Potential links between continental rifting, CO2 degassing and climate change through time

By S. Brune, S. Williams, R. Müller. Nature Geoscience, 2017

193 citations recorded by the source corpus.

Subfields: Atmospheric Science, Geophysics, Paleontology

View Paper: https://www.semanticscholar.org/paper/d237f58427f3ba80069f81d51638cd01f374747d

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. Alexander J. Krause
2. R. Dietmar Müller
3. T. Lenton
4. D. Hill
5. G. Shields
6. Benjamin J. W. Mills
7. C. Scotese

In Geophysics

1. R. Dietmar Müller
2. Michael Gurnis
3. Shijie Zhong
4. Clinton P. Conrad

In Paleontology

1. R. Dietmar Müller

Citations in the corpus

• Modelling the long-term carbon cycle, atmospheric CO2, and Earth surface temperature from late Neoproterozoic to present day (2019, methodology): “…reconstructions for the Mesozoic and Cenozoic now display broad peaks in the Cretaceous and Paleogene, reasonably consistent with the long-term pattern shown in proxy data, with the difference driven primarily by the consideration of rift activity in the degassing rate of CO2 (Brune et al., 2017).”
• GPlates: Building a Virtual Earth Through Deep Time (2018, background): “…exposed GPlates functionality to a wide range of community Python automation tools and interfaces, which has been applied to tectonics (Brune et al., 2016; Merdith et al., 2017), to the deep carbon cycle (Brune et al., 2017; Müller & Dutkiewicz, 2018), and to paleobiogeography (Cao et al., 2018).”