The effect of seaweed fertilisation on sulfur isotope ratios (δ34S) and grain size in barley: implications for agronomy and archaeological research

Introduction Stable sulfur isotope ratios (δ 34 S) in bone collagen are often employed to study the consumption of marine and freshwater fish, wetland grazing, marine foraging patterns, and the possible geographic origins of food sources. However, a recent small-scale crop experiment showed that biofertilisation with seaweed can elevate δ 34 S in Celtic beans by ca. 10 ‰. Consumption of this food could erroneously suggest a marine diet and therefore has important implications for the reconstruction of past diets and dietary origins. However, limited research has so far been undertaken on cereals. Methods To address this issue, a large-scale field trial was undertaken on the Orkney Islands, whereby bere barley (a Scottish landrace, Hordeum vulgare L.) was biofertilised with seaweed at different dosages (25 t/ha, 50 t/ha), with a mineral NPK fertiliser, and left unfertilised as a control. Results The total barley biomass yield was higher and barley grains were enlarged following all fertilisation treatments compared to the control barley. Barley grain and straw from seaweed-fertilised crops had more elevated δ 34 S values by around 2–3 ‰ compared to unfertilised plants, while the NPK-fertilised grains and plants had δ 34 S values 1 ‰ lower. Discussion These results confirm previous hypotheses that seaweed fertilisation can elevate cereal δ 34 S values. The comparatively small δ 34 S difference between control and seaweed fertilised crops in this field trial is likely due to background elevated δ 34 S values in the soil (+12.7 ‰), which in turn may be due to long-term exposure to oceanic-influenced rain and sea spray and/or possible historical application of seaweed, or the underlying bedrock composition. The results of this study show that seaweed fertilisation can increase barley grain sizes and δ 34 S values, and thus should be considered when reconstructing land management and dietary practices in the archaeological record.

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Journal
Frontiers in Environmental Archaeology
Published
2024-11-25
DOI
https://doi.org/10.3389/fearc.2024.1465082
Citations
2
Primary Topic
Archaeology and ancient environmental studies
Type
article
Field-Weighted Citation Impact
3.18
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article

The effect of seaweed fertilisation on sulfur isotope ratios (δ34S) and grain size in barley: implications for agronomy and archaeological research

Magdalena Blanz, Mike J. Church, Peter Martin, Darren Richard Gröcke
2 citations
Frontiers in Environmental Archaeology
Archaeology and ancient environmental studies
3.18
article

The effect of seaweed fertilisation on sulfur isotope ratios (δ34S) and grain size in barley: implications for agronomy and archaeological research

Magdalena Blanz, Mike J. Church, Peter Martin, Darren Richard Gröcke
article en
2 citations

Abstract

Introduction Stable sulfur isotope ratios (δ 34 S) in bone collagen are often employed to study the consumption of marine and freshwater fish, wetland grazing, marine foraging patterns, and the possible geographic origins of food sources. However, a recent small-scale crop experiment showed that biofertilisation with seaweed can elevate δ 34 S in Celtic beans by ca. 10 ‰. Consumption of this food could erroneously suggest a marine diet and therefore has important implications for the reconstruction of past diets and dietary origins. However, limited research has so far been undertaken on cereals. Methods To address this issue, a large-scale field trial was undertaken on the Orkney Islands, whereby bere barley (a Scottish landrace, Hordeum vulgare L.) was biofertilised with seaweed at different dosages (25 t/ha, 50 t/ha), with a mineral NPK fertiliser, and left unfertilised as a control. Results The total barley biomass yield was higher and barley grains were enlarged following all fertilisation treatments compared to the control barley. Barley grain and straw from seaweed-fertilised crops had more elevated δ 34 S values by around 2–3 ‰ compared to unfertilised plants, while the NPK-fertilised grains and plants had δ 34 S values 1 ‰ lower. Discussion These results confirm previous hypotheses that seaweed fertilisation can elevate cereal δ 34 S values. The comparatively small δ 34 S difference between control and seaweed fertilised crops in this field trial is likely due to background elevated δ 34 S values in the soil (+12.7 ‰), which in turn may be due to long-term exposure to oceanic-influenced rain and sea spray and/or possible historical application of seaweed, or the underlying bedrock composition. The results of this study show that seaweed fertilisation can increase barley grain sizes and δ 34 S values, and thus should be considered when reconstructing land management and dietary practices in the archaeological record.

Frontiers in Environmental ArchaeologyVol. 3
University of Vienna (AT), Austrian Academy of Sciences (AT), Durham University (GB), University of the Highlands and Islands (GB)
Openalex Percentile: Top 8%
Archaeology and ancient environmental studies
3.18
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