The Experts below are selected from a list of 309 Experts worldwide ranked by ideXlab platform
Marc Waelkens - One of the best experts on this subject based on the ideXlab platform.
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Man, vegetation and climate during the Holocene in the territory of Sagalassos, Western Taurus Mountains, SW Turkey
Vegetation History and Archaeobotany, 2012Co-Authors: Johan Bakker, Etienne Paulissen, David Kaniewski, Véronique Laet, Gert Verstraeten, Marc WaelkensAbstract:Past vegetation change and the influence of climate change and anthropogenic pressure during the Holocene is constructed from a series of palynological records sampled from three locations within the territory of the antique site of Sagalassos. The disappearance of the original deciduous oak woodlands and increases in anthropogenic indicator species around 5300 and 4300 b.c. correspond with an increase in settlements in the region. A period of drought following the deforestation may have hampered the recovery of deciduous oak. The timing of the onset of the Beyşehir Occupation Phase (BO-Phase) in the territory differs between locations, estimates ranging from ca. 1000–800 b.c. to the start of the Hellenistic period (334 b.c. ). The most intense period of arboriculture coincides with the Roman and late-Roman periods. Increases in human pressure on the landscape as reflected in the pollen record correspond with an increased rate of sedimentation and fire activity. The timing of the end of the BO-Phase again differs between locations. Estimates range from the 4th century a.d. to the mid 7th century a.d. , when a region-wide shift to Dry Environmental Conditions is observed. Numerical analyses show that post BO-Phase vegetation change is largely driven by climate and displays a succession of Dry and wet periods that coincided with well-defined European climate shifts, including the Medieval Climate Anomaly and the Little Ice Age. Current agricultural activities in the region are of a very recent (20th century) origin.
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Man, vegetation and climate during the Holocene in the territory of Sagalassos, Western Taurus Mountains, SW Turkey
Vegetation History and Archaeobotany, 2011Co-Authors: Johan Bakker, Etienne Paulissen, David Kaniewski, Véronique Laet, Gert Verstraeten, Marc WaelkensAbstract:Past vegetation change and the influence of climate change and anthropogenic pressure during the Holocene is constructed from a series of palynological records sampled from three locations within the territory of the antique site of Sagalassos. The disappearance of the original deciduous oak woodlands and increases in anthropogenic indicator species around 5300 and 4300 BC, correspond with an increase in settlements in the region. A period of drought, following the deforestation may have hampered the recovery of deciduous oak. The timing of the onset of the Beysehir Occupation Phase (BO-Phase) in the territory differs between locations, estimates ranging from c. 1000-800 BC to the start of the Hellenistic period (334 BC). The most intense period of arboriculture coincides with the Roman and late-Roman periods. Increases in human pressure on the landscape as reflected in the pollen record correspond with an increased rate of sedimentation and fire activity. The timing of the end of the BO-Phase again differs between locations. Estimates range from the 4th century AD to the mid 7th century AD, when a region-wide shift to Dry Environmental Conditions is observed. Numerical analyses show that post BO-Phase vegetation change is largely driven by climate and displays a succession of Dry and wet periods that coincided with well-defined European climate shifts, including the Medieval Climate Anomaly and the Little Ice Age. Current agricultural activities in the region are of a very recent (20th century) origin.status: publishe
Johan Bakker - One of the best experts on this subject based on the ideXlab platform.
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Man, vegetation and climate during the Holocene in the territory of Sagalassos, Western Taurus Mountains, SW Turkey
Vegetation History and Archaeobotany, 2012Co-Authors: Johan Bakker, Etienne Paulissen, David Kaniewski, Véronique Laet, Gert Verstraeten, Marc WaelkensAbstract:Past vegetation change and the influence of climate change and anthropogenic pressure during the Holocene is constructed from a series of palynological records sampled from three locations within the territory of the antique site of Sagalassos. The disappearance of the original deciduous oak woodlands and increases in anthropogenic indicator species around 5300 and 4300 b.c. correspond with an increase in settlements in the region. A period of drought following the deforestation may have hampered the recovery of deciduous oak. The timing of the onset of the Beyşehir Occupation Phase (BO-Phase) in the territory differs between locations, estimates ranging from ca. 1000–800 b.c. to the start of the Hellenistic period (334 b.c. ). The most intense period of arboriculture coincides with the Roman and late-Roman periods. Increases in human pressure on the landscape as reflected in the pollen record correspond with an increased rate of sedimentation and fire activity. The timing of the end of the BO-Phase again differs between locations. Estimates range from the 4th century a.d. to the mid 7th century a.d. , when a region-wide shift to Dry Environmental Conditions is observed. Numerical analyses show that post BO-Phase vegetation change is largely driven by climate and displays a succession of Dry and wet periods that coincided with well-defined European climate shifts, including the Medieval Climate Anomaly and the Little Ice Age. Current agricultural activities in the region are of a very recent (20th century) origin.
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Man, vegetation and climate during the Holocene in the territory of Sagalassos, Western Taurus Mountains, SW Turkey
Vegetation History and Archaeobotany, 2011Co-Authors: Johan Bakker, Etienne Paulissen, David Kaniewski, Véronique Laet, Gert Verstraeten, Marc WaelkensAbstract:Past vegetation change and the influence of climate change and anthropogenic pressure during the Holocene is constructed from a series of palynological records sampled from three locations within the territory of the antique site of Sagalassos. The disappearance of the original deciduous oak woodlands and increases in anthropogenic indicator species around 5300 and 4300 BC, correspond with an increase in settlements in the region. A period of drought, following the deforestation may have hampered the recovery of deciduous oak. The timing of the onset of the Beysehir Occupation Phase (BO-Phase) in the territory differs between locations, estimates ranging from c. 1000-800 BC to the start of the Hellenistic period (334 BC). The most intense period of arboriculture coincides with the Roman and late-Roman periods. Increases in human pressure on the landscape as reflected in the pollen record correspond with an increased rate of sedimentation and fire activity. The timing of the end of the BO-Phase again differs between locations. Estimates range from the 4th century AD to the mid 7th century AD, when a region-wide shift to Dry Environmental Conditions is observed. Numerical analyses show that post BO-Phase vegetation change is largely driven by climate and displays a succession of Dry and wet periods that coincided with well-defined European climate shifts, including the Medieval Climate Anomaly and the Little Ice Age. Current agricultural activities in the region are of a very recent (20th century) origin.status: publishe
Véronique Laet - One of the best experts on this subject based on the ideXlab platform.
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Man, vegetation and climate during the Holocene in the territory of Sagalassos, Western Taurus Mountains, SW Turkey
Vegetation History and Archaeobotany, 2012Co-Authors: Johan Bakker, Etienne Paulissen, David Kaniewski, Véronique Laet, Gert Verstraeten, Marc WaelkensAbstract:Past vegetation change and the influence of climate change and anthropogenic pressure during the Holocene is constructed from a series of palynological records sampled from three locations within the territory of the antique site of Sagalassos. The disappearance of the original deciduous oak woodlands and increases in anthropogenic indicator species around 5300 and 4300 b.c. correspond with an increase in settlements in the region. A period of drought following the deforestation may have hampered the recovery of deciduous oak. The timing of the onset of the Beyşehir Occupation Phase (BO-Phase) in the territory differs between locations, estimates ranging from ca. 1000–800 b.c. to the start of the Hellenistic period (334 b.c. ). The most intense period of arboriculture coincides with the Roman and late-Roman periods. Increases in human pressure on the landscape as reflected in the pollen record correspond with an increased rate of sedimentation and fire activity. The timing of the end of the BO-Phase again differs between locations. Estimates range from the 4th century a.d. to the mid 7th century a.d. , when a region-wide shift to Dry Environmental Conditions is observed. Numerical analyses show that post BO-Phase vegetation change is largely driven by climate and displays a succession of Dry and wet periods that coincided with well-defined European climate shifts, including the Medieval Climate Anomaly and the Little Ice Age. Current agricultural activities in the region are of a very recent (20th century) origin.
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Man, vegetation and climate during the Holocene in the territory of Sagalassos, Western Taurus Mountains, SW Turkey
Vegetation History and Archaeobotany, 2011Co-Authors: Johan Bakker, Etienne Paulissen, David Kaniewski, Véronique Laet, Gert Verstraeten, Marc WaelkensAbstract:Past vegetation change and the influence of climate change and anthropogenic pressure during the Holocene is constructed from a series of palynological records sampled from three locations within the territory of the antique site of Sagalassos. The disappearance of the original deciduous oak woodlands and increases in anthropogenic indicator species around 5300 and 4300 BC, correspond with an increase in settlements in the region. A period of drought, following the deforestation may have hampered the recovery of deciduous oak. The timing of the onset of the Beysehir Occupation Phase (BO-Phase) in the territory differs between locations, estimates ranging from c. 1000-800 BC to the start of the Hellenistic period (334 BC). The most intense period of arboriculture coincides with the Roman and late-Roman periods. Increases in human pressure on the landscape as reflected in the pollen record correspond with an increased rate of sedimentation and fire activity. The timing of the end of the BO-Phase again differs between locations. Estimates range from the 4th century AD to the mid 7th century AD, when a region-wide shift to Dry Environmental Conditions is observed. Numerical analyses show that post BO-Phase vegetation change is largely driven by climate and displays a succession of Dry and wet periods that coincided with well-defined European climate shifts, including the Medieval Climate Anomaly and the Little Ice Age. Current agricultural activities in the region are of a very recent (20th century) origin.status: publishe
Etienne Paulissen - One of the best experts on this subject based on the ideXlab platform.
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Man, vegetation and climate during the Holocene in the territory of Sagalassos, Western Taurus Mountains, SW Turkey
Vegetation History and Archaeobotany, 2012Co-Authors: Johan Bakker, Etienne Paulissen, David Kaniewski, Véronique Laet, Gert Verstraeten, Marc WaelkensAbstract:Past vegetation change and the influence of climate change and anthropogenic pressure during the Holocene is constructed from a series of palynological records sampled from three locations within the territory of the antique site of Sagalassos. The disappearance of the original deciduous oak woodlands and increases in anthropogenic indicator species around 5300 and 4300 b.c. correspond with an increase in settlements in the region. A period of drought following the deforestation may have hampered the recovery of deciduous oak. The timing of the onset of the Beyşehir Occupation Phase (BO-Phase) in the territory differs between locations, estimates ranging from ca. 1000–800 b.c. to the start of the Hellenistic period (334 b.c. ). The most intense period of arboriculture coincides with the Roman and late-Roman periods. Increases in human pressure on the landscape as reflected in the pollen record correspond with an increased rate of sedimentation and fire activity. The timing of the end of the BO-Phase again differs between locations. Estimates range from the 4th century a.d. to the mid 7th century a.d. , when a region-wide shift to Dry Environmental Conditions is observed. Numerical analyses show that post BO-Phase vegetation change is largely driven by climate and displays a succession of Dry and wet periods that coincided with well-defined European climate shifts, including the Medieval Climate Anomaly and the Little Ice Age. Current agricultural activities in the region are of a very recent (20th century) origin.
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Man, vegetation and climate during the Holocene in the territory of Sagalassos, Western Taurus Mountains, SW Turkey
Vegetation History and Archaeobotany, 2011Co-Authors: Johan Bakker, Etienne Paulissen, David Kaniewski, Véronique Laet, Gert Verstraeten, Marc WaelkensAbstract:Past vegetation change and the influence of climate change and anthropogenic pressure during the Holocene is constructed from a series of palynological records sampled from three locations within the territory of the antique site of Sagalassos. The disappearance of the original deciduous oak woodlands and increases in anthropogenic indicator species around 5300 and 4300 BC, correspond with an increase in settlements in the region. A period of drought, following the deforestation may have hampered the recovery of deciduous oak. The timing of the onset of the Beysehir Occupation Phase (BO-Phase) in the territory differs between locations, estimates ranging from c. 1000-800 BC to the start of the Hellenistic period (334 BC). The most intense period of arboriculture coincides with the Roman and late-Roman periods. Increases in human pressure on the landscape as reflected in the pollen record correspond with an increased rate of sedimentation and fire activity. The timing of the end of the BO-Phase again differs between locations. Estimates range from the 4th century AD to the mid 7th century AD, when a region-wide shift to Dry Environmental Conditions is observed. Numerical analyses show that post BO-Phase vegetation change is largely driven by climate and displays a succession of Dry and wet periods that coincided with well-defined European climate shifts, including the Medieval Climate Anomaly and the Little Ice Age. Current agricultural activities in the region are of a very recent (20th century) origin.status: publishe
David Kaniewski - One of the best experts on this subject based on the ideXlab platform.
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Man, vegetation and climate during the Holocene in the territory of Sagalassos, Western Taurus Mountains, SW Turkey
Vegetation History and Archaeobotany, 2012Co-Authors: Johan Bakker, Etienne Paulissen, David Kaniewski, Véronique Laet, Gert Verstraeten, Marc WaelkensAbstract:Past vegetation change and the influence of climate change and anthropogenic pressure during the Holocene is constructed from a series of palynological records sampled from three locations within the territory of the antique site of Sagalassos. The disappearance of the original deciduous oak woodlands and increases in anthropogenic indicator species around 5300 and 4300 b.c. correspond with an increase in settlements in the region. A period of drought following the deforestation may have hampered the recovery of deciduous oak. The timing of the onset of the Beyşehir Occupation Phase (BO-Phase) in the territory differs between locations, estimates ranging from ca. 1000–800 b.c. to the start of the Hellenistic period (334 b.c. ). The most intense period of arboriculture coincides with the Roman and late-Roman periods. Increases in human pressure on the landscape as reflected in the pollen record correspond with an increased rate of sedimentation and fire activity. The timing of the end of the BO-Phase again differs between locations. Estimates range from the 4th century a.d. to the mid 7th century a.d. , when a region-wide shift to Dry Environmental Conditions is observed. Numerical analyses show that post BO-Phase vegetation change is largely driven by climate and displays a succession of Dry and wet periods that coincided with well-defined European climate shifts, including the Medieval Climate Anomaly and the Little Ice Age. Current agricultural activities in the region are of a very recent (20th century) origin.
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Man, vegetation and climate during the Holocene in the territory of Sagalassos, Western Taurus Mountains, SW Turkey
Vegetation History and Archaeobotany, 2011Co-Authors: Johan Bakker, Etienne Paulissen, David Kaniewski, Véronique Laet, Gert Verstraeten, Marc WaelkensAbstract:Past vegetation change and the influence of climate change and anthropogenic pressure during the Holocene is constructed from a series of palynological records sampled from three locations within the territory of the antique site of Sagalassos. The disappearance of the original deciduous oak woodlands and increases in anthropogenic indicator species around 5300 and 4300 BC, correspond with an increase in settlements in the region. A period of drought, following the deforestation may have hampered the recovery of deciduous oak. The timing of the onset of the Beysehir Occupation Phase (BO-Phase) in the territory differs between locations, estimates ranging from c. 1000-800 BC to the start of the Hellenistic period (334 BC). The most intense period of arboriculture coincides with the Roman and late-Roman periods. Increases in human pressure on the landscape as reflected in the pollen record correspond with an increased rate of sedimentation and fire activity. The timing of the end of the BO-Phase again differs between locations. Estimates range from the 4th century AD to the mid 7th century AD, when a region-wide shift to Dry Environmental Conditions is observed. Numerical analyses show that post BO-Phase vegetation change is largely driven by climate and displays a succession of Dry and wet periods that coincided with well-defined European climate shifts, including the Medieval Climate Anomaly and the Little Ice Age. Current agricultural activities in the region are of a very recent (20th century) origin.status: publishe
