Stable oxygen isotopes and winter bottom water temperature data from Gullmar Fjord, Skagerrak (North Sea) ...
We present 2500 years of reconstructed bottom-water temperatures (BWT) in annual to subdecadal resolution by using a fjord sediment archive from the NE Atlantic region. The BWT represent winter conditions due to the fjord hydrography and associated timing and frequency of bottom-water renewals. The...
| Main Authors: | , , |
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| Format: | Dataset |
| Language: | English |
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PANGAEA
2018
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| Subjects: | |
| Online Access: | https://dx.doi.org/10.1594/pangaea.892500 https://doi.pangaea.de/10.1594/PANGAEA.892500 |
| Summary: | We present 2500 years of reconstructed bottom-water temperatures (BWT) in annual to subdecadal resolution by using a fjord sediment archive from the NE Atlantic region. The BWT represent winter conditions due to the fjord hydrography and associated timing and frequency of bottom-water renewals. The study is based on a ca. 8-m long sediment core from Gullmar Fjord (Sweden), dated by 210Pb and AMS 14C and analysed for stable oxygen isotopes (δ18O) measured on shallow infaunal benthic foraminiferal species Cassidulina laevigata. The BWT, calculated by using the palaeotemperature equation of McCorkle et al (1997), range between 2.7 - 7.8°C and are within the annual temperature variability, instrumentally recorded in the deep fjord basin since the 1890s. The record demonstrates a warming during the Roman Warm Period (~350 BCE - 450 CE), variable BWT during the Dark Ages (~450 - 850 CE), positive BWT anomalies during the Viking Age/Medieval Climate Anomaly (~850 - 1350 CE) and a long-term cooling with distinct ... : Supplement to: Polovodova Asteman, Irina; Filipsson, Helena L; Nordberg, Kjell (2018): Tracing winter temperatures over the last two millennia using a north-east Atlantic coastal record. Climate of the Past, 14(7), 1097-1118 ... |
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