{"id":273,"date":"2024-04-05T17:31:52","date_gmt":"2024-04-05T17:31:52","guid":{"rendered":"https:\/\/fs.wp.odu.edu\/gcutter\/?page_id=273"},"modified":"2024-04-09T16:00:56","modified_gmt":"2024-04-09T16:00:56","slug":"geotraces-epzt-gp16","status":"publish","type":"page","link":"https:\/\/fs.wp.odu.edu\/gcutter\/geotraces-epzt-gp16\/","title":{"rendered":"Geotraces EPZT GP16"},"content":{"rendered":"\n<p><\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><a href=\"https:\/\/fs.wp.odu.edu\/gcutter\/wp-content\/uploads\/sites\/1996\/2024\/04\/GP16_2-scaled.gif\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"460\" src=\"https:\/\/fs.wp.odu.edu\/gcutter\/wp-content\/uploads\/sites\/1996\/2024\/04\/GP16_2-1024x460.gif\" alt=\"\" class=\"wp-image-322\" srcset=\"https:\/\/fs.wp.odu.edu\/gcutter\/wp-content\/uploads\/sites\/1996\/2024\/04\/GP16_2-1024x460.gif 1024w, https:\/\/fs.wp.odu.edu\/gcutter\/wp-content\/uploads\/sites\/1996\/2024\/04\/GP16_2-300x135.gif 300w, https:\/\/fs.wp.odu.edu\/gcutter\/wp-content\/uploads\/sites\/1996\/2024\/04\/GP16_2-768x345.gif 768w, https:\/\/fs.wp.odu.edu\/gcutter\/wp-content\/uploads\/sites\/1996\/2024\/04\/GP16_2-1536x690.gif 1536w, https:\/\/fs.wp.odu.edu\/gcutter\/wp-content\/uploads\/sites\/1996\/2024\/04\/GP16_2-2048x920.gif 2048w\" sizes=\"(max-width: 1024px) 100vw, 1024px\" \/><\/a><\/figure>\n\n\n\n<p>Departed:&nbsp;Manta Ecuador<\/p>\n\n\n\n<p>Date: 25 October 2013<\/p>\n\n\n\n<p>Arrived:&nbsp;Papeete, French Polynesia<\/p>\n\n\n\n<p>Date: 20 December 2013<\/p>\n\n\n\n<p>The East Pacific&nbsp; Zonal Transect (EPZT) GP16 2013 cruise from Peru to Tahiti was the second cruise conducted through the U.S.GEOTRACES Program. A zonal transect in the eastern tropical South Pacific (ETSP) from Peru to Tahiti as the second cruise of the U.S.GEOTRACES Program. This Pacific section includes a large area characterized by high rates of primary production and particle export in the eastern boundary associated with the Peru Upwelling, a large oxygen minimum zone that is a major global sink for fixed nitrogen, and a large hydrothermal plume arising from the East Pacific Rise. This particular section was selected as a result of open planning workshops in 2007 and 2008, with a final recommendation made by the U.S.GEOTRACES Steering Committee in 2009. It is the first part of a two-stage plan that will include a meridional section of the Pacific from Tahiti to Alaska as a subsequent expedition<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><a href=\"https:\/\/fs.wp.odu.edu\/gcutter\/wp-content\/uploads\/sites\/1996\/2024\/04\/image-3.png\"><img loading=\"lazy\" decoding=\"async\" width=\"1020\" height=\"545\" src=\"https:\/\/fs.wp.odu.edu\/gcutter\/wp-content\/uploads\/sites\/1996\/2024\/04\/image-3.png\" alt=\"\" class=\"wp-image-415\" srcset=\"https:\/\/fs.wp.odu.edu\/gcutter\/wp-content\/uploads\/sites\/1996\/2024\/04\/image-3.png 1020w, https:\/\/fs.wp.odu.edu\/gcutter\/wp-content\/uploads\/sites\/1996\/2024\/04\/image-3-300x160.png 300w, https:\/\/fs.wp.odu.edu\/gcutter\/wp-content\/uploads\/sites\/1996\/2024\/04\/image-3-768x410.png 768w\" sizes=\"(max-width: 1020px) 100vw, 1020px\" \/><\/a><\/figure>\n","protected":false},"excerpt":{"rendered":"<p>Departed:&nbsp;Manta Ecuador Date: 25 October 2013 Arrived:&nbsp;Papeete, French Polynesia Date: 20 December 2013 The East&#8230;<\/p>\n<div class=\"more-link-wrapper\"><a class=\"more-link\" href=\"https:\/\/fs.wp.odu.edu\/gcutter\/geotraces-epzt-gp16\/\">Read the post<span class=\"screen-reader-text\">Geotraces EPZT GP16<\/span><\/a><\/div>\n","protected":false},"author":26740,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"_links":{"self":[{"href":"https:\/\/fs.wp.odu.edu\/gcutter\/wp-json\/wp\/v2\/pages\/273"}],"collection":[{"href":"https:\/\/fs.wp.odu.edu\/gcutter\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/fs.wp.odu.edu\/gcutter\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/fs.wp.odu.edu\/gcutter\/wp-json\/wp\/v2\/users\/26740"}],"replies":[{"embeddable":true,"href":"https:\/\/fs.wp.odu.edu\/gcutter\/wp-json\/wp\/v2\/comments?post=273"}],"version-history":[{"count":5,"href":"https:\/\/fs.wp.odu.edu\/gcutter\/wp-json\/wp\/v2\/pages\/273\/revisions"}],"predecessor-version":[{"id":418,"href":"https:\/\/fs.wp.odu.edu\/gcutter\/wp-json\/wp\/v2\/pages\/273\/revisions\/418"}],"wp:attachment":[{"href":"https:\/\/fs.wp.odu.edu\/gcutter\/wp-json\/wp\/v2\/media?parent=273"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}