Copy of `USGS Paleontology - Glossary of Terms`
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USGS Paleontology - Glossary of Terms
Category: Earth and Environment > Paleontology
Date & country: 17/05/2009, USA Words: 108
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AcanthodiansA primitive group of Silurian to Permian jawed bony fishes, bearing bony spines in front of all but their caudal fins.
AlbianEuropean stage of the uppermost Lower Cretaceous, spanning the time between 107 and 95 million years ago.
AlgaePhotosynthetic, almost exclusively aquatic, nonvascular plants that range in size from simple unicellular forms to giant kelps several feet long. They have extremely varied life cycles and first appeared in the Precambrian.
AmmoniteA coiled, chambered fossil shell of a cephalopod mollusk of the extinct order Ammonoidea.
AmoebaA microscopic, one-celled animal consisting of a naked mass of protoplasm.
ApertureA relatively large opening on the last-formed chamber of a foraminiferal shell.
AptianEuropean stage of the Lower Cretaceous, spanning the time between 114 and 107 million years ago.
ArchaeanThe middle era of Precambrian time, spanning the period between 3.8 and 2.5 billion years ago. Life arose on Earth during the early Archaean, as indicated by the appearance of fossil bacteria in rocks thought to be about 3.5 billion years old. Its name means 'ancient.'
BarremianEuropean stage of the Lower Cretaceous, spanning the time between 118 and 114 million years ago.
BenthicUsed to describe aquatic organisms that are bottom dwelling.
BerriasianEuropean stage of the lowermost Lower Cretaceous, spanning the time between 135 and 131 million years ago.
BioluminescenceThe production of light by living organisms.
BiostratigraphyThe branch of geology concerned with the separation and differentiation of rock units by means of the study of the fossils they contain.
BivalveA mollusk having two shells hinged together, as the oyster, clam, or mussel; or any animal with two halves to its shell such as an ostracode or brachiopod.
Bony FishesFish of the class Osteichthyes, characterized by a skeleton composed of bone in addition to cartilage, gill covers, and an air bladder.
CaeciliansWormlike, almost blind, tropical amphibians of the order Apoda.
CalcareousOf, containing, or like calcite (calcium carbonate).
Calcareous NannofossilsFossil remains of calcareous nannoplankton.
Calcareous NannoplanktonProtists that normally produce coccoliths during some phase in their life cycle.
CalciteA common rock-forming mineral: CaCO
3. Calcite can be white, colorless, or pale shades of gray, yellow, and blue. It readily effervesces (bubbles) in hydrochloric acid and is the principal component of limestone.
CambrianThe earliest period of the Paleozoic era, spanning the time between 544 and 505 million years ago. It is named after Cambria, the Roman name for Wales, where rocks of this age were first studied.
CampanianEuropean stage of the Upper Cretaceous, spanning the time between 84 and 72 million years ago.
CarboniferousA period of time in the Paleozoic era that includes the Pennsylvanian and Mississippian periods and extended from 360 to 286 million years ago.
Cartilaginous FishesFish having a skeleton composed mostly of cartilage, as sharks and rays. Cartilage is gristle or a firm, elastic, flexible type of connective tissue.
CenomanianEuropean stage of the lowermost Upper Cretaceous, spanning the time between 95 and 91 million years ago.
CenozoicAn era of geologic time from the beginning of the Tertiary period (65 million years ago) to the present. Its name is from Greek and means 'new life.'
CoccolithsMicroscopic structures of varying shape and size that are made of calcite, are secreted by calcareous nannoplankton, and are found in marine deposits from the Triassic period to the Recent. Coccoliths range in size from one to thirty-five micrometers in size.
ConiacianEuropean stage of the Upper Cretaceous, spanning the time between 90 and 88 million years ago.
CoreA cylindrical section of rock, usually 2-4 inches in diameter and up to several feet long, that is the result of coring into the earth. Individual cores are brought to the surface for geologic examination and/or laboratory analysis.
CretaceousThe final period of the Mesozoic era, spanning the time between 145 and 65 million years ago. The name is derived from the Latin word for chalk ('creta') and was first applied to extensive deposits of this age that form white cliffs along the English Channel between Great Britain and France.
DevonianA period of the Paleozoic era, spanning the time between 410 and 360 million years ago. It is named after Devonshire, England, where rocks of this age were first studied.
DiagenesisAll chemical, physical, and biological modifications undergone by a sediment after its initial deposition.
DinocystA resting stage or reproductive stage in the life cycle of a dinoflagellate.
DinoflagellateSmall organisms with both plant-like and animal-like characteristics, usually classified as algae (plants). They take their name from their twirling motion and their whip-like flagella.
EcologyA branch of biology dealing with the relations between living plants and animals and their environment.
EcosystemA part of ecology consisting of the environment, its living parts, and the nonliving factors that affect it.
EoceneAn epoch of the lower Tertiary period, spanning the time between 55.5 and 33.7 million years ago. Its name is from the Greek words 'eos' (dawn) and 'ceno' (new).
FaunaAnimals of a given region or period of geologic time.
FloraPlants of a given region or period of geologic time.
ForaminiferProtozoans that belong to the subclass Sarcodina, order Foraminifera, that have a test of one to many chambers composed of secreted calcite or agglutinated particles.
FossilFossils are the recognizable remains, such as bones, shells, or leaves, or other evidence, such as tracks, burrows, or impressions, of past life on Earth.
FossilizationAll the processes that involve the burial of a plant or animal in sediment and the eventual preservation of all, part, or a trace of it.
GeochemistryThe science that deals with chemical changes in and composition of the earth's crust.
Geologic TimeThe period of time extending from the formation of the earth to the present.
Geologic Time ScaleAn arbitrary chronologic sequence of geologic events, used as a measure of the age of any part of geologic time, usually presented in the form of a chart showing the names of the various rock-stratigraphic, time-stratigraphic, or geologic-time units.
GeologyThe study of the planet Earth - the materials of which it is made, the processes that act on these materials, the products formed, and the history of the planet and its life forms since its origin
HadeanThe earliest subdivision of the Precambrian, spanning the time between the formation of the Earth, about 4.5 billion years ago, and the start of the Archaean era, 3.8 billion years ago. This interval predates the period of true geologic time since no rocks of this age are known on Earth, with the exception of a few meteorites.
HauterivianEuropean stage of the Lower Cretaceous, spanning the time between 122 and 118 million years ago.
HoloceneAn epoch of the Quaternary period, spanning the time from the end of the Pleistocene (8,000 years ago) to the present. It is named after the Greek words 'holos' (entire) and 'ceno' (new).
HydrogeologyThe science that deals with subsurface waters and geologic aspects of surface waters.
Isotopic DatingRadiometric dating; all methods of age determination based on nuclear decay of naturally occurring radioactive isotopes. Age in years for geologic materials are calculated by measuring the presence of a short-life radioactive element, e.g. carbon-14, or by measuring the presence of a long-life radioactive element plus its decay product, e.g. potass...
JurassicThe middle period of the Mesozoic era, spanning the time between 213 and 145 million years ago. It is named after the Jura Mountains between France and Switzerland, where rocks of this age were first studied.
Lithologic UnitLithostratigraphic unit; a body of rock that is consistently dominated by a certain lithology or similar color, mineralogic composition, and grain size. It may be igneous, sedimentary, or metamorphic and may or may not be consolidated.
MaastrichtianEuropean stage of the Upper Cretaceous, spanning the time between 72 and 66 million years ago.
MacrofossilA fossil that is large enough to be studied without a microscope.
MesozoicAn era of geologic time between the Paleozoic and the Cenozoic, spanning the time between 248 and 65 million years ago. The word Mesozoic is from Greek and means 'middle life.'
MicrofossilA fossil so small that it must be studied with a microscope.
MicrometerA unit of measure. There are one million micrometers in one meter.
MioceneA epoch of the upper Tertiary period, spanning the time between 23.8 and 5.3 million years ago. It is named after the Greek words 'meion' (less) and 'ceno' (new).
MississippianA period of the Paleozoic era, spanning the time between 360 and 325 million years ago. It is named after the Mississippi River valley, which contains good exposures of rocks of this age.
MorphologyThe study of form and structure of animals and plants and their fossil remains.
NektonicUsed to describe aquatic organisms that swim.
NotochordA rodlike cord of cells in lower chordates that forms the main lengthwise support structure of the body.
OligoceneAn epoch of the early Tertiary period, spanning the time between 33.7 and 23.8 million years ago. It is named after the Greek words 'oligos' (little, few) and 'ceno' (new).
OrdovicianThe second earliest period of the Paleozoic era, spanning the time between 505 and 440 million years ago. It is named after a Celtic tribe called the Ordovices.
OstracodermsPrimitive jawless fishes, covered by bony armor, that lived in the Cambrian through Devonian periods.
PaleobathymetryThe study of ocean depths and topography of the ocean floor in the geologic past.
PaleobiogeographyThe branch of paleontology that deals with the geographic distribution of plants and animals in past geologic time, especially with regard to ecology, climate, and evolution.
PaleoceanographyThe study of oceans in the geologic past, including its physical, chemical, biologic, and geologic aspects.
PaleoceneEarliest epoch of the Tertiary period, spanning the time between 65 and 55.5 million years ago. It is named after the Greek words 'palaois' (old) and 'ceno' (new).
PaleoclimateThe climate of a given period of time in the geologic past.
PaleoecologyThe study of the relationships between ancient plants and animals and their environments.
PaleoenvironmentEnvironment in the geologic past.
PaleontologistScientists who study fossils.
PaleontologyThe study of life in past geologic time.
PaleozoicAn era of geologic time, from the end of the Precambrian to the beginning of the Mesozoic, spanning the time between 544 and 248 million years ago. The word Paleozoic is from Greek and means 'old life.'
PelagicReferring to open water marine habitats free of direct influence of the shore or ocean bottom. Pelagic organisms are generally free-swimming (nektonic) or floating (planktonic).
PennsylvanianA period of the Paleozoic era, spanning the time between 325 and 286 million years ago. It is named after the state of Pennsylvania where rocks of this age are widespread.
PermianThe final period of the Paleozoic era, spanning the time between 286 and 248 million years ago. It is named after the province of Perm, Russia, where rocks of this age were first studied.
PhanerozoicThe period of time, also known as an eon, between the end of the Precambrian and today, The Phanerozoic begins with the start of the Cambrian period, 544 million years ago. It encompasses the period of abundant, complex life on the Earth.
PlacodermsA peculiar group of primitive armored jawed fish, found almost exclusively in rocks from the Devonian Period.
PlanktonAquatic organisms that drift, or swim weakly.
PlanktonicUsed to describe aquatic organisms that float.
PleistoceneAn epoch of the Quaternary period, spanning the time between 1.8 million years ago and the beginning of the Holocene at 8,000 years ago. It is named after the Greek words 'pleistos' (most) and 'ceno' (new).
PlioceneFinal epoch of the Tertiary period, spanning the time between 5.3 and 1.8 million years ago. It is named after the Greek words 'pleion' (more) and 'ceno' (new).
PrecambrianAll geologic time before the beginning of the Paleozoic era. This includes about 90% of all geologic time and spans the time from the beginning of the earth, about 4.5 billion years ago, to 544 million years ago. Its name means 'before Cambrian.'
ProterozoicThe final era of the Precambrian, spanning the time between 2.5 billion and 544 million years ago. Fossils of both primitive single celled and more advanced multicellular organisms begin to appear in abundance in rocks from this era. Its name means 'early life.'
ProtistAn organism that belongs to the kingdom Protista, which includes forms with both plant and animal affinities, i.e., protozoans, bacteria, and some algae, fungi, and viruses.
ProtozoanA member of the phylum Protozoa or animals consisting of one cell or a colony of like or similar cells.
PseudopodiaTemporary protrusions of the protoplasm of a protozoan, which serve for locomotion or grasping.
QuaternaryThe second period of the Cenozoic era, spanning the time between 1.8 million years ago and the present. It contains two epochs: the Pleistocene and the Holocene. It is named after the Latin word 'quatern' (four at a time).
RhizopodA protozoan of the class Rhizopoda that has pseudopodia.
RudistAn extinct bivalve mollusk from the Jurassic and Cretaceous that had two different sized and shaped shells; they usually were attached to the substrate and were either solitary or in reeflike masses.
SantonianEuropean stage of the Upper Cretaceous, spanning the time between 88 and 84 million years ago.
Scanning Electron Microscope(SEM) A microscope in which a finely focused beam of electrons is scanned across a specimen, and the electron intensity variations are used to construct an image of the specimen. This type of microscope is ideal for magnifications from 200 to 35,000.
SedimentSolid unconsolidated rock and mineral fragments that come from the weathering of rocks and are transported by water, air, or ice and form layers on the Earth's surface. Sediments can also result from chemical precipitation or secretion by organisms.
Sedimentary RockA rock that is the result of consolidation of sediments.
SilurianA period of the Paleozoic, spanning the time between 440 and 410 million years ago. It is named after a Celtic tribe called the Silures.
StratigraphyThe branch of geology concerned with the formation, composition, ordering in time, and arrangement in space of sedimentary rocks.
SubtropicalBordering on the tropics or nearly tropical.