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25 Cards in this Set

  • Front
  • Back

fossilization

to convert into a fossil; replace organic with mineral substances in the remains of an organism

Carbonization

convert into carbon

Petrifaction

the process by which organic matter exposed to minerals over a long period is turned into a stony substance.


Tectonic activity

when two tectonic plates crush together or drift or slide against eachother

Microfossil

A fossil only visible with a microscope

Gastroliths

a small stone swallowed by a bird, reptile, or fish, to aid digestion in the gizzard.

Coprolites

Fossilized dung

Transitional fossil

any fossilized remains of a life form that exhibits traits common to both an ancestral group and its derived descendant group.

Archaeopteryx

Oldest fossil bird

Amber

hard translucent fossilized resin produced by extinct coniferous trees of the Tertiary period, typically yellowish in color.

Replacement Fossilization

Most organisms become fossils when they're changed through various other means. ... In another fossilization process, called replacement, the minerals in groundwater replace the minerals that make up the bodily remains after the water completely dissolves the original hard parts of the organism.

Zoolite

Zeolites are microporous, aluminosilicate minerals commonly used as commercial adsorbents and catalysts. ... Based on this, he called the material zeolite, from the Greek ζέω (zéō), meaning "to boil" and λίθος (líthos), meaning "stone". Zeolites occur naturally but are also produced industrially on a large scale.

Scolecodont

A scolecodont is the jaw of a polychaete annelid, a common type of fossil-producing segmented worm useful in invertebrate paleontology. Scolecodonts are common and diverse microfossils, which range from the Cambrian period (around half a billion years ago at the start of the Paleozoic era) to the present.

Cast

shaped

concentric

of or denoting circles, arcs, or other shapes that share the same center, the larger often completely surrounding the smaller.

paleontology

the branch of science concerned with fossil animals and plants.

Igneous Inclusions

A xenolith (Ancient Greek: "foreign rock") is a rock fragment which becomes enveloped in a larger rock during the latter's development and solidification. In geology, the term xenolith is almost exclusively used to describe inclusions in igneous rock during magma emplacement and eruption.

Lithification

Lithification (from the Ancient Greek word lithos meaning 'rock' and the Latin-derived suffix -ific) is the process in which sediments compact under pressure, expel connate fluids, and gradually become solid rock. Essentially, lithification is a process of porosity destruction through compaction and cementation

Remineralization

In biogeochemistry, remineralisation (UK, US Spelling: remineralization) refers to the breakdown or transformation of organic matter (those molecules derived from a biological source) into its simplest inorganic forms

Ichnofossil

A trace fossil, also called an ichnofossil (pronunciation: /ˈɪknoʊfɒsᵻl/; Greek: ιχνος ikhnos "trace, track"), is a geological record of biological activity.

Mold

a hollow container used to give shape to molten or hot liquid material (such as wax or metal) when it cools and hardens.

Boring & Burrows

to create a hole using a tool of some sort

Transitional fossil

A transitional fossil is any fossilized remains of a life form that exhibits traits common to both an ancestral group and its derived descendant group.

fossil beds

The hardened remains or imprint of a plant or animal that lived long ago. Fossils are often found in layers of sedimentary rock and along the beds of rivers that flow through them. ... Petroleum, coal, and natural gas, which are derived from the accumulated remains of ancient plants and animals, are called fossil fuels.

organisms

an individual animal, plant, or single-celled life form.