HS1 records bases on isotope, inorganic and organic geochemistry of sediment cores GeoB16224-1 and GeoB16212-2 ...

The temporal succession of changes in Amazonian hydroclimate during Heinrich Stadial 1 (HS1) (ca. 18-14.7 cal ka BP) is currently poorly resolved. Here we present HS1 records based on isotope, inorganic and organic geochemistry from a marine sediment core influenced by the Amazon River discharge. Ou...

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Bibliographic Details
Main Authors: Crivellari, Stefano, Chiessi, Cristiano Mazur, Kuhnert, Henning, Häggi, Christoph, Portilho-Ramos, Rodrigo Costa, Zeng, Jing-Ying, Zhang, Yancheng, Schefuß, Enno, Mollenhauer, Gesine, Hefter, Jens, Alexandre, Felipe, Mulitza, Stefan, Sampaio, Gilvan
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2018
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.887797
https://doi.pangaea.de/10.1594/PANGAEA.887797