D H Rothman

Summary

Affiliation: Massachusetts Institute of Technology
Country: USA

Publications

  1. pmc Global biodiversity and the ancient carbon cycle
    D H Rothman
    Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, USA
    Proc Natl Acad Sci U S A 98:4305-10. 2001
  2. pmc Dynamics of the Neoproterozoic carbon cycle
    Daniel H Rothman
    Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, USA
    Proc Natl Acad Sci U S A 100:8124-9. 2003
  3. ncbi request reprint Re-examination of the "3/4-law" of metabolism
    P S Dodds
    Department of Mathematics, Massachusetts Institute of Technology, Cambridge, MA 02139, USA
    J Theor Biol 209:9-27. 2001
  4. ncbi request reprint Geometry of river networks. I. Scaling, fluctuations, and deviations
    P S Dodds
    Department of Mathematics, Massachusetts Institute of Technology, Cambridge, MA 02139, USA
    Phys Rev E Stat Nonlin Soft Matter Phys 63:016115. 2001
  5. ncbi request reprint Geometry of river networks. II. Distributions of component size and number
    P S Dodds
    Department of Mathematics, Massachusetts Institute of Technology, Cambridge, MA 02139, USA
    Phys Rev E Stat Nonlin Soft Matter Phys 63:016116. 2001
  6. ncbi request reprint Geometry of river networks. III. Characterization of component connectivity
    P S Dodds
    Department of Mathematics, Massachusetts Institute of Technology, Cambridge, MA 02139, USA
    Phys Rev E Stat Nonlin Soft Matter Phys 63:016117. 2001

Detail Information

Publications6

  1. pmc Global biodiversity and the ancient carbon cycle
    D H Rothman
    Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, USA
    Proc Natl Acad Sci U S A 98:4305-10. 2001
    ..As a consequence, the paleontological record of biodiversity provides an indirect estimate of the fluctuations of ancient CO(2) levels...
  2. pmc Dynamics of the Neoproterozoic carbon cycle
    Daniel H Rothman
    Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, USA
    Proc Natl Acad Sci U S A 100:8124-9. 2003
    ..The terminal event, at the Proterozoic-Cambrian boundary, signals the final diminution of the reservoir, a process that was likely initiated by evolutionary innovations that increased export of organic matter to the deep sea...
  3. ncbi request reprint Re-examination of the "3/4-law" of metabolism
    P S Dodds
    Department of Mathematics, Massachusetts Institute of Technology, Cambridge, MA 02139, USA
    J Theor Biol 209:9-27. 2001
    ..We find that present theories for alpha = 3/4 require assumptions that render them unconvincing for rejecting the null hypothesis that alpha = 2/3...
  4. ncbi request reprint Geometry of river networks. I. Scaling, fluctuations, and deviations
    P S Dodds
    Department of Mathematics, Massachusetts Institute of Technology, Cambridge, MA 02139, USA
    Phys Rev E Stat Nonlin Soft Matter Phys 63:016115. 2001
    ..The extent of approximate scaling is significantly restricted by these deviations, and will not be improved by increases in network resolution...
  5. ncbi request reprint Geometry of river networks. II. Distributions of component size and number
    P S Dodds
    Department of Mathematics, Massachusetts Institute of Technology, Cambridge, MA 02139, USA
    Phys Rev E Stat Nonlin Soft Matter Phys 63:016116. 2001
    ..The calculations identify a single length scale as a measure of size fluctuations in network components. This article is the second in a series of three addressing the geometry of river networks...
  6. ncbi request reprint Geometry of river networks. III. Characterization of component connectivity
    P S Dodds
    Department of Mathematics, Massachusetts Institute of Technology, Cambridge, MA 02139, USA
    Phys Rev E Stat Nonlin Soft Matter Phys 63:016117. 2001
    ..Fluctuations in side stream numbers are shown to be a direct result of fluctuations in stream lengths. This is the last paper in a series of three on the geometry of river networks...