Geologic Time Life and Geologic Time Chapter 6---Section 1 Geologic Time Scale • Division of Earth’s history into time units based largely on the types of life-forms that lived only during certain time periods • Four major subdivisions: • • • • Eons (largest) Eras Periods Epochs (smallest) http://thestonescryout.com/yahoo_site_admin/assets/images/Geologic_Time_Chart.289193940_std.jpg • The geologic time scale takes us all the way back from present day • • • • Phanerozoic Eon Cenozoic Era Quaternary Period Holocene Epoch to the origin of Earth 4.5 billion years ago during the • Hadean Eon (Precambrian Time) Evolution • The process of change that occurs over time Lamarck’s Theory of Evolution • Organisms pass on characteristics that they acquired during their lifetimes to their offspring • Ex: He thought giraffes necks got longer after a lifetime of eating foliage that was very high up in trees. Each succeeding generation would have a longer neck. • Was his theory correct? • NO!!!! • Think: Does a mouse that had its tail chopped off have a baby mouse with no tail? Charles Darwin • Famous biologist who wrote a book called The Origin of Species in 1859 • Based on what he learned during his travels to the Galapagos Islands while traveling aboard the HMS Beagle in the 1830s Darwin’s Theory of Evolution by Natural Selection • Main points: • Overproduction - most organisms produce more offspring than can be supported by the environment…not all of them can survive • Variation - there are many variations within a species…those who possess the most favorable ones have a better chance of survival • Natural Selection - Organisms with more favorable variations will live longer and, thus, have more opportunities to reproduce • Change Over Time - If organisms with favorable traits reproduce more than others, then these traits will be passed on more to future generations. If enough changes occur in a group, a new species may develop Natural Selection • The process by which organisms best suited to the environment survive and reproduce • Also known as “survival of the fittest” Modern Day Example of Evolution by Natural Selection • Peppered Moth - light-colored in countryside where no pollution, but dark-colored in industrial cities where there is a lot of dark soot from pollution on tree trunks • Light moths have a better chance of surviving and passing on their white genes in the countryside • Dark moths have a better chance of surviving and passing on their dark genes in the city Trilobites • Organisms with a three-lobed exoskeleton • Lived in the ocean during the Paleozoic • Are considered to be index fossils • Different kinds of trilobites lived during different periods. All the different types show how trilobites evolved in response to changes in the environment. Species • A group of organisms that normally reproduces only with other members of their group and whose offspring are fertile Artificial Selection • Humans use artificial selection when breeding domestic animals. • By carefully breeding individuals with desired characteristics, animal breeders have created many breeds of cats, dogs, cattle, chicken, etc. What drives evolution? • A response to major changes in: • Type of environment • Climate • Caused by Earth processes or dramatic life-changing events • Organisms are left with two choices: • adapt or become extinct! Early Earth History Chapter 6---Section 2 Precambrian Time • • • • Longest part of Earth’s history (90%) Hadean, Archean, Proterozoic Eons 4.5 billion to 544 million years ago Life-forms: • Cyanobacteria • Invertebrates • Ediacaran Fauna • May be the longest time period, but relatively little is known about the organisms that lived then • Buried so deeply that they have been changed by heat and pressure • Have long since eroded • Most organisms didn’t have hard parts Cyanobacteria • Blue-green algae thought to be one of the oldest life-forms on Earth • Colonies formed layered mats called stromatolites • Contained chlorophyll and used photosynthesis • Produced the first oxygen for Earth’s atmosphere Invertebrates • Animals without backbones that appeared toward the end of the Precambrian • Not often preserved as fossils because of their soft bodies • Most evidence of their existence comes in the form of trace fossils Ediacaran Fauna • Group of very unusual animals with shapes similar to modern jellyfish, worms, and soft corals that arose late in Precambrian Time • First found in Ediacara Hills in Australia • Bottom dwellers • Might have had tough outer coverings like air mattresses • Trilobites might have outcompeted them and caused their extinction, but nobody knows for sure Paleozoic Era • 544 million to 248 million years ago • Traces of life are much easier to find in Paleozoic rocks because organisms with hard parts, such as shells, started to become common • Warm, shallow seas covered large parts of continents, so there are many marine fossils • i.e. trilobites • Life-forms: • Vertebrates • Amphibians • Reptiles Vertebrates • Animals with backbones • First ones were fishlike creatures without jaws • Armored fish with jaws appeared during the Devonian • Some were large enough to eat sharks! Life on Land • Many ancient fish had lungs as well as gills • Enabled fish to live in water with low oxygen levels because they could swim to the surface and breathe • Similar creatures are alive today that can get their oxygen from both water and air • Some had lungs and leglike fins, which they used to swim and crawl around on the bottom • Amphibians may have evolved from them • Still had to lay eggs in moist places • Then, some amphibians evolved an egg with a membrane that protected it from drying out, meaning it could be laid on land • These were the first reptiles • Had skin with hard scales that prevented the loss of bodily fluids • Now they could live far from water Extinction • At the end of the Paleozoic Era (Permian Period), more than 90% of all marine species and 70% of all land species went extinct • Might have been caused by changes in climate and lowering of sea level caused by the formation of Pangaea • Might have been caused by extremely high level of volcanic activity • Might have been caused by an asteroid or comet impact • Perhaps it was a combination of all these factors Mountain Building • Several mountain-building episodes occurred during the Paleozoic Era. • This is when the Appalachian Mountains formed. Middle and Recent Earth History Chapter 6---Section 3 Mesozoic Era • 248 million to 65 million years ago • Pangea started to break apart during the Mesozoic Era. • Life-forms: • • • • • Dinosaurs Birds Mammals Gymnosperms Angiosperms Dinosaurs • First small dinosaurs appeared during the Triassic Period • Larger species, like the Tyrannosaurus and Apatosaurus appeared during the Jurassic and Cretaceous • Dinosaurs were active • Gallimimus could run up to 65 mph! • Some may have been warm-blooded • Some dinosaurs nurtured their young and traveled in herds in which adults cared for their young. • Ex. Maiasaura Birds • First appeared during the Jurassic Period • Some paleontologists think birds evolved from small, meat-eating dinosaurs. • The earliest known bird fossil is Archeopteryx. • Not a direct ancestor of modern birds Mammals • Warm-blooded vertebrates that have hair covering their bodies. Females produce milk to feed their young. • First appeared during the Triassic Period • Earliest mammals were small, mouselike creatures Gymnosperms • Plants that produce seeds, but no flowers • Ex: pine and ginkgo trees • First appeared during the Paleozoic and dominated for the majority of the Mesozoic Angiosperms • Flowering plants that produce seeds with hard outer coverings • Ex: magnolia and oak trees • First evolved during the Cretaceous Period • Because their seeds are enclosed and protected, they can live in many environments • Angiosperms are the most diverse and abundant land plants today. Extinction • The Mesozoic Era ended when many groups of animals, including the dinosaurs, disappeared suddenly. • Probably caused by an asteroid impact that sent up a huge cloud of dust and smoke, which blocked out sunlight causing many plants to die. All the animals that depended on these plants also died. Cenozoic Era • 65 million years ago to present • The climate became much colder and ice ages occurred. • All the organisms that are alive today are descendants of survivors of the last mass extinction. • Mammals continued to evolve and became dominant. Mammals • Many kinds of mammals became larger • Ex: horses • Not all mammals remained on land • Ex: ancestors of present-day whales and mammals evolved to live in the sea • Many species became isolated and evolved separately from other life-forms • Ex: marsupials in S. America and Australia • Homo sapiens evolved around 140,000 years ago. Mountain Building • Many mountain ranges formed during the Cenozoic Era. • Alps in Europe • Andes in S. America • Himalayas in Asia