# data[].attributes.body
is any preserved remains, impression, or trace of any once-living thing from a past geological age

# data[].attributes.body
Coprolites are classified as trace fossils as opposed to body fossils, as they give evidence for the animal's behaviour

# data[].attributes.body
is a type of trace fossil, a trackway made by an organism. Many fossil trackways were made by dinosaurs, early tetrapods, and other quadrupeds and bipeds on land

# data[].attributes.body
when minerals replace all or part of an organism. Water is full of dissolved minerals

# data[].attributes.body
Organisms buried in sediment may decay or dissolve away leaving a cavity or mold

# data[].attributes.body
a restatement of Charles Lyell's original principle of inclusions and components from his 1830 to 1833 multi-volume Principles of Geology, which states that, with sedimentary rocks,

# data[].attributes.body
is a principle of geology that states that the geologic feature which cutsanother is the younger of the two features

# data[].attributes.body
that layers of sediment initially extend laterally in all directions; in other words, they are laterally continuous

# data[].attributes.body
states that layers of sediment are originally deposited horizontally under the action of gravity

# data[].attributes.body
states that, for all linear systems, the net response caused by two or more stimuli is the sum of the responses that would have been caused by each stimulus individually

# data[].attributes.body
"the fundamental principle or doctrine that geologic processes and natural laws now operating to modify the Earth's crust have acted in the same regular manner