NO GLOBAL SHIFT IN LEAF MASS PER AREA ACROSS THE CRETACEOUS-PALEOGENE BOUNDARY
We did not observe a loss of high LMA species after the KPB: the expectation if plants stopped following slow return-on-investment strategies. Indeed, we found no evidence for a shift in leaf economic strategies across the KPB: neither the median species LMA nor the distribution of species in LMA-space appreciably changed for over two million years straddling the KPB. Around 64 Ma, LMA declined at sites interpreted as rainforests near the western margin of the basin; similarly low values are commonly observed in present-day rainforests. The western margin localities where we observed this downward shift are found close to the Front Range of the Rocky Mountains, where an orographic precipitation regime is thought to have developed during the deposition of the Denver Basin. We found that among these Front Range adjacent localities, LMA and mean annual precipitation were inversely correlated, a pattern consistent with observations of extant plants.
Overall, in the Denver Basin we found that local climate and biome type played a larger role in determining leaf ecological strategies than a global signal associated with the Chicxulub bolide impact.