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Paleozoology

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excess of a small fossil—such as teeth—could exaggerate quantity of the species. There was also an amount of confusion as to whether bone fragments should be assembled and counted as one bone or tallied individually. Stock and Howard then devised the Minimum Number of Individuals (MNI), which estimated the minimum number of animals needed to produce the fossils recorded. For example, if five scapulae from a species were found, it might be difficult to determine whether some of them were paired right and left on one individual or whether each came from a different individual, which could alter census, but it could be said that there must be at least three individuals to produce five scapulae. Three would thus be the MNI. In rare cases where enough of a collection of fossils can be assembled into individuals as to provide an accurate number of individuals, the unit used is Actual Number of Individuals, or ANI.
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might have been harvested by prehistoric hunters. For example, a male Wapiti has an average weight of 400 kg, and in a particular study, the MNI of Wapiti was found to be 10. This would create a biomass of 4,000 kg. If the amount of edible meat is estimated at 50 percent, this would result in a meat weight of 2,000 kg. The biggest problem with this method is the debate over "percent of usable meat." Different views on which parts of a species are edible and which are not as well as whether or not primitive butchers would have been able to access and prepare different parts have led to controversy.
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population of a species may have weighed. Problems with this measurement include the difference in weight between youngsters and adults, seasonal weight changes due to diet and hibernation, and the difficulty of accurately estimating the weight of a creature with only a skeletal reference. It is also difficult to determine exact age of fossilized matter within a year or a decade, so a biomass might be grossly exaggerated or under exaggerated if the estimated time frame in which the fossils were alive is incorrect.
60: 1739: 31: 808:, writes that paleozoological research can provide data such as extinction rates and causes and "benchmark" peaks and drops in population which can be used to predict future patterns and to design maximally effective methods of controlling these patterns. In addition, paleozoological data can be used to compare current to former population and distribution of a species. 751:
Vertebrate paleozoology refers to the use of morphological, temporal, and stratigraphic data to map vertebrate history in evolutionary theory. Vertebrates are classified as a subphylum of Chordata, a phylum used to classify species adhering to a rod-shaped, flexible body type called a notochord. They
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Another unit commonly used in quantitative paleozoology is biomass. Biomass is defined as the amount of tissue in an area or from a species. It is calculated by estimating an average weight based on similar modern species and multiplying it by the MNI. This yields an estimate of how much the entire
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devised special units for quantitative paleozoology and quantitative paleontology. The first unit used, Number of Identified Species (NISP), specified exact quantity of fossils from a specific species recorded. Stock and Howard determined this unit to be problematic for quantitative purposes as an
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Quantitative paleozoology is a process of taking a census of fossil types rather than inventory. They differ in that inventory refers to a detailed log of individual fossils, whereas census attempts to group individual fossils to tally the total number of a species. This information can be used to
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A similar measurement to biomass is meat weight. To determine meat weight, MNI is multiplied by the amount of meat an individual is thought to have provided, then multiplied by the percentage of that meat thought to be edible. This gives an estimate of "pounds of usable meat" per individual which
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Evolutionary origins of vertebrates as well as the phylum Chordata have not been scientifically determined. Many believe vertebrates diverged from a common ancestor of chordates and echinoderms. This belief is well supported by the prehistoric marine creature Amphioxus. Amphioxus does not possess
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Classes of vertebrates listed in chronological order from oldest to most recent include heterostracans, osteostracans, coelolepid agnathans, acanthodians, osteichthyan fishes, chondrichthyan fishes, amphibians, reptiles, mammals, and birds. All vertebrates are studied under standard evolutionary
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bone, making it an invertebrate, but it has common features with vertebrates including a segmented body and a notochord. This could imply that Amphioxus is a transitional form between an early chordate, echinoderm or common ancestor, and vertebrates.
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differ from other phyla in that other phyla may have cartilage or cartilage-like tissues forming a sort of skeleton, but only vertebrates possess what we define as bone.
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groups. This is because hard organic parts, such as bones, teeth, and shells resist decay, and are the most commonly preserved and found animal fossils. Exclusively
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generalizations of behavior and life process, although there is controversy over whether population can be accurately estimated from limited fossil resources.
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determine which species were most dominant and which had the largest population at a time period or in a geological region.
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R. Lee Lyman, Professor and Chair Department of Anthropology at the
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era onwards, although they do not become common until the Late
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In the early 1930s, paleontologists Chester Stock and
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Paleozoological data is used in research concerning
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New York: Wiley-Interscience. 903:covers the subphylum Vertebrata 853:—easily visible fossil evidence 120:List of human evolution fossils 1026: 13: 1: 917: 865:—microscopic fossil evidence 596:"animal"), is the branch of 115:List of transitional fossils 7: 1081: 811: 231:Mammalian auditory ossicles 10: 1795: 982:Olson, Everett C. (1971). 39:, fish fossil from Wyoming 1769:Subfields of paleontology 1733: 1707: 1644: 1619: 1527: 1518: 1445: 1395: 1382: 1308: 1102: 1089: 1006:Evolutionary Anthropology 960:Quantitative Paleozoology 876:—biology and paleontology 845:Invertebrate paleontology 764:Quantitative paleozoology 739:—are consequently rarely 627:in the reconstruction of 428:Invertebrate paleontology 377:Biological classification 357:Introduction to evolution 258:Evolution of various taxa 847:covers most animal phyla 412:Branches of paleontology 400:Timeline of paleontology 1170:Biological anthropology 984:Vertebrate Paleozoology 901:Vertebrate paleontology 747:Vertebrate paleozoology 668:Perhaps the best known 518:Vertebrate paleontology 395:History of paleontology 389:History of paleontology 110:Lagerstätte fossil beds 958:Lyman, R. Lee (2008). 820:, taxonomic kingdom of 806:University of Missouri 438:Molecular paleontology 40: 1699:Alfred Russel Wallace 1609:Water vascular system 836:—a.k.a. guide fossils 178:Timeline of evolution 33: 1774:Subfields of zoology 1560:Cellular respiration 795:conservation biology 789:Conservation biology 195:Organs and processes 105:List of fossil sites 1725:Timeline of zoology 1654:Karl Ernst von Baer 1555:Respiratory pigment 1430:Mineralized tissues 721:soft-bodied animals 529:Paleontology Portal 183:Transitional fossil 153:Geologic time scale 46:Part of a series on 1540:Respiratory system 1528:General physiology 1425:Connective tissues 1019:10.1002/evan.20083 636:ancient ecosystems 572:, also spelled as 90:Fossil preparation 41: 1751: 1750: 1694:Jakob von Uexküll 1640: 1639: 1627:Insect physiology 1520:Animal physiology 1514: 1513: 1506:Insect morphology 1437:Molecular anatomy 1410:Epithelial tissue 1388:Animal morphology 869:Micropaleontology 774:Hildegarde Howard 645:are found 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Index

Palaeozoology

Priscacara liops
Paleontology

Fossilization
Trace fossil
Microfossil
Fossil preparation
Index fossil
List of fossils
List of fossil sites
Lagerstätte fossil beds
List of transitional fossils
List of human evolution fossils
Biogeography
Extinction event
Geochronology
Geologic time scale
Geologic record
History of life
Origin of life
Paleoclimatology
Timeline of evolution
Transitional fossil
Avian flight
Cells
Multicells
Eyes
Flagella

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