{"id":12060,"date":"2026-04-08T11:30:47","date_gmt":"2026-04-08T09:30:47","guid":{"rendered":"https:\/\/www.igg.cnr.it\/?page_id=12060"},"modified":"2026-04-08T11:59:34","modified_gmt":"2026-04-08T09:59:34","slug":"laboratorio-micropaleontologia-pisa","status":"publish","type":"page","link":"https:\/\/www.igg.cnr.it\/en\/laboratorio-micropaleontologia-pisa\/","title":{"rendered":"Micropaleontology Laboratory of Pisa"},"content":{"rendered":"<h6 class=\"wp-block-heading\">The laboratory is housed in the IGG Pisa headquarter<\/h6>\n\n\n\n<div style=\"height:20px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<div class=\"wp-block-essential-blocks-accordion  root-eb-accordion-63d5q\"><div class=\"eb-parent-wrapper eb-parent-eb-accordion-63d5q\"><div class=\"eb-accordion-container eb-accordion-63d5q\" data-accordion-type=\"accordion\" data-tab-icon=\"dashicons-plus-alt2\" data-expanded-icon=\"dashicons-minus\" data-transition-duration=\"500\"><div class=\"eb-accordion-inner\">\n<div class=\"wp-block-essential-blocks-accordion-item eb-accordion-item-jbbes eb-accordion-wrapper\" data-clickable=\"false\"><div class=\"eb-accordion-title-wrapper eb-accordion-title-wrapper-eb-accordion-63d5q\" tabindex=\"0\"><span class=\"eb-accordion-icon-wrapper eb-accordion-icon-wrapper-eb-accordion-63d5q\"><span class=\"dashicon dashicons dashicons-plus-alt2 eb-accordion-icon\"><\/span><\/span><div class=\"eb-accordion-title-content-wrap title-content-eb-accordion-63d5q\"><h3 class=\"eb-accordion-title\">The Laboratory<\/h3><\/div><\/div><div class=\"eb-accordion-content-wrapper eb-accordion-content-wrapper-eb-accordion-63d5q\"><div class=\"eb-accordion-content\">\n<p class=\"wp-block-paragraph\">Ostracods are small, mostly benthic crustaceans adapted to diverse aquatic environments. Their average size is less than 1 mm. Becouse their calcareous carapece fossilize, ostracods are widely used in stratigraphy, paleoecology, and in paleoclimatology. Ostracods have a long fossil record dating back to the Paleozoic and are well represented in marine and continental sediments. They are particularly sensitive to changes in environmental parameters. Quantitative and qualitative analysis of fossil assemblages allows for a detailed reconstruction of the depositional paleoenvironments. Sample collection, preparation, and study procedures depend on the type of sedimentary rock.  Ostracods are studied using a stereomicroscope.<\/p>\n\n\n\n<div style=\"height:20px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full is-resized\"><img loading=\"lazy\" decoding=\"async\" width=\"600\" height=\"333\" src=\"https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_5.jpeg\" alt=\"\" class=\"wp-image-12065\" style=\"width:600px\" srcset=\"https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_5.jpeg 600w, https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_5-300x167.jpeg 300w, https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_5-18x10.jpeg 18w\" sizes=\"auto, (max-width: 600px) 100vw, 600px\" \/><figcaption class=\"wp-element-caption\">The Micropaleontology Laboratory at the CNR Area in Pisa.<\/figcaption><\/figure>\n<\/div><\/div><\/div><\/div>\n\n\n\n<div class=\"wp-block-essential-blocks-accordion-item eb-accordion-item-xfxnw eb-accordion-wrapper\" data-clickable=\"false\"><div class=\"eb-accordion-title-wrapper eb-accordion-title-wrapper-eb-accordion-63d5q\" tabindex=\"0\"><span class=\"eb-accordion-icon-wrapper eb-accordion-icon-wrapper-eb-accordion-63d5q\"><span class=\"dashicon dashicons dashicons-plus-alt2 eb-accordion-icon\"><\/span><\/span><div class=\"eb-accordion-title-content-wrap title-content-eb-accordion-63d5q\"><h3 class=\"eb-accordion-title\">Instruments<\/h3><\/div><\/div><div class=\"eb-accordion-content-wrapper eb-accordion-content-wrapper-eb-accordion-63d5q\"><div class=\"eb-accordion-content\">\n<p class=\"wp-block-paragraph\"><strong>Sample preparation laboratory:<\/strong><\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>Hood for samples treatment.<\/li>\n\n\n\n<li>Oven for drying residues.<\/li>\n<\/ul>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Sample analysis:<\/strong><\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>LEITZ LABORLUX POL 12 microscope<\/li>\n\n\n\n<li>SLT Series Dual OPTECH zoom stereomicroscope<\/li>\n\n\n\n<li>LEICA S9D microscope<\/li>\n\n\n\n<li>Photographic equipment for the microscope<\/li>\n<\/ul>\n\n\n\n<div style=\"height:20px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full is-resized\"><img loading=\"lazy\" decoding=\"async\" width=\"600\" height=\"450\" src=\"https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_4.jpeg\" alt=\"\" class=\"wp-image-12064\" style=\"width:600px\" srcset=\"https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_4.jpeg 600w, https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_4-300x225.jpeg 300w, https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_4-16x12.jpeg 16w\" sizes=\"auto, (max-width: 600px) 100vw, 600px\" \/><figcaption class=\"wp-element-caption\">Metodo di raccolta campioni per lo studio ad alta definizione dei microfossili.<br><br><\/figcaption><\/figure>\n<\/div><\/div><\/div><\/div>\n\n\n\n<div class=\"wp-block-essential-blocks-accordion-item eb-accordion-item-7e36t eb-accordion-wrapper\" data-clickable=\"false\"><div class=\"eb-accordion-title-wrapper eb-accordion-title-wrapper-eb-accordion-63d5q\" tabindex=\"0\"><span class=\"eb-accordion-icon-wrapper eb-accordion-icon-wrapper-eb-accordion-63d5q\"><span class=\"dashicon dashicons dashicons-plus-alt2 eb-accordion-icon\"><\/span><\/span><div class=\"eb-accordion-title-content-wrap title-content-eb-accordion-63d5q\"><h3 class=\"eb-accordion-title\">Staff and Contacts<\/h3><\/div><\/div><div class=\"eb-accordion-content-wrapper eb-accordion-content-wrapper-eb-accordion-63d5q\"><div class=\"eb-accordion-content\">\n<p class=\"wp-block-paragraph\"><strong>Responsable<\/strong>:<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>Dr. Simone Da Prato (CNR Reseracher)<\/li>\n<\/ul>\n\n\n\n<p class=\"wp-block-paragraph\"><strong>Contacts<\/strong>:<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Telefono: 050 6212388<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">email: <a href=\"mailto:marco.chiari@igg.cnr.it\"><a href=\"mailto:simone.daprarto@cnr.it\">simone.daprarto@cnr.it<\/a><\/a><\/p>\n<\/div><\/div><\/div>\n\n\n\n<div class=\"wp-block-essential-blocks-accordion-item eb-accordion-item-n6kmd eb-accordion-wrapper\" data-clickable=\"false\"><div class=\"eb-accordion-title-wrapper eb-accordion-title-wrapper-eb-accordion-63d5q\" tabindex=\"0\"><span class=\"eb-accordion-icon-wrapper eb-accordion-icon-wrapper-eb-accordion-63d5q\"><span class=\"dashicon dashicons dashicons-plus-alt2 eb-accordion-icon\"><\/span><\/span><div class=\"eb-accordion-title-content-wrap title-content-eb-accordion-63d5q\"><h3 class=\"eb-accordion-title\">Methods and Applications<\/h3><\/div><\/div><div class=\"eb-accordion-content-wrapper eb-accordion-content-wrapper-eb-accordion-63d5q\"><div class=\"eb-accordion-content\">\n<p class=\"wp-block-paragraph\">Sampling, preparation and studying techniques use the standard methods adopted for micropaleontology and are different for the diverse kind of microfossils investigated.<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>Study of calcareous nannofossil assemblages consists in collecting tiny fragments of rock (about 3 cm3), preparing them as smear-slides and observing under optical polarizing microscope, both in cross and transmitted light, at 1250 magnification.<\/li>\n\n\n\n<li>Ostracods are extracted from disaggregated rocks (about 250 g) that are washed with H<sub>2<\/sub>O<sub>2<\/sub>, dried and analysed for the picking and observation of the species through a reflected and transmitted light microscope at 100 magnification.<\/li>\n\n\n\n<li>Data collected with quantitative and semi-quantitative methods prove to be a reliable and consistent dating tool, moreover allow observations on environment and climate changes.<\/li>\n<\/ul>\n\n\n\n<p class=\"wp-block-paragraph\">The Micropaleontology Lab\u2019s activity is precious for solving geological problems, in the Earth\u2019s natural resource exploration, and for paleoclimatic studies.<\/p>\n\n\n\n<div style=\"height:20px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full is-resized\"><img loading=\"lazy\" decoding=\"async\" width=\"600\" height=\"397\" src=\"https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_6.jpeg\" alt=\"\" class=\"wp-image-12066\" style=\"width:500px\" srcset=\"https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_6.jpeg 600w, https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_6-300x199.jpeg 300w, https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_6-18x12.jpeg 18w\" sizes=\"auto, (max-width: 600px) 100vw, 600px\" \/><figcaption class=\"wp-element-caption\">Tosya Basin succession along the North Anatolia Fault Zone (Northern Turkey).<\/figcaption><\/figure>\n<\/div>\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full is-resized\"><img loading=\"lazy\" decoding=\"async\" width=\"600\" height=\"450\" src=\"https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_7.jpeg\" alt=\"\" class=\"wp-image-12067\" style=\"width:500px\" srcset=\"https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_7.jpeg 600w, https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_7-300x225.jpeg 300w, https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_7-16x12.jpeg 16w\" sizes=\"auto, (max-width: 600px) 100vw, 600px\" \/><figcaption class=\"wp-element-caption\">Mt. Antola Flysch in the Trebbia Valley area (Piacenza Apennine).<\/figcaption><\/figure>\n<\/div>\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full is-resized\"><img loading=\"lazy\" decoding=\"async\" width=\"600\" height=\"398\" src=\"https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_8.jpeg\" alt=\"\" class=\"wp-image-12068\" style=\"width:500px\" srcset=\"https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_8.jpeg 600w, https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_8-300x199.jpeg 300w, https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_8-18x12.jpeg 18w\" sizes=\"auto, (max-width: 600px) 100vw, 600px\" \/><figcaption class=\"wp-element-caption\">Sampling of the Val Luretta Flysch along Luretta Valley (Piacenza Apennine).<\/figcaption><\/figure>\n<\/div>\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full is-resized\"><img loading=\"lazy\" decoding=\"async\" width=\"600\" height=\"449\" src=\"https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_9-1.jpeg\" alt=\"\" class=\"wp-image-12083\" style=\"width:500px\" srcset=\"https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_9-1.jpeg 600w, https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_9-1-300x225.jpeg 300w, https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_9-1-16x12.jpeg 16w\" sizes=\"auto, (max-width: 600px) 100vw, 600px\" \/><figcaption class=\"wp-element-caption\">Tectonic contact between Acquerino and Carigiola units along Tavaiano Creek (Futa Pass, Tuscan-Emilian Apennine).<\/figcaption><\/figure>\n<\/div><\/div><\/div><\/div>\n\n\n\n<div class=\"wp-block-essential-blocks-accordion-item eb-accordion-item-gno6p eb-accordion-wrapper\" data-clickable=\"false\"><div class=\"eb-accordion-title-wrapper eb-accordion-title-wrapper-eb-accordion-63d5q\" tabindex=\"0\"><span class=\"eb-accordion-icon-wrapper eb-accordion-icon-wrapper-eb-accordion-63d5q\"><span class=\"dashicon dashicons dashicons-plus-alt2 eb-accordion-icon\"><\/span><\/span><div class=\"eb-accordion-title-content-wrap title-content-eb-accordion-63d5q\"><h3 class=\"eb-accordion-title\">Scientific Projects and Interests<\/h3><\/div><\/div><div class=\"eb-accordion-content-wrapper eb-accordion-content-wrapper-eb-accordion-63d5q\"><div class=\"eb-accordion-content\">\n<p class=\"wp-block-paragraph\">The laboratory can operate within multidisciplinary projects covering a wide variety of topics (geological, stratigraphic, hydrogeological, geotechnical, etc.).<\/p>\n\n\n\n<ul class=\"wp-block-list\">\n<li>2022-2025 Official Geological Map of Italy at 1:50,000 scale (CARG Project): micropaleontological analyses, Sheet n. 274 \u201cEmpoli\u201d (Geological Survey of Italy, ISPRA).<\/li>\n\n\n\n<li>2025 Official Geological Map of Italy at 1:50,000 scale (CARG Project):  analysis of ostracod fauna in samples from deep core, Sheet n. 087 \u201cPalmanova\u201d (Geological Survey of Italy, ISPRA).<\/li>\n\n\n\n<li>2024 Official Geological Map of Italy at 1:50,000 scale (CARG Project):  analysis of ostracod assemblages from Pliocene continental deposits, Sheet n. 286 \u201cPoggibonsi\u201d (Geological Survey of Italy, ISPRA).<\/li>\n\n\n\n<li>2018: Geological and geomorphological study of the Val di Fine and Volterra-Cerbaie basins, Province of Pisa (Union of Municipalities of Valdera).<\/li>\n<\/ul>\n\n\n\n<div style=\"height:20px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full is-resized\"><img loading=\"lazy\" decoding=\"async\" width=\"600\" height=\"584\" src=\"https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_10.jpeg\" alt=\"\" class=\"wp-image-12070\" style=\"width:auto;height:500px\" srcset=\"https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_10.jpeg 600w, https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_10-300x292.jpeg 300w, https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_10-12x12.jpeg 12w\" sizes=\"auto, (max-width: 600px) 100vw, 600px\" \/><figcaption class=\"wp-element-caption\">Litho-, bio-, and chrono-stratigraphy of the Boeotian Flysch between Iti Mountains and Levadhia area (Central Greece). For details see Nirta et al. 2015 - The Boeotian flysch revisited: new constraints on ophiolite obduction in central Greece. Ofioliti. 40, 107-123.<\/figcaption><\/figure>\n<\/div>\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full is-resized\"><img loading=\"lazy\" decoding=\"async\" width=\"600\" height=\"803\" src=\"https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_11.jpeg\" alt=\"\" class=\"wp-image-12071\" style=\"width:auto;height:600px\" srcset=\"https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_11.jpeg 600w, https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_11-224x300.jpeg 224w, https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_11-9x12.jpeg 9w\" sizes=\"auto, (max-width: 600px) 100vw, 600px\" \/><figcaption class=\"wp-element-caption\">Eocene biozones and biohorizons of Agnini et al. 2014 with diagnostic calcareous nannofossil species and climatic events. For details see Agnini et al. 2014 - Biozonation and biochronology of Paleogene calcareous nannofossils from low and middle latitudes. Newsletters on Stratigraphy. 47, 131-181.<\/figcaption><\/figure>\n<\/div>\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full is-resized\"><img loading=\"lazy\" decoding=\"async\" width=\"600\" height=\"496\" src=\"https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_12.jpeg\" alt=\"\" class=\"wp-image-12072\" style=\"width:600px\" srcset=\"https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_12.jpeg 600w, https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_12-300x248.jpeg 300w, https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_12-15x12.jpeg 15w\" sizes=\"auto, (max-width: 600px) 100vw, 600px\" \/><figcaption class=\"wp-element-caption\">Integrated high-resolution stratigraphic framework of the Palaeocene\u2013early Eocene Contessa composite section with documented and suspected hyperthermals. For details see Coccioni et al., 2012- An integrated stratigraphic record of the Palaeocene\u2013lower Eocene at Gubbio (Italy): new insights into the early Palaeogene hyperthermals and carbon isotope excursions. Terra Nova, 24, 380-386.<\/figcaption><\/figure>\n<\/div>\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full is-resized\"><img loading=\"lazy\" decoding=\"async\" width=\"600\" height=\"443\" src=\"https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_13.jpeg\" alt=\"\" class=\"wp-image-12073\" style=\"width:600px\" srcset=\"https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_13.jpeg 600w, https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_13-300x222.jpeg 300w, https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig_13-16x12.jpeg 16w\" sizes=\"auto, (max-width: 600px) 100vw, 600px\" \/><figcaption class=\"wp-element-caption\">Synthetic curves for the cyclostratigraphic study of Messinian Cava Serredi section.<\/figcaption><\/figure>\n<\/div>\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-full is-resized\"><img loading=\"lazy\" decoding=\"async\" width=\"600\" height=\"344\" src=\"https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig-14.png\" alt=\"\" class=\"wp-image-12074\" style=\"width:600px\" srcset=\"https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig-14.png 600w, https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig-14-300x172.png 300w, https:\/\/www.igg.cnr.it\/wp-content\/uploads\/2026\/04\/laboratorio-micropaleontologia-Fig-14-18x10.png 18w\" sizes=\"auto, (max-width: 600px) 100vw, 600px\" \/><figcaption class=\"wp-element-caption\">Idrostructural 3D model of a Versilian Plane area and idrogeology.<\/figcaption><\/figure>\n<\/div><\/div><\/div><\/div>\n\n\n\n<div class=\"wp-block-essential-blocks-accordion-item eb-accordion-item-hhhj9 eb-accordion-wrapper\" data-clickable=\"false\"><div class=\"eb-accordion-title-wrapper eb-accordion-title-wrapper-eb-accordion-63d5q\" tabindex=\"0\"><span class=\"eb-accordion-icon-wrapper eb-accordion-icon-wrapper-eb-accordion-63d5q\"><span class=\"dashicon dashicons dashicons-plus-alt2 eb-accordion-icon\"><\/span><\/span><div class=\"eb-accordion-title-content-wrap title-content-eb-accordion-63d5q\"><h3 class=\"eb-accordion-title\">Publications<\/h3><\/div><\/div><div class=\"eb-accordion-content-wrapper eb-accordion-content-wrapper-eb-accordion-63d5q\"><div class=\"eb-accordion-content\">\n<ul class=\"wp-block-list\">\n<li>CATANZARITI R. &amp; DA PRATO S. (2020) &#8211; New biostratigraphic and lithological data on the Neogene and Quaternary of the Livorno area (Tuscany, Central Italy). Rivista Italiana di Paleontologia e Stratigrafia (Research in Paleontology and Stratigraphy) vol. 126(3): 725-749.<\/li>\n<\/ul>\n<\/div><\/div><\/div>\n<\/div><\/div><\/div><\/div>\n\n\n\n<div style=\"height:100px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<p class=\"wp-block-paragraph\"><\/p>","protected":false},"excerpt":{"rendered":"<p>The laboratory is housed in the IGG Pisa headquarter<\/p>","protected":false},"author":1,"featured_media":12058,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_eb_attr":"","neve_meta_sidebar":"","neve_meta_container":"","neve_meta_enable_content_width":"","neve_meta_content_width":0,"neve_meta_title_alignment":"","neve_meta_author_avatar":"","neve_post_elements_order":"","neve_meta_disable_header":"","neve_meta_disable_footer":"","neve_meta_disable_title":"","footnotes":""},"folder":[36],"class_list":["post-12060","page","type-page","status-publish","has-post-thumbnail","hentry"],"_links":{"self":[{"href":"https:\/\/www.igg.cnr.it\/en\/wp-json\/wp\/v2\/pages\/12060","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.igg.cnr.it\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.igg.cnr.it\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.igg.cnr.it\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.igg.cnr.it\/en\/wp-json\/wp\/v2\/comments?post=12060"}],"version-history":[{"count":12,"href":"https:\/\/www.igg.cnr.it\/en\/wp-json\/wp\/v2\/pages\/12060\/revisions"}],"predecessor-version":[{"id":12090,"href":"https:\/\/www.igg.cnr.it\/en\/wp-json\/wp\/v2\/pages\/12060\/revisions\/12090"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.igg.cnr.it\/en\/wp-json\/wp\/v2\/media\/12058"}],"wp:attachment":[{"href":"https:\/\/www.igg.cnr.it\/en\/wp-json\/wp\/v2\/media?parent=12060"}],"wp:term":[{"taxonomy":"folder","embeddable":true,"href":"https:\/\/www.igg.cnr.it\/en\/wp-json\/wp\/v2\/folder?post=12060"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}