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 Marine Climate Research
Last Update
01.11.2011
 

Research Group Paleooceanography and Climate

Christian Schwab


Institute of Geosciences, Dep. Geology

Kiel University

Ludewig-Meyn-Str. 10
D-24118 Kiel, Germany

Tel.: +49 (0)431 880 3789 
Fax.: +49 (0)431 880 1912
E-mail: chs[@]gpi.uni-kiel.de

Raum 452

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Research interest

  • relation between primary productivity and climate
  • use of coccolithophorides as paleoceanographic proxys
  • quaternary climate

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Curiculum vitae

since 02/2009

PhD student

Christian-Albrechts-Universität Kiel,

Institute of Geosciences


04 - 10/2008

Diploma thesis:

"Millenial scale climate cycles in the equatorial east atlantic"


10/2001 - 10/2008

Diploma studies of geosciences

at the Christian-Albrechts-Universität Kiel


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Study areas

  • subtropical North Atlantic (south of the Azores Islands)

 

 

Map of the North Atlantic with distribution of chlorophyll a

concentration (MODIS satellite data processed with SeaDAS, 

http//oceancolor.gsfc.nasa.gov). Yellow star marks 

position of cores used in the study.

 

 

Title: Reconstructing paleoproductivity in the vicinity of the Azores Islands using coccolith assemblages


Description:
The study aims to reconstruct paleoproductivity in the midlatitude North Atlanic. Furthermore possible relations to changes in paleoclimate and/or changes in AMOC (Atlantic Meridional Overturning Circulation) should be investigated. Therefor coccolith assemblages will be used. There are two reasons for this: 1. coccolithophorids are one of the three major primary producers in todays world oceans and hence they are perfect for paleoproductivity estimates. 2. due to photosynthetic activity and calcification processes the impact the oceans organic and inorganic carbon pump.

The studies are conducted on sediment cores obtained slightly south of the Azores Islands. The core location corresponds to the northern margin of the subtropical gyre (SG). Therefore we might have the opportunity to reconstruct the extend of the SG.

Today primary productivity in the SG is very low ("oceanic desert") but their area is quiet large. Threfore the extend of the SG might be an important feedbackmechanism for climate changes.

 

 

 

  1.)    2.)    3.)

 

SEM pictures of coccoliths in the investigated sediment cores. 1.) coccolith of Emiliania huxleyi (magnification: 12000); 2.) coccosphere of Gephyrocapsa muellerae (magnification: 10000); 3.) from left to right: F. profund, U. tenius and C. mediterranea (magnification: 10500).

 

 

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AMOCINT (Atlantic Meridional Overturning Circulation during INTerglacials)

 

The PhD thesis is conducted in the framework of the ESF (European Science Foundation) founded project AMOCINT. The project aims to reconstruct AMOC and its relations to climate changes and other climate relevant processes during interglacials. Attention is mainly given to interglacials MIS5 and MIS11. During these intervalls high resolution proxy measurements on marine sediment cores are made. These data are compared with data from the youngest interglacial (Holocene). Correlations possibly will give insights into future climate changes.

 

 

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Workshops & Meetings

 

  • ECOLMAS-course: Modelling the global carbon cycle; November 2008; MARUM; Bremen
  • 2nd EuroMARC conferenz; France; 14 - 16.09.2009
  • EGU General Assembly 2010; Vienna; 02 - 04.05.2010
  • ICP 10; San Diego; 29.08 - 05.09.2010
  • Final EuroMARC conference; Portugal; 7 - 9-02.2011

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Presentations and Publications

  • Poster presentation at the 2nd EuroMARC conference (France, 2009): "Holocene and deglacial changes in coccolith assemblages and its hydrographic implications south of the Azores Islands"
  • Oral presentation at the EGU 2010 in Vienna: "A high resolution coccolithophore record of interglacial surface water variability from the Mid Atlantic Ridge"
  • Poster presentation at ICP 10 in San Diego:"Interglacial surface water variability in the subtropical North Atlantic as reveal by coccoliths"
  • Oral and Poster presentation at the Final EuroMARC conference in Portugal:"Comparison of interglacial coccolith assemblages from the central subtropical North Atlantic and their relation to hydrographic and productivity changes"