Introduction AOGCM results and Eocene/PETM ocean circulation Hydrate modelling Conceptual model for hyperthermal orbital pacing A mechanism for the orbital.
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Carbon dioxide and Ozone changes and their influence on soybean root production: an experiment conducted in open field conditions. Verónica Rodríguez.
Introduction AOGCM results and Eocene/PETM ocean circulation Hydrate modelling
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Figure 8. Potential sink or source for Atmospheric CO 2 -C .
Karol Kuli n ski Marine Chemistry and Biochemistry Department Supervisor: Janusz Pempkowiak
