Insect leaf-chewing damage tracks herbivore richness in modern and ancient forests.

However, this relationship has not been systematically addressed, and the consistent correlation in the fossil record of total and endophytic DTR strongly suggests that it may be significant [3] , [9] .

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Spearman's rank-order correlations between each fossil site and the pooled extant sites were all highly significant ( Table S4 ), indicating that the ranking of DTs in the Cretaceous and Paleogene floras is broadly similar to that of DTs most commonly induced by our living insect species.

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