The Life Of A Paleontologist

We use fossils to compare and contrast how and organism has evolved over a long period of time and how it has adapted to new changes.

Fossils are the remains of either a plant or animal that lived in prehistoric times, the fossil is usually found preserved into rock. Fossils show us the steps of evolution that life has taken until today. When we trace fossil records back we can start to understand how species have progressed and what they appeared to look like. We can then compare (if the species still exists) what changes they have undertaken by using the fossils as a source. From that proof we can also compare the prehistoric biota with modern day biota and consider possible relatives. As well as being a window to the past, the remains of flora and fauna let us predict how Australian biota may evolve in future.

In the following space, explain the role of fossils in developing the Geologic column. Your explanation must be between 200 and 300 words.

Ichnology, the study of trace fossils, is the principal study in following and learning about trace fossils and how these fossil types indicate habitats. Ichnologists can use trace fossils, such as a track way and walking patterns of dinosaurs, to determine the specific area a dinosaur walked on, which can express a dinosaur species preferred habitat. By examining sedimentary layers and structures, ichnologists can use fossilized tracks to determine what specific habitat a species of dinosaur lived in. The use of uniformitarianism can be used to conclude what specific environment a dinosaur lived in through sedimentary structures. Ichnology uses tracks to determine what habitat a dinosaur inhabited by the pattern that a dinosaur walked in. With nests, Ichnologists can use information to determine what habitat a species of dinosaur lived in to ensure a safe environment for the eggs. Ichnologists can determine if a species of dinosaur stayed in a specific environment by studying the walking patterns of track ways and the indications of dinosaur nests. Ichnologists use track ways and nests to determine preferred habitats due to a plethora of trace fossils that a species of dinosaur can make in its

Paleontology or paleobiology is the study of plant, animal, and microorganism fossils found on the earth. Paleobotany focuses on algae, fungi, mosses, ferns, seed plants

From both the title of the chapter and the introduction by Dr. Shubin, this chapter begins with a focus on teeth. Because the function of teeth is to break down food before it enters the esophagus, the different shapes of teeth can represent many different things about the organism it belongs to including what type of eater it was (carnivore, herbivore, or omnivore). Teeth are the hardest tissue (not bone) in the human body and therefore fossilize well. As Dr. Shubin stated in chapter one, there must be many points that permit a fossil to make any kind of scientific conclusion. Obviously, the state of their presence is important, so the fact that teeth preserve well allows for them to be great specimens for analysis. Dr. Shubin and his team analyzed fossilized teeth in areas as different as Nova Scotia and the Arizona desert. Studying different fossils in these diverse regions allowed the team to see that mammalian and reptilian teeth are very different. For example, mammalian teeth differ from organism to organism to fit with the organisms need (Cheetahs that eat only meat will have different teeth than deer who are herbivores) and are replaced only once in the lifetime of the organism while reptilian teeth are usually sharp and are constantly replaced if damaged. These differences allowed scientists to characterize fossils as either a reptile or a mammal. Similar to Tiktaalik discussed in chapter one, the discovery of fossils that were part reptile and part mammal allowed the researchers to see that mammals evolved from reptiles, and further supported the theory of evolution. Further studies yielded even more

Archaeology is the most common way to learn about the existence of humans. Many cultures have left written records behind providing information about life for them. The records left behind often tells about wealth, religion, hierarchy, important dates, property ownership and etc. Those records are often written from one person prospective and may not be all true. Understanding the life of past cultures that have no written records is what make archeology important. Archeology gives a voice to the voiceless with the hope of discovering their story.

The first chapter of the book discusses the way we can use fossil records to study the biological world. Fossils are one of the major lines of evidence we use to understand ourselves. Surprisingly, we are able to discover them with a high amount of precision and predictability. In particular, field paleontologists have it easier than it has ever been before due to the current information age. The physical hunt for important fossils, however, is much like it has always been. Three factors limiting the number of useful fossil sites include rock age, type (whether or not it can preserve fossils), and number of exposed rocks. So, it takes a bit of luck to reliably find fossils. Thankfully, rock

Layers of soil are laid down on dead animals or plants embalming them. The minerals replace the organic matter creating the fossil.

(B) - The recognizable remains of a plant or animal are known as fossils. Unlike artifacts, fossils are not made by man and instead come from living things. Those who study fossils are known as paleontologists. The word “fossil” comes from the Latin word “fossilis”, which means “found by digging”.

In the science of paleontology, the history of life is studied. Paleontologists study fossils to learn the past ecologies, evolution, and the origins of humans. In order to understand the processes that have led to both the origination and destruction of organisms since life began, paleontologists incorporate both scientific knowledge and studies. Fossil findings are critically important for confirming predictions of evolution theory. Of the many discoveries that are made yearly to add depth to the understanding of evolution, an example is a recent discovery of a creature they named Tiktaalik. The Tiktaalik was uncovered to be a transitional animal between shallow-water fishes and limbed animals. The creature supports the idea that it emerged from both mammals and reptiles, suggesting that the two are related. These findings support prediction of evolution, contradicting the belief that God

The fossil record is evidence of evolution. Fossils are often fingerprints of evolution. They help scientists track how species evolved

: Fossils are the remains or traces of ancient organisms which have been preserved. For example, a fossil can exist as skeletal remains or even as a footprint. Such organisms are subjected to a slow rate of decaying since they have been rapidly buried under conditions that facilitate this. It is common for fossils to occur as hard-bodied organisms as these are more resistant to environmental influences. Fossils are usually found embedded in rock. The layers of rock are of different age and makeup. Hence fossils found in one layer would vary in characteristics from those found in another layer. They can be observed and analyzed through visual as well as radiometric means so that the age and morphology can be determined. These features indicate

When we think of history, we think of important people, places, cultures, events, and much more. The backbone of history rests on its chronology. It gives us the "when" of basic analysis. It gives us a frame of reference, the order of things. Before having an "absolute" way of determining dates, history was based in guesses and assumptions. Many attempts were made to organize the dates of the past. Some of these attempts were made by geologist. Geologist used the idea of "stratigraphic succession" (Renfrew, 1973) which is based on the "principle that when successive layers or strata are observed in position, the underlying ones are the earliest." (Pg. 23 Renfrew, 1973) By setting the layers in

These techniques led to the discovery of the boundary between the two eras. A single thin layer of clay found within predominantly limestone rocks established this. By comparing the marine life found in, above, and below the clay, the marine life, like the dinosaurs, had been terribly affected by the extinction event. The percentage of life in the upper layers was dramatically lower than that in the lower. This was far more compelling than what was suggested by dinosaur’s fossils.