Effects of Bioturbation through the Late Eocene Impactoclastic Layer near Massignano, Italy

نویسندگان

  • Heinz Huber
  • Christian Koeberl
  • David T. King
  • Alessandro Montanari
چکیده

Effects of bioturbation through the Late 'Institute of Geochemistry, University of Vienna, Althanstrasse 14, A-1090 Vienna, Austria, Eocene impactoclastic layer near (*christian,koeberl@univie,ac,at) 'Department of Geology, Auburn University, Auburn, AL 36849-5305, USA, Masignano, Italy. 'Osservatorio Geologico di Coldigioco, 1-62020 Frontale di Apiro (MC), Italy, r In: Geological and Biological Effects of Impact Events (ed. E. Buffetaut and C. Abstract. The purpose of this study was to investigate the variations in trace element composition resulting from bioturbation of a Late Eocene impactoclastic layer at Massignano, Italy, This layer has an age of 35.7 ± 0.4 Ma and is, Koeberl), "Impact Studies" Series, Springer Verlag, Heidelberg-Berlin, p. 197-216. therefore, coeval with both the North American tektite event (related to the Chesapeake Bay impact structure, USA) and the Popigai impact event (Siberia, Russia). The layer shows a distinct iridium anomaly of up to about 270 ppt. The i ~, stratigraphic leakage within Planolites and Zoophycos burrows was studied by using iridium coincidence spectrometry and conventional neutron activation analysis, on samples obtained by a micro drilling procedure. The iridium contents of the burrow fillings vary from 50 ppt about 20 cm below the impactoclastic layer

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تاریخ انتشار 2008