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Derived From Organisms livingin the water sea floor Calcareous CaCO3 Siliceous SiO2-nH20 Organic Matter (C6H12O6) If Pelagic sediment are more than 30% biogenic material they are called oozes Calcareous Oooze (Foram Ooze) Siliceous Ooze (Diatom Ooze Etc) |
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Foraminifera - Single Cell Animals Pleropods - Snail like organisms Coccolithphorids - Single Celled Plants Coral - multi Celled Colonial Animals Calcareous Algae - Multicelled plants Mollusks - Gastropod, Pelecrypods, Cephalapods |
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Algae. Snowflake of the sea, Used for filters |
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Diatoms and Radiolarians Dissolve Rate |
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Form onthe seafloor or within the seidment Minerals Precipitate directly out of seawater or sediments porewater Phosphorite |
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PHOSPHORATES are used as: (Part of Agricultural Revolution) |
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Space between sediments is known as " " space |
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Occur on Abyssal Planes with low seidment accumialation and grow slowly over thousands of years |
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Have to consume to survive |
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Sediments Distribution is largely a function of |
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Water Depth Surface water productivity Distance from land latitue Global Sea Water Circulation patterns |
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Continental Shelf Sedimentation |
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Definition
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Sea level oscillates by what rate? |
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120 meteres over 100,000 year intervals |
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Sea level was 400 feet lower 1800 ypd |
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Sedimentationin the deep sea occurs by: |
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The transport of large amoun of sediment as a mass. The transport is induced by gravity |
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Settling of Palagic sediment Biochemical precipitation Due to teh Accumulation of a large uildup of river material on teh outer shelf and slope especially during lowered sea level |
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Bulk emplacement cont. SLUMPS are: |
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Definition
sediment piles that move as a mass their internal structure (bedding) is retained |
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Bulk emplacement continued: MUD FLOWS are: |
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slumping and transport of mud as a sheet across the shelf |
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Bulk Emplacement Continued TURBIDITY CURRENTS |
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are large slurries in which rapidly move downslope |
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In shallow areas and tropical to subtropical environments (warm) |
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In areas of very high productivity (UPWELLING) and cold waters |
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In deepes areas and where oldest deep water occurs |
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What is the Chemical Forumula for: CALCITE PRECIPITATION and DISSOLUTION? |
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CA2+2HCO3 <----> CaCO3+CO2+H20 (Simple Make Shift Biological Formula) |
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Zone over which dissolution occurs |
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Calcite Compensation depth |
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The corrosiveness of water to calcite increases downward because: |
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of higher pressure lower temperature and higher CO2 Concentrations |
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At CCD CAlcite deposition - |
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CCD Occurs at average depth of |
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Abyssal Clays are below CCD? |
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Five Sediment Sampling Devices |
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Grab Samplers Coring Devices Vibracore Gravity Core Piston Cre Rotary Drills |
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Significance of Oceanography (Why is the ocean important?) |
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Have a major influence on teh weather and climate Are a source of food energy medical resources bilogical diversity Are important in transportationa nd trade Have military significance (Bombing sites/Submarines etc) Are an important recreational source Have a major influence on the health of the planet |
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USGS NOAA EPA NMFS DOD ONR NRL USACE etc... |
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Earliest Records of exploration date back to |
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Egyptions 4000BC Navigated the Nile and eastern Mediteranian Pheonicians 1100 BC -1200 AD navigated the entired mediterranean red sea and indian ocean Africa and British Isles Greeks 3 and 4th Centuries BC |
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Gree Explorer compiled a map of the world showing the Mediterranean sea as the center surrounded by three land masses North Africa Europe and Asia |
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First to circumnavigate england and sailed north to scotland Norway and Germany Discovered the tides had to do with phases of the moon Discovered how to tell your latitude using the N Star |
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Produced first world atlas Overestimated extent of Asia to teh east Underestimated Circumfrance of the earth |
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expored teh far north Atlantic and established colonies in iceland Greenland and Newfoundland during Medival Warm period Arabs Controlled North Africa and Spain and trade routes eat and became dominant navigators f the time PORTOLANOS (early charts first appeared) |
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Explorations by Europeans increased |
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The prupose of the European Voyages |
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find faster safer trade routs to teh orient spurred on by the need for riches and spices |
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Underestimated extent of Atlantic ocean and size of earth due to Ptolemys calculations |
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Underestimated extent of Pacific ocean do to Ptolemy Circumnavigated teh earth Established true length of a degree of latitude Hudnered by Profivision probs mutiny and storms Killed by natives in Phillippines |
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Used harrison fourth chronometer to produce accurate charts 3 voyages to teh pacific between 1768 and 1779 Charted coasts of teh South Pacific Australia New Zealand and NW North American Haw Isalnds Made sounding and logged winds currents and water temps |
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In simple terms its necessary to know teh position of the sun or stars related to the time So accuracte navigation had to wait for accurate clocks that worked on ships john Harrison successed in making an ACCURATE CHRONOMETETER in 1761 |
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Challenger Expedition 1872 |
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Lithosphere – Asthenosphere – Mesosphere – Outer Core – Inner Core |
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Pangaia (Northern Vs Southern parts) |
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Remember the concept of Paleo (Ancient) Magnetism. Can be defined on Polarity Compass needle points toward N and South |
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Align themselves along the magnetic field. Crystals of Magnetite get locked into place at that temp. Rock cools. |
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LINEAR MAGNETIC ANOMALIES |
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– Age then created GPTS Geomagnetic Polarity Time Scale (6:13) tell the inclination which give you latitude. Can tell where a rock formed basically and based on the paliomagnetism of that rock you can tell that it actually formed wherever said point is. |
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Out in the ocean a divergent boundary |
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gives an idea of where Pacific plate is moving, it tell latitude, very important fundamental data that supports plate tectonics. |
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Mid Ocean ridges are shallow because |
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Definition
because they are hotter (the rock is hotter which is less dense therefor more buoyant so it rises up) Something more dense is going to sink lower if you take something warmer its going to rise because you have very young or warm rock along the ridges that’s where the sea floor forms that’s where it cools sinks comes out and the abyssal planes are characterized by being flat. For years sediment has been building up except where there are sea mounts. |
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Flat for years sediment has been building up |
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Seizmic From of Subduction |
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Associates with Divergent boundaries |
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Sediments in Mid Ocean Ridge are |
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Continental Rise and Slope are buiolt up by these oil is often found |
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Calcareous Algae (An Autotroph) Made of = CaCO3 So if more than 30 % its Calcareous Ooze but if the dominant is Coccolithophores htan it is Cacareous. |
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Definition
Siliceous (Frustal is the name of skeleton) |
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Siliceous Chemical Make Up |
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Calcareous Single Cell Heterotoph |
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Radolarians are important bc |
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Important because things dissolve at different rates. Silic dissolves at a faster rate. |
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(30:04_ Calcite Compensation Data) Below a certain depth calcium carbonate dissolves. At a very deep depth it is pretty much gone. So the amound of Calcium Carbonate going down is equal t otaht going up. “The Snow Line” – Conecepts to be understood |
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Water temperature starts dissolving calcium carbonate at a colder temperature. (:41) The temperature is mainly driving down sediments pressure also is also playing effect, which means increased CO2 in water. CO2 – Dissolves Calcium Carbonate. CC=CC Up and Down. RATE OF CC INPUT = RATE OF DISSOLUTIONS. |
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Ca2 + 2HCO3 <->CaCO3+CO2+H2O |
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Ca2 + 2HCO3 <->CaCO3+CO2+H2O – Drives Eq to the left therefore calcium carbonate dissolves. -- surface water - underwater |
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