Biotic enhancement of weathering, atmospheric oxygen and carbon dioxide in the Neoproterozoic

By T. Lenton, A. Watson. 2003

106 citations recorded by the source corpus.

Subfields: Atmospheric Science, Environmental Chemistry, Paleontology

View Paper: https://www.semanticscholar.org/paper/cd1c8a4d9e5b5e3fe564682c74f7c2f735554484

How researchers see this paper

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In Atmospheric Science

1. G. Shields-Zhou
2. L. Och
3. P. Strother
4. C. Wellman

In Environmental Chemistry

1. P. Strother
2. C. Wellman

In Paleontology

1. G. Shields-Zhou
2. L. Och
3. P. Strother
4. C. Wellman

Citations in the corpus

• Modelling the long-term carbon cycle, atmospheric CO2, and Earth surface temperature from late Neoproterozoic to present day (2019, unknown): “, 2016), or biologically-driven chemical weathering (Lenton and Watson, 2004).”
• The late Precambrian greening of the Earth (2009, background): “Thiswouldhaveincreasedproduction andburialpreservationoforganicCtowardsmodernvalues 5,27,28 and consequently facilitated the stepwise rise in atmospheric O 2 necessary to support multicellularity.”
• The case for a Neoproterozoic Oxygenation Event: Geochemical evidence and biological consequences (2011, background): “The first green algae (and possibly lichen) emerged around this time (Porter, 2004; Knoll et al., 2006) and would have revolutionized weathering and the global carbon cycle once they made it to land (Heckman et al., 2001; Lenton and Watson, 2004).”