An efficient method for estimating vein density of Glossopteris and its application

Abstract

Glossopteris‐type leaves are the most abundant floristic element from the Gondwanan continent and are recorded throughout the Permian, which was a period of extreme icehouse‐to‐hothouse climatic global change. Fossil leaf traits can be useful for the reconstruction of palaeoenvironments and identification of climatic changes throughout geological time, but the conservative morphology of Glossopteris leaves has thus far made them difficult to use for this purpose. If the characters of Glossopteris can be better quantified then it should make them useful for tracking environmental changes over a wide geographical area and over a long time interval. Venation density is a highly variable leaf trait that might be useful for this purpose. This trait can be calculated, usually as vein length per centimetre squared, but this can be a time‐consuming procedure. In this paper we propose a new rapid method to estimate venation density in a conical sector of Glossopteris leaf lamina using an accurate linear model whose predictors are three linear venation densities, measured as veins per centimetre. In addition to substantially reducing the data collection time, it is less biased and more reproducible than methods applied previously with this leaf type. Using this more robust method, preliminary results significantly distinguish the venation densities of leaves produced in wet and drier ecosystems, matching a pattern similar to modern plants. This is the first survey using a large sample size to reveal that environmental stress controlled the vein architecture of Palaeozoic plants, in a manner similar to plants in modern ecosystems.

Functional traits of fossil plants

“…Vein density is measurable on compression/impression leaf fossils and has been used extensively in taxonomic work and to infer paleoecophysiology (Uhl & Mosbrugger, 1999;Boyce et al, 2009;Esperanc ¸a Júnior et al, 2023;Fig. 2a).…”

“…(a) Vein density trait illustrated for Permian Glossopteris from Esperança Júnior et al . (2023, reused with permission) Bar, 5 mm. (b) Leaf g max trait (a function of stomatal density and pore geometry) illustrated on Cretaceous aged Podocarpaceae compression fossils (Pole & Philippe, 2010, reused with permission) Bar, 50 μm.…”