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High-resolution integrated magnetobiostratigraphy of a new middle Eocene section from the Neotethys (Elazığ Basin, eastern Turkey)

2017; Geological Society of America; Volume: 130; Issue: 1-2 Linguagem: Inglês

10.1130/b31704.1

1943-2674

Daniel Rodelli, Luigi Jovane, Ercan Özcan, Martino Giorgioni, Rodolfo Coccioni, Fabrizio Frontalini, Eric Siciliano Rêgo, Andrea Brogi, Rita Catanzariti, Gy. Less, Masoud Asgharian Rostami,

Geological and Geochemical Analysis

Research Article| September 06, 2017 High-resolution integrated magnetobiostratigraphy of a new middle Eocene section from the Neotethys (Elazığ Basin, eastern Turkey) D. Rodelli; D. Rodelli † 1Instituto Oceanográfico, Universidade de São Paulo, São Paulo 05508-120, Brazil †rodelli.daniel@gmail.com Search for other works by this author on: GSW Google Scholar L. Jovane; L. Jovane 1Instituto Oceanográfico, Universidade de São Paulo, São Paulo 05508-120, Brazil Search for other works by this author on: GSW Google Scholar E. Özcan; E. Özcan 2Faculty of Mines, Department of Geological Engineering, İstanbul Technical University (İTU), Maslak, 34469, İstanbul, Turkey Search for other works by this author on: GSW Google Scholar M. Giorgioni; M. Giorgioni 1Instituto Oceanográfico, Universidade de São Paulo, São Paulo 05508-120, Brazil Search for other works by this author on: GSW Google Scholar R. Coccioni; R. Coccioni 3Dipartimento di Scienze Pure e Applicate (DiSPeA), Università degli Studi di Urbino "Carlo Bo," 61029 Urbino, Italy Search for other works by this author on: GSW Google Scholar F. Frontalini; F. Frontalini 3Dipartimento di Scienze Pure e Applicate (DiSPeA), Università degli Studi di Urbino "Carlo Bo," 61029 Urbino, Italy Search for other works by this author on: GSW Google Scholar E.S. Rego; E.S. Rego 1Instituto Oceanográfico, Universidade de São Paulo, São Paulo 05508-120, Brazil Search for other works by this author on: GSW Google Scholar A. Brogi; A. Brogi 4Dipartimento di Scienze della Terra e Georisorse, Università di Bari "Aldo Moro," 70125 Bari, Italy Search for other works by this author on: GSW Google Scholar R. Catanzariti; R. Catanzariti 5Istituto di Geoscienze e Georisorse, Consiglio Nazionale delle Ricerche (CNR), 56124 Pisa, Italy Search for other works by this author on: GSW Google Scholar Gy. Less; Gy. Less 6Institute of Mineralogy and Geology, University of Miskolc, H-3515, Miskolc-Egyetemváros, Hungary Search for other works by this author on: GSW Google Scholar M.A. Rostami M.A. Rostami 7Department of Geological Sciences, University of Florida, Gainesville, Florida 32611, USA Search for other works by this author on: GSW Google Scholar GSA Bulletin (2018) 130 (1-2): 193–207. https://doi.org/10.1130/B31704.1 Article history received: 11 Nov 2016 rev-recd: 19 May 2017 accepted: 07 Jul 2017 first online: 28 Dec 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation D. Rodelli, L. Jovane, E. Özcan, M. Giorgioni, R. Coccioni, F. Frontalini, E.S. Rego, A. Brogi, R. Catanzariti, Gy. Less, M.A. Rostami; High-resolution integrated magnetobiostratigraphy of a new middle Eocene section from the Neotethys (Elazığ Basin, eastern Turkey). GSA Bulletin 2017;; 130 (1-2): 193–207. doi: https://doi.org/10.1130/B31704.1 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 SocietyGSA Bulletin Search Advanced Search Abstract The progressive closure of the Neotethys Ocean had a profound impact on the ocean-climate system during the Cenozoic. In this perspective, Turkey represents a key area for studying the climate evolution during the Eocene, because it was located at the gateway between the Neotethys and the Atlantic Ocean. Here, we present a high-resolution integrated magnetobiostratigraphic record of a new middle Eocene sedimentary section from the Elazığ Province, eastern Turkey. The continuous, undisturbed, and undeformed sedimentary record, together with preserved geomagnetic signal and fossil assemblages, allows the establishment of a detailed age model, which spans from the upper part of chron C19n.1r to the base of chron C17n.1n (42.4–37.8 Ma). Field observations and paleontological and paleomagnetic data show that the section has not been affected by the widespread tectonic deformation that characterizes the region. We suggest that the magnetostratigraphically and biostratigraphically calibrated Baskil section represents a new, outstanding shallow- to deep-marine sequence where paleoceanographic and paleogeographic studies can be conducted to understand the middle Eocene climate evolution. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.