Holocene δ¹⁸O diatom from ODP Hole 178-1098A

The causes for rising temperatures along the Antarctic Peninsula during the late Holocene have been debated, particularly in light of instrumental records of warming over the past decades (Russell and McGregor, 2010, doi:10.1007/s10584-009-9673-4). Suggested mechanisms range from upwelling of warm d...

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Bibliographic Details
Main Authors: Pike, Jennifer, Swann, George E A, Leng, Melanie J, Snelling, Andrea M
Format: Dataset
Language:English
Published: PANGAEA 2013
Subjects:
AGE
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.857260
https://doi.org/10.1594/PANGAEA.857260