Geoarchaeological contexts for Late Pleistocene archaeological sites with human-modified woolly mammoth remains in southeastern Wisconsin, U.S.A.

2002 ◽  
Vol 18 (1) ◽  
pp. 91-114 ◽  
Author(s):  
David F. Overstreet ◽  
Michael F. Kolb
Keyword(s):  
Late Pleistocene ◽  
Archaeological Sites ◽  
Woolly Mammoth

scholarly journals Radiocaron Dates and Archaeology of the Late Pleistocene in the Japanese Islands

Radiocarbon ◽  
2002 ◽  
Vol 44 (2) ◽  
pp. 477-494 ◽  
Author(s):  
Akira Ono ◽  
Hiroyuki Sato ◽  
Takashi Tsutsumi ◽  
Yuichiro Kudo
Keyword(s):  
Late Pleistocene ◽  
New World ◽  
Upper Paleolithic ◽  
Archaeological Sites ◽  
Early Upper Paleolithic ◽  
Strongly Connected ◽  
Radiocarbon Chronology ◽  
Japanese Islands ◽  
Late Upper Paleolithic ◽  
Early Upper

We discuss the radiocarbon chronology of Late Pleistocene archaeology in the Japanese islands. In sum, 429 samples from more than 100 archaeological sites were compiled and then divided into three periods and four stages. The Early Upper Paleolithic, characterized by Trapezoid industries, lasted during approximately 34-26 ka. The Late Upper Paleolithic period includes both the backed-blade stage and point-tool stage, the latter appearing chronologically later than the former. This stage covers ~25–15 ka. The Final Upper Paleolithic and Incipient Jomon are distinguished by the appearance of microblade industries and the emergence of pottery at the end of this period. This period covers approximately 14-12 ka. The microblade tradition, in the broadest sense, is strongly connected to the background of peopling of the New World. New data on the transitional stage from the Middle to the Upper Paleolithic are also discussed in regards to three archaeological sites. Issues on the application of the 14C calibration to the whole Japanese Upper Paleolithic are critically evaluated.

Introduction

2018 ◽  
pp. 1-7
Author(s):  
Albert C. Goodyear ◽  
Christopher R. Moore
Keyword(s):  
Sea Level ◽  
Late Pleistocene ◽  
Coastal Plain ◽  
Younger Dryas ◽  
Archaeological Sites ◽  
Impact Hypothesis

This chapter reviews the significant features of early prehistoric occupations of the Southeastern U.S. Coastal Plain. Along with the Pleistocene age archaeological sites, salient aspects of the geology, including sea level positions, are presented. Possible Pre-Clovis sites dating from pre-LGM to late Pleistocene times are considered. Clovis is seen to have a Coastal Plain settlement focus that includes the now-drowned shelf. The dramatic onset of the Younger Dryas and its potential effects on people, including the “Younger Dryas Impact Hypothesis,” are reviewed.

scholarly journals Mammoths, Deer, and a Dog: Fossil and (Sub) Recent Allochthonous Remains from the Northeastern Croatia (Podravina Region), with the First Radiocarbon Dating of the Croatian Woolly Mammoths (Mammuthus primigenius)

Quaternary ◽  
2018 ◽  
Vol 1 (2) ◽  
pp. 11 ◽  
Author(s):  
Jadranka Mauch Lenardić ◽  
Siniša Radović ◽  
Ankica Oros Sršen ◽  
Nada Horvatinčić ◽  
Petar Kostešić ◽  
...  
Keyword(s):  
Late Pleistocene ◽  
Cervus Elaphus ◽  
Red Deer ◽  
Pannonian Basin ◽  
Canis Familiaris ◽  
Mammuthus Primigenius ◽  
Maxillary Bone ◽  
Fluvial Deposits ◽  
Animal Remains ◽  
Woolly Mammoth

Eight anatomically and taxonomically different finds are presented in this paper, and they belong to four taxa: woolly mammoth (Mammuthus primigenius), giant deer (Megaloceros giganteus), red deer (Cervus elaphus), and dog (Canis familiaris). All specimens represent allochthonous Late Pleistocene and Holocene animal remains, and all were dredged during the gravel exploitation at the Sekuline site near Molve (Podravina region, SW Pannonian basin, NE Croatia). Mammoth remains (bone and tusk fragments) were radiocarbon dated, and these are the first absolute dates on mammoths in Croatia. One upper last left deciduous premolar (dP4 sin.) also belongs to the same species. Ascribed to a dog is one well-preserved skull with a peculiar abscess scar on the maxillary bone as the result of an inflammatory process on the carnassial (P4) premolar. The Late Pleistocene cervid remains are giant deer, while the other cervid finds were determined to be red deer of the Holocene age. Morphometrical and taphonomical data are presented for each specimen. Such fossil and recent bone/tooth aggregates are characteristic of fluvial deposits and selective collecting. Although lacking stratigraphic provenance, these finds help to fulfil the gaps in palaeoenvironmental, palaeoecological, and palaeoclimate reconstructions of Podravina and its neighbouring areas.

scholarly journals Remains of large mammals from the Epigravettian site of Yudinovo

2021 ◽  
Vol 325 (1) ◽  
pp. 71-81
Author(s):  
M.V. Sablin ◽  
K.Yu. Iltsevich
Keyword(s):  
Late Pleistocene ◽  
Arctic Fox ◽  
Body Parts ◽  
Large Mammals ◽  
Symbolic System ◽  
Faunal Assemblage ◽  
Stable Isotopic ◽  
Milk Teeth ◽  
Cultural Layers ◽  
Woolly Mammoth

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 interpretation of the existence of the site during the very end of the final part of the Late Pleistocene. In total, 38 268 mammalian bones were identified from cultural layers excavated between 1947–2019. The faunal assemblage is relatively small with a dominance of woolly mammoth and arctic fox, typical of a cold and dry tundra-steppe environment. 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. Traces of gnawing by dogs were recorded on a few bones. We also present in this article the results of the study of so-called “dwellings”, constructed by stacking up body parts and bones that were extracted from carcasses of freshly killed mammoths. We interpret these structures as middens representing the remains of ritually deposited hunted game. It can be assumed that these “dwellings” were probably an important part of the socio-symbolic system of the peoples, who created them.

Rabbits and Bergmann’s rule: how cold was Portugal during the last glaciation?

2019 ◽  
Vol 128 (3) ◽  
pp. 526-549 ◽  
Author(s):  
Simon J M Davis
Keyword(s):  
Late Pleistocene ◽  
Inverse Correlation ◽  
Alternative Interpretation ◽  
Bergmann’S Rule ◽  
Archaeological Sites ◽  
Bergmann's Rule ◽  
The Past ◽  
Last Glaciation ◽  
Size Relationship ◽  
Rabbit Bone

Abstract Osteometric data from > 450 modern wild rabbits, mostly from Portugal, Spain and France, show an inverse correlation between their size and the temperature of the environment, in accordance with Bergmann’s rule. Similar measurements made on some 1660 rabbit bones from 14 Portuguese late Pleistocene and Holocene archaeological sites indicate that rabbits became considerably smaller at the Pleistocene–Holocene boundary. Thus, rabbit size varies or varied with temperature both today and in the past. A direct temperature–size relationship was assumed, and the regression of modern rabbit bone size on temperature was then used to calibrate the temperature equivalent for the change of size of rabbit bones in the past. The result indicates a Last Glacial Maximum to present-day difference, Δt°, of 7 or 8 °C. An alternative interpretation that does not assume a direct temperature–size relationship would indicate that the environment in Portugal 15 000–30 000 years ago was similar to that in northern France today.

CHRONOLOGY OF THE MIS 3 MEGAFAUNA IN SOUTHEASTERN WEST SIBERIA AND THE POSSIBILITY OF LATE SURVIVAL OF THE KHOZARIAN STEPPE MAMMOTH (MAMMUTHUS TROGONTHERII CHOSARICUS)

Radiocarbon ◽  
2021 ◽  
pp. 1-10
Author(s):  
Andrei V Shpansky ◽  
Yaroslav V Kuzmin
Keyword(s):  
Late Pleistocene ◽  
West Siberia ◽  
Mis 3 ◽  
Woolly Rhinoceros ◽  
Mis 5E ◽  
Late Survival ◽  
Woolly Mammoth

ABSTRACT We report a new series of radiocarbon (14C) dates on the MIS 3 megafauna for a previously poorly studied region of southeastern West Siberia. Some species, like woolly mammoth and woolly rhinoceros, and Pleistocene bison and horse, existed throughout the MIS 3 (ca. 29–59 ka cal BP); cave hyaena is dated to ca. 46,400 cal BP. The very late 14C dates on Khozarian steppe elephant (Mammuthus trogontherii chosaricus), ca. 45,100–45,400 cal BP, may indicate the survival of this species in Siberia up to MIS 3. More work is needed to confirm or reject this suggestion. Previously, Khozarian steppe elephant was known in Siberia only at the beginning of the Late Pleistocene (MIS 5e).

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