Deciphering bottom current velocity and paleoclimate signals from contourite deposits in the Gulf of Cádiz during the last 140 kyr: An inorganic geochemical approach-Reference-Cited by-同舟云学术

Deciphering bottom current velocity and paleoclimate signals from contourite deposits in the Gulf of Cádiz during the last 140 kyr: An inorganic geochemical approach

Published:2014-08 Issue:8 Volume:15 Page:3145-3160
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Bahr André¹,Jiménez-Espejo Francisco J.²,Kolasinac Nada¹,Grunert Patrick³,Hernández-Molina F. Javier⁴,Röhl Ursula⁵,Voelker Antje H. L.⁶,Escutia Carlota⁷,Stow Dorrik A. V.⁸,Hodell David⁹,Alvarez-Zarikian Carlos A.¹⁰

Affiliation:

1. Institute of Geosciences, University Frankfurt; Frankfurt Germany

2. Department of Biogeochemistry; Japan Agency for Marine-Earth Science and Technology; Yokosuka Japan

3. University of Graz, Institute for Earth Sciences, NAWI Graz; Graz Austria

4. Department of Earth Sciences; Royal Holloway University of London; Egham Surrey UK

5. MARUM - Center of Marine Environmental Sciences; University of Bremen, Leobener Strasse; Bremen Germany

6. Divisão de Geologia e Georecursos Marinhos; Instituto Português do Mar e da Atmosfera (IPMA), Rua C do Aeroporto; Lisbon Portugal

7. Instituto Andaluz de Ciencias de la Tierra (CSIC-UGR); Armilla Granada Spain

8. Institute of Petroleum Engineering, Heriot-Watt University; Edinburgh UK

9. Department of Earth Sciences; University of Cambridge; Cambridge Cambridgeshire UK

10. Department of Oceanography; Texas A&M University; Texas USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

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5. Deposition of a muddy sediment drift in the southern Straits of Florida during the late Quaternary;Brunner;Mar. Geol.,1986

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