UCL Discovery Stage
UCL home » Library Services » Electronic resources » UCL Discovery Stage

Reconstruction of short-term storm surge-driven increases in shallow coastal lake salinity using ostracod shell chemistry

Holmes, Jonathan; (2022) Reconstruction of short-term storm surge-driven increases in shallow coastal lake salinity using ostracod shell chemistry. Natural Hazards , 114 (2) pp. 2059-2085. 10.1007/s11069-022-05459-9. Green open access

[thumbnail of Roberts et al_NHaz_accepted[41].pdf]
Preview
Text
Roberts et al_NHaz_accepted[41].pdf - Accepted Version

Download (11MB) | Preview

Abstract

Climate change threatens the current protection provided by coastal defences in low-lying mid-latitude regions and increases the risk to coastal lakes from future frequent and intense storms. Quantifying and understanding the impacts of past storm surges, therefore, has significant implications for the management and conservation of coastal wetlands worldwide. However, short-term (< 10 year) increases in salinity driven by storm surges are problematic to reconstruct via the palaeolimnological record due to sampling resolution and smoothing of trends. Here, we propose that the geochemistry (Sr/Ca and δ18O) of calcitic shells of ostracods (small bivalved crustaceans readily preserved in lacustrine sediments) is a potentially sensitive proxy for reconstructing salinity, in some cases quantitatively, in comparison with sedimentary proxies of allochthonous sediment inputs (XRF and grain size) or other biological proxies. The coastal lakes of the Thurne Broads (Norfolk and Suffolk Broads National Park) in East Anglia, UK, have a long history of sea floods associated with storm surge events in the North Sea, providing a test bed to compare ostracod palaeosalinity reconstructions (using a site-specific calibration) with known storm surges in the region. We show that Sr/Cashell values closely match known salinity changes associated with storm surges; archival records of the salinity of Horsey Mere in CE 1940 suggest a maximum salinity of 13.4 PSU with ostracod Sr/Cashell palaeosalinity calibrations giving a maximum value of 18.3 PSU. Ostracod shell chemistry, therefore, has the potential to afford more reliable reconstructions of high intensity short-term increases in salinity in mid-latitude low-lying coastal lakes.

Type: Article
Title: Reconstruction of short-term storm surge-driven increases in shallow coastal lake salinity using ostracod shell chemistry
Open access status: An open access version is available from UCL Discovery
DOI: 10.1007/s11069-022-05459-9
Publisher version: https://doi.org/10.1007/s11069-022-05459-9
Language: English
Additional information: This version is the author accepted manuscript. For information on re-use, please refer to the publisher’s terms and conditions.
Keywords: Cyprideis torosa; ostracods; oxygen isotope; Sr/Ca; coastal lakes; storm surge; salinisation
UCL classification: UCL > Provost and Vice Provost Offices > UCL SLASH > Faculty of S&HS
UCL > Provost and Vice Provost Offices > UCL SLASH > Faculty of S&HS > Dept of Geography
UCL > Provost and Vice Provost Offices > UCL SLASH
UCL
URI: https://discovery-pp.ucl.ac.uk/id/eprint/10151115
Downloads since deposit
1,596Downloads
Download activity - last month
Download activity - last 12 months
Downloads by country - last 12 months

Archive Staff Only

View Item View Item