CL
Climate: Past, Present & Future

Vegetation

When ozone enters a leaf: why the details matter for Earth system models

When ozone enters a leaf: why the details matter for Earth system models

(Schematic cross-section showing leaf stomatal O_3 uptake, chloroplast oxidative stress, and the resulting downregulation of Earth’s global photosynthetic carbon uptake (GPP)) We usually think of ozone as a shield high in the atmosphere or as an air pollutant that harms human lungs near the ground. But plants also “breathe” ozone. Through microscopic pores called stomata, leaves take in carb ...[Read More]

Pollen, more than forests’ story-tellers

Pollen, more than forests’ story-tellers

Name of proxy Sporomorphs (pollen grains and fern spores) Type of record Biostratigraphy and Geochronology markers, Vegetation dynamics Paleoenvironment Terrestrial environment Period of time investigated Present to 360 million years How does it work? The sporomorphs (pollen grains and fern spores) are cells produced by plants involved in the reproduction. They are microscopic (less than a fifth o ...[Read More]