{"id":1027,"date":"2022-09-05T17:51:14","date_gmt":"2022-09-05T17:51:14","guid":{"rendered":"https:\/\/imars.marine.usf.edu\/?page_id=1027"},"modified":"2024-06-14T16:39:36","modified_gmt":"2024-06-14T16:39:36","slug":"cariaco","status":"publish","type":"page","link":"https:\/\/imars.usf.edu\/?page_id=1027","title":{"rendered":"CARIACO Ocean Time-Series Program"},"content":{"rendered":"\n<p><\/p>\n\n\n\n<div class=\"wp-block-group\" style=\"padding-top:var(--wp--preset--spacing--60);padding-right:var(--wp--preset--spacing--40);padding-bottom:var(--wp--preset--spacing--60);padding-left:var(--wp--preset--spacing--40)\"><div class=\"wp-block-group__inner-container is-layout-constrained wp-container-core-group-is-layout-bfcbe384 wp-block-group-is-layout-constrained\"><style id=\"kb-image_267208-3e\">.kb-image_267208-3e.kb-image-is-ratio-size, .kb-image_267208-3e .kb-image-is-ratio-size{max-width:696px;width:100%;}.kb-image_267208-3e{max-width:696px;}.image-is-svg.kb-image_267208-3e img{width:100%;}<\/style>\n<figure class=\"wp-block-kadence-image kb-image_267208-3e size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"266\" height=\"90\" src=\"http:\/\/imars.usf.edu\/wp-content\/uploads\/2024\/06\/CARIACO_logo.jpg\" alt=\"\" class=\"kb-img wp-image-1137\"\/><\/figure>\n\n\n\n<p class=\"has-medium-font-size\" style=\"padding-top:var(--wp--preset--spacing--30);padding-right:var(--wp--preset--spacing--30);padding-bottom:var(--wp--preset--spacing--30);padding-left:var(--wp--preset--spacing--30)\">The CARIACO Ocean Time-Series Program collected various oceanographic parameters from 1995 until 2017 at the Cariaco station (10\u00b030\u2019N, 64\u00b040\u2019W). The Cariaco Basin, located off eastern Venezuela in the southeastern Caribbean Sea, is the world&#8217;s largest marine anoxic basin and the site of one of the longest-running oceanographic studies on record (CARIACO). The Cariaco Basin exhibits pronounced seasonal and interannual variations in hydrographic properties and primary production due to seasonal coastal upwelling. Additionally, due to its restricted circulation and high primary production, the basin is anoxic below approximately 250 meters.<\/p>\n\n\n\n<p class=\"has-medium-font-size\" style=\"padding-top:var(--wp--preset--spacing--30);padding-right:var(--wp--preset--spacing--30);padding-bottom:var(--wp--preset--spacing--30);padding-left:var(--wp--preset--spacing--30)\">Monthly oceanographic cruises were conducted aboard the R\/V Hermano Gin\u00e9s of the Fundaci\u00f3n La Salle de Ciencias Naturales de Venezuela. These cruises collected data on hydrographic conditions, nutrient and carbon concentrations, primary productivity, phytoplankton and zooplankton populations, and other biogeochemical observations throughout the water column (surface to 1300 meters). Additional seasonal cruises to the station focused on chemical and microbial processes. The downward flux of particulate material was measured using sediment traps moored at various depths.<\/p>\n\n\n\n<p class=\"has-medium-font-size\" style=\"padding-top:var(--wp--preset--spacing--30);padding-right:var(--wp--preset--spacing--30);padding-bottom:var(--wp--preset--spacing--30);padding-left:var(--wp--preset--spacing--30)\">Different datasets generated by the CARIACO Oceanographic Time-Series are available through USF Digital Commons (<a href=\"https:\/\/digitalcommons.usf.edu\/msc_facpub\/2587\/\">https:\/\/digitalcommons.usf.edu\/msc_facpub\/2587\/<\/a>).<\/p>\n<\/div><\/div>\n\n\n<style id=\"kb-image_8173d7-ed\">.kb-image_8173d7-ed.kb-image-is-ratio-size, .kb-image_8173d7-ed .kb-image-is-ratio-size{max-width:881px;width:100%;}.kb-image_8173d7-ed{max-width:881px;}.image-is-svg.kb-image_8173d7-ed img{width:100%;}<\/style>\n<figure class=\"wp-block-kadence-image kb-image_8173d7-ed size-full\"><img loading=\"lazy\" decoding=\"async\" width=\"364\" height=\"215\" src=\"http:\/\/imars.usf.edu\/wp-content\/uploads\/2024\/06\/CariacoBasin.jpg\" alt=\"\" class=\"kb-img wp-image-1138\" srcset=\"https:\/\/imars.usf.edu\/wp-content\/uploads\/2024\/06\/CariacoBasin.jpg 364w, https:\/\/imars.usf.edu\/wp-content\/uploads\/2024\/06\/CariacoBasin-300x177.jpg 300w\" sizes=\"auto, (max-width: 364px) 100vw, 364px\" \/><\/figure>\n\n\n\n<p class=\"has-medium-font-size\" style=\"padding-top:var(--wp--preset--spacing--50);padding-right:var(--wp--preset--spacing--50);padding-bottom:var(--wp--preset--spacing--50);padding-left:var(--wp--preset--spacing--50)\"><strong>Additional links:<\/strong><\/p>\n\n\n\n<p style=\"padding-top:var(--wp--preset--spacing--50);padding-right:var(--wp--preset--spacing--50);padding-bottom:var(--wp--preset--spacing--50);padding-left:var(--wp--preset--spacing--50)\"><strong><em>NOAA National Centers for Environmental Information (NCEI):<\/em><\/strong><br>Zooplankton:<a href=\" http:\/\/accession.nodc.noaa.gov\/0191571 \"> http:\/\/accession.nodc.noaa.gov\/0191571 <\/a><br>Phytoplankton: <a href=\"http:\/\/accession.nodc.noaa.gov\/0191567\">http:\/\/accession.nodc.noaa.gov\/0191567<\/a><br>Biogeochemical and microbiological data: <a href=\"http:\/\/accession.nodc.noaa.gov\/0191401\">http:\/\/accession.nodc.noaa.gov\/0191401<\/a><br>Composite CTD: <a href=\"https:\/\/accession.nodc.noaa.gov\/0189595\">https:\/\/accession.nodc.noaa.gov\/0189595<\/a><br>Niskin bottle data: <a href=\"https:\/\/accession.nodc.noaa.gov\/0201747\">https:\/\/accession.nodc.noaa.gov\/0201747<\/a><\/p>\n\n\n\n<p style=\"padding-top:var(--wp--preset--spacing--50);padding-right:var(--wp--preset--spacing--50);padding-bottom:var(--wp--preset--spacing--50);padding-left:var(--wp--preset--spacing--50)\"><em><strong>SeaWiFS Bio-optical Archive and Storage System (SeaBASS)<\/strong>:<\/em><br><a href=\"https:\/\/seabass.gsfc.nasa.gov\/experiment\/CARIACO\">https:\/\/seabass.gsfc.nasa.gov\/experiment\/CARIACO<\/a> (DOI: 10.5067\/SeaBASS\/CARIACO\/DATA001)<br>For Niskin Chlorophyll and phaeopigments, CTD fluorescence, beam attenuation, salinity, temperature, Niskin HPLC, PRR, Surface Spectra.<\/p>\n\n\n\n<p style=\"padding-top:var(--wp--preset--spacing--50);padding-right:var(--wp--preset--spacing--50);padding-bottom:var(--wp--preset--spacing--50);padding-left:var(--wp--preset--spacing--50)\"><strong><em>Biological and Chemical Oceanography Data Management Office (BCO-DMO)<\/em><\/strong><br>Hydrographic data (Niskin bottle samples): <a href=\"https:\/\/www.bco-dmo.org\/dataset\/3093\">https:\/\/www.bco-dmo.org\/dataset\/3093<\/a><br>Biogeochemistry microbiology: <a href=\"https:\/\/www.bco-dmo.org\/dataset\/3120\">https:\/\/www.bco-dmo.org\/dataset\/3120<\/a><br>Phytoplankton taxonomy: <a href=\"https:\/\/www.bco-dmo.org\/dataset\/3095\">https:\/\/www.bco-dmo.org\/dataset\/3095<\/a><br>Zooplankton biomass: <a href=\"https:\/\/www.bco-dmo.org\/dataset\/3149\">https:\/\/www.bco-dmo.org\/dataset\/3149<\/a><br>CTD Composite Profiles:<a href=\" https:\/\/www.bco-dmo.org\/dataset\/3092\"> https:\/\/www.bco-dmo.org\/dataset\/3092<\/a><br>CTD individual files: <a href=\"https:\/\/www.bco-dmo.org\/dataset\/773146\">https:\/\/www.bco-dmo.org\/dataset\/773146<\/a><br>HPLC from four laboratories: <a href=\"https:\/\/www.bco-dmo.org\/dataset\/3293\">https:\/\/www.bco-dmo.org\/dataset\/3293<\/a>, <a href=\"https:\/\/www.bco-dmo.org\/dataset\/3292\">https:\/\/www.bco-dmo.org\/dataset\/3292<\/a>, <a href=\"https:\/\/www.bco-dmo.org\/dataset\/3235\">https:\/\/www.bco-dmo.org\/dataset\/3235<\/a>, <a href=\"https:\/\/www.bco-dmo.org\/dataset\/777689\">https:\/\/www.bco-dmo.org\/dataset\/777689<\/a>.<\/p>\n\n\n\n<p style=\"padding-top:var(--wp--preset--spacing--50);padding-right:var(--wp--preset--spacing--50);padding-bottom:var(--wp--preset--spacing--50);padding-left:var(--wp--preset--spacing--50)\"><\/p>\n\n\n\n<p style=\"padding-top:var(--wp--preset--spacing--30);padding-right:var(--wp--preset--spacing--30);padding-bottom:var(--wp--preset--spacing--30);padding-left:var(--wp--preset--spacing--30)\"><\/p>\n","protected":false},"excerpt":{"rendered":"<p>The CARIACO Ocean Time-Series Program collected various oceanographic parameters from 1995 until 2017 at the Cariaco station (10\u00b030\u2019N, 64\u00b040\u2019W). The Cariaco Basin, located off eastern Venezuela in the southeastern Caribbean Sea, is the world&#8217;s largest marine anoxic basin and the site of one of the longest-running oceanographic studies on record (CARIACO). The Cariaco Basin exhibits&#8230;<\/p>\n","protected":false},"author":2,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_kad_post_transparent":"","_kad_post_title":"","_kad_post_layout":"","_kad_post_sidebar_id":"","_kad_post_content_style":"","_kad_post_vertical_padding":"","_kad_post_feature":"","_kad_post_feature_position":"","_kad_post_header":false,"_kad_post_footer":false,"footnotes":""},"class_list":["post-1027","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/imars.usf.edu\/index.php?rest_route=\/wp\/v2\/pages\/1027","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/imars.usf.edu\/index.php?rest_route=\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/imars.usf.edu\/index.php?rest_route=\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/imars.usf.edu\/index.php?rest_route=\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/imars.usf.edu\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=1027"}],"version-history":[{"count":22,"href":"https:\/\/imars.usf.edu\/index.php?rest_route=\/wp\/v2\/pages\/1027\/revisions"}],"predecessor-version":[{"id":1154,"href":"https:\/\/imars.usf.edu\/index.php?rest_route=\/wp\/v2\/pages\/1027\/revisions\/1154"}],"wp:attachment":[{"href":"https:\/\/imars.usf.edu\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=1027"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}