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CHARLES DARWIN 1809-1882.

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Presentation on theme: "CHARLES DARWIN 1809-1882."— Presentation transcript:

1 CHARLES DARWIN

2 TRIP ON THE BEAGLE 1830’S BEAGLE TOURED AROUND THE WORLD
SPENT TIME ON THE GALAPAGOS ISLANDS off the COAST OF ECUADOR TRIP LASTED 5 YEARS COLLECTED MANY SAMPLES, SPECIMENS AND SENT THEM HOME KEPT A JOURNAL THE ENTIRE TRIP OF HIS OBSERVATIONS

3 DARWIN’S OBSERVATIONS ON HIS TRIP
SAW lots of DIVERISTY of ANIMALS & PLANTS HE realized there were an enormous amounts of species ESTIMATE-3-20 MILLION MORE THEN 99.9% of all SPECIES that ever lived are now EXTINCT Causes-mass extinction events 5 and human actions 1. He asked- Where did all these SPECIES come from & WHY did some of them DISAPPEAR?

4 MORE OBSERVATIONS He saw the many ways organisms lived & reproduced
HE CALLED this FITNESS- TRAITS & BEHAVIORS which enable ORGANISMS to SURVIVE/REPRODUCE in their ENVIRONMENT 2. How did these organisms develop structures that give them this fitness? 3. Why were there so many techniques for survival?

5 1. Modern organisms arise through EVOLUTION
1859 “THE ORIGIN OF SPECIES” IS PUBLISHED 30 YRS. AFTER THE BEAGLE Why did he wait so long? 5 KEY CONCEPTS of Darwins Theory on Evolution: 1. Modern organisms arise through EVOLUTION 2. Each species comes from a preceding one, they have a COMMON ANCESTOR. AKA COMMON DESCENT 3. FITNESS comes from ADAPTATION 4. SUCCESSFUL ADAPTATION allows organisms to SURVIVE & REPRODUCE 5. ADAPTATION is any characteristic that INCREASES an organism’s FITNESS

6 THE AGE OF THE EARTH 18TH 19TH centuries scientists HYPOTHESISED that the EARTH is VERY OLD, & CHANGED VERY SLOWLY due to their observations weathering of rock, Earthquakes, sea levels, SCIENTISTS observed the EARTH moved & exposed FOSSILS in the layers. Fossils resembled organisms that were still alive on Earth, other fossils did not resemble any current organisms on Earth. How do you explain this? These ideas influenced DARWIN’S idea about the Evolution of organisms.

7 Rock ID Interactive http://www. learner

8 RELATIVE DATING-NOT DATING YOUR COUSIN!
GEOLOGIST noticed that certain types of rock could always be found in the same vertical order If they knew the type of rock and how old it was then … The age of the rock can be estimated by its position in the rock layers. Older layer Newer layers

9 RADIOACTIVE DATING-YOU HAVE A GLOW ABOUT YOU! Uranium
The age of rocks can be determined by what element(s) it is made from As you recall, many elements are radioactive (isotopes) ATOMS DECAY OVER TIME SO…

10 Radioactive Dating is More Exact Dating of Fossils
When the atoms decay they become new elements because the number of sub atomic particles has been reduced. The decay rate of an element is called HALF LIFE. HALF LIFE Is the time it takes for half the atoms of a molecule of an element to decay. Half life animation

11 URANIUM 238 HALF LIFE is 4.5 Billion years
When URANIUM decays it becomes LEAD Scientist determine ROCK AGE by comparing Uranium to Lead RATIO If the ratio of uranium:lead is higher then, is the rock younger or older? younger

12 C14, CARBON DATING of ONCE LIVING ORGANISMS
The element Carbon exists as radioactive Carbon14 & non-radioactive Carbon12 Living cells take in BOTH forms. When cells die they no longer take in C14. The longer an organism is dead, the lower the ratio of C14 :C12 C14 CARBON’s half life is 5,730 YEARS So after 5,730 years ½ is left, 11,460 2 half lives ¼ is left, 17,190 3 half lives 1/8 is left, 22,920 4 half lives 1/16 is left Can date clothing, bones, some prehistoric items, etc

13 FOSSIL RECORD Information of the GEOLOGICAL RECORD of EARTH. Can tell us about climate, life forms. SEA CREATURES IN ARIZONA, COASTLINE CHANGES GIANT FERNS IN N. AMERICA WARMER CLIMATE WHAT DOES A PALEONTOLOGIST STUDY? Fossils, bones

14 MOST FOSSILS ARE FOUND IN WHICH TYPE OF ROCK?
FORMATION OF FOSSILS MOST FOSSILS ARE FOUND IN WHICH TYPE OF ROCK? SEDIMENTARY ROCK -SEDIMENT FORMS WHEN SAND & SILT FROM WATER SETTLE TO THE BOTTOM OF A BODY OF WATER Animals & plants that die in the water are compressed by pressure from sediments and water

15 FORMATION OF FOSSILS BONES & TEETH can be preserved by SAND, MUD OR VOLCANIC ASH. Footprints or soft tissue can be preserved by ash, but this is very rare. They have no hard parts so they are harder to make impressions and molds. Sap from trees can trap insects, & plants and preserve them. The sap is preserved is called Amber.

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17 FORMATION OF FOSSILS PETRIFICATION can occur when the remains are covered with water DISSOLVED MINERALS from the water replace the decaying tissues & hardens like stone.

18 Petrified wood

19 GAPS IN THE FOSSIL RECORD
Why are there gaps in the fossil record? CONDITIONS TO FORM FOSSILS NOT PRESENT SOME TISSUES ARE TOO SOFT TO FORM FOSSILS-JELLY FISH, WORMS EROSION DESTROYS FOSSILS FOSSILS CAN BE BURIED AND NOT FOUND

20 How to determine Ancestry COMPARISON OF LIVING ORGANISMS Video
EMBRYOLOGY CHARACTERISTICS LOST IN ADULTHOOD are present in unrelated embryo species ALL VERTEBRATE EMBRYOS HAVE GILL POUCHES-NECK FOLDS IN FISH DEVELOP INTO GILLS IN HUMANS-EAR BONES This is evidence of inheritance from a fish-like ancestor. The common ancestor of these organisms passed on a gene for development in the embryonic stage. Mutations passed on changes to the adult form to create differences in anatomy and evolvement to new species.

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22 COMPARATIVE ANATOMY Remember the frog arm & chicken wing?
HOMOLOGOUS STRUCTURES -SIMILAR STRUCTURES DUE TO A COMMON ANCESTOR Remember the frog arm & chicken wing?

23 COMPARATIVE ANATOMY ANALOGOUS STRUCTURES -Similar looking but not from a recent, common ancestor.

24 COMPARATIVE ANATOMY VESTIGIAL STRUCTURES -INHERITED from an ancestor, but no longer used Whale pelvis

25 COMPARATIVE BIOCHEMISTRY big picture
COMPARISON OF GENETIC SEQUENCES among organisms. HOW CLOSELY RELATED ORGANISMS ARE TO EACH OTHER comparing their genes Organisms with a recent COMMON ANCESTOR HAVE SIMILAR GENE SEQUENCES This has caused re-thinking of the ancestry of some animals.

26 OLD SCHOOL THINKING NEW SCHOOL

27 OLD SCHOOL NEW SCHOOL

28 CLADOGRAM-shows ancestral relationships, timeline http://www. pbs


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