EGU25-5945, updated on 14 Mar 2025
https://doi.org/10.5194/egusphere-egu25-5945
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Tuesday, 29 Apr, 14:20–14:30 (CEST)
 
Room -2.93
How well does palynological data represent vegetation phylogenetic diversity?
Phillip Jardine
Phillip Jardine
  • Institute of Geology and Palaeontology, University of Münster, Münster, Germany (jardine@uni-muenster.de)

Reconstructing past biodiversity changes, and integrating these with modern biodiversity assessments, requires that fossil assemblages accurately capture key aspects of diversity (as represented by biodiversity metrics, for example). This is particularly true for the plant fossil record, where separate organs such as sporomorphs (pollen and spores) and leaves have to be used as proxies for understanding vegetation composition and diversity change through time. Although much attention has been focused on how well fossil plant assemblages capture variations in species richness, other aspects of diversity have until recently been relatively overlooked.

Here, I focus on phylogenetic diversity (PD), which represents the amount of evolutionary history contained in an assemblage of taxa. It can therefore provide a more detailed assessment of biodiversity gains and losses through time and space, and their underlying causes and consequences, relative to simple counts of the number of species present in a sample, and as such is used both as a conservation metric and as a tool to understand community assembly. To date, however, PD has been underexplored by palaeoecologists, and it is not currently known how well variations in vegetation PD across broad spatial scales are captured by sporomorph assemblage data. I compare estimates of seed plant PD from vegetation data and surface pollen samples from across North and South America. The results indicate a relatively low concordance between vegetation and pollen PD, and differing relationships with climate data, suggesting that sporomorph data cannot be used as a straightforward PD record. Other data sources (e.g. aDNA data for late Quaternary datasets, macrofossil data in deeper time settings) need to be considered for reconstructing vegetation PD through time. More generally, how well sporomorph data captures other aspects of plant biodiversity, and how successfully the plant fossil record can be used for conservation-relevant questions, ought to be critically (re-)assessed.

How to cite: Jardine, P.: How well does palynological data represent vegetation phylogenetic diversity?, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-5945, https://doi.org/10.5194/egusphere-egu25-5945, 2025.