Nannoplankton extinction and origination across the Paleocene-Eocene Thermal Maximum.
The Paleocene-Eocene Thermal Maximum (PETM, approximately 55 million years ago) was an interval of global warming and ocean acidification attributed to rapid release and oxidation of buried carbon. We show that the onset of the PETM coincided with a prominent increase in the origination and extinction of calcareous phytoplankton. Yet major perturbation of the surface-water saturation state across the PETM was not detrimental to the survival of most calcareous nannoplankton taxa and did not impart a calcification or ecological bias to the pattern of evolutionary turnover. Instead, the rate of environmental change appears to have driven turnover, preferentially affecting rare taxa living close to their viable limits.
Gibbs
Samantha J
SJ
School of Ocean and Earth Sciences, National Oceanography Centre, Southampton, European Way, Southampton, SO14 3ZH, UK. sxg@noc.soton.ac.uk
Bown
Paul R
PR
Sessa
Jocelyn A
JA
Bralower
Timothy J
TJ
Wilson
Paul A
PA
D001272:Atmosphere; D044822:Biodiversity; D005075:Biological Evolution; D002113:Calcification, Physiologic; D002245:Carbon Dioxide; D017753:Ecosystem; D004777:Environment; D053476:Extinction, Biological; D005580:Fossils; D019015:Geologic Sediments; D009515:New Jersey; D009792:Oceans and Seas; D010140:Pacific Ocean; D010839:Phytoplankton / Q000145:classification; D010933:Plankton / Q000145:classification; D045483:Rivers; D013696:Temperature
D002245:Carbon Dioxide