The history of Life Section 19.1: The fossil record

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1 The history of Life Section 19.1: The fossil record

2 Fossils and Ancient Life Fossils provide information about extinct species Fossils can vary greatly Different sizes, types and degrees of preservation Not every organism will become a fossil

3 Types of Fossils

4 Trace Fossils

5 Fossils in Sedimentary rocks Why don t all organisms become fossils?

6 What information can fossils tell you? The structure of an organism Lead to ideas about evolutionary relationships The Environment an Organisms lived in Fossilized plants and leaves give an idea of the ecosystem The way in which an organism lived Footprints and bone structure give information about how an animal moved Groups of fossils give information about how organisms interacted

7 How do researchers know the age of fossil specimens? Two types of dating Relative dating Radiometric dating Relative dating used the presence of an index fossil or other feature to determine whether a rock is older or younger than another rock Can allow paleontologists to tell the age of a rock

8 What is an index fossil? Index fossils are fossils used to establish the relative age of a rock layer Often distinctive Found in many places Only existed on Earth for a small amount of time Trilobites are a great example 15,000 different species Can be used to date nearly 300 million years worth of rocks

9 What is radiometric dating? Radiometric dating uses the proportion of radioactive to stable isotopes to calculate the age of a sample Different elements decay at different rates The rate of decay is referred to as the half life Carbon 14 decays to Carbon 12 naturally in the atmosphere When a plant photosynthesizes it will take in a small amount of Carbon 14 Upon death, this amount of carbon is fixed and will decay over time to carbon 12 Carbon 14 will not be replenished, so by measuring the amount of carbon 14 remaining, the age of the plant can be calculated Animals also get carbon from eating plants so can be dated this way Half life of carbon is 5730 years

10 How do you date samples older than 60,000 years? Carbon-14 is not the only isotope used for radiometric dating Elements such as Rubidium (half life 48.8 billion years), Uranium (half life 4.5 billion years). By choosing the correct element you can essentially date anything on Earth These are often used alongside index fossils to determine the ages of geological units

11 Why don t we just radiometrically date everything? Because it is very expensive and takes a very long time!

12 How old is the Earth? 4.6 billion years old Divided into Eons, Eras, Periods and Epochs Precambrian is the first 3.5 billion years Our Geological period only started 1.8 million years ago

13 Geological time as a clock It is often hard to comprehend simply how old the Earth is, and for how little humans have occupied it This graphic puts it into perspective

14 How has the Earth changed through geological time?

15 What has affected conditions on Earth through time? Physical Forces Climate is constantly changing Great ice age 10,000 years ago, average temperature was only 5 Celsius lower, During the Mesozoic, average temperatures were only 6 12 Celsius higher Earth is constantly changing Mountains, Volcanoes, New Coastlines, which has knock on effects to habitats Plate Tectonics and Super-continental Cycles are a powerful driving force

16 Biological effects on Earth through time Life can have a large affect in shaping Earth Early Oceans were full of dissolved Iron Atmosphere did not have much Oxygen Some of the first organisms to Evolve were photosynthetic bacteria These took in CO2 and gave out O2 CO2 is a greenhouse gas the reduction in CO2 levels lead to drops in global temperatures As temperatures dropped, Iron reacted with atmospheric oxygen, was no longer soluble in the oceans and precipitated out This settled to the ocean floor producing banded Iron formations

17 Key points Fossils are a powerful tool used to aid our understanding of the evolution of the Earth They can be dated through either relative or radiometric dating Earth is 4.6 billion years old The Earth s surface has been shaped a number of different physical and biological factors over the course of it s history

18 Patterns and processes of Evolution Section 19.2

19 Why do some organisms live but others die? Some changes occur within a species Others can be over much larger scales When changes occur in clades greater than a single species they are referred to as Macroevolutionary patterns Creation of species through speciation Disappearance through extinction Emergence of large clades dinosaurs, mammals examples of macro evolutionary patterns

20 Classification of fossils Fossils can be classified into clades Either clades only containing extinct organisms Or clades also containing living organisms Cladograms illustrate how closely related organisms are Relation does not mean direct ancestor

21 Why do species go extinct? They fail to adapt to a changing environment Some clades appear more susceptible to extinction than others - why? The rate of speciation within a clade must equal to or greater than the rate of extinction for a clade to continue to survive over the long term Reptillia is an example of a highly successful clade Living organisms continue to adapt and thrive Most species in clade dinosauria are extinct, but birds survived because they adapted to the new environment

22 What drives extinction of a species? Two types of extinction Extinction due to Natural selection always occurring (background extinction) Extinction due to a mass Extinction A mass extinction is when a many species become extinct over a short period of time. Entire ecosystems vanish, food webs collapse Earth has experiences many of these throughout it s history

23 What causes mass extinctions?

24 Is there a good side to a mass extinction? Yes, there can be. It creates many new opportunities for survivors to adapt and speciate Recovery takes about 5 10 million years

25 Does evolution always occur at the same rate? No! Some organisms change consistently through time gradualism Some organisms do not really change over time, until something happens to upset their equilibrium punctuated equilibrium. It has been proposed that most new species are produced during this period of rapid change

26 Why does evolution occur at different rates? Rapid evolution may occur if a small population gets separated from the main populations Small population will evolve faster as there are fewer individuals to spread change to Migration to a new environment Eg. Galapagos Islands Mass extinctions create many new ecological niches Organisms that survive will fluorish

27 Macroevolution There are two main types of macroevolution Adaptive Radiation One ancestral species (or small group) evolves to produce a number of different species that live in different ways Can be caused by migration, extinctions Species can also evolve a new feature allowing them to take advantage of the environment Example dinosaurs and mammals Mammals were around during dinosaurs but were not successful After dinosaur extinction, an adaptive radiation of mammals began. Convergent Evolution Unrelated organisms in different places but similar environments evolve similar features Emus, Rheas and Ostriches

28 What is Coevolution? The process by which two species evolve in response to changes in each other over time Often they become so intertwined that neither can live without the other If one has an evolutionary change so will the other Examples Specific flowers and pollinators Plants and herbivores Plants produce poisons to stop themselves being eaten But insects resistant to the poisons will flourish Often these insects use the poisons to their advantage

29 Key Points Macro-evolutionary patterns are changes that affect many species of entire clades Examples speciation and extinction Earth has experienced a number of mass extinctions Evolution can occur at different rates Gradualism vs punctuated equilibrium Paleontologists have identified patterns of macroevolution Adaptive radiation and convergent evolution

30 Earth s Early History Section 19.3

31 The Early Earth Earth formed through collision of a series of cosmic debris 4.2 billion years ago it cooled enough for rocks to form Early atmosphere had little to no oxygen, Largely CO 2, water vapor and nitrogen Very inhospitable!

32 The first organic molecules It was shown by Miller and Urey in 1953 that Earth s early primitive atmosphere was capable of creating organic molecules they created 21 amino acids! Although the composition for the Early Earth that they used was incorrect, but the general idea was correct

33 How do you go from organic molecules to living cells? A lot remains unknown about this step Evidence suggests million years after the first rocks formed, cells similar to bacteria were common how? Scientists have shown that under the correct conditions, large organic molecules can form protenoid bubbles called microspheres Not cells but have some characteristics of cells Thought to acquire characteristics of living cells 3.8 billion years ago

34 Where did DNA and RNA come from? No one is sure, but a number of hypotheses exist RNA is thought to be able to form from simple organic molecules Based on experimental evidence RNA is very versatile lead to the RNA world hypothesis RNA existed before DNA, and lead to direct DNA directed protein synthesis

35 Where did the Oxygen come from? First fossils that resemble bacteria come from 3.5 billion years ago Evolved in the absence of oxygen 2.2 billion years ago, photosynthetic organisms evolved Change the chemistry of the atmosphere Cooled the Earth Oxygen reacted with Iron in the Oceans precipitating out Atmospheric composition changed over time became toxic to many early organisms on Earth - adapt or die!

36 When did Eukaryotic cells originate? Proposed that 2 billion years, some ancient prokaryotes began to evolve internal cell membranes Endosymbiotic theory: prokaryotic cells entered these prokaryotes with an internal memberane Intruders did not infect or be digested, instead they began living within larger cells A symbiotic relationship developed between primitive eukaryotic cells and the prokaryotic cells within them Proposed due to similarities identified between membranes of chloroplasts and mitochondria and prokaryotes

37 Endosymbiotic theory explained

38 Modern Evidence DNA evidence shows that DNA from bacteria and DNA from mitochondria and chloroplasts are similar All have ribosomes of a similar structure and size They all reproduce by binary fission - division by mitosis All together these features suggest a common ancestor!

39 Sexual reproduction Sexual reproduction increases genetic variation and therefore sped yo evolutionary change Asexual reproduction leads to a direct genetic copy Genetic variation is restricted to mutations In sexual reproduction, genetic material comes from two parents Increased variation and increased chance of adapting to new or changing environmental conditions Multicellular organisms evolved a few hundred million years after the evolution of sexual reproduction Adaptive radiation lead to great diversity

40 Key points Earth s original atmosphere was a harsh environment that could not support life as we know it The exact origin of life is unclear, but it is though to stem from the production of organic molecules such as proteins and RNA, leading to the formation of protenoid microspheres Photosynthetic bacteria lead to the production of an oxygen rich environment 2.2 billion years ago Eukaryotic cells developed through endosymbiotic theory the ingestion of prokaryotes by a slightly altered prokaryote Sexual reproduction has lead to increased amounts of genetic variation and evolution