Compound‐specific δ15N amino acid signals in palaeosols as indicators of early land use
A preliminary study
Bibliographic Data
| ID | 12429648 |
|---|---|
| Authors | Ian A Simpson (0000-0003-2447-7877, University of Stirling, corresponding author), R Bol, Stephen J Dockrill (University of Bradford), Klaus J Petzke (German Institute of Human Nutrition), K-J Petzke, R P Evershed (0000-0002-9483-2750, University of Bristol) |
| Year | 1997 |
| Volume | 4 |
| Issue | 3 |
| Pages | 147-152 |
| Publication date | 1997-09-01 |
| Open Access | Yes |
| Type | ARTICLE |
| Venue | Archaeological Prospection (JOURNAL) |
| Journal identifiers | ISSN: 1075-2196 • E-ISSN: 1099-0763 |
| Publisher | Wiley (PUBLISHER • GB) |
| DOI | 10.1002/(sici)1099-0763(199709)4:3<147::aid-arp74>3.3.co;2-x |
| OpenAlex | W4244864814 |
| Language | EN |
Compound-specific δ15N amino acid signals in soils demonstrate differences between manured grassland, unmanured grassland and continuous cereal cultivation under long-term experimental land-use control conditions, with δ15N values of hydrophobic amino acids providing the most distinctive signals. Analysis of anthropogenic palaeosols from Orkney demonstrates that such signals are retained in archaeological contexts. Relict medieval to early modern soils retain signals that suggest cereal cultivation, with a later phase of manured grassland; fossil Bronze Age soils retain signals that suggest continuous cereal cultivation only. These analyses are the first identification of compound-specific δ15N amino acid signals in archaeological soils. © 1997 John Wiley & Sons, Ltd
Amino acid · Archaeology · Biology · Geography · Grassland · Soil water · Archaeology and ancient environmental studies · Chemistry · Geology and Paleoclimatology Research · Isotope Analysis in Ecology · Ecology · Geology · Soil Science
| Highly cited | No |
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