Geology 105- Age of the Dinosaurs – Flashcards
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            Hypothesis
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        a proposed explanation for an observable phenomenon (testable idea)
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            Theory
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        an agreed upon scientific fact that (so far) cannot be disproven
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            Evidence
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        is based on current assumptions & physical evidence (changes through time)
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            Assumptions
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        may distort the outcome when you assume
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            Dinosaur
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        One of Earth's most successful ; diverse branches of life.  Mesozoic Era
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            Mesozoic Era
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        lasted for ~180 Ma
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            Tetrapod
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        four limbs
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            Paleontology
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        The study of ancient life, including the evolution of organisms ; their interactions with each other ; their environments. (a minor)
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            Preserved
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        skeletons are still made of bone
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            Fossil
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        remains of once-living organisms (anything dug out of the ground, to dig in the ground- word origin)
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            Anatomy
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        how skeletons are constructed ; information about the animals
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            Extinction
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        is the discontinuation of the evolution of a branch of life, caused by climate change.
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            Historical Science
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        tries to describe the past ; explain the causes of past phenomena, rather than create experiments to observe effects.
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            Geology
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        study of earth (rocks, what they are comprised of and how they change)
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            Biology
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        The study of life
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            Archeology
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        study of the artifacts left behind by humans
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            Comparative anatomy
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        comparison of bones between very different organisms
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            Paleoecology
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        the ecology of fossil animals and plants
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            Vertebrate
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        an animal with a spine
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            Invertebrate
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        an animal without a spine
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            Eon
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        major division of geological time, subdivided into eras
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            Era
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        subdivision of an eon--> periods
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            Period
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        subdivision of an era
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            Epoch
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        subdivision of a period
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            Phanerozoic
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        Eon
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            Paleozoic
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        Era
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            Mesozoic
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        Era
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            Cenozoic
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        Era
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            Triassic
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        Period (began 248Ma)
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            Jurassic
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        Period
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            Cretaceous
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        Period (ended 65 Ma)
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            Cambrian
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        Period
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            Tertiary
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        Period
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            Permian
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        Period
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            ****Lecture two colorful chart on periods and eras
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        got to moodle
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            Apatosaurus
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        Sauropodomorpha-Sauropoda 157-146 Ma (J)
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            Brachiosaurus
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        Sauropodomorpha-Sauropoda 156-145 Ma (J)
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            Oviraptor
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        Theropoda-Coelurosauria 88-70 Ma (K)
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            Velociraptor
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        Theropoda-Coelurosauria 88-85 Ma (K)
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            Tyrannosaurus
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        Theropoda-Coelurosauria 85-65 Ma (K)
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            Allosaurus
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        Theropoda- Carnocauria 154-144 Ma (J)
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            Iguanodon
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        Ornithopoda  135-125 Ma (K)
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            Parasaurolophus
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        Ornithopoda  76-74 Ma (K)
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            Maiasauria
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        Ornithopoda  80-65 Ma (K)
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            Stegosaurus
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        Thyrephorans 156-140 Ma (J)
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            Ankylosaurus
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        Thyrephorans 70-65 Ma (K)
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            Triceratops
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        Marginocephalians 72-65 Ma (K)
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            Pachycephalosaurus
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        Marginocephalians 76-65 Ma (K)
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            body fossils
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        fossils made of hard parts such as shells, teeth, bones, woody trunks, branches, and stems
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            Lagerstatten environment
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        sedimentary deposit that exhibits extraordinary fossils with exceptional preservation
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            Lagerstatten fossils
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        preserved soft tissues
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            Trace fossils
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        impressions or other preserved signs of life (footprints, tracks, burrows, feces, etc.) rather than the actual body of the animals
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            geochemical evidence
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        organic molecules are evidence of biological activity, environmental changes, relationships between fossils and body color
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            Metamorphism
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        altering of the composition or structure of a rock by heat, pressure, or other natural agency
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            Fossil record
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        history of life as documented by fossils
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            Bias in the fossil record
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        hard parts, environment-burial, low oxygen, minerals, timing, human preference
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            types of fossilization
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        Permineralization, replacement (cast and mould), Compression, Trace, Resin
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            Permineralization
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        when mineral deposits form internal casts of organisms
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            Replacement (cast and mould)
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        cast-flesh decays and bones deteriorate due to chemical reactions; minerals gradually enter into the cavity, resulting in a cast Mould-the general form of the original organism
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            Compression
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        a fossil preserved in sedimentary rock that has undergone physical compression. While it is uncommon to find animals preserved as good compression fossils, it is very common to find plants preserved this way.
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            Resin
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        any of various hard natural resins (as amber or some copals) usually found in the earth as exudates of trees long dead.
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            stratigraphy
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        the branch of geology concerned with the order and relative position of strata and their relationship to the geological time scale.
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            stratification
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        Stratigraphy is a branch of geology which studies rock layers (strata) and layering (stratification). It is primarily used in the study of sedimentary and layered volcanic rocks.
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            principals of stratigraphy
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        1) sediment deposited horizontally (original horizontality) ex. grand canyon 2) wide spread layers can be correlated  3)older layers are deposited first and are below younger layers 4) the timeline of the evolution of life is recorded in the fossil record
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            wide spread layer correlation (lateral continuity)
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        all types of one rock were formed at the same time  (navajo rock) and we can assume it's continuous presence in the same place of different national parks examples: grand canyon, zion national park, mesa verde national park
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            layer from bottom to top
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        bottom oldest, top youngest
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            Disturbances
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        tiliting, folding, faulting
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            faunal succession
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        faunal organisms succeed one another in definite and determinable order and therefore any time can be recognized by its fossil content
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            index fossil
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        geographically widespread fossil that is limited to a short span of geologic time, lived everywhere but only existed for a couple million years, bookmark for time
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            relative age of rocks (fossil succession)
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        An English scientist, William Smith is accredited with the discovery of this idea. Smith noticed that specific forms of life were fossilized in particular layers of rock, giving a time line story indicating when, in time, events occurred. This progression of or evolution of life occurred in a vertical fashion up through the layers. The same vertical changes in fossils occur in different places all over the earth.
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            radiometric dating
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        gives us ABSOLUTE (approximate numerical) ages (plus or minus some years)
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            igneous (volcanic)
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        most easily dated (first type of rock on earth), can be dated to the age of magma solidification
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            metamorphic
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        sometimes can be dated, but to time of metamorphism, not formation of original parent rock
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            sedimentary
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        usually can't be dated, any date is from the age of the parent, not the deposition of the sediment
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            weathering
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        breaking up of surfaces by air and water
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            erosion
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        the transportation of broken clasts, mostly by wind and water, also gravity
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            deposition
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        broken clasts settle at lower elevations as depositional landforms
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            biochemical
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        death and accumulation of organisms (mostly in the ocean)
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            sedimentary classes
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        clastic, chemical, biogenic
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            clastic
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        sediment is loose fragments of rock debris produced by physical weathering (sand and clay), most fossils formed here
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            chemical
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        sediment precipitates from solution in water (calcium carbonate and salt)
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            biogenic (life generated)
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        composed of the remains of plants or animals = organics, very rarely well preserved (coal, oil, natural gas)
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            sedimentary accumulation
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        =deposition
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            lithification
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        cementing together of sediments after burial
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            sandstone
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        sand accumulates on beaches, in/near water, in deserts
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            siltstone
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        silt accumulates mostly on beaches, in/near water, more detailed fossils
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            shale (mudstone)
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        mud accumulates mostly in/near water, more detailed than siltstone
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            limestone
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        made out of organisms from the ocean , accumulates in shallow seas-mostly microscopic dead sea creatures
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            volcanic ash (clastic igneous) -broken pieces of magma
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        ash accumulates on land/in water as it falls from the sky, during/after a volcanic eruption
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            Mesozoic rocks in North America
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        more cretaceous than Jurassic and Triassic -Montana, Utah, Texas, Nebraska, Wyoming
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            fossilization
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        during lithification bone becomes rock (sometimes)
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            5 fabulous fossilizers
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        1) shale (mud) 2) siltstone 3) sandstone 4) limestone 5) volcanic ash
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            crust
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        continental(less dense), oceanic (more dense), when you have an oceanic crust hitting a continental crust the oceanic crust will always go under
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            3 types of plate boundaries
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        1. Divergent (constructive) 2. Convergent (destructive) 3. Transform (conservative)
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            plates
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        -16 plates on earth, 90% earthquakes on plate boundaries
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            convergence-destructive
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        plates moving against each other causing subduction
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            divergence-constructive
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        plates are moving away from each other, new land is constructed by magma in the ocean, how pangaea separated
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            transform-conservative
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        ex. San Andreas fault, earthquakes happen but the plate is not being destroyed
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            continental plate
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        less dense than oceanic plate
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            oceanic plate
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        more dense than continental plate
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            earthquakes
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        movement of plates cause earthquakes (move next to each other)
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            volcanism
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        movements of plates cause volcanism between the plates (divergence)
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            mountain-building
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        movement of plates cause mountain building (convergence)
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            mid-ocean ridge
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        a divergent plate boundary, magma rising from mantle forms new crust, called this because most divergent boundaries meet in the middle of the atlantic, where continents break apart and move away from each other
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            age of ocean floor
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        -ocean is youngest at Mid-Ocean Ridge and older as the magma spreads outward, symmetric spreading out from the plate
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            atlantic ocean formation
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        pangaea separates due to divergent plates first with north american and Europe separating then south america and africa
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            plate tectonic evidence
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        1.glaciers: appear to move from sea to land 2.mountain belts dissected  3.hot spot volcanoes: crust moves over hotspot magma source which is stationary relative to the mantle 4.fossils  5.earthquake epicenter locations 6. active volcano locations 7.GPS
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            triassic plate tectonics
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        when pangaea starting to break up,
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            jurassic plate tectonics
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        -more division, atlantic ocean is getting wider,
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            cretaceous plate tectonics
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        -pangaea is almost all split up
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            ocean-continent convergence
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        dense oceanic crust formed at the MOR descends into the mantle at subduction zone trenches, forming a volcanic arc (ex. northwest US cascade volcanic range and andes volcanic range)
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            ocean-ocean convergence
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        when 2 oceanic plates meet 1 of them is always denser and subjects beneath the other forming a volcanic island arc
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            continent-continent convergence
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        continental crust can't subduct but is forced upwards during the collision ex. how the himalayas formed
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            What technique is used to determine the age of rocks by looking for radioactive elements that decay predictably?
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        radioactive dating
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            Water accumulates on Earth. Where did it come from?
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        Comet/asteroids/meteoroids
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            90% of the Earth was a vast iron-rich ocean with small volcanic islands. Is this ancient atmosphere favorable to complex life forms, like humans? What does it look like?
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        No. It was heavy, dense, carbon dioxide rich, very hot, and reddish in color
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            Where did the first life evolve on Earth?
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        primitive single-celled organisms lived off of the heat of ocean flood volcanic vents (and still exist today)
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            With the formation of the photo-continents, the shallow seas along the coastal margins were inhabited by __________, which are made of layers of __________. Through the process of photosynthesis they _______________ Earth's atmosphere.
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        Stromatolites; algae; oxygenated (technically cyanobacteria is the organism and Stromatolites are the rocky waste products of the cyanobacteria)
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            Oxygen first filled the __________ and then filled the __________ and cleared the air.
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        oceans; atmosphere
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            What is one of the primary lines of evidence that the continents are not stationary?
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        fossil locations of species (like trilobites) that lived in fresh water on the opposite sides of today's oceans
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            What fossils provide the greatest argument for continental drift?
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        trilobites
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            The first global maps of the ocean floor were created by the Navy in WW2 and revealed _________________, __________________ and __________________.
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        rifts, trenches and plate boundary network
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            How fast do plates move on average?
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        2.5 cm or 1 inch per year
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            Which hemisphere was the supercontinent Rodinia formed? What were some characteristics of this continent?
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        S. hemisphere barren and lifeless
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            What triggered Snowball earth?
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        The supercontinent Rodinia blocked warm ocean currents, which caused temperatures to freeze in the Polar regions and ice covered the earth.
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            During Snowball Earth, surface temperatures were ____________ and the ice was ______________ deep. This killed most life.
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        -a mile deep
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            What splits Rodinia?
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        excessive volcanism, which causes the Earth to warm and the ice to melt
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            Excessive volcanism triggers a temporary _____________ effect. New smaller continents diverge.
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        greenhouse
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            The Cambrian Explosion marks a huge increase in a variety of life forms in the oceans. Many fossil organisms are found today in the Burgess ___________, providing evidence of life developing teeth, eyes, and skeletons.
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        shale
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            Oxygen levels reach today's levels and the ___________ forms in the upper atmosphere, providing a UV radiation shield.
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        ozone layer
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            Life emerges on land. The warm climate triggers rapid plant growth, creating a green swampy tropical world. The evidence of excessive plant life in fresh water swampy regions is found in ______________ deposits, which are accumulated partially decomposed plant matter.
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        coal
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            Shallow waters teamed with life and preserved these organisms in the form of _______________.
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        oil and gas
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            What were the first animals to evolve on land? Followed by ________________ then __________________.
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        enormous insects; amphibians; reptilians
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            What happened to cause a mass extinction of 95% of life on Earth?
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        Eruption of a mantle plume of lava in modern Siberia that released a million cubic miles of lava for over 1 million years, poisoning the atmosphere with noxious gases
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            The supercontinent Pangaea forms and oxygen returns to high levels in the atmosphere. Dinosaurs appear on Earth. What fraction of the history of life on Earth was dominated by dinosaurs?
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        1/3
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            What was the average size of a dinosaur?
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        larger than a grizzly bear
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            What does the word dinosaur mean?
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        terrible lizard
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            What may be the reason(s) that the dinosaurs grew to such enormous sizes?
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        dinosaurs were lukewarm blooded, and/or the sweltering oxygen-rich environment triggered by volcanism
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            Why was there such an increase in volcanism?
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        the supercontinent Pangaea was beginning to break apart
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            Which continents did the dinosaurs end up on when paleocontinents Gondwanaland and Laurasia form and split into the 7 continents we know today?
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        all of them
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            Volcanism increased CO2 levels in the atmosphere (global warming gone wild), which allows plants to grow fast and big. This allows dinosaurs to ______________.
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        get extremely large, a biological response to a volcanically overreactive planet
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            What triggered the creation of diamond found in South Africa. Formed through volcanic eruptions 3x deeper than usual.
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        triggered by the break-up of the Pangaea supercontinent
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            Dinosaur bones are found continuously throughout the sedimentary record from about _____________ up to ______________.
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        230Ma; 65Ma
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            What percentage of species went extinct at the end of the Mesozoic?
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        Over 70% of the species on Earth
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            What rock is the 65Ms tombstone layer made of?
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        Clay (shale) - sedimentary rock
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            What exceptionally rare element is found in the tombstone layer?
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        Iridium
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            Where does most of this element come from?
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        Space rock (meteorites and asteroids)
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            What is proposed to have caused the extinction?
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        asteroid/comet impact
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            How big was the crater? Where was it found?
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        ;100 miles across and is located in the Gulf of Mexico
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            How much iridium was deposited on Earth by the space object impact?
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        ~200,000 tons of iridium
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            How big was the meteor (actually meteoroid or asteroid or comet) that hit Earth 65Ma?
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        over six miles in diameter
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            How fast was the space object moving when it hit Earth?
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        20 km/second= 12.4 miles/second= 744 miles/minute
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            What other events occurred at the same time and contributed to the extinction? (65Ma)
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        Indian lava flows produced poisonous gases that choked the atmosphere
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            Emerging land
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        tectonic uplift or falling sea level= erosion and no fossilization 1) erosion: surface being decomposed and transported to lower elevations 2) uplift: tectonic process land rising it elevation (plate collisions or inflation due to magma rising from below) 3) falling sea level: lowering due to colder atmospheric temperatures (ice forms) and/or decrease in rate of divergence
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            Submergent land
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        tectonic subsidence or rising sea level= deposition and fossilization 1) deposition: clasts from higher elevations are transported to these lower elevations where clasts accumulate and are buried 2) subsidence: tectonic process of land decreasing in elevation (plate divergence or tectonically quiet) 3) rising sea level: increasing due to warmer atmospheric temperatures (ice melts) and/or increase in rate of divergence
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            The role of water
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        water weathers(decomposes), erodes(transports), and ultimately flows to lower elevations where class are deposited on to flatter landforms
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            Sedimentary (depositional) environments
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        where sedimentary clasts accumulate. Type of environment determines the types of sedimentary that accumulate
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            Sedimentary structures and ancient environments
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        type of sedimentary structures: strata or beds (=layers), cross-bedding (=desert), graded beds (=deep water), ripple marks (=water body), mud cracks (=drying mud), fossils (=life) IMPORTANT: provide information about the environment
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            Where to look for dinosaurs...
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        areas that were depositional over most of the last 245Ma (Mesozoic and Cenozoic eras) and have recently eroded, exposing Mesozoic Era sedimentary layers to the earth's surface.
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            Global climate change
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        -constant through time, changed by life for almost 4 billion years, change in atmosphere temperature= ocean temperature= amount of ice= sea level= weather patterns and intensity, some life adapts, some die (extinction), some thrives
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            Causes of natural climate variability
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        -atmospheric temperature, atmospheric composition, amount of greenhouse gas, ocean temperature, albedo(surface area of ice), sea level, ocean circulation change, variations in solar activity, landmass distribution (tectonic), mountain building (tectonic), volcanic activity (tectonic), meteorite/comet impacts, release of clathrates (methane)
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            greenhouse effect
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        earth absorbs short-wave radiation (UV) and emits long-wave radiation (infrared heat) Heat which is absorbed by atmospheric gages, warming earth by 33 degrees Celsius.
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            greenhouse gases
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        Natural greenhouse gases: CO2, O3, H2O vapor, NO2, methane CH4 Human created greenhouse gases: chlorofluorocarbons (CFCs)
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            How did life begin?:
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        CHON (carbon, hydrogen, oxygen and nitrogen), organic compounds, cells, metabolize (extract energy), membrane boundary (lipids), make copies, emergence, seeding, procreate (amino acids/proteins=RNA/DNA)
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            Where did life begin?
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        -1.primoridial soup: water + lightning + ancient atmosphere, 2.hydrothermal vents: deep-sea volcanic vents at high temperatures and pressures 3.Clays: surface charges concentrate organic molecules
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            Evidence of evolution
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        1) Inheritance- genetic traits are inherited from parent and are passed on to offspring 2) Selection- organisms with traits that are favorable to their survival live and pass on their genes to the next generation 3) Variation- all life forms vary genetically within a population. Selection uses this genetic variation.  4) Time- evolution takes time. Evolution can happen in a few generations, but major changes, such as speciation, usually take long periods of time.
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            Keys to survival
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        procreation, mutations, specialized traits, predatory skills or herbivore strategies, and natural selection
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            Megafauna
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        extremely large animals
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            Mesozoic Era Evolution: P-T mass extinction, K-T mass extinction
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        -middle life, gymnosperms (cycads, confers, and ginkgo) were dominant trees, later angiosperms evolve, first dinosaurs, pterosaurs, mammals, birds, "Age of Reptiles" most dominant and diverse: carnivorous, and herbivorous dinosaurs, marine reptiles, pterosaurs, other non-dino reptiles, birds (in the jurassic), ended with mass extinction 75% of all species
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            Animals that evolved alongside dinosaurs
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        Marine reptiles pterosaurs mammals turtles lizards birds
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            reptiles
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        Anapsid(no fenestra): amphibians and turtles(exist), synapsid (1 low fenestra): mammal-like reptiles (lived Permian to triassic-extinct), euryapsid (1 high fenestra):marine reptiles (mostly Mesozoic-extinct), diapsid (2 fenestra):lepidosaurs (exist) and archosaurs (some exist)
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            Dinos: hips, breathing, endothermy
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        -diverged from archosaurs, hips adapted to bring their legs directly under torso, efficient breathing while walking/running, adaptation favors endothermy (body temperature control)
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            Earliest dino-eoraptor
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        -first dinosaurs were small, about 1m, bipedal predator/insectivore, terrestrial (walker/runner)
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            Cenozoic Era Evolution: Angiosperms, mammals
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        -"Age of the Mammals": 2 groups; marsupials and placentals, some groups become very large, "Age of Flowering Plants": angiosperms strongly influenced evolution of birds and herbivorous mammals, reptiles that survived the K-T extinction included: turtles, snakes, lizards, birds