HERBIVORE AND POLLINATOR EVENTS DURING THE PREANGIOSPERMOUS MESOZOIC: A CONNECTION TO GLOBAL CLIMATE?
The second event was expansion of associations during the Middle Jurassic of western Eurasia, involving long-proboscid, fluid- and pollen feeding lineages of Mecoptera (aneuretopsychine scorpionflies), Neuroptera (kalligrammatid lacewings), and Diptera (brachyceran flies). Suspect plant taxa accommodating these long siphonate mouthparts were cheirolepidiaceous conifers, caytonialeans, ginkgophytes, bennettitaleans and gnetaleans providing secretory fluid and pollen rewards. This distinctive feeding type formed a gymnosperm pollination mode lasting to the mid Cretaceous, at which time angiosperm pollination originated and replaced older gymnosperm associations.
Importantly, Middle Triassic to Early Cretaceous atmospheric concentrations range from 12–19 pO2, well below the current norm. Such low partial pressures exert distinctive responses from insects with a respiratory system of ramifying tubules originating from valvular spiracles. Also, atmospheric pCO2 was considerably more elevated than current levels, suggesting low levels of accessible nitrogen from foliage, tissue secretions and pollen. Insect herbivores and pollinators require both O2 levels adequate for respiratory activity and access to nitrogen sufficient for body maintenance, reproduction and activities such as flight. Both requirements may explain the expansion of herbivory and pollination as a consequence of greater access to nitrogen while maintaining safe levels of respiratory metabolism.