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25th International Meeting on Organic Geochemistry IMOG 2011

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P-009<br />

A new method for the combined detecti<strong>on</strong> of different faecal<br />

biomarker classes and their binding types in soils using GC/MS<br />

Michaela Dippold 1,2 , Jago Birk 1,3 , Guido Wiesenberg 2 , Bruno Glaser 3<br />

1 Soil Physics Secti<strong>on</strong>, BAYCEER, University of Bayreuth, Bayreuth, Germany, 2 Department of<br />

Agroecosystem Research, BAYCEER, University of Bayreuth, Bayreuth, Germany, 3 Soil Biogeochemistry,<br />

Institute of Agricultural and Nutriti<strong>on</strong>al Science, Martin-Luther-University Halle-Wittenberg, Bayreuth,<br />

Germany (corresp<strong>on</strong>ding author:midipp@gmx.de)<br />

The detecti<strong>on</strong> of faeces in lacustrine, marine and<br />

terrestrial ecosystems has already been established<br />

based <strong>on</strong> quantificati<strong>on</strong> of several derivatives of the<br />

∆ 5 -steroles, namely the stanoles, the stan<strong>on</strong>es and<br />

the bile acids. However, up to now, the combined<br />

detecti<strong>on</strong> of these substance classes in soil was not<br />

reliably possible so far. A joint quantificati<strong>on</strong> of these<br />

substances would have the advantage to assess<br />

robust and specific informati<strong>on</strong> about the faecal input<br />

into soils. Thus, the objective of this work was the<br />

development of a GC-MS-method for these faecal<br />

biomarkers in soils, which accounts for the<br />

methodological difficulties due to the high organic<br />

matter c<strong>on</strong>tents of many Anthrosols and for the<br />

different binding types of these biomarker classes.<br />

For this purpose, a joint method was developed<br />

based <strong>on</strong> existing methods for single biomarker<br />

classes. After the weak alkaline sap<strong>on</strong>ificati<strong>on</strong> of the<br />

total lipid extract separati<strong>on</strong> of the neutral (∆ 5 -sterols,<br />

stanoles and stan<strong>on</strong>es) and the acidic lipid fracti<strong>on</strong><br />

(bile acids) was performed by means of a sequential<br />

liquid-liquid-extracti<strong>on</strong>. The neutral fracti<strong>on</strong> was<br />

directly purified by deactivated silica whereas the<br />

acidic lipids first had to be methylated before purifying<br />

their methyl esters using activated silica. Finally both<br />

fracti<strong>on</strong>s were derivatized by silylati<strong>on</strong>. Evaluati<strong>on</strong> of<br />

this method was performed by standard additi<strong>on</strong> to<br />

lipid extracts from three Anthrosol-reference-profilepairs<br />

with different soil properties and history: <strong>on</strong>e<br />

sandy and <strong>on</strong>e clayey Amaz<strong>on</strong>ian Anthrosol under<br />

pre-Columbian settlements, <strong>on</strong>e loamy German<br />

Anthrosol next to a Celtic settlement and reference<br />

soils close to each Anthrosol. To get further<br />

informati<strong>on</strong> about the c<strong>on</strong>tent of faecal biomarkers in<br />

differently bound lipid fracti<strong>on</strong>s sap<strong>on</strong>ified lipid<br />

extracts were compared with not-sap<strong>on</strong>ified extracts<br />

and direct sap<strong>on</strong>ificati<strong>on</strong> of soil samples.<br />

The method evaluati<strong>on</strong> by standard additi<strong>on</strong> revealed<br />

no significant differences between the recoveries of<br />

the single substances and the applied first internal<br />

standard. The precisi<strong>on</strong> and the high recoveries<br />

(> 84%) of this method c<strong>on</strong>firm its applicability in soils.<br />

The different sap<strong>on</strong>ificati<strong>on</strong> treatments show that at<br />

least 20% of the neutral biomarker classes were<br />

bound to the soil matrix. For bile acids, which were<br />

bound to about 50% to the soil matrix, this could be<br />

explained by ester b<strong>on</strong>dings via their carboxyl groups.<br />

However, for less polar alcohol substance classes<br />

(∆ 5 -steroles and stanoles) there are two potential<br />

mechanisms for their stabilizati<strong>on</strong>. These include<br />

covalent b<strong>on</strong>ding of the hydroxyl group and a close<br />

associati<strong>on</strong> of these hydrophobic molecules to the<br />

organic substance of the soil, which could not be<br />

distinguished by this method. The high c<strong>on</strong>tent of<br />

stan<strong>on</strong>es in the bound lipid fracti<strong>on</strong> can be attributed<br />

to a very efficient associati<strong>on</strong> of this hydrophobic<br />

substance class with the macromolecular network of<br />

the organic substance. These stabilizati<strong>on</strong> processes<br />

prevent the extracti<strong>on</strong> of bound or encapsulated<br />

molecules. Thus, a direct sap<strong>on</strong>ificati<strong>on</strong> of the soil is<br />

necessary to make a high amount of faecal<br />

biomarkers accessible for extracti<strong>on</strong>.<br />

The determinati<strong>on</strong> of the faecal biomarker fingerprint<br />

in the Anthrosol-reference pairs revealed that input of<br />

omnivorous faeces was <strong>on</strong>ly present in the<br />

Amaz<strong>on</strong>ian Anthrosols but not in the reference<br />

profiles. By means of bile acid fingerprint, these inputs<br />

were identified as human faeces. The profiles<br />

sampled in Germany showed a combined influence of<br />

herbivorous and omnivorous faeces in both profiles,<br />

which could be attributed to cattle, human, pig and<br />

chicken.<br />

Thus, this method copes with the often stipulated<br />

multiproxy-approach for the quantificati<strong>on</strong> of faecal<br />

biomarkers of different substance classes. The<br />

additi<strong>on</strong>al c<strong>on</strong>siderati<strong>on</strong> of the bound lipid pool in soil<br />

enables the detecti<strong>on</strong> of a wide range of lipids<br />

differing in age and origin in soil. Due to polygenetic<br />

sources and the high recalcitrance of faecal<br />

biomarkers, this is decisive for a correct and<br />

comprehensive interpretati<strong>on</strong> of ancient depositi<strong>on</strong> of<br />

faeces. Therefore this method is especially suitable<br />

for the applicati<strong>on</strong> in geoarcheological investigati<strong>on</strong>s<br />

of Anthrosols.<br />

157

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