A review of climate reconstructions from terrestrial climate archives covering the first millennium AD in northwestern Europe
Dados Bibliográficos
| ID | 24088453 |
|---|---|
| Autores | Dana F C Riechelmann (0000-0002-3863-8216, Utrecht University, autor correspondente), Marjolein T I J Gouw-Bouman (0000-0002-1976-2991, Utrecht University) |
| Ano | 2019 |
| Volume | 91 |
| Fascículo | 1 |
| Páginas | 111-131 |
| Data de publicação | 2019-01-01 |
| Peer Reviewed | Sim |
| Open Access | Sim |
| Tipo | ARTICLE |
| Periódico | Quaternary Research (JOURNAL) |
| Identificadores do periódico | ISSN: 0033-5894 • E-ISSN: 1096-0287 |
| Editora | Cambridge University Press (CUP) (PUBLISHER) |
| DOI | 10.1017/qua.2018.84 |
| OpenAlex | W2898028996 |
| Idioma | EN |
| Citações recebidas | 5 |
| Referências citadas | 69 |
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.
Archaeology · Climate change · Climatology · Geography · Holocene · Paleoclimatology · Peat · Period (music) · Physical geography · Precipitation · Sphagnum · Stalagmite · Testate amoebae · Vegetation (pathology) · Archaeology and ancient environmental studies · Geology · Geology and Paleoclimatology Research · Oceanography · Paleontology · Tree-ring climate responses
Towards a rigorous understanding of societal responses to climate change
The Fimbulwinter myth in the context of Nordic tree-ring climate proxy data
Roman Imperialism and the Transformation of Rural Society in a Frontier Province
Late Holocene vegetation dynamics
Holocene Floodplain Transformation Through Catchment‐Scale Human‐Environment Interactions
Environmental changes and the Migration Period in northern Germany as reflected in the sediments of Lake Dudinghausen
Holocene Climate Variability in Sicily from a Discontinuous Stalagmite Record and the Mesolithic to Neolithic Transition
Old World megadroughts and pluvials during the Common Era
World Map of the Köppen-Geiger climate classification updated
Climatic change and contemporaneous land-use phases north and south of the Alps 2300 BC to 800 AD
A synchronized dating of three Greenland ice cores throughout the Holocene
Cooling and societal change during the Late Antique Little Ice Age from 536 to around 660 AD
Structure and origin of Holocene cold events
Years of European Climate Variability and Human Susceptibility
A new Greenland ice core chronology for the last glacial termination
Mid- to Late Holocene climate change
Centennial-Scale Holocene Climate Variability Revealed by a High-Resolution Speleothem δ 18 O Record from SW Ireland
Fennoscandian summers from ad 500
European summer temperatures since Roman times
Lateglacial calendar year chronology based on annually laminated sediments from Lake Meerfelder Maar, Germany
Dark Ages Cold Period
Quantitative estimates of water tables and soil moisture in Holocene peatlands from testate amoebae
Seven tephra isochrones in Scotland
Holocene evolution of a lowland Scottish landscape
A 5500-year proxy-climate and vegetation record from blanket mire at Talla Moss, Borders, Scotland
Climate Change during and after the Roman Empire
Twilight of the gods? The 'dust veil event' of AD 536 in critical perspective
The disappearance of the ancient landscape and the climatic anomaly of the early Middle Ages
| Obras citantes distintas | 5 |
|---|---|
| Citações por ano | 0,83 |
| Intervalo de citações | 2020 - 2026 (7) |
| Velocidade de citação | current |
| Altamente citado | Não |
| Tipos de citação | Neutras: 5 |