{"id":3,"date":"2024-04-04T05:55:38","date_gmt":"2024-04-04T02:55:38","guid":{"rendered":"https:\/\/sisu.ut.ee\/eluarengmaal\/juhtkivistis\/"},"modified":"2024-04-04T05:56:27","modified_gmt":"2024-04-04T02:56:27","slug":"juhtkivistis","status":"publish","type":"page","link":"https:\/\/sisu.ut.ee\/eluarengmaal\/juhtkivistis\/","title":{"rendered":"Juhtkivistis"},"content":{"rendered":"<p>\n\t<font face=\"Arial\"><font style=\"medium;font-style:normal;font-weight:400;letter-spacing:normal;text-align:start;text-indent:0px;text-transform:none\"><b>Juhtkivistis<\/b>\u00a0on suhteliselt l\u00fchikeses ajavahemikus, kuid suurel alal elutsenud organismi kivistis. Juhtkivistised v\u00f5imaldavad kindlaks m\u00e4\u00e4rata neid sisaldavate kivimite tekkeaega, enamasti on juhtkivivtisteks mingit kindlat liiki organismi kivistised. Eriti h\u00e4id juhtkivistisi on\u00a0<\/font><\/font><a data-url=\"https:\/\/sisu.ut.ee\/eluarengmaal\/graptoliidid\" href=\"https:\/\/sisu.ut.ee\/eluarengmaal\/graptoliidid\" target=\"_blank\" title=\"\" rel=\"noopener\">graptoliitide<\/a><font face=\"Arial\"><font style=\"medium;font-style:normal;font-weight:400;letter-spacing:normal;text-align:start;text-indent:0px;text-transform:none\">\u00a0ja <\/font><\/font><a data-url=\"https:\/\/sisu.ut.ee\/eluarengmaal\/ammoniidid\" href=\"https:\/\/sisu.ut.ee\/eluarengmaal\/ammoniidid\" target=\"_blank\" title=\"\" rel=\"noopener\">ammoniitide<\/a><font face=\"Arial\"><font style=\"medium;font-style:normal;font-weight:400;letter-spacing:normal;text-align:start;text-indent:0px;text-transform:none\"> hulgas.<\/font><\/font>\n<\/p>\n<p>\n\t<img loading=\"lazy\" decoding=\"async\" width=\"84\" height=\"120\" class=\"alignnone wp-image-98\" src=\"https:\/\/sisu.ut.ee\/wp-content\/uploads\/sites\/426\/grapt_2a.jpg\" title=\"grapt_2a.jpg\" alt=\"grapt2\"><br><font face=\"Arial\">Foto 1. Graptoliit, Panga pank, Jaani lade<\/font>\n<\/p>\n<p style=\"text-align:start\">\n\t<br><span><span style=\"color:#000000\"><span><span style=\"font-style:normal\"><span><span><span style=\"font-weight:400\"><span style=\"letter-spacing:normal\"><span><span style=\"text-transform:none\"><span><span><span><span><span>Koostanud ja fotografeerinud \u00a9 2003 Mare Isakar<\/span><\/span><\/span><\/span><\/span><\/span><\/span><\/span><\/span><\/span><\/span><\/span><\/span><\/span><\/span><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Juhtkivistis\u00a0on suhteliselt l\u00fchikeses ajavahemikus, kuid suurel alal elutsenud organismi kivistis. Juhtkivistised v\u00f5imaldavad kindlaks m\u00e4\u00e4rata neid sisaldavate kivimite tekkeaega, enamasti on juhtkivivtisteks mingit kindlat liiki organismi kivistised. Eriti h\u00e4id juhtkivistisi on\u00a0graptoliitide\u00a0ja ammoniitide hulgas. Foto 1. Graptoliit, Panga pank, Jaani lade Koostanud &#8230;<\/p>\n","protected":false},"author":226,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_acf_changed":false,"inline_featured_image":false,"footnotes":""},"class_list":["post-3","page","type-page","status-publish","hentry"],"acf":[],"_links":{"self":[{"href":"https:\/\/sisu.ut.ee\/eluarengmaal\/wp-json\/wp\/v2\/pages\/3","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/sisu.ut.ee\/eluarengmaal\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/sisu.ut.ee\/eluarengmaal\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/sisu.ut.ee\/eluarengmaal\/wp-json\/wp\/v2\/users\/226"}],"replies":[{"embeddable":true,"href":"https:\/\/sisu.ut.ee\/eluarengmaal\/wp-json\/wp\/v2\/comments?post=3"}],"version-history":[{"count":1,"href":"https:\/\/sisu.ut.ee\/eluarengmaal\/wp-json\/wp\/v2\/pages\/3\/revisions"}],"predecessor-version":[{"id":491,"href":"https:\/\/sisu.ut.ee\/eluarengmaal\/wp-json\/wp\/v2\/pages\/3\/revisions\/491"}],"wp:attachment":[{"href":"https:\/\/sisu.ut.ee\/eluarengmaal\/wp-json\/wp\/v2\/media?parent=3"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}