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Belief, Ritual, and the Evolution of Religion
Belief, Ritual, and the Evolution of Religion Oxford Handbooks Online Belief, Ritual, and the Evolution of Religion Matt J. Rossano and Benjamin Vandewalle The Oxford Handbook of Evolutionary Psychology and Religion Edited by James R. Liddle and Todd K. Shackelford Subject: Psychology, Personality and Social Psychology Online Publication Date: Oct 2016 DOI: 10.1093/oxfordhb/9780199397747.013.8 Abstract and Keywords This chapter outlines an evolutionary scenario for the emergence of religion. From cognitive science, four mental prerequisites of religious cognition are discussed: (1) hyperactive agency detection, (2) theory of mind, (3) imagination, and (4) altered states of consciousness. Evidence for these prerequisites in nonhuman primates suggests their presence in our early hominin ancestors. From comparative psychology, evidence of ritual behavior in nonhuman primates and other species is reviewed. Archeological evidence of ritual behavior is also discussed. Collectively, these data indicate that the first step toward religion was an elaboration of primate social rituals to include group synchronized activities such as dancing, chanting, and singing. Control of fire, pigment use, and increasing brain size would have intensified group synchronized rituals over time, which, in the context of increased intergroup interactions, eventually led to the first evidence of supernatural ritual at about 70,000 years before present. Keywords: agency detection, burial, cave art, costly signals, evolution, religion, ritual, synchronized movement, theory of mind Anyone interested in probing the evolutionary origins of religion faces a formidable challenge: Belief is central to religion, and belief does not fossilize in the archeological record. Looking at a half-million-year-old Acheulean hand axe may tell us something about the maker’s technical skills, diet, hunting practices, and lifestyle, but very little about his or her beliefs—let alone the supernatural beliefs inherent to most religions. -
Surface Runoff to the Black Sea from the East European Plain During Last Glacial Maximum–Late Glacial Time
Downloaded from specialpapers.gsapubs.org on September 18, 2012 The Geological Society of America Special Paper 473 2011 Surface runoff to the Black Sea from the East European Plain during Last Glacial Maximum–Late Glacial time Aleksey Yu. Sidorchuk Andrey V. Panin Geographical Faculty, Moscow State University, Vorob’evy Gory, Moscow 119991, Russia Olga K. Borisova Institute of Geography, Russian Academy of Sciences, Staromonetny per., Moscow 119017, Russia ABSTRACT Hydromorphological and hydroclimatic methods were used to reconstruct the former surface runoff from the East European part of the Black Sea drainage basin. Data on the shape and dynamics of the last Fennoscandian ice sheet were used to cal- culate meltwater supply to the headwaters of the Dnieper River. The channel width and meander wavelength of well-preserved fragments of large paleochannels were measured at 51 locations in the Dnieper and Don River basins (East European Plain), which allowed reconstruction of the former surface runoff of the ancient rivers, as well as the total volume of fl ow into the Black Sea, using transform functions. Studies of the composition of fossil fl oras derived from radiocarbon-dated sediments of vari- ous origins and ages make it possible to locate their modern region analogues. These analogues provide climatic and hydrological indexes for the Late Pleniglacial and Late Glacial landscapes. Morphological, geological, geochronological, and palyno- logical studies show that the landscape, climatic, and hydrologic history of the region included: -
Respiratory Adaptation to Climate in Modern Humans and Upper Palaeolithic Individuals from Sungir and Mladeč Ekaterina Stansfeld1*, Philipp Mitteroecker1, Sergey Y
www.nature.com/scientificreports OPEN Respiratory adaptation to climate in modern humans and Upper Palaeolithic individuals from Sungir and Mladeč Ekaterina Stansfeld1*, Philipp Mitteroecker1, Sergey Y. Vasilyev2, Sergey Vasilyev3 & Lauren N. Butaric4 As our human ancestors migrated into Eurasia, they faced a considerably harsher climate, but the extent to which human cranial morphology has adapted to this climate is still debated. In particular, it remains unclear when such facial adaptations arose in human populations. Here, we explore climate-associated features of face shape in a worldwide modern human sample using 3D geometric morphometrics and a novel application of reduced rank regression. Based on these data, we assess climate adaptations in two crucial Upper Palaeolithic human fossils, Sungir and Mladeč, associated with a boreal-to-temperate climate. We found several aspects of facial shape, especially the relative dimensions of the external nose, internal nose and maxillary sinuses, that are strongly associated with temperature and humidity, even after accounting for autocorrelation due to geographical proximity of populations. For these features, both fossils revealed adaptations to a dry environment, with Sungir being strongly associated with cold temperatures and Mladeč with warm-to-hot temperatures. These results suggest relatively quick adaptative rates of facial morphology in Upper Palaeolithic Europe. Te presence and the nature of climate adaptation in modern humans is a highly debated question, and not much is known about the speed with which these adaptations emerge. Previous studies demonstrated that the facial morphology of recent modern human groups has likely been infuenced by adaptation to cold and dry climates1–9. Although the age and rate of such adaptations have not been assessed, several lines of evidence indicate that early modern humans faced variable and sometimes harsh environments of the Marine Isotope Stage 3 (MIS3) as they settled in Europe 40,000 years BC 10. -
SPATIAL DISTRIBUTION and PROBLEMS in the INTERPRETATION of RADIOCARBON DATES of the SUNGIR SITE, RUSSIA Taisiya Soldatova
Radiocarbon, Vol 61, 2019, p e1–15 DOI:10.1017/RDC.2019.61 © 2019 by the Arizona Board of Regents on behalf of the University of Arizona. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons. org/licenses/by/4.0/), which permits unrestricted reuse, distribution, and reproduction in any medium, provided the original work is properly cited. SPATIAL DISTRIBUTION AND PROBLEMS IN THE INTERPRETATION OF RADIOCARBON DATES OF THE SUNGIR SITE, RUSSIA Taisiya Soldatova Institute of Pre- and Protohistory, Department Old World and Asian Cultures, Friedrich-Alexander-University Erlangen-Nürnberg (FAU), Kochstrasse 4/18, 91054 Erlangen, Germany ABSTRACT. The Upper Paleolithic open-air site Sungir is located in the central Russian Plain. The blank production of the lithic industry is characterized by parallel reduction with flakes being the main blank type. The tool assemblage has two components: archaic types (Mousterian-like) on the one hand and Upper Paleolithic types on the other. The available data does not allow for a confident determination of the chronological position of the Sungir site, nor does it enable researchers to distinguish different stages of human occupation. The horizontal distribution of the dated samples demonstrates the almost complete absence of radiocarbon (14C) dates for household features identified at the site (fireplaces, fire and ritual pits, large accumulations of bones, etc.). In addition, the vertical distribution of 14C dates in the rather thick cultural layer points to the exposure of the site to solifluction. KEYWORDS: Aurignacian, Early Upper Paleolithic, radiocarbon chronology, spatial distribution, Streletskian culture, Sungir site. -
Human Origin Sites and the World Heritage Convention in Eurasia
World Heritage papers41 HEADWORLD HERITAGES 4 Human Origin Sites and the World Heritage Convention in Eurasia VOLUME I In support of UNESCO’s 70th Anniversary Celebrations United Nations [ Cultural Organization Human Origin Sites and the World Heritage Convention in Eurasia Nuria Sanz, Editor General Coordinator of HEADS Programme on Human Evolution HEADS 4 VOLUME I Published in 2015 by the United Nations Educational, Scientific and Cultural Organization, 7, place de Fontenoy, 75352 Paris 07 SP, France and the UNESCO Office in Mexico, Presidente Masaryk 526, Polanco, Miguel Hidalgo, 11550 Ciudad de Mexico, D.F., Mexico. © UNESCO 2015 ISBN 978-92-3-100107-9 This publication is available in Open Access under the Attribution-ShareAlike 3.0 IGO (CC-BY-SA 3.0 IGO) license (http://creativecommons.org/licenses/by-sa/3.0/igo/). By using the content of this publication, the users accept to be bound by the terms of use of the UNESCO Open Access Repository (http://www.unesco.org/open-access/terms-use-ccbysa-en). The designations employed and the presentation of material throughout this publication do not imply the expression of any opinion whatsoever on the part of UNESCO concerning the legal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. The ideas and opinions expressed in this publication are those of the authors; they are not necessarily those of UNESCO and do not commit the Organization. Cover Photos: Top: Hohle Fels excavation. © Harry Vetter bottom (from left to right): Petroglyphs from Sikachi-Alyan rock art site. -
The Origins of the Gravettians
bioRxiv preprint doi: https://doi.org/10.1101/685404; this version posted July 2, 2019. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. 1 The origin of the Gravettians: genomic evidence from a 36,000-year-old Eastern 2 European 3 4 E. Andrew Bennett1, Sandrine Prat2, Stéphane Péan3, Laurent Crépin3, Alexandr Yanevich4, 5 Simon Puaud2, Thierry Grange1, Eva-Maria Geigl1 6 7 1Institut Jacques Monod, CNRS, Université de Paris, 75013 Paris, France; 2 UMR 7194 (HNHP), 8 MNHN/CNRS/UPVD, Alliance Sorbonne Université, Musée de l’Homme, Palais de Chaillot, 17 9 Place du Trocadéro, 75116, Paris, France; 3UMR 7194 (HNHP), MNHN/CNRS/UPVD, Muséum 10 national d’Histoire naturelle, Alliance Sorbonne Université, Institut de Paléontologie Humaine, 1 11 rue René Panhard, 75013, Paris, France; 4Institute of Archaeology, National Academy of Sciences 12 of Ukraine, Heroiv Stalingrada 12, 04210 Kyiv, Ukraine. 13 14 15 16 17 18 19 20 1 bioRxiv preprint doi: https://doi.org/10.1101/685404; this version posted July 2, 2019. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. 21 Abstract 22 The Gravettian technocomplex was present in Europe from more than 30,000 years ago until 23 the Last Glacial Maximum, but the source of this industry and the people who manufactured 24 it remain unsettled. -
Dry Grasslands on Sandy Soils in the Forest and Forest-Steppe Zones of the Plains Region of Ukraine: Present State of Syntaxonomy - Anna Kuzemko
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Tuexenia - Mitteilungen der Floristisch- soziologischen Arbeitsgemeinschaft Jahr/Year: 2009 Band/Volume: NS_29 Autor(en)/Author(s): Kuzemko Anna Artikel/Article: Dry grasslands on sandy soils in the forest and forest- steppe zones of the plains region of Ukraine: present state of syntaxonomy 369-390 ©Floristisch-soziologische Arbeitsgemeinschft; www.tuexenia.de; download unter www.zobodat.at Tuexenia 29: 369-390. Göttingen 2009. Dry grasslands on sandy soils in the forest and forest-steppe zones of the plains region of Ukraine: present state of syntaxonomy - Anna Kuzemko - Abstract This paper compiles and synthesizes the present knowledge of dry grassland vegetation on sandy soils in northern Ukraine, based on published and unpublished sources. In total, 391 relevés from 29 association-level syntaxa of the class Koelerio-Corynephoretea (inch Sedo-Scleranthetea and Festucetea vaginatae), as well as of the alliance Agrostion vinealis from the class Molinio-Arrhenatheretea were used for the analysis. Based on cluster analysis and comparison of synoptic tables, a compact classifica tion scheme of the sandy dry grassland vegetation in the forest and forest-steppe zones of the plains region of Ukraine has been developed. It comprises 10 associations from the Koelerio-Corynephoretea and one from the Agrostion vinealis (Molinio-Arrhenatheretea). The Koelerio-Corynephoretea include four orders in Ukraine: Alysso-Sedetalia, Trifolio arvensis- Festucetalia ovinae, Corynephoretalia canescentis, and Sedo acris-Festucetalia. The Alysso-Sedetalia are represented by two associations, the Aurinio saxatilis-Allietum podolici and the Minuartio auctae- Festucetum pallentis from West Podillya. The associations Stipetum pulcherrimae, Astragalo-Stipetum, and Poetum versicoloris, which also had been included in the Alysso-Sedetalia by some authors, are assigned to the class Festuco-Brometea based on their species composition. -
The Early Upper Palaeolithic of Kostenki: Chronology, Taxonomy, and Cultural Affiliation
27 THE EARLY UPPER PALAEOLITHIC OF KOSTENKI: CHRONOLOGY, TAXONOMY, AND CULTURAL AFFILIATION A. A. Sinitsyn Abstract represents a distinct regional pattern comparable to much larg- er geographic areas of Europe. This paper deals with the structure, composition, and chro- Nine major geographic areas or zones of cultural evolu- nology of the early stage of the Upper Palaeolithic in the tion are identified for the European Upper Palaeolithic (Fig. Kostenki-Borshchevo area, from the earliest manifestation of 1). There seems to be consensus that each of these areas, such Upper Palaeolithic technocomplexes to the appearance of the as the Aquitanian, western Mediterranean, Central Europe, local Gravettian. This is a principal unit of Upper Palaeolithic Balkans, eastern Mediterranean, and others, represents distinct classification showing a fundamental change in the organiza- zones of local cultural development during the Upper Palaeo- tion of the Upper Palaeolithic European world at 28–30 ka. lithic. During some time periods, one or more areas reflect The Kostenki model provides evidence of both general Eu- common developments (see DJINDJIAN 2006): ropean evolutional trends and particular local features, which a) the Early Upper Palaeolithic (EUP) exhibits a binary pat- appear to be the basis for its distinction as a separate period of tern, one component of which is the Aurignacian with a con- Upper Palaeolithic classification. tinental distribution, while the other is represented by series of local “transitional” cultures: Castelperronean for Western Eu- Keywords rope; Uluzzo for a limited part of the Western Mediterranean, Upper Palaeolithic, Kostenki’ model of evolution, EUP-MUP Szeletian and Bohunician traditions for Central Europe; and boundary. -
1077 the Age of Upper Paleolithic Sites in The
THE AGE OF UPPER PALEOLITHIC SITES IN THE MIDDLE DNIEPER RIVER BASIN OF EASTERN EUROPE Z A Abramova • G V Grigorieva • G I Zaitseva Institute for the History of Material Culture, the Russian Academy of Sciences. St.Petersburg, Dvortsovaya nab. 18, 191186, Russia. Email: [email protected]. ABSTRACT. This paper discusses the comparative chronology of Upper Paleolithic sites in the Middle Dnieper River basin, based on archaeological and radiocarbon evidence. Three chronological periods of the development of the Upper Paleolithic are distinguished in this area. According to the data obtained, the third period is similar to the European Magdalenian, yet its economies were different. The base of the subsistence economy for Dnieperian hunters was the procurement of mammoth, while reindeer was the most important for the subsistence of European Magdalenian. The abundance of mammoths and the raw material in the form of mammoth tusks made a deep impact on both the economy and material culture of the hunters in the Dnieper River basin. The 14C dates confirm the chronological subdivision. INTRODUCTION From the character and peculiarities in the development of material culture during the Upper Pale- olithic (UP), six major regions may be distinguished in eastern Europe. These are the Caucasus, Crimea, the Northern Black Sea and the Asov Sea areas, the basins of the Middle Dniestr, the Mid- dle Dnieper, and the Middle Doñ (Rogachev 1969) Rivers. Among these, the Middle Dnieper basin takes a special position. It includes several geographically distinct areas, with the varying concen- tration of Upper Paleolithic sites: the Desna River basin (particularly rich in UP sites), as well as the Upper and Middle Dnieper River basins. -
Landscape Archaeology and the Dispersal of Modern Humans in Eastern Europe
Hoffecker & Holliday ● Landscape Archaeology & Dispersal of Modern Humans in Eastern Europe Landscape Archaeology and the Dispersal of Modern Humans in Eastern Europe John F. Hoffecker Institute of Arctic and Alpine Research University of Colorado at Boulder 1560 30th Street Boulder, Colorado 80309-0450 USA Vance T. Holliday Departments of Anthropology and Geosciences University of Arizona PO Box 210030 Tucson, Arizona 85721-0030 USA Running Title: Modern Human Dispersal in Eastern Europe 1 Hoffecker & Holliday ● Landscape Archaeology & Dispersal of Modern Humans in Eastern Europe ABSTRACT Homo sapiens dispersed into Eastern Europe before 40,000 cal BP and both the genetics of living humans and the archaeological record indicate that they may have arrived in two or more migratory waves. The archaeological record of the arrival and early settlement of modern humans in Eastern Europe (45,000–30,000 cal BP) is dominated by open-air sites on the large lowland plain that extends from the Carpathian to the Ural Mountains. The record exhibits many parallels to the terminal Upper Paleolithic (or Paleoindian) sites of the North American Plains and Southwest. Traces of large-mammal kill-butchery events and carcass-processing areas are common, although they often are associated with a habitation area (which is known but less common in the North American sites). The earliest movement of modern humans in Eastern Europe may be represented by an archaeological proxy in the form of many Levallois blade and point assemblages that appear to date to the same interval as the Bohunician assemblages of Central Europe (~45,000 cal BP). Direct migration from the Near East via the Caucasus Mountains is documented by bladelet assemblages in the Caucasus and on the central plain at roughly the same time the Proto-Aurignacian industry moved into southern Europe (i.e., 43,000– 42,000 cal BP). -
The Religious Mind and the Evolution of Religion
Evolution of Religion 1 Running Head: THE RELIGIOUS MIND The Religious Mind and the Evolution of Religion Matt J. Rossano Southeastern Louisiana University Author contact: Department of Psychology, Box 10831 Southeastern Louisiana University Hammond, LA 70402 [email protected] Phone: 985-549-5537 Fax: 985-549-3892 Evolution of Religion 2 Abstract This paper summarizes the literature on the religious mind and connects it to archeological and anthropological data on the evolution of religion. These connections suggest a three stage model in the evolution of religion. (1) The earliest form of religion (pre-Upper Paleolithic or pre-UP religion) would have been restricted to ecstatic rituals used to facilitate social bonding. (2) The transition to UP religion was marked by the emergence of shamanistic healing rituals and, (3) the cave art, elaborate burials, and other artifacts associated with the UP represent the first evidence of ancestor worship and the emergence of theological narratives of the supernatural. The emergence of UP religion was associated with the move from egalitarian to transegalitarian hunter-gatherers. Keywords: evolution of religion, Upper Paleolithic, religious mind, shamanism Evolution of Religion 3 The Religious Mind and the Evolution of Religion William James (1902/1961) argued that the mystical experience was the foundation for religion. Nearly a century after James, research into the neurological and cognitive basis of religion has advanced rapidly (Barrett, 2000; Boyer & Ramble, 2001; d'Aquili & Newberg, 1999; Lewis-Williams, 2002; Newberg, d'Aquili & Rause, 2001; Norenzayan & Atran, 2002; Ramachandran & Blakslee, 1998, chap. 9). Paralleling this work has been that addressing the evolutionary origins of religion (Atran, 2002; Boyer, 2001; Hayden, 2003; Sosis & Alcorta, 2003; Wilson, 2002). -
Remains of Large Mammals from the Epigravettian Site of Yudinovo
Mammals from the Epigravettian site of Yudinovo M.V. Sablin and K.Yu. Iltsevich Proceedings of the Zoological Institute RAS Vol. 325, No. 1, 2021, pp. 71–81 10.31610/trudyzin/2021.325.1.71 УДК 569:591.9 (470.333) Remains of large mammals from the Epigravettian site of Yudinovo M.V. Sablin* and K.Yu. Iltsevich Zoological Institute of the Russian Academy of Sciences, Universitetskaya Emb., 1, 199034 Saint Petersburg, Russia; e-mail: [email protected] Submitted October 9, 2020; revised November 27, 2020; accepted November 30, 2020. ABSTRACT The Epigravettian site of Yudinovo (Bryansk oblast, Russia) was discovered in 1930 by K.M. Polikarpovich. It is located in the Sudost’ river valley and has a unique stratigraphy. This article presents the results of the study of the remains of large mammals from Yudinovo and also discusses their significance in revising the former interpreta- tion of the existence of the site during the very end of the final part of the Late Pleistocene. In total, 38 268 mam- malian bones were identified from cultural layers excavated between 1947–2019. The faunal assemblage is rela- tively small with a dominance of woolly mammoth and arctic fox, typical of a cold and dry tundra-steppe envi- ronment. We undertook stable isotopic tracking from samples of bones. Our analyses confirm the hunting of both adult and juvenile larger mammals by ancient humans. Based on the eruption sequence and wear of the milk teeth from young animals, we were able to clarify the season of their death. It seems that these individuals were hunted during the late spring or early autumn.