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Geologic essays on the cambrian explosion
Geologic essays on the cambrian explosion
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A Review of Early Life: The Cambrian Period by Thom Holmes
Early Life: The Cambrian Period is a nonfiction book written by Thom Holmes and published in 2008. The book explores the Cambrian Period, an exciting time span in Earth’s history. During this time period the basis of all life originated. In his introduction Holmes sets the foundation for the book. Also, providing the readers with a general idea of the topics to be discussed. He states that Early Life: The Cambrian Period “draws from the latest research to tell the compelling story of Earth’s earliest organisms and their enormous importance to understanding other species of life that have evolved since”, giving readers a small insight to his commitment to thoroughly explain each step
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Holmes introduced James Hutton to his readers. He explains Hutton’s role by describing him as a scientist “whose Plutonist theory was one of the first to explain the interior composition of Earth, originated his theories about geological processes in the observation of natural forces that could be seen in the planet’s crust” (p.45). Holmes wrote that in the same year as Hutton’s death in 1797 Sir Charles Lyell, a British naturalist, was born and it was as though he “[picked] up where Hutton left off” (Holmes, 2008, p.47). Holmes goes on to explain how Lyell embraced Hutton’s ideas and used them as motivation for his own work (Holmes, 2008, p.47). In 1830 Lyell introduced his “simple guiding principle to explain the age of Earth: The present is the key to the past” (p. 47). Before Lyell’s theory was proposed it was commonly accepted in the science community that God created Earth, all life, and that it was merely 6,000 years old. The time scale for categorizing age is broken into intervals of descending size: eons, eras, and periods. According to Holmes (2008), “From the work of early geologists came two basic guidelines for examining layers of Earth: the principles of superposition and cross-cutting” (p. 48). Readers also learn about relative dating and absolute dating. Cross-cutting is the idea that an object is younger than anything it cuts across. Relative dating is when one layer of Earth is compared to a previously identified layer. This method is only accurate if the time line is within a few million years through. Absolute dating is when the age of a fossil is narrowed down to within a few
Herndon J. M, 2005, Current Science, Scientific Basis of Knowledge of Earth’s Composition, 88, 1034-1036)
The primordial Soup theory was discovered in 1920. According to the Russian scientist A.I. Oparin and English Geneticist J.B.S. Haldane life started in a warm pond/ocean in a process that took place 3.8 billion years ago. A combination of chemicals made fatty acids which made protein. In this process a molecule was born in the atmosphere. The molecule was energized with lightning and rain making “organic soup”. The first organisms would have to be simple heterotrophs in order to survive.
Charles Lyell Charles Lyell was a British lawyer and one of the smartest geologists known at his time. He was known as the author of the Principles of Geology, which helped popularize the theories and concepts of uniformitarianism. The Principles of Geology was the first book written by Lyell and explained the changes in the earth’s surface. He used the research and information in the book as his proof to determine that the earth was over 6,000 years old. The central argument in his book was “the present is the key to the past”, this meant that to find out what happened in the past you had to look at what was happening now.
Geologic development contributed to the Cambrian explosion. There was a supercontinent called Rodina that broke up to make continents. There was an ice age but the Earth continued to warm creating new life forms. There things called invertebrates that had no backbone. Life forms also had a hard outer shell to protect them. The trilobite is an arthropod that had a hard outer shell. In only 15 million years many different types of organisms evolved. Cambrian reefs made up of sponges flourished.
There are many ways to determine the authenticity of findings. Scientists need to use methods of dating organic material to determine when it lived and if it is authentic. It is important for anthropologists to study when an organism lived to see how they lived at that time. Sometimes people produce objects claimed to be real artifacts from a certain point in time for fame and for money. These fake artifacts produce false information and fool the public to believing these false claims. By using dating techniques, such as carbon dating, x-ray analysis, infrared analysis, and neutron activation, scientists can determine the authenticity of discovered artifacts.
Henry Thoreau, like Goethe before him, showed a lasting interest in science. (2) He belonged to the Boston Natural History Society from 1850 onwards, and read widely in the current scientific literature. Beyond this, Thoreau was intensely interested in the scientific puzzles suggested by his own rambles around Concord, Massachusetts. In the years following Walden’s publication he observed more systematically and tested his hypotheses more rigorously, and published one of the first scholarly discussions on forest succession. Some historians rate Thoreau as one of the founders of the modern science of ecology. (3)
...l between 40,000 and 80,000 years old Anthropologists date modern human fossils from the same area at between 92,000 and
regions of the earth can indicate which rock layer is older than the other. Trilobite fossils
Charles Lyell was born on November 14, 1797 at Forfarshire, Scotland. He was a Scottish lawyer, a geologist as well as a supporter of Uniformitarianism. He was the author of Principles of Geology. His theory was that earth must be very old and that throughout time the planet has undergone processes that change the shape the land. That includes erosion, earthquakes, glacial movements, volcanoes, and the decomposition of dead plants and animals.
In 1785 James Hutton could no longer credit what the biblical inscriptions were stating about how old the Earth was, so he decided to try to find out the history and what the true age of the Earth. This breakthrough took two men to complete and justify; uniformitarianism is a “theory that processes that occurred in the geological past are still at work today” (Larsen 2017 pg25). With evidence that Hutton collected, he came to the conclusion that the Earth’s surface changed due to natural forces which include the wind and rain. These changes have been recorded from the multiple layers of rock or the strata, that have been discovered on multiple mountains and canyons. From the different strata’s that Hutton gathered evidence from he was able to, “… calculate Earth’s age in the millions of years” (Larsen 2017 pg24). Although this discovery was forgotten about, it remained and became the work of Charles Lyell, he made it his mission to oversee and confirm that uniformitarianism was accurate. Lyell gathered evidence and personal observations that tested Hutton’s idea in order to prove that it is a theory, which he was able to accomplish.
There are several theories about how the Cambrian Explosion started. There were major changes in marine environments and chemistry from the late Precambrian into the Cambrian, and these also may have impacted the rise of mineralized skeletons among previously soft-bodied organisms. One theory as to what happened is that oxygen in the atmosphere, with the contribution of photosy...
Over the past century, the Burgess Shale has revealed important information about the development of earth’s history. The excavation of the Burgess Shale formation provided evidence for what was once just a theory in evolution. The taphonomic findings of the Burgess Shale have played a significant role in understanding the large diversity that resulted from the Cambrian explosion, advancing the study of evolutionary assemblages for Paleontologists worldwide.
4. The Paleozoic era began with the Cambrian period, around 540 million years ago. At this time, marine life became very abundant, and the first fish started to appear. Animal families became more diverse 480 million years ago, starting the Ordovician period, which ended
At the very dawning of the science of historical geology, James Hutton developed views on the earth’s geologic processes and ow they affect the planet unlike any other scientist before him. His idea that the planet’s processes revolved in a cyclic fashion were the cornerstone of uniformitarianism. Although he did not coin the phrase himself, an honor bestowed upon William Whewell, he did form the basic idea that the history of the earth can be explained by what is happening now.
Radiocarbon dating is used to tell how old something is. When some normal carbon gets hit by the rays of the sun it turns into carbon 14. Plants absorb this radioactive carbon in the form of carbon dioxide. Animals receive this carbon from eating the plants. When the organism is dead it loses the carbon 14. Scientists can tell how old something is based on the amount of carbon 14 in a dead object. Carbon dating is accurate if the amount of carbon 14 in the atmosphere has remained the same throughout time. The second is if carbon 14 has always decayed at the same