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Oceanography in northwestern Europe during the last interglacial from intrashell δO ranges in Littorina littorea gastropods
Authors:Johan Burman  Tore Psse
Institution:aDepartment of Earth Sciences, Marine Geology, University of Gothenburg, Box 460, SE-405 30 Göteborg, Sweden;bSwedish Geological Survey, Guldhedsgatan 5A, SE-413 20 Göteborg, Sweden
Abstract:Coastal sea-surface temperature (SST) and sea-surface salinity (SSS), including seasonality, in northwest (NW) Europe during the early phase of the Eemian interglacial ca. 125 ka ago were reconstructed from Littorina littorea (common periwinkle) gastropods. The results were based on intra-annual δ18O analyses in recent and fossil shells, mainly originating from the sea of Kattegat (Sweden) and the English Channel (United Kingdom), and confined to intertidal settings. The Eemian L. littorea shells indicated annual SSTs in the range 8–18°C for the English Channel and 8–26°C for Kattegat. All specimens from the Eemian sites experienced summer SSTs of ca. 1–3°C above recent conditions. The estimated winter SST in the English Channel during the Eemian was comparable to modern measurements of ca. 8°C. However, the Kattegat region displayed Eemian winter SST approximately 8°C warmer than today, and similar to conditions in the western English Channel. The recent-fossil isotope analogue approach indicated high SSS above 35 practical salinity units (psu) for a channel south of England in full contact with the North Atlantic Ocean during the last interglacial. In addition, the Kattegat shells indicated a SSS of ca. 29 psu, which points out a North Sea affinity for this region during the Eemian.
Keywords:Eemian  Last interglacial  Oxygen isotopes  Sea-surface temperature  Sea-surface salinity  Seasonality  Littorina littorea  Gastropod shells
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