Fossils - Introduction to Evolution - Lecture Slides, Slides of Theory of Evolution

The important key points of Introduction to Evolution are: Fossils, Paleontologists, Volcanic Ash from Eruptions, Formation of Fossils, Quick Burial, Types of Fossils, Unaltered Soft Parts, Traces of Animals, Modification of Tetrapod Skeleton

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2012/2013

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Fossils
What are they?
They are the remains of plants and animals naturally
embedded (preserved) in the rocks.
During the 19th Century, scientists (including Charles
Darwin) noticed that the older rocks contained fossils
different from those in newer rocks.
The study of such fossils illustrated the changes that
occurred throughout history.
NB: Very few living things fossilize due to decay when
they die or being eaten or destroyed if the rock
metamorphoses but enough fossils have been found to
construct the history of life.
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Fossils

What are they?

  • They are the remains of plants and animals naturally embedded (preserved) in the rocks.
  • During the 19th Century, scientists (including Charles Darwin) noticed that the older rocks contained fossils different from those in newer rocks.
  • The study of such fossils illustrated the changes that occurred throughout history.
  • NB: Very few living things fossilize due to decay when they die or being eaten or destroyed if the rock metamorphoses but enough fossils have been found to construct the history of life.

Where do they occur?

  • They are most frequent in SEDIMENTARY

ROCKS especially, LIMESTONE &

SANDSTONES,.

  • SHALES could have some fossils as well as

TUFFS is the volcanic ash from eruptions

showered over organisms.

  • Who are paleontologists?
    • They study fossils as well as search for oil and coal.

TYPES OF FOSSILS

ALTERED HARD PARTS

UNALTERED HARD PARTS

UNALTERED SOFT PARTS

TRACES OF ORGANISMS

(A) Moulds (B) Casts (C) Tracks, (D) Trails, (E) Borings

1. UNALTERED SOFT PARTS

  • In order for hard and soft parts of an organism

to be preserved, no bacterial should be

present. For example, in the frozen mud (eg

Siberia) entire corpses of Mammoths and

Rhinocerous have been found. Also

mummified animals have been located in

moisture-less desserts due to lack of bacteria.

3. ALTERED HARD PARTS

Here chemical reactions take place changing the fossil but not its appearance eg

  • Carbonisation – where tissues of plants and animals change to a thin film of Carbon because water dissolved Hydrogen, Oxygen and Nitrogen from it eg graptolites, trilobites etc are found as carbon traces.
  • Petrifaction – trickling water can combine new elements eg SILICA which changes the soft calcite of bones and shells to a hard material ie petrify them.
  • Recrystallisation – where atoms are rearranged causing the formation of micro-crystals but not changing the physical structure of the fossils
  • Dehydration – many fossils originate from hydrous silica (found in opal) but this breaks down releasing water and silica changing the fossils to quartz.
  • Replacement – hard parts may be washed away and slowly replaced by other molecules (eg opal, iron pyrites) etc without changing the appearance of the fossil.

4. TRACES OF ANIMALS

  • Moulds – where the organism dissolves away leaving a cavity in the rock showing the exact shape of the hard parts of the fossils. There are usually found near fine grained sediments e.g. mud.
  • Casts – where the natural mould is filled with mineral material of another chemical composition eg Calcite. It can be lifted or chipped out of the rock.
  • Track and Trails – these are marks made in soft mud by the feet and tails of animals which are preserved in the rocks eg fossil foot prints, or burrows and tubes left behind by worms borer shells and jelly fish.
  • There are numerous examples of transitional forms in the fossil record, providing an abundance of evidence for change over time. Pakicetus (below), is described as an early ancestor to modern whales.

Although pakicetids were land mammals, it is clear that they are related to whales and dolphins based on a number of specializations of the ear, relating to hearing. The skull shown here displays nostrils at the front of the skull.

the beluga whale (below ) has its nostrils placed

at the top of its skull.

We would expect to see intermediate forms that

have nostrils between the front and top of skull.

  • Distribution in Time and Space
  • Understanding the history of life on Earth requires a grasp of the depth of time and breadth of space.
  • We must keep in mind that the time involved is vast compared to a human lifetime and the space necessary for this to occur includes all the water and land surfaces of the world.
  • Establishing chronologies, both relative and absolute, and geographic change over time are essential for viewing the motion picture that is the history of life on Earth.
  • Anatomy (1 of 2)

  • Individual organisms contain, within their bodies, abundant evidence of their histories. Theexistence of these features is best explained by evolution.

  • Several animals, including pigs, cattle, deer, and dogs have reduced, nonfunctional digits,referred to as dewclaws. The foot of the pig has lost digit 1 completely, digits 2 and 5 have been greatly reduced, and only digits 3 and 4 support the body. Evolution best explains such vestigial features. They are the remnants of ancestors with a larger number of functional digits.

  • People (and apes) have chests that are broader than they are deep, with the shoulder bladesflat in back. This is because we, like apes, are descended from an ancestor who was able to suspend itself using the upper limbs.

  • On the other hand, monkeys and other quadrupeds have a different form of locomotion.Quadrupeds have narrow, deep chests with shoulder blades on the sides.

  • The cellular level All organisms are made of cells, which consist of membranes filled with water containing genetic material, proteins, lipids, carbohydrates, salts and other substances. The cells of mostliving things use sugar for fuel while producing proteins as building blocks and messengers. Notice the similarity between the typical animal and plant cells pictured below — only threestructures are unique to one or the other.

  • The molecular level Different species share genetic homologies as well as anatomical ones. Roundworms, for example, share 25% of their genes with humans. These genes are slightly different in eachspecies, but their striking similarites nevertheless reveal their common ancestry. In fact, the DNA code itself is a homology that links all life on Earth to a common ancestor. DNA and RNApossess a simple four-base code that provides the recipe for all living things. In some cases, if we were to transfer genetic material from the cell of one living thing to the cell of another,the recipient would follow the new instructions as if they were its own.

  • These characteristics of life demonstrate the fundamental sameness of all living things onEarth and serve as the basis of today's efforts at genetic engineering.

  • Chronology

  • The age of the Earth and its inhabitants has been determined through two complementary lines ofevidence: relative dating and numerical (or radiometric) dating.

  • Relative dating strata. As shown in the diagram, fossils found in lower strata were typically deposited first and are deemed places fossils in a temporal sequence by noting their positions in layers of rocks, known as to be older (this principle is known asbecause the layers weren't deposited horizontally to begin with, or because they have been overturned. superposition ). Sometimes this method doesn't work, either If that's the case, we can use one of three other methods to date fossil-bearing layers relative to oneanother: faunal succession, crosscutting relationships, and inclusions. By studying and comparing strata from all over the world we can learn which came first and which camenext, but we need further evidence to ascertain the specific, or numerical, ages of fossils.

  • Numerical dating carbon. Very old rocks must be dated using volcanic material. By dating volcanic ash layers both above and relies on the decay of radioactive elements, such as uranium, potassium, rubidium and below a fossil-bearing layer, as shown in the diagram, you can determine “older than X, but younger thanY” dates for the fossils. Sedimentary rocks less than 50,000 years old can be dated as well, using their radioactive carbon content. Geologists have assembled a geological time scale on the basis of numericaldating of rocks from around