2 OCE 3008_Ch1
Academic Activity
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Introduction to Planet Earth
Quote by Arthur C. Clarke: "How inappropriate to call this planet Earth, when clearly it is Ocean."
Key Concepts in Oceanography
Definition and Significance:
Explore the marine environment and its characteristics.
Oceanography is considered an interdisciplinary science encompassing various fields.
Topics Covered:
Characteristics of Earth’s oceans.
Scientific inquiry and the scientific method.
Understanding the Earth’s age.
Formation of the Earth and Solar System.
Development of Earth’s atmosphere and oceans.
Origin of life thought to be in the oceans.
What is Oceanography?
Overview:
Oceanography is studying the oceans' past, present, and future.
Synonymous with marine science.
Sub-disciplines:
Geological Oceanography/Marine Geology: Study of rocks, processes forming ocean basins, and seafloor structure.
Chemical Oceanography: Composition of seawater and element distribution, impacts of pollutants.
Physical Oceanography: Study of waves, tides, currents, and ocean-atmosphere interactions.
Biological Oceanography: Examination of life forms, their interactions, and adaptations to marine environments.
The World Ocean
Coverage:
Oceans cover 70.8% of Earth’s surface.
Connection to Life:
The origin and development of life are closely linked to the ocean.
Historical Significance:
Oceans have a long history on Earth.
Earth's Water Composition
Saltwater vs. Freshwater:
97.2% of Earth's surface water is seawater; 2.8% is freshwater.
Breakdown of freshwater: 78% trapped in ice and glaciers, 11% in deep groundwater, 11% in surface groundwater.
Less than 1% of freshwater is in lakes and rivers (approx. 0.3%).
Major Oceans of Earth
Overview: The ocean is an interconnected body of water divided into four principal oceans plus the Southern Ocean:
Pacific Ocean: Largest and deepest (3940 m) covering 50.1% of the Earth's oceans.
Atlantic Ocean: 26% of Earth's ocean, shallower than the Pacific at 3844 m depth.
Indian Ocean: 20.5%, primarily in the Southern Hemisphere, similar depth to Atlantic.
Arctic Ocean: Smallest and shallowest (3.4% of Earth's ocean).
Southern Ocean: Circumnavigates Antarctica.
Ocean Zonation
Depth Zones:
Benthic: Seafloor.
Pelagic: Water column divided into zones (e.g., Epipelagic: 0-200 m; Mesopelagic: 200-1000 m).
Layers of the ocean vary greatly in depth and characteristics.
Comparisons of Ocean Depths
Average ocean depth ranges from 3682-3729 meters.
Key Features:
Mt. Everest (8850 m) compared to the Mariana Trench (11022 m).
Characteristics of Seas vs. Oceans
Definition of a Sea: Smaller, shallower, saltwater body, usually enclosed by land.
Latitude and Longitude Measurements
Latitude: Determined by the North Star (Polaris); Equator is 0 degrees.
Longitude: Measured from the Prime Meridian at Greenwich, England.
Historical Voyages for Science
Captain James Cook: Conducted significant scientific voyages, mapped Pacific islands, and measured ocean characteristics.
Advancements in Oceanography
Modern Tools:
Sonar, robotics, computers, satellites, and models are utilized for oceanographic study.
Nature of Scientific Inquiry
Scientific Method:
Does not claim absolute truth; relies on testing hypotheses.
Theories develop from extensive observation, experimentation, and provide explanations of natural phenomena.
Age of the Earth
Radiometric Dating: Earth is estimated to be approximately 4.6 billion years old.
Geologic Time Scale
Event Markers: Includes key extinctions and the Great Oxidation Event (~2.45 billion years ago).
Formation of Earth and Solar System
Nebular Hypothesis: Solar system bodies formed from a nebula cloud mainly composed of hydrogen and helium.
Structure of the Earth
Layers:
Crust, Mantle, Core defined by chemical composition and physical properties.
Isostatic Adjustment
Vertical Movements: Resulting from crustal buoyancy and glaciers' weight.
Origin of Earth’s Atmosphere and Oceans
Outgassing: Contributed to the formation of Earth’s second atmosphere, leading to the creation of oceans.
Did Life Begin in the Oceans?
Earliest Life Forms: 3.5 billion-year-old bacteria fossils suggest life originated in the ocean.
The Importance of Oxygen to Life
Current Atmosphere Composition: 78% Nitrogen, 21% Oxygen, and 0.9% Argon.
The lack of ozone might have facilitated the origins of life.
Evolution and Natural Selection
Adaptation Mechanism: Organisms adapt over time, and beneficial traits are naturally selected.
Photosynthesis and Respiration
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Photosynthetic Process: Allowed complex organisms to capture sunlight, leading to oxygen production.
Great Oxidation Event**:
Ventured a shift to an oxygen-rich atmosphere due to photosynthesis.
Changes in Earth’s Atmosphere**:
Impact of Fossil Fuels: Human activity currently alters atmospheric composition.