From pre-historic Charophytes to Angiosperms.A crash course in the evolution of terrestrial plants.

The evolution of seedless vascular plants towards the end of the Silurian period, 425 million years ago, allowed for the re-transformation of the pre-historic landscape. Originally desolate, then gradually filled with vertically challenged, ground hugging bryophytes; The rise and prominence of seedless vascular plants allowed for rigidity & vertical growth, which had previously eluded the first permanent land dwelling flora (Evert, Raven & Eichhorn 2013).   As we’ve learnt from previous posts, both charophytes and bryophytes lacked vascular tissue. This inevitably restricted their ability to grow vertically, but also radiate in their new found terrestrial environment without the constant availability of surface or ground water (Willis & McElwain 2014). So, what enabled seedless vascular plants to rise above their non-vascular counterparts, and successfully dominant the Silurian-Carboniferous landscape? One of the most significant evolutionary innovations, along wit

During the Upper Ordovician era 475 million years ago, the terrestrialization of charophycean algae led to the evolution of the first permanent land-dwelling plants, the bryophytes (Willis & McElwain 2014). The term bryophyte is derived from the Greek words Byron , meaning moss, and Phyton , meaning plant (Reece & Campbell 2012). It is used to describe plants with no vascular or specialised transportation system. There are three phyla within the bryophyte group. Anthocerophyta , the hornworts . Bryophyta , which are the mosses. And lastly,  Hepatophyta or the liverworts (Reece & Campbell 2012). (Classification of bryophytes, Plant science 4 U 2016) Although bryophytes lack a specialised vascular system, they do have simple water conducting cells which are non-lignified (Willis & McElwain 2014). They also have several shared characteristics with vascular plants of today, which enables them to be distinguished from charophytes (Evert, Raven & Eichhor

One of the most important evolutionary events in the history of life, which shaped our global environment as we see it today, can be dated back to the mid-Paleozoic era between 460 and 360 million years ago (Crane & Kenrick 1997, p. 33). The transition of aquatic plant life to terra firma enabled the commencement of terrestrial life. Phylogenetic studies have linked the ancestral origin of land plants to a charophycean green algae. Charophycean green algae share several similarities with land plants (Crane & Kenrick 1997, p. 34). Both plants and charophyceans are multicellular, eukaryotic, photosynthetic autotrophs. Both groups also share similarities in the structure of their cell walls, which contain cellulose. Chloroplasts containing the photosynthetic pigments chlorophyll a and b are also evident in both groups (Reece & Campbell 2012, p. 600). So how did charophytes make the transition onto land? Charophycean algae inhabited shallow waters around the banks o

Take a look outside at the lush green mountain ranges that surround you. Take a leisurely hike through a nearby nature track. Perhaps take a walk through your local botanic garden, or even your own garden, and count the number of different types of trees, plants and flowers you see. Chances are, there will be more plants than you would want to, or could care to count. Close your eyes and take a deep breath, fill your lungs with the oxygen that plants produce through photosynthesis. When the Earth formed approximately 4.5 billion years ago, our planet was lifeless and vastly different from the unique and diversified ‘David Attenborough style’ planet we see today.  The origin of plant life remained stagnant for several billions of years until a photosynthetic algae, Cyanobacteria, changed the surface of the Earth 1.2 billion years ago and paved the way for other terrestrial plant forms to flourish around 500 million years ago. It is estimated that there are now more th