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6 results for “livestock history”
FIG. 3 in Rodents in grassland habitats: does livestock grazing matter? A comparison of two Alpine sites with different grazing histories
FIG. 3. — Rank/abundance plots for the Carex sempervirens (CS) and Dactylis glomerata (DG) pastoral types. Plots are based on data published by Cavallero et al. (2003, 2007) and refer to: A, the pastoral type of the lightly grazed areas (CS type); B, the abandoned, formerly intensively grazed areas (DG type).
FIG. 2 in Rodents in grassland habitats: does livestock grazing matter? A comparison of two Alpine sites with different grazing histories
FIG. 2. — Box and whisker plots showing the median, first and third quartile and the minimum and maximum values for the log of the captured animals in each plot. Outliers are plotted as open circles.
FIG. 1 in Rodents in grassland habitats: does livestock grazing matter? A comparison of two Alpine sites with different grazing histories
FIG. 1. — Simplified land use in the study area overlaid onto a topographic map. Sampling plots were located within the lightly grazed and in the intensively grazed areas. For the latter areas, in particular, plots were located in sites not used by cattle at present. Plot locations are approximate since we could not leave traps unattended between sessions, with the result that, for each session, plots were not exactly in the same locations as the one before.
FIG. 4 in Rodents in grassland habitats: does livestock grazing matter? A comparison of two Alpine sites with different grazing histories
FIG. 4. — Apodemus Spp. caught during the study.
Data from: Long livestock farming history and human landscape shaping revealed by lake sediment DNA
The reconstruction of human-driven, Earth-shaping dynamics is important for understanding past human/environment interactions and for helping human societies that currently face global changes. However, it is often challenging to distinguish the effects of the climate from human activities on environmental changes. Here we evaluate an approach based on DNA metabarcoding used on lake sediments to provide the first high-resolution reconstruction of plant cover and livestock farming history since the Neolithic Period. By comparing these data with a previous reconstruction of erosive event frequency, we show that the most intense erosion period was caused by deforestation and overgrazing by sheep and cowherds during the Late Iron Age and Roman Period. Tracking plants and domestic mammals using lake sediment DNA (lake sedDNA) is a new, promising method for tracing past human practices, and it provides a new outlook of the effects of anthropogenic factors on landscape-scale changes.
Data from: Long livestock farming history and human landscape shaping revealed by lake sediment DNA
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