5-2 The Fossil Record http://www.kpbsd.k12.ak.us/chapman/demers/images/collage2.JPG.

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5-2 The Fossil Record http://www.kpbsd.k12.ak.us/chapman/demers/images/collage2.JPG

What is a fossil? Some of the most important clues to Earth’s past are fossils. A fossil is the preserved remains or traces of an organism that lived in the past. Most fossils form when organisms that die become buried in sediments (particles of soil and rock).

Why are fossils important? It enabled scientists to see occurrence of extinction in different species It gave Darwin evidence that earth is older than previously believed and that very slow changes over a long period of time can add up to substantial changes in organisms It shows evidence of continental drift – the belief that the continents were once one large landmass

Plummer et al 2003

Fossilization Hard parts of organisms are more likely to be preserve than soft parts. Soft parts are likely to decay or be consumed by other organisms Because of this soft bodied creatures such as jellyfish may not be fossilized either Buried organisms are more likely to be fossilized because it minimizes the decay, consumption, and destruction of the remains

Types of Fossils Petrified Fossils – remains that become buried in sediments and actually changed to rock. Mold – a hollow space in sediment in the shape of an organism or part of an organism Cast – copy of the shape of the organism that made the mold Preserved Remains – entire organisms kept intact in ice, tar, or amber Traces – other evidence that an organism existed, ex. tracks, trails, footprints

Impression - Cast and Mold Preserved Remains Petrified Fossils http://www.fossilmall.com/Stonerelic/amber/a25/bazaar_hemipteran_a25.htm http://www.fp.sfasu.edu/geology/GeologyTutorial/Fossils/CARBONization01.JPG Impression - Cast and Mold http://gpc.edu/~pgore/myphotos/fossils/cast&mold.jpg

Petrified wood Trace fossil http://www.clas.ufl.edu/users/pciesiel/gly3603c/wood1.jpg http://www.dinosaursrock.com/SteveDiloposaurusFootPrint.jpg

Age on Earth Scientists can determine a fossils age in two ways: relative dating: used to determine which of two rocks is older (layers at the top of the rock are younger than layers at the bottom) Absolute dating : used to determine the actual age of fossils

Fossil Record The millions of fossils that scientists have collected A species is extinct if no members of that species are still alive

Relative Dating Using Fossils http://www.carleton.ca/~tpatters/teaching/climatechange/rocks/rocks11.gif

Geologic Time Scale A calendar of Earth’s history that spans over 4.6 billion years. Scientists have divided this large time period into smaller units called eras and periods. The largest span in the calendar is the Precambrian Era. Very few fossils are found from the Precambrian Era

Plummer et al 2003 Also called Hadean

http://books.nap.edu/html/creationism/evidence.html

Theories of Evolution Gradualism – evolution occurs slowly but steadily Punctuated equilibria – species evolve during short periods of rapid change