Extreme triple oxygen isotope fractionation in Equisetum

Triple oxygen isotope values of xylem water were measured along the length of smooth horsetail stems ( Equisetum laevigatum ). Extreme isotope enrichment is observed moving from base to stem tip. δ 18 O values range from −8.3‰ at the base to 82.6‰ at the tip. Δ′ 17 O values range from 0 to −1,797 per meg. The δ 18 O and Δ′ 17 O values are the most extreme measured for any terrestrial material and expand the known range of Δ′ 17 O values by fivefold for mass-dependent fractionation on Earth. The extreme isotope enrichments are explained using a hybrid evaporation/chain-of-lakes model, allowing us to refine the leaf respiration coefficient to θ k = 0.511 ± 0.001. This new value is required to explain the low Δ′ 17 O values previously measured in desert plants and animals and is critical when using fossil samples for paleoclimate reconstruction. Coexisting phytoliths and stem water were also measured. The 1000 ln 18 α silica-water value at the plant base (35.89‰) appears to be in isotopic equilibrium, with far smaller fractionations of 10.3‰ near the tip. The smaller fractionations at higher levels are explained by continual silica deposition as the plant elongates and the δ 18 O values of each segment become higher. The overall integrated phytolith value is a combination of early and late silica growth. The Δ′ 17 O silica − Δ′ 17 O water values are not in equilibrium, explained by a kinetic isotope effect, with a λ value of 0.5205 vs. 0.5244 for equilibrium. Phytolith isotope values may lead to erroneous interpretations for paleoclimate reconstruction.