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geo quizlet 2

geology quiz 2

QuestionAnswer
Angular unconformity Siccar Point, Scotland, when rocks are tilted and form more in another direction, caused by erosion
Nonconformity two fundamentally distinct rocks, metamorphic rock below, sedimentary above
Disconformity sedimentary rocks parallel to each other above and below
Fossils preserved remains or evidence of biological activity that’s at least 10,000 years old
Why fossils? provide evidence of evolution over long time frames, ex. Causes, rates, and pathways
Where are fossils? caves, deep lagoons, tar, glaciers
Paleontology study of old life (1800)
Which type of rock are fossils? sedimentary and volcanic ash
What helps preserve fossils? rapid deposition, low oxygen, low energy, hard parts, fine, impermeable sediment cover (ash, clay)
Taphonomy study of fossilization
Vertebrates backbone
Invertebrates no backbone
Turbidity currents way to fossilize organisms
Body fossils a whole or part of an actual organism ex. Preserved in amber, exoskeleton, carbon fern
Trace fossils imprint, indirect evidence, no actual organism, ex. Dino footprint, imprints, worm burrows, trailmarks
Extraordinary fossil locales Geiseltal Formation, Germany, Solenhofen Formation, Germany, Burgess Shale, Canadian Rockies
Taxonomy classification of organisms, in order to find the relationships between organisms
Carolus Linaeus (1707-1778) Swedish Botanist, Father of Taxonomy, used naming, ranking, sent 19 students on voyages worldwide, binomial system
Biology species definition species are capable of producing viable offspring
Paleontology species definition species are defined based on similar morphology
Modern taxonomy system 3 domains system
6 kingdoms animalia, plantae, fungi, Protista, bacteria, archaea
Prokaryotes single cell that lacks a central nucleus, ex. Bacteria, archaea
Eukaryotes has a nucleus, some single cell some many, ex. Animalia, plantae, fungi, Protista
Why fossil record is incomplete? physical destruction, chemical destruction (dissolution), biological destruction (scavengers, bacteria), deformation, sampling problems(bias lack of data)
Uses of fossils correlation(relative age), paleo-env’t (determine env’ts deposition and distribution), plate tectonics, evolution(rates, causes, paths)
Unaltered body fossils 1 soft parts= tissue, hair, organs, skin found from freezing, tar, or amber, ex. La Brea Tar Pits, CA
Altered, permineralized body fossil inorganic material fills void
Altered, replaced body fossil orginal material dissolved and rplaced with inorganic ex. Petrified wood
Unaltered body fossil 2 hard parts= bones, teeth, shells, woody tissue from plants
Altered recrystallized body fossil crystal structure changed, no chemical alteration
Altered carbonized body fossil mostly plants, Hydrogen, oxygen and nitrogen escape and carbon film is left
Mold trace fossil imprint, 2D, solutions dissolve organism and leave void
Cast trace fossil mold filled with sediment, looks more 3D
Burrows trace fossil holes or tubes
Chemical trace fossils amino acids
Evolution inheritable changes in organisms over time
Evolutionary theory all organism are descendants of previously existing oranisms
Theory supported by a large body of evidence, used to make testable predictions, has not been discredited by any new data
Charles Darwin (1809-1882) English Naturalist, 1831-36 Beagle Voyage (Africa, s. America, Australia, Islands), takes “Principles of Geology” by Charles Lyell
Cape Verde Islands first part of Darwin’s trip, Africa, discovers a shelly rock layer, 50 ft above sea level
Punta Alta SA, Darwin, discovers large fossil bones in a cliff (rodents, sloths, etc.)
Falkland Islands SA, Darwin, discovers how species or fossils on the island differ from mainland, adapted env’t idea begins to form
Chile SA, Darwin, large earthquake, total destruction and fossil layers are uplifted near shore, evidence that continents have been uplifted over time
Galapagos Islands 600 mi from SA, yr 4, Archipelago, hotspots, finds many unique species, focus on Finches(13 species, but only 1 in SA, 5-6 weeks
Darwin’s 2 main conclusions new species originate only from pre-existing ones and species have a common ancestor, but each species has changed slightly as a result of living in a slightly different envt
Elder Darwin made observations in 1830s but presented in 1858 in London, co-presented with Wallace
Alfred Russell Wallace (1823-1913) British Naturalist, Explorer, Geographer, biologist, “father of biogeography”, came to same ideas as Darwin in Asia and Australia, Bio-geographical map of the world
Darwin-Wallace Model Natural Variations occur in any population, competition for resources, not all young will survive (organisms produce more young than necessarily sustainable), some traits more favorable than others
Thomas Matthus (1766-1834) political economist, 18th century England, said all organisms produce more young than necessary
Johann Gregor Mendel (1822-1884) Austrian monk, studied plant hybrids, 28,000 pea variations, father of modern genetics, laws of inheritance, papers from 1860 found in 1900
Mutations random changes at the molecular level that produce new inheritable traits
Phyletic gradualism Darwinian evolution-ancestors change continuously and gradually become new species, transitional species are common ex. Horses, Archaeopteryx
Punctuated equilibria ancestor species remain unchanged for most of time, rapid mutations occur and new species results, caused by mass extinctions, sudden climate change, isolation
Stephen Jay Gould (1941-2002) Harvard professor of paleontology, proposed punctuated equilibria, many popular and scientific publications
Archaeopteryx “Berlin specimen” part bird part reptile, avian feathers and wishbone, reptilian teeth and bony tail
Horses 25 mya were smaller, 4 toes, less ridges on teeth for woodlands, and now larger, single toe for grassland
Niles Eldredge curator, invertebrate fossils at American Museum of Natural History in NY, co-proposed “punctuated equilibria” with Gould in 1972
Organisms most at risk large, tropical animals because few in number, delicate balance in ecosystem
Georges Cuvier (1769-1832) said extinction occurs
Louis Dollo (1857-1931) proposed extinction is forever
Mass extinctions whole species going extinct in a short period of time
Causes of mass extinction flood basalts, sea level falling, impact events, global cooling/warming, plate tectonics
Pseudo-extinction evolution
Domino effect delicate balance where one species goes extinct and many others follow
Hadeon Eon 3.8-4.5 bya, Earth forms, differentiation, moon forms, crust forms (cratons), cratering, outgassing, oceans form by the end
Differentiation Earth becomes layered
Oldest rock formed 4.03 bya, metamorphic rock from Northwest Canada
Oldest mineral from 4.4 bya from Australia
Atmosphere of Hadeon Eon dense of water, Nitrogen gas and carbon dioxide but no oxygen
Archean Eon 2.5-3.8 bya, real rock record begins, bombardment ceases, really high heat flow, plate tectonics unknown, continental formations, <1% oxygen so single-cell prokaryotes
Rocks of Archean Eon , igneous/metamorphic rocks preserved, immature sedimentary rocks (deep water chert, coarse sand/clay mixes), few shallow sandstones, limestones or shales
Created by: lfalkens
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