Temporal and spatial variability of bone collagen stable carbon and nitrogen isotopic ratios of Norwegian reindeer

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14210%2F21%3A00123736" target="_blank" >RIV/00216224:14210/21:00123736 - isvavai.cz</a>

Výsledek na webu

<a href="https://www.sciencedirect.com/science/article/pii/S2352409X21001024?via%3Dihub#" target="_blank" >https://www.sciencedirect.com/science/article/pii/S2352409X21001024?via%3Dihub#</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.jasrep.2021.102890" target="_blank" >10.1016/j.jasrep.2021.102890</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Temporal and spatial variability of bone collagen stable carbon and nitrogen isotopic ratios of Norwegian reindeer

Popis výsledku v původním jazyce

Carbon and nitrogen stable isotopes of reindeer (Rangifer tarandus) bones from three Norwegian modern wild reindeer populations (Setesdal Ryfylke, Hardangervidda and Rondane) were used to investigate variations in δ13C and δ15N between, and within, populations. Each of these reindeer populations lives in different climatic and environmental conditions, thus vegetation and climatic conditions could be linked to their stable isotopic signature. Reindeer bones from several archaeological sites on Hardangervidda representing three chronological ranges (275–350 CE, 11th, and 13th century CE) were then analysed for their stable isotopic composition. No statistically significant differences were found within the populations, but the stable isotopic values differed between populations. Subsequently, these stable isotopic values were used to infer modern climatic conditions to sub-fossil palaeoenvironmental conditions on Hardangervidda.

Název v anglickém jazyce

Temporal and spatial variability of bone collagen stable carbon and nitrogen isotopic ratios of Norwegian reindeer

Popis výsledku anglicky

Carbon and nitrogen stable isotopes of reindeer (Rangifer tarandus) bones from three Norwegian modern wild reindeer populations (Setesdal Ryfylke, Hardangervidda and Rondane) were used to investigate variations in δ13C and δ15N between, and within, populations. Each of these reindeer populations lives in different climatic and environmental conditions, thus vegetation and climatic conditions could be linked to their stable isotopic signature. Reindeer bones from several archaeological sites on Hardangervidda representing three chronological ranges (275–350 CE, 11th, and 13th century CE) were then analysed for their stable isotopic composition. No statistically significant differences were found within the populations, but the stable isotopic values differed between populations. Subsequently, these stable isotopic values were used to infer modern climatic conditions to sub-fossil palaeoenvironmental conditions on Hardangervidda.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

60102 - Archaeology

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2021

Kód důvěrnosti údajů

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

Název periodika

Journal of Archaeological Science : Reports

ISSN

2352-409X

e-ISSN

—

Svazek periodika

37

Číslo periodika v rámci svazku

červen

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

10

Strana od-do

1-10

Kód UT WoS článku

000670214500007

EID výsledku v databázi Scopus

2-s2.0-85103388349