However, there are still many conflicting theories surrounding the origins of bacteria. Even though microfossils of ancient bacteria have been discovered, some scientists argue that the lack of identifiable morphology in these fossils means they can not be utilised to draw conclusions on an accurate evolutionary timeline of bacteria. Nevertheless, more recent technological developments means more evidence has been discovered.
Bacteria evolve in a similar process to other organisms. This is through the process of natural selection, whereby beneficial adaptations are passed onto future generations until the trait becomes common within the entire population.[10] However, since bacteria reproduce via binary fission—a form of asexual reproduction—the daughter cell and parent cell are genetically identical. This makes bacteria susceptible to environmental pressures, an issue that is overcome by sharing genetic information via transduction, transformation, or conjugation. This allows for new genetic and physical adaptations to develop, allowing bacteria to adapt to their environment and evolve. Furthermore, bacteria can reproduce in as little as 20 minutes,[11] which allows for fast adaptation, meaning new strains of bacteria can evolve quickly. This has become an issue regarding antibiotic resistant bacteria.[citation needed]
Thermophile bacteria from deep-sea vent. This organism eats sulfur and hydrogen and fixes its own carbon from carbon dioxide.
Thermotogales
Apex Chert near ancient hydrothermal vents.[12][13] These rocks date back 3.46 billion years and these fossils are thought to have belonged to early thermophilic bacteria. This is because these organisms do not require oxygen to survive, which was an element that was not present in large quantities in Earth's early atmosphere.[14] Furthermore, this phylum still has living species such as Thermotoga neapolitana, which still largely resemble their ancestral form and still live around these vents, which some scientists have used as evidence to support this theory.[citation needed
]
More recent evidence has emerged, which suggests that Thermotogales evolved roughly between 3.2-3.5 billion years ago. This evidence was collected via gene sequencing of bacterial nucleoids to reconstruct their phylogeny.[1][2] The first major divergence within the Thermotogales phylum was between Thermotogaceae and Fervidobacteriaceae, however, it is yet to be determined as to when this occurred. The family of Thermotogaceae then diverged into the genus Thermotoga and the genus Pseudothermotoga.[15] The genus Thermotoga represents the majority of existing hyperthermophiles and are unique in that they are wrapped in an outer membrane that is referred to as a "toga". Some extant Thermotoga species include T. neapolitana.[citation needed]
Colourful Thermophilic (Heat-loving) Archaebacteria Stain. Archaebacteria are nowadays regarded as their own domain Archaea, distinct from Thermotogales.
Cyanobacteria or blue green-algae is a gram negative bacteria, a phylum of photosynthetic bacteria that evolved between 2.3-2.7 billion years ago.[16] This prokaryote produces oxygen as a byproduct of its photosynthetic processes.[17] They have made a distinctive impact in pharmaceutical and agricultural industry due to their potential of making bioactive compounds with antibacterial, anti-fungal, antiviral, and anti-algal properties. Typically they form motile filaments referred to as hormogonia, which can form colonies and then bud and travel to colonise new areas. They have been located in environments including freshwater, oceans, soil and rock (both damp and dry), as well as arctic rock.[citation needed]
These organisms had evolved photosynthetic reaction centres and became the first oxygen producing
Great Oxygenation Event roughly 2.3 billion years ago[19]
English: Bloom of cyanobacteria in a freshwater pond. This accumulation in one corner of the pond was caused by wind drift. It looked as if someone had dumped a bucket color into the water.
However, the closest known relatives of oxygen producing Cyanobacteria did not produce oxygen.[20] These relatives are Melainabacteria and Sericytochromatia, neither of which can photosynthesise. Through genetic sequencing, scientists discovered that these two groups did not have any remnants of the genes required for the functioning of photosynthetic reactions.[20] This suggests that Cyanobacteria, Melainabacteria, and Sericytochromatia evolved from a non-photosynthetic common ancestor.[citation needed]
^"The Rise of Oxygen". Astrobiology Magazine. 2003-07-30. Archived from the original on 2015-09-06. Retrieved 2019-05-21.{{cite web}}: CS1 maint: unfit URL (link)
^"When Did Bacteria Appear?". Astrobiology Magazine. 2004-04-18. Archived from the original on 2019-01-12. Retrieved 2019-05-21.{{cite web}}: CS1 maint: unfit URL (link)
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