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Reconstructing climate change and ombrotrophic bog development during the last 4000 years in northern Poland using biotic proxies, stable isotopes and trait-based approach

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Reconstructing climate change and ombrotrophic bog development during the last 4000 years in northern Poland using biotic proxies, stable isotopes and trait-based approach

Graph Chatbot

Chattez avec Graph Search

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Persistence of the isotopic signature of pentavalent uranium in magnetite

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Plant and root‐zone water isotopes are difficult to measure, explain, and predict: some practical recommendations for determining plant water sources

Isotope Ratio - Discharge Relationships of Solutes Derived From Weathering Reactions

Tree water deficit and dynamic source water partitioning

Persistence of the isotopic signature of pentavalent uranium in magnetite

Plant and root‐zone water isotopes are difficult to measure, explain, and predict: some practical recommendations for determining plant water sources

Rapid grain boundary diffusion in foraminifera tests biases paleotemperature records

Persistence of the isotopic signature of pentavalent uranium in magnetite

Surface snow isotopic composition: Post-depositional processes in an alpine snowpack

A 2000-year temperature reconstruction on the East Antarctic plateau from argon-nitrogen and water stable isotopes in the Aurora Basin North ice core