Ferns are classified as the most advanced seedless vascular plants.
They exhibit characteristics commonly observed in seed plants, including:
Large leaves
Branching roots
Whisk Ferns (Psilophytes)
Whisk ferns, in contrast, lack both:
Roots
Leaves
The absence of these structures is believed to be a result of evolutionary reduction.
Evolutionary reduction is defined as a process whereby natural selection leads to the decrease in size of a structure that is no longer advantageous in a given environment.
Photosynthesis occurs in the green stem of whisk ferns.
Sporangia are contained in small yellow knobs located at the tips of branch stems.
Whisk ferns have been classified outside the domain of true ferns, yet:
Recent comparative DNA analysis indicates that this group may have lost their vascular tissue and roots through evolution.
This analysis suggests whisk ferns are closely related to true ferns.
Characteristics and Habitat of Ferns
Ferns are identifiable for their large fronds and are regarded as the most recognizable seedless vascular plants.
Approximately 12,000 species of ferns are found across diverse environments, including:
Tropical regions
Temperate forests
While certain fern species can adapt to dry environments, the majority thrive in moist and shaded habitats.
Historical Appearance in the Fossil Record
Ferns first appeared in the fossil record during the Devonian period, estimated at 416-359 million years ago.
Their diversification occurred during the Carboniferous period, around 359-299 million years ago.
Geological Time Scale
The geological time scale is divided into Eons, Eras, and Periods, detailed as follows:
Quaternary: 1.6 million years ago (Cenozoic Era)
Tertiary: 66 million years ago (Cenozoic Era)
Cretaceous: 138 million years ago (Mesozoic Era)
Jurassic: 205 million years ago (Mesozoic Era)
Triassic: 240 million years ago (Mesozoic Era)
Permian: 290 million years ago (Paleozoic Era)
Carboniferous: 360 million years ago (Paleozoic Era)