Global wood anatomical perspective on the onset of the Late Antique Little Ice Age (LALIA) in the mid-6th century CE
Jazyk angličtina Země Nizozemsko Médium print-electronic
Typ dokumentu časopisecké články
PubMed
36546223
DOI
10.1016/j.scib.2022.10.019
PII: S2095-9273(22)00479-0
Knihovny.cz E-zdroje
- Klíčová slova
- Blue Rings, Climate extremes, Dendrochronology, Late Antiquity, Tree rings, Volcanic eruptions,
- MeSH
- dřevo * MeSH
- lesy MeSH
- podnebí * MeSH
- roční období MeSH
- stromy MeSH
- teplota MeSH
- Publikační typ
- časopisecké články MeSH
Linked to major volcanic eruptions around 536 and 540 CE, the onset of the Late Antique Little Ice Age has been described as the coldest period of the past two millennia. The exact timing and spatial extent of this exceptional cold phase are, however, still under debate because of the limited resolution and geographical distribution of the available proxy archives. Here, we use 106 wood anatomical thin sections from 23 forest sites and 20 tree species in both hemispheres to search for cell-level fingerprints of ephemeral summer cooling between 530 and 550 CE. After cross-dating and double-staining, we identified 89 Blue Rings (lack of cell wall lignification), nine Frost Rings (cell deformation and collapse), and 93 Light Rings (reduced cell wall thickening) in the Northern Hemisphere. Our network reveals evidence for the strongest temperature depression between mid-July and early-August 536 CE across North America and Eurasia, whereas more localised cold spells occurred in the summers of 532, 540-43, and 548 CE. The lack of anatomical signatures in the austral trees suggests limited incursion of stratospheric volcanic aerosol into the Southern Hemisphere extra-tropics, that any forcing was mitigated by atmosphere-ocean dynamical responses and/or concentrated outside the growing season, or a combination of factors. Our findings demonstrate the advantage of wood anatomical investigations over traditional dendrochronological measurements, provide a benchmark for Earth system models, support cross-disciplinary studies into the entanglements of climate and history, and question the relevance of global climate averages.
CNR IBE Institute of BioEconomy National Research Council Trento 38121 Italy
Department of Earth Sciences the College of Wooster Wooster OH 44691 USA
Department of Geography Johannes Gutenberg University Mainz 55099 Germany
Department of Geography University of Cambridge Cambridge CB2 3EN UK
Department of Geography University of Innsbruck Innsbruck 6020 Austria
Department of Geology State University of New York at Cortland Cortland NY 13045 USA
Global Change Research Centre Brno 60300 Czech Republic
Institute of Humanities Siberian Federal University Krasnoyarsk 660041 Russia
Laboratorio de Dendrocronología y Cambio Global Universidad Austral de Chile Valdivia 509000 Chile
Laboratory of Tree Ring Research University of Arizona Tucson AZ 85721 USA
School of Environment The University of Auckland Auckland 1010 New Zealand
Swiss Federal Research Institute Birmensdorf 8903 Switzerland
The University of New South Wales Sydney NSW 2052 Australia
Tree Ring Laboratory Lamont Doherty Earth Observatory Columbia University Palisades NY 10964 USA
Citace poskytuje Crossref.org
Reply to: Biogeographic implications of plant stature and microclimate in cold regions