“fossil”的概念、定义、翻译、参考文献-科学参考

fossil

Biology

The remains or traces of any organism that lived in the geological past. In general only the hard parts of organisms become fossilized (e.g. bones, teeth, shells, and wood) but under certain circumstances the entire organism is preserved. For example, virtually unaltered fossils of extinct mammals, such as the woolly mammoth and woolly rhinoceros, have been found preserved in ice in the Arctic. Small organisms or parts of organisms (e.g. insects, leaves, flowers) have been preserved in amber.
In the majority of fossils the organism has been turned to stone—a process known as petrification. This may take one of three forms. In permineralization, solutions originating underground fill the microscopic cavities in the organism. Minerals in these solutions (e.g. silica or calcite) may actually replace the original material of the organism so that even microscopic structures may be preserved; this process is known as replacement (or mineralization). A third form of petrification—carbonization (or distillation)—occurs in certain soft tissues that are composed chiefly of compounds of carbon, hydrogen, and oxygen (e.g. cellulose). After the organism has been buried, and in the absence of oxygen, carbon dioxide and water are liberated until only free carbon remains. This forms a black carbon film in the rock outlining the original organism. Moulds are formed when the original fossil is dissolved away leaving a mould of its outline in the solid rock. The deposition of mineral matter from underground solutions in a mould forms a cast. Palaeontologists often produce casts from moulds using such substances as dental wax. Moulds of thin organisms (e.g. leaves) are commonly known as imprints. Trace fossils are the fossilized remnants of the evidence of animal life, such as tracks, trails, footprints, burrows, and coprolites (fossilized faeces).
The ideal conditions for the formation of fossils occur in areas of rapid sedimentation, especially those parts of the seabed that lie below the zone of wave disturbance. See also chemical fossil; index fossil; microfossil; molecular fossil; taphonomy.

Geology and Earth Sciences

1. Generally, anything ancient, especially if it is discovered buried below ground (e.g. fossil fuel, fossil soil).
2. The remains of a once-living organism. Formerly, only the preserved remains of an organism that lived prior to the end of the last glacial period was called a fossil, i.e. fossils were older than 10 000 years, and remains younger than 10 000 years were called subfossils. That limitation has now been abandoned and any ancient remains of a living organism can be called a fossil, regardless of its age. The term includes skeletons, tracks, impressions, trails, borings, and casts. Fossils are usually found in consolidated rock, but not always (e.g. woolly mammoths living 20 000 years ago were recovered from the frozen tundra of Siberia). In its original sense, fossil meant anything dug up from the earth, including ores, precious stones, etc. The modern use of the word dates from the late 17th century. See also living fossil; trace fossil.

单词	fossil
释义	fossil Biology The remains or traces of any organism that lived in the geological past. In general only the hard parts of organisms become fossilized (e.g. bones, teeth, shells, and wood) but under certain circumstances the entire organism is preserved. For example, virtually unaltered fossils of extinct mammals, such as the woolly mammoth and woolly rhinoceros, have been found preserved in ice in the Arctic. Small organisms or parts of organisms (e.g. insects, leaves, flowers) have been preserved in amber. In the majority of fossils the organism has been turned to stone—a process known as petrification. This may take one of three forms. In permineralization, solutions originating underground fill the microscopic cavities in the organism. Minerals in these solutions (e.g. silica or calcite) may actually replace the original material of the organism so that even microscopic structures may be preserved; this process is known as replacement (or mineralization). A third form of petrification—carbonization (or distillation)—occurs in certain soft tissues that are composed chiefly of compounds of carbon, hydrogen, and oxygen (e.g. cellulose). After the organism has been buried, and in the absence of oxygen, carbon dioxide and water are liberated until only free carbon remains. This forms a black carbon film in the rock outlining the original organism. Moulds are formed when the original fossil is dissolved away leaving a mould of its outline in the solid rock. The deposition of mineral matter from underground solutions in a mould forms a cast. Palaeontologists often produce casts from moulds using such substances as dental wax. Moulds of thin organisms (e.g. leaves) are commonly known as imprints. Trace fossils are the fossilized remnants of the evidence of animal life, such as tracks, trails, footprints, burrows, and coprolites (fossilized faeces). The ideal conditions for the formation of fossils occur in areas of rapid sedimentation, especially those parts of the seabed that lie below the zone of wave disturbance. See also chemical fossil; index fossil; microfossil; molecular fossil; taphonomy. Geology and Earth Sciences 1. Generally, anything ancient, especially if it is discovered buried below ground (e.g. fossil fuel, fossil soil). 2. The remains of a once-living organism. Formerly, only the preserved remains of an organism that lived prior to the end of the last glacial period was called a fossil, i.e. fossils were older than 10 000 years, and remains younger than 10 000 years were called subfossils. That limitation has now been abandoned and any ancient remains of a living organism can be called a fossil, regardless of its age. The term includes skeletons, tracks, impressions, trails, borings, and casts. Fossils are usually found in consolidated rock, but not always (e.g. woolly mammoths living 20 000 years ago were recovered from the frozen tundra of Siberia). In its original sense, fossil meant anything dug up from the earth, including ores, precious stones, etc. The modern use of the word dates from the late 17th century. See also living fossil; trace fossil.
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