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Reply to 'Limited Late Antique cooling'

Cooling and societal change during the Late Antique Little Ice Age from 536 to around 660 AD

Cooling and societal change during the Late Antique Little Ice Age from 536 to around 660 AD

Dendro-provenancing of Arctic driftwood

Tree rings reveal globally coherent signature of cosmogenic radiocarbon events in 774 and 993 CE

Diverse growth trends and climate responses across Eurasia’s boreal forest

Editorial

Феноритмы некоторых представителей семейства Amaryllidaceae Jaume St.-Hil. в условиях защищенного грунта

Measurements of the superconducting anisotropy in FeSe with a resonance frequency technique

Ranking of tree-ring based temperature reconstructions of the past millennium well include W-Himalaya and Karakorum from Asia, Tatra and S-Finland from Europe, and Great Basin from

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