After the cores arrived to the
CORESTORE laboratory we split them longwise. Then we packed, labeled and deposited them in the cold room.
All the
working halves* were taken to the
GEOLOGICAL WELL SAMPLE LABORATORY. Here, with the help of Sebastian a Geology and Geography undergrad student working in the lab, we sliced each half section every 1 cm.
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Dark gray layer: volcanic ashes? |
The sediment composing the cores is high in carbonate content, hence the light color, however on the cores’ surface it was possible to distinguish some darker layers that we think are volcanic ashes. Some of these layers appear gray while others look greenish. The analysis of the elemental composition of the sediments will tell us why the difference in color and will confirm if those are, in fact, pyroclastic particles.
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Sebastian showing a slice of the core sediment |
We use a CD to slice the cores. The physical and chemical characteristics of the polymer plastic use to produce CDs prevents the sticking of the sediment to the CD surface, making the slicing process (that is already time consuming and a little tedious) much easier than when using aluminium or regular plastic cutters.
Each of the sample-slices was divided in 3, and each of these subsamples will be used for something different:
1. Elemental analysis (composition of the sediment) and magnetic susceptibility
2. Planktic and benthic foraminifera (assemblage changes, stable isotopes, etc)
3. Sediment characteristics (granulometric analysis)
At the end, the linning is empty and we have 265 x 3 little bags full of mud.
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The end of the core, finally!!! |
*The half of the core that is used for all the analyses is commonly referred as the Working half. The half that is keep intact and preserved in the cold room is the Archive.