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Book perseus 4 _12 send Brussels
Book perseus 4 _12 send Brussels

... cost­effective management measures for marine governance The MeTaLi model – MERMAID project ................217 ...
Exploring the Red Sea seasonal ecosystem functioning using a
Exploring the Red Sea seasonal ecosystem functioning using a

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Summer cyanobacterial blooms in
Summer cyanobacterial blooms in

... Contradicting this view, the studies presented here show that these cyanobacteria in fact support zooplankton recruitment. Moreover is the ecological role of the most famous cyanobacterial toxin in the Baltic Sea, nodularin, evaluated. As blooms are predicted to increase due to global climate change ...
The Red Sea: Birth of an Ocean
The Red Sea: Birth of an Ocean

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Sea Water' - ResearchGate
Sea Water' - ResearchGate

... nutrient agar was examined by the replica plate procedure but in no case was evidence obtained for production of an antibiotic active against either E. coli or B. subtilis. Although these results indicate that antibiotic-producing marine bacteria did not occur commonly, their presence in sea water h ...
inferences from the COADS dataset - Horizon documentation-IRD
inferences from the COADS dataset - Horizon documentation-IRD

... Fig. 3. Data density was, in the 1950s, low all over the region except along trade lanes such as that passing through the MalaccaStrait to Singapore. Later, data density increases alonc the eastern part of the China Sea but remains "spotty" over thwestern part of Southeast Asia. For the purpose of t ...
Climate and fish - Havforskningsinstituttet
Climate and fish - Havforskningsinstituttet

... significant reduction in sea-ice coverage, mainly in spring and summer, while changes in winter ice cover will be much less dramatic. Some areas that are presently covered by permanent sea ice will become seasonal ice zones with open water in summer. Certain models suggest that the whole of the Arct ...
Climate Change and Biodiversity Effects in Turkish Seas
Climate Change and Biodiversity Effects in Turkish Seas

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MIT Sea Grant College Program
MIT Sea Grant College Program

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10750_2017_3120_MOESM1_ESM
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BG3.3 Abstracts - The Future Ocean
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28. Miocene Evaporates in Red Sea Cores, Their Relevance to the
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Maritime Spatial Planning (MSP) is currently gaining momentum
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April 18, 1996 - Ms. Peggy ”Binzer
April 18, 1996 - Ms. Peggy ”Binzer

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Geo 221_19 copy
Geo 221_19 copy

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Red Sea



The Red Sea, (also the Erythraean Sea), is a seawater inlet of the Indian Ocean, lying between Africa and Asia. The connection to the ocean is in the south through the Bab el Mandeb strait and the Gulf of Aden. In the north, there is the Sinai Peninsula, the Gulf of Aqaba, and the Gulf of Suez (leading to the Suez Canal). The Red Sea is a Global 200 ecoregion. The sea is underlain by the Red Sea Rift which is part of the Great Rift Valley.The Red Sea has a surface area of roughly 438,000 km2 (169,100 mi2). It is about 2250 km (1398 mi) long and, at its widest point, 355 km (220.6 mi) wide. It has a maximum depth of 2211 m (7254 ft) in the central median trench, and an average depth of 490 m (1,608 ft). However, there are also extensive shallow shelves, noted for their marine life and corals. The sea is the habitat of over 1,000 invertebrate species, and 200 soft and hard corals. It is the world's northernmost tropical sea.
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