Chapter 11 - Other Evidence of Evolution Flashcards
What is FOSSIL?
Examples
Any well-preserved trace or part of an organism that lived a long time ago.
- A fossil is any preserved remains, impression, or trace of any once-living thing from a past geological age.
eg. PARTS OF AN ORGANISM
- Bones, shells, teeth
OTHER
- footprints, burrows, faeces, or impressions of all or part of an animal or plant.
Human ancestors = bones, teeth, sometimes footprints
What is an example of a human ancestor and its fossil remains
The ancestor of Modern Human = Australopithecus afarensis
- Fossil remains found in the Hadar, region of Ethiopia
Why are fossils and remains of organisms’ important?
Extremely important as they allow scientists to
- DETERMINE exactly what EXTINCT Species were like.
Other material associated with bones such as the rock which they were found and fossils of other plants and animals, allow the scientists to
- DEVELOP A PICTURE OF LIFE IN THE PAST - what the organism ATE, what OTHER organism EXISTED at the TIME, CLIMATE CONDITIONS.
FOSSIL RECORD has allowed scientists to BUILD A SEQUENCE of the EVOLUTION of a PARTICULAR PLANT/ANIMAL.
eg. Horse (best example) - traced from fossil remains to have been evolved from creature not much bigger than a small dog to current horse.
What happens if conditions for fossilisation does not come into effect?
What are the 2 main CONDITIONS FOR FOSSILISATION IN TERMS OF DECAY?
Billions of organisms have lived on Earth, the Chance that a plant or animal will be fossilised is very small.
- BECAUSE normally, dead organisms are DECAYED by MICRO-ORGANISMS and NO TRACE OF EXISTENCE is left.
CONDITIONS FOR FOSSILISATION
1. Parts/organism may be fossilised when BURIED BY DRIFTING SAND, MUD DEPOSITED BY RIVES, VOLCANIC ASH, OR (HUMAN ANCESTORS) MEMBERS OF A SPECIES.
- if BURIED RAPIDLY, CONDITIONS MAY NOT BE SUITABLE FOR THE ACTIVITY OF DECAY ORGANISMS (DECOMPOSERS), AND THE DECOMPOSITION WILL BE SLOW OR PREVENTED.
What is the effect of soil type on fossilisation? (FOR BONE)
WHAT ARE THE GOOD CONDITIONS?
- EXPLANATION
WHAT ARE THE BAD CONDITIONS
- EXPLANATION
NATURE OF SOIL = is very important for the FOSSILISATION OF BONE (OR OTHER FORMS OF TISSUE)
BAD CONDITIONS OF SOIL
- WET,
- ACIDIC SOIL
Causes the bone to be DISSOLVED, = no fossilisation occurs.
- Oxygen present = decomposers will be abundant and able to survive - cause decay to organism body.
GOOD CONDITIONS OF SOIL
1. No OXYGEN; as in the case of peat, complete preservation of soft tissues and the bones of the animal may occur.
- ALKALINE soil = BEST FOSSILS PRODUCED
Because the MINERALS IN THE BONE ARE NOT DISSOLVED.
- NEW MINERALS (eg. Lime or iron oxide) are DEPOSITED in the PORES of the BONE, REPLACING THE ORGANIC MATTER THAT MAKES UP ABOUT 35% by weight of the bone.
- Bone becomes PETRIFIED (TURNED INTO ROCK), but the DETAILS OF THE STRUCTURE ARE STILL PRESERVED.
Where are Fossils usually located and explain how and why they are preserved in each location.
Examples of Location in which human or other organism fossils are found =
- EDGES OF ANCIENT LAKES AND RIVER SYSTEMS,
- IN CAVES OR VOLCANICALLY ACTIVE AREAS
this is because the organisms can be BURIED RAPIDLY, PREVENTING DECOMPOSITION.
- RIVERS AND LAKES BUILD UP SEDIMENTS WHEN FLOODING OCCURS OR WHEN THE WATER FLOW SLOWS RAPIDLY.
- many CAVES are in Limestone (CALCIUM CARBONATE)
This chemical may be deposited around DEAD organisms,
- or the cave roof or walls may COLLAPSE, covering the bodies of animals. - unusual for animals to be preserved NEAR VOLCANIC ERUPTIONS - because the HEAT FROM THE VOLCANIC MATERIAL DESTROYS THE ORGANISMS
- but in EAST AFRICA ASH FALLS HAVE PRESERVED FOSSILS OF MANY HUMAN ANCESTORS.
How are fossils usually found?
- Fossils sometimes found by CHANCE
- at the SURFACE OF THE GROUND where they might have been UNCOVERED DUE to EROSION.
OFTEN DISCOVERY OF FOSSILS IS THE RESULT OF SLOW AND PAINSTAKING
- EXCAVATION OF LIKELY SITES.
- surface discoveries such as fossil fragments, or evidence of human occupation such as that found in many CAVES, are INDICATIONS, of the places where excavations may PROVE FRUITFUL.
What is Excavation?
What are the steps
Excavation = ‘the dig’
- In archaeology, excavation is the exposure, processing and recording of archaeological remains.
- These locations range from one to several areas at a time during a project and can be conducted over a few weeks to several years.
- SURFACE DISCOVERIES such as fossil fragments, or evidence of human occupation such as that found in many CAVES, are INDICATIONS, of the places where excavations may PROVE FRUITFUL.
- the area to be Investigated is SURVEYED AND MARKED OUT IN SECTIONS
- SMALL HAND TOOLS are used to REMOVE SOIL GENTLY so as NOT TO DAMAGE ANY OF THE MATERIAL.
- THE SOIL REMOVED is usually SIEVED so that even very SMALL FRAGMENTS are NOT OVERLOOKED
- PHOTOGRAPHS are Taken at every stage of a dig so that DETAILED STUDIES of the POSITIONS of UNCOVERED MATERIAL can be CARRIED out LATER.
- EACH ITEM IS carefully LABELLED AND CATALOGUED for the PROLONGED STUDY THAT FOLLOWS THE EXCAVATION OF THE SITE.
- IN THE LAB. Fossil bones AND ARTEFACTS are carefully SCRAPED CLEAN, BROKEN PARTS ARE POEICED TOGETHER, MEASUREMENTS ARE TAKEN.
- PLASTER CASTS OR LATEX MOULDS MAY BE MADE
What are artefacts?
examples?
In which case are artefacts found?
Artefacts = objects that have been deliberately made by humans
examples = stone tools, beads, carvings, charcoal from cooking fires and cave paintings.
Found in the case of fossils of human ancestors - artefacts are found in association with the fossils.
What is dating?
Why is it important?
One of the major tasks following the excavation of fossils or artefacts
DETERMINING THE AGE OF THE FOSIISL/MATERIAL
knowledge of the age is crucial in FINDING OUT THE SEQUENCE OF CHANGES THAT HAVE RESULTED IN PRESENT-DAY HUMANS or species.
What are the two different types of dating?
Explain them.
Various methods of dating exist - which can provide
- ABSOLUTE DATES - the actual age of the specimens
- methods are LIMITED in their application because each depends on the occurrence of a particular set of circumstances before it can be sued
- do give a number of ways of determining the actual age of ancient material
- new methods are being developed, with constant improvements of accuracy older methods - RELATIVE DATES - A Comparison of fossils to tell us whether one sample is Older or Younger than other
- determining the relative order of past events, without necessarily determining their absolute age.
- considered in relation or in proportion to something else.
What has modern tech. allowed fossils to be dated?
Modern Tech has ENABLED ACCURATE ESTIMATES to be MADE of the ABSOLUTE AGE of many samples.
However, when that is not possible, knowing whether one fossil is older or younger than another is very important.
The age (or date) of a fossil or artefact is usually given in years before the present time. eg. A fossil may be said to date from 45 000 yrs BP, which is another way of saying it is 45 000 yrs.
BP = before present
Examples of Absolute dating.
Examples of Relative dating
Absolute dating
- Potassium-argon dating
- Carbon-14 dating
Relative dating
- Stratigraphy
- Tree-ring dating
What is potassium-argon dating?
Absolute dating technique that is based on the decay of radioactive potassium top form Calcium and Argon.
What are Isotopes?
Isotopes are atoms of the same element with different numbers of neutrons.
What are the isotopes of Potassium?
What is used in K-Ar dating?
why is it used?
K all have 19 protons
K-39 =. 20 N
K-40 = 21 N
K-41 = 22 N
K-40
- radioactive isotope and DECAYS TO FORM Ca-40 or. Ar-40.
- such decay takes place at an extremely SLOW BUT CONSTANT RATE,
- so determining the amounts of K-40, Ar-40 in a rock sample enables the age of the rock to be calculated.
As the rock AGES, the PROPORTION OF K-40 DECREASES WHILE THE Ar-40 INCREASES.
What are the limitations of K-Ar dating?
- Not all rock types are suitable for this method of dating
- Can only DATE ROCKS OLDER THAN 100 000 - 200 000 years.
Define Half-life
The time required for half of any quantity of radioactive material to decay into stable non-radioactive material
Explain the half-life of K.
Why can it only date samples older than 200 000 yrs
The half-life of K-40 is 1250 BILLION YEARS (1.25 x 10^9)
- this means it takes 1250 billion years for half of the K-40 to decay.
- therefore after 100 000 YRS ONLY 0.0053% OF THE K-40 in a rock would have decayed to argon-40.
Such a small amount pushes the limits of detection services currently in use.
- hence it is more useful on samples that are older than 200 000yrs.
How to use K-Ar dating to determine the age of a sample?
- Some suitable rock of the same age as the fossil must be available
- The age of the rock is determined Using K-Ar dating, and hence the age of the fossil is INFERRED.
- the situation can occur when rocks PRODUCED IN VOLCANIC ERUPTIONS BURY BONES
What is Carbon-14 dating?
The radiocarbon dating method is based on the DECAY of the RADIOACTIVE ISOTOPE OF CARBON (C), to Nitrogen.
How is Carbon-14 produced?
- Carbon-14 is produced in the UPPER ATMOSPHERE by the action of the cosmic radiation (emitted from stars), ON NITROGEN (N) at about the SAME RATE AT WHICH IT DECAYS
- In the atmosphere there is a RATIO OF ONE C-14 TO VERY MILLION MILLION (10^12) ATOMS OF THE STABLE ISOTOPE CARBON-12.