Mathematics – Logic
Scientific paper
Dec 2008
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2008agufm.p51a1395f&link_type=abstract
American Geophysical Union, Fall Meeting 2008, abstract #P51A-1395
Mathematics
Logic
0419 Biomineralization, 0489 Trace Element Cycling (4875), 5215 Origin Of Life, 5225 Early Environment Of Earth, 9623 Archean
Scientific paper
Sea floor pillow basalts contain tubular and granular bioalteration micro textures in their glassy margins1,2 created by microbes etching the rock3,4, hypothetically to get access to nutrients and electrons donors5. The etched pits in the rock can be regarded as trace fossils6 that later become mineralized by titanite (CaTiSiO5). Such trace fossils are known from recent oceanic crust to some of the oldest preserved Archean ocean floor, in the Barberton greenstone belt (BGB), in S-Africa7. However, the antiquity of BGB trace fossils has been questioned by some since only the host rock was dated until now8. Here, we report for the first time in situ U-Pb radiometric dating of titanite mineralizing the BGB trace fossils using LA-MC-ICPMS. An U-Pb date of of approx. 3.15 ± 0.05 Ga (95.4 % confidence) for the titanite demonstrates the antiquity of the BGB trace fossils. This result confirms the BGB trace fossils as the oldest directly dated morphological trace of life on Earth. We will present addition data to reveal the mineralization of trace fossils by titanite, comparing the BGB trace fossils to other similar tubular titanite mineralized textures from different locations and younger ages. Our data confirms that a sub-oceanic biosphere was already established in the early Archean by at least 3.2 Ga. Further the results highlight the importance of the sub-ocean habitats for the development and possibly refuge for life on (early) Earth. 1. Furnes, H. et al. Bioalteration of basaltic glass in the oceanic crust. Geochemistry Geophysics Geosystems 2, (2001). 2. Staudigel, H. et al. 3.5 billion years of glass bioalteration: vulcanic rocks as a basis for microbial life. Earth-Science Reviews 89, 156-176 (2008). 3. Furnes, H. et al. Links Between Geological Processes, Microbial Activeties and Evolution of Life. Dilek, Y., Furnes, H. and Muehlenbachs, K. (eds.), pp. 1-68 (Springer,2008). 4. McLoughlin, N. et al. Current Developments in Bioerosion (Erlangen Earth Conference). Wisshak, M. and Tapinla, L. (eds.), pp. 372-396 (Springer, Berlin,2008). 5. Santelli, C. M. et al. Abundance and diversity of microbial life in ocean crust. Nature 453, 653-6U7 (2008). 6. Bertling, M. et al. Names for trace fossils: a uniform approach. Lethaia 39, 265-286 (2006). 7. Furnes, H., Banerjee, N. R., Muehlenbachs, K., Staudigel, H. and De Wit, M. Early life recorded in archean pillow lavas. Science 304, 578-581 (2004). 8. Rincon, P. Early life thrived in lava flows. BBC News Channel . 4-22-2004.
de Wit Maarten
Fliegel Daniel
Furnes Harald
McLoughlin Nicola
Simonetti Antonio
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