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(Reference retrieved automatically from Web of Science through information on FAPESP grant and its corresponding number as mentioned in the publication by the authors.)

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

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Author(s):
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Rodelli, D. [1] ; Jovane, L. [1] ; Ozcan, E. [2] ; Giorgioni, M. [1, 3] ; Coccioni, R. [4] ; Frontalini, F. [4] ; Rego, E. S. [1] ; Brogi, A. [5] ; Catanzariti, R. [6] ; Less, Gy. [7] ; Rostami, M. A. [8]
Total Authors: 11
Affiliation:
[1] Univ Sao Paulo, Inst Oceanog, BR-05508120 Sao Paulo - Brazil
[2] Istanbul Tech Univ, Fac Mines, Dept Geol Engn, TR-34469 Istanbul - Turkey
[3] Univ Brasilia, Inst Geociencias, BR-70910900 Brasilia, DF - Brazil
[4] Univ Urbino Carlo Bo, Dipartimento Sci Pure & Applicate DiSPeA, I-61029 Urbino - Italy
[5] Univ Bari Aldo Moro, Dipartimento Sci Terra & Georisorse, I-70125 Bari - Italy
[6] CNR, Ist Geosci & Georisorse, I-56124 Pisa - Italy
[7] Univ Miskolc, Inst Mineral & Geol, H-3515 Miskolc - Hungary
[8] Univ Florida, Dept Geol Sci, Gainesville, FL 32611 - USA
Total Affiliations: 8
Document type: Journal article
Source: GEOLOGICAL SOCIETY OF AMERICA BULLETIN; v. 130, n. 1-2, p. 193-207, JAN 2018.
Web of Science Citations: 2
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 Elazig 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. (AU)

FAPESP's process: 12/21212-3 - Unravel middle Eocene-Oligocene paleoclimate and paleoceanography using paleomagnetism
Grantee:Daniel Rodelli
Support type: Scholarships in Brazil - Doctorate
FAPESP's process: 12/15995-5 - Stable isotope geochemistry as main tool to unravel Eocene-Oligocene paleoclimate and paleoceanography
Grantee:Martino Giorgioni
Support type: Scholarships in Brazil - Post-Doctorate
FAPESP's process: 11/22018-3 - Primary productivity in oceans studying magnetotactic bacteria in sediments
Grantee:Luigi Jovane
Support type: Research Program on Global Climate Change - Young Investigators