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The case-studies presented here show that luminescence approaches are a valuable tool to reconstruct landscape histories.
Optically stimulated luminescence dated sand dunes and Pleistocene beach ridges in northwest Ohio are used to reconstruct landscape modification more than 5000 yr after deglaciation.
This is particularly true for historical landscapes, where the relationship between viewer location and view may be one of the few recoverable elements available to reconstruct landscape meaning.
Few studies have aimed to reconstruct landscape change in the area of Eretria (South Central Euboea, Greece) during the last 6000 years.
A paleosol sequence in the Teotihuacan valley was studied in order to reconstruct landscape evolution during the Late Pleistocene Holocene, in a cut belonging to a river gully (San Pablo).
Old maps and aerial photographs from 1950s and today were used to reconstruct landscape patterns in four time-steps to investigate how present plant species richness relates to past grassland extent and decline in old and new grassland habitats.
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The study of how prehistoric residents of the area lived will try to reconstruct landscapes from the Paleo-Indian Period, 10,000 to 12,000 year ago.
Investigating these sediment archives, we reconstructed landscape evolution for the Upper Guadalentín Basin, SE Spain, placing recent erosion processes in a landscape evolution context.
The reconstructed landscape near the ancient city of Assur is used as the example setting to test the effectiveness of simulated cultivation strategies.
Being compared with the previously reconstructed landscape and climate dynamics for the sedimentary succession of Lake Kotokel for this time interval, the above parameters reveal that the Lake Baunt bottom sediments reliably fix the regional paleoclimate signal.
This can assist with targeted field sampling strategies for full dating back in the laboratory, for example when the study is concerned with reconstructing landscape dynamics during a specific time period.
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