scholarly journals ATLANTIS IN SPAIN V

2017 ◽  
Vol 43 (1) ◽  
pp. 138
Author(s):  
S.P Papamarinopoulos

Following strictly Plato’s information we reach Iberia and there we discovered the basic geomorphological characteristics of a horseshow shape flat and elongated basin which is surrounded by mountains. The basin reaches the Atlantic Ocean. This valley is Andalusia and it was missed by Herodotus and Hecateus, who lived a century earlier than Plato, and constructed North West Europe’s map. The Iberian civilization is reflected in the Greek myths prior to Plato too. Atlantis’ catastrophe in the shape of the concentric scheme’s, being in Iberia’s coast, was realized by earthquakes and a tsunami. The discovery of the very first Mycenaean vase’s fragment, in Guadalquivir’s estuary by Spanish archaeologists in 1990, offered the first archaeological evidence that the prehistoric Greeks had visited Atlantis after all before the 12th century B.C. The recent interest of the Spanish Archaeological Survey in Andalusia initiated because it has been proved geologically that the region had not been submerged since the last ice age. New evidence suggests that the waters may have receded in time for the Iberians in the period Tartesssos to build an urban centre, which was later destroyed by earthquakes and a tsunami as Plato describes in Timaeos and Critias for this region. Although platonic Atlantis could not be considered, as Thucydides would prefer, a historical text but it cannot be considered as a single paramyth either since some parts of his text have been proved already. It can be considered as a genuine myth containing a true prehistoric kernel covered firstly by a layer of inventions produced by transmitting people, the story, from generation to generation between the actual occurrence of the event within the 12th century B.C. and Solon’s 6th century B.C. who recorded it and then of the 4th century B.C. when Plato wrote down. Atlantis is also covered by a platonic paramythical layer full of mathematics and musicological information which is recognized and can be removed liberating the genuine myth’s kernel from the platonic intervention.

Author(s):  
Sigrún Dögg Eddudóttir ◽  
Eva Svensson ◽  
Stefan Nilsson ◽  
Anneli Ekblom ◽  
Karl-Johan Lindholm ◽  
...  

AbstractShielings are the historically known form of transhumance in Scandinavia, where livestock were moved from the farmstead to sites in the outlands for summer grazing. Pollen analysis has provided a valuable insight into the history of shielings. This paper presents a vegetation reconstruction and archaeological survey from the shieling Kårebolssätern in northern Värmland, western Sweden, a renovated shieling that is still operating today. The first evidence of human activities in the area near Kårebolssätern are Hordeum- and Cannabis-type pollen grains occurring from ca. 100 bc. Further signs of human impact are charcoal and sporadic occurrences of apophyte pollen from ca. ad 250 and pollen indicating opening of the canopy ca. ad 570, probably a result of modification of the forest for grazing. A decrease in land use is seen between ad 1000 and 1250, possibly in response to a shift in emphasis towards large scale commodity production in the outlands. Emphasis on bloomery iron production and pitfall hunting may have caused a shift from agrarian shieling activity. The clearest changes in the pollen assemblage indicating grazing and cultivation occur from the mid-thirteenth century, coinciding with wetter climate at the beginning of the Little Ice Age. The earliest occurrences of anthropochores in the record predate those of other shieling sites in Sweden. The pollen analysis reveals evidence of land use that predates the results of the archaeological survey. The study highlights how pollen analysis can reveal vegetation changes where early archaeological remains are obscure.


Author(s):  
Lesley Newson ◽  
Peter Richerson

It’s time for a new story of our origins. One reason is that there a great deal of new evidence about what humans are like and the conditions that shaped human evolution. Another is that the thinking on human evolution has shifted. Evolutionists recognize that humans are very different from other animals, and they have been working to explain the different evolutionary path that humans took. There are still many gaps in the story, but this book describes seven points in our ancestors’ tale and explains the evidence behind these descriptions. The story begins seven million years ago, with the life of our ape ancestors, which were also the ancestors of today’s chimpanzees and bonobos. The second point is three million years ago with an ape that walked upright and lived outside the forest. Then follows a description of the life of early humans who lived one and a half million years ago. At the fourth point, 100,000 years ago, humans lived in Africa who were physically very similar to modern humans. The fifth is 30,000 years ago, during the last ice age, when our ancestors had evolved more complex cultures. The sixth is the period of accelerating cultural evolution that began as the planet started to recover from this ice age. Finally, beginning in the 1700s, there is the transformational period we are in now, which we call “modern times.” The style of this book is unusual for a science book because it has narrative sections that illustrate the lives of our ancestors and the problems they faced.


1970 ◽  
Vol 20 ◽  
pp. 119-137 ◽  
Author(s):  
Harold R. Cohen

The origins of agriculture and domestication have long been identified, in theory, with the beginning of permanent settlements; the beginning of the Early Neolithic Period is known, in fact, to be synchronous with the ending of the Last Ice Age. To some scholars, fact and theory have suggested that this synchronism implies a causal relationship between certain assumed climatic changes and the beginnings of food production; for others, this synchronism is not more than a misleading coincidence. It is not the purpose of the writer to discuss the validity of these assumptions except to indicate that opinion seems to be hardening that food production may have had a more complicated and lengthy history than these assumptions suggest. There has grown up over the last 25 years a considerable body of literature expressing the most varied opinion about the causes for the origins of food production, and its variety has not narrowed with the emergence of new evidence. In my opinion, the basis for the solution of this problem will be derived essentially from palaeoecological analyses of selected areas and regions in various parts of the world, and not only in the Near East. This paper is intended to open such a study for the region of south central Anatolia. As might be expected in an ecological study, the evidence derives from a number of disciplines, and, accordingly, several colleagues have contributed to the formulation of the suggested ecological pattern. That pattern itself, however, is the responsibility of the writer.


Nature ◽  
1980 ◽  
Vol 286 (5772) ◽  
pp. 479-482 ◽  
Author(s):  
Jean-Claude Duplessy ◽  
J. Moyes ◽  
C. Pujol

2013 ◽  
Vol 13 (3) ◽  
pp. 625-648 ◽  
Author(s):  
L. O'Brien ◽  
J. M. Dudley ◽  
F. Dias

Abstract. The island of Ireland is battered by waves from all sides, most ferociously on the west coast as the first port of call for waves travelling across the Atlantic Ocean. However, when discussing ocean events relevant to the nation of Ireland, one must actually consider its significantly larger designated continental shelf, which is one of the largest seabed territories in Europe. With this expanded definition, it is not surprising that Ireland has been subject to many oceanic events which could be designated as "extreme"; in this paper we present what we believe to be the first catalogue of such events, dating as far back as the turn of the last ice age.


Author(s):  
Richard Bradley ◽  
Colin Haselgrove ◽  
Marc Vander Linden ◽  
Leo Webley

The Later Prehistory of North-West Europe provides a unique, up-to-date, and easily accessible synthesis of the later prehistoric archaeology of north-west Europe, transcending political and language barriers that can hinder understanding. By surveying changes in social forms, landscape organization, monument types, and ritual practices over six millennia, the volume reassesses the prehistory of north-west Europe from the late Mesolithic to the end of the pre-Roman Iron Age. It explores how far common patterns of social development are apparent across north-west Europe, and whether there were periods when local differences were emphasized instead. In relation to this, it also examines changes through time in the main axes of contact between the various regions of continental Europe, Britain, and Ireland. Key to the volume's broad scope is its focus on the vast mass of new evidence provided by recent development-led excavations. The authors collate data that has been gathered on thousands of sites across Britain, Ireland, northern France, the Low Countries, western Germany, and Denmark, using sources including unpublished 'grey literature' reports. The results challenge many aspects of previous narratives of later prehistory, allowing the volume to present a distinctively fresh perspective.


Languages ◽  
2021 ◽  
Vol 6 (2) ◽  
pp. 63
Author(s):  
Benedetta Baldi ◽  
Leonardo Maria Savoia

This article investigates the contact-induced reorganization of the possessive system in the Gallo-Romance dialects spoken from around the 12th century in the villages of Celle and Faeto in North Apulia and Guardia Piemontese in North-West Calabria. Gallo-Romance possessives exclude the article in the prenominal position, whereas in the Southern Italian dialects, possessives follow the noun preceded by the definite article. This original contrast is no longer visible in the varieties of Celle, Faeto and Guardia which changed the original prenominal position to the postnominal position combining with the article, except with kinship terms, preserving the original prenominal position. At the heart of contact phenomena, there are bilingualism and transfer mechanisms between the languages included in the complex knowledge of the speaker, suggesting a test bed for the treatment of language variation and parameterization. We propose an account of morpho-syntactic and interpretive properties of possessives, making use of the insights from the comparison of contact systems with prenominal (Franco-Provençal and Occitan varieties) and postnominal (Southern Italian dialects) possessives. The final part examines the distribution of possessives, tracing it back to the definiteness properties of DP and proposes a phasal treatment based on syntactic and interpretive constraints.


2021 ◽  
Author(s):  
Jesse R. Farmer ◽  
Daniel M. Sigman ◽  
Julie Granger ◽  
Ona M. Underwood ◽  
François Fripiat ◽  
...  

AbstractSalinity-driven density stratification of the upper Arctic Ocean isolates sea-ice cover and cold, nutrient-poor surface waters from underlying warmer, nutrient-rich waters. Recently, stratification has strengthened in the western Arctic but has weakened in the eastern Arctic; it is unknown if these trends will continue. Here we present foraminifera-bound nitrogen isotopes from Arctic Ocean sediments since 35,000 years ago to reconstruct past changes in nutrient sources and the degree of nutrient consumption in surface waters, the latter reflecting stratification. During the last ice age and early deglaciation, the Arctic was dominated by Atlantic-sourced nitrate and incomplete nitrate consumption, indicating weaker stratification. Starting at 11,000 years ago in the western Arctic, there is a clear isotopic signal of Pacific-sourced nitrate and complete nitrate consumption associated with the flooding of the Bering Strait. These changes reveal that the strong stratification of the western Arctic relies on low-salinity inflow through the Bering Strait. In the central Arctic, nitrate consumption was complete during the early Holocene, then declined after 5,000 years ago as summer insolation decreased. This sequence suggests that precipitation and riverine freshwater fluxes control the stratification of the central Arctic Ocean. Based on these findings, ongoing warming will cause strong stratification to expand into the central Arctic, slowing the nutrient supply to surface waters and thus limiting future phytoplankton productivity.


2017 ◽  
Vol 30 (60) ◽  
pp. 253-272 ◽  
Author(s):  
Diego Olstein

Abstract World history can be arranged into three major regional divergences: the 'Greatest Divergence' starting at the end of the last Ice Age (ca. 15,000 years ago) and isolating the Old and the New Worlds from one another till 1500; the 'Great Divergence' bifurcating the paths of Europe and Afro-Asia since 1500; and the 'American Divergence' which divided the fortunes of New World societies from 1500 onwards. Accordingly, all world regions have confronted two divergences: one disassociating the fates of the Old and New Worlds, and the other within either the Old or the New World. Latin America is in the uneasy position that in both divergences it ended up on the 'losing side.' As a result, a contentious historiography of Latin America evolved from the very moment that it was incorporated into the wider world. Three basic attitudes toward the place of Latin America in global history have since emerged and developed: admiration for the major impact that the emergence on Latin America on the world scene imprinted on global history; hostility and disdain over Latin America since it entered the world scene; direct rejection of and head on confrontation in reaction the former. This paper examines each of these three attitudes in five periods: the 'long sixteenth century' (1492-1650); the 'age of crisis' (1650-1780); 'the long nineteenth century' (1780-1914); 'the short twentieth century' (1914-1991); and 'contemporary globalization' (1991 onwards).


2003 ◽  
Vol 59 (1) ◽  
pp. 114-121 ◽  
Author(s):  
Martin J. Siegert ◽  
Richard C. A. Hindmarsh ◽  
Gordon S. Hamilton

AbstractInternal isochronous ice sheet layers, recorded by airborne ice-penetrating radar, were measured along an ice flowline across a large (>1 km high) subglacial hill in the foreground of the Transantarctic Mountains. The layers, dated through an existing stratigraphic link with the Vostok ice core, converge with the ice surface as ice flows over the hill without noticeable change to their separation with each other or the ice base. A two-dimensional ice flow model that calculates isochrons and particle flowpaths and accounts for ice flow over the hill under steady-state conditions requires net ablation (via sublimation) over the stoss face for the predicted isochrons to match the measured internal layers. Satellite remote sensing data show no sign of exposed ancient ice at this site, however. Given the lack of exposed glacial ice, surface balance conditions must have changed recently from the net ablation that is predicted at this site for the last 85,000 years to accumulation.


Sign in / Sign up

Export Citation Format

Share Document