Paleodietary Patterns of the Cherepakha 13 Site Population (Early Iron Age) in Primorye (Maritime) Province, Russian Far East, based on Stable Isotope Analysis

Radiocarbon ◽  
2018 ◽  
Vol 60 (5) ◽  
pp. 1611-1620 ◽  
Author(s):  
Yaroslav V Kuzmin ◽  
Vsevolod S Panov ◽  
Viacheslav V Gasilin ◽  
Sergei V Batarshev
Keyword(s):  
Stable Isotope ◽  
Iron Age ◽  
Isotope Composition ◽  
Russian Far East ◽  
Isotope Analysis ◽  
Far East ◽  
Bone Collagen ◽  
Early Iron Age ◽  
Terrestrial Mammals ◽  
Maritime Province

ABSTRACTNew paleodietary data were obtained after the discovery and excavation in 2015–2017 of the Cherepakha 13 site in the southern part of Primorye (Maritime) Province in far eastern Russia. The site is located near the coast of Ussuri Bay (Sea of Japan) and belongs to the Yankovsky cultural complex of the Early Iron Age 14C-dated to ca. 3000 BP (ca. 1200 cal BC). The stable isotope composition of the bone collagen for 11 humans and 30 animals was determined. For humans, the following values (with±1 sigma) were yielded: δ13C=–10.2±0.8‰; and δ15N=+12.4±0.3‰. The majority of terrestrial animals show the usual isotopic signals: δ13C=–19.4 ÷ –23.3‰; and δ15N=+4.6÷+6.6‰ (for wolves, up to +10.1‰); dogs, however, have an isotopic composition similar to humans: δ13C= –11.7±1.2‰; and δ15N=+12.4±0.4‰. Marine mammals have common values for pinnipeds: δ13C=–13.7 ÷ –14.6‰; and δ15N=+17.4 ÷ +18.0‰. The main food resources for the population of Cherepakha 13 site were (1) marine mollusks, fish, and mammals; and (2) terrestrial mammals; and possibly C4 plants (domesticated millets).

scholarly journals Chronology of Prehistoric Cultural Complexes of Sakhalin Island (Russian Far East)

Radiocarbon ◽  
2004 ◽  
Vol 46 (1) ◽  
pp. 353-362 ◽  
Author(s):  
Yaroslav V Kuzmin ◽  
Alexander A Vasilevski ◽  
Sergei V Gorbunov ◽  
G S Burr ◽  
A J Timothy Jull ◽  
...  
Keyword(s):  
Middle Ages ◽  
Iron Age ◽  
Russian Far East ◽  
Far East ◽  
Sakhalin Island ◽  
Upper Paleolithic ◽  
Early Iron Age ◽  
Radiocarbon Dates ◽  
Continuous Sequence ◽  
The Middle Ages

A chronological framework for the prehistoric cultural complexes of Sakhalin Island is presented based on 160 radiocarbon dates from 74 sites. The earliest 14C-dated site, Ogonki 5, corresponds to the Upper Paleolithic, about 19,500–17,800 BP. According to the 14C data, since about 8800 BP, there is a continuous sequence of Neolithic, Early Iron Age, and Medieval complexes. The Neolithic existed during approximately 8800–2800 BP. Transitional Neolithic-Early Iron Age complexes are dated to about 2800–2300 BP. The Early Iron Age may be dated to about 2500–1300 BP. The Middle Ages period is dated to approximately 1300–300 BP (VII–XVII centuries AD).

scholarly journals Ancient Beringian paleodiets revealed through multiproxy stable isotope analyses

2020 ◽  
Vol 6 (36) ◽  
pp. eabc1968
Author(s):  
Carrin M. Halffman ◽  
Ben A. Potter ◽  
Holly J. McKinney ◽  
Takumi Tsutaya ◽  
Bruce P. Finney ◽  
...  
Keyword(s):  
Native Americans ◽  
Stable Isotope ◽  
Tooth Enamel ◽  
Isotope Composition ◽  
Isotope Analysis ◽  
Nitrogen Isotope ◽  
Essential Amino Acids ◽  
Bone Collagen ◽  
Carbon And Nitrogen ◽  
Isotope Analyses

The earliest Native Americans have often been portrayed as either megafaunal specialists or generalist foragers, but this debate cannot be resolved by studying the faunal record alone. Stable isotope analysis directly reveals the foods consumed by individuals. We present multi-tissue isotope analyses of two Ancient Beringian infants from the Upward Sun River site (USR), Alaska (~11,500 years ago). Models of fetal bone turnover combined with seasonally-sensitive taxa show that the carbon and nitrogen isotope composition of USR infant bone collagen reflects maternal diets over the summer. Using comparative faunal isotope data, we demonstrate that although terrestrial sources dominated maternal diets, salmon was also important, supported by carbon isotope analysis of essential amino acids and bone bioapatite. Tooth enamel samples indicate increased salmon use between spring and summer. Our results do not support either strictly megafaunal specialists or generalized foragers but indicate that Ancient Beringian diets were complex and seasonally structured.

Bronze-early iron age environment of the Iman River Basin, Russian far east

1994 ◽  
Vol 9 (6) ◽  
pp. 503-513 ◽  
Author(s):  
Natalya B. Verkhovskaya ◽  
Aleksandr S. Kundyshev ◽  
Nikolay A. Kliuev
Keyword(s):  
River Basin ◽  
Iron Age ◽  
Russian Far East ◽  
Far East ◽  
Early Iron Age

Dating and Stable Isotope Analysis of Charred Residues from Neolithic Sites in the Primorye, Russian Far East

Radiocarbon ◽  
2017 ◽  
Vol 59 (2) ◽  
pp. 565-573 ◽  
Author(s):  
Dai Kunikita ◽  
Alexander N Popov ◽  
Boris V Lazin ◽  
Kazuki Morisaki ◽  
Hiroyuki Matsuzaki
Keyword(s):  
Stable Isotope ◽  
Freshwater Fish ◽  
Stable Isotope Analysis ◽  
Food Habits ◽  
Russian Far East ◽  
Isotope Analysis ◽  
Far East ◽  
Nitrogen Isotope ◽  
Carbon And Nitrogen ◽  
The Russian Far East

AbstractThis study attempts to reconstruct food habits through carbon (C) and nitrogen (N) isotope analysis and C/N analysis of charred residues inside pottery from the Primorye in the Russian Far East (Luzanova Sopka 2, Sergeyevka 1, Boisman 2, and Vetka 2 sites). Dates were obtained that were from the later stages of the Rudnaya culture (6980–6485 BP, 7800–7400 cal BP), proto-Boisman type (6760–6330 BP, 7600–7300 cal BP), Boisman culture (6155–4720 BP, 7100–5400 cal BP), and Vetka culture (6030–5870 BP, 6900–6700 cal BP). There are major differences in the carbon and nitrogen isotope ratios between inland sites (δ13C –26.9 to –30.0‰, δ15N 7.6 to 9.3‰) and coastal sites (δ13C –18.1 to –24.2‰, δ15N 9.5 to 14.9‰). The results show that the diet of inland cultures consisted primarily of freshwater fish and terrestrial animals and plants, whereas that of coastal cultures consisted mainly of marine organisms.

Civilizational Border

2019 ◽  
pp. 110-150
Author(s):  
Alyssa M. Park
Keyword(s):  
Russian Far East ◽  
Far East ◽  
Border Region ◽  
Korean Population ◽  
Legal Regime ◽  
Korean Chinese ◽  
Laws And Policies ◽  
Asian Migration ◽  
Maritime Province ◽  
The Russian Far East

This chapter examines Russian officials’ debates and policies regarding Koreans in the Maritime Province from 1880 to the 1920s. It sees these policies as part of a broader project to revise the practice of plural jurisdiction, in which the empire ruled its vast territories and peoples through a flexible legal regime. Amidst a growing wave of nativist sentiment, officials aimed to standardize the privileges respectively held by subjects and foreigners and to institutionalize borders. In the Russian Far East, suspicions about the interference of the Korean, Chinese, and Japanese governments led officials to categorize the resident Korean population as subjects and aliens, experiment with policies to ban the settlement of Koreans in the border region, institute border and passport laws, and discuss the benefits and dangers of continued Asian migration to Russia. The chapter further explores how Koreans subverted these laws and policies to their own ends.

scholarly journals Revision of rock fossils of Dryinidae and Embolemidae (Hymenoptera: Chrysidoidea)

Zootaxa ◽  
2010 ◽  
Vol 2499 (1) ◽  
pp. 21 ◽  
Author(s):  
MASSIMO OLMI ◽  
ALEXANDER P. RASNITSYN ◽  
ADALGISA GUGLIELMINO
Keyword(s):  
Early Cretaceous ◽  
Upper Cretaceous ◽  
Middle Miocene ◽  
Russian Far East ◽  
Far East ◽  
Left Bank ◽  
Rock Unit ◽  
Central Mongolia ◽  
Lake Deposits ◽  
Maritime Province

New fossil taxa of Embolemidae and Dryinidae (Hymenoptera: Chrysidoidea) are described. For Embolemidae, Embolemopsis baissensis n. gen. n. sp. and Baissobius minutus n. sp., are described from Central Siberia, West Transbaikalia, left bank of Vitim River (facing downstream), Baissa, lake deposits from earlier Early Cretaceous (Neocomian stage) (130–140 mybp). For Dryinidae, Anteonopsis antiquus n. gen. n. sp., Bocchus ? cenomanianus n. sp. and Gonatopus ? cretacicus n. sp., are described from Siberia, Magadan Region, Obeschchayushchiyi, tuffaceous deposits from Upper Cretaceous (Cenomanian) (90–95 mybp); Deinodryinus ? aptianus n. sp., is described from Central Mongolia, Bayanhongor Aimag, 5–8 Km N Bon Tsagan Nuur Lake, from impressed in lake deposits of the Khurilt rock unit probably of Aptian (Early Cretaceous) (100–115 mybp). In addition, an unidentified fossil belonging to Deinodryinus ? or Dryinus ? is recorded from Russian Far East, Maritime Province, Velikaya Kema (later Earlier or early Middle Miocene) (about 30 mybp). The known species of Baissobius Rasnitsyn are reviewed and a key is presented.

Evaluating bone collagen extraction methods for stable isotope analysis in dietary studies

2007 ◽  
Vol 34 (11) ◽  
pp. 1824-1829 ◽  
Author(s):  
Marie Louise S. Jørkov ◽  
Jan Heinemeier ◽  
Niels Lynnerup
Keyword(s):  
Stable Isotope ◽  
Stable Isotope Analysis ◽  
Isotope Analysis ◽  
Extraction Methods ◽  
Bone Collagen
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