Carbon and nitrogen isotopic ratios in archaeological and modern Swiss fish as possible markers for diachronic anthropogenic activity in freshwater ecosystems. (December 2016)

• Record Type: Journal Article
• Authors: Häberle, Simone; Nehlich, Olaf; Fuller, Benjamin T.; Schibler, Jörg; Van Neer, Wim; Plogmann, Heide Hüster
• Is Part Of: Journal of archaeological science. Volume 10(2016)
• Page Start: 411
• Page End: 423
• Publication Date: 2016-12
• Subjects: Freshwater fish -- Middle Ages -- Stable isotope analysis -- Archaeoichthyology -- Water condition -- Pollution -- Human impact; Archaeology -- Periodicals; Archaeology -- Research -- Periodicals; 930.1
• DOI: 10.1016/j.jasrep.2016.10.012
• Languages: English
• ISSNs: 2352-409X

Abstract

Abstract: The aim of this study is to investigate isotopic variability in archaeological ( n = 85) and modern ( n = 29) freshwater fish specimens from Switzerland. Here, carbon (δ 13 C) and nitrogen (δ 15 N) stable isotope ratio analysis was performed on bone collagen samples of pike ( Esox lucius), perch (Perca fluviatilis), barbel (Barbus barbus), roach (Rutilus rutilus) and carp (Cyprinus carpio ) from eleven archaeological (11th to 18/19th centuries CE) and modern sites. The archaeological vs. modern fish data revealed significant isotopic differences for pike, perch and barbel (δ 13 C p ≤ 0.03; δ 15 N p ≤ 0.008), and provides possible evidence for a temporal change in Swiss aquatic ecosystems from Medieval to modern times. In comparison to archaeological fish (δ 13 C mean ± SD; − 23.3 ± 1.6‰; δ 15 N mean ± SD; 8.3 ± 1.8‰), the modern fish samples show decreased δ 13 C and increased δ 15 N values (δ 13 C mean ± SD; − 27.4 ± 2.3‰; δ 15 N mean ± SD; 12.5 ± 4.1‰) that can be associated with anthropogenic effects: fossil fuel combustion, deforestation and organic waste in the form of sewage and fertilizers. The isotopic signatures of archaeological fish remains indicate a local fishery practice, but also the exploitation of distant fishing grounds and freshwater fish transportation. Furthermore, a diachronic isotopic trend is observed in young perch from sites in Basel, dating between the 12th and 15/16th centuries CE, and the isotopic data from the Rhine freshwater fish (18/19th century CE) suggests that a significant shift in the river's trophic state was possibly caused by organic pollution from urban and industrial wastewater. This retrospective research illustrates possible natural processes and human activities which can cause differences in fish stable isotope data and highlights the ability to elucidate changes in past bodies of water. Furthermore, this study provides an interpretative framework for additional palaeoenvironmental studies and modern restoration projects focused on freshwater ecosystems. Highlights: Isotopic signatures can reconstruct past aquatic ecosystems in Switzerland. Significant isotopic differences between modern & archaeological fish species Archaeological fish results indicate possible water pollution since c.18th/19th CE. Modern fish have ↓ δ 13 C and ↑ δ 15 N values associated anthropogenic activity.