Lookup NU author(s): Dr Luke Handley
Full text for this publication is not currently held within this repository. Alternative links are provided below where available.
Sea-surface temperature (SST) estimates of similar to 30 degrees C from planktic foraminifera and archaeal membrane lipids in bathyal sediments in the Canterbury Basin, New Zealand, support paleontological evidence for a warm subtropical to tropical climate in the early Eocene high-latitude (55 degrees S) southwest Pacific. Such warm SSTs; call into quest-ion previous estimates based on oxygen isotopes and present a major challenge to climate modelers. Even under hypergreenhouse conditions (2240 ppm CO2), modeled summer SSTs for the New Zealand region do not exceed 20 degrees C.
Author(s): Hollis CJ, Handley L, Crouch EM, Morgans HEG, Baker JA, Creech J, Collins KS, Gibbs SJ, Huber M, Schouten S, Zachos JC, Pancost RD
Publication type: Article
Print publication date: 01/02/2009
ISSN (print): 0091-7613
ISSN (electronic): 1943-2682
Publisher: Geological Society of America
Notes: ISI Document Delivery No.: 403QK
Times Cited: 1
Cited Reference Count: 39
Altmetrics provided by Altmetric