Cyanobacteria fossils are the oldest known fossils on Earth. Stromatolites found near Shark Bay, Western Australia, which are made by cyanobacteria, have been dated back to 3.5 billion years in the Paleoarchean Era . They survive to modern day. Identical stromatolites are being formed not 15 miles from there 3.5 billion year old fossilised ancestors.
Icthyosaurs on the other had appeared in the fossil record about 245 million years ago in the Middle Triassic Epoch. They died out about 90 million years ago in the Upper Cretaceous Epoch, about 25 million years before the KT extinction that saw the deaths of the other great marine reptiles the mosasaurs and the pleisoasurs as well as all non avian dinosaurs.
fossils
Some index fossils during the Triassic period include ammonites, conodonts, and certain marine reptiles like nothosaurs and thalattosaurs. These fossils are used by paleontologists to help date and correlate rock layers from that time period. They provide important information about the environments and life forms of the Triassic era.
Geologists used a combination of fossil evidence, rock layers, and radiometric dating techniques to develop the geologic time scale. Fossils provide a record of past life forms, while rock layers indicate the relative ages of different geological events. Radiometric dating allows for assigning numerical ages to specific rock formations.
Fossils can be buried and subjected to heat and pressure during the rock cycle, but they do not usually melt. Instead, the organic material in fossils can be transformed into carbon-rich substances like graphite or coal under high temperature and pressure conditions. In some cases, fossils may be destroyed or altered by extreme heat, but melting is not a common outcome.
the fossils show massive change at one time (for instance the Grand Canyon; this massive change occurs usually from significant weather/environmental events) , and during the periods between the significant changes not much evolution (changes in genetic expression/genes) occurs.
Cyanobacteria fossils can be dated back to the Proterozoic Era.
oxygen
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Thylakoid membranes of chloroplasts resemble those of cyanobacteria because chloroplasts are believed to have evolved from endosymbiotic cyanobacteria. During evolution, the cyanobacteria that were engulfed by a host cell eventually became mutually beneficial, leading to the development of chloroplasts. The structural similarity between the thylakoid membranes of chloroplasts and cyanobacteria is a remnant of this evolutionary relationship.
Plesiosaurs and icthyosaurs were two unrelated groups of marine reptiles that lived during the Mesozoic. Plesiosaurs had long necks and short tails, or short necks and long tails, and they propelled themselves using their flippers. Icthyosaurs were reptiles that looked much like fish, with a long narrow snout, and a vertical tail fin. Both plesiosaurs and icthyosaurs ate marine animals.
fossils
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Fossils that are widespread geographically are commonly referred to as cosmopolitan fossils. These fossils are found in multiple locations around the world, indicating a broad distribution during the time period in which they were alive.
Fossils are nothing to do with weathering they are formed during the deposition of sediments before they become rocks.
They are called index fossils.
Index fossils are used to compare the relative ages of fossils. These are fossils that are known to have lived during a specific time period, helping to date the rock layers in which they are found. By identifying and comparing index fossils, scientists can determine the relative ages of different rock layers and fossils.
Marine creatures like sharks existed in the Jurassic. Marine reptiles like icthyosaurs, plesiosaurs, and thalattosuchians also existed. Thalattosuchians are fully marine reptiles.