Quantifying Benthic δ18O Lags Across Termination 1: A Probabilistic Approach Based on Radiocarbon and Benthic δ18O Chronologies

Abstract Temporal offsets (“lags”) between benthic δ18O (δ18Ob) signals in different locations are not only a source of age model uncertainty during δ18Ob stratigraphic alignment but also provide an opportunity to improve reconstructions of deep ocean circulation change during Termination 1 (T1). Wh...

Celý popis

Podrobná bibliografie

Hlavní autoři:	D. Rand, L. E. Lisiecki, T. Lee, C. W. Lawrence, G. Gebbie
Médium:	Artigo
Jazyk:	Inglês
Vydáno:	Wiley 2024-02-01
Edice:	Geochemistry, Geophysics, Geosystems
On-line přístup:	https://doi.org/10.1029/2023GC011068
Tagy:	Přidat tag Žádné tagy, Buďte první, kdo vytvoří štítek k tomuto záznamu!