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The first example (Kugelstattmoos, Bavarian Forest, Germany) combines a Holocene pollen diagram derived from a small mire with late medieval/early modern times charcoal spectra from charcoal production sites which are situated on the margin of the mire.
We report pollen and charcoal records from Vega Ñandú (∼ 51°0′S, 72°45′W), a small mire located near the modern forest-steppe ecotone in Torres del Paine National Park, southern Chile.
Five megalithic graves of the Funnel Beaker Culture are located very close, i.e. ca. 100 m south-west of a small mire which was investigated for pollen and charcoal records.
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The pollen sites are small mires or larger forested peat bogs and thus mostly reflect local conditions.
A case study comparing the off-site and on-site pollen records from the Vladař hillfort (Hallstatt) is presented to demonstrate the local signal of the pollen profiles of small mires.
In valleys where clastic input overreached the accommodation space production (A/S < 1), clastics filled all the available accommodation and no or small mires disturbed by fluvial deposition developed.
Charcoal samples were taken in a spatially detailed manner during excavation, as well as a new pollen core from a small spring mire directly next to the site.
Montenegro, small and mired by organized crime, is still on an upward trajectory.
Peat and lake sediments as well as a nearby soil catena were sampled to reconstruct the environmental history of a small infilled lake basin (mire) in the central alpine foreland of Switzerland.
Mostly small but long-lasting mires developed in sedimentary shadows located along the valley margins or in smaller valleys away from the main clastic transport and fluvial dynamics.
Two are from mires with small pollen source areas close to (< 100 m) and distant from (≥ 1500 m) probable farming activities.
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