Marjolein T I J Gouw-Bouman
Biographic Data
| ID | 6383034 |
|---|---|
| NAME | Marjolein T I J Gouw-Bouman |
| GIVEN NAMES | Marjolein T I J |
| FAMILY NAME | Gouw-Bouman |
| SIGNATURE | GOUW-BOUMAN M T I J |
| AFFILIATIONS | Utrecht University |
| ORCID | 0000-0002-1976-2991 |
| VERIFIED | Yes |
| TOTAL WORKS | 5 |
| TOTAL CITATIONS | 5 |
| WORKS AS AUTHOR | 5 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2018 |
| LATEST PUBLICATION YEAR | 2024 |
| H-INDEX | 1 |
Late Holocene vegetation dynamics
During the Dark Ages, which include the Late Roman period ( ad 270–450) and the Early Middle Ages ( ad 450–1050), large-scale vegetation development in northwest Europe was characterised by widespread regeneration of woodlands. This regeneration phase represents a break from the extensive reduction in woodland from human activities in late Holocene vegetation history. In the Netherlands, possible causes for this reversal can be found in a decreas…
Unlocking the wealth of Dutch pollen data for future research and education
Nearly 100 years ago, scientists started analysing fossil pollen and spores in the Netherlands. Since then, an enormous number of fossil pollen datasets have been generated by several researchers at different research institutes. Until recently, most pollen data from the Netherlands was not publicly available. With this communication we like to advertise that this situation has changed and present progress on the Dutch pollen database project. Th…
A review of climate reconstructions from terrestrial climate archives covering the first millennium AD in northwestern Europe
Large changes in landscape, vegetation, and culture in northwestern (NW) Europe during the first millennium AD seem concurrent with climatic shifts. Understanding of this relation requires high-resolution palaeoclimate reconstructions. Therefore, we compiled available climate reconstructions from sites across NW Europe (extent research area: 10°W–20°E, 45°–60°N) through review of literature and the underlying data, to identify supraregional clima…
The landscape setting of bog bodies
Past studies of archaeological bog finds, such as bog bodies, wooden trackways and a wide variety of other materials, are characterized by a strong focus on material culture. Their original environmental and cultural context has received far less attention. This paper centres on the original landscape setting of bog bodies. Interdisciplinary reconstructions of the physical and cultural landscape at the time of deposition can lead to significant n…
Controls on late-Holocene drift-sand dynamics
Holocene drift-sand activity in the northwest European sand belt is commonly directly linked to population pressure (agricultural activity) or to climate change (e.g. storminess). In the Pleistocene sand areas of the Netherlands, small-scale Holocene drift-sand activity began in the Mesolithic, whereas large-scale sand drifting started during the Middle Ages. This last phase not only coincides with the intensification of farming and demographic p…
Controls on late-Holocene drift-sand dynamics
Holocene drift-sand activity in the northwest European sand belt is commonly directly linked to population pressure (agricultural activity) or to climate change (e.g. storminess). In the Pleistocene sand areas of the Netherlands, small-scale Holocene drift-sand activity began in the Mesolithic, whereas large-scale sand drifting started during the Middle Ages. This last phase not only coincides with the intensification of farming and demographic p…
Unlocking the wealth of Dutch pollen data for future research and education
Nearly 100 years ago, scientists started analysing fossil pollen and spores in the Netherlands. Since then, an enormous number of fossil pollen datasets have been generated by several researchers at different research institutes. Until recently, most pollen data from the Netherlands was not publicly available. With this communication we like to advertise that this situation has changed and present progress on the Dutch pollen database project. Th…
Controls on late-Holocene drift-sand dynamics
Holocene drift-sand activity in the northwest European sand belt is commonly directly linked to population pressure (agricultural activity) or to climate change (e.g. storminess). In the Pleistocene sand areas of the Netherlands, small-scale Holocene drift-sand activity began in the Mesolithic, whereas large-scale sand drifting started during the Middle Ages. This last phase not only coincides with the intensification of farming and demographic p…
A review of climate reconstructions from terrestrial climate archives covering the first millennium AD in northwestern Europe
Large changes in landscape, vegetation, and culture in northwestern (NW) Europe during the first millennium AD seem concurrent with climatic shifts. Understanding of this relation requires high-resolution palaeoclimate reconstructions. Therefore, we compiled available climate reconstructions from sites across NW Europe (extent research area: 10°W–20°E, 45°–60°N) through review of literature and the underlying data, to identify supraregional clima…
The landscape setting of bog bodies
Past studies of archaeological bog finds, such as bog bodies, wooden trackways and a wide variety of other materials, are characterized by a strong focus on material culture. Their original environmental and cultural context has received far less attention. This paper centres on the original landscape setting of bog bodies. Interdisciplinary reconstructions of the physical and cultural landscape at the time of deposition can lead to significant n…
Unlocking the wealth of Dutch pollen data for future research and education
Nearly 100 years ago, scientists started analysing fossil pollen and spores in the Netherlands. Since then, an enormous number of fossil pollen datasets have been generated by several researchers at different research institutes. Until recently, most pollen data from the Netherlands was not publicly available. With this communication we like to advertise that this situation has changed and present progress on the Dutch pollen database project. Th…
Late Holocene vegetation dynamics
During the Dark Ages, which include the Late Roman period ( ad 270–450) and the Early Middle Ages ( ad 450–1050), large-scale vegetation development in northwest Europe was characterised by widespread regeneration of woodlands. This regeneration phase represents a break from the extensive reduction in woodland from human activities in late Holocene vegetation history. In the Netherlands, possible causes for this reversal can be found in a decreas…
Geography (5 works) · Geology and Paleoclimatology Research (5 works) · Archaeology (3 works) · Ecology (3 works) · Geology (3 works) · Holocene (3 works) · Physical geography (3 works) · Archaeology and ancient environmental studies (2 works) · Biogeosciences (2 works) · Biology (2 works)