Archive · collection · 2019
Compilation of radionuclides, mercury contaminations, and ln(Zr/Rb) ratios, together with mean grain size and organic carbon data records, obtained from sediment sequences of the south-eastern North Sea region
Listed in PANGAEA
Depositional processes in coastal wetlands respond to a changing climate as documented in the sediment successions of salt marshes.
Description
In this context, robust chronologies are crucial for the reconstruction of salt-marsh depositional processes in the past. However, salt-marsh sediments from the highly dynamic North Sea coast often lack a reliable stratigraphy due to the combined influences of natural processes and human activities, causing a reworking and re-deposition of the sediments.
Here, a combination of absolute and relative dating methods was applied in order to establish an integrated stratigraphic framework for active foreland salt marshes along the south-eastern North Sea coast. This stratigraphic framework is based on radionuclides (210Pb, 137Cs, 14C) and mercury (Hg) contaminations, together with ln(Zr/Rb) as a grain-size proxy for additional inter-correlation between the sites. The studied salt marshes encompass different environmental settings concerning the inundation frequency and intensity, and anthropogenic influences.
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As a result, the reconstructed average sediment accretion rates range from 1.31 cm yr-1 in the more sheltered and semi-enclosed salt marshes in the Bay of Tümlau, to 1.16 cm yr-1 in the anthropogenic modified and grazed coastal salt marsh at Friedrichskoog, and to 1.75 cm yr-1 in the dynamic open coastal salt marsh at Kaiser-Wilhelm-Koog. Similar mean high accretion rates of 1.72 cm yr-1 are documented for the Eider estuary until AD 1965, before they dropped to 0.72 cm yr-1 after completion of the Eider tidal barrier in AD 1973.
The results highlight the advantage of combining independent dating methods for the establishment of salt-marsh chronologies. The reconstructed sediment-accretion rates suggest a high resilience of salt-marsh systems to ongoing sea-level rise as long as sediment availability and natural flooding dynamics are maintained.
Links
Where it is published
- DOI doi.org/10.1594/pangaea.905240 ↗
DOI / persistent id · from PANGAEA
Catalogue records · 1
- OAI-PMH record ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=oai_dc&identifier=o… ↗
metadata API · from PANGAEA
Topics
- From keywords
- Earth & Environmental Science
- Inferred from text
- Palaeoclimatology 77%
Provenance · 1 source records, 8 field assertions
| Source | Key | Last seen | Raw |
|---|---|---|---|
| PANGAEA | oai:pangaea.de:doi:10.1594/PANGAEA.905240 | 15 d ago | JSON v1 |
| Field | Assertion | Extractor | Evidence |
|---|---|---|---|
| access_level | source · PANGAEA | connector:pangaea@1.0.0 | |
| concepts[field].anzsrc:field:370904 | enrichment · PANGAEA | taxonomy-embedding@1.1.0 | title+keywords+description (77%) |
| concepts[field].local:field:earth-environmental | mapping · PANGAEA | connector:pangaea@1.0.0 | |
| description | source · PANGAEA | connector:pangaea@1.0.0 | /metadata/dc/description |
| license | source · PANGAEA | connector:pangaea@1.0.0 | /metadata/dc/rights |
| publication_date | source · PANGAEA | connector:pangaea@1.0.0 | |
| spatial | source · PANGAEA | connector:pangaea@1.0.0 | |
| title | source · PANGAEA | connector:pangaea@1.0.0 | /metadata/dc/title |