Tree‐Ring Stable Isotopes Reveal a Hydroclimate Shift in Eastern England Around 4.2 ka Ago

Tree‐Ring Stable Isotopes Reveal a Hydroclimate Shift in Eastern England Around 4.2 ka Ago

Abstract Tree ring‐based climate reconstructions are fundamental for high‐resolution paleoclimatology, but only a few of them extend back into the mid‐Holocene (8,200–4,200 years BP). Here, we present annually‐resolved tree‐ring stable carbon and oxygen isotopes (δ13C and δ18O) from subfossil yew (T...

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Main Authors: Tatiana Bebchuk, Otmar Urban, Tito Arosio, Alexander Kirdyanov, Ronny Friedrich, Natálie Pernicová, Josef Čáslavský, Mirek Trnka, Alis Franсis, Mark Macklin, Jan Esper, Ulf Büntgen
Format: Article
Language:English
Published: Wiley 2025-04-01
Series:Geophysical Research Letters
Subjects:
4.2 ka event
climate reconstruction
dendrochronology
mid‐Holocene
paleoclimate
sea level
Online Access:https://doi.org/10.1029/2024GL114313
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https://doi.org/10.1029/2024GL114313

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