Gene

Devonian

Structural basin

Physics

Sporangium

Propagule

Genome

Paleontology

Spore

Sporophyte

Photosynthesis

Ecology

Acoustics

Macrofossil

Xanthium

Fern

Pennsylvanian

Pollen

Period (music)

Biochemistry

Algae

Plant evolution

Botany

Biology

Nature Plants

The colonization of land by vascular plants is an extremely important phase in Earth’s life history. This key evolutionary process is thought to have begun during the Middle Cambrian                  1                 period and culminated in the Silurian/Early Devonian period (interval about 509–393 million years ago (Ma)), and is documented primarily by microfossils (that is, by dispersed spores, phytodebris including fragments of algae, tissues, sporangia and cuticles), tubes and rare megafossils                  2                . A newly recognized fossil cooksonioid plant with in situ spores from the Barrandian area, Czech Republic, is of the highest importance because it represents extremely ancient megafossil evidence of land plant diploid generation: sporophytes (~432 Ma). The robust size of this plant places it among the largest known early polysporangiate land plants and it is probable that it attained adequate size for both aeration and effective photosynthetic competence. This would mean not only that sporophytes were photosynthetically autonomous but also that the they might have been able to sustain a relatively gametophyte-independent existence. Ancient fossil Cooksonia plants from the Czech Republic are among the largest known early polysporangiate plants from when vascular plants were colonizing the land. They were of sufficient size to support effective photosynthesis.

Sporophytes of polysporangiate land plants from the early Silurian period may have been photosynthetically autonomous