{"id":664,"date":"2017-04-19T19:28:15","date_gmt":"2017-04-19T19:28:15","guid":{"rendered":"https:\/\/courses.lumenlearning.com\/geophysical\/?post_type=chapter&#038;p=664"},"modified":"2017-04-19T22:16:50","modified_gmt":"2017-04-19T22:16:50","slug":"interactions-among-ocean-organisms","status":"publish","type":"chapter","link":"https:\/\/courses.lumenlearning.com\/suny-geophysical\/chapter\/interactions-among-ocean-organisms\/","title":{"raw":"Interactions Among Ocean Organisms","rendered":"Interactions Among Ocean Organisms"},"content":{"raw":"The previous section briefly discussed the adaptations different types of organisms have to live in the ocean. A look at a few of the different habitats organisms live in can focus even more on these important adaptations.\r\n<h2>Intertidal<\/h2>\r\n<img class=\"alignright wp-image-729\" src=\"https:\/\/s3-us-west-2.amazonaws.com\/courses-images\/wp-content\/uploads\/sites\/250\/2017\/04\/19213257\/ISS018-E-018129_lrg.jpg\" alt=\"Atafu Atoll. It appears to be an island that is nearly covered in a lake. There is just a thin bar of sand showing above the sea.\" width=\"400\" height=\"267\" \/>A great abundance of life is found in the intertidal zone. High energy waves pound the organisms that live in this zone and so they must be adapted to pounding waves and exposure to air during low tides. Hard shells protect from pounding waves and also protect against drying out when the animal is above water. Strong attachments keep the animals anchored to the rock.In a tide pool, as in the photo, what organisms are found where and what specific adaptations do they have to that zone? The mussels on the top left have hard shells for protection and to prevent drying because they are often not covered by water. The sea anemones in the lower right are more often submerged and have strong attachments but can close during low tides. Many young organisms get their start in estuaries and so they must be adapted to rapid shifts in salinity.\r\n<h2>Reefs<\/h2>\r\nCorals and other animals deposit calcium carbonate to create rock <strong>reefs<\/strong> near the shore. Coral reefs are the \u201crainforests of the oceans\u201d with a tremendous amount of species diversity.Reefs can form interesting shapes in the oceans. Remember that hot spots create volcanoes on the seafloor. If these volcanoes rise above sea level to become islands, and if they occur in tropical waters, coral reefs will form on them. Since the volcanoes are cones, the reef forms in a circle around the volcano. As the volcano comes off the hot spot, the crust cools. The volcano subsides and then begins to erode away. Eventually, all that is left is a reef island called an <a href=\"https:\/\/www.google.com\/search?q=atol&amp;client=firefox-a&amp;hs=Syp&amp;rls=org.mozilla:en-US:official&amp;channel=sb&amp;tbm=isch&amp;tbo=u&amp;source=univ&amp;sa=X&amp;ei=v-MhU-arEImGogT71YG4Aw&amp;ved=0CEQQsAQ&amp;biw=1881&amp;bih=1019#channel=sb&amp;q=atoll&amp;rls=org.mozilla:en-US:official&amp;tbm=isch\" target=\"_blank\"><strong>atoll<\/strong><\/a>. A <strong>lagoon<\/strong> is found inside the reef.\r\n\r\nCoral reef are near shore and so are subject to pollution from land. The coral animals are very sensitive to temperature and reefs around the world are stressed from rising ocean temperatures.\r\n\r\nhttps:\/\/youtu.be\/u0VHC1-DO_8","rendered":"<p>The previous section briefly discussed the adaptations different types of organisms have to live in the ocean. A look at a few of the different habitats organisms live in can focus even more on these important adaptations.<\/p>\n<h2>Intertidal<\/h2>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"alignright wp-image-729\" src=\"https:\/\/s3-us-west-2.amazonaws.com\/courses-images\/wp-content\/uploads\/sites\/250\/2017\/04\/19213257\/ISS018-E-018129_lrg.jpg\" alt=\"Atafu Atoll. It appears to be an island that is nearly covered in a lake. There is just a thin bar of sand showing above the sea.\" width=\"400\" height=\"267\" \/>A great abundance of life is found in the intertidal zone. High energy waves pound the organisms that live in this zone and so they must be adapted to pounding waves and exposure to air during low tides. Hard shells protect from pounding waves and also protect against drying out when the animal is above water. Strong attachments keep the animals anchored to the rock.In a tide pool, as in the photo, what organisms are found where and what specific adaptations do they have to that zone? The mussels on the top left have hard shells for protection and to prevent drying because they are often not covered by water. The sea anemones in the lower right are more often submerged and have strong attachments but can close during low tides. Many young organisms get their start in estuaries and so they must be adapted to rapid shifts in salinity.<\/p>\n<h2>Reefs<\/h2>\n<p>Corals and other animals deposit calcium carbonate to create rock <strong>reefs<\/strong> near the shore. Coral reefs are the \u201crainforests of the oceans\u201d with a tremendous amount of species diversity.Reefs can form interesting shapes in the oceans. Remember that hot spots create volcanoes on the seafloor. If these volcanoes rise above sea level to become islands, and if they occur in tropical waters, coral reefs will form on them. Since the volcanoes are cones, the reef forms in a circle around the volcano. As the volcano comes off the hot spot, the crust cools. The volcano subsides and then begins to erode away. Eventually, all that is left is a reef island called an <a href=\"https:\/\/www.google.com\/search?q=atol&amp;client=firefox-a&amp;hs=Syp&amp;rls=org.mozilla:en-US:official&amp;channel=sb&amp;tbm=isch&amp;tbo=u&amp;source=univ&amp;sa=X&amp;ei=v-MhU-arEImGogT71YG4Aw&amp;ved=0CEQQsAQ&amp;biw=1881&amp;bih=1019#channel=sb&amp;q=atoll&amp;rls=org.mozilla:en-US:official&amp;tbm=isch\" target=\"_blank\"><strong>atoll<\/strong><\/a>. A <strong>lagoon<\/strong> is found inside the reef.<\/p>\n<p>Coral reef are near shore and so are subject to pollution from land. The coral animals are very sensitive to temperature and reefs around the world are stressed from rising ocean temperatures.<\/p>\n<p><iframe loading=\"lazy\" id=\"oembed-1\" title=\"Jeremy Jackson: How we wrecked the ocean\" width=\"500\" height=\"281\" src=\"https:\/\/www.youtube.com\/embed\/u0VHC1-DO_8?feature=oembed&#38;rel=0\" frameborder=\"0\" allowfullscreen=\"allowfullscreen\"><\/iframe><\/p>\n\n\t\t\t <section class=\"citations-section\" role=\"contentinfo\">\n\t\t\t <h3>Candela Citations<\/h3>\n\t\t\t\t\t <div>\n\t\t\t\t\t\t <div id=\"citation-list-664\">\n\t\t\t\t\t\t\t <div class=\"licensing\"><div class=\"license-attribution-dropdown-subheading\">CC licensed content, Shared previously<\/div><ul class=\"citation-list\"><li>Dynamic Earth: Introduction to Physical Geography. <strong>Authored by<\/strong>: R. Adam Dastrup. <strong>Located at<\/strong>: <a target=\"_blank\" href=\"http:\/\/www.opengeography.org\/physical-geography.html\">http:\/\/www.opengeography.org\/physical-geography.html<\/a>. <strong>Project<\/strong>: Open Geography Education. <strong>License<\/strong>: <em><a target=\"_blank\" rel=\"license\" href=\"https:\/\/creativecommons.org\/licenses\/by-sa\/4.0\/\">CC BY-SA: Attribution-ShareAlike<\/a><\/em><\/li><\/ul><div class=\"license-attribution-dropdown-subheading\">All rights reserved content<\/div><ul class=\"citation-list\"><li>How we wrecked the ocean. <strong>Authored by<\/strong>: Jeremy Jackson. <strong>Provided by<\/strong>: TED . <strong>Located at<\/strong>: <a target=\"_blank\" href=\"https:\/\/youtu.be\/u0VHC1-DO_8\">https:\/\/youtu.be\/u0VHC1-DO_8<\/a>. <strong>License<\/strong>: <em>All Rights Reserved<\/em>. <strong>License Terms<\/strong>: Standard YouTube License<\/li><\/ul><div class=\"license-attribution-dropdown-subheading\">Public domain content<\/div><ul class=\"citation-list\"><li>Atafu Atoll, Tokelau, Southern Pacific Ocean. <strong>Provided by<\/strong>: NASA. <strong>Located at<\/strong>: <a target=\"_blank\" href=\"https:\/\/earthobservatory.nasa.gov\/IOTD\/view.php?id=37753\">https:\/\/earthobservatory.nasa.gov\/IOTD\/view.php?id=37753<\/a>. <strong>License<\/strong>: <em><a target=\"_blank\" rel=\"license\" href=\"https:\/\/creativecommons.org\/about\/pdm\">Public Domain: No Known Copyright<\/a><\/em><\/li><\/ul><\/div>\n\t\t\t\t\t\t <\/div>\n\t\t\t\t\t <\/div>\n\t\t\t <\/section>","protected":false},"author":17,"menu_order":14,"template":"","meta":{"_candela_citation":"[{\"type\":\"cc\",\"description\":\"Dynamic Earth: Introduction to Physical Geography\",\"author\":\"R. Adam Dastrup\",\"organization\":\"\",\"url\":\"http:\/\/www.opengeography.org\/physical-geography.html\",\"project\":\"Open Geography Education\",\"license\":\"cc-by-sa\",\"license_terms\":\"\"},{\"type\":\"pd\",\"description\":\"Atafu Atoll, Tokelau, Southern Pacific Ocean\",\"author\":\"\",\"organization\":\"NASA\",\"url\":\"https:\/\/earthobservatory.nasa.gov\/IOTD\/view.php?id=37753\",\"project\":\"\",\"license\":\"pd\",\"license_terms\":\"\"},{\"type\":\"copyrighted_video\",\"description\":\"How we wrecked the ocean\",\"author\":\"Jeremy Jackson\",\"organization\":\"TED \",\"url\":\"https:\/\/youtu.be\/u0VHC1-DO_8\",\"project\":\"\",\"license\":\"arr\",\"license_terms\":\"Standard YouTube License\"}]","CANDELA_OUTCOMES_GUID":"","pb_show_title":"on","pb_short_title":"","pb_subtitle":"","pb_authors":[],"pb_section_license":""},"chapter-type":[],"contributor":[],"license":[],"class_list":["post-664","chapter","type-chapter","status-publish","hentry"],"part":593,"_links":{"self":[{"href":"https:\/\/courses.lumenlearning.com\/suny-geophysical\/wp-json\/pressbooks\/v2\/chapters\/664","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/courses.lumenlearning.com\/suny-geophysical\/wp-json\/pressbooks\/v2\/chapters"}],"about":[{"href":"https:\/\/courses.lumenlearning.com\/suny-geophysical\/wp-json\/wp\/v2\/types\/chapter"}],"author":[{"embeddable":true,"href":"https:\/\/courses.lumenlearning.com\/suny-geophysical\/wp-json\/wp\/v2\/users\/17"}],"version-history":[{"count":3,"href":"https:\/\/courses.lumenlearning.com\/suny-geophysical\/wp-json\/pressbooks\/v2\/chapters\/664\/revisions"}],"predecessor-version":[{"id":730,"href":"https:\/\/courses.lumenlearning.com\/suny-geophysical\/wp-json\/pressbooks\/v2\/chapters\/664\/revisions\/730"}],"part":[{"href":"https:\/\/courses.lumenlearning.com\/suny-geophysical\/wp-json\/pressbooks\/v2\/parts\/593"}],"metadata":[{"href":"https:\/\/courses.lumenlearning.com\/suny-geophysical\/wp-json\/pressbooks\/v2\/chapters\/664\/metadata\/"}],"wp:attachment":[{"href":"https:\/\/courses.lumenlearning.com\/suny-geophysical\/wp-json\/wp\/v2\/media?parent=664"}],"wp:term":[{"taxonomy":"chapter-type","embeddable":true,"href":"https:\/\/courses.lumenlearning.com\/suny-geophysical\/wp-json\/pressbooks\/v2\/chapter-type?post=664"},{"taxonomy":"contributor","embeddable":true,"href":"https:\/\/courses.lumenlearning.com\/suny-geophysical\/wp-json\/wp\/v2\/contributor?post=664"},{"taxonomy":"license","embeddable":true,"href":"https:\/\/courses.lumenlearning.com\/suny-geophysical\/wp-json\/wp\/v2\/license?post=664"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}