{"id":9,"date":"2018-09-07T13:22:15","date_gmt":"2018-09-07T17:22:15","guid":{"rendered":"https:\/\/www2.whoi.edu\/staff\/template-blue-prepop\/?page_id=9"},"modified":"2024-03-08T09:41:00","modified_gmt":"2024-03-08T13:41:00","slug":"gallery","status":"publish","type":"page","link":"https:\/\/www2.whoi.edu\/staff\/adunlea\/gallery\/","title":{"rendered":"Gallery"},"content":{"rendered":"\n\n\t<h1>Research Expedition Photo Gallery<\/h1>\n<p>Our research projects start when we sail on research cruises, often 20 to 60 days at sea, to core sediment from the seafloor. Deeper layers of sediment were deposited earlier than the shallower layers, so coring deep below the seafloor is like looking back through time. Many land and ocean processes affect the type and geochemistry of marine sediment that accumulates on the seafloor. By analyzing different layers in the core, we can determine how these processes have changed over time.<\/p>\n<p>Check out the gallery of photos from research expeditions I&#8217;ve sailed on for an idea of what it is like coring marine sediment and doing science at sea.<\/p>\n\t\r\n<div class=\"aigpl-gallery-album-wrp aigpl-gallery-album aigpl-album-design-1 aigpl-clearfix \" id=\"aigpl-gallery-1\">\r\n<div class=\"aigpl-cnt-wrp aigpl-col-4 aigpl-columns aigpl-first\" data-id=\"75\">\r\n\t<div class=\"aigpl-inr-wrp\">\r\n\t\t<div class=\"aigpl-img-wrp\" style=\"\">\r\n\t\t\t<a class=\"aigpl-img-link\" href=\"https:\/\/www2.whoi.edu\/staff\/adunlea\/gallery\/?album=75&#038;album_ses=1\" target=\"_self\">\r\n\t\t\t\t\t\t\t\t<img class=\"aigpl-img\"  src=\"https:\/\/www2.whoi.edu\/staff\/adunlea\/wp-content\/uploads\/sites\/196\/2018\/09\/IMG_4770.jpg\" alt=\"Line Islands Ridge Paleoceanography\" title=\"Line Islands Ridge Paleoceanography\" \/>\r\n\t\t\t\t\t\t\t<\/a>\r\n\t\t<\/div>\r\n\t\t<div class=\"aigpl-desc-wrapper\">\r\n\t\t\t\t\t\t<a class=\"aigpl-img-link\" href=\"https:\/\/www2.whoi.edu\/staff\/adunlea\/gallery\/?album=75&#038;album_ses=1\" target=\"_self\">\r\n\t\t\t\t<div class=\"aigpl-img-title aigpl-center\">Line Islands Ridge Paleoceanography<\/div>\r\n\t\t\t<\/a>\r\n\t\t\t\r\n\t\t\t\t\t\t<div class=\"aigpl-img-count aigpl-center\">10 Photos<\/div>\r\n\t\t\t\r\n\t\t\t\t\t\t\t<div class=\"aigpl-img-desc aigpl-center\">R\/V Marcus G. Langseth sailed to the Line Islands Ridge to examine glacial-interglacial cycles in the\u00a0central tropical Pacific.<\/div>\r\n\t\t\t\t\t<\/div>\r\n\t<\/div>\r\n<\/div>\r\n<div class=\"aigpl-cnt-wrp aigpl-col-4 aigpl-columns\" data-id=\"76\">\r\n\t<div class=\"aigpl-inr-wrp\">\r\n\t\t<div class=\"aigpl-img-wrp\" style=\"\">\r\n\t\t\t<a class=\"aigpl-img-link\" href=\"https:\/\/www2.whoi.edu\/staff\/adunlea\/gallery\/?album=76&#038;album_ses=1\" target=\"_self\">\r\n\t\t\t\t\t\t\t\t<img class=\"aigpl-img\"  src=\"https:\/\/www2.whoi.edu\/staff\/adunlea\/wp-content\/uploads\/sites\/196\/2018\/09\/Exp-346_Aug-8_Mud-Play-starts4.jpg\" alt=\"East Asian Monsoon\" title=\"East Asian Monsoon\" \/>\r\n\t\t\t\t\t\t\t<\/a>\r\n\t\t<\/div>\r\n\t\t<div class=\"aigpl-desc-wrapper\">\r\n\t\t\t\t\t\t<a class=\"aigpl-img-link\" href=\"https:\/\/www2.whoi.edu\/staff\/adunlea\/gallery\/?album=76&#038;album_ses=1\" target=\"_self\">\r\n\t\t\t\t<div class=\"aigpl-img-title aigpl-center\">East Asian Monsoon<\/div>\r\n\t\t\t<\/a>\r\n\t\t\t\r\n\t\t\t\t\t\t<div class=\"aigpl-img-count aigpl-center\">11 Photos<\/div>\r\n\t\t\t\r\n\t\t\t\t\t\t\t<div class=\"aigpl-img-desc aigpl-center\">The International Ocean Discovery Program's R\/V JOIDES Resolution \u00a0 set out to study the variability of the East Asian Monsoon.<\/div>\r\n\t\t\t\t\t<\/div>\r\n\t<\/div>\r\n<\/div>\r\n<div class=\"aigpl-cnt-wrp aigpl-col-4 aigpl-columns\" data-id=\"77\">\r\n\t<div class=\"aigpl-inr-wrp\">\r\n\t\t<div class=\"aigpl-img-wrp\" style=\"\">\r\n\t\t\t<a class=\"aigpl-img-link\" href=\"https:\/\/www2.whoi.edu\/staff\/adunlea\/gallery\/?album=77&#038;album_ses=1\" target=\"_self\">\r\n\t\t\t\t\t\t\t\t<img class=\"aigpl-img\"  src=\"https:\/\/www2.whoi.edu\/staff\/adunlea\/wp-content\/uploads\/sites\/196\/2018\/09\/P1030219.jpg\" alt=\"Last Glacial Maximum Deep Water Chemistry\" title=\"Last Glacial Maximum Deep Water Chemistry\" \/>\r\n\t\t\t\t\t\t\t<\/a>\r\n\t\t<\/div>\r\n\t\t<div class=\"aigpl-desc-wrapper\">\r\n\t\t\t\t\t\t<a class=\"aigpl-img-link\" href=\"https:\/\/www2.whoi.edu\/staff\/adunlea\/gallery\/?album=77&#038;album_ses=1\" target=\"_self\">\r\n\t\t\t\t<div class=\"aigpl-img-title aigpl-center\">Last Glacial Maximum Deep Water Chemistry<\/div>\r\n\t\t\t<\/a>\r\n\t\t\t\r\n\t\t\t\t\t\t<div class=\"aigpl-img-count aigpl-center\">14 Photos<\/div>\r\n\t\t\t\r\n\t\t\t\t\t\t\t<div class=\"aigpl-img-desc aigpl-center\">The final cruise of the R\/V Knorr collected porewater and sediment from the North Atlantic to examine the chemistry of relict bottom water from the last glacial maximum.<\/div>\r\n\t\t\t\t\t<\/div>\r\n\t<\/div>\r\n<\/div>\r\n<div class=\"aigpl-cnt-wrp aigpl-col-4 aigpl-columns\" data-id=\"125\">\r\n\t<div class=\"aigpl-inr-wrp\">\r\n\t\t<div class=\"aigpl-img-wrp\" style=\"\">\r\n\t\t\t<a class=\"aigpl-img-link\" href=\"https:\/\/www2.whoi.edu\/staff\/adunlea\/gallery\/?album=125&#038;album_ses=1\" target=\"_self\">\r\n\t\t\t\t\t\t\t\t<img class=\"aigpl-img\"  src=\"https:\/\/www2.whoi.edu\/staff\/adunlea\/wp-content\/uploads\/sites\/196\/2018\/09\/IMG_2945_Thomas.jpg\" alt=\"Western Australia Climate History\" title=\"Western Australia Climate History\" \/>\r\n\t\t\t\t\t\t\t<\/a>\r\n\t\t<\/div>\r\n\t\t<div class=\"aigpl-desc-wrapper\">\r\n\t\t\t\t\t\t<a class=\"aigpl-img-link\" href=\"https:\/\/www2.whoi.edu\/staff\/adunlea\/gallery\/?album=125&#038;album_ses=1\" target=\"_self\">\r\n\t\t\t\t<div class=\"aigpl-img-title aigpl-center\">Western Australia Climate History<\/div>\r\n\t\t\t<\/a>\r\n\t\t\t\r\n\t\t\t\t\t\t<div class=\"aigpl-img-count aigpl-center\">10 Photos<\/div>\r\n\t\t\t\r\n\t\t\t\t\t\t\t<div class=\"aigpl-img-desc aigpl-center\">The R\/V SONNE collected sediment archives from the Eastern Indian Ocean to examine climate variability of Western Australia.<\/div>\r\n\t\t\t\t\t<\/div>\r\n\t<\/div>\r\n<\/div>\r\n\t\r\n<\/div>\n\n","protected":false},"excerpt":{"rendered":"<p>The R\/V SONNE collected sediment archives from the Eastern Indian Ocean to examine climate variability of Western Australia.<\/p>\n","protected":false},"author":191,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":[],"_links":{"self":[{"href":"https:\/\/www2.whoi.edu\/staff\/adunlea\/wp-json\/wp\/v2\/pages\/9"}],"collection":[{"href":"https:\/\/www2.whoi.edu\/staff\/adunlea\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www2.whoi.edu\/staff\/adunlea\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www2.whoi.edu\/staff\/adunlea\/wp-json\/wp\/v2\/users\/191"}],"replies":[{"embeddable":true,"href":"https:\/\/www2.whoi.edu\/staff\/adunlea\/wp-json\/wp\/v2\/comments?post=9"}],"version-history":[{"count":3,"href":"https:\/\/www2.whoi.edu\/staff\/adunlea\/wp-json\/wp\/v2\/pages\/9\/revisions"}],"predecessor-version":[{"id":269,"href":"https:\/\/www2.whoi.edu\/staff\/adunlea\/wp-json\/wp\/v2\/pages\/9\/revisions\/269"}],"wp:attachment":[{"href":"https:\/\/www2.whoi.edu\/staff\/adunlea\/wp-json\/wp\/v2\/media?parent=9"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}