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History of Oceanography
History of Oceanography

... (Canada) Later James Ross took samples from Antarctic ocean bottom at 4.3 Miles John Ross and James Ross found that there are some bottom dwelling creatures in Baffin Bay and Antarctic Ocean. They discovered that deep Atlantic is uniformly cold. Forbes – Oceans divided into life-depth zones; conclud ...
press release
press release

... research by scientists from the University of Hawaiʻi, Mānoa (UHM) and the University of Alaska, Fairbanks (UAF) finds that for some organisms the onset of such critical conditions will be so abrupt, and the duration of events so long, that adaption may become impossible. The study, published this w ...
Lecture 7. Marine Sediments
Lecture 7. Marine Sediments

... Carbonate Compensation Depth The depth at which carbonate input from the surface waters is balanced by dissolution in corrosive deep waters In today’s ocean this depth (CCD) varies between 3 km (polar) and 5 km (tropical) Thus, accumulation rates vary a lot! ...
Global Ocean Legacy - The Pew Charitable Trusts
Global Ocean Legacy - The Pew Charitable Trusts

... and protecting the overall health of the marine environment,6 but only about 2 percent of the ocean is fully protected, compared with about 15 percent of land. When Yellowstone National Park was established in 1872, it not only ensured protection for one of the United States’ most spectacular landsc ...
Earth Science Common Assessment #8
Earth Science Common Assessment #8

... • The floor of some ocean basins may lie 18,000 to 20,000 feet or more beneath the surface. • The greatest depths, however, occur not in the central portion of the ocean but in trenches—long, narrow, deep cracks in the ocean bottom that are usually found near continents and on the seaward side of is ...
Salt water
Salt water

... Biogenous – comes from living sources such as shells and skeletons from tiny marine animals ...
Ch. 6 Marine Vertebrates Lecture Notes Page
Ch. 6 Marine Vertebrates Lecture Notes Page

... •Part of complex food web: •Feed on fish, shellfish & mammals •Sick & dying •Larger animals (whales, seals, tuna) that have few predators •If removed, ecosystem balance is altered •If shark numbers decrease, population sizes of seals & sea lions increase, which causes fish populations to decrease be ...
A Short History of Ocean Conservation and
A Short History of Ocean Conservation and

... Pioneers of the Field • Specific references to marine life were first recorded by Aristotle in 384 BC. • Modern day study of marine biology began with the exploration of Captain James Cook in 18th century Britain. • Charles Darwin is notably famous for the Theory of Evolution (1831-1836). ...
Spanish researchers sequence the genome of global deep ocean
Spanish researchers sequence the genome of global deep ocean

... we are analyzing samples from the deep ocean, covering the great oceans. The new protocols of sequencing and analysis allow us to extract quite more information than in previous studies, which were limited to specific regions or surface waters, to an unprecedented level of resolution". Researchers h ...
Modern Ocean Research
Modern Ocean Research

... satellites. Scientists use the data to make computer models of the ocean floor or to track global trends such as ocean temperatures. An increasingly important task for oceanographers is the study of how humans affect the oceans. Pollution, oil spills, and deep-sea mining all threaten marine ecosyste ...
2003 marine ecology event - Florida 4-H
2003 marine ecology event - Florida 4-H

... a. all seaweed is algae b. all algae is seaweed c. Rhodophyta is the phylum name for green algae d. seaweeds have true roots, stems, and leaves like other plants 2. Which statement is NOT true about red algae? a. It is capable of photosynthesis b. It is the only alga that has true roots. c. The scie ...
ocean water
ocean water

... THE IMMENSE OCEAN FLOOR The partially submerged outer extension of a continent is called the continental margin which is made of continental crust. The continental margin is divided into ...
The coastal ocean
The coastal ocean

...  1.h - Although the ocean is large, it is finite and resources are limited.  5.f - Ocean habitats are defined by environmental factors. Due to interactions of abiotic factors such as salinity, temperature, oxygen, pH, light, nutrients, pressure, substrate and circulation, ocean life is not evenly ...
Chapter 11: The coastal ocean
Chapter 11: The coastal ocean

...  1.h - Although the ocean is large, it is finite and resources are limited.  5.f - Ocean habitats are defined by environmental factors. Due to interactions of abiotic factors such as salinity, temperature, oxygen, pH, light, nutrients, pressure, substrate and circulation, ocean life is not evenly ...
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Earth Science Common Assessment #8
Earth Science Common Assessment #8

... • A deep-sea trench is a narrow, elongate, v-shaped depression in the ocean floor. Trenches * are the deepest parts of the ocean, and the lowest points on Earth, reaching depths of nearly 7 mi below sea level. • These long, narrow, curving depressions can be thousands of miles in length, yet as litt ...
Save Our Shoreline - Submission - 24 December
Save Our Shoreline - Submission - 24 December

... The monitoring of the quality of shellfish waters helps to prevent them becoming contaminated, as there is a risk poor water quality could mean that shellfish become contaminated, which could then affect the people who eat them. The Island should also have a duty to protect areas such as the Ramsar ...
Class Reptilia (marine reptiles)
Class Reptilia (marine reptiles)

... • Approximately 55 species of sea snakes are found in the tropical Indian and Pacific oceans • The tail end of sea snakes is flattened into a paddle-shape for swimming • A few species return to land to lay eggs, but most give birth to live ...
Ocean floor - deb-or-ah
Ocean floor - deb-or-ah

... boring. Just off the continental shelf, the ocean floor is known as the abyssal plain. The depth of the abyssal plain is between 2200 and 5500 meters. It cover roughly 40% of the ocean floor. Less than one tenth of 1% of the abyssal plain has been explored by man. ...
Ocean-atmosphere interactions related to the AMO caused
Ocean-atmosphere interactions related to the AMO caused

... Maurice Lamontagne Institute, DFO, Mont Joli, Canada ...
Chapter 16: Marine and Costal Systems
Chapter 16: Marine and Costal Systems

... fluctuation of salinity shorebirds, commercial fishes transition for anadromous fishes (salmon) urban and coastal development ...
Marine Ecosystems
Marine Ecosystems

... found in both the Pacific and Atlantic Oceans at an average underwater depth of about 2,100 meters (7,000 feet). They are concentrated along the Mid-Ocean Ridge. The Mid-Ocean Ridge is the underwater mountain chain that winds its way around the globe. Hydrothermal vent ecosystems support familiar, y ...
Post Test Study Guide Answer Key 1. HMS Challenger: first voyage
Post Test Study Guide Answer Key 1. HMS Challenger: first voyage

... Oceanography  is  the  study  of  the  oceans  including  the  physical  aspects  (seafloor   topography),  chemical  (salt  content,  etc)  and  biological  (living  things)   ...
Grant Report - SG315 Title: Effects of noise on marine invertebrates
Grant Report - SG315 Title: Effects of noise on marine invertebrates

Oceanography Overview Notes
Oceanography Overview Notes

... ________________________________________made by corals (living organisms) Corals are actually animals and the reef is the habitat they build. ...
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Marine biology



Marine biology is the scientific study of organisms in the ocean or other marine or brackish bodies of water. Given that in biology many phyla, families and genera have some species that live in the sea and others that live on land, marine biology classifies species based on the environment rather than on taxonomy. Marine biology differs from marine ecology as marine ecology is focused on how organisms interact with each other and the environment, while biology is the study of the organisms themselves.A large proportion of all life on Earth lives in the ocean. Exactly how large the proportion is unknown, since many ocean species are still to be discovered. The ocean is a complex three-dimensional world covering about 71% of the Earth's surface. The habitats studied in marine biology include everything from the tiny layers of surface water in which organisms and abiotic items may be trapped in surface tension between the ocean and atmosphere, to the depths of the oceanic trenches, sometimes 10,000 meters or more beneath the surface of the ocean. Specific habitats include coral reefs, kelp forests, seagrass meadows, the surrounds of seamounts and thermal vents, tidepools, muddy, sandy and rocky bottoms, and the open ocean (pelagic) zone, where solid objects are rare and the surface of the water is the only visible boundary. The organisms studied range from microscopic phytoplankton and zooplankton to huge cetaceans (whales) 30 meters (98 feet) in length.Marine life is a vast resource, providing food, medicine, and raw materials, in addition to helping to support recreation and tourism all over the world. At a fundamental level, marine life helps determine the very nature of our planet. Marine organisms contribute significantly to the oxygen cycle, and are involved in the regulation of the Earth's climate. Shorelines are in part shaped and protected by marine life, and some marine organisms even help create new land.Many species are economically important to humans, including food fish (both finfish and shellfish). It is also becoming understood that the well-being of marine organisms and other organisms are linked in very fundamental ways. The human body of knowledge regarding the relationship between life in the sea and important cycles is rapidly growing, with new discoveries being made nearly every day. These cycles include those of matter (such as the carbon cycle) and of air (such as Earth's respiration, and movement of energy through ecosystems including the ocean). Large areas beneath the ocean surface still remain effectively unexplored.
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