TL;DR: The leaves of stinging trees appeared better suited to the rapid colonisation of rainforest gaps, than in fending off or avoiding herbivore damage.
Abstract: Leaf growth dynamics and leaf quality of Dendrocnide moroides (Wedd.) and Dendrocnide cordifolia (L.S.Sm.) Jackes and Hurley varied widely with age, season, plant height and habitat. Althoughleaves were produced continuously, growth rates varied seasonally. Leaf moisture and nitrogen content increased in spring and summer and decreased with age, while toughness increased with age. All leaf growth attributes varied with height, with the majority of activity occurring on mid-sized plants. Leafgrowth rates and proportions of different leaf age classes were similar for both species. Leaves were larger and lived longer in shade. Size and longevity responded rapidly to changing light conditions, reflecting their ability to survive in small rainforest gaps. Leaves of all ages were highly nutritious and the exceptionally nutritious young leaves were abundant throughout the year making them susceptible to herbivore attack. However, immature stinging tree leaves were densely covered with painful stinging hairs and hair density decreased with age. Further to causing pain, stinging hairs of D. moroides and D. cordifolia are shed continuously and may deter mammalian herbivores by causing allergic reactions. However, the leaves of stinging trees appeared better suited to the rapid colonisation of rainforest gaps, than in fending off or avoiding herbivore damage.
TL;DR: A Miocene flora from the Chalk Mountain Formation occurring on a spur of the Warrumbungle Volcano Complex to the north-west of Coonabarabran near Bugaldie is described in this article.
Abstract: A Miocene flora from the Chalk Mountain Formation occurring on a spur of the Warrumbungle Volcano Complex to the north-west of Coonabarabran, near Bugaldie is described. The flora consists of representatives in the families Equisetaceae ( Equisetum sp. indet.), Isoetaceae and Araucariaceae ( Agathis sp.). Among the angiosperm families are Cunoniaceae ( Ceratopetalum priscum ), Moraceae, Myrtaceae ( Eucalyptus bugaldiensis ), Urticaceae ( Dendrocnide sp. A aff. D. excelsa ). This paper describes the first fossil record of Dendrocnide (Urticaceae) leaves from Australia and the second post-Cretaceous record of the genus Equisetum , the first from the Miocene. The flora includes rainforest, swamp and sclerophyll plant forms and indicates a warming and drying climate as the Australian plate moved northwards during the Middle Miocene.