Koen Sabbe
Biographic Data
| ID | 6375154 |
|---|---|
| NAME | Koen Sabbe |
| GIVEN NAMES | Koen |
| FAMILY NAME | Sabbe |
| SIGNATURE | SABBE K |
| AFFILIATIONS | Ghent University |
| ORCID | 0000-0001-5163-5581 |
| VERIFIED | Yes |
| TOTAL WORKS | 4 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 4 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2004 |
| LATEST PUBLICATION YEAR | 2024 |
| H-INDEX | 0 |
A medieval embankment near the lost harbour of Mude (Zeeland, the Netherlands)
Terrestrial and aquatic ecological conditions were reconstructed from tidal flat deposits evolving into a medieval embankment. • Local brackish-freshwater diatoms indicate that the embankment was outside of frequent tidal reach. • Palynomorphs were associated with anthropogenic activities (e.g. the use of peat for fuel and of hemp for rope making). • Cultivated plants were likely grown in the vicinity, while fig seeds testify to Mediterranean foo…
Relative sea-level history from the Lambert Glacier region, East Antarctica, and its relation to deglaciation and Holocene glacier readvance
We present a relative sea-level (RSL) history, constrained by AMS radiocarbon-dated marine–freshwater transitions in isolation basins from a site adjacent to the Lambert Glacier, East Antarctica. The RSL data suggest an initial ice retreat between c. 15,370 and 12,660 cal yr B.P Within this period, meltwater pulse IA (mwp IA, between c. 14,600–14,200 and 14,100–13,700 cal yr B.P.) occurred; an exceptionally large ice melting event, inferred from …
Late Quaternary climate-driven environmental change in the Larsemann Hills, East Antarctica, multi-proxy evidence from a lake sediment core
Little is known about the response of terrestrial East Antarctica to climate changes during the last glacial–interglacial cycle. Here we present a continuous sediment record from a lake in the Larsemann Hills, situated on a peninsula believed to have been ice-free for at least 40,000 yr. A mutli-proxy data set including geochronology, diatoms, pigments and carbonate stable isotopes indicates warmer and wetter conditions than present in the early …
Coastal oceanographic conditions in the Prydz Bay region (East Antarctica) during the Holocene recorded in an isolation basin
Information on East Antarctic coastal environments during the Holocene is relatively sparse. This is surprising as sedimentary records from the interface between land and sea can provide chronologies of climatic change, isostatic uplift, relative sea level and the colonization of newly formed biomes. Here we examine a sediment core from Pup Lagoon, a coastal lake in the Larsemann Hills, East Antarctica. Sediment stratigraphy, fossil pigments and …
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Coastal oceanographic conditions in the Prydz Bay region (East Antarctica) during the Holocene recorded in an isolation basin
Information on East Antarctic coastal environments during the Holocene is relatively sparse. This is surprising as sedimentary records from the interface between land and sea can provide chronologies of climatic change, isostatic uplift, relative sea level and the colonization of newly formed biomes. Here we examine a sediment core from Pup Lagoon, a coastal lake in the Larsemann Hills, East Antarctica. Sediment stratigraphy, fossil pigments and …
Relative sea-level history from the Lambert Glacier region, East Antarctica, and its relation to deglaciation and Holocene glacier readvance
We present a relative sea-level (RSL) history, constrained by AMS radiocarbon-dated marine–freshwater transitions in isolation basins from a site adjacent to the Lambert Glacier, East Antarctica. The RSL data suggest an initial ice retreat between c. 15,370 and 12,660 cal yr B.P Within this period, meltwater pulse IA (mwp IA, between c. 14,600–14,200 and 14,100–13,700 cal yr B.P.) occurred; an exceptionally large ice melting event, inferred from …
Late Quaternary climate-driven environmental change in the Larsemann Hills, East Antarctica, multi-proxy evidence from a lake sediment core
Little is known about the response of terrestrial East Antarctica to climate changes during the last glacial–interglacial cycle. Here we present a continuous sediment record from a lake in the Larsemann Hills, situated on a peninsula believed to have been ice-free for at least 40,000 yr. A mutli-proxy data set including geochronology, diatoms, pigments and carbonate stable isotopes indicates warmer and wetter conditions than present in the early …
A medieval embankment near the lost harbour of Mude (Zeeland, the Netherlands)
Terrestrial and aquatic ecological conditions were reconstructed from tidal flat deposits evolving into a medieval embankment. • Local brackish-freshwater diatoms indicate that the embankment was outside of frequent tidal reach. • Palynomorphs were associated with anthropogenic activities (e.g. the use of peat for fuel and of hemp for rope making). • Cultivated plants were likely grown in the vicinity, while fig seeds testify to Mediterranean foo…
Geology and Paleoclimatology Research (4 works) · Holocene (3 works) · Physical geography (3 works) · Polar Research and Ecology (3 works) · Cryospheric studies and observations (2 works) · Deglaciation (2 works) · Geography (2 works) · Geology (2 works) · Geology (2 works) · Oceanography (2 works)