{"id":282,"date":"2023-06-15T13:41:05","date_gmt":"2023-06-15T13:41:05","guid":{"rendered":"https:\/\/www.paleoclima.cnr.it\/irene-cornacchia\/"},"modified":"2023-06-15T13:42:15","modified_gmt":"2023-06-15T13:42:15","slug":"irene-cornacchia","status":"publish","type":"page","link":"https:\/\/www.paleoclima.cnr.it\/en\/irene-cornacchia\/","title":{"rendered":"Irene Cornacchia"},"content":{"rendered":"\t\t
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\n\t\t\t\t\t\t\t\t\tIrene Cornacchia<\/b> is a researcher at the Institute of Geosciences and Earth Resources (IGG) of the Italian National Research Council from November 2019.\r\nMaster Degree in Esploration Geology (2014) and PhD in Sedimentology and Stratigraphy (2018) at the Earth Sciences Department of the Sapienza, University of Rome. Postdoctoral fellow at the GeoZentrum Nordbayern of the Friedrich-Alexander University of Erlangen, Germany (2018-2019), Irene is currently Associated Editor of the Geological Magazine and member of the Coordinating Committee of GeoSed (Sedimentology and Stratigraphy section of the Italian Geological Society).\r\n

Irene Cornacchia\u2019s research focuses on how shallow-water carbonate systems responded to climate changes and perturbations of the carbon cycle, in particular in the Cenozoic record of the Mediterranean area. In this framework, Irene studies the relationship between climate trends and regional controlling factors \u2013geodynamics and oceanographic changes- affecting carbonate production as well as its changes and crises. With a multidisciplinary approach, Irene integrates a solid facies and microfacies analyses with detailed isotope geochemistry studies of oxygen and carbon isotope stratigraphy, to identify climate changes and carbon cycle perturbations, as well as strontium and neodymium radiogenic isotopes, proxies of seawater chemistry and powerful tools to identify the role of oceanographic changes in controlling carbonate production.\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t
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Eleonora Regattieri<\/a><\/h3>

CNR-IGG\n
(Coordinatrice)\n
(Geochimica, paleoclimatologia)<\/p><\/div><\/div>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t

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Biagio Giaccio<\/a><\/h3>

CNR-IGAG\n
(Vide-Coordinatore)\n
(Tefrocronologia, stratigrafia del Quaternario)<\/p><\/div><\/div>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t

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Roberto Bellucci<\/h3>

CNR-DSSTTA\n
(Segreteria tecnico-scientifica)<\/p><\/div><\/div>\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

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Alessandra Asioli<\/a><\/h3>

CNR-ISMAR\n
(Micropaleontologia, \npaleoceanografia del Quaternario)<\/p><\/div><\/div>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t

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Carlo Baroni<\/a><\/h3>

Universit\u00e0 di Pisa\n
(Geomorfologo, geologo glaciale)<\/p><\/div><\/div>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t

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Michele Brunetti<\/a><\/h3>

CNR-ISAC\n
(Fisica, climatologia)<\/p><\/div><\/div>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t

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Lucilla Capotondi<\/a><\/h3>

CNR-ISMAR\n
(Biostratigrafia, paleoceanografia)<\/p><\/div><\/div>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t

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Francesco Cavalcante<\/a><\/h3>

CNR-IMAA\n
(Mineralogia delle argille)<\/p><\/div><\/div>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t

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Irene Cornacchia<\/a><\/h3>

CNR-IGAG\n
(Stratigrafia, paleoceanografia)<\/p><\/div><\/div>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t

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Roberta D\u2019agostino<\/a><\/h3>

CNR-ISAC\n
(Modellistica paleoclimatica)<\/p><\/div><\/div>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t

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Donatella Domenica Insinga<\/a><\/h3>

CNR-ISMAR\n
(Tefrocronologia, geologia marina)<\/p><\/div><\/div>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t

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Andrea Lami<\/a><\/h3>

CNR-IRSA\n
(Paleolimnologia, biomarker)<\/p><\/div><\/div>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t

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Fabrizio Lirer<\/a><\/h3>

Universit\u00e0 Sapienza\n
(Biostratigrafia, paleoceanografia)<\/p><\/div><\/div>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t

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Giovanni Monegato<\/a><\/h3>

CNR-IGG\n
(Geologia del Quaternario)<\/p><\/div><\/div>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t

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Paolo Montagna<\/a><\/h3>

CNR-ISP\n
(Geochimica, paleoceanografia)<\/p><\/div><\/div>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t

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Cesare Ravazzi<\/a><\/h3>

CNR-IGAG\n
(Ecologia del Quaternario)<\/p><\/div><\/div>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t

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Barbara Stenni<\/a><\/h3>

Universit\u00e0 C\u00e0 Foscari Venezia\n
(Geochimica, paleoclimatologa)<\/p><\/div><\/div>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t

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Chunxue Yang<\/a><\/h3>

CNR-ISMAR\n
(Dinamica climatica, Modelli climatici)<\/p><\/div><\/div>\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>\n\t\t\t\t<\/div>\n\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>\n\t\t\t\t<\/div>\n\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>\n\t\t","protected":false},"excerpt":{"rendered":"

Irene Cornacchia<\/b> is a researcher at the Institute of Geosciences and Earth Resources (IGG) of the Italian National Research Council from November 2019.
\nMaster Degree in Esploration Geology (2014) and PhD in Sedimentology and Stratigraphy (2018) at the Earth Sciences Department of the Sapienza, University of Rome. Postdoctoral fellow at the GeoZentrum Nordbayern of the Friedrich-Alexander University of Erlangen, Germany (2018-2019), Irene is currently Associated Editor of the Geological Magazine and member of the Coordinating Committee of GeoSed (Sedimentology and Stratigraphy section of the Italian Geological Society).<\/p>\n

Irene Cornacchia\u2019s research focuses on how shallow-water carbonate systems responded to climate changes and perturbations of the carbon cycle, in particular in the Cenozoic record of the Mediterranean area. In this framework, Irene studies the relationship between climate trends and regional controlling factors \u2013geodynamics and oceanographic changes- affecting carbonate production as well as its changes and crises. With a multidisciplinary approach, Irene integrates a solid facies and microfacies analyses with detailed isotope geochemistry studies of oxygen and carbon isotope stratigraphy, to identify climate changes and carbon cycle perturbations, as well as strontium and neodymium radiogenic isotopes, proxies of seawater chemistry and powerful tools to identify the role of oceanographic changes in controlling carbonate production.<\/p>\n","protected":false},"author":1,"featured_media":168,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"elementor_header_footer","meta":{"footnotes":""},"class_list":["post-282","page","type-page","status-publish","has-post-thumbnail","hentry"],"yoast_head":"\nIrene Cornacchia - CNR Paleoclima<\/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:\/\/www.paleoclima.cnr.it\/irene-cornacchia\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Irene Cornacchia - CNR Paleoclima\" \/>\n<meta property=\"og:description\" content=\"Irene Cornacchia is a researcher at the Institute of Geosciences and Earth Resources (IGG) of the Italian National Research Council from November 2019. 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With a multidisciplinary approach, Irene integrates a solid facies and microfacies analyses with detailed isotope geochemistry studies of oxygen and carbon isotope stratigraphy, to identify climate changes and carbon cycle perturbations, as well as strontium and neodymium radiogenic isotopes, proxies of seawater chemistry and powerful tools to identify the role of oceanographic changes in controlling carbonate production.\" \/>\n<meta property=\"og:url\" content=\"https:\/\/www.paleoclima.cnr.it\/irene-cornacchia\/\" \/>\n<meta property=\"og:site_name\" content=\"CNR Paleoclima\" \/>\n<meta property=\"article:modified_time\" content=\"2023-06-15T13:42:15+00:00\" \/>\n<meta property=\"og:image\" content=\"https:\/\/www.paleoclima.cnr.it\/wp-content\/uploads\/2023\/06\/chi-siamo10.jpg\" \/>\n\t<meta property=\"og:image:width\" content=\"500\" \/>\n\t<meta property=\"og:image:height\" content=\"500\" \/>\n\t<meta property=\"og:image:type\" content=\"image\/jpeg\" \/>\n<meta name=\"twitter:card\" content=\"summary_large_image\" \/>\n<script type=\"application\/ld+json\" class=\"yoast-schema-graph\">{\"@context\":\"https:\\\/\\\/schema.org\",\"@graph\":[{\"@type\":\"WebPage\",\"@id\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/irene-cornacchia\\\/\",\"url\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/irene-cornacchia\\\/\",\"name\":\"Irene Cornacchia - CNR Paleoclima\",\"isPartOf\":{\"@id\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/#website\"},\"primaryImageOfPage\":{\"@id\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/irene-cornacchia\\\/#primaryimage\"},\"image\":{\"@id\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/irene-cornacchia\\\/#primaryimage\"},\"thumbnailUrl\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/wp-content\\\/uploads\\\/2023\\\/06\\\/chi-siamo10.jpg\",\"datePublished\":\"2023-06-15T13:41:05+00:00\",\"dateModified\":\"2023-06-15T13:42:15+00:00\",\"breadcrumb\":{\"@id\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/irene-cornacchia\\\/#breadcrumb\"},\"inLanguage\":\"en-US\",\"potentialAction\":[{\"@type\":\"ReadAction\",\"target\":[\"https:\\\/\\\/www.paleoclima.cnr.it\\\/irene-cornacchia\\\/\"]}]},{\"@type\":\"ImageObject\",\"inLanguage\":\"en-US\",\"@id\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/irene-cornacchia\\\/#primaryimage\",\"url\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/wp-content\\\/uploads\\\/2023\\\/06\\\/chi-siamo10.jpg\",\"contentUrl\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/wp-content\\\/uploads\\\/2023\\\/06\\\/chi-siamo10.jpg\",\"width\":500,\"height\":500},{\"@type\":\"BreadcrumbList\",\"@id\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/irene-cornacchia\\\/#breadcrumb\",\"itemListElement\":[{\"@type\":\"ListItem\",\"position\":1,\"name\":\"Home\",\"item\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/\"},{\"@type\":\"ListItem\",\"position\":2,\"name\":\"Irene Cornacchia\"}]},{\"@type\":\"WebSite\",\"@id\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/#website\",\"url\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/\",\"name\":\"CNR Paleoclima\",\"description\":\"\",\"publisher\":{\"@id\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/#organization\"},\"potentialAction\":[{\"@type\":\"SearchAction\",\"target\":{\"@type\":\"EntryPoint\",\"urlTemplate\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/?s={search_term_string}\"},\"query-input\":{\"@type\":\"PropertyValueSpecification\",\"valueRequired\":true,\"valueName\":\"search_term_string\"}}],\"inLanguage\":\"en-US\"},{\"@type\":\"Organization\",\"@id\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/#organization\",\"name\":\"CNR Paleoclima\",\"url\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/\",\"logo\":{\"@type\":\"ImageObject\",\"inLanguage\":\"en-US\",\"@id\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/#\\\/schema\\\/logo\\\/image\\\/\",\"url\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/wp-content\\\/uploads\\\/2023\\\/06\\\/cropped-logo2.png\",\"contentUrl\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/wp-content\\\/uploads\\\/2023\\\/06\\\/cropped-logo2.png\",\"width\":2479,\"height\":674,\"caption\":\"CNR Paleoclima\"},\"image\":{\"@id\":\"https:\\\/\\\/www.paleoclima.cnr.it\\\/#\\\/schema\\\/logo\\\/image\\\/\"}}]}<\/script>\n<!-- \/ Yoast SEO plugin. -->","yoast_head_json":{"title":"Irene Cornacchia - CNR Paleoclima","robots":{"index":"index","follow":"follow","max-snippet":"max-snippet:-1","max-image-preview":"max-image-preview:large","max-video-preview":"max-video-preview:-1"},"canonical":"https:\/\/www.paleoclima.cnr.it\/irene-cornacchia\/","og_locale":"en_US","og_type":"article","og_title":"Irene Cornacchia - CNR Paleoclima","og_description":"Irene Cornacchia is a researcher at the Institute of Geosciences and Earth Resources (IGG) of the Italian National Research Council from November 2019. 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