When does large woody debris influence ancient rivers? Dendrochronology applications in the Permian and Triassic, Antarctica-Reference-Cited by-同舟云学术

When does large woody debris influence ancient rivers? Dendrochronology applications in the Permian and Triassic, Antarctica

Published:2020-03 Issue: Volume:541 Page:109544
ISSN:0031-0182
Container-title:Palaeogeography, Palaeoclimatology, Palaeoecology
language:en
Short-container-title:Palaeogeography, Palaeoclimatology, Palaeoecology

Author:

Gulbranson Erik L.,Cornamusini Gianluca,Ryberg Patricia E.,Corti Valentina

Funder

National Science Foundation

Publisher

Elsevier BV

Subject

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

Reference80 articles.

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3. Permian palynomorphs from southern Victoria Land, Antarctica;Askin;Antarctic Journal of the U.S.,1995

4. Later Permian and Triassic palynomorphs from the Allan Hills, central Transantarctic Mountains, South Victoria Land, Antarctica;Awatar;Curr. Sci.,2014

5. A simple cross-dating program for tree-ring research;Baillie;Tree-Ring Bull.,1973

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