T56 Fossils Plants as Paleoenvironmental Recorders II
Sunday, 4 November 2012
1:30 PM - 5:30 PM
202AB
USING BUG BITES ON FOSSIL LEAVES TO RECONSTRUCT FOREST HEALTH AND ECOSYSTEM STABILITY
Paper number: T56-10
Program: Technical Sessions
Time: 3:45 PM – 4:05 PM
Authors
Abstract
These conclusions were applied to the early Paleogene of the Bighorn Basin, Wyoming, to test whether Paleocene-Eocene Thermal Maximum forests were stressed, unbalanced ecosystems. Because insect damage diversity and frequency are correlated with temperature, the PETM flora (20.1 ± 2.8oC mean annual temperature, or MAT) was compared with a flora from the Early Eocene Climatic Optimum (22.2 ± 2oC MAT). Leaf area damaged during the PETM is significantly higher than during the EECO, suggesting decreased leaf nitrogen concentrations and a corresponding increase in insect feeding rates. However, both floras have the combination of high plant diversity, insect damage diversity, and insect damage specialization that suggest balanced and fully functional ecosystems. In particular. the diversity and prevalence of host-specialized damage types on many different PETM plant species is striking, indicating well-developed specialized feeding associations on a broad spectrum of host lineages.