Olaf Jöris - Profile on Academia.edu (original) (raw)
Books by Olaf Jöris
Site-internal spatial organization of hunter-gatherer societies: Case studies from the European Palaeolithic and Mesolithic.
Beiträge in: F. Sirocko 2009 (Hrsg.), Wetter, Klima, Menschheitsentwicklung. Von der Eiszeit bis ins 21. Jahrhundert.
Setting the record straight: Toward a systematic chronological understanding of the Middle to Upper Paleolithic boundary in Eurasia.
DOWNLOAD AT: http://www.anth.uconn.edu/faculty/adler/ FOLLOW: Publications D. S. Adler, and O. ... more DOWNLOAD AT: http://www.anth.uconn.edu/faculty/adler/
FOLLOW: Publications
D. S. Adler, and O. Jöris, O. (Guest Editors) 2008. Journal of Human Evolution: Chronology of the Middle-Upper Paleolithic Transition in Eurasia, 55/5.
Dating the Middle to Upper Palaeolithic Boundary across Eurasia.
DOWNLOAD AT: http://www.anth.uconn.edu/faculty/adler/ FOLLOW: Publications Jöris, O., D. S. Adl... more DOWNLOAD AT: http://www.anth.uconn.edu/faculty/adler/
FOLLOW: Publications
Jöris, O., D. S. Adler (Guest Editors). 2008. Dating the Middle to Upper Palaeolithic Boundary Across Eurasia, a special issue of the Eurasian Prehistory 2007, 5(2).
Der altpaläolithische Fundplatz Dmanisi (Georgien, Kaukasus). Archäologische Funde und Befunde des Liegenden Fundkomplexes im Kontext der frühen Menschheitsentwicklung.
Die georgische Ruinenstadt Dmanisi erregt als einer der bedeutendsten Fundplätze des Altpaläolith... more Die georgische Ruinenstadt Dmanisi erregt als einer der bedeutendsten Fundplätze des Altpaläolithikums internationales Aufsehen. Die Entdeckung eines ersten, auf 1,8 Millionen Jahre datierten menschlichen Unterkiefers machte Dmanisi 1991 weltberühmt. Bestehende Modelle zur Ausbreitung des Frühen Menschen von Afrika nach Eurasien waren neu zu überdenken. Weitere bedeutende Fossilfunde im Kontext einer reichen Fauna folgten. Ihre Analyse erlaubt u.a. Rückschlüsse auf die Art der Landnutzung durch den Frühen Menschen.
Der Künstler Otmar Alt thematisiert phantasievoll und unterhaltsam Schwerpunktthemen aus unserer ... more Der Künstler Otmar Alt thematisiert phantasievoll und unterhaltsam Schwerpunktthemen aus unserer frühesten Vergangenheit. In seiner Formensprache >transskribiert< er archäologische Themen in eigene >Bildvokabeln<. Das Ergebnis ist ein Bilderzyklus, in dem Alt die archäologischen Objekte ihrem ursprünglichen Kontext entreißt, zu neuen Szenen komponiert, oder sie in einem anderen Zusammenhang setzt.
Aus dem Mittelrheingebiet stammen einzigartige Belege, die wesentlich zum Verständnis der Lebensw... more Aus dem Mittelrheingebiet stammen einzigartige Belege, die wesentlich zum Verständnis der Lebensweise der ersten Menschen vor rund 600.000 Jahren bis zum Beginn von Ackerbau und Viehzucht vor etwa 7.500 Jahren beitragen. Das Buch stellt mittelrheinische Originalfunde sowie Repliken anderer europäischer Fundplätze im Kontext der internationalen Steinzeitforschung mit reicher Illustrierung vor.
Contributions to: A. Debénath / H.L. Dibble 1994, Handbook of Palaeolithic Typology. Volume One: Lower and Middle Palaeolithic of Europe.
Papers by Olaf Jöris
Today, the Late Glacial interstadials Bolling and Allerod, originally defined in northern Europe,... more Today, the Late Glacial interstadials Bolling and Allerod, originally defined in northern Europe, are often applied as chronozones in different palaeoclimate contexts across the Northern Hemisphe- re. The scientific community in both palaeoclimate research and archaeology often disregards the fact that the Meiendorf interstadial has long been identified as preceding the Bolling-Allerod sequence, and that there are lots of difficulties with the synchronization of the Oldest Dryas-Bolling-Older Dryas-sequence. Synchronization of important Central European high-resolution pollen records with the Greenland GRIP ice core demonstrates a strong climatic gradient from the South to the North of Europe over the entire Late Glacial. Therefore, the northern European interstadials (Meiendorf, Bolling, Allerod) cannot serve universally as Late Glacial chronozones with reference to their characteristic pollen compositions, even though they are of greatest importance for the understanding of the re...
Dat Ing the Mid Dle to Up Per Palaeo Lithic Bound Ary Across Eur Asia
&amp;amp;quot;DOWNLOAD AT: http://www.anth.uconn.edu/faculty/adler/ FOLLOW: Publications ... more &amp;amp;quot;DOWNLOAD AT: http://www.anth.uconn.edu/faculty/adler/ FOLLOW: Publications Jöris, O., D. S. Adler (Guest Editors). 2008. Dating the Middle to Upper Palaeolithic Boundary Across Eurasia, a special issue of the Eurasian Prehistory 2007, 5(2).&amp;amp;quot;
Replacement of Neanderthals by Modern Humans Series, 2019
The planned series of volumes will report the results of a major research project entitled "Repla... more The planned series of volumes will report the results of a major research project entitled "Replacement of Neanderthals by Modern Humans: Testing Evolutionary Models of Learning", offering new perspectives on the process of replacement and on interactions between Neanderthals and modern humans and hence on the origins of prehistoric modern cultures. The projected volumes will present the diverse achievements of research activities, originally designed to implement the project's strategy, in the fields of archaeology, paleoanthropology, cultural anthropology, population biology, earth sciences, developmental psychology, biomechanics, and neuroscience. Comprehensive research models will be used to integrate the discipline-specific research outcomes from those various perspectives. The series, aimed mainly at providing a set of multidisciplinary perspectives united under the overarching concept of learning strategies, will include monographs and edited collections of papers focusing on specific problems related to the goals of the project, employing a variety of approaches to the analysis of the newly acquired data sets.
Hominin occupation of the Tibetan Plateau during the Last Interglacial Complex
Quaternary Science Reviews, 2021
Abstract The Paleolithic archaeological record of the Tibetan Plateau is crucial for understandin... more Abstract The Paleolithic archaeological record of the Tibetan Plateau is crucial for understanding human ecological and genetic adaptation to life in high altitudes. Recent work on the Tibetan Plateau has documented hominin occupations by Denisovans at Baishiya Karst Cave (BKC) from at least ca. 160, and again around 100 and 60 thousand years ago (ka), followed by modern human occupation at Nwya Devu (ND) around 30–40 ka. However, with the exception of these two geographically distinct sites, there are very few Paleolithic sites with secure stratigraphy and reliable dates on the Tibetan Plateau. Thus, the spatial and temporal history of Paleolithic hominin occupation of the Tibetan Plateau remains poorly understood. Here we report a newly discovered well-stratified and well-dated Paleolithic site, Jiangjunfu 01 (JJF01), from the northeastern margin of the plateau. Optical dating of sediments from cultural layers shows that the site was occupied by hominin who employed simple core-and-flake technology, during warmer interglacial environments ∼90–120 ka. To date, JJF01 is one of the three oldest archaeological sites with secure stratigraphy and reliable dating from the Tibetan Plateau, further confirming that hominins, potentially Denisovans, occupied and inhabited the highest region of our planet at least by the early Upper Pleistocene.
A New Continuous Terrestrial Archive of Environmental Change during the Last Interglacial/Glacial Cycle – The Loess-Palaeosol-Sequences of the Schwalbenberg (Middle Rhine Valley, Germany)
&amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;... more &amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;amp;am…
Kombinierte nicht-invasive PIXE/PIGE-Analysen von aurignacienzeitlichen Objekten aus Mammutelfenbein bedeutender archäologischer Fundstätten
Angewandte Chemie, 2018
Hunters of the "Golden Mile": The late Allerød Federmessergruppen site at Bad Breisig, Central Rhineland, Germany
The late Allerød eruption of the Central Rhineland Laacher See-volcano (10,966 cal BC) was of lar... more The late Allerød eruption of the Central Rhineland Laacher See-volcano (10,966 cal BC) was of large environmental impact, both on a regional and on a supraregional scale. Its eruptiva were deposited over an area of more than 2000 km², covering large parts of the landscape. The recent discovery of a Final Palaeolithic site near Bad Breisig shows that the human re-occupation of the Central Rhineland of Germany by a late Federmessergruppen band took place much earlier than previously thought. The presence of backed points of Malaurie-type as well as remains of red and roe deer dates the occupation into the last 200 years of the Allerød interstadial, which is also indicated by radiocarbon dating.
Radiocarbon evidence of the Middle to Upper Paleolithic transition in Southwestern Europe
Trabajos de Prehistoria
Online: http://tp.revistas.csic.es/index.php/tp/article/view/79/79
Tab. 1 14 C dates for Font del Ros, comprising charcoal samples (Ch) and charred fragments of Cor... more Tab. 1 14 C dates for Font del Ros, comprising charcoal samples (Ch) and charred fragments of Corylus (Cor). The chronological range has been calibrated using the SFCP 2005 age model with 2σ.-(Weninger et al. 2006).
Aus einer anderen Welt - Europa zur Zeit des Neandertalers