Animal gigantism was prevalent during the Carboniferous period of the Paleozoic era. Gigantism in flying insects occurred in abundance; however, arthropods, such as arthropleurids, also experienced gigantism. Arthropleurids existed during the Paleozoic era and were the largest land dwelling arthropods in the history of the Earth. 1m long millipedes are classified as arthropleurids. Amphibians such as the terrestrial labyrinthodont amphibians also became gigantic during the Carboniferous period. Large amphibians reached body lengths of up to 2m. However, these amphibians are limited by respiration through the skin, which is known to restrict maximum body size. The wingspan of a certain extinct dragon fly exceeded 70cm and the wingspan of late Paleozoic Paleodictyoptera was between .9-43cm.
There are a few hypotheses that have been aimed at explaining the gigantism during the Paleozoic era. Some are predatory defense and enhanced flight performance. However, the most plausible is the idea that the oxygen increase in the atmosphere caused the increase in body size. Increased oxygen partial pressure caused an increase in diffusive flux in the tracheal system. This led to the adaptation of the bodies of insects, amphibians, and arthropods to the new environment.
Carboniferous - is a major division of the geologic timescale that extends from the end of the Devonian period, about 359.2 Ma (million years ago), to the beginning of the Permian period, about 299.0 Ma (ICS 2004).
Geological records of atmospheric oxygen and carbon dioxide
Since plants have been able to survive on land by carbon dioxide fixation, also known as terrestrializaion, the earth’s atmosphere has undergone a ...
... middle of paper ...
...f terrestrial arthropods with diffusion-limited respiratory systems is consistent with the levels of atmospheric oxygen. (This can be seen in the charts included in the article) A second peak of insect gigantism appears to occur in the Cretaceous period when the atmosphere was also hyperoxic, or contained a high concentration of oxygen.
References
Orr, W. C. and Sohal, R. S. (1994). Extension of life-span by
overexpression of superoxide dismutase and catalase in Drosophila
melanogaster. Science 263, 1128–1130.
Tyler, R. H., Brar, H., Singh, M., Latorre, A., Graves, J. L.,
Mueller, L. D., Rose, M. R. and Ayala, F. J. (1993). The effect
of superoxide dismutase alleles on aging in Drosophila. Genetica
91, 143–149.
Withers, P.C. (1981). The effects of ambient air pressure on oxygen
consumption of resting and hovering honeybees. J. comp. Physiol.
..., Department of Zoology, Miami University, Oxford, OH, Available from Journal of Insect Physiology. (46 (2000) 655–661)Retrieved from http://www.units.muohio.edu/cryolab/publications/documents/IrwinLee00.pdf
Oxygen breathing lungs are a universal trait of class reptilia. As such, it would have been necessary for the Plesiosauroid - a marine reptile, to return to the ocean surface to inhale air. Oxygen expenditure in reptiles is proportional to strenuosity of locomotion (Frappell, Schultz & Christian, 2002). Therefore the Plesiosauroid must have held physiological traits that enabled the species to avoid oxygen deficit while hunting deep-sea dwelling prey. This essay will outline the hypothesised respiratory, circulatory, pulmonary and sensory attributes of the Plesiosauroid as they relate to diving. These hypotheses will be supported by investigating the physiological adaptations of the Plesiosaur’s biological analogues, and the prospect of similar adaptations in the former will be speculated upon.
Paleontologist L.B. Tarlo said that it was very difficult to ascertain the length of Liopleurodon. This was so because no complete skeleton was found. He then predicted from the skull, the skull was approximately one-seventh of the total length of the body. When we apply this ratio to the largest skull specimen of L. ferox, the total length of the body comes out to be a little more than 10 meters. The normal size from this calculation would be around 5-7 meters in length. The weight of it was estimated to be around between 75 to 150 tons. The more recent study and the finding of the complete skull of Liopleurodon. It showed the total size of the body was actually five times more the length of the skull. Thus, reducing the expected body size of it furthermore. The maximum size that a L. ferox could reach is just up to 6.4
Feder and Park present a list of traits that are used by paleoanthropologists to distinguish the appearance of skeletal features and characterize these changes over time. Th...
The Precambrian Era is when the Earth formed. Earth was barley a spec of dust in outer space and as time went by it gathered ice, rock and more dust particles. It eventually formed into a big rock flying around in space. The Earth was extremely hot and so when it rained the rain would evaporate in mid air or immediately after it hit the ground. But even though it evaporated these great rains cooled the Earth eventually building up water in lower areas creating oceans. The Earths atmosphere was water vapor, carbon dioxide, nitrogen and gases. After awhile oxygen level grew in the atmosphere. The earliest life forms were single celled organisms that lived in the oceans. These organisms used light energy to produce food called photosynthesis. These were called Prokaryotes and Eukaryotes. The evolution of multi celled organisms were Dramatic in change.
Mother earth has gone through a lot of changes throughout its four and a half billion-year existence. Earth has seen many different climates and many different species. Because of these changes geologists have broken earths history into different time periods. One such time period was the Pennsylvanian time period. The Pennsylvanian time period is a subdivision of the Carboniferous period. The Pennsylvanian period saw the introduction of many different species that are still present today along with a very different climate and different geographical features than are present today.
This breaking up of the mega continent of Pangaea allowed for more diversification of plant species and as the continents continued to break apart, plant life became even more diversified. As the continents shifted and moved from one area of the ocean to another the climates began to change drastically which allowed for plant and dinosaur species both to begin adapting to suit their new ecosystems. All the water that was produced by the split of Pangaea gave the previously hot and dry climate a more humid and drippy subtropical weather. Dry deserts took on a greener look. Before the Mesozoic Era, livings things were confined to only surviving in the oceans. It was not until the Jurassic Period that livings things evolved the capability of living on the land rather than just the ocean. Towards the beginning of the Jurassic, plant life evolved from Bryophytes, the low-growin...
Much of the debate over whether species should be separated into different groups arises from the morphological differences between individuals of the same species. For example, Australopithecus Afarensis fossils express high sexual dimorphism, which proposes two individual species (Reno et al., 2003). While Australopithecus Africanus, in comparison, shows more realistic size ratios between males and females suggesting one species (Lockwood, 1999). A study performed by Richmond and Jungers looked at the size variation in Australopithecus Afarensis compared to living hominoids to answer the following question: whether it is possible to see such high differences in size between genders of the same species or whether it makes more sense to divide the species into two (1995). In this study, a conclusion of two separate species for the Australopithecus Afarensis was made based on comparisons of fossils such as the humorous and femur with modern gorillas (Richmond & Jungers, 1995). This study compared the size of postcranial fossils. While most of the research has focused on making interpretations based on only cranial fossils, research by Harmon agrees that by looking at postcranial evidence we can gain better insight into the real variations between and within species (2009). Most research assumes high dimorphism wi...
The Permian Period occurred around 298 million years ago. It stretched from the Carboniferous Era to the Triassic. Sir Roderick Murchison in the early 1800’s noticed a differentiation among the overlay of the rock formation in the Ural Mountains in Russia. These rocks differed from the older Carboniferous rocks in Britain, and seemed younger than the Triassic rocks of Europe. Murchison named this differentiation after the prehistoric kingdom of Perm, thus the Permian Period.
The plants that we know today as terrestrial organisms were not always on land. The land plants of today can be linked back to aquatic organisms that existed millions of years ago. In fact, early fossil evidence shows that the earliest land plants could have arisen some 450 million years ago (Weng & Chappie 2010). Plants that used to reside strictly in water were able to adapt in ways that allowed them to move onto land. It is speculated the need for plants to move onto land was created by water drying up, causing plants to have less room and pushing them to move onto land. Although the exact cause of plant’s need to move to a terrestrial environment is unclear, it is known that plants had to undergo several adaptations to be able to live on land. These adaptations include: lignin, cellulose, suberin, and changes to plant’s surface, including the formation of a waxy cuticle.
According to scientists, one of the most extraordinary bursts of evolution ever known was the Cambrian Explosion. For most of the nearly 4 billion years that life has existed on Earth, evolution produced little beyond bacteria, plankton, and multi-celled algae. Then, about between 570 and 530 million years ago, another burst of diversification occurred. This stunning period is termed the "Cambrian explosion," taking the name of the geological age in which the earlier part occurred. A recent study revealed that life evolved during the Cambrian Period at a rate about five times faster than today. But it was certainly not as rapid as an explosion; the changes seems to have taken around 30 million years, and some stages took 5 to 10 million years. The Cambrian explosion was a period of time where life evolved into numerous multifaceted organisms that developed into the vertebrates and human life as we know today.
...deposition and blanket of sediment kept the organisms compressed with little exposure to oxygen for decay. If life was predominately terrestrial during the Cambrian, the organisms predictably would have been left untouched after death long enough to decay, preventing the fine preservation of many soft-bodied organisms. Fortunately enough, it was marine life that dominated the Cambrian (Scott, et al., 2000).
Sauropod dinosaurs were extremely big size. They varied in sizes depending on their age. Young Anchisaurids were 8 feet long while the giant ones like diplodocidis, titanosauris and branchiosaurids grew up to 100 feet (Levin, 2012). With such a huge size, they required large amounts of feed to maintain themselves. Drinking large volumes of water was also important.
Thesis: Forests provide the earth with a regulated climate, strong biodiversity, and good nutrient rich soil for plants to strive on.
Arthropods are in the kingdom Animalia which is in the subphylum Arthropoda. A species can be classified as an Arthropod if they have an exoskeleton, a coelom, and if they are mostly dioecious. An “ exoskeleton is an external skeleton made of chitin. [A] coelom is fluid filled cavity between organs and body wall” (Babin,2017). Examples of Arthropods are: spiders, ticks, millipedes, and centipedes. The objective of this experiment was to find Arthropods and test. Different habitats were established to see which will produce a greater amount of Arthropod. It was believed that the Arthropod diversity of a shaded area will be more that that of an area near a canal. The shaded area would have more arthropod diversity because more plants would be around it. Since there will be leaves and trees, plant diversity will be greater. Also, having “ plant diversity can positively affect arthropod{s}” ( Bennett and Gratton, 2013) because there will be more arthropods to utilize.