Planktic foraminifera at the Paleocene-Eocene transition in the Antarctic Indian Ocean

Isotopic depth stratification and relative abundance studies of planktic foraminifera at ODP Site 738 reveal three major faunal turnovers during the latest Paleocene and early Eocene, reflecting the climatic and structural changes in the Antarctic surface ocean. Faunal Event 1 occurred near the Pale...

Full description

Bibliographic Details
Main Authors: Lu, Gangyi, Keller, Gerta
Format: Other/Unknown Material
Language:English
Published: PANGAEA 1993
Subjects:
119-738C
DRILL
Drilling/drill rig
Indian Ocean
Joides Resolution
Leg119
Ocean Drilling Program
ODP
Antarc*
Antarctic
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.683876
https://doi.org/10.1594/PANGAEA.683876

Similar Items