Prelim 1 Flashcards
(140 cards)
Fossil
remains, traces, or impressions of once living organisms ie. skeleton, impression, cast, trace, or coprolite (poop); most found in sedimentary rocks
Forces that impede fossilization
natural processes such as predators/scavengers, bacterial decay (soft tissue), dissolution in water (soft and hard tissue), or physical disturbance (wave action, wind)
Conditions that promote fossilization
rapid burial, protection from physical disturbance ie. quiet, deep water, anaerobic conditions (prevent bacterial decay)
Sedimentary rock formation
formed from the deposition of sediment falling to the bottom of a body of water
What gets preserved in fossils of animals
hard parts ie. teeth, bone, chitinous exoskeleton, or calcium carbonate shells
What gets preserved in fossils of plants
seeds, pollen, leaves, wood, rarely flowers (fragile petals)
What gets preserved in fossils of microbes
bacteria, microbial mats ie. stromatalites are formed from biofilms of cyanobacteria that trap sediment which eventually harden and form layers
Types of preservation
original remains (skeletal body, other body elements), permineralization/petrification, trace fossils, impression fossils, casts and molds
Permineralization/petrification
process where minerals are deposited in tiny holes within bones, or wood and over time completely replacing the original organism and all that remains is a stone structure
Impression fossils
made up of carbonaceous film imprint of an organism
Lagerstatten
German word that means “storage place”, place where fossils are exceptionally preserved (numerous and well preserved)
Burgess Shale
a famous Lagerstatten from the Cambrian which has yielded many of the organisms that contribute to our understanding of the Cambrian explosion
How do we know the age of a fossil?
relative and absolute dating
Geological chronology
the science of dating geological layers and fossils
4 principles relative dating is based on
superposition, original horizontality, lateral continuity, and cross-cutting
Principle of superposition
geological layers are formed by laying one on top of the other so that the youngest layer is on top
Principle of original horizontality
layers are first deposited horizontally and then they may be deformed later such as from the movement of continental plates
Principle of lateral continuity
layers continue laterally over distances; each layer is deposited at the same so that even if erosion has removed some of the layer, the layer is still the same layer after the gap
Principle of cross-cutting
if there is a cross-cutting layer or intrusion in rock layers, the intrusion is always younger than any of the layers it is cross-cutting
Index fossils
fossil organisms that are only found in a particular rock layer and are also geographically widespread so that the layers can be stratiagraphically correlated with each other in different locations according to the principle of lateral continuity
How was geological time scale (GTS) created?
by correlating layers based on index fossils; derived from the spatial distribution of rocks and the vertical sequence of rocks and contained fossils
How/when did absolute dating become possible
with the discovery of radioactivity in the late 19th century
Absolute dating
done by examining the radioactive decay of unstable isotopes
Radioactive decay
decay of a parent isotope gives rise to a stable daughter isotope at some characteristic rate of decay