{"id":1012019,"date":"2026-02-26T13:19:17","date_gmt":"2026-02-26T12:19:17","guid":{"rendered":"https:\/\/new.obsnev.es\/?post_type=protocolos&#038;p=1012019"},"modified":"2026-02-27T09:41:14","modified_gmt":"2026-02-27T08:41:14","slug":"analisis-de-indicadores-paleolimnologicos-en-las-lagunas-de-sierra-nevada","status":"publish","type":"protocolos","link":"https:\/\/obsnev.es\/en\/protocolos\/analisis-de-indicadores-paleolimnologicos-en-las-lagunas-de-sierra-nevada\/","title":{"rendered":"An\u00e1lisis de indicadores paleolimnol\u00f3gicos en las lagunas de Sierra Nevada"},"content":{"rendered":"<div data-elementor-type=\"wp-post\" data-elementor-id=\"1012019\" class=\"elementor elementor-1012019\" data-elementor-post-type=\"protocolos\">\n\t\t\t\t<div class=\"elementor-element elementor-element-63787e3 e-flex e-con-boxed e-con e-parent\" data-id=\"63787e3\" data-element_type=\"container\" data-e-type=\"container\">\n\t\t\t\t\t<div class=\"e-con-inner\">\n\t\t\t\t<div class=\"elementor-element elementor-element-4db42ea elementor-widget elementor-widget-text-editor\" data-id=\"4db42ea\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<div id=\"panel-gb4326-69a033732152e-0-0-0\" class=\"so-panel widget widget_sow-editor panel-first-child\" data-index=\"0\"><div class=\"fila_ficha panel-widget-style panel-widget-style-for-gb4326-69a033732152e-0-0-0\"><div class=\"so-widget-sow-editor so-widget-sow-editor-base\"><h3 class=\"widget-title\">Aims<\/h3><div class=\"siteorigin-widget-tinymce textwidget\"><p>The analysis of the fossil record of aquatic organisms in the lakes of Sierra Nevada enable us to evaluate the changes undergone in these ecosystems over a broad time interval.  The groups analysed are diatoms, cladocerans, and chironomids, at a time scale of roughly 200 years.<\/p><\/div><\/div><\/div><\/div>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-e2fa565 elementor-widget elementor-widget-image\" data-id=\"e2fa565\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<img fetchpriority=\"high\" decoding=\"async\" width=\"992\" height=\"430\" src=\"https:\/\/obsnev.es\/wp-content\/uploads\/2019\/09\/Figura_1_2_1-1_ES.png\" class=\"attachment-2048x2048 size-2048x2048 wp-image-4587\" alt=\"\" srcset=\"https:\/\/obsnev.es\/wp-content\/uploads\/2019\/09\/Figura_1_2_1-1_ES.png 992w, https:\/\/obsnev.es\/wp-content\/uploads\/2019\/09\/Figura_1_2_1-1_ES-300x130.png 300w, https:\/\/obsnev.es\/wp-content\/uploads\/2019\/09\/Figura_1_2_1-1_ES-768x333.png 768w, https:\/\/obsnev.es\/wp-content\/uploads\/2019\/09\/Figura_1_2_1-1_ES-18x8.png 18w\" sizes=\"(max-width: 992px) 100vw, 992px\" \/>\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-95f591f elementor-widget elementor-widget-text-editor\" data-id=\"95f591f\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<div id=\"panel-gb4326-69a033732152e-0-0-0\" class=\"so-panel widget widget_sow-editor panel-first-child\" data-index=\"0\"><div class=\"fila_ficha panel-widget-style panel-widget-style-for-gb4326-69a033732152e-0-0-0\"><div class=\"so-widget-sow-editor so-widget-sow-editor-base\"><div id=\"panel-gb4326-69a033732152e-0-0-2\" class=\"so-panel widget widget_sow-editor\" data-index=\"2\"><div class=\"fila_ficha panel-widget-style panel-widget-style-for-gb4326-69a033732152e-0-0-2\"><div class=\"so-widget-sow-editor so-widget-sow-editor-base\"><h3 class=\"widget-title\">Method and effort<\/h3><div class=\"siteorigin-widget-tinymce textwidget\"><p>Cores samples are taken from the sediment in the zone of maximum depth of several lakes.  The length of the cores must span the last two centuries and they are selected in intervals of 0.25 cm in the first 7 cm, and 0.5 cm in the following ones.  The sediments are dated radiometrically by gamma and alpha spectrometry.<\/p><p>In each interval of sediment, the fossils of different species of diatoms, cladocerans, and chironomids are identified and specific abundance is determined.<\/p><\/div><\/div><\/div><\/div><\/div><\/div><\/div>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-07a90e4 elementor-widget elementor-widget-image\" data-id=\"07a90e4\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<img decoding=\"async\" width=\"544\" height=\"592\" src=\"https:\/\/obsnev.es\/wp-content\/uploads\/2019\/09\/Figura_1_2_1-2_ES.png\" class=\"attachment-2048x2048 size-2048x2048 wp-image-4590\" alt=\"\" srcset=\"https:\/\/obsnev.es\/wp-content\/uploads\/2019\/09\/Figura_1_2_1-2_ES.png 544w, https:\/\/obsnev.es\/wp-content\/uploads\/2019\/09\/Figura_1_2_1-2_ES-276x300.png 276w, https:\/\/obsnev.es\/wp-content\/uploads\/2019\/09\/Figura_1_2_1-2_ES-11x12.png 11w\" sizes=\"(max-width: 544px) 100vw, 544px\" \/>\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-0f416af elementor-widget elementor-widget-text-editor\" data-id=\"0f416af\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<div id=\"panel-gb4326-69a033732152e-0-0-0\" class=\"so-panel widget widget_sow-editor panel-first-child\" data-index=\"0\"><div class=\"fila_ficha panel-widget-style panel-widget-style-for-gb4326-69a033732152e-0-0-0\"><div class=\"so-widget-sow-editor so-widget-sow-editor-base\"><div id=\"panel-gb4326-69a033732152e-0-0-2\" class=\"so-panel widget widget_sow-editor\" data-index=\"2\"><div class=\"fila_ficha panel-widget-style panel-widget-style-for-gb4326-69a033732152e-0-0-2\"><div class=\"so-widget-sow-editor so-widget-sow-editor-base\"><div id=\"panel-gb4581-69a0338952d0b-0-0-2\" class=\"so-panel widget widget_sow-editor\" data-index=\"2\"><div class=\"so-widget-sow-editor so-widget-sow-editor-base\"><h3 class=\"widget-title\">Periodicity<\/h3><div class=\"siteorigin-widget-tinymce textwidget\"><p>These samples are taken only once.<\/p><\/div><\/div><\/div><div id=\"panel-gb4581-69a0338952d0b-0-0-3\" class=\"so-panel widget widget_sow-editor\" data-index=\"3\"><div class=\"so-widget-sow-editor so-widget-sow-editor-base\"><h3 class=\"widget-title\">Results<\/h3><div class=\"siteorigin-widget-tinymce textwidget\"><p>Download PDF:\u00a0<a href=\"https:\/\/obsnev.es\/wp-content\/uploads\/2019\/12\/121_Indicadores_Paleolimnologicos_RESULTADOS.pdf\" target=\"_blank\" rel=\"noopener\">Espa\u00f1ol<\/a>\u00a0\/\u00a0<a href=\"https:\/\/obsnev.es\/wp-content\/uploads\/2019\/12\/121_Indicadores_Paleolimnologicos_RESULTS.pdf\" target=\"_blank\" rel=\"noopener\">English<\/a><\/p><\/div><\/div><\/div><div id=\"panel-gb4581-69a0338952d0b-0-0-4\" class=\"so-panel widget widget_sow-editor panel-last-child\" data-index=\"4\"><div class=\"so-widget-sow-editor so-widget-sow-editor-base\"><h3 class=\"widget-title\">References<\/h3><div class=\"siteorigin-widget-tinymce textwidget\"><p>Smol, J.P. (Series Editor). 2001. Developments in Paleoenvironmental Research (DPER Series): Tracking Environmental Change Using Lake Sediments, vols 1 a 5. Springer-Verlag.<\/p><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div><\/div>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<\/div>","protected":false},"featured_media":4587,"template":"","meta":{"_acf_changed":false},"ambito-tematico":[345],"class_list":["post-1012019","protocolos","type-protocolos","status-publish","has-post-thumbnail","hentry","ambito-tematico-reconstruccion-del-pasado"],"acf":[],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/obsnev.es\/en\/wp-json\/wp\/v2\/protocolos\/1012019","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/obsnev.es\/en\/wp-json\/wp\/v2\/protocolos"}],"about":[{"href":"https:\/\/obsnev.es\/en\/wp-json\/wp\/v2\/types\/protocolos"}],"version-history":[{"count":5,"href":"https:\/\/obsnev.es\/en\/wp-json\/wp\/v2\/protocolos\/1012019\/revisions"}],"predecessor-version":[{"id":1012080,"href":"https:\/\/obsnev.es\/en\/wp-json\/wp\/v2\/protocolos\/1012019\/revisions\/1012080"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/obsnev.es\/en\/wp-json\/wp\/v2\/media\/4587"}],"wp:attachment":[{"href":"https:\/\/obsnev.es\/en\/wp-json\/wp\/v2\/media?parent=1012019"}],"wp:term":[{"taxonomy":"ambito-tematico","embeddable":true,"href":"https:\/\/obsnev.es\/en\/wp-json\/wp\/v2\/ambito-tematico?post=1012019"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}