{"id":14231,"date":"2019-02-18T13:42:32","date_gmt":"2019-02-18T12:42:32","guid":{"rendered":"https:\/\/www.ig.cas.cz\/?page_id=14231"},"modified":"2019-02-19T12:56:14","modified_gmt":"2019-02-19T11:56:14","slug":"project-global-carbon-cycle","status":"publish","type":"page","link":"https:\/\/www.ig.cas.cz\/en\/project-global-carbon-cycle\/","title":{"rendered":"Sea-level changes and global carbon cycle in greenhouse climate: trans-Atlantic correlation of Turonian (mid-Cretaceous) sedimentary archives"},"content":{"rendered":"<p>[et_pb_section fb_built=&#8221;1&#8243; _builder_version=&#8221;3.0.47&#8243; custom_padding=&#8221;0px|0px|0px|0px&#8221;][et_pb_row custom_padding=&#8221;31.7167px|0px|10px|0px&#8221; _builder_version=&#8221;3.0.99&#8243;][et_pb_column type=&#8221;2_3&#8243; _builder_version=&#8221;3.0.47&#8243; parallax=&#8221;off&#8221; parallax_method=&#8221;on&#8221;][et_pb_text _builder_version=&#8221;3.0.105&#8243;]<\/p>\n<h3>Sea-level changes and global carbon cycle in greenhouse climate: trans-Atlantic correlation of Turonian (mid-Cretaceous) sedimentary archives<\/h3>\n<div class=\"nova-e-text nova-e-text--size-m nova-e-text--family-sans-serif nova-e-text--spacing-s nova-e-text--color-inherit redraft-text\">Funding: Czech Science Foundation (GA\u010cR), 2017-2019<br \/> Project Reg. No. 17-10982S<\/div>\n<div class=\"nova-e-text nova-e-text--size-m nova-e-text--family-sans-serif nova-e-text--spacing-s nova-e-text--color-inherit redraft-text\"><\/div>\n<p style=\"text-align: justify;\">The project focuses on fluctuations in carbon cycle and sea level during\u00a0 the Turonian peak greenhouse interval (mid-Cretaceous), studied using comparison of new data at high temporal resolution from two unique sedimentary archives: the Western Interior Seaway (SW North America) and the Bohemian Cretaceous Basin (Czech Republic). The correlation between the two records is facilitated by a&nbsp;combination of carbon-isotope chemostratigraphy and biostratigraphy, providing the highest temporal resolution achieved so far in this interval. Sedimentological profiles and geophysical wireline logs used for interpreting the relative sea-level histories are linked to stable-isotope and elemental-proxy time series, as a&nbsp;basis for interpreting climatic cyclicity and for further improvement and refinement of the Turonian astrochronological timescale. The results are expected to shed light on the controversial issues of the timing and causes of short-term sea-level changes in the mid-Cretaceous greenhouse climate, and the functioning of the global carbon cycle as a&nbsp;key component of the climatic system.<\/p>\n<p>[\/et_pb_text][\/et_pb_column][et_pb_column type=&#8221;1_3&#8243; _builder_version=&#8221;3.0.47&#8243; parallax=&#8221;off&#8221; parallax_method=&#8221;on&#8221;][et_pb_text _builder_version=&#8221;3.0.105&#8243;]<\/p>\n<p style=\"text-align: center;\"><strong>Principal investigator<\/strong>: <a href=\"https:\/\/www.ig.cas.cz\/kontakty\/seznam-pracovniku\/david-ulicny\/\"><strong>David Uli\u010dn\u00fd<\/strong><\/a> (Institute of Geophysics, <a href=\"..\/departments\/geodynamics\/\">Geodynamics<\/a>)<\/p>\n<p style=\"text-align: center;\"><strong>Co-PIs<\/strong>: Stanislav \u010cech, Czech Geological Survey; Ji\u0159\u00ed Zachari\u00e1\u0161, Charles University, Faculty of Science<\/p>\n<p style=\"text-align: center;\"><strong>Team members<\/strong>: <a href=\"https:\/\/www.ig.cas.cz\/kontakty\/seznam-pracovniku\/jiri-laurin\/\">J. Laurin<\/a> (Institute of Geophysics), I. Ja\u010dkov\u00e1 (Czech Geological Survey), J. Truba\u010d (Charles University, Faculty of Science)<\/p>\n<p style=\"text-align: center;\"><strong>International collaboration:<\/strong> B.B. Sageman, Northwestern University, Evanston, IL, USA; M.M. Jones, University of Michigan \/ Northwestern University, USA; Nikolai Pedentchouk, University of East Anglia, Norwich, U.K.; A.G. Plint, University of Western Ontario, London, ON, Canada; I. Walaszczyk, Uniwersytet Warszawski, Poland<\/p>\n<p style=\"text-align: center;\"><a href=\"..\/departments\/geodynamics\/\"><\/a><\/p>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section][et_pb_section fb_built=&#8221;1&#8243; _builder_version=&#8221;3.0.99&#8243; custom_padding=&#8221;3px|0px|0px|0px&#8221;][et_pb_row custom_padding=&#8221;0px|0px|28.125px|0px&#8221; _builder_version=&#8221;3.0.99&#8243;][et_pb_column type=&#8221;1_2&#8243; _builder_version=&#8221;3.0.47&#8243; parallax=&#8221;off&#8221; parallax_method=&#8221;on&#8221;][et_pb_text _builder_version=&#8221;3.0.105&#8243;]<\/p>\n<h3><strong>Publications<\/strong><\/h3>\n<ul>\n<li>Laurin, J., R\u016f\u017eek, B. &#038; Giorgioni, M. (2017). Orbital signals in carbon isotopes: phase distortion as a&nbsp;signature of the carbon cycle. Paleoceanography, 32, ISSN 0883-8305. <a href=\"https:\/\/doi.org\/10.1002\/2017PA003143\">https:\/\/doi.org\/10.1002\/2017PA003143<\/a><\/li>\n<li>Ko\u0161\u0165\u00e1k, M., \u010cech, S., Uli\u010dn\u00fd, D. &#038; Ekrt, B. (2018). Ammonites, inoceramids and stable carbon isotopes of the Cenomanian-Turonian OAE2 interval in central Europe: Pec\u00ednov quarry, Bohemian Cretaceous Basin (Czech Republic). Cretaceous Research, 87, 150-173. \u00a0<a href=\"http:\/\/dx.doi.org\/10.1016\/j.cretres.2017.04.013\">http:\/\/dx.doi.org\/10.1016\/j.cretres.2017.04.013<\/a><\/li>\n<\/ul>\n<h3><strong>Submitted papers<\/strong><\/h3>\n<ul>\n<li>Laurin, J., Barclay, R.S., Sageman, B.B., Dawson, R., Pagani, M., Schmitz, M., Eaton, J., McElwain, J.C., McInerney, F.A. (in review). Terrestrial and marginal-marine record of the Oceanic Anoxic Event 2 (OAE 2): high-resolution framework, carbon isotopes, CO<sub>2<\/sub> and sea-level change. Palaeogeography, Palaeoclimatology, Palaeoecology<\/li>\n<li>Baker, S.J., Belcher, C.M., Barclay, R.S., Hesselbo, S.P., Laurin, J., Sageman, B.B. (revision submitted). CO<sub>2<\/sub> induced climate forcings on the fire record during Cretaceous OAE2. GSA Bulletin<\/li>\n<\/ul>\n<p>[\/et_pb_text][\/et_pb_column][et_pb_column type=&#8221;1_2&#8243; _builder_version=&#8221;3.0.47&#8243; parallax=&#8221;off&#8221; parallax_method=&#8221;on&#8221;][et_pb_text _builder_version=&#8221;3.0.105&#8243;]<\/p>\n<h3><strong>Selected conference presentations<\/strong><\/h3>\n<ul>\n<li>Plint, A.G., Uli\u010dn\u00fd, D., \u010cech, S., Walaszczyk, I., Gr\u00f6cke, D.R., Shank, J.A., Laurin, J., Jarvis, I. (2017): High-frequency, shallow marine clastic sequences across the Turonian &#8211; Coniacian boundary, correlated between the Bohemian Cretaceous and Western Canada basins.<br \/> In Sames, B: 10th International Symposium on the Cretaceous &#8211; Abstracts, 21-26 August 2017, Vienna. &#8211; Berichte der Geologischen Bundesanstalt, svazek 120.&nbsp;s. 264. \u2013 Geologische Bundesanstalt. Wien<\/li>\n<li>\u010cech, S. &amp; Uli\u010dn\u00fd, D. (2017): The Turonian-Coniacian stage boundary in the Bohemian Cretaceous Basin (Czech Republic), correlated between nearshore and offshore facies.In Sames, B: 10th International Symposium on the Cretaceous &#8211; Abstracts, 21-26 August 2017, Vienna. &#8211; Berichte der Geologischen Bundesanstalt, svazek 120.&nbsp;s. 45. \u2013 Geologische Bundesanstalt. Wien<\/li>\n<li>Chroustov\u00e1, M., Holcov\u00e1, K., Hradeck\u00e1, L., Uli\u010dn\u00fd, D. (2018). Foraminifera assemblages and lithological variability, Upper Turonian, Bohemian Cretaceous Basin. In Abstract Book, FORAMS 2018 (International Symposium on foraminifera: Foraminifera in changing world, Edinburgh, UK, June 2018), 108-109.<\/li>\n<\/ul>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section]<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Sea-level changes and global carbon cycle in greenhouse climate: trans-Atlantic correlation of Turonian (mid-Cretaceous) sedimentary archives Funding: Czech Science Foundation (GA\u010cR), 2017-2019 Project Reg. No. 17-10982S The project focuses on fluctuations in carbon cycle and sea level during\u00a0 the Turonian peak greenhouse interval (mid-Cretaceous), studied using comparison of new data at high temporal resolution from [&hellip;]<\/p>\n","protected":false},"author":2,"featured_media":5566,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_et_pb_use_builder":"on","_et_pb_old_content":"<p>Vztah mezi anizotropi\u00ed magnetick\u00e9 susceptibility (AMS) a deforma\u010dn\u00ed mikrostrukturou bude studov\u00e1n v\u00a0p\u0159\u00edrodn\u00edch stri\u017en\u00fdch z\u00f3n\u00e1ch a srovn\u00e1n s analogov\u00fdm a numerick\u00fdm modelov\u00e1n\u00edm. Stri\u017en\u00e9 z\u00f3ny v\u00a0monominer\u00e1ln\u00edch hornin\u00e1ch (kalcit, kvarcit) p\u0159edstavuj\u00ed vhodn\u00e9 p\u0159\u00edrodn\u00ed laborato\u0159e ke studiu magnetick\u00e9 stavby, textury a mikrostruktury pro pochopen\u00ed mikrostrukturn\u00edch proces\u016f, kter\u00e9 kontroluj\u00ed vznik AMS.\u00a0Analogov\u00e9 modelov\u00e1n\u00ed bude prov\u00e1d\u011bno v r\u016fzn\u00fdch tektonick\u00fdch re\u017eimech pomoc\u00ed reologicky neline\u00e1rn\u00edch materi\u00e1l\u016f. Numerick\u00e9 modely budou po\u010d\u00edtat AMS na z\u00e1klad\u011b re\u00e1ln\u00e9 mikrostruktury a srovn\u00e1vat ji s\u00a0pozorovanou a m\u011b\u0159enou stavbou a stavebn\u00edmi p\u0159etisky. Kombinace ter\u00e9nn\u00ed, laboratorn\u00ed a numerick\u00e9\u00a0studie je nutn\u00e9 k pochopen\u00ed probl\u00e9mu \u010dasov\u00fdch a prostorov\u00fdch vztah\u016f mezi AMS horninovou stavbou a\u00a0kone\u010dnou deformac\u00ed. Z\u00edskan\u00e9 v\u00fdsledky p\u0159isp\u011bj\u00ed k pochopen\u00ed magnetick\u00e9 stavby ve st\u0159i\u017en\u00fdch z\u00f3n\u00e1ch na\u00a0z\u00e1klad\u011b hodnocen\u00ed vz\u00e1jemn\u00e9ho reologick\u00e9ho ovliv\u0148ov\u00e1n\u00ed z\u00e1kladn\u00ed hmoty a magnetick\u00fdch miner\u00e1l\u016f.<\/p>","_et_gb_content_width":"","footnotes":""},"categories":[],"tags":[],"class_list":["post-14231","page","type-page","status-publish","has-post-thumbnail","hentry"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v25.9 - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>Sea-level changes and global carbon cycle in greenhouse climate: trans-Atlantic correlation of Turonian (mid-Cretaceous) sedimentary archives - Geofyzik\u00e1ln\u00ed \u00fastav Akademie v\u011bd \u010cR, v.v.i.<\/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.ig.cas.cz\/en\/project-global-carbon-cycle\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Sea-level changes and global carbon cycle in greenhouse climate: trans-Atlantic correlation of Turonian (mid-Cretaceous) sedimentary archives - Geofyzik\u00e1ln\u00ed \u00fastav Akademie v\u011bd \u010cR, v.v.i.\" \/>\n<meta property=\"og:description\" content=\"Sea-level changes and global carbon cycle in greenhouse climate: trans-Atlantic correlation of Turonian (mid-Cretaceous) sedimentary archives Funding: Czech Science Foundation (GA\u010cR), 2017-2019 Project Reg. 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