paleobotany

Paleobotany is the scientific study of fossil plants and ancient plant life. It seeks to understand how plants originated and diversified, how past floras formed ecosystems, and how plant life influenced and responded to changes in climate and atmosphere over geological time. The field combines paleontology, botany, geology, and geochemical methods to reconstruct past vegetations, their physiologies, and their ecological roles.

Paleobotanical evidence includes macrofossils such as leaves, stems, seeds, and wood, as well as microfossils such as pollen, spores, and phytoliths. Techniques include the analysis of plant cuticles and stomata, palynology (pollen and spores), microfossil processing, carbon isotope studies, and imaging methods. Fossil floras can reveal plant lineages, growth forms, and adaptations to terrestrial environments.

Research spans major intervals such as the rise of land plants in the Paleozoic, the evolution of seed plants, the diversification of gymnosperms, and the rapid emergence of angiosperms in the Cretaceous. Paleobotany also investigates ancient forests, coal-forming swamps, and vegetation shifts associated with climate change. Data from fossil plants are used to infer atmospheric composition, climate, and biogeography of the past.

Overall, paleobotany provides essential context for understanding plant evolution, ecosystem dynamics, and the history of Earth's biosphere. It is an interdisciplinary field that relies on field collection, stratigraphy, microscopy, geochemical analysis, and comparative biology to interpret plant life from millions of years ago.