Tracing chalcolithic population mobility using strontium isotopes and proteomics at Gumelnita site, Romania

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F25%3A00141664" target="_blank" >RIV/00216224:14310/25:00141664 - isvavai.cz</a>

Výsledek na webu

<a href="https://www.nature.com/articles/s41598-025-05671-0" target="_blank" >https://www.nature.com/articles/s41598-025-05671-0</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1038/s41598-025-05671-0" target="_blank" >10.1038/s41598-025-05671-0</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Tracing chalcolithic population mobility using strontium isotopes and proteomics at Gumelnita site, Romania

Popis výsledku v původním jazyce

The Kodjadermen-Gumelnita-Karonovo VI human group (KGK VI) reached its maximal extension around 4500 BC, covering a large area comprised between southern Ukraine and northern Greece. Afterward, its distribution gradually receded, before vanishing altogether at the end of the fifth - early fourth millenniums BC. This study seeks to investigate the role of individual mobility during this process by performing strontium isotopic analyses on the human remains found at Gumelnita, Romania. It provides 87Sr/86Sr values for 21 human tooth enamel samples from 17 different individuals, together with those of 60 plant samples from 20 different locations (15 in Romania and 5 in Bulgaria) that were used to create a bioavailable strontium (BASr) baseline of the region. To obtain reliable sex estimations, proteomic analysis of amelogenin of human tooth enamel were also performed on seven individuals. According to the results, four individuals, three females and one male, should be considered as non-local, and may have spent their childhood on the southern bank of the Danube River. These data suggest that individual mobility was particularly prevalent during the last centuries of the fifth millennium, when the KGK VI complex was undergoing a process of disintegration. Main Text.

Název v anglickém jazyce

Tracing chalcolithic population mobility using strontium isotopes and proteomics at Gumelnita site, Romania

Popis výsledku anglicky

The Kodjadermen-Gumelnita-Karonovo VI human group (KGK VI) reached its maximal extension around 4500 BC, covering a large area comprised between southern Ukraine and northern Greece. Afterward, its distribution gradually receded, before vanishing altogether at the end of the fifth - early fourth millenniums BC. This study seeks to investigate the role of individual mobility during this process by performing strontium isotopic analyses on the human remains found at Gumelnita, Romania. It provides 87Sr/86Sr values for 21 human tooth enamel samples from 17 different individuals, together with those of 60 plant samples from 20 different locations (15 in Romania and 5 in Bulgaria) that were used to create a bioavailable strontium (BASr) baseline of the region. To obtain reliable sex estimations, proteomic analysis of amelogenin of human tooth enamel were also performed on seven individuals. According to the results, four individuals, three females and one male, should be considered as non-local, and may have spent their childhood on the southern bank of the Danube River. These data suggest that individual mobility was particularly prevalent during the last centuries of the fifth millennium, when the KGK VI complex was undergoing a process of disintegration. Main Text.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10600 - Biological sciences

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2025

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Scientific Reports

ISSN

2045-2322

e-ISSN

—

Svazek periodika

15

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

DE - Spolková republika Německo

Počet stran výsledku

22

Strana od-do

1-22

Kód UT WoS článku

001522988200008

EID výsledku v databázi Scopus

2-s2.0-105009973174