Evidence for xylem adaptations to drought in ancient Cordaites of the Carboniferous

Ancient land plants faced the same challenges to growth and survival as modern land plants, including the need to resist xylem embolisms imposed by drought in order to main water supply to leaves. Cordaites, considered to be ancestors of the conifers, were some of the first trees on Earth and are often described as the most drought resistant plants in the North American landscape from the Late Missisipian (~320 MYA) to the early Permian (~250 MYA). Cordaites were common in both mires and dry uplands, however, suggesting considerable variation in drought tolerance, but neither the extent of this variation nor the particular xylem features associated with dryland habitats have been previously examined. We measured xylem anatomical traits including tracheid diameter (D) and wall thickness (t), for Cordaites roots and stems from three sites in Central North America: What Cheer IA, Sahara IL and Lewis Creek KY. From these data we calculated mechanical strength (t/b), which was used to estimate vulnerability to drought embolism (P50) based on comparisons with modern plants. In addition, we used the model of Wilson et al. (2008) to calculate the specific conductivity (Ksp), a measure of xylem water transport capacity. D and Ksp of Cordaites stems were similar to that typical of modern conifers but t/b tended to be lower. However, Cordaites exhibited significant variation in D, t, Ksp and t/b across sites. Stem P50 estimated from comparisons with modern plants ranged from approximately -4 at Lewis Creek to as low as -7 MPa at Sahara. We also found differences between stems and roots for Cordaites. Compared to stems, roots had larger D and higher Ksp, but lower t and t/b, resulting in a P50 ranging from approximately -2 to -4 MPa. In the roots of Sahara Cordaites, lower t/b in roots was a result of both significantly larger conduits and significantly thinner conduit walls compared to stems. Thus, hydraulic segmentation in Cordaites could have facilitated their survival in drier upland habitats, as root embolisms early on during drought could have hydraulically isolated the plant from drying soil. Our data suggest that Cordaites were similar in water transport properties but with low to moderate drought tolerance compared to modern conifers. Observation that Cordaites water transport properties varied across sites supports the idea that they were an ecological diverse plant group. Furthermore, Cordaites from Sahara exhibited a suite of traits typical of modern drought adapted plants, including: low D and Ksp combined with greater t, higher t/b and greater differentiation in t/b between roots and stems. Thus, we provide evidence from fossilized plants that associations between xylem features and habitat, as well as some modern drought adaptations, may be nearly as old as trees themselves.