Spanish researcher Carme Huguet further refined the recently developed TEX 86 paleothermometer during her doctoral research at the Royal Netherlands Institute for Sea Research (NIOZ). The thermometer measures seawater temperature dependent changes in the cell wall composition of archeabacteria.
Real thermometers have been available since the 17th century. For all periods before this, researchers depend on signs from nature. For such determinations, geochemists resort to molecules from microorganisms whose structure is well preserved in seabeds. The TEX86 index has recently been developed at Royal Netherlands Institute for Sea Research (NIOZ). It is based on temperature-dependent changes in the lipid composition of the cell walls of certain types of archeabacteria. Their cell membranes are composed from special lipids of which the number of carbon rings in the molecule changes with the temperature of the surrounding seawater. These organisms therefore adjust the degree of fluidity of their membranes to the prevailing conditions. Carme Huguet studied several aspects of this in greater detail and made significant improvements to the determination.
With a new detection method the analytical reproducibility of the TEX86 paleothermometer was brought to 0.3C and the deviation in the results measured was reduced to 5% of the average. The TEX86 values for organic material out of the water column and from the uppermost layer of the floor sediment best match the temperature of the uppermost 100 m of seawater. However, the small cells of Crenarchaeota cannot sink to the floor by themselves; they are far too light for that. This is, however, achieved more rapidly if the cells of Crenarchaeota are eaten, for example, by crustaceous zooplankton. Fortunately, the time spent in the gastrointestinal tract of the crustaceans does not harm the molecules. Once they have landed on the sea floor, the preservation of the original fat molecules takes place best in ana
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| Contact: Dr. Carme Huguet carme.huguet@nioz.nl Netherlands Organization for Scientific Research Source:Eurekalert |