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Biological oceanography is the study of how organisms affect and are affected by the physics, chemistry, and geology of the oceanographic system. Biological oceanography may also be referred to as ocean ecology, in which the root word of ecology is Oikos (oικoσ), meaning ‘house’ or ‘habitat’ in Greek.
Marine life is a field of study both in marine biology and in biological oceanography. Biological oceanography is the study of how organisms affect and are affected by the physics, chemistry, and geology of the oceanographic system. Biological oceanography mostly focuses on the microorganisms within the ocean; looking at how they are affected ...
Thermohaline circulation. Oceanography (from Ancient Greek ὠκεανός (ōkeanós) 'ocean' and γραφή (graphḗ) 'writing'), also known as oceanology, sea science, ocean science, and marine science, is the scientific study of the ocean, including its physics, chemistry, biology, and geology.
“We have recently had dinoflagellate blooms up and down the California coast,” Clarissa Anderson, a biological oceanographer at Scripps and director of the Southern California Coastal Ocean ...
Pages in category "Biological oceanography" The following 93 pages are in this category, out of 93 total. This list may not reflect recent changes. ...
Marine Biological Station and Concarneau Marinarium, associated with the French National Museum of Natural History. Station Marine de Concarneau; Marine Station of Arcachon, associated with the University Bordeaux, on Arcachon Bay. Station marine d'Arcachon; Mediterranean Institute of Oceanography in Marseille. MIO [16]
Biological evolution and the functioning of ecosystems, in turn, are to a large degree conditioned by geophysical and geological processes. Understanding the interactions between organisms and their abiotic environment, and the resulting coupled evolution of the biosphere and geosphere is a central theme of research in biogeology.
In biological oceanography, critical depth is defined as a hypothetical surface mixing depth where phytoplankton growth is precisely matched by losses of phytoplankton biomass within the depth interval. [1] [note 1] This concept is useful for understanding the initiation of phytoplankton blooms.
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