Jonathan L Payne

Summary

Affiliation: Stanford University
Country: USA

Publications

  1. doi request reprint A shift in the long-term mode of foraminiferan size evolution caused by the end-Permian mass extinction
    Jonathan L Payne
    Department of Geological and Environmental Sciences, Stanford University, Stanford, CA 94305, USA
    Evolution 67:816-27. 2013
  2. doi request reprint Late paleozoic fusulinoidean gigantism driven by atmospheric hyperoxia
    Jonathan L Payne
    Department of Geological and Environmental Sciences, Stanford University, 450 Serra Mall, Building 320, Stanford, California 94305, USA
    Evolution 66:2929-39. 2012
  3. pmc The effect of geographic range on extinction risk during background and mass extinction
    Jonathan L Payne
    Department of Geological and Environmental Sciences, Stanford University, Stanford, CA 94305, USA
    Proc Natl Acad Sci U S A 104:10506-11. 2007
  4. pmc Two-phase increase in the maximum size of life over 3.5 billion years reflects biological innovation and environmental opportunity
    Jonathan L Payne
    Department of Geological and Environmental Sciences, Stanford University, 450 Serra Mall, Building 320, Stanford, CA 94305, USA
    Proc Natl Acad Sci U S A 106:24-7. 2009
  5. pmc Calcium isotope constraints on the end-Permian mass extinction
    Jonathan L Payne
    Department of Geological and Environmental Sciences, Stanford University, Stanford, CA 94305, USA
    Proc Natl Acad Sci U S A 107:8543-8. 2010
  6. doi request reprint The evolutionary consequences of oxygenic photosynthesis: a body size perspective
    Jonathan L Payne
    Department of Geological and Environmental Sciences, Stanford University, 450 Serra Mall, Bldg 320, Stanford, CA 94305, USA
    Photosynth Res 107:37-57. 2011
  7. pmc Long-term differences in extinction risk among the seven forms of rarity
    Paul G Harnik
    Department of Geological and Environmental Sciences, Stanford University, Stanford, CA 94305, USA
    Proc Biol Sci 279:4969-76. 2012
  8. ncbi request reprint Large perturbations of the carbon cycle during recovery from the end-permian extinction
    Jonathan L Payne
    Department of Earth and Planetary Sciences, Harvard University, 20 Oxford Street, Cambridge, MA 02138, USA
    Science 305:506-9. 2004

Detail Information

Publications8

  1. doi request reprint A shift in the long-term mode of foraminiferan size evolution caused by the end-Permian mass extinction
    Jonathan L Payne
    Department of Geological and Environmental Sciences, Stanford University, Stanford, CA 94305, USA
    Evolution 67:816-27. 2013
    ..These findings illustrate the potential for mass extinction to alter macroevolutionary dynamics for hundreds of millions of years...
  2. doi request reprint Late paleozoic fusulinoidean gigantism driven by atmospheric hyperoxia
    Jonathan L Payne
    Department of Geological and Environmental Sciences, Stanford University, 450 Serra Mall, Building 320, Stanford, California 94305, USA
    Evolution 66:2929-39. 2012
    ..These findings provide the first quantitative confirmation of a direct connection between Paleozoic gigantism and atmospheric hyperoxia...
  3. pmc The effect of geographic range on extinction risk during background and mass extinction
    Jonathan L Payne
    Department of Geological and Environmental Sciences, Stanford University, Stanford, CA 94305, USA
    Proc Natl Acad Sci U S A 104:10506-11. 2007
    ..Although factors other than geographic range have certainly affected extinction risk during many intervals, geographic range is likely the most consistently significant predictor of extinction risk in the marine fossil record...
  4. pmc Two-phase increase in the maximum size of life over 3.5 billion years reflects biological innovation and environmental opportunity
    Jonathan L Payne
    Department of Geological and Environmental Sciences, Stanford University, 450 Serra Mall, Building 320, Stanford, CA 94305, USA
    Proc Natl Acad Sci U S A 106:24-7. 2009
    ..These size steps coincide with, or slightly postdate, increases in the concentration of atmospheric oxygen, suggesting latent evolutionary potential was realized soon after environmental limitations were removed...
  5. pmc Calcium isotope constraints on the end-Permian mass extinction
    Jonathan L Payne
    Department of Geological and Environmental Sciences, Stanford University, Stanford, CA 94305, USA
    Proc Natl Acad Sci U S A 107:8543-8. 2010
    ..Collectively, the results point toward Siberian Trap volcanism as the trigger of mass extinction...
  6. doi request reprint The evolutionary consequences of oxygenic photosynthesis: a body size perspective
    Jonathan L Payne
    Department of Geological and Environmental Sciences, Stanford University, 450 Serra Mall, Bldg 320, Stanford, CA 94305, USA
    Photosynth Res 107:37-57. 2011
    ....
  7. pmc Long-term differences in extinction risk among the seven forms of rarity
    Paul G Harnik
    Department of Geological and Environmental Sciences, Stanford University, Stanford, CA 94305, USA
    Proc Biol Sci 279:4969-76. 2012
    ..These results suggest that current reductions in geographic range size will lead to pronounced increases in long-term extinction risk even if local populations are relatively large at present...
  8. ncbi request reprint Large perturbations of the carbon cycle during recovery from the end-permian extinction
    Jonathan L Payne
    Department of Earth and Planetary Sciences, Harvard University, 20 Oxford Street, Cambridge, MA 02138, USA
    Science 305:506-9. 2004
    ....