Ulf Büntgen, Lukas Wacker, J Diego Galván, Stephanie Arnold, Dominique Arseneault, Michael Baillie, Jürg Beer, Mauro Bernabei, Niels Bleicher, Gretel Boswijk, Achim Bräuning, Marco Carrer, Fredrik Charpentier Ljungqvist, Paolo Cherubini, Marcus Christl, Duncan A Christie, Peter W Clark, Edward R Cook, Rosanne D'Arrigo, Nicole Davi, Ólafur Eggertsson, Jan Esper, Anthony M Fowler, Ze'ev Gedalof, Fabio Gennaretti, Jussi Grießinger, Henri Grissino-Mayer, Håkan Grudd, Björn E Gunnarson, Rashit Hantemirov, Franz Herzig, Amy Hessl, Karl-Uwe Heussner, A J Timothy Jull, Vladimir Kukarskih, Alexander Kirdyanov, Tomáš Kolář, Paul J Krusic, Tomáš Kyncl, Antonio Lara, Carlos LeQuesne, Hans W Linderholm, Neil J Loader, Brian Luckman, Fusa Miyake, Vladimir S Myglan, Kurt Nicolussi, Clive Oppenheimer, Jonathan Palmer, Irina Panyushkina, Neil Pederson, Michal Rybníček, Fritz H Schweingruber, Andrea Seim, Michael Sigl, Olga Churakova Sidorova, James H Speer, Hans-Arno Synal, Willy Tegel, Kerstin Treydte, Ricardo Villalba, Greg Wiles, Rob Wilson, Lawrence J Winship, Jan Wunder, Bao Yang, Giles H F Young
Though tree-ring chronologies are annually resolved, their dating has never been independently validated at the global scale. Moreover, it is unknown if atmospheric radiocarbon enrichment events of cosmogenic origin leave spatiotemporally consistent fingerprints. Here we measure the 14 C content in 484 individual tree rings formed in the periods 770-780 and 990-1000 CE. Distinct 14 C excursions starting in the boreal summer of 774 and the boreal spring of 993 ensure the precise dating of 44 tree-ring records from five continents...
September 6, 2018: Nature Communications