Clinal variation in aperture shape in Southwest Pacific Globorotalia partimlabiata and its ancestor about the time of the Middle Miocene Climatic Transition-Reference-Cited by-同舟云学术

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Clinal variation in aperture shape in Southwest Pacific Globorotalia partimlabiata and its ancestor about the time of the Middle Miocene Climatic Transition

Published:2018-05 Issue: Volume:141 Page:1-9
ISSN:0377-8398
Container-title:Marine Micropaleontology
language:en
Short-container-title:Marine Micropaleontology

Author:

Scott George H.^ORCID

Publisher

Elsevier BV

Subject

Paleontology,Oceanography

Reference34 articles.

1. Geometric morphometrics: ten years progress following the ‘revolution’;Adams;Ital. J. Zool.,2004

2. Notes on the evolution of some planktonic foraminifera from the Miocene of Central Italy;Cati;G. Geol. II,1968

3. Middle to late Miocene marine ecostratigraphy: clay minerals, planktonic foraminifera and stable isotopes from Sicily;Chamley;Oceanol. Acta,1986

4. Aspects of Neogene Palaeoceanography in the Southern Tasman Sea (DSDP Site 593);Cooke,2002

5. Southern Tasman Sea DSDP 593 stable isotope data;Cooke,2007

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