Campanian Stage
The Campanian (84–71 Ma) is the fifth epoch of the Late Cretaceous, occurring after the Santonian, before the Maastrichtian.
Geologic Age
83.6±0.2–72.1±0.2 Ma
Eon / Era / Period / Epoch
What happened during this time?
Palms (Arecaceae) are the first modern family of monocots appearing in the fossil record around this time
Based on fossil leaves, modern-looking tropical rainforests already existed since 80 Ma in northeastern Africa in an area corresponding to 10 % of the modern Amazonian or 25 % of the Congolese (Coiffard et al. 2023)
Study by Mallon and Anderson (2013) indicates that during this time food resources were limiting for dinosaurs, and that niche partitioning was present for these animals
Plants weren't super-abundant to support large herbivores; species had to share available food sources by specializing on different types of vegetation
Ankylosaurs probably specialized on eating ferns, because they stood low to the ground, and their wide beaks would have allowed them to feed efficiently on abundant, relatively low-nutrient plants.
However, within this group, the family known as nodosaurids (clubless ankylosaurs) had more efficient jaw mechanics that might have enabled them to include tougher plants in their diets.
Ceratopsids had skulls that suggest they were adapted to feeding on mid-sized shrubs
Taller hadrosaurs were less picky and would have fed on anything within reach.
Mite houses, or acarodomatia, found on the leaves from angiosperm leaves discovered in the Kaiparowits Formation (76.6-74.5 Ma) in southern UT (Macracken, Miller, and Labandeira 2019)
These structures facilitate tri-trophic interactions between the host plant, its fungi or herbivore adversaries, and fungivorous or predaceous mites by providing shelter for the mite consumers
Left: Acrodomatia from mites living in angiosperm leaves