|2011 GSA Annual Meeting in Minneapolis (9–12 October 2011)|
|Paper No. 58-2|
|Presentation Time: 1:50 PM-2:05 PM|
EARTHWORM SECRETED CALCIUM CARBONATE – A NEW PALEOTHERMOMETER?
VERSTEEGH, Emma A.A.1, BLACK, Stuart2, and HODSON, Mark E.1, (1) Department of Geography and Environmental Science, University of Reading, Whiteknights, PO Box 233, Reading, RG6 6DW, United Kingdom, email@example.com, (2) Department of Archaeology, University of Reading, Whiteknights, Reading, RG6 6AB, United Kingdom|
The chemical composition of calcium carbonate (CaCO3) skeletons produced by a range of aquatic and terrestrial organisms has been proven to be a useful tool in paleoenvironmental reconstructions. Oxygen isotope ratios (δ18O values) are generally found to be in equilibrium with the environment, solely depending on oxygen isotopic composition of ambient water and temperature. Stable carbon isotope ratios (δ13C values) of biogenic CaCO3 are generally the result of mixing of different C sources ingested by the animal, and can shed light on ecological variables like vegetation composition and food sources.
Although they do not form skeletons, many earthworm species are true biomineralizing animals, secreting calcium carbonate granules, predominantly of calcite but also containing aragonite and amorphous calcium carbonate. These granules are frequently found in archaeological finds and buried soils. We are currently engaged in research investigating the utility of stable isotope compositions of earthworm secreted calcite granules for reconstructing past environments.
Experiments were designed in which individual earthworms (Lumbricus terrestris) were kept in bags of soil for up to four months at a constant temperature. Three different types of soil (with both C3 and C4 vegetation) were used which were air-dried and then moistened with three (isotopically) different types of mineral water. The experiment was performed at three different temperatures. δ13C and δ18O values were measured for the soil organic matter, soil pore water, food (manure), soil air, earthworm tissues and CaCO3 granules. Preliminary results show that the δ18O values of the granules accurately reflect those of the pore water in the soils, in a similar way as for inorganically precipitated calcite. δ13C values appear to reflect those of food (manure) offered to the earthworms.
Our initial results suggest that, in combination with U/Th dating of the granules, the stable isotope composition of earthworm secreted calcite granules can help in the reconstruction of past temperatures, vegetation and soil organic matter composition. As such it provides a much needed new terrestrial proxy for the reconstruction of past environments in archaeological and geological contexts.
2011 GSA Annual Meeting in Minneapolis (9–12 October 2011)
General Information for this Meeting
|Session No. 58|
Advances in Terrestrial Paleoclimatology and Paleoecology: Geochemical Techniques and Examples Using Inorganic and Organic Molecules in Fossil Soils, Plants, Invertebrates, and Vertebrates I
Minneapolis Convention Center: Room 200FG
1:30 PM-5:30 PM, Sunday, 9 October 2011
Geological Society of America Abstracts with Programs, Vol. 43, No. 5, p. 162
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