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• W2080228896 abstract "Research Article| November 01, 2009 The combined effect of sea level and supply during Milankovitch cyclicity: Evidence from shallow-marine δ18O records and sequence architecture (Adriatic margin) D. Ridente; D. Ridente * 1Istituto di Geologia Ambientale e Geoingegneria (IGAG) Consiglio Nazionale delle Ricerche, c/o Dipartimento di Scienze della Terra, Università Sapienza, Piazzale Moro 5, 00185 Rome, Italy *E-mail: domenico.ridente@cnr.it. Search for other works by this author on: GSW Google Scholar F. Trincardi; F. Trincardi 2Istituto di Scienze Marine (ISMAR) Consiglio Nazionale delle Ricerche, via Gobetti 101, 40129 Bologna, Italy Search for other works by this author on: GSW Google Scholar A. Piva; A. Piva 2Istituto di Scienze Marine (ISMAR) Consiglio Nazionale delle Ricerche, via Gobetti 101, 40129 Bologna, Italy Search for other works by this author on: GSW Google Scholar A. Asioli A. Asioli 3Istituto di Geoscienze e Georisorse (IGG) Consiglio Nazionale delle Ricerche, via Giotto 1, 35100 Padova, Italy Search for other works by this author on: GSW Google Scholar Author and Article Information D. Ridente * 1Istituto di Geologia Ambientale e Geoingegneria (IGAG) Consiglio Nazionale delle Ricerche, c/o Dipartimento di Scienze della Terra, Università Sapienza, Piazzale Moro 5, 00185 Rome, Italy F. Trincardi 2Istituto di Scienze Marine (ISMAR) Consiglio Nazionale delle Ricerche, via Gobetti 101, 40129 Bologna, Italy A. Piva 2Istituto di Scienze Marine (ISMAR) Consiglio Nazionale delle Ricerche, via Gobetti 101, 40129 Bologna, Italy A. Asioli 3Istituto di Geoscienze e Georisorse (IGG) Consiglio Nazionale delle Ricerche, via Giotto 1, 35100 Padova, Italy *E-mail: domenico.ridente@cnr.it. Publisher: Geological Society of America Revision Received: 13 Jun 2009 Accepted: 17 Jun 2009 Received: 05 Dec 2009 First Online: 02 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2009 Geological Society of America Geology (2009) 37 (11): 1003–1006. https://doi.org/10.1130/G25730A.1 Article history Revision Received: 13 Jun 2009 Accepted: 17 Jun 2009 Received: 05 Dec 2009 First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation D. Ridente, F. Trincardi, A. Piva, A. Asioli; The combined effect of sea level and supply during Milankovitch cyclicity: Evidence from shallow-marine δ18O records and sequence architecture (Adriatic margin). Geology 2009;; 37 (11): 1003–1006. doi: https://doi.org/10.1130/G25730A.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract The combination of sequence stratigraphy and multiproxy chronostratigraphic data, including δ18O records, unravels the record of Milankovitch cyclicity through the past ~400 ka on the Adriatic margin. Chronostratigraphic data and stable isotope records from planktic and benthic foraminifera are derived from borehole PRAD1-2, a 71 m continuous core drilled on the Western Adriatic slope. The cored interval encompasses the distal parts of stacked progradational wedges that are the main building blocks of 100 ka depositional sequences. These sequences and their internal progradational units reflect a cyclic interplay between sea level and oceanographic circulation, with relevant feedbacks on sediment supply fluctuations and regional long-shore sediment dispersal. Calibration of slope units with isotope stratigraphy and direct slope-shelf correlation indicates that two types of progradational clinoforms alternate in phase with the pattern of composite climate and sea-level changes figured by δ18O records. Changes in clinoform geometry of the kind observed in the Adriatic are consistent with a mechanism of switching supply from dominant advection on a flooded shelf, during highstands, to overall sediment starvation on a narrowed shelf, during lowstands. Seismic and core data document that this mechanism is related to ~100 and 20 ka cyclicity reflecting rearrangement of the oceanographic setting and sediment pathways during the last four glacial-interglacial cycles. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2080228896 title "The combined effect of sea level and supply during Milankovitch cyclicity: Evidence from shallow-marine δ18O records and sequence architecture (Adriatic margin)" @default.
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