Intro to earth science definitions

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34 Terms

1
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Protosomes

Mouth develops from the blastopire during embryonic development

e.g. molluscs, arhtropods, annelids

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Deutrosomes

Anus develops first

e.g echinoderms, chordates

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The three domains in the tree of life are..

Bacteria, Archaea, Eukarya

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The origin of life from non-living matter is..

Abiogenesis

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One model for the evolution of eularyotes from prokaryotes is..

The endosymbiotic theory of cell evolution

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The boundary between the Hadean and Archaea is at…

4.0Ga

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Different stable isotopes of an element are defined on the basis of..

Variation in the no. of neutrons in the nucleus of the atom

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(a) A = marine bicarbonate B = atmospheric Co2 C = living autotrophic organisms

This is due to the fact that living organisms (photosynthesis - plant, algae..rewuires less energy for them) have a more negative (12C) value than marine bicarbonate, formed from inorganic precipitation of calcium carbonate (CaCO₃) or from organisms with carbonate shells.(13C)

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What is a polymorph of calcium carbonate?

Aragonite

10
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<p>What is the kingdom of animals in order?</p>

What is the kingdom of animals in order?

knowt flashcard image
11
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Vendobionta

Refers to an extinct group of Ediacaran organisms with soft, quilted bodies

12
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Pneu structure

internal structure of an organism with a fluid-filled, inflatable body, like a mattress

13
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Tekites

natural glass objects formed by intense heat and pressure of meteorite impacts

very low water content indicates that it was formed under conditions where water was rapidly driven off, hence HIGH Temperature and HIGH Pressure

14
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Shocked quartz

A form of quartz that has been deformed by intesnet pressure like the bolide (meteorite) impact.

Wide geographic distribution, making it the strongest and most global evidence of a large impact event.

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Suveite

Type of impact breccia only found near the impact site, luke Chicxulub

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Ejecta blanket

Refers to materal ejected around the impact site, not found globally.

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Lazarus taxa

Species or groups that diseappear from the fossil record for one or more periods. Presumed to be decreased population size or poor preseration conditions, later reappearing again.

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Reapperance of an exticnt group is known as

Lazarus taxa

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What is the boradest effect from the K-T boundary between fern spike or tsunami deposit

Fern spike

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Elatina formation, South Australia

Late proerozoic (~634Ma), glacial deposit

Laminated siltstone

Tidal depsoits (e.g. low altitude)

<p>Late proerozoic (~634Ma), glacial deposit</p><p>Laminated siltstone</p><p>Tidal depsoits (e.g. low altitude)</p>
21
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Contributing factor of a cooler planet back then…

  1. Highe albedo → Low albedo. There was more land mass before, and land surfaces had High albedo that reflected 90% of solar radiation back into space, whereas open ocean would absorb at least 94% of sun.

  2. The rise of atmospheric oxygen, reducing methane (potent greenhouse gas) therefore contributing to a cooler earth.

22
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What is geological record of a snowball earth event?

varies in detail

same general stratigraphy

<p>varies in detail </p><p>same general stratigraphy</p>
23
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Stromalites

a calcareous mound built up of layers of lime-secreting cyanobacteria and trapped sediment, found in Precambrian rocks as the earliest known fossils, and still being formed in lagoons in Australasia.

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Cyanobacteria

a division of microorganisms that are related to the bacteria but are capable of photosynthesis. They are prokaryotic and represent the earliest known form of life on the earth.

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Ordovician: 440 mya -> small marine organisms died out Devonian: 365 mya -> tropical marine species extinct Permian: 250 mya -> Largest mass extinction event, many vertebrates Triassic: 210 mya -> more vertebrates which lead to dinosaurs to flourish K-T: 66/65 mya -> dinosaurs were K.O'd and mammals emerged

<p><span style="color: oklab(0.952331 0.000418991 -0.00125992)">Ordovician: 440 mya -&gt; small marine organisms died out Devonian: 365 mya -&gt; tropical marine species extinct Permian: 250 mya -&gt; Largest mass extinction event, many vertebrates Triassic: 210 mya -&gt; more vertebrates which lead to dinosaurs to flourish K-T: 66/65 mya -&gt; dinosaurs were K.O'd and mammals emerged</span></p>
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The three germ layer

Ectoderm = Forms exoskeleton

Mesoderm = Develops into organs

Endoderm = Forms the inner lining of organs

<p>Ectoderm = Forms exoskeleton</p><p>Mesoderm = Develops into organs</p><p>Endoderm = Forms the inner lining of organs</p>
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Difference between diploblastic vs triploblastic

Diploblastic

Triploblastic

Animals are radially symmetric

Animals are bilaterally symmetric

No mesoderm

Mesoderm

No body caivity

Body cavitiy in coelom

Endoderm forms true tissues and the gut

Endoderm forms lungs, stomach, colon, liver, urinary bladder etc.

Ectoderm forms epidermis, nervous tissue and nephridia

Ectoderm forms epidermis, hair, eye lens, brain, spinal cord..

No organs

Organs

Not complex

Complex

EXAMPLES:

Jellyfish, comb jellies, corals and sea anemones

EXAMPLES:

Molluscs, worms, arthropods, echinodermeta and vertebrates

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Small shelly fossils

  • Biomineralised tissue

  • Uncertain affinites and function

  • Microdictvon and Cambroclavus as shields and spines on soft-bodied lobopods (from extinct phylum lobopodia)

  • Defence mechanism = implies there was predation

<ul><li><p>Biomineralised tissue </p></li><li><p>Uncertain affinites and function</p></li><li><p><em>Microdictvon </em>and <em>Cambroclavus</em> as shields and spines on soft-bodied <strong>lobopods </strong>(from extinct phylum lobopodia)</p></li><li><p>Defence mechanism = implies there was predation</p></li></ul><p></p>
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Burgess Shale, Middle Cambrian = Canada

  • deeper water setting

  • series of fossiliferous levels

  • buried in situ below depositing event beds (e.g. avalance)

  • incorpodated into depositing

  • valuable source of data on biodiversity

<ul><li><p>deeper water setting</p></li><li><p>series of fossiliferous levels</p></li><li><p>buried in situ below depositing event beds (e.g. avalance)</p></li><li><p>incorpodated into depositing</p></li><li><p>valuable source of data on biodiversity</p></li></ul><p></p>
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Olenoides

  • Spines on limbs used for capturing and shredding prey

<ul><li><p>Spines on limbs used for capturing and shredding prey</p></li></ul><p></p>
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Leanchoilia

  • mid-gut glands replaced in calcium phosphate

  • digestive function

  • implies macrophagy (feeding of foods large relative to size of organism) and predation/scavenging

<ul><li><p>mid-gut glands replaced in calcium phosphate</p></li><li><p>digestive function</p></li><li><p>implies macrophagy (feeding of foods large relative to size of organism) and predation/scavenging</p></li></ul><p></p>
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Anomalocaris

  • ‘pineapple’ shaped jaw with ‘blades’,

<ul><li><p>‘pineapple’ shaped jaw with ‘blades’, </p></li></ul><p></p>
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Great Oxidation Event (GOE) SUMMARY

  • ~2.4-2.1ga during the Paleoproterozoic era

  • Caused by cyanobacteria producing O via photosynthesis. Began to accumate in the atmosphere and oceans.

  • Before GOE: Earth’s atmosphere had little to no O; methane, ammonia and other gases were dominante.

  • Formation of branded iron formations (BIFs) as oxygen reacted with dissolved iron in oceans.

  • Mass extinction of many anaerobic (oxygen-intolerant) organisms

  • May have been a trigger for ‘‘Snowball Earth’’ glaciations due to methane reduction (potent greenhouse gas)

  • Aerobic life and complex multicellular organisms emerged

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How stromatolies grow

  1. Microorganisms live on the surface of the stromatolite

  2. Sediments deposited on the microorganisms

  3. React by growing upward trhough the sediment, forming a new layer

Modern stromatolies are still growin in Shark bay, Australia

<ol><li><p>Microorganisms live on the surface of the stromatolite</p></li><li><p>Sediments deposited on the microorganisms</p></li><li><p>React by growing upward trhough the sediment, forming a new layer</p></li></ol><p>Modern stromatolies are still growin in Shark bay, Australia</p>