A sediment sequence (Co1260, 717 cm) from Late Glacial to Holocene of Lake Dojran, located at the border between Greece and F.Y.R. of Macedonia, has been investigated to provide a high-resolution pollen and NPPs analysis. Percentage, concentration and influx values have been interpreted to reconstruct the vegetational dynamics of the last 12500 years. Late Glacial is characterized by steppic taxa replaced by Holocene vegetation after 11500 yr BP. Mesophilous plants dominate for the entire Holocene. The first human trace is clear since 5000 yr BP, but the start of a strong human impact is dated at 2600 yr BP. The data have been also compared with other proxies available for the same core to better comprehend the past climatic dynamics. Geoch...
In this study, we present lipid biomarker and palynological data for a sediment core from Lake Dojra...
This study centres on palaeoenvironmental analysis of the upper part of a long core from the partial...
How have the societies of the past afforded climatic changes? How prolonged dryness, exceptionally c...
A new high-resolution pollen and NPP (non-pollen palynomorph) analysis has been performed on the sed...
A new high-resolution pollen and NPP (non-pollen palynomorph) analysis has been performed on the sed...
A new high-resolution pollen and NPP (non-pollen palynomorph) analysis has been performed on the se...
A new high-resolution pollen and NPP (non- pollen palynomorph) analysis has been performed on the se...
A Late Glacial to Holocene sediment sequence (Co1260, 717 cm) from Lake Dojran, located at the board...
A Late Glacial to Holocene sediment sequence (Co1260, 717 cm) from Lake Dojran, located at the board...
A Late Glacial to Holocene sediment sequence (Co1260, 717 cm) from Lake Dojran, located at the board...
A Late Glacial to Holocene sediment sequence (Co1260, 717 cm) from Lake Dojran, located at the board...
A Late Glacial to Holocene sediment sequence (Co1260, 717 cm) from Lake Dojran, located at the board...
In this study, we present lipid biomarker and palynological data for a sediment core from Lake Dojra...
A Late Glacial to Holocene sediment sequence (Co1260, 717 cm) from Lake Dojran, located at the board...
In this study, we present lipid biomarker and palynological data for a sediment core from Lake Dojra...
In this study, we present lipid biomarker and palynological data for a sediment core from Lake Dojra...
This study centres on palaeoenvironmental analysis of the upper part of a long core from the partial...
How have the societies of the past afforded climatic changes? How prolonged dryness, exceptionally c...
A new high-resolution pollen and NPP (non-pollen palynomorph) analysis has been performed on the sed...
A new high-resolution pollen and NPP (non-pollen palynomorph) analysis has been performed on the sed...
A new high-resolution pollen and NPP (non-pollen palynomorph) analysis has been performed on the se...
A new high-resolution pollen and NPP (non- pollen palynomorph) analysis has been performed on the se...
A Late Glacial to Holocene sediment sequence (Co1260, 717 cm) from Lake Dojran, located at the board...
A Late Glacial to Holocene sediment sequence (Co1260, 717 cm) from Lake Dojran, located at the board...
A Late Glacial to Holocene sediment sequence (Co1260, 717 cm) from Lake Dojran, located at the board...
A Late Glacial to Holocene sediment sequence (Co1260, 717 cm) from Lake Dojran, located at the board...
A Late Glacial to Holocene sediment sequence (Co1260, 717 cm) from Lake Dojran, located at the board...
In this study, we present lipid biomarker and palynological data for a sediment core from Lake Dojra...
A Late Glacial to Holocene sediment sequence (Co1260, 717 cm) from Lake Dojran, located at the board...
In this study, we present lipid biomarker and palynological data for a sediment core from Lake Dojra...
In this study, we present lipid biomarker and palynological data for a sediment core from Lake Dojra...
This study centres on palaeoenvironmental analysis of the upper part of a long core from the partial...
How have the societies of the past afforded climatic changes? How prolonged dryness, exceptionally c...