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Origin of Earth’s Ocean Origin of Earth’s Ocean Scientific Observations and Explanations on the Scientific Observations and Explanations on the Origin and Evolution of Earth’s Ocean Origin and Evolution of Earth’s Ocean Introductory Oceanography Introductory Oceanography Ray Rector - Instructor
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Origin of the Ocean -Spring2015 - SeaSciSurf Home Page of H20 2) Comet Impacts ... in the Ocean? 1) Earliest life forms found are ... Found in both shallow and Stromatolites Microfossils

Mar 07, 2018

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Page 1: Origin of the Ocean -Spring2015 - SeaSciSurf Home Page of H20 2) Comet Impacts ... in the Ocean? 1) Earliest life forms found are ... Found in both shallow and Stromatolites Microfossils

Origin of Earth’s OceanOrigin of Earth’s OceanScientific Observations and Explanations on the Scientific Observations and Explanations on the

Origin and Evolution of Earth’s OceanOrigin and Evolution of Earth’s Ocean

Introductory OceanographyIntroductory OceanographyRay Rector - Instructor

Page 2: Origin of the Ocean -Spring2015 - SeaSciSurf Home Page of H20 2) Comet Impacts ... in the Ocean? 1) Earliest life forms found are ... Found in both shallow and Stromatolites Microfossils

Preview of TopicsPreview of Topics

�� The Scientific MethodThe Scientific Method

�� Origin Origin of the of the Universe Universe –– Forces, Energy, Matter, SpaceForces, Energy, Matter, Space

�� Origin of the Solar SystemOrigin of the Solar System

�� Origin of EarthOrigin of Earth--Moon SystemMoon System�� Origin of EarthOrigin of Earth--Moon SystemMoon System

�� Origin of the Ocean and AtmosphereOrigin of the Ocean and Atmosphere

�� Origin of LifeOrigin of Life

�� The Age of the EarthThe Age of the Earth

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The Scientific Method The Scientific Method –– Heart of ScienceHeart of Science

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Investigation and Application of the Investigation and Application of the Scientific MethodScientific Method

Page 5: Origin of the Ocean -Spring2015 - SeaSciSurf Home Page of H20 2) Comet Impacts ... in the Ocean? 1) Earliest life forms found are ... Found in both shallow and Stromatolites Microfossils

Investigation Investigation and Application of the and Application of the Scientific MethodScientific Method

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THE SCIENTIFIC METHODTHE SCIENTIFIC METHOD

The Basic ComponentsThe Basic Components

�Empirical Observations

� Questions / Problems

� Hypotheses / Models

6

� Predictions

� Tests / Experiments

� Analysis of Results

� Draw Conclusions

� Reevaluate Hypothesis

Note: Scientific method is NOT a Recipe – it’s a Cyclic Process

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EmpiricalEmpirical Observations: Basis of All Observations: Basis of All Scientific Studies and TheoriesScientific Studies and Theories

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EmpiricalEmpirical Observations: Observations: Basis of All Basis of All Scientific Studies and TheoriesScientific Studies and Theories

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Hypotheses and Scientific TestingHypotheses and Scientific Testing

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ObservationsObservations and and

PredictionsPredictions

1) A hypothesis is a proposed explanation, model, or prediction

of nature that requires testing (attempt to falsify or confirm).

2) Hypotheses are based on empirical physical evidence (data).

3) Hypotheses must be falsifiable (testable/predictable).

TestingTestingHypotheses Hypotheses andand TheoriesTheories

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3) Hypotheses must be falsifiable (testable/predictable).

4) Hypotheses can never be proven as an absolute fact.

5) Hypotheses are always open to elimination or modification.

6) A theory is a broad, elegant, set of unifying explanations of a

set of otherwise unconnected natural phenomena.

7) A theory is established by the interconnection (framework) of

well-tested and confirmed hypotheses that are, in turn,

supported by an enormous amount of physical evidence.

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Testing Your HypothesisTesting Your Hypothesis

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Scientific Scientific PredictionsPredictions

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Scientific Scientific ModelingModeling and and PredictingPredicting

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Purpose of Modeling:Purpose of Modeling: Understand and predict how

parts of the Earth operate and interact with each other

--- Start simple and get more complicated over time

--- Add more and more parameters over time

--- Test computer models with real historic data

---- Develop and refine models to predict future scenarios

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A Twisted COSMIC TimescaleA Twisted COSMIC TimescaleA Twisted COSMIC TimescaleA Twisted COSMIC TimescaleA Twisted COSMIC TimescaleA Twisted COSMIC TimescaleA Twisted COSMIC TimescaleA Twisted COSMIC Timescale

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The Visible and Invisible UniverseThe Visible and Invisible Universe

The Basic ComponentsThe Basic Components�� Expanding SpaceExpanding Space�� 4 Fundamental Forces4 Fundamental Forces�� Energy Energy -- EMREMR�� MatterMatter�� Dark energyDark energy�� Dark MatterDark Matter

13.7 Billion Years of Creation and Destruction13.7 Billion Years of Creation and Destruction

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How Much Stuff Is Out There?How Much Stuff Is Out There?

The Rough Stats:The Rough Stats:1) Size1) Size: 30 x 10: 30 x 1099 cubic light yearscubic light years

�� 1x101x1066 light yrs between galaxieslight yrs between galaxies

2) Matter2) Matter: 100 billion galaxies: 100 billion galaxies

�� 1.6 x 101.6 x 106060 kilogramskilograms

�� Position in the sky and the extent of the magnification Position in the sky and the extent of the magnification

Hubble Deep Field ImageHubble Deep Field Image

Every spot

of light is a

galaxy!

@ 1.4 kg per cubic meter@ 1.4 kg per cubic meter

3) Only3) Only 0.0000000000000000000042 % 0.0000000000000000000042 %

of the universe contains any matterof the universe contains any matter

�� It’s a SUPER empty place!It’s a SUPER empty place!

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Survey of Elements Found in NatureSurvey of Elements Found in Nature

Cosmic Abundances of Elements

� 92 Naturally-occurring elements

� Mostly Hydrogen and Helium

� Lots of Carbon, Nitrogen, Oxygen,

Silica, Sulfur, and common metals

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BIG BANG Theory BIG BANG Theory -- 14 Billion Years of Cosmic Evolution14 Billion Years of Cosmic Evolution

?

The Big Bang The Big Bang ElementsElements

�� HydrogenHydrogen�� HeliumHelium

?

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Galaxies Galaxies –– Gigantic Star ClustersGigantic Star Clusters

�� Galaxies are “island universes” where Galaxies are “island universes” where stars are born, live and die stars are born, live and die

�� Gravity is the controlling force on galaxy Gravity is the controlling force on galaxy formation and evolutionformation and evolution

�� Universe contains roughly 100 billion Universe contains roughly 100 billion starsstars

�� Typical galaxy contains 100 billion starsTypical galaxy contains 100 billion starsCircus of Galaxies

Key Points:Key Points:

�� Typical galaxy contains 100 billion starsTypical galaxy contains 100 billion stars�� A typical star located in a galaxy is much A typical star located in a galaxy is much

like our Sunlike our Sun�� Stars generate new elements during Stars generate new elements during

fusion and novafusion and nova�� All elements except for the very light All elements except for the very light

ones can only form inside starsones can only form inside stars�� Our galaxy Our galaxy –– the Milky Way the Milky Way –– looks very looks very

much like our neighbor much like our neighbor –– the Andromeda the Andromeda galaxy.galaxy.

Andromeda Galaxy

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Our Very Own Island UniverseOur Very Own Island Universe

�� Milky Way Galaxy is 100 Milky Way Galaxy is 100 million light in diametermillion light in diameter

�� Our galaxy contains Our galaxy contains roughly 400 billion starsroughly 400 billion stars

Sun is a very typical star Sun is a very typical star

Milky Way GalaxyMilky Way Galaxy

�� Sun is a very typical star Sun is a very typical star located in one of the arms located in one of the arms of the Milky Way Galaxyof the Milky Way Galaxy

�� Other planetary systems Other planetary systems have been found in our have been found in our galaxygalaxy

We are

here

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Nebula Nebula –– Star NurseriesStar Nurseries�� Nebula are regions of dense Nebula are regions of dense

hot gases, stellar debris, and hot gases, stellar debris, and very young starsvery young stars

�� New stars and planetary New stars and planetary systems form from the both systems form from the both primordial matter and the primordial matter and the primordial matter and the primordial matter and the remnants of exploded stars remnants of exploded stars within nebulawithin nebula

�� Our solar system most likely Our solar system most likely formed in a nebula much like formed in a nebula much like this onethis one

�� Condensation Theory for Condensation Theory for star and planet formationstar and planet formation

Carina Nebula

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Observed Stellar Systems in the MakingObserved Stellar Systems in the Making

Observations of Newly Observations of Newly

Forming Stars Within a Forming Stars Within a

Nebula CloudNebula Cloud

The Trifid NebulaCondensation TheoryCondensation Theory

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Stellar Fusion Stellar Fusion –– The Element FactoryThe Element Factory

1) Normal Star

The Fusion ProcessThreeThree--Stage Star EvolutionStage Star Evolution

1) Normal Star

= Helium

3) Red Supergiant Star

= Neon through Iron

2) Red Giant Star

= Carbon

Note: Stellar fusion processes can generate light to medium weight elements: from Helium (He) all the way up to Iron (Fe).

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Supernova Supernova –– Heavy Element FactoryHeavy Element Factory

A Stellar ImplosionA Stellar Implosion––Explosion EventExplosion Event

Supernova

Process

Collapse of Red Supergiants

Tycho-supernova

Note: Supernova events generate medium-to heavyweight elements: from Iron (Fe) all the way up to Uranium (U)

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Planet Formation: Planet Formation: The Nebula The Nebula

Condensation TheoryCondensation Theory

Animation1

Animation2

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We are

here Our Solar SystemOur Solar System

4 Inner Planets

� Mercury

� Venus

� Earth

� Mars

4 Outer Planets

� Jupiter

� Saturn

� Uranus

� Neptune

What

about

poor little

Pluto?

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We are

here

Our Solar SystemOur Solar System

Poor little

Pluto

demoted to

Dwarf

Planethere Planet

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Origin of the MoonOrigin of the MoonMultiple Theories

� Twin Planet Theory

� Moon Capture Theory

� Earth-Birthed Theory� Earth-Birthed Theory

� Giant Impact Theory

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Most Likely Origin of the Moon

Giant Impact Theory

Impact Sequence of Earth

and Mars-size Body

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Density Differentiation of Young EarthDensity Differentiation of Young EarthDensity Differentiation of Young EarthDensity Differentiation of Young EarthDensity Differentiation of Young EarthDensity Differentiation of Young EarthDensity Differentiation of Young EarthDensity Differentiation of Young Earth

� Proto-earth was homogenous

� Proto-earth underwent complete

melting due to accretion energy and

radioactive decay

EarlyEarly--stage Differentiation Modelstage Differentiation Model

radioactive decay

� Heaviest elements sank down to

form core – mainly iron and nickel

� Medium weight elements formed

mantle and crust– mainly silicate

minerals

� Lighter elements floated up to form

ocean and atmosphere

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Terrestrial Planet ComparisonTerrestrial Planet Comparison

� Earth and Venus very similar in overall size and composition

� Mars much smaller, with cooler interior

� Each planet has unique crustal characteristics, in terms of

temperature, crustal composition and processes,

atmospheres, and water.

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Composition and Structure of EarthComposition and Structure of Earth

Five Chemically

Distinct Layers

Eight Physically

Distinct Layers

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Formation of the Earth’s Ocean Formation of the Earth’s Ocean and Atmosphere and Atmosphere

1) The Origins of Earth’s

Atmosphere and Ocean are

Closely Tied Together

2) The Composition of the 2) The Composition of the

Atmosphere Has Greatly

Changed Over the Last

Four Billion Years

3) The Composition of Ocean

Initially Changed Over the

First Billion Years But Has

Since Remained Stable

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Evolution of Earth’s AtmosphereEvolution of Earth’s Atmosphere

Three StagesThree Stages

1) Primordial Atmosphere ???

� Hydrogen and helium from original condensed nebula

� Probably stripped away by early solar wind and heating

2) Secondary Atmosphere2) Secondary Atmosphere

� Volcanic outgassing of volatiles from inside planet

� Primarily water and carbon dioxide with sulphuric and

hydrochloric acid, and methane

� No free oxygen – a nasty, poisonous, acidic mixture

3) Modern Atmosphere

� Modification of earlier atmosphere by life processes

� Removal of carbon dioxide and enrichment of free oxygen

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Terrestrial Atmosphere ComparisonTerrestrial Atmosphere Comparison

Venus MarsEarth

Venus atmosphere

super thick, hot

and nearly all CO2

Mars atmosphere

super thin, cold and

nearly all CO2

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The Oxygen The Oxygen

RevolutionRevolution

1)1) Photosynthetic marine bacteria Photosynthetic marine bacteria

begin releasing oxygen (Obegin releasing oxygen (O22) into ) into the ocean and the atmosphere the ocean and the atmosphere by 3 billion years agoby 3 billion years ago

Photosynthesizing Photosynthesizing

2) By about 2 billion years ago, sufficient 2) By about 2 billion years ago, sufficient

OO22 in atmosphere to oxidize (rust) rocksin atmosphere to oxidize (rust) rocks

� Protects Earth’s surface from ultraviolet solar radiationProtects Earth’s surface from ultraviolet solar radiation

Photosynthesizing Photosynthesizing

CyanobacteriaCyanobacteria

3) Also by 2 billion years ago, protective ozone (O3) Also by 2 billion years ago, protective ozone (O33) layer ) layer

built up in atmospherebuilt up in atmosphere

4) By about 500 million years ago, O4) By about 500 million years ago, O22 levels in atmosphere levels in atmosphere

approach today’s levelsapproach today’s levels

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Original Sources of Ocean WaterOriginal Sources of Ocean Water

Two Primary SourcesTwo Primary Sources

1) Volcanic Outgassing

� Majority? of H20

2) Comet Impacts

� Minority? Amount� Minority? Amount

Outgassing of Interior

Comet Strikes

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Water from OutgassingWater from Outgassing

Majority Primary Source = Volcanic Outgassing

Composition of volcanic

gases for three volcanoes

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Terrestrial Atmosphere ComparisonTerrestrial Atmosphere Comparison

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Formation of Our OceanFormation of Our OceanThree Phase HistoryThree Phase History

1) Initially there was only water Initially there was only water

vapor in atmospherevapor in atmosphere – Air and

ground surface too hot for liquid

2) Cooling of atmosphere led to Cooling of atmosphere led to

1)

2) Cooling of atmosphere led to Cooling of atmosphere led to

condensation and raincondensation and rain – Ground

surface still too hot for pooling

3) Further cooling of ground Further cooling of ground

surface finally led to the surface finally led to the

accumulation of liquid water on accumulation of liquid water on

surfacesurface – Ocean formed by 4 billion

years ago

2)

3)

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Timeline of Earth’s First Billion YearsTimeline of Earth’s First Billion Years

� First Organisms

� End of Bombardment

� Oldest Existing Rocks� Oldest Existing Rocks

� Formation of Ocean

� Formation of Moon

� Formation of Earth

and Solar System

You Tube VideoYou Tube VideoYou Tube VideoYou Tube Video

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The Origin of Life on EarthThe Origin of Life on Earth

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Why Life on Earth?Why Life on Earth?

Mars

Venus

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Did Life Start Did Life Start in the Ocean?in the Ocean?

1) Earliest life forms found are 1) Earliest life forms found are fossilized bacteria in rocks dated fossilized bacteria in rocks dated 3.5 billion years old.3.5 billion years old.

2) Found in both shallow and 2) Found in both shallow and

Stromatolites Microfossils

2) Found in both shallow and 2) Found in both shallow and deep ocean sedimentary rocks.deep ocean sedimentary rocks.

3) Exposed land surfaces back 3) Exposed land surfaces back then were barren and hellish.then were barren and hellish.

4) The ocean was much milder, 4) The ocean was much milder, particularly the deep ocean.particularly the deep ocean.

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Conditions for Sparking LifeConditions for Sparking LifeLab ExperimentsLab Experiments

1) Simulate early Earth conditions

2) Formed life-giving organic chemicals

3) No actual life created

4) Still an unsolved mystery4) Still an unsolved mystery

Comet Impacts?Comet Impacts?

5) Recent studies point to comet impacts

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Most Likely Cradle for Life on Earth?Most Likely Cradle for Life on Earth?

Deep Sea Hydrothermal Vents?Deep Sea Hydrothermal Vents?

� Warm, water-rich environment

� Chemical-rich volcanic fluids

� Protected from harsh surface

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Life and the Geological TimescaleLife and the Geological TimescaleKey Ideas:Key Ideas:

�� Originally based on Originally based on

relative dating and use relative dating and use

of ageof age--specific fossils specific fossils

�� Periods separated Periods separated

by mass extinctions by mass extinctions

�� Numeric ages from Numeric ages from �� Numeric ages from Numeric ages from

radiometric analysis of radiometric analysis of

igneous rocks found igneous rocks found

between fossil layersbetween fossil layers

�� First life forms occur First life forms occur

3.5 billions years ago3.5 billions years ago

�� MultiMulti--cellular marine cellular marine

life established 600 life established 600

million years agomillion years agoYou Tube VideoYou Tube VideoYou Tube VideoYou Tube Video

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The Twisted Geological TimescaleThe Twisted Geological TimescaleThe Twisted Geological TimescaleThe Twisted Geological TimescaleThe Twisted Geological TimescaleThe Twisted Geological TimescaleThe Twisted Geological TimescaleThe Twisted Geological Timescale

Video Review of Big Bang to Present Day - YouTube

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Class DiscussionClass Discussion

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Review of Study TopicsReview of Study Topics

�� Origin Origin of Universe of Universe –– Forces, Energy, Matter, SpaceForces, Energy, Matter, Space

�� Origin Origin of the Solar Systemof the Solar System

�� Origin of EarthOrigin of Earth--Moon SystemMoon System

�� Origin of the AtmosphereOrigin of the Atmosphere

�� Origin of the Ocean Origin of the Ocean

�� Origin of the LifeOrigin of the Life

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Preparation for Next MeetingPreparation for Next Meeting

Next Meeting TopicsNext Meeting Topics

1) Age of Earth1) Age of Earth

2) Earth Physiology2) Earth Physiology

3) Continental Drift Hypothesis3) Continental Drift Hypothesis

4) The Plate Tectonic Theory4) The Plate Tectonic Theory4) The Plate Tectonic Theory4) The Plate Tectonic Theory

Homework Assignment:Homework Assignment:� Read Chapter 2 in Textbook

� Study the Instructor’s Website

@ www.oceansci.com

� Lecture Notes

� PowerPoint

� EV Videos 3 and 4

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Continental Drift HypothesisContinental Drift Hypothesis

Alfred Wegener (1880-1930)