The Pleistocene epoch was a time period of almost 2 million years of repeating glaciation around the globe. This epoch was known for its megafauna that roamed the Earth during the last great ice age. Although this was a time of mass extinction for species that could not adapt to the climate changes, many mammals and vertebrates that can be identified today were found during this time (Zimmermann, 2013). The Pleistocene epoch is an important foundation for understanding life that exists today, including carnivores, herbivores as well as the evolution of humans.
Fossil preservation has always been the most accurate way to determine what species lived during a specific time period. Through correlations and radiometric dating, time periods have become more accurate and being able to tell what lived during those times became possible. Although conditions have to be correct for fossilization, Pleistocene fossils are widespread and often well preserved. In the La Brea tar pits of present day Los Angeles, hundreds of thousands of preserved bones have been found that give a good idea of the animals that were present during this time. Many of the animals preserved are animals that can still be found today and would be found in the Los Angeles area if not for urbanization. Animals that were present during this time include camels, mammoths, and saber-toothed cats among others (Harris and Jefferson, 1985). Below is a picture of a saber-tooth fossil found in the La Brea tar pits.
The species that were present were not exclusive to North America, but lived all over the globe. During the Pleistocene, saber-tooth cats were present on all the continents as very fierce mammal carnivores that would hunt large herbivores such as mastodons. As th...
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...redators and were well established as creatures that could survive the harsh climate changes. There were also many flightless birds that didn’t do as well because of the competition for food and water due to glaciation and predators attacking them (Zimmerman, 2013).
The Pleistocene epoch is a well-known time period thanks to the glorification of now extinct megafauna as well as the proximity to our current epoch. Through the rapid climate changes and glaciation that occurred many times during this epoch, the fauna
could either survive through adaptation or die off due to an inability to adapt rapidly enough. All different types of animals, carnivorous and herbivorous mammals, birds, and reptiles, lived during the Pleistocene epoch and thanks to preservations such as the La Brea tar pits, we are able to observe and study the life forms of millions of years ago.
In this paper Martin is arguing that late quaternary or near time extinctions where caused by human activity or as he calls it “overkill”. Martin recognizes that there have been many forces that have triggered extinctions in the planet on the past but disagrees with the idea that near time extinctions where caused by some commonly believed causes like climate change, disease or nutrient shortage. He argues that the arrival of humans to different continents, islands and the subsequent excessive hunting, the introduction of diseases and other competitors and predators was the cause of extinction of a great number of species “As our species spread to various continents we wiped out their large
Fossil records from 12,000 years ago show the appearance of the Large Mammals followed by Paleoindian in Eastern North America. Another piece of the fossil record shows that the appearance of Paleoindian brought about the disappearance of the large mammals. Some people feel that, "there is evidence to suggest that rapacious hunting practice of the paleohunters in North and South America 12,000 years ago may have caused…The demise of the very animals they hunted" (Powell 1987). The evidence Powell suggests is that the extinction of a large mammal is usually followed by the appearance of humans in the fossil record. This coincidence is not only seen in the fossil records of North and South America but Europe and Asia as well. Powell shows that as human populations increased local extinctions of large mammals occurred. This was probably due to the fact that there were not many predators that could hunt the large mammals except man. For this reason it is also highly like likely that man and large mammals did not co-evolve which ultimately resulted in the extinction of large mammals.
The question of what caused the extinction of megafauna during the Late Pleistocene period is one that archaeologists have struggled to answer for decades, but why should it matter? Discovering with certainty the cause of megafaunal extinction would simultaneously prove or disprove any of the proposed implications of each existing theory regarding this massive extinction.
Man is responsible for the extinction of the North American megafauna (Donlan 2005, Rubenstein et al. 2006). Since our ancestors are responsible for the extinction, it’s our duty to fix what our ancestors have destroyed (Donlan 2005). Moreover, according to Donlan (2005) most megafauna species in Africa and Asia are endangered or under threat. Hence, relocating them to North American is a best way of conserving them because the country carries “Global conservation implications” and contrary to that Africa and Asia practice poor conservation strategies (Donlan 2005). He further argues that N...
There is evidence to suggest that Homo neanderthalensis and Homo sapiens had coexisted for approximately 35-40,000 years, (Fagan 2010) from around 60,000 years ago to 25,000 years ago when they finally went extinct (Gibbon 2001). Anthropologists are still uncertain what the cause of their extinction was. This paper will analyze three main theories of Neanderthal extinction. The first theory is the competition theory, which claims that the Homo sapiens and Neanderthals had to compete for resources, ultimately leading to their demise. The second theory I will discuss is the climate change theory, which claims that Homo sapiens lived while Neanderthals died because they were better adapted to the climate. The last theory I will discuss is the possible “extinction through absorption” theory which claims the Neanderthal interbred with the Homo sapiens and became one species. In this paper I will also be comparing the technologies, and diets of both species. In addition, I will look at the anatomic relation between the Neanderthals and Homo sapiens, how their body shape and size differed, and if this gave any advantage to one side or the other. My thesis for this paper will state that Homo sapiens and Homo neanderthalensis had co-existed but the disappearance of the Neanderthal in Eurasia is due to the appearance of the more culturally advanced and genetically superior Homo sapiens and the failure of the Neanderthal to adapt in an evolving climate.
The Woolly Mammoth saw periods of glaciation, when temperatures were reduced, and the Earth entered an Ice Age. They lived in dry northern ecosystems which they were well adapted to with their characteristic long shaggy coat. However, most of the time there were periods of snow. They are also associated with grassy plains which. Although the grass was not very nutritious, they grew in large enough amounts that it became part of their diet. They also fed on saplings of trees such as birch. Because of a grown Woolly Mammoth’s size and sheer strength, the Woolly Mammoth didn’t have many predators. Those who were preyed upon were juvenile wooly mammoths who were targeted by big cats like Homotheriums and, later, the early
Examining the Cretaceous-Paleogene Extinction Event Over 98% of all organisms that have lived on Earth are now extinct. A mass extinction event occurs when a large number of species die out within a small time frame (relative to the age of Earth). Mass extinctions are intensively studied for both cause and effect, as there is usually room for debate regarding catalysts that precede the extinction and the massive influx of new biological species that follows. There have been five major mass extinctions, dubbed the “Big Five,” that have wiped out at least 50% of the species living at those times. The most well-known mass extinction of the Big Five, with the decimation of every species of non-avian dinosaur, is the Cretaceous-Paleogene extinction event (K-Pg).
Changing seasons was to the advantages of mammals who were warm blooded over reptiles who couldn’t control their metabolic temperatures. Thus, many reptiles, such as lizards and crocodiles, did not evolve the way mammals did since they weren’t able to flourish as much as rodents and hoofed animals. Due to this climate change, it was crucial that animals evolve in order to develop the certain traits, characteristics, and skills to be able to survive and adapt to this new environment. When the forests began to cool, mammals evolved to possess the traits of being a scavenger and being short legged. As a result of the insect group expanding, it provided a more plentiful amount of food to the small sized mammals, which further increased their population. In account of the growth of the polar ice cap and it attaining more ocean water, sea levels dropped and connected certain areas of Asia and Europe together which had once been separate, which allowed species to travel from one area to the other since they were now connected and can explain how one species migrated from one continent to the other. However, many herbivores could not adapt to this
Earth has experienced many episodes of dramatic climate changes with different periods in earth history. There have been periods during which the entire planet has been covered in ice and at another time it has been scorchingly hot and dry. In this regards, earth has experienced at least three major periods of long- term frigid climate and ice ages interspersed with periods of warm climate. The last glacial period which current glaciers are the result of it, occurring during the last years of Pleistocene, from approximately 110,000 to 10,000 years age (Clayton, 1997). Indeed, glaciers present sensitive indicators of climate change and global warming and by estimating and monitoring the dynamic evolution of these ice masses, several aspect of climate change impact on environmental phenomena can be revealed.
The Smilodon, the most recent type of saber tooth cats, went extinct about 10,000 years ago, around the time when Pangea began separating and breaking up. Sabertooth Cats did not go extinct due to lack of prey. However, around 12,000 years ago (end of the late Pleistocene) sabertooth cats, american lions, wooly mammoths and other gigantic creatures considered the “megafauna” went extinct. A die-off called the Quaternary extinction. A popular theory for the extinction is that the changing in climate during the end of the last ice age, human activity, or a combination of both killed off most large
Earth has gone through five fully major extinctions before. We currently are in the process of Earth’s sixth mass extinction. This mass extinction is closely related in severity to the extinction of the dinosaurs. Earth’s extinctions are broken into three different areas. The first area was the large number of animals caught by hunter-gathers. The discovery of agriculture led to the second area of extinction, wildlife habitats. These wildlife habitats were destroyed due to humans starting to stay in one area.
Thousands of years ago, hunting may have been the cause of the extinction of the North American large land mammals. “Moving up into the 1940’s and 50’s some of today’s most prominent game animals were almost non-existent.”(Kerry G) Over-hunting will directly cause the decline in the particular animal’s species. This will effect everything around it, for example ...
Paleolithic age presents the era when key human adaptations evolved in response to a variety of environmental changes experienced at the time. This period of human evolution coincided with change within the surrounding of man. Such included cooling, drying and unpredictable climatic patterns over the time. This increased amount of variability in environmental conditions raised the level of uncertainty and instability in their respective terms of survival, necessitated the man to adopt new habits to increase adaptability to the new and changing surroundings. The evolved structures and behaviors led to specialization to enable coping with changing and unpredictable conditions.
Welsh, Jennifer. "Fossil Teeth Show Mammals Thrived Before Dinos Died." LiveScience. TechMedia Network, 14 Mar. 2012. Web. 14 Mar. 2014.
Perhaps it is too premature to explore an additional paleoecological implication, namely that the human that had settled in Australia from the land bridge were in competition with Thylacoleo carnifex for the resources of meat from the megafauna (Horton and Wright 1981). To date, there has not been any archeological discovery that has been found which from fossil record predicts that humans might have been killing and eating the megafauna and depleting the supply of food for Thylacoleo carnifex. From the fossil record, we can only describe how the animal could have lived and its diet. There is not yet enough evidence that proves that humans killed off the lions. However, like most of the megafauna that died off after the ice age, the Thylacoleo carnifex could not adapt well enough (Trivedi 2004).