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Global Biodiversity, Biochemical Kinetics, and the Energetic-Equivalence Rule
Andrew P. Allen,*James H. Brown,James F. Gillooly
The latitudinal gradient of increasing
biodiversity from poles to equator is one of the most prominent but
least understoodfeatures of life on Earth. Here we show that species
diversitycan be predicted from the biochemical kinetics of metabolism.We first demonstrate that the average energy flux of populationsis
temperature invariant. We then derive a model that quantitativelypredicts how species diversity increases with environmental
temperature.Predictions are supported by data for terrestrial,
freshwater,and marine taxa along latitudinal and elevational
gradients. Theseresults establish a thermodynamic basis for the
regulation ofspecies diversity and the organization of ecological
communities.
Department of Biology, University of New Mexico, Albuquerque, NM
87131, USA.
*
To whom correspondence should be addressed. E-mail:
drewa{at}unm.edu
The editors suggest the following Related Resources on Science sites:
In Science Magazine
LETTERS
Michael A. Huston;, James H. Brown, Andrew P. Allen, and James F. Gillooly (24 January 2003) Science299 (5606), 512.
[DOI: 10.1126/science.299.5606.512] |Full Text »|PDF »
TECHNICAL COMMENTS
David Storch (17 January 2003) Science299 (5605), 346b.
[DOI: 10.1126/science.1078627] |Full Text »|PDF »
TECHNICAL COMMENTS
Andrew P. Allen, James H. Brown, and James F. Gillooly (17 January 2003) Science299 (5605), 346c.
[DOI: 10.1126/science.1079964] |Full Text »|PDF »
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