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DOI10.1016/j.quascirev.2018.11.031
Frost rings in 1627 BC and AD 536 in subfossil pinewood from Finnish Lapland
Helama S.; Saranpää P.; Pearson C.L.; Arppe L.; Holopainen J.; Mäkinen H.; Mielikäinen K.; Nöjd P.; Sutinen R.; Taavitsainen J.-P.; Timonen M.; Uusitalo J.; Oinonen M.
发表日期2019
ISSN0277-3791
起始页码208
结束页码215
卷号204
英文摘要Frost rings can provide direct evidence of anomalously cold summertime conditions on hemispheric scales. Here we report frost rings in subfossil pinewood from Finnish Lapland dated dendrochronologically to AD 536 and 1627 BC. These exact calendar dates have been vividly discussed in the literature in the respective contexts of a cold climate anomaly/dust veil/crop failure/famine/Justinianic Plague and the Minoan eruption of Thera (Santorini). Coinciding anomalies in growth and carbon isotope ratios (δ13C) indicate cold and overcast conditions in these years in Finnish Lapland, typical to conditions induced by volcanic dust veils. This evidence reinforces the view of multiple climatic drivers strongly effecting contemporary societies around AD 536 and provides important new evidence regarding the 1627 BC event. We report a frost ring for this year, and also consider evidence from Lapland for other Thera candidate eruptions in the 16th century BC. The marker years 1560 BC and 1546 BC in bristlecone pine tree rings in North America are positioned within negative departures in our δ13C data. Most likely, the frosts occurred somewhere in July and were driven by dust veils from Northern Hemisphere. Although not indicative of volcanic provenance, frost rings and other dendroclimatic proxies dated to exact calendar years offer important time markers for chronological frameworks which can synchronize archaeological, historical and environmental data to further our understanding of environmental changes at scales that matter to human societies. © 2018 Elsevier Ltd
英文关键词Europe; Holocene; Ice cores; Late antiquity; Minoan eruption; North America; Paleoclimatology; Scandinavia; Tree-rings
语种英语
scopus关键词Dust; Forestry; Volcanoes; Europe; Holocenes; Ice core; Late antiquity; Minoan eruption; North America; Paleoclimatology; Scandinavia; Tree rings; Trees (mathematics); anomaly; carbon isotope ratio; climate; dendrochronology; frost; growth; Holocene; ice core; Northern Hemisphere; paleoclimate; subfossil; tree ring; volcanic eruption; wood; Cyclades; Finland; Greece; Lappi [Finland]; North America; Santorin; Santorini [Southern Aegean]; Scandinavia; Southern Aegean; Pinus aristata; Thera
来源期刊Quaternary Science Reviews
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/152056
作者单位Natural Resources Institute Finland, Eteläranta 55, Rovaniemi, 96301, Finland; Natural Resources Institute Finland, Tietotie 2, Espoo, 02150, Finland; Laboratory of Tree-Ring Research, University of Arizona, Tucson, AZ 85721, United States; Laboratory of Chronology, Finnish Museum of Natural History, University of Helsinki, Gustaf Hällströmin katu 2, Helsinki, 00014, Finland; Department of Geographical and Historical Studies, University of Eastern Finland, Yliopistokatu 7, Joensuu, 80100, Finland; Geological Survey of Finland, Lähteentie 2, Rovaniemi, 96101, Finland; Department of Archaeology, University of Turku, Henrikinkatu 2, Turku, 20014, Finland
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GB/T 7714
Helama S.,Saranpää P.,Pearson C.L.,et al. Frost rings in 1627 BC and AD 536 in subfossil pinewood from Finnish Lapland[J],2019,204.
APA Helama S..,Saranpää P..,Pearson C.L..,Arppe L..,Holopainen J..,...&Oinonen M..(2019).Frost rings in 1627 BC and AD 536 in subfossil pinewood from Finnish Lapland.Quaternary Science Reviews,204.
MLA Helama S.,et al."Frost rings in 1627 BC and AD 536 in subfossil pinewood from Finnish Lapland".Quaternary Science Reviews 204(2019).
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