Members of the Archaea (the third domain of life) that can produce methane are referred to as methanogens. These organisms are prevalent in a wide range of anoxic environments, including the human distal gut, and account for 75 to 80 percent of the annual methane emissions on our planet. Therefore methanogens have significant implications for climate science, biotechnology and even aspects of human health. Despite their importance, the physiology and evolution of methanogens is still poorly understood.

Nature-inspired solutions have spawned such products as potential cancer cures from animal and plants, novel antibiotics, and gecko-inspired adhesives. This “bio-inspired” approach applies integrative methods from anatomy, animal function, evolution, and biomechanics to inspire novel synthetic materials.  Further, new methods for visualizing animals has opened new doors into understanding the diversity of life.  This lecture will discuss how studies of gecko form and functions have contributed to a broader understanding of bio-inspiration.

The historical environments in which species evolved have lasting influence on the communities and ecosystems that provide services to humanity today. Dr. Cavender-Bares considers the unfolding of evolutionary history in the deep past, the role of diversification in community assembly, and its consequences for ecosystem function. Current threats to naturally assembled systems are transforming the biosphere to novel conditions, with consequences for the trade-offs we face in managing Planet Earth.

In connection with our development of Viburnum (Adoxaceae) as a model lineage for studies of plant evolution and ecology, we have inferred a comprehensive dated phylogeny based on multiple lines of evidence.  Jointly with our phylogenetic inference, we have estimated past geographic movements and shifts between mesic forest biomes.  This provides us with reliable estimates for movements within and between continents throughout the Cenozoic, as well as for multiple instances of adaptation to colder climates.  Much of the action took place in Asia, with&nbsp