Epiphyllous fungi and leaf physiognomy indicate an ever-wet humid mesothermal (subtropical) climate in the late Eocene of southern New Zealand-Reference-Cited by-同舟云学术

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Epiphyllous fungi and leaf physiognomy indicate an ever-wet humid mesothermal (subtropical) climate in the late Eocene of southern New Zealand

Published:2016-06 Issue: Volume:452 Page:1-10
ISSN:0031-0182
Container-title:Palaeogeography, Palaeoclimatology, Palaeoecology
language:en
Short-container-title:Palaeogeography, Palaeoclimatology, Palaeoecology

Author:

Conran John G.^ORCID,Bannister Jennifer M.,Reichgelt Tammo^ORCID,Lee Daphne E.

Funder

Australian Research Council

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

Reference99 articles.

1. Miocene to Pleistocene floras and climate of the eastern Himalayan Siwaliks, and new palaeoelevation estimates for the Namling–Oiyug Basin, Tibet;Ali Khan;Glob. Planet. Chang.,2014

2. Life on the phylloplane: Eocene epiphyllous fungi from Pikopiko Fossil Forest, Southland, New Zealand;Bannister;N. Z. J. Bot.,2015

3. Late Eocene epiphyllous fungi from Pikopiko, Southland, New Zealand;Bannister,2003

4. Convergent Cenozoic CO2 history;Beerling;Nat. Geosci.,2011

5. Ecological processes and interactions occurring in leaf surface fungi;Bélanger,2002

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