PHANEROZOIC INCREASE IN HUBBELL'S THETA: LINKING DIVERSITY FROM THE ALPHA LEVEL TO THE PROVINCIAL LEVEL
If neutrality is supported, it would allow for a linkage of diversity across a wide range of scales, providing a mechanism explaining the Phanerozoic correlation of global and alpha diversity. Arguments based on additive diversity partitioning questioned the importance of the linkage between alpha and global diversity, and these arguments suggested that the primary cause of the Phanerozoic rise in diversity must lie in an increasing number of provinces through the Phanerozoic or their increasing distinctiveness. If marine communities behave as neutral systems, the increase in Hubbell's theta would suggest that the rise in Phanerozoic diversity was also driven by diversification at the alpha through provincial levels.
In addition, the Phanerozoic increase in Hubbell's theta would also be reflected in an increase in evenness. Such an increase in evenness was previously seen as a complication because rarefaction requires communities to have the same evenness. If neutrality holds, an increase in evenness is an expected result of an increase in theta: it would be a symptom of increasing diversification, not a complication.