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Connexion

(StuttgartInternational Conference "Landscapes and Soils through Time" en Anglais - 2014)

Document title

Palustrine carbonates and pedogenic calcretes in the Çal basin of SW Anatolia : Implications for the Plio-Pleistocene regional climatic pattern in the eastern Mediterranean

published at : Landscapes and soils through time

Authors(s) and Affiliation(s)

ALÇIÇEK H. (1) ; CIHAT ALÇIÇEK M. (1) ;
(1) Dept. of Geology, Pamukkale Univ., Denizli, TURQUIE

Abstract

Sedimentologic and stable isotopic studies in the Çal basin-fill provide new insights on the late Neogene–Quaternary climatic pattern in the eastern Mediterranean. An erosional unconformity separates the Pleistocene siliciclastic and calcrete deposits above as a single sedimentary unit resting on top of floodplain fines and restricted to the basin center. The stable isotopic analysis of the palustrine carbonates and pedogenic calcretes displays a wide range of values and the lack of significant δ18 O-δ13 C may indicate subhumid conditions or significant diagenetic alteration. The δ13 C values of these carbonates, organic δ13 C data from calcretes and floral remains indicate that the landscapes were dominated by C3 forest plants

Source

Congrès

International Conference "Landscapes and Soils through Time", Stuttgart , ALLEMAGNE (29/07/2011 - 01/08/2011)

published at : Catena / ISSN 0341-8162

Editor : Catena, Cremlingen-Destedt - ALLEMAGNE (1973)

Millesime : 2014, vol. 112 [pp. 48-55]

Bibliographic references : 34 ref.

Collation : fig., tabl.

Language

Anglais

INIST-CNRS, Cote INIST : 16767

Digital Object Identifier

Go to electronic document thanks to its DOI : doi:10.1016/j.catena.2013.03.010

Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 2014
Refdoc record number (ud4) : 28164085 : Permanent link - XML version
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