I didn’t mean questioning the idea of models explaining the variations in fossils over time. I meant rethinking how to model them. Are you saying that there hasn’t been any discussion of revising the models, to account for the Cambrian explosion? However that may be, has anyone even tried to simulate the Cambrian explosion, or anything like it?
A quick google scholar search gives the following:
https://www.cambridge.org/core/jour...arine-orders/A6C7BA0BBD638ECFB2DA91AD655468A2
"This model appears to describe adequately the “explosive” diversification of known metazoan orders across the Precambrian-Cambrian Boundary, suggesting that no special event, other than the initial appearance of Metazoa, is necessary to explain this phenomenon."
https://www.sciencedirect.com/science/article/pii/S0012825215000744
Here we reveal the dynamics of the earliest diverse skeletal metazoan communities known, the early Cambrian (Tommotian–Atdabanian) archaeocyathan sponge reefs, over a period of 20 million years from their first appearance ~ 535 million years ago (Ma) until the first mass extinction event ~ 512 Ma."
https://www.annualreviews.org/doi/abs/10.1146/annurev.earth.33.031504.103001
"The increase in disparity (the origin of the phyla) and diversity are best understood as being the result of the interplay of the combinatorial bilaterian developmental system and the increase in the number of needs the first bilaterians had to meet as complex ecological interactions developed. "
Diversity partitioning during the Cambrian radiation
"Using a comprehensive database and sampling standardization, we dissect global diversity patterns. The trajectories of within-community, between-community, and global diversity during the main phase of the Cambrian radiation revealed a low-competition model,"
Does that help?