Deep mantle to atmosphere: Understanding the role of vanished intra-oceanic subduction zones on paleoclimate reconstructions
GPlates digital plate reconstruction files of reconstructed global seafloor ages from 200 to 0 Ma for the Matthews et al. (2016) and Tomopac version 1 (Wu et al., 2022) plate reconstructions.
Supplemental files for the submitted manuscript: "Deep mantle to atmosphere: Understanding the role of vanished intra-oceanic subduction zones on paleoclimate since 200 Ma" by Moloud Rahimzadeh Bajgiran1, Jonny Wu1, Sabin Zahirovic2, Jeremy Tsung-Jui Wu3, Lorenzo Colli4, Yi-An Lin5
Author affiliations:
- University of Arizona, Department of Geosciences, USA;
- Sydney University, School of Geosciences, Australia;
- National Taiwan University, Department of Geosciences, Taiwan;
- Bluethink, Italy;
- Centerpoint Energy, USA
For inquiries regarding the contents of this dataset, please contact the Corresponding Author listed in the README.txt file. Administrative inquiries (e.g., removal requests, trouble downloading, etc.) can be directed to data-management@arizona.edu
Funding
NSF EAR-2422671
NSF EAR-1848327
ARC DE210100084
Sydney University Robinson Fellowship
CAREER: Unfolding Earth history back to the Mesozoic by incorporating seismic tomography into Pacific realm plate tectonic reconstructions
Directorate for Geosciences
Find out more...The interplay of tectonics and sea level on carbonate platform evolution
Australian Research Council
Find out more...CAREER: Unfolding Earth history back to the Mesozoic by incorporating seismic tomography into Pacific realm plate tectonic reconstructions
Directorate for Geosciences
Find out more...