SEAFOOD THROUGH TIME REVISITED: THE PHANEROZOIC INCREASE IN MARINE TROPHIC RESOURCES AND ITS MACROEVOLUTIONARY CONSEQUENCES
In order to pull together available information and focus attention on this issue, we have developed a new, synthetic curve of global average marine productivity for the Phanerozoic. We have then used simple but explicit models of the stages of allopatric speciation to develop a general theory (based in part on previous concepts of speciation on islands, such as Wilson's "Taxon Cycle" and the Grants’ “Speciation Cycle”) of how changes represented in this curve might have contributed to local, regional, and global taxonomic diversity patterns. The role of trophic resources (“food”) in species formation depends on where in the cycle of isolate formation, persistence, differentiation, and persistence/expansion a species is. The Speciation Cycle attempts to develop explicit and testable hypotheses of the frequently very different effects of food on each of these stages of speciation. Application of the Speciation Cycle to intervals of the Phanerozoic marine productivity curve may reveal and/or improve understanding of important connections between ecology and macroevolution.