UCL Discovery
UCL home » Library Services » Electronic resources » UCL Discovery

Nitrogen palaeo-isoscapes: Changing spatial gradients of faunal δ^{15}N in late Pleistocene and early Holocene Europe

Reade, Hazel; Tripp, Jennifer A; Frémondeau, Delphine; Sayle, Kerry L; Higham, Thomas FG; Street, Martin; Stevens, Rhiannon E; (2023) Nitrogen palaeo-isoscapes: Changing spatial gradients of faunal δ^{15}N in late Pleistocene and early Holocene Europe. PLoS One , 18 (2) , Article e0268607. 10.1371/journal.pone.0268607. Green open access

[thumbnail of Stevens_Nitrogen palaeo-isoscapes_VoR2.pdf]
Preview
Text
Stevens_Nitrogen palaeo-isoscapes_VoR2.pdf

Download (3MB) | Preview

Abstract

Nitrogen isotope ratio analysis (δ15N) of animal tissue is widely used in archaeology and palaeoecology to investigate diet and ecological niche. Data interpretations require an understanding of nitrogen isotope compositions at the base of the food web (baseline δ15N). Significant variation in animal δ15N has been recognised at various spatiotemporal scales and related to changes both in baseline δ15N, linked to environmental and climatic influence on the terrestrial nitrogen cycle, and animal ecology. Isoscapes (models of isotope spatial variation) have proved a useful tool for investigating spatial variability in biogeochemical cycles in present-day marine and terrestrial ecosystems, but so far, their application to palaeo-data has been more limited. Here, we present time-sliced nitrogen isoscapes for late Pleistocene and early Holocene Europe (c. 50,000 to 10,000 years BP) using herbivore collagen δ15N data. This period covers the Last Glacial-Interglacial Transition, during which significant variation in the terrestrial nitrogen cycle occurred. We use generalized linear mixed modelling approaches for interpolation and test models which both include and exclude climate covariate data. Our results show clear changes in spatial gradients of δ15N through time. Prediction of the lowest faunal δ15N values in northern latitudes after, rather than during, the Last Glacial Maximum is consistent with the Late Glacial Nitrogen Excursion (LGNE). We find that including climatic covariate data does not significantly improve model performance. These findings have implications for investigating the drivers of the LGNE, which has been linked to increased landscape moisture and permafrost thaw, and for understanding changing isotopic baselines, which are fundamental for studies investigating diets, niche partitioning, and migration of higher trophic level animals.

Type: Article
Title: Nitrogen palaeo-isoscapes: Changing spatial gradients of faunal δ^{15}N in late Pleistocene and early Holocene Europe
Location: United States
Open access status: An open access version is available from UCL Discovery
DOI: 10.1371/journal.pone.0268607
Publisher version: https://doi.org/10.1371/journal.pone.0268607
Language: English
Additional information: © 2023 Reade et al. This is an open access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0/).
UCL classification: UCL
UCL > Provost and Vice Provost Offices > UCL SLASH
UCL > Provost and Vice Provost Offices > UCL SLASH > Faculty of S&HS
UCL > Provost and Vice Provost Offices > UCL SLASH > Faculty of S&HS > Institute of Archaeology
URI: https://discovery.ucl.ac.uk/id/eprint/10164590
Downloads since deposit
43Downloads
Download activity - last month
Download activity - last 12 months
Downloads by country - last 12 months

Archive Staff Only

View Item View Item