{"version":"1.0","provider_name":"Institute of Oceanography, NTU","provider_url":"https:\/\/www.oc.ntu.edu.tw\/en\/","title":"Decoding climate signals and non-climate variability in paleotemperature records - Institute of Oceanography, NTU","type":"rich","width":600,"height":338,"html":"<blockquote class=\"wp-embedded-content\" data-secret=\"1cEmqggtj7\"><a href=\"https:\/\/www.oc.ntu.edu.tw\/en\/research-highlights\/35009\/\">Decoding climate signals and non-climate variability in paleotemperature records<\/a><\/blockquote><iframe sandbox=\"allow-scripts\" security=\"restricted\" src=\"https:\/\/www.oc.ntu.edu.tw\/en\/research-highlights\/35009\/embed\/#?secret=1cEmqggtj7\" width=\"600\" height=\"338\" title=\"&#8220;Decoding climate signals and non-climate variability in paleotemperature records&#8221; &#8212; Institute of Oceanography, NTU\" data-secret=\"1cEmqggtj7\" frameborder=\"0\" marginwidth=\"0\" marginheight=\"0\" scrolling=\"no\" class=\"wp-embedded-content\"><\/iframe><script>\n\/*! This file is auto-generated *\/\n!function(d,l){\"use strict\";l.querySelector&&d.addEventListener&&\"undefined\"!=typeof URL&&(d.wp=d.wp||{},d.wp.receiveEmbedMessage||(d.wp.receiveEmbedMessage=function(e){var t=e.data;if((t||t.secret||t.message||t.value)&&!\/[^a-zA-Z0-9]\/.test(t.secret)){for(var s,r,n,a=l.querySelectorAll('iframe[data-secret=\"'+t.secret+'\"]'),o=l.querySelectorAll('blockquote[data-secret=\"'+t.secret+'\"]'),c=new RegExp(\"^https?:$\",\"i\"),i=0;i<o.length;i++)o[i].style.display=\"none\";for(i=0;i<a.length;i++)s=a[i],e.source===s.contentWindow&&(s.removeAttribute(\"style\"),\"height\"===t.message?(1e3<(r=parseInt(t.value,10))?r=1e3:~~r<200&&(r=200),s.height=r):\"link\"===t.message&&(r=new URL(s.getAttribute(\"src\")),n=new URL(t.value),c.test(n.protocol))&&n.host===r.host&&l.activeElement===s&&(d.top.location.href=t.value))}},d.addEventListener(\"message\",d.wp.receiveEmbedMessage,!1),l.addEventListener(\"DOMContentLoaded\",function(){for(var e,t,s=l.querySelectorAll(\"iframe.wp-embedded-content\"),r=0;r<s.length;r++)(t=(e=s[r]).getAttribute(\"data-secret\"))||(t=Math.random().toString(36).substring(2,12),e.src+=\"#?secret=\"+t,e.setAttribute(\"data-secret\",t)),e.contentWindow.postMessage({message:\"ready\",secret:t},\"*\")},!1)))}(window,document);\n<\/script>\n","thumbnail_url":"https:\/\/www.oc.ntu.edu.tw\/wp-content\/uploads\/2024\/12\/Announcement_fig-scaled.jpg","thumbnail_width":2560,"thumbnail_height":1440,"description":"Instrumental sea surface temperature data only cover the last two centuries. Beyond that, our knowledge of sea surface temperature relies on indirect inference from geochemical indicators in marine sediments known as paleotemperature proxies. Past ocean temperature reconstructions typically rely on a single sediment core to infer climate changes at a study site and across an [&hellip;]"}