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274 - CIESM
274 - CIESM

... eventually die due to the lack of light necessary for photosynthetic processes, but their carbon load was transported to depths. The results from optical measurements showed that POC was generally low, but with a peak at 300 m depth at M600, not corresponding with either Chl a concentration or diato ...
Ecological Relationships Overview Directions
Ecological Relationships Overview Directions

... from the surface through the water column to the seafloor. Most of the living space on Earth is in the ocean. • Principle 5f: Ocean habitats are defined by environmental factors. Due to interactions of abiotic factors such as salinity, temperature, oxygen, pH, light, nutrients, pressure, substrate ...
On November 29 - the National Sea Grant Library
On November 29 - the National Sea Grant Library

... for survival? Scientists have discovered that during its early life stages, the tubeworm has a mouth and gut for bacteria to enter. But as the worm rapidly grows, these features disappear! After riding the ocean currents for up to a month and sometimes hundreds of miles, tiny tubeworms no larger tha ...
Introduction to Marine Science
Introduction to Marine Science

... The oceanic zone is the life zone that extends beyond the neritic zone and includes most of the open ocean. The upper part of the oceanic zone receives light, whereas the lower part (most of the ocean) is in darkness. The part of the ocean that light penetrates is called the photic (meaning “light”) ...
Oceanography – MARSC 100: Study Guide – Exam 3 (Ch
Oceanography – MARSC 100: Study Guide – Exam 3 (Ch

... What are the characteristics of scientific names and what advantage exists in using scientific names, compared to using common names? Plankton, Algae, and Plants - Chapter #14 ...
Oceanography
Oceanography

... minerals in the Ocean -mining magnesium nodules from ocean floor brings up colder waters -reduce the transparency of the water –less photosynthesis ...
Climate and fish - Havforskningsinstituttet
Climate and fish - Havforskningsinstituttet

... it is expected that the whole of the Barents Sea, for example, will be ice-free all year round as we approach 2100. In the Fram Strait, on the other hand, there will still be major ice transport coming from the Arctic during the winter months. Much of the multi-year ice will disappear from the Arcti ...
Deep-sea fisheries and vulnerable ecosystems in the northeast
Deep-sea fisheries and vulnerable ecosystems in the northeast

... habitats such as sponge grounds and ancient deep-water coral reefs. Scientific reports conclude that bottom trawling in waters as deep as 1,500 metres or more poses the greatest threat to deep-sea corals and sponges.6 The International Council for the Exploration of the Seas has indicated that all f ...
Society and the Sea, Fall 2008 - University of California San Diego
Society and the Sea, Fall 2008 - University of California San Diego

... a)will be straight, no curve b)will slightly curve right c)will slightly curve left d)would hit Texas 64. The geology of the Andes Mountains in South America: a)Continent-Continent Collision b) Divergence of two plates creating volcanism c)Subduction of Oceanic plate under Continental plate d)Hot sp ...
The last frontier on Earth - Centre for International Law
The last frontier on Earth - Centre for International Law

... I AGREE with Cameron that the ocean space is our last frontier. One of the mysteries of the deep seabed and ocean floor is the discovery of deposits of polymetallic nodules, polymetallic sulphides, and cobalt-rich ferromanganese crusts. The polymetallic nodules contain precious metals such as mangan ...
Ten years of coastal fish monitoring in Estonia: dynamics of fish
Ten years of coastal fish monitoring in Estonia: dynamics of fish

... related both to human impact (mostly fishery) and environmental changes affecting reproduction and natural mortality (temperature, salinity, abundance of predatory fish and fish-eating cormorants, etc.). ...
Marine Ecosystems - Distribution Access
Marine Ecosystems - Distribution Access

... camouflage — An adaptation that helps creatures to blend in with surroundings so that they appear less obvious to their predators. photic zone — The part of a body of water through which sunlight can penetrate.“Photo” means light. It is where photosynthesis occurs, where there are higher levels of o ...
Moss_UTL_GOA-IERP_jul
Moss_UTL_GOA-IERP_jul

... – Combine detailed bathymetry, substrate, and species habitat preferences to create habitat suitability maps by region – Overlay data on nearshore prey, competitor, and predator fields to predict ability of YOY to feed, compete, and avoid predation • Nearshore stations from existing and new surveys ...
Deep-sea fisheries and vulnerable ecosystems in the northeast
Deep-sea fisheries and vulnerable ecosystems in the northeast

... habitats such as sponge grounds and ancient deep-water coral reefs. Scientific reports conclude that bottom trawling in waters as deep as 1,500 metres or more poses the greatest threat to deep-sea corals and sponges.6 The International Council for the Exploration of the Seas has indicated that all f ...
marine and esturian ecosystem-2012
marine and esturian ecosystem-2012

... In general, water is most essential for the maintenance and activities in all life forms. Water is an important component of cell constituting about 80% of the weight of protoplasm. For the photosynthetic process in autotrophic plants, water itself is an important raw material. It is a universal sol ...
Sweeping The Ocean Floor
Sweeping The Ocean Floor

... other things that lived in the ocean, including obscure but biologically important organisms like polychaetes. The Census of Marine Life was born in 2000. “It is what it says it is,” Ausubel says. “If you pick up any textbook, there isn’t one that can tell you what lives in the ocean. From microbes ...
2008, final Lecture 12 deep sea and hydro vents
2008, final Lecture 12 deep sea and hydro vents

... – It continuously spews super-hot, mineral-rich water that helps support a diverse community of organisms. – Although most of the deep sea is sparsely populated, vent sites teem with a fascinating array of life. • Tubeworms and huge clams are the most distinctive inhabitants of Pacific Ocean vent si ...
OBIS Report - Census of Marine Life Secretariat
OBIS Report - Census of Marine Life Secretariat

... marine protected areas in the nodule mining claim area off Hawaii (Clarion Clipperton Fracture Zone, CCZ) were compiled during a workshop and forwarded to the ISA. It has been suggested that in each of the nine subregions of the CCZ, about 25% of the area should be designated PRAs (Protected Referen ...
General Oceanography, GEOL 105, Summer 2012 Session II Page
General Oceanography, GEOL 105, Summer 2012 Session II Page

... vast majority is found in the forms that cannot be seen by the naked eye. 4. The Carbon Cycle and Carbon Pump Make a simple diagram (simpler than the one on the WWW page) showing the flow of carbon between the land, atmosphere, sea and seafloor. ...
Mr. Perfect UNDER THE SEA
Mr. Perfect UNDER THE SEA

... float at or near the surface where sunlight can penetrate.  Most of the plankton are very small, such as algae.  These organisms drift with the currents or tides.  Plankton are the main food for many larger organisms. They account for most of the organisms in the ocean. ...
Oceanography Quick Notes
Oceanography Quick Notes

... returns to the ocean in underwater channels in sandbars) and turbidity currents (cause by an underwater landslide and moves along the bottom – very dense, very cloudy).  Most waves on the ocean surface are generated by wind. The top of a wave is the crest; the bottom is the trough. The distance be ...
File - GAIA POWER PLANTS
File - GAIA POWER PLANTS

... a cheap way. Then such an invention will make all other inventions through the history to small events. ...
ángeles garcía pardo
ángeles garcía pardo

... The deep sea, the largest biome on Earth, has a series of characteristics that make this environment both distinct from other marine and land ecosystems and unique for the entire planet. Nevertheless, the deep sea is still mostly unknown and current discovery rates of both habitats and species remai ...
Oceanography
Oceanography

... the food web in these environments 1. phytoplankton – plant plankton – example – diatoms 2. zooplankton – animal-like plankton exampleprotists, crustaceans B. Nekton – organisms that swim in the ocean freely. examples – larger fish, squid, sea turtles, whales C. Benthos – community of organisms that ...
Abundance and distribution of the larval stages of the mesopelagic
Abundance and distribution of the larval stages of the mesopelagic

... of the shelf break and on the shelf break is not surprising as the adults are mesopelagic and are normally found at 200m depths, only migrating into the upper 100m to feed at night (Whitehead et al., 1989). In each study period, all the larval stages remained west of the shelf break, unlike other sp ...
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Deep sea fish



Deep-sea fish are fish that live in the darkness below the sunlit surface waters, that is below the epipelagic or photic zone of the sea. The lanternfish is, by far, the most common deep-sea fish. Other deep sea fish include the flashlight fish, cookiecutter shark, bristlemouths, anglerfish, and viperfish.Only about 2% of known marine species inhabit the pelagic environment. This means that they live in the water column as opposed to the benthic organisms that live in or on the sea floor. Deep-sea organisms generally inhabit bathypelagic (1000m-4000m deep) and abyssopelagic (4000m-6000m deep) zones. However, characteristics of deep-sea organisms, such as bioluminescence can be seen in the mesopelagic (200m-1000m deep) zone as well. The mesopelagic zone is the disphotic zone, meaning light there is minimal but still measurable. The oxygen minimum layer exists somewhere between a depth of 700m and 1000m deep depending on the place in the ocean. This area is also where nutrients are most abundant. The bathypelagic and abyssopelagic zones are aphotic, meaning that no light penetrates this area of the ocean. These zones make up about 75% of the inhabitable ocean space.The epipelagic zone (0m-200m) is the area where light penetrates the water and photosynthesis occurs. This is also known as the photic zone. Because this typically extends only a few hundred meters below the water, the deep sea, about 90% of the ocean volume, is in darkness. The deep sea is also an extremely hostile environment, with temperatures that rarely exceed 3 °C and fall as low as -1.8 °C (with the exception of hydrothermal vent ecosystems that can exceed 350 °C), low oxygen levels, and pressures between 20 and 1,000 atmospheres (between 2 and 100 megapascals).
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