Hässeldala – a key site for Last Termination climate events in northern Europe
dc.contributor.author | Wohlfarth, B | en |
dc.contributor.author | MUSCHITIELLO, F | en |
dc.contributor.author | Greenwood, S | en |
dc.contributor.author | Andersson, A | en |
dc.contributor.author | Kylander, M | en |
dc.contributor.author | SMITTENBERG, R | en |
dc.contributor.author | STEINTHORSDOTTIR, M | en |
dc.contributor.author | Watson, J | en |
dc.contributor.author | Whitehouse, N | en |
dc.date.accessioned | 2016-08-23T14:05:17Z | |
dc.date.available | 2016-08-23T14:05:17Z | |
dc.date.issued | 2016-11-02 | en |
dc.identifier.uri | http://hdl.handle.net/10026.1/5363 | |
dc.description.abstract |
The Last Termination (19 000-11 000 a BP) with its rapid and distinct climate shifts provides a perfect laboratory to study the nature and regional impact of climate variability. The sedimentary succession from the ancient lake at Hässeldala Port in southern Sweden with its distinct Lateglacial/early Holocene stratigraphy (>14.1-9.5 cal. ka BP) is one of the few chronologically well- constrained, multi-proxy sites in Europe that capture a variety of local and regional climatic and environmental signals. Here we present Hässeldala’s multi- proxy records (lithology, geochemistry, pollen, diatoms, chironomids, biomarkers, hydrogen isotopes) in a refined age model and place the observed changes in lake status, catchment vegetation, summer temperatures and hydroclimate in a wider regional context. Reconstructed mean July temperatures increased between ~14.1 and ~13.1 cal. ka BP and subsequently declined. This latter cooling coincided with drier hydroclimatic conditions that were likely associated with a freshening of the Nordic Seas and started a few hundred years before the onset of Greenland Stadial 1 (~12.9 cal. ka BP). Our proxies suggest a further shift towards colder and drier conditions as late as ~12.7 cal. ka BP, which was followed by the establishment of a stadial climate regime (~12.5-11.8 cal. ka BP). The onset of warmer and wetter conditions led the Holocene warming over Greenland by ~200 years. Hässeldala’s proxies thus highlight the complexity of environmental and hydrological responses across abrupt climate transitions in northern Europe. | en |
dc.language.iso | en | en |
dc.title | Hässeldala – a key site for Last Termination climate events in northern Europe | en |
dc.type | Journal Article | |
plymouth.journal | Boreas | en |
plymouth.organisational-group | /Plymouth | |
plymouth.organisational-group | /Plymouth/Faculty of Science and Engineering | |
plymouth.organisational-group | /Plymouth/REF 2021 Researchers by UoA | |
plymouth.organisational-group | /Plymouth/REF 2021 Researchers by UoA/UoA14 Geography and Environmental Studies | |
dcterms.dateAccepted | 2016-08-18 | en |
dc.rights.embargodate | 2017-11-02 | en |
dc.rights.embargoperiod | 12 months | en |
rioxxterms.licenseref.uri | http://www.rioxx.net/licenses/under-embargo-all-rights-reserved | en |
rioxxterms.licenseref.startdate | 2016-11-02 | en |
rioxxterms.type | Journal Article/Review | en |