Pollen diagrams from mountain lakes and marshes in SW Turkey show evidence of intensive anthropogenic influence in the landscape between 3500 and 1300 BP. Three cores from within the territory of the classical city Sagalassos (Western Taurus, Pisidia) were palynologically analysed to make a reconstruction of the past vegetation in the territory of Sagalassos and to estimate the impact of its inhabitants on the landscape in Pisidia. Two cores originate from an intramontane marsh (Gravgaz; elevation 1215 m) and one from a seasonal intramontane lake (Canakh; elevation 1030 m). Human acitivity is apparent from c. 2530 BP in the pollen diagrams. A deforestation phase/'disturbance' phase (from c. 2530 BP/c. 2480 BP till c. 2280 BP/c. 2270 BP), an...
The Marmara region in northwestern Turkey provides a unique opportunity for studying the vegetation ...
Late Holocene local vegetation succession is reconstructed in two different sites in a small-scale o...
Anatolia is characterized by a very complex history of climate and human related vegetation change, ...
Pollen diagrams from mountain lakes and marshes in SW Turkey show evidence of intensive anthropogeni...
Pollen diagrams from mountain lakes and marshes in SW Turkey show evidence of intensive anthropogeni...
Pollen diagrams from mountain lakes and marshes in SW Turkey show evidence of intensive anthropogeni...
Pollen diagrams from mountain lakes and marshes in SW Turkey show evidence of intensive anthropogeni...
Past vegetation change and the influence of climate change and anthropogenic pressure during the Hol...
A well-dated pollen diagram from Gravgaz marsh, near the archaeological site of Sagalassos (western ...
Late Holocene vegetation and geomorphological history is reconstructed from a 800 cm long high-resol...
Anatolia forms a bridge between Europe, Africa and Asia and is influenced by all three continents in...
Northwestern Turkey and the southern Levant are key regions for studying vegetation and climate deve...
Percentage, concentration and accumulation pollen data together with diatom and non-siliceous microf...
Percentage, concentration and accumulation pollen data together with diatom and non-siliceous microf...
Annually laminated sediments from Lake Van, spanning about 13000 varve years, were sampled for stabl...
The Marmara region in northwestern Turkey provides a unique opportunity for studying the vegetation ...
Late Holocene local vegetation succession is reconstructed in two different sites in a small-scale o...
Anatolia is characterized by a very complex history of climate and human related vegetation change, ...
Pollen diagrams from mountain lakes and marshes in SW Turkey show evidence of intensive anthropogeni...
Pollen diagrams from mountain lakes and marshes in SW Turkey show evidence of intensive anthropogeni...
Pollen diagrams from mountain lakes and marshes in SW Turkey show evidence of intensive anthropogeni...
Pollen diagrams from mountain lakes and marshes in SW Turkey show evidence of intensive anthropogeni...
Past vegetation change and the influence of climate change and anthropogenic pressure during the Hol...
A well-dated pollen diagram from Gravgaz marsh, near the archaeological site of Sagalassos (western ...
Late Holocene vegetation and geomorphological history is reconstructed from a 800 cm long high-resol...
Anatolia forms a bridge between Europe, Africa and Asia and is influenced by all three continents in...
Northwestern Turkey and the southern Levant are key regions for studying vegetation and climate deve...
Percentage, concentration and accumulation pollen data together with diatom and non-siliceous microf...
Percentage, concentration and accumulation pollen data together with diatom and non-siliceous microf...
Annually laminated sediments from Lake Van, spanning about 13000 varve years, were sampled for stabl...
The Marmara region in northwestern Turkey provides a unique opportunity for studying the vegetation ...
Late Holocene local vegetation succession is reconstructed in two different sites in a small-scale o...
Anatolia is characterized by a very complex history of climate and human related vegetation change, ...