Definition: Protracheophytes are an extinct intermediary group existing between Non-Vascular Plants and Seedless Vascular Plants.
Morphology: Characterized by dichotomous branching.
Cellular Evolution: Parenchyma cells evolved into Hydroid cells. These cells contained some lignin but lacked the specialized tracheids found in later vascular plants.
Embryology: In the transition to vascular plants, the apical meristem (A.M.) switches to the top in embryology.
Example Species:Aglaophyton.
Hydroids in Aglaophyton contained lignin and specialized further to evolve into tracheids in SVPs.
Seedless Vascular Plants (SVPs / Tracheophytes)
Ecological Impact: Their emergence caused an "explosion" of plant life that turned barren land green.
Atmospheric Impact: SVPs helped stabilize $O_2$ levels in the atmosphere.
Biological Foundation: They formed the basis for the web of terrestrial life.
Adaptation: Significant evolutionary changes allowed these plants to move further away from water sources.
The Rhynie Chert and Early Colonization
Age: Over 400mya (million years ago).
Source: Silica from volcanic hot springs petrified this specific ecosystem.
Biodiversity in the Chert: The fossil record from this site includes:
Fungi
Lichens
Plants
Arthropods
First SVPs: Rhyniophytes
Status: Extinct.
Representative Genus:Cooksonia (425mya).
Defining Features:
Tracheids: Contained specialized vascular cells.
Primary Organ: The stem was the first organ of the plant.
Sporophyte Dominant: This shift occurred because tracheids evolved specifically in the sporophyte generation.
Lack of Organs: Had no roots or leaves.
Reproduction: Featured terminal sporangia and were homosporous.
Major SVP Clades: Lycophytes and Monilophytes
Lycophytes (Club Mosses):
Leaves: Evolved microphylls (leaves with a single vascular strand/vein).
Roots: Evolved from underground stems.
Rhizoids: Functioned as possible root hairs.
Key Genera:Lycopodium and Selaginella.
Monilophytes (Ferns and relatives):
Leaves: Evolved megaphylls (leaves with branching veins).
Megaphyll Evolution: Arose from the overlapping and fusing of branches.
Roots: Evolved from stems.
Rhizoids: Functioned as possible root hairs.
Diversity: Includes Ferns, Horsetails, and Whisk Ferns.
The Carboniferous Era: Height and Gigantism (360mya)
Selection Pressure: The evolution of megaphylls created pressure for plants to grow larger, leading to the development of secondary growth.
Giant Flora:
SVP trees reached heights of 100ft.
Lepidodendron: Featured unifacial vascular cambium (V.C.) and produced 2∘ (secondary) xylem only.
Giant Horsetails: Also dominated the landscape.
Geological Legacy: SVP remains from this era eventually compressed into coal.
Atmospheric Changes: Huge amounts of $O_2$ were produced, leading to giant fauna:
Insects:3ft Scorpions, 6ft Millipedes, and giant winged insects.
Amphibians:Eogyrinus (4.6m), Diadectes (2−3m), Limnoscelis (1.5m), and Seymouria (0.6m).
End of the Era (300mya):
The climate cooled and became arid.
Reason for Cooling: Giant megaphylls absorbed massive amounts of $CO_2$ and stored it as wood, reducing the greenhouse effect.
Mass Die-off: Giant SVPs died out because external fertilization requires water, which became scarce.
Anatomy and Reproduction in Lycophytes
Derived Traits: Roots, leaves (microphylls), and the strobilus.
Strobilus (Cone) Definition: A cluster of sporangia and leaves (sporophylls) located on branch tips.
Sporophylls: Specifically microphylls that bear sporangia.
Evolutionary Significance: Cones drastically increased spore production compared to the solitary terminal sporangia of ancestral plants (e.g., Cooksonia).