{"id":6765,"date":"2024-04-12T14:38:47","date_gmt":"2024-04-12T12:38:47","guid":{"rendered":"https:\/\/muzeumewolucji.pl\/?p=6765"},"modified":"2025-03-07T13:14:58","modified_gmt":"2025-03-07T12:14:58","slug":"ocean-temperature-reconstruction","status":"publish","type":"post","link":"https:\/\/muzeumewolucji.pl\/?p=6765&lang=en","title":{"rendered":"Ocean temperature reconstruction"},"content":{"rendered":"\t\t
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Ocean temperature reconstruction<\/h3>\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t
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\"\"<\/p>

The published study offers a comprehensive analysis of geochemical<\/a> proxies<\/a> extracted from reef coral skeletons (Porites<\/i> and Diploastrea<\/i>) aimed to reconstruct sea surface temperature<\/a> (SST). Employing a multi-element<\/a> approach (e.g., Sr\/Ca and Li\/Mg) notably reduced uncertainties in temperature calibration. Discrepancies in SST reconstructions were more pronounced in Porites<\/i> compared to Diploastrea<\/i> colonies, attributed to variations in ratios between major microstructural skeletal components. These ratios influence the integration of trace elements<\/a> and reflect physiological differences between taxa<\/a>.<\/div>
\u00a0<\/div>

Figure: Reconstruction of sea surface temperature (SST) based on multi-proxy analysis of elements in the skeletons of reef corals Porites<\/i> and Diploastrea<\/i> (upper panel), and differences in ratios between major microstructural skeletal components (Rapid Accretion Deposits vs. Thickening Deposits) in Porites<\/i> and Diploastrea<\/i> (lower panel).<\/p>\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t

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PUBLICATION:<\/b> Canesi, M., Douville, E., Montagna, P., Bordier, L., Caquineau, S., Pons-Branchu, E., Iwankow, G., Stolarski, J.<\/a>, Allemand, D., Planes, S., Moulin, C., Lombard, F., Bourdin, G., Troubl\u00e9, R., Agostini, S., Banaigs, B., Boissin, E., Boss, E., Bowler, C., Vargas, C., Flores, M., Forcioli, D., Furla, P., Gilson, E., Galand, P.E., Pesant, S., Sunagawa, S., Thomas, O., Thurber, R.V., Voolstra, C.R., Wincker, P., Zoccola, D., Reynaud, S. 2024. Sea surface temperature reconstruction in the Pacific Ocean using multi-elemental proxy in Porites<\/i> and Diploastrea<\/i> corals: Application to Palau Archipelago. Chemical Geology<\/i> 645: 121884<\/a>, doi:10.1016\/j.chemgeo.2023.121884.<\/p>\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t\t\t\t<\/div>\n\t\t","protected":false},"excerpt":{"rendered":"

Reconstruction of the Ocean surface water temperature based on calibration of many geochemical indicators from skeletons.<\/p>\n","protected":false},"author":3,"featured_media":6759,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_jetpack_memberships_contains_paid_content":false,"footnotes":""},"categories":[93],"tags":[],"class_list":["post-6765","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-sc_news"],"yoast_head":"\nOcean temperature reconstruction - Muzeum Ewolucji Instytutu Paleobiologii PAN<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/muzeumewolucji.pl\/?p=6765&lang=en\" \/>\n<meta property=\"og:locale\" content=\"pl_PL\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Ocean temperature reconstruction - Muzeum Ewolucji Instytutu Paleobiologii PAN\" \/>\n<meta property=\"og:description\" content=\"Reconstruction of the Ocean surface water temperature based on calibration of many geochemical indicators from skeletons.\" \/>\n<meta property=\"og:url\" content=\"https:\/\/muzeumewolucji.pl\/?p=6765&lang=en\" \/>\n<meta property=\"og:site_name\" content=\"Muzeum Ewolucji Instytutu Paleobiologii PAN\" \/>\n<meta property=\"article:published_time\" content=\"2024-04-12T12:38:47+00:00\" \/>\n<meta property=\"article:modified_time\" content=\"2025-03-07T12:14:58+00:00\" \/>\n<meta property=\"og:image\" content=\"https:\/\/muzeumewolucji.pl\/wp-content\/uploads\/2024\/04\/Canesi_2024_POP.jpg\" \/>\n\t<meta property=\"og:image:width\" content=\"2507\" \/>\n\t<meta property=\"og:image:height\" content=\"2089\" \/>\n\t<meta property=\"og:image:type\" content=\"image\/jpeg\" \/>\n<meta name=\"author\" content=\"Agnieszka K.\" \/>\n<meta name=\"twitter:card\" content=\"summary_large_image\" \/>\n<meta name=\"twitter:label1\" content=\"Napisane przez\" \/>\n\t<meta name=\"twitter:data1\" content=\"Agnieszka K.\" \/>\n\t<meta name=\"twitter:label2\" content=\"Szacowany czas czytania\" \/>\n\t<meta name=\"twitter:data2\" content=\"1 minuta\" \/>\n<script type=\"application\/ld+json\" class=\"yoast-schema-graph\">{\"@context\":\"https:\/\/schema.org\",\"@graph\":[{\"@type\":\"Article\",\"@id\":\"https:\/\/muzeumewolucji.pl\/?p=6765&lang=en#article\",\"isPartOf\":{\"@id\":\"https:\/\/muzeumewolucji.pl\/?p=6765&lang=en\"},\"author\":{\"name\":\"Agnieszka K.\",\"@id\":\"https:\/\/muzeumewolucji.pl\/#\/schema\/person\/71a186d6f255ae6d2725b8c048ab5eb7\"},\"headline\":\"Ocean temperature reconstruction\",\"datePublished\":\"2024-04-12T12:38:47+00:00\",\"dateModified\":\"2025-03-07T12:14:58+00:00\",\"mainEntityOfPage\":{\"@id\":\"https:\/\/muzeumewolucji.pl\/?p=6765&lang=en\"},\"wordCount\":225,\"publisher\":{\"@id\":\"https:\/\/muzeumewolucji.pl\/#organization\"},\"image\":{\"@id\":\"https:\/\/muzeumewolucji.pl\/?p=6765&lang=en#primaryimage\"},\"thumbnailUrl\":\"https:\/\/i0.wp.com\/muzeumewolucji.pl\/wp-content\/uploads\/2024\/04\/Canesi_2024_POP.jpg?fit=2507%2C2089&ssl=1\",\"articleSection\":[\"Science News\"],\"inLanguage\":\"pl-PL\"},{\"@type\":\"WebPage\",\"@id\":\"https:\/\/muzeumewolucji.pl\/?p=6765&lang=en\",\"url\":\"https:\/\/muzeumewolucji.pl\/?p=6765&lang=en\",\"name\":\"Ocean temperature reconstruction - 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