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Geology 3015 Lecture Notes Week 4b
Geology 3015 Lecture Notes Week 4b

... Explained by continents drifting across stationary magnetic poles. Importantly, drift paths recorded by paleomagnetism culminate in the assembly of a supercontinent during the Late Paleozoic. This is consistent with the previously considered evidence for continental drift and validates the hypothese ...
Earth`s Oceans Power Point
Earth`s Oceans Power Point

... rivers run into the ocean. Salinity levels are also affected by animals such as clams and oysters that use calcium salts to build their shells. They remove salt from the water. In warm ocean areas where there is little rainfall and much evaporation, the amount of dissolved salts is much greater. In ...
Harmful Algal Blooms in Southern Californian Waters
Harmful Algal Blooms in Southern Californian Waters

... food webs, a few are capable of producing substances that are noxious or toxic, resulting in illness and even death of marine life and occasionally humans who consume contaminated seafood. When microalgae create these conditions, we refer to them as harmful algal blooms (HABs). An older term often u ...
The Chemical Composition of the Earth`s Original Atmosphere
The Chemical Composition of the Earth`s Original Atmosphere

Plate_tectonics_2 - Red Hook Central Schools
Plate_tectonics_2 - Red Hook Central Schools

... Name this plate boundary Match the labels to the letters F E ...
Investigation OCEAN IN THE GLOBAL WATER CYCLE
Investigation OCEAN IN THE GLOBAL WATER CYCLE

... condensation (or deposition) of water vapor into tiny water droplets (or ice crystals) forming clouds, some of which produce rain or snow that falls back to Earth’s surface. The freshening of seawater by evaporation and subsequent downwind precipitation of the fresh water is the major cause of varia ...
Ch. 14 The Oceans
Ch. 14 The Oceans

... b. It is harmful to only a few organisms. c. It can destroy an animal’s natural insulation. d. It is harmful only to animals that swallow it. 19. What is the natural cleaning process that slowly takes place after oil spills? Certain bacteria that live in the ocean feed on the oil and multiply, event ...
C1b 6.2 The Restless Earth
C1b 6.2 The Restless Earth

... Evidence for Continental Drift The theory is supported by several pieces of evidence. For example, if we consider Africa and South America there is: – The “jig-saw fit” – The similarities in the rock layers from Africa and South America. – Similarities in the type and age of fossils. – Evidence of ...
GEOL_106_lecture_03_..
GEOL_106_lecture_03_..

... Plate velocities determined from the rate of sea floor spreading or by making measurements across a plate boundary are only relative velocities. That is we know the velocity of one plate only if we can assume that the adjacent plate is not moving. In order to determine absolute plate velocities, we ...
Continental crust - British Academy Wiki
Continental crust - British Academy Wiki

... The Earth is divided into three layers—the crust, the mantle, and the core—based on the compounds that make up each layer. ...
Investigating Large Igneous Province Formation and
Investigating Large Igneous Province Formation and

... a variety of surface expressions (Fig. 1a and 1b); the most common present-day examples are oceanic plateaus (e.g., Kerguelen/Broken Ridge, Ontong Java, Manihiki, Hikurangi, Shatsky), ocean basin flood basalts (e.g., Caribbean, Nauru), magma-dominated divergent continental margins (e.g., the North A ...
No Slide Title
No Slide Title

... Mapping Ocean Basins • Ocean mapping revealed ...
MIKROBIOLOGI DASAR
MIKROBIOLOGI DASAR

... referred to as cross-feeding or the satellite phenomenon; an important example is interspecies hydrogen transfer, which occurs in anaerobic environments (described below) a. Fermentative bacteria produce low molecular weight fatty acids ...
Worksheet as a MS Word file ( format)
Worksheet as a MS Word file ( format)

... Plates move towards convergent plate boundaries, allowing one of the plates to sink back into the Earth by a process called subduction -- thus the lithosphere beneath the ocean, known as oceanic lithosphere, is recycled The process of subduction also produces deep-sea trenches, which mark the deepes ...
expedition 8 worksheet as a pdf
expedition 8 worksheet as a pdf

... Plates move towards convergent plate boundaries, allowing one of the plates to sink back into the Earth by a process called subduction -- thus the lithosphere beneath the ocean, known as oceanic lithosphere, is recycled The process of subduction also produces deep-sea trenches, which mark the deepes ...
ch9
ch9

... • Rock Types and Structures - Rock evidence for continental exists in the form of several mountain belts that end at one coastline, only to reappear on a landmass across the ocean. • Ancient Climates ...
Marine Sediments Why Sediments?
Marine Sediments Why Sediments?

Dissolving rocks - Lockland Local Schools
Dissolving rocks - Lockland Local Schools

... – When dissolved in water it makes a weak acid called _________________ carbonic acid – Carbonic acid weathers rocks like ___________ marble and ____________ limestone ...
Chapter 5 – Sea/Air Interactions
Chapter 5 – Sea/Air Interactions

The Sulfur Cycle
The Sulfur Cycle

... through subduction zones by targeting processes that fractionate sulfur isotopes (separate atoms of sulfur that have different numbers of neutrons and thus different atomic mass). In Costa Rica, we collected volcanic gases by inserting a titanium tube into a degassing vent and running the gas sample ...
Beyond_the_Beach
Beyond_the_Beach

... Beach erosion Sea-level rise Carbon burial, greenhouse gases, global warming History of Earth recorded by marine sedimentary deposits ...
Script - FOG - City College of San Francisco
Script - FOG - City College of San Francisco

... Now that we have the understanding of Plate Tectonics that we developed in last week’s lecture, let’s go down to the bottom of the seafloor and explore its depths a little further. First, it’s important to note that less than 1% of the surface of the seafloor has ever been directly sampled. What we ...
Biogeosciences Coastal hypoxia and sediment biogeochemistry
Biogeosciences Coastal hypoxia and sediment biogeochemistry

Morphology_of_Ocean_Basins
Morphology_of_Ocean_Basins

... The trench is about 2,550 kilometres long but has a mean width of only 69 kilometres. It reachess a maximum-known depth of about 10.91 km at he Challenger Deep, a small slot-shaped valley in its floor, at its southern end, although some unrepeated measurements place the deepest portion at 11.03 km.[ ...
Oxidation-Reduction Processes in Natural Waters
Oxidation-Reduction Processes in Natural Waters

... Organisms catalyze all significant redox reaction in natural waters. As illustrated in the table, with the exception of photosynthesis and hydrogen generation, all of the reactions in the table are thermodynamically favorable as written. That is, the reactions as written have a negative free energy. ...
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Anoxic event



Oceanic anoxic events or anoxic events (Anoxia conditions) refer to intervals in the Earth's past where portions of oceans become depleted in oxygen (O2) at depths over a large geographic area. During some of these events, euxinia develops - euxinia refers to anoxic waters that contain H2S hydrogen sulfide. Although anoxic events have not happened for millions of years, the geological record shows that they happened many times in the past. Anoxic events coincide with several mass extinctions and may contribute to these events. These mass extinctions include some that geobiologists use as time markers in biostratigraphic dating. It is believed oceanic anoxic events are strongly linked to slowing of ocean circulation, climatic warming and elevated levels of greenhouse gases. Enhanced volcanism (through the release of CO2 and other greenhouse gases) is the proposed central external trigger for the development of these events.
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