Benthic foraminiferal species colonize wide areas of the ocean floor and are widely used in paleoceanography. In paleoceanography it is important to continuously develop and refine proxies. The main focus of this thesis is a regional examination of the trace element ratios of O. umbonatus and test their suitability in paleoceanographic applications. Trace elements were measured using LA-ICP-MS on core top samples collected along a transect off Namibia and Mg/Ca ratios where than calibrated against BWTs. The influence of the carbonate ion concentration of sea water and pore-water on trace element and stable isotope incorporation in tests has been discussed and the implications on O. umbonatus was analyzed. These findings were used to investi...
Trace element incorporation into foraminiferal shells (tests) is governed by physical and chemical c...
Determination of Mg/Ca in foraminifer shells as a proxy of seawater temperature is of particular int...
The North Brazil Current in the western equatorial Atlantic is the main route for poleward heat tran...
Benthic foraminiferal species colonize wide areas of the ocean floor and are widely used in paleocea...
Benthic foraminiferal species colonize wide areas of the ocean floor and are widely used in paleocea...
The different benthic foraminiferal species (epibenthic as well as endobenthic) colonize wide areas ...
This thesis examined the reliability and potential paleoceanographic applications of multiple chemic...
We have developed a technique to determine the variability of trace elements (including Li, B, Na, M...
Stable oxygen (δ18O) and carbon (δ13C) isotopic signature registered in fossil planktonic foraminife...
Biological activity introduces variability in element incorporation during calcification and thereby...
Closure of the Central American Seaway (CAS) and hydrology of the Caribbean Sea triggered Northern H...
Trace element ratios (Mg/Ca, Al/Ca, Mn/Ca, Zn/Ca, Sr/Ca, Ba/Ca) measured by laser ablation inductive...
We applied laser-ablation inductively coupled plasma–mass spectrometry (LA-ICP-MS) as a new and pre...
Stable oxygen (δ18O) and carbon (δ13C) isotopic signature registered in fossil planktonic ...
Trace element incorporation into foraminiferal shells (tests) is governed by physical and chemical c...
Trace element incorporation into foraminiferal shells (tests) is governed by physical and chemical c...
Determination of Mg/Ca in foraminifer shells as a proxy of seawater temperature is of particular int...
The North Brazil Current in the western equatorial Atlantic is the main route for poleward heat tran...
Benthic foraminiferal species colonize wide areas of the ocean floor and are widely used in paleocea...
Benthic foraminiferal species colonize wide areas of the ocean floor and are widely used in paleocea...
The different benthic foraminiferal species (epibenthic as well as endobenthic) colonize wide areas ...
This thesis examined the reliability and potential paleoceanographic applications of multiple chemic...
We have developed a technique to determine the variability of trace elements (including Li, B, Na, M...
Stable oxygen (δ18O) and carbon (δ13C) isotopic signature registered in fossil planktonic foraminife...
Biological activity introduces variability in element incorporation during calcification and thereby...
Closure of the Central American Seaway (CAS) and hydrology of the Caribbean Sea triggered Northern H...
Trace element ratios (Mg/Ca, Al/Ca, Mn/Ca, Zn/Ca, Sr/Ca, Ba/Ca) measured by laser ablation inductive...
We applied laser-ablation inductively coupled plasma–mass spectrometry (LA-ICP-MS) as a new and pre...
Stable oxygen (δ18O) and carbon (δ13C) isotopic signature registered in fossil planktonic ...
Trace element incorporation into foraminiferal shells (tests) is governed by physical and chemical c...
Trace element incorporation into foraminiferal shells (tests) is governed by physical and chemical c...
Determination of Mg/Ca in foraminifer shells as a proxy of seawater temperature is of particular int...
The North Brazil Current in the western equatorial Atlantic is the main route for poleward heat tran...