Insights into Holocene relative sea-level changes in the southern North Sea using an improved microfauna-based transfer function
In light of global warming and rising relative sea level (RSL), detailed reconstructions of RSL histories and their controlling processes are essential in order to manage coastal-protection challenges. This study contributes to unravelling Holocene RSL change on the East Frisian North Sea coast in h...
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| Hauptverfasser: | , , , , , , , , |
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| Dokumenttyp: | Article (Journal) |
| Sprache: | Englisch |
| Veröffentlicht: |
January 2022
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| In: |
Journal of quaternary science
Year: 2022, Jahrgang: 37, Heft: 1, Pages: 71-85 |
| ISSN: | 1099-1417 |
| DOI: | 10.1002/jqs.3380 |
| Online-Zugang: | Verlag, kostenfrei, Volltext: https://doi.org/10.1002/jqs.3380 Verlag, kostenfrei, Volltext: https://onlinelibrary.wiley.com/doi/abs/10.1002/jqs.3380 
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| Verfasserangaben: | Juliane Scheder, Friederike Bungenstock, Kristin Haynert, Anna Pint, Frank Schlütz, Peter Frenzel, Achim Wehrmann, Helmut Brückner and Max Engel |
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| 245 | 1 | 0 | |a Insights into Holocene relative sea-level changes in the southern North Sea using an improved microfauna-based transfer function |c Juliane Scheder, Friederike Bungenstock, Kristin Haynert, Anna Pint, Frank Schlütz, Peter Frenzel, Achim Wehrmann, Helmut Brückner and Max Engel |
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| 520 | |a In light of global warming and rising relative sea level (RSL), detailed reconstructions of RSL histories and their controlling processes are essential in order to manage coastal-protection challenges. This study contributes to unravelling Holocene RSL change on the East Frisian North Sea coast in high resolution and with a new approach for the German Bight. For the first time, a transfer function (vertical error: 29.7 cm ≙ 11% of the mean tidal range) for RSL change based on a combined training set of benthic foraminifers and ostracods from the back-barrier tidal basin of Spiekeroog is applied to the Holocene record of the back-barrier tidal basin of Norderney. The resulting RSL curve for the Norderney tidal basin is corrected for decompaction and shows a deceleration in RSL rise between 6000 and 5000 cal bp. The smallest possible error envelope ( 1 m) results from the good suitability of salt-marsh layers between 5000 and 4000 cal bp. The RSL curve provides an approach towards the closure of the common data gap of peat-based curves for the southern North Sea related to a lack of basal peats in the youngest age range, and verifies regional differences in glacial isostatic adjustment. | ||
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