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Tier II: High frequency words used across content areas. Key to understanding directions & relationships, and for making inferences.
Tier III: Low frequency, domain specific terms.
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Make connections to prior knowledge. This is where we build from.
A fossil is physical evidence of former life, from before recorded human history.
How do fossils form?
Adapted from Discoveringfossils.co.uk, by Roy Shepherd
Fossilization is the process of preserving the remains of organisms.
It happens under these conditions:
* rapid, permanent burial – this protects the specimen from being disturbed by other organisms or the weather.
* Low oxygen – therefore most bacteria and insects won’t live here, so they won’t scavenge the dead organism.
* sediment builds up over it. So it remains buried.
* Stable environment. Very little, or no, heat or compression. (Otherwise the fossil could be destroyed.)
This usually occurs beneath water.
Most of the Earth, about 70%, is under water.
Even fossils from land, including dinosaur bones and organisms preserved within amber (fossilized tree resin) were ultimately preserved in sediments deposited beneath water i.e. in wetlands, lakes, rivers, estuaries or swept out to sea.
Stages of fossilization
Adapted from Discoveringfossils.co.uk, by Roy Shepherd
Death – This fish died. Soon after death its body became water-logged and sank to the seafloor.
More often than not the carcass would be pulled apart and scattered by scavenging crustaceans and other fish.
However on this occasion the absence of any large scavengers leaves the fish relatively undisturbed.
After several weeks the fish is partially decomposed. Despite the calm conditions on the seafloor, several thousand meters into the bedrock pressure is building along an active geological fault.
Suddenly the stressed rock slips, sending shockwaves to the rock above and causing the sediment nearby to mobilise. The mobile sediment travels across the seafloor burying the fish in the process, in what is often termed a rapid burial event.
Once entombed beneath the sediment the remaining flesh and soft tissue are broken down by bacteria, leaving just the skeleton in the position of burial.
Rapid burial is a common component for optimal fossilisation, as prolonged exposure would otherwise increase the likelihood of disturbance from scavengers and/or currents. Burial may also occur quickly if a high volume of sediment is deposited in the area following a period of heavy rain that delivers sediment from major rivers (for example).
Sediment accumulation and permineralisation
Over time the skeleton is gradually buried deeper by accumulating sediment. Slowly the weight of the sediment compacts the underlying areas, pressing the grains together, driving excess water out, and depositing minerals in the pores, and ultimately turning the soft sediment to hard rock – a process known as lithification.
As this process takes place, minerals contained within the waters-saturated sediment replace the original minerals in the skeleton and fill any voids formed as parts of the skeleton dissolve. The process of mineral replacement is known as per-mineralisation and results in a re-mineralised copy of the original skeleton.
Left: Several months pass and all that remains of the buried fish is its skeleton.
Right: As times passes more sediment accumulates above the fish and the skeleton is gradually compressed and permineralised.
Uplift and exposure
Many millions of years pass and the rock remains buried deep within the bedrock; however tectonic forces associated with the collision between neighbouring continental plates have begun to buckle and uplift the bedrock, raising it above sea level and exposing it to erosion. Gradually, the exposed rock is stripped away, until eventually the top of the fish’s skull is visible at the surface.
Left: Over time the rock is distorted and uplifted by geological forces associated with continental movement, raising it above sea level.
Right: The uplifted rock is exposed to weathering and gradually erodes away, eventually exposing the tip of the fish’s skull at the surface.
Discovery and extraction
Finally, having lain beneath the ground for millions of years, the partially exposed skull is spotted by a palaeontologist, who undertakes a careful extraction of the skeleton. The process requires patience and precision work to avoid damaging the specimen; a generous amount of rock is retained around the specimen to protect it.
What are the types of fossils?
from http://quizlet.com/1584445/5-different-types-of-fossils-flash-cards/ )
Mold (imprint) fossils – When a leaf, feather, bone or even a body of an organism leaves an imprint on sediment, which hardens and becomes rock
Cast fossils – When minerals fill in the hollows of an animal track, a mollusk shell, or another part of an organism
Fossil fuels – Fuels formed by the remains of dead plants and animals. These include petroleum, coal and natural gas. Although technically a “fossil”, this isn’t usually what people mean by that term.
Actual remains – The body of an organism, with all the parts intact. Usually preserved in ice, amber, or tar. There may be some organic molecules still intact, such as collagens, other proteins, or even short strands of DNA.
Petrified wood – When minerals replace wood or stone to create either petrified wood or a mineralized fossil
How do fossils help us understand evolution?
The appearance of fossils of different places in the ground is not random.
The principle of fossil succession:
fossils succeed one another in a definite and determinable order.
fossils found in deeper levels are older
fossils found in less deep levels are younger
Evolution by natural selection:
the environment changes in many ways over time.
Not all living things survive long enough to have offspring
Those individual organisms that do survive long enough to have offspring are fit, they pass their genes on to the next generation. Those genes become more common.
Those individual organisms that do not survive long enough to have offspring are not fit, they don’t pass their genes on to the next generation. So their genes become less common.
This means that over time organisms may become entirely extinct. Other organisms may survive but their genes are different.
When there are enough differences of genes we can say that the organism is a new species.
Geologists used fossils to improve the correlation of rock layers and reconstruct past
An index fossil is the fossil of an organism that was geographically widespread and abundant in the fossil record, but that existed for only a limited span of time.
This section from the Earth Science study guide by Tarbuck and Lutgens.
What do we learn from fossils?
Fossils are among the most valuable sources of information about the Earth’s history. They tell us about the organisms that lived on Earth from the time of the oldest fossils, about 3.8 billion years ago, to the present.
By studying fossils we can learn not only about the creatures and plants of the distant past, but how they grew, what they ate, how they interacted, and many aspects of their behavior.
Fossils reveal many fascinating facts about the past, but they do a lot more. Do you own anything made out of plastic? Plastic comes from oil, which also provides gasoline, gas heat, and many other necessities of modern life. Fossils are one of the most useful aids to finding oil, because oil tends to accumulate in the pores of particular rock layers.
Rocks of different ages contain different fossils. Study of microscopic fossils brought up in chips of rock during drilling of wells has led to many major oil and gas discoveries. Also, the oil itself is derived from fossil remains of ancient organisms.
Study of fossils has led to important new understanding about how life evolved on earth and about diseases, both ancient and modern. Fossils also help us understand past climates, including ice ages and periods that were warmer than our present climate.
Knowledge from the study of fossils is helping geoscientists understand global warming and its effects. By studying the catastrophic extinction of the dinosaurs and many other life forms at the end of the Cretaceous Period, geoscientists have gained insight into the evolutionary implications of impacts by extraterrestrial objects.
Investigating the physical and chemical characteristics of fossil organisms that lived during times of drastic climatic change helps us understand the implications of the changes we are making in our own environment.
Information about Earth history, practical help in finding energy resources, and information that helps us anticipate the effects of possible environmental changes are not the only benefits derived from fossils.
Fossils are beautiful. Many thousands of people collect, buy, sell, and trade fossils all over the world. Some jewelry and furniture are made from fossils, and many stone buildings are made from stone that is composed largely of fossils. Many people collect fossils simply because they are beautiful, but others do so because fossils tell fascinating stories. Neither Barney the Dinosaur nor Jurassic Park would exist if there were no fossils.
Massachusetts Science Frameworks Curriculum, High School
HS-LS4-1. Communicate scientific information that common ancestry and biological evolution are supported by multiple lines of empirical evidence, including molecular, anatomical, and developmental similarities inherited from a common ancestor (homologies), seen through fossils and laboratory and field observations.
Massachusetts Disciplinary Core Idea Progression Matrix, based The Framework for K-12 Science Education (NRC, 2012)
College Board Standards for College Success: Science
Objective ES.3.2 Rock and Fossil Records. Students understand that the rock and fossil records provide evidence of the evolution of Earth’s environment and the associated changes in life over time.
ESM-PE.3.2.1 Infer the environment in which a fossil formed. Inference is based on the physical characteristics of both the fossil and the rock in which the fossil was found.
ESM-PE.3.2.2 Determine, using the law of superposition and using cross-sectional representations of fossil-bearing rocks, the relative ages of fossils from different locations.
ESH-PE.3.2.1 Explain, based on evidence found in the rock and fossil records, species extinction and evolution.