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News & Views |
Plankton in a greenhouse world
The Palaeocene–Eocene Thermal Maximum was marked by global warming and ocean acidification. Fossil and experimental analyses show that different species of marine calcifying algae responded very differently to the environmental upheavals.
- Gerald Langer
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Letter |
Rapid fluvial incision along the Yellow River during headward basin integration
The onset of fluvial erosion in an area of tectonic uplift is thought to reflect the timing of the uplift. Geomorphological data from the Yellow River in Tibet, indicate that the rapid incision of this river channel occurred as a result of climate change, at least six million years after the onset of plateau uplift.
- William H. Craddock
- , Eric Kirby
- & Jianhui Liu
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Letter |
Carbon sequestration activated by a volcanic CO2 pulse during Ocean Anoxic Event 2
Ninety-four million years ago, during Ocean Anoxic Event 2, there was a marked increase in the burial of organic carbon in marine sediments. Measurements of stomata in fossil leaves show that the two main pulses of carbon burial were associated with a decline in atmospheric CO2 levels of up to 26%.
- Richard S. Barclay
- , Jennifer C. McElwain
- & Bradley B. Sageman