Fresh Fields and Pastures New Papers Presented in Honor of Andrew M.T
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The Late Neolithic Colonization of the Eastern Badia of Jordan
The Late Neolithic colonization of the Eastern Badia of Jordan 1 Gary Rollefson1, Yorke Rowan2 and Alexander Wasse Pioneering research by Betts and by Garrard in the eastern steppe and desert of Jordan demonstrated the presence of Late Neolithic (c. 7000–5000 cal BC) pastoral exploitation of this currently arid/hyper-arid region, but the scale of Late Neolithic presence in the area was difficult to assess from the reports of their surveys and excavations. Recent investigations by the Eastern Badia Archaeological Project at Wisad Pools and the Wadi al-Qattafi in the Black Desert have shown that conditions during the latter half of the 7th millennium and into the 6th, permitted substantial numbers of pastoralists to occupy substantial dwellings recurrently, in virtual village settings, for considerable amounts of time on a seasonal basis, relying heavily on the hunting of wild animals and perhaps practising opportunistic agriculture in addition to herding caprines. Keywords Late Neolithic, pastoralism, architecture, palaeoclimate, caprines Introduction The combination of high demands for farmland and The middle of the 8th millennium in the southern pasturage on unstable resources resulted in drastically Levant witnessed considerable turmoil: substantial reduced populations at some of the sites (e.g. ‘Ain 2numbers of Middle PPNB settlements in the Jordan Ghazal and Wadi Shu’eib) and the outright abandon- Valley and areas to the west were abandoned, and ment of other population centres. With population large numbers of people migrated to -
Tell Abu Suwwan, a Neolithic Site in Jordan: Preliminary Report on the 2005 and 2006 Field Seasons
Tell Abu Suwwan, A Neolithic Site in Jordan: Preliminary Report on the 2005 and 2006 Field Seasons Maysoon al-Nahar Department of Archaeology Institute of Archaeology University of Jordan Amman 11942, Jordan [email protected] Tell Abu Suwwan is the only Neolithic site excavated north of the Zarqa River in Jordan. Its architectural characteristics and the diagnostic lithic artifacts discovered at the site during the University of Jordan 2005 and 2006 field seasons, directed by the author, suggest that the site was occupied continually from the Middle Pre-Pottery Neolithic Phase B (MPPNB) to the Yarmoukian (Pottery Neolithic) period. The site was divided by the excavator into two areas—A and B. Area A yielded a few walls, plaster floors, and orange clay. Area B yielded a large square or rectangular building with three clear types of plaster floors and an orange clay area. Both Areas A and B include numerous lithics, bones, and some small finds. Based on a recent survey outward from the excavated area, the probable size of Abu Suwwan is 10.5 ha (26 acres), and it contains complex architecture with a long chronological sequence. These attributes suggest that Tell Abu Suwwan is one of the Jordanian Neolithic megasites. introduction though the site contains a distinctive architecture, it shares various similarities with several other Levan- ell Abu Suwwan is a large Neolithic site in tine Pre-Pottery Neolithic (PPN) sites, e.g., Jericho T north Jordan; it is on the east side of the old (Kenyon 1956: 69–77; 1969), Tell Ramad (de Con- Jarash–Amman highway, immediately before tenson 1971: 278–85), Tell Abu Hureyra (Moore, the turn west to Ajlun (fig. -
Hrvatski Jadranski Otoci, Otočići I Hridi
Hrvatski jadranski otoci, otočići i hridi Sika od Mondefusta, Palagruţa Mjerenja obale istoĉnog Jadrana imaju povijest; svi autori navode prvi cjelovitiji popis otoka kontraadmirala austougarske mornarice Sobieczkog (Pula, 1911.). Glavni suvremeni izvor dugo je bio odliĉni i dosad još uvijek najsustavniji pregled za cijelu jugoslavensku obalu iz godine 1955. [1955].1 Na osnovi istraţivanja skupine autora, koji su ponovo izmjerili opsege i površine hrvatskih otoka i otoĉića većih od 0,01 km2 [2004],2 u Ministarstvu mora, prometa i infrastrukture je zatim 2007. godine objavljena opseţna nova graĊa, koju sad moramo smatrati referentnom [2007].3 No, i taj pregled je manjkav, ponajprije stoga jer je namijenjen specifiĉnom administrativnom korištenju, a ne »statistici«. Drugi problem svih novijih popisa, barem onih objavljenih, jest taj da ne navode sve najmanje otoĉiće i hridi, iako ulaze u konaĉne brojke.4 Brojka 1244, koja je sada najĉešće u optjecaju, uopće nije dokumentirana.5 Osnovni izvor za naš popis je, dakle, [2007], i u graniĉnim primjerima [2004]. U napomenama ispod tablica navedena su odstupanja od tog izvora. U sljedećem koraku pregled je dopunjen podacima iz [1955], opet s obrazloţenjima ispod crte. U trećem koraku ukljuĉeno je još nekoliko dodatnih podataka s obrazloţenjem.6 1 Ante Irić, Razvedenost obale i otoka Jugoslavije. Hidrografski institut JRM, Split, 1955. 2 T. Duplanĉić Leder, T. Ujević, M. Ĉala, Coastline lengths and areas of islands in the Croatian part of the Adriatic sea determined from the topographic maps at the scale of 1:25.000. Geoadria, 9/1, Zadar, 2004. 3 Republika Hrvatska, Ministarstvo mora, prometa i infrastrukture, Drţavni program zaštite i korištenja malih, povremeno nastanjenih i nenastanjenih otoka i okolnog mora (nacrt prijedloga), Zagreb, 30.8.2007.; objavljeno na internetskoj stranici Ministarstva. -
Ch. 4. NEOLITHIC PERIOD in JORDAN 25 4.1
Borsa di studio finanziata da: Ministero degli Affari Esteri di Italia Thanks all …………. I will be glad to give my theses with all my love to my father and mother, all my brothers for their helps since I came to Italy until I got this degree. I am glad because I am one of Dr. Ursula Thun Hohenstein students. I would like to thanks her to her help and support during my research. I would like to thanks Dr.. Maysoon AlNahar and the Museum of the University of Jordan stuff for their help during my work in Jordan. I would like to thank all of Prof. Perreto Carlo and Prof. Benedetto Sala, Dr. Arzarello Marta and all my professors in the University of Ferrara for their support and help during my Phd Research. During my study in Italy I met a lot of friends and specially my colleges in the University of Ferrara. I would like to thanks all for their help and support during these years. Finally I would like to thanks the Minister of Fournier of Italy, Embassy of Italy in Jordan and the University of Ferrara institute for higher studies (IUSS) to fund my PhD research. CONTENTS Ch. 1. INTRODUCTION 1 Ch. 2. AIMS OF THE RESEARCH 3 Ch. 3. NEOLITHIC PERIOD IN NEAR EAST 5 3.1. Pre-Pottery Neolithic A (PPNA) in Near east 5 3.2. Pre-pottery Neolithic B (PPNB) in Near east 10 3.2.A. Early PPNB 10 3.2.B. Middle PPNB 13 3.2.C. Late PPNB 15 3.3. -
The Macrobotanical Evidence for Vegetation in the Near East, C. 18 000/16 000 B.C to 4 000 B.C
University of Pennsylvania ScholarlyCommons University of Pennsylvania Museum of University of Pennsylvania Museum of Archaeology and Anthropology Papers Archaeology and Anthropology 1997 The Macrobotanical Evidence for Vegetation in the Near East, c. 18 000/16 000 B.C to 4 000 B.C. Naomi F. Miller University of Pennsylvania, [email protected] Follow this and additional works at: https://repository.upenn.edu/penn_museum_papers Part of the Near Eastern Languages and Societies Commons Recommended Citation Miller, N. F. (1997). The Macrobotanical Evidence for Vegetation in the Near East, c. 18 000/16 000 B.C to 4 000 B.C.. Paléorient, 23 (2), 197-207. http://dx.doi.org/10.3406/paleo.1997.4661 This paper is posted at ScholarlyCommons. https://repository.upenn.edu/penn_museum_papers/36 For more information, please contact [email protected]. The Macrobotanical Evidence for Vegetation in the Near East, c. 18 000/16 000 B.C to 4 000 B.C. Abstract Vegetation during the glacial period, post-glacial warming and the Younger Dryas does not seem to have been affected by human activities to any appreciable extent. Forest expansion at the beginning of the Holocene occurred independently of human agency, though early Neolithic farmers were able to take advantage of improved climatic conditions. Absence of macrobotanical remains precludes discussion of possible drought from 6,000 to 5,500 ВС. By farming, herding, and fuel-cutting, human populations began to have an impact on the landscape at different times and places. Deleterious effects of these activities became evident in the Tigris-Euphrates drainage during the third millennium ВС based on macrobotanical evidence from archaeological sites. -
Aquamarine 2015 (.Pdf | 1.18
ISSN 1849-6172 Annual Magazine of the Blue World Institute of Marine Research and Conservation Dear friends! Another successful year is behind us, In addition to the dolphins, our researchers also which was confirmed by an award that Blue World had many encounters with sea turtles - the 2015 Institute recently received. At the ceremony of loggerhead turtles. In the Turtle Rescue Centre the Annual Awards of Croatian tourism, as part one turtle named Viktorija was held for recovery. of the “Days of Croatian Tourism” in Poreč, Blue It was found close to the island of the Unije by qu e World Institute won the award in the category tourists. Volume: 15 Issue: 1 of sustainable tourism for concern of the environment. On the 1st of July we celebrated 23rd Dolphin Day that was filled with various art and educational This summer we started with organised dolphin- workshops, our well-known “Treasure Hunt” watching tours, where everybody who is game and a photo-contest “Sense the Sea”. interested can go and search for dolphins with an experienced skipper. These trips focus on During the year we had a lot of reported cases learning about the dolphins and their environment, of dolphin entanglement in fishing gear. These as well as conserving their habitat and behaving cases point to the fact that dolphins in coastal respectful towards them as living beings. waters are increasingly getting hurt due to such fishing tools. Due to the large interest of children we introduced two educational programmes in cooperation with Unfortunately, we also had a case where a mother Bioteka from Zagreb - “Little Marine School” lost its new-born baby. -
Primary Sources of Archaeobotanical Datasets and Radiocarbon Dates from Southwest Asia
Asouti, Eleni, and Dorian Q Fuller. A Contextual Approach to the Emergence of Agriculture in Southwest Asia: Reconstructing Early Neolithic Plant-Food Production. Supplement A: Primary Sources of Archaeobotanical Datasets and Radiocarbon Dates from Southwest Asia. Current Anthropology 54(3). Supplement A: Primary Sources of Archaeobotanical Datasets and Radiocarbon Dates from Southwest Asia We have assembled in this supplement the primary sources of archaeobotanical datasets retrieved from sites in Southwest Asia (Part 1) and the radiocarbon dates by which these sites have been assigned calendrical ages (Part 2). Part 3 presents the radiocarbon dates for early PPN sites that, to date, have not produced relevant published archaeobotanical assemblages. Part 1: Sites with Published Archaeobotanical Datasets For general overviews see Asouti and Fuller (2012), Charles (2007), Colledge and Conolly (2007), Colledge, Conolly, and Shennan (2004), Fuller et al. (2012), Garrard (1999), Willcox (1999, 2007) and Zohary, Hopf, and Weiss (2012). Sources for individual sites are indicated below, listed alphabetically by site name, followed by a short assessment of plant domestication status for all sites listed in Tables 3-4, and a list of bibliographic references. 1A. Archaeobotanical primary data sources Abdul Hosein, Tepe Iran Hubbard 1990. ‘Abr, Tell Syria Willcox et al. 2009, Willcox et al. 2008. Abu Hureyra, Tell Syria Colledge and Conolly 2010; Hillman 2000; Hillman et al. 1989; Hillman et al. 2001; de Moulins 1997, 2000. ‘Ain Ghazal Jordan Rollefson et al. 1985. Ali Kosh Iran Helbaek 1969. Aşıklı Höyük Turkey van Zeist and de Roller 1995. Aswad, Tell Syria van Zeist and Bakker-Heeres 1985 [1982]. Ayios Epiktitos Vrysi Cyprus Kyllo 1982. -
New Version of the Theory of Unique and Recent Origin of Modern Man
13 International Journal of Modern Anthropology Int. J. Mod. Anthrop. (2014) 7: 13 - 42 ailable online at: www.ata.org.tn DOI: http://dx.doi.org/10.4314/ijma.v1i7.1 Original Synthesis Article Recent out of Yemen: new version of the theory of unique and recent origin of modern man Hassen Chaabani Hassen Chaabani was born the 07 / 09 / 1947 in Tunis (Tunisia). He is Full Professor and research unit Director at Monastir University. He is the Founder and the President of the Tunisian Association of Anthropology. He is the Founder and the Editor of the International Journal of Modern Anthropology. Specialist in Human Genetics, Biological Anthropology and some cultural and religious subjects, he wrote dozens of academic articles and two books. In 2014, he was awarded the honorary title of Professor Emeritus. University of Monastir, Faculty of Pharmacy, 5000 Monastir, Tunisia. Abstract - It is generally accepted that the human evolutionary history was started in sub-Saharan Africa by the emergence of first individuals belonging to our genus Homo. But details of this evolution, particularly those of its last stage relating to the modern man (Homo sapiens sapiens) emergence, represent until now a controversial topic. Confusion and imprecision associated with certain concepts and definitions have accentuated this controversy and therefore helped to curb the progress of the research in this topic. In this paper I present these problems before presenting a new detailed version of the theory of unique and recent origin of modern man. This version designated “Recent out of Yemen” thesis represents a refined grand synthesis in which my advanced hypotheses are brought together with new additional details. -
List of Islands
- List of islands CI Name on the map 1:25000 Name on nautic map Location Latitude Longitude IOTA Note 1 Aba D. Aba V. nr. Kornat 43° 51' 55,6'' N 15° 12' 48,9'' E EU-170 2 Arkanđel Arkanđel nr. Drvenik Mali 43° 28' 20,5'' N 16° 01' 41,0'' E EU-016 3 Arta M. Arta M. nr. Murter 43° 51' 12,2'' N 15° 33' 41,2'' E EU-170 4 Arta V. Arta V. nr. Murter 43° 51' 21,0'' N 15° 32' 40,1'' E EU-170 5 Babac Babac nr. Pašman 43° 57' 21,6'' N 15° 24' 11,6'' E EU-170 6 Badija Badija nr. Korčula 42° 57' 14,3'' N 17° 09' 39,4'' E EU-016 7 Biševo Biševo nr. Vis 42° 58' 44,0'' N 16° 01' 00,0'' E EU-016 8 Bodulaš Bodulaš Medulin gulf 44° 47' 28,1'' N 13° 56' 53,8'' E Not 9 Borovnik Borovnik nr. Kornat 43° 48' 39,7'' N 15° 15' 12,8'' E EU-170 10 O. Brač Brač 43° 20' 00,0'' N 16° 40' 00,0'' E EU-016 11 Ceja Ceja Medulin gulf 44° 47' 05,6'' N 13° 56' 00,0'' E Not 12 O. Cres Cres 44° 51' 21,4'' N 14° 24' 29,6'' E EU-136 13 O. Čiovo Čiovo nr. Split 43° 30' 00,0'' N 16° 18' 00,0'' E Not 14 Dolfin Dolfin nr. Pag 44° 41' 29,6'' N 14° 41' 28,1'' E EU-170 15 Dolin Dolin nr. -
Sourcing Epi-Palaeolithic to Chalcolithic
Marginal Perspectives: Sourcing Epi-Palaeolithic to Chalcolithic Obsidian from the Öküzini Cave (SW Turkey) Tristan Carter, François-Xavier Le Bourdonnec, Metin Kartal, Gérard Poupeau, Thomas Calligaro, Philippe Moretto To cite this version: Tristan Carter, François-Xavier Le Bourdonnec, Metin Kartal, Gérard Poupeau, Thomas Calligaro, et al.. Marginal Perspectives: Sourcing Epi-Palaeolithic to Chalcolithic Obsidian from the Öküzini Cave (SW Turkey). Paléorient, CNRS, 2011, 37 (2), pp.123 - 149. 10.3406/paleo.2011.5427. hal-01743167 HAL Id: hal-01743167 https://hal.archives-ouvertes.fr/hal-01743167 Submitted on 21 Dec 2018 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. PART À MARGINAL PERSPECTIVES: SOURCING TIRÉS - EPI-PALAEOLITHIC TO CHALCOLITHIC OBSIDIAN FROM THE ÖKÜZINI CAV E ÉDITIONS (SW TURKEY) CNRS • T. CARTER, F.-X. LE BOURDONNEC, M. KARTAL, G. POUPEAU, T. CALLIGARO PART À and P. MORETTO TIRÉS - Abstract: Fifty-six pieces of obsidian from the Öküzini Cave in SW Anatolia were elementally characterised using particle induced X-ray emission [PIXE], the artefacts coming from strata that span the early Epi-Palaeolithic to Late Chalcolithic. The obsidian comes from two sources in southern Cappadocia, East Göllü Dağ and Nenezi Dağ (380 km distant), representing the earliest evidence for these sources’ use at distance. -
JAHRBUCH DER GEOLOGISCHEN BUNDESANSTALT Jb
JAHRBUCH DER GEOLOGISCHEN BUNDESANSTALT Jb. Geol. B.-A. ISSN 0016–7800 Band 149 Heft 1 S. 61–109 Wien, Juli 2009 A Revision of the Tonnoidea (Caenogastropoda, Gastropoda) from the Miocene Paratethys and their Palaeobiogeographic Implications BERNARD LANDAU*), MATHIAS HARZHAUSER**) & ALAN G. BEU***) 2 Text-Figures, 10 Plates Paratethys Miozän Gastropoda Caenogastropoda Tonnoidea Österreichische Karte 1 : 50.000 Biogeographie Blatt 96 Taxonomie Contents 1. Zusammenfassung . 161 1. Abstract . 162 1. Introduction . 162 2. Geography and Stratigraphy . 162 3. Material . 163 4. Systematics . 163 1. 4.1. Family Tonnidae SUTER, 1913 (1825) . 163 1. 4.2. Family Cassidae LATREILLE, 1825 . 164 1. 4.3. Family Ranellidae J.E. GRAY, 1854 . 170 1. 4.4. Family Bursidae THIELE, 1925 . 175 1. 4.5. Family Personidae J.E. GRAY, 1854 . 179 5. Distribution of Species in Paratethyan Localities . 180 1. 5.1. Diversity versus Stratigraphy . 180 1. 5.2. The North–South Gradient . 181 1. 5.3. Comparison with the Pliocene Tonnoidean Fauna . 181 6. Conclusions . 182 3. Acknowledgements . 182 3. Plates 1–10 . 184 3. References . 104 Revision der Tonnoidea (Caenogastropoda, Gastropoda) aus dem Miozän der Paratethys und paläobiogeographische Folgerungen Zusammenfassung Die im Miozän der Paratethys vertretenen Gastropoden der Überfamilie Tonnoidea werden beschrieben und diskutiert. Insgesamt können 24 Arten nachgewiesen werden. Tonnoidea weisen generell eine ungewöhnliche weite geographische und stratigraphische Verbreitung auf, wie sie bei anderen Gastropoden unbekannt ist. Dementsprechend sind die paratethyalen Arten meist auch in der mediterranen und der atlantischen Bioprovinz vertreten. Einige Arten treten zuerst im mittleren Miozän der Paratethys auf. Insgesamt dokumentiert die Verteilung der tonnoiden Gastropoden in der Parate- thys einen starken klimatischen Einfluss. -
Mollusca, Gastropoda
Contr. Tert. Quatern. Geol. 32(4) 97-132 43 figs Leiden, December 1995 An outline of cassoidean phylogeny (Mollusca, Gastropoda) Frank Riedel Berlin, Germany Riedel, Frank. An outline of cassoidean phylogeny (Mollusca, Gastropoda). — Contr. Tert. Quatern. Geo!., 32(4): 97-132, 43 figs. Leiden, December 1995. The phylogeny of cassoidean gastropods is reviewed, incorporating most of the biological and palaeontological data from the literature. Several characters have been checked personally and some new data are presented and included in the cladistic analysis. The Laubierinioidea, Calyptraeoidea and Capuloidea are used as outgroups. Twenty-three apomorphies are discussed and used to define cassoid relations at the subfamily level. A classification is presented in which only three families are recognised. The Ranellidae contains the subfamilies Bursinae, Cymatiinae and Ranellinae. The Pisanianurinae is removed from the Ranellidae and attributed to the Laubierinioidea.The Cassidae include the Cassinae, Oocorythinae, Phaliinae and Tonninae. The Ranellinae and Oocorythinae are and considered the of their families. The third the both paraphyletic taxa are to represent stem-groups family, Personidae, cannot be subdivided and for anatomical evolved from Cretaceous into subfamilies reasons probably the same Early gastropod ancestor as the Ranellidae. have from Ranellidae the Late Cretaceous. The Cassidae (Oocorythinae) appears to branched off the (Ranellinae) during The first significant radiation of the Ranellidae/Cassidaebranch took place in the Eocene. The Tonninae represents the youngest branch of the phylogenetic tree. Key words — Neomesogastropoda, Cassoidea, ecology, morphology, fossil evidence, systematics. Dr F. Riedei, Freie Universitat Berlin, Institut fiir Palaontologie, MalteserstraBe 74-100, Haus D, D-12249 Berlin, Germany. Contents superfamily, some of them presenting a complete classifi- cation.