER stress markedly afforded cytoprotection from oxidants H2O2 and tert-Butyl hydroperoxide and from chemical hypoxia induced by antimycin A. In contrast, inhibition of ER stress-induced autophagy or autophagy-deficient cells markedly enhanced cell death in response to oxidant injury and chemical hypoxia. In mouse kidney, similarly to renal epithelial cells in culture, tunicamycin triggered ER stress, markedly upregulated Grp78, and activated autophagy without impairing the autophagic flux. In addition, ER stress-induced autophagy markedly ameliorated renal IR injury as evident from significant improvement in renal function and histology. Inhibition of autophagy by chloroquine markedly increased renal IR injury. These studies highlight beneficial impact of ER stress-induced autophagy in renal ischemia-reperfusion injury both in vitro and in vivo.
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- 2015
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31. The Eurasian Modern Pollen Database (EMPD), version 2
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Juliana Atanassova, Christine M. Åkesson, Piotr Kołaczek, Marco Zanon, Kari Loe Hjelle, Lyudmila S. Shumilovskikh, Heikki Seppä, Nathalie Combourieu-Nebout, Vachel A. Carter, James Edward Schofield, Krystyna Milecka, Iria García-Moreiras, Takeshi Nakagawa, Walter Finsinger, Willy Tinner, Castor Muñoz Sobrino, Anne Birgitte Nielsen, José Antonio López-Sáez, Elena Marinova, Philipp Stojakowits, Tatiana G. Antipina, Silvia Sabariego Ruiz, Roman Abegglen, Vlasta Jankovská, Oksana G. Zanina, Mariusz Gałka, Arsenii T. Galimov, Maria Papadopoulou, Manfred Rösch, Kevin J. Edwards, Patricia L. Fall, Basil A. S. Davis, Philipp Sommer, Elissaveta Bozilova, Ulrike Herzschuh, Verushka Valsecchi, Natalia Ryabogina, Ikuko Kitaba, Elena Novenko, Michelle Leydet, Anna Pędziszewska, Nata K. Panova, Almut Mrotzek, Donatella Magri, Eleonora Clo, Isabelle Matthias, R. Scott Anderson, Tatiana Blyakharchuk, Kazimierz Tobolski, Vincent Lebreton, Leanne N. Phelps, Irina G. Gvozdeva, André F. Lotter, Nina I. Belyanina, Assunta Florenzano, William J. Fletcher, Ioan Tantau, Suzanne A.G. Leroy, Roxana Grindean, Normunds Stivrins, Elena G. Lapteva, Francisca Alba-Sánchez, J. Sakari Salonen, Tatiana I. Petrenko, Tatyana V. Sapelko, Angelica Feurdean, Anna Maria Mercuri, Yuri A. Mikishin, G Furlanetto, Susanne Jahns, Cesare Ravazzi, Helena Svobodova Svitavska, Anastasia Mavridou, Carlo Alessandro Montanari, Jose Manuel Mesa-Fernández, Sampson Panajiotidis, Ruth Beer, Stéphanie Desprat, Federico Di Rita, María J. Ramos-Román, Emna Gaceur, Joanna Święta-Musznicka, Małgorzata Latałowa, Thomas Giesecke, Olga K. Borisova, Galina Bukreeva, M. Jane Bunting, Manuel Chevalier, Achille Mauri, Maria Angela Guido, Darya A. Lopatina, César Morales-Molino, Spassimir Tonkov, Marcelina Zimny, Monika Karpińska-Kołaczek, Sergey Ivanov, Gonzalo Jiménez-Moreno, Daniele Colombaroli, Morteza Djamali, Heather S. Pardoe, Olga D. Naidina, Margarita Tsakiridou, Université de Lausanne, Swiss National Science Foundation, López Sáez, José Antonio [0000-0002-3122-2744], Institute of Earth Surface Dynamics [Lausanne], Université de Lausanne = University of Lausanne (UNIL), Institut des Sciences de l'Evolution de Montpellier (UMR ISEM), Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-École Pratique des Hautes Études (EPHE), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Montpellier (UM)-Institut de recherche pour le développement [IRD] : UR226-Centre National de la Recherche Scientifique (CNRS), Charles University [Prague] (CU), Lomonosov Moscow State University (MSU), Oeschger Centre for Climate Change Research (OCCR), University of Bern, Histoire naturelle de l'Homme préhistorique (HNHP), Muséum national d'Histoire naturelle (MNHN)-Université de Perpignan Via Domitia (UPVD)-Centre National de la Recherche Scientifique (CNRS), Environnements et Paléoenvironnements OCéaniques (EPOC), Observatoire aquitain des sciences de l'univers (OASU), Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-École Pratique des Hautes Études (EPHE), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Centre National de la Recherche Scientifique (CNRS), Institut méditerranéen de biodiversité et d'écologie marine et continentale (IMBE), Avignon Université (AU)-Aix Marseille Université (AMU)-Institut de recherche pour le développement [IRD] : UMR237-Centre National de la Recherche Scientifique (CNRS), Department of physical chemistry, Uppsala University, Senckenberg biodiversität und klima forschungszentrum (BIK-F), Forschungsinstitut Senckenberg (SGN), Laboratorio di Palinologia e Paleobotanica, Adam Mickiewicz University in Poznań (UAM), Department of Palynology and Climate Dynamics, Georg-August-University = Georg-August-Universität Göttingen, Alfred Wegener Institute for Polar and Marine Research (AWI), Natural History Collections, University of Bergen (UiB)-University of Bergen (UiB), A.F. Ioffe Physical-Technical Institute, Russian Academy of Sciences [Moscow] (RAS), Brandenburgisches Landesamt für Denkmalpflege und Archäologisches Landesmuseum, Universidad de Granada = University of Granada (UGR), Institute of Geoecology and Geoinformation, Department of Plant Ecology, Gdansk University, University of Gdańsk (UG), Laboratoire de Recherche en Sciences Humaines (Lares-Las), Université de Rennes 2 (UR2), Dipartimento di biologia ambientale, Università degli Studi di Roma 'La Sapienza' = Sapienza University [Rome] (UNIROMA), Department of Botany, Sofia University 'St. Kliment Ohridski', NASA Ames Research Center (ARC), Department of Biogeography and Palaeoecology, Institut Méditerranéen d'Ecologie et de Paléoécologie (IMEP), Université Paul Cézanne - Aix-Marseille 3-Université de Provence - Aix-Marseille 1-Avignon Université (AU)-Centre National de la Recherche Scientifique (CNRS), Lund University [Lund], Laboratoire d'Informatique, Systèmes, Traitement de l'Information et de la Connaissance (LISTIC), Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry]), CNR-IDPA, Dipartimento di Scienze dell'Ambiente e del Territorio, Università degli Studi di Milano-Bicocca = University of Milano-Bicocca (UNIMIB), Department of Physics and Astronomy [Turku], University of Turku, Helsingin yliopisto = Helsingfors universitet = University of Helsinki, Department of Geography [Riga], Софийски университет = Sofia University, University of Portsmouth, Aix Marseille Université (AMU), Avignon Université (AU), López Sáez, José Antonio, Davis, B, Chevalier, M, Sommer, P, Carter, V, Finsinger, W, Mauri, A, Phelps, L, Zanon, M, Abegglen, R, Akesson, C, Alba-Sanchez, F, Scott Anderson, R, Antipina, T, Atanassova, J, Beer, R, Belyanina, N, Blyakharchuk, T, Borisova, O, Bozilova, E, Bukreeva, G, Jane Bunting, M, Clo, E, Colombaroli, D, Combourieu-Nebout, N, Desprat, S, Di Rita, F, Djamali, M, Edwards, K, Fall, P, Feurdean, A, Fletcher, W, Florenzano, A, Furlanetto, G, Gaceur, E, Galimov, A, Galka, M, Garcia-Moreiras, I, Giesecke, T, Grindean, R, Guido, M, Gvozdeva, I, Herzschuh, U, Hjelle, K, Ivanov, S, Jahns, S, Jankovska, V, Jimenez-Moreno, G, Karpinska-Kolaczek, M, Kitaba, I, Kolaczek, P, Lapteva, E, Latalowa, M, Lebreton, V, Leroy, S, Leydet, M, Lopatina, D, Lopez-Saez, J, Lotter, A, Magri, D, Marinova, E, Matthias, I, Mavridou, A, Mercuri, A, Mesa-Fernandez, J, Mikishin, Y, Milecka, K, Montanari, C, Morales-Molino, C, Mrotzek, A, Sobrino, C, Naidina, O, Nakagawa, T, Nielsen, A, Novenko, E, Panajiotidis, S, Panova, N, Papadopoulou, M, Pardoe, H, Pedziszewska, A, Petrenko, T, Ramos-Roman, M, Ravazzi, C, Rosch, M, Ryabogina, N, Ruiz, S, Sakari Salonen, J, Sapelko, T, Schofield, J, Seppa, H, Shumilovskikh, L, Stivrins, N, Stojakowits, P, Svitavska, H, Swieta-Musznicka, J, Tantau, I, Tinner, W, Tobolski, K, Tonkov, S, Tsakiridou, M, Valsecchi, V, Zanina, O, Zimny, M, University of St Andrews. School of Geography & Sustainable Development, University of St Andrews. Environmental Change Research Group, Department of Geosciences and Geography, Université de Lausanne (UNIL), École pratique des hautes études (EPHE), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Montpellier (UM)-Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-Centre National de la Recherche Scientifique (CNRS)-Institut de recherche pour le développement [IRD] : UR226, Department of Botany, Faculty of Science, Charles University, Université Sciences et Technologies - Bordeaux 1-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Sciences et Technologies - Bordeaux 1-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-École pratique des hautes études (EPHE), Georg-August-University [Göttingen], Departamento de Estratigrafía y Paleontología, Universidad de Granada, Universidad de Granada (UGR), Université de Rennes (UNIV-RENNES)-Université de Rennes (UNIV-RENNES), Università degli Studi di Roma 'La Sapienza' = Sapienza University [Rome], Sofia University 'Sv. Kliment Ohridski', Université Paul Cézanne - Aix-Marseille 3-Centre National de la Recherche Scientifique (CNRS)-Avignon Université (AU)-Université de Provence - Aix-Marseille 1, Department of Geology, Lund University, Sölvegatan 12, SE-22362 Lund, Sweden, Università degli Studi di Milano-Bicocca [Milano] (UNIMIB), University of Helsinki, and University of Sofia
- Subjects
0106 biological sciences ,LAKE CONSTANCE REGION ,Palynology Palaeoecology Palaeoclimatology ,010504 meteorology & atmospheric sciences ,HUMAN IMPACT ,recent pollen deposition ,580 Plants (Botany) ,medicine.disease_cause ,01 natural sciences ,2417.10 Paleobotánica ,[SDV.SA.SF]Life Sciences [q-bio]/Agricultural sciences/Silviculture, forestry ,ddc:550 ,SURFACE POLLEN ,SOUTHERN NORWAY ,SDG 13 - Climate Action ,ComputingMilieux_MISCELLANEOUS ,lcsh:Environmental sciences ,SDG 15 - Life on Land ,lcsh:GE1-350 ,0303 health sciences ,CLIMATE-CHANGE ,GE ,APUSENI NATURAL PARK ,lcsh:QE1-996.5 ,Foundation (engineering) ,European pollen database ,[SDV.BV.BOT]Life Sciences [q-bio]/Vegetal Biology/Botanics ,[SDV.BIBS]Life Sciences [q-bio]/Quantitative Methods [q-bio.QM] ,Europe ,LAST GLACIAL MAXIMUM ,Geography ,NORTHERN IBERIAN PLATEAU ,pollen ,GE Environmental Sciences ,1171 Geosciences ,010506 paleontology ,[SDE.MCG]Environmental Sciences/Global Changes ,Earth and Planetary Sciences(all) ,Library science ,Climate change ,[SDU.STU]Sciences of the Universe [physics]/Earth Sciences ,010603 evolutionary biology ,neotoma ,03 medical and health sciences ,Eurasian Modern Pollen Database ,2502.05 Paleoclimatología ,Pollen ,medicine ,SIERRA-NEVADA ,[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces, environment ,0105 earth and related environmental sciences ,030304 developmental biology ,Botánica ,HOLOCENE VEGETATION HISTORY ,DAS ,15. Life on land ,2416.03 Palinología ,[SDE.ES]Environmental Sciences/Environmental and Society ,lcsh:Geology ,[SDU]Sciences of the Universe [physics] ,MCP ,General Earth and Planetary Sciences ,[SDE.BE]Environmental Sciences/Biodiversity and Ecology - Abstract
The Eurasian (née European) Modern Pollen Database (EMPD) was established in 2013 to provide a public database of high-quality modern pollen surface samples to help support studies of past climate, land cover, and land use using fossil pollen. The EMPD is part of, and complementary to, the European Pollen Database (EPD) which contains data on fossil pollen found in Late Quaternary sedimentary archives throughout the Eurasian region. The EPD is in turn part of the rapidly growing Neotoma database, which is now the primary home for global palaeoecological data. This paper describes version 2 of the EMPD in which the number of samples held in the database has been increased by 60% from 4826 to 8134. Much of the improvement in data coverage has come from northern Asia, and the database has consequently been renamed the Eurasian Modern Pollen Database to reflect this geographical enlargement. The EMPD can be viewed online using a dedicated map-based viewer at https://empd2.github.io and downloaded in a variety of file formats at https: //doi.pangaea.de/10.1594/PANGAEA.909130 (Chevalier et al., 2019)., Swiss National Science Foundation (SNSF) 200021_169598, University of Lausanne
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- 2020
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32. Alteration of the metabolite interconversion enzyme in sperm and Sertoli cell of non-obstructive azoospermia: a microarray data and in-silico analysis.
- Author
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Hashemi Karoii D, Baghaei H, Abroudi AS, Djamali M, Hasani Mahforoozmahalleh Z, Azizi H, and Skutella T
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- Male, Humans, Computer Simulation, Computational Biology methods, Gene Expression Profiling, Adult, Azoospermia genetics, Azoospermia metabolism, Azoospermia pathology, Sertoli Cells metabolism, Spermatozoa metabolism
- Abstract
Numerous variables that regulate the metabolism of Sertoli cells and sperm have been identified, one of which is sex steroid hormones. These hormones play a vital role in maintaining energy homeostasis, influencing the overall metabolic balance of the human body. The proper functioning of the reproductive system is closely linked to energy status, as the reproductive axis responds to metabolic signals. The aim of this study was to investigate the gene expression patterns of metabolite interconversion enzymes in testicular cells (Sertoli cells and spermatogonia) of non-obstructive azoospermia (NOA) patients, as compared to normal controls, to understand the molecular mechanisms contributing to NOA. We used microarray and bioinformatics techniques to analyze 2912 genes encoding metabolite interconversion enzymes, including methyltransferase, monooxygenase, transmembrane reductase, and phosphohydrolase, in both testicular cells and normal samples. In sperm, the upregulation of MOXD1, ACAD10, PCYT1A, ARG1, METTL6, GPLD1, MAOA, and CYP46A1 was observed, while ENTPD2, CPT1C, ADC, and CYB5B were downregulated. Similarly, in the Sertoli cells of three NOA patients, RPIA, PIK3C3, LYPLA2, CA11, MBOAT7, and HDHD2 were upregulated, while NAA25, MAN2A1, CYB561, PNPLA5, RRM2, and other genes were downregulated. Using STRING and Cytoscape, we predicted the functional and molecular interactions of these proteins and identified key hub genes. Pathway enrichment analysis highlighted significant roles for G1/S-specific transcription, pyruvate metabolism, and citric acid metabolism in sperm, and the p53 signaling pathway and folate metabolism in Sertoli cells. Additionally, Weighted Gene Co-expression Network Analysis (WGCNA) and single-cell RNA sequencing (scRNA-seq) were performed to validate these findings, revealing significant alterations in gene expression and cellular distribution in NOA patients. Together, these results provide new insights into the molecular mechanisms underlying NOA and identify potential therapeutic targets., (© 2024. The Author(s).)
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- 2024
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33. Exploring the interaction between immune cells in the prostate cancer microenvironment combining weighted correlation gene network analysis and single-cell sequencing: An integrated bioinformatics analysis.
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Hashemi Karoii D, Bavandi S, Djamali M, and Abroudi AS
- Abstract
Background: The rise of treatment resistance and variability across malignant profiles has made precision oncology an imperative in today's medical landscape. Prostate cancer is a prevalent form of cancer in males, characterized by significant diversity in both genomic and clinical characteristics. The tumor microenvironment consists of stroma, tumor cells, and various immune cells. The stromal components and tumor cells engage in mutual communication and facilitate the development of a low-oxygen and pro-cancer milieu by producing cytokines and activating pro-inflammatory signaling pathways., Methods: In order to discover new genes associated with tumor cells that interact and facilitate a hypoxic environment in prostate cancer, we conducted a cutting-edge bioinformatics investigation. This included analyzing high-throughput genomic datasets obtained from the cancer genome atlas (TCGA)., Results: A combination of weighted gene co-expression network analysis and single-cell sequencing has identified nine dysregulated immune hub genes (AMACR, KCNN3, MME, EGFR, FLT1, GDF15, KDR, IGF1, and KRT7) that are believed to have significant involvement in the biological pathways involved with the advancement of prostate cancer enviriment. In the prostate cancer environment, we observed the overexpression of GDF15 and KRT7 genes, as well as the downregulation of other genes. Additionally, the cBioPortal platform was used to investigate the frequency of alterations in the genes and their effects on the survival of the patients. The Kaplan-Meier survival analysis indicated that the changes in the candidate genes were associated with a reduction in the overall survival of the patients., Conclusions: In summary, the findings indicate that studying the genes and their genomic changes may be used to develop precise treatments for prostate cancer. This approach involves early detection and targeted therapy., (© 2024. The Author(s).)
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- 2024
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34. Nile waterscapes facilitated the construction of the Giza pyramids during the 3rd millennium BCE.
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Sheisha H, Kaniewski D, Marriner N, Djamali M, Younes G, Chen Z, El-Qady G, Saleem A, Véron A, and Morhange C
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- Egypt, History, Ancient, Construction Industry history, Rivers
- Abstract
The pyramids of Giza originally overlooked a now defunct arm of the Nile. This fluvial channel, the Khufu branch, enabled navigation to the Pyramid Harbor complex but its precise environmental history is unclear. To fill this knowledge gap, we use pollen-derived vegetation patterns to reconstruct 8,000 y of fluvial variations on the Giza floodplain. After a high-stand level concomitant with the African Humid Period, our results show that Giza's waterscapes responded to a gradual insolation-driven aridification of East Africa, with the lowest Nile levels recorded at the end of the Dynastic Period. The Khufu branch remained at a high-water level (∼40% of its Holocene maximum) during the reigns of Khufu, Khafre, and Menkaure, facilitating the transportation of construction materials to the Giza Pyramid Complex.
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- 2022
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35. Climate change: A driver of future conflicts in the Persian Gulf Region?
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Naderi Beni A, Marriner N, Sharifi A, Azizpour J, Kabiri K, Djamali M, and Kirman A
- Abstract
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., Competing Interests: The authors declare no conflict of interest., (© 2021 Published by Elsevier Ltd.)
- Published
- 2021
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36. A Review of C 4 Plants in Southwest Asia: An Ecological, Geographical and Taxonomical Analysis of a Region With High Diversity of C 4 Eudicots.
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Rudov A, Mashkour M, Djamali M, and Akhani H
- Abstract
Southwest Asia is climatically and topographically a highly diverse region in the xeric belt of the Old World. Its diversity of arid habitats and climatic conditions acted as an important area for the evolution and diversification of up to 20 (of 38 known) independent Eudicot C
4 origins. Some of these lineages present unique evolutionary strategies like single-cell functioning C4 and C3 -C4 switching mechanisms. The high diversity of C4 taxa in Southwest (SW) Asia is also related to the presence of seven phytogeographic zones including the Irano-Turanian region as a center of diversification of many Caryophyllales lineages and the Somali-Masai region (Southern Oman and Yemen) as a center of diversification for C4 Monocots. Nevertheless, the C4 flora of SW Asia has not received detailed attention. This paper presents a comprehensive review of all known C4 species in the area based on a literature survey, own floristic observations, as well as taxonomic, phylogenetic and herbarium data, and δ13 C-isotope ratio analysis. The resulting checklist includes a total number of 923 (861 native, of which 141 endemic, and 62 introduced) C4 species, composed of 350 Eudicots and 509 Monocots, most of which are therophytic and hemicryptophytic xerophytes with pluriregional and Irano-Turanian distribution. Two hundred thirty-nine new δ13 C-isotope ratios of C4 and C3 plants, as well as some taxonomic changes are presented. An analysis of the distribution of the three main C4 plant families (Chenopodiaceae, Poaceae, and Cyperaceae) in the region in relation to climatic variables indicates that the increase of C4 species follows more or less a latitudinal gradient similar to global patterns, while separate taxonomic groups seem to depend on specific factors as continentality (Chenopodiaceae), average annual temperature (Cyperaceae), and the presence of summer precipitation (Poaceae). An increase of C4 Eudicots in W-E direction even in similar longitudinal belts is explained by a combination of edaphic and climatic conditions. The provided data should encourage a deeper interest in the evolution of C4 lineages in SW Asia and their adaptation to ecological and climatical conditions and awaken interest in the importance of local C4 crops, the conservation of threatened C4 taxa, and awareness of human impacts on the rapid environmental changes in the region., (Copyright © 2020 Rudov, Mashkour, Djamali and Akhani.)- Published
- 2020
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37. 20,000 years of societal vulnerability and adaptation to climate change in southwest Asia.
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Jones MD, Abu-Jaber N, AlShdaifat A, Baird D, Cook BI, Cuthbert MO, Dean JR, Djamali M, Eastwood W, Fleitmann D, Haywood A, Kwiecien O, Larsen J, Maher LA, Metcalfe SE, Parker A, Petrie CA, Primmer N, Richter T, Roberts N, Roe J, Tindall JC, Ünal-İmer E, and Weeks L
- Abstract
The Fertile Crescent, its hilly flanks and surrounding drylands has been a critical region for studying how climate has influenced societal change, and this review focuses on the region over the last 20,000 years. The complex social, economic, and environmental landscapes in the region today are not new phenomena and understanding their interactions requires a nuanced, multidisciplinary understanding of the past. This review builds on a history of collaboration between the social and natural palaeoscience disciplines. We provide a multidisciplinary, multiscalar perspective on the relevance of past climate, environmental, and archaeological research in assessing present day vulnerabilities and risks for the populations of southwest Asia. We discuss the complexity of palaeoclimatic data interpretation, particularly in relation to hydrology, and provide an overview of key time periods of palaeoclimatic interest. We discuss the critical role that vegetation plays in the human-climate-environment nexus and discuss the implications of the available palaeoclimate and archaeological data, and their interpretation, for palaeonarratives of the region, both climatically and socially. We also provide an overview of how modelling can improve our understanding of past climate impacts and associated change in risk to societies. We conclude by looking to future work, and identify themes of "scale" and "seasonality" as still requiring further focus. We suggest that by appreciating a given locale's place in the regional hydroscape, be it an archaeological site or palaeoenvironmental archive, more robust links to climate can be made where appropriate and interpretations drawn will demand the resolution of factors acting across multiple scales. This article is categorized under:Human Water > Water as Imagined and RepresentedScience of Water > Water and Environmental ChangeWater and Life > Nature of Freshwater Ecosystems., Competing Interests: The authors have declared no conflicts of interest for this article., (© 2019 The Authors. WIREs Water published by Wiley Periodicals, Inc.)
- Published
- 2019
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38. Past and future global transformation of terrestrial ecosystems under climate change.
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Nolan C, Overpeck JT, Allen JRM, Anderson PM, Betancourt JL, Binney HA, Brewer S, Bush MB, Chase BM, Cheddadi R, Djamali M, Dodson J, Edwards ME, Gosling WD, Haberle S, Hotchkiss SC, Huntley B, Ivory SJ, Kershaw AP, Kim SH, Latorre C, Leydet M, Lézine AM, Liu KB, Liu Y, Lozhkin AV, McGlone MS, Marchant RA, Momohara A, Moreno PI, Müller S, Otto-Bliesner BL, Shen C, Stevenson J, Takahara H, Tarasov PE, Tipton J, Vincens A, Weng C, Xu Q, Zheng Z, and Jackson ST
- Subjects
- Biodiversity, Climate Change
- Abstract
Impacts of global climate change on terrestrial ecosystems are imperfectly constrained by ecosystem models and direct observations. Pervasive ecosystem transformations occurred in response to warming and associated climatic changes during the last glacial-to-interglacial transition, which was comparable in magnitude to warming projected for the next century under high-emission scenarios. We reviewed 594 published paleoecological records to examine compositional and structural changes in terrestrial vegetation since the last glacial period and to project the magnitudes of ecosystem transformations under alternative future emission scenarios. Our results indicate that terrestrial ecosystems are highly sensitive to temperature change and suggest that, without major reductions in greenhouse gas emissions to the atmosphere, terrestrial ecosystems worldwide are at risk of major transformation, with accompanying disruption of ecosystem services and impacts on biodiversity., (Copyright © 2018 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. No claim to original U.S. Government Works.)
- Published
- 2018
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39. A note on the biogeographical origin of the brine shrimp Artemia urmiana Günther, 1899 from Urmia Lake, Iran.
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Eimanifar A, Asem A, Djamali M, and Wink M
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- Animal Distribution, Animal Structures anatomy & histology, Animal Structures growth & development, Animals, Artemia anatomy & histology, Artemia genetics, Artemia growth & development, Body Size, Ecosystem, Female, Iran, Lakes chemistry, Male, Organ Size, Phylogeny, Artemia classification
- Abstract
The brine shrimp Artemia urmiana, an abundant inhabitant of the hypersaline Urmia Lake in northwestern Iran, has recently been described from Lake Koyashskoe, also a shallow hypersaline lake that is located on the Black Sea coast of the Crimean Peninsula (Ukraine). This discovery has questioned the endemicity of A. urmiana in Urmia Lake and has also brought into question the biogeographical origin of this species. In the present study, we combined recent genetic divergence data (mtDNA-COI) with palaeoecological evidence to address the biogeographical origin of A. urmiana. Calibration of the molecular clock of the COI region was set by assigning the age of the micro-crustacean Daphnia pulex minimally at 145 Mya. The divergence age of A. urmiana in Urmia Lake dates back to 383,000 years, whereas Ukrainian Artemia reflects a very young populations that diverged about 196,000 years ago. Palaeoecological evidence suggests that the age of the major habitat of A. urmiana i.e. Urmia Lake goes back to the Tertiary Period while the Ukranian habitats of the species are very young, by virtue of geological features of the Holocene age. We conclude that the biogeographical origin of A. urmiana is outside of Europe and the current state of knowledge strongly suggests that Urmia Lake has been the major source of its expansion into its modern habitats in Europe.
- Published
- 2016
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40. [Pollen analysis from two littoral marshes (Bourdim and Garaat El-Ouez) in the El-Kala wet complex (North-East Algeria). Lateglacial and Holocene history of Algerian vegetation].
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Benslama M, Andrieu-Ponel V, Guiter F, Reille M, de Beaulieu JL, Migliore J, and Djamali M
- Subjects
- Algeria, Cedrus, Climate Change, Ecosystem, Geologic Sediments analysis, History, Ancient, Pinus, Poaceae, Quercus, Radiometric Dating, Pollen chemistry, Trees growth & development, Wetlands
- Abstract
The study of two pollen sequences from El-Kala marshes allowed the reconstruction of the regional vegetation history supported by eight radiocarbon dates. Pollen assemblages from Bourdim site were dominated by local input of Alnus and Salix, while regional vegetation was characterized by scattered Quercus suber forests with a well-developed Erica arborea matorral. While the vegetation dynamics recorded at Bourdim is recent (Late Holocene), the majority of the pollen diagram from Garaat El-Ouez is contemporaneous to the Late Pleniglacial and is characterized by open woodlands with Pinus, Poaceae and several heliophilous herbs. The significant values of Cedrus pollen identified in this period indicate that the region of El-Kala most probably played the role of a refugium for this tree., (Copyright © 2010 Académie des sciences. Published by Elsevier SAS. All rights reserved.)
- Published
- 2010
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