The Paleo-ecology of C4 Evolution

Abstract:

Molecular clock analysis of extant plant lineages consistently place the earliest appearance of the C4 photosynthetic pathway in the mid-to-late Oligocene, coincident with a decline in atmospheric CO2 and a spread of dry environments. Most of the approximately 70 known lineages of C4 photosynthesis, however, evolved over the subsequent 23 million years since the Oligocene. Examination of living C3-C4 intermediate species, and close C3 relatives of modern C4 lineages, indicate that the C4 pathway evolved in regions of high heat and episodic drought and/or salinity, usually in the drier ends of the monsoon belts of the subtropics. Soils associated with transitional species are typically sandy, rocky, or salinized, and have low vegetation density, which in combination with high air temperature allows for high surface heat loads that warm leaves to near 45°C. Under such conditions in low CO2 atmospheres, the rate of photorespiration is very high and would greatly impair C3 photosynthesis and establish conditions favoring C4 evolution. However, studies with modern taxa do not address whether the extreme habitats proposed to facilitate C4 evolution were actually present at the time when the C4 pathway evolved in any given lineage. Here, we examine the paleo-record to evaluate the environmental conditions present in the C4 centres of origin when the respective transitions from C3 to C4 photosynthesis are estimated to have occurred.