Changes in the mode of Southern Ocean circulation over the last glacial cycle revealed by foraminiferal stable isotopic variability

Benthic foraminiferal oxygen and carbon isotopic records from Southern Ocean sediment cores show that during the last glacial period, the South Atlantic sector of the deep Southern Ocean filled to roughly 2500 m with water uniformly low in δ 13C, resulting in the appearance of a strong mid-depth nut...

Ausführliche Beschreibung

Bibliographische Detailangaben

Veröffentlicht in:	Earth and planetary science letters 2002-07, Vol.201 (2), p.383-396
Hauptverfasser:	Ninnemann, Ulysses S, Charles, Christopher D
Format:	Artikel
Sprache:	eng
Schlagworte:	Foraminifera ocean circulation South Atlantic stable isotopes
Online-Zugang:	Volltext
Tags:	Tag hinzufügen Keine Tags, Fügen Sie den ersten Tag hinzu!