A review of climate reconstructions from terrestrial climate archives covering the first millennium AD in northwestern Europe. Issue 1 (8th October 2018)

• Record Type: Journal Article
• Authors: Riechelmann, Dana F.C.; Gouw-Bouman, Marjolein T.I.J.
• Is Part Of: Quaternary research. Volume 91:Issue 1(2019)
• Page Start: 111
• Page End: 131
• Publication Date: 2018-10-08
• Subjects: Palaeoclimatology, -- Dark Ages Cold Period, -- Roman Warm Period, -- Seasonality, -- Temperature reconstructions, -- Precipitation reconstructions; Geology, Stratigraphic -- Quaternary -- Periodicals; Glacial epoch -- Periodicals; Stratigraphie -- Quaternaire -- Périodiques; Époque glaciaire -- Périodiques; Geology, Stratigraphic; Glacial epoch; Quaternary Geologic Period; Electronic journals; Periodicals; 551.79
• DOI: 10.1017/qua.2018.84
• Languages: English
• ISSNs: 0033-5894

Abstract

Abstract: Large changes in landscape, vegetation, and culture in northwestern (NW) Europe during the first millennium AD seem concurrent with climatic shifts. Understanding of this relation requires high-resolution palaeoclimate reconstructions. Therefore, we compiled available climate reconstructions from sites across NW Europe (extent research area: 10°W–20°E, 45°–60°N) through review of literature and the underlying data, to identify supraregional climatic changes in this region. All reconstructions cover the period from AD 1 to 1000 and have a temporal resolution of ≤50 yr. This resulted in 22 climate reconstructions/proxy records based on different palaeoclimate archives: chironomids (1), pollen (6), Sphagnum mosses (1), stalagmites (8), testate amoebae (4), and tree rings (2). Comparing all temperature reconstructions, we conclude that summer temperatures between AD 1 and 250 were relatively high, and the period between AD 250 and 700 was characterised by colder summer conditions. The period from AD 700 to 1000 was again characterised by warmer summers. These temperature shifts occurred in the whole of NW Europe. In contrast, the compilation of precipitation reconstructions does not show a common pattern across NW Europe either as a result of a heterogeneous precipitation pattern or the lack of suitable and consistent precipitation proxies.