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

Author:

Huber Heinz,Koeberl Christian,King David T.,Petruny Lucille W.,Montanari Alessandro

Publisher

Springer Berlin Heidelberg

Reference52 articles.

1. Alvarez W, Asaro F, Michel H, Alvarez LW (1982) Iridium anomaly approximately synchronous with terminal Eocene extinctions. Science 216: 886–888.

2. Berggren WA, Kent DV, Swisher C III (1995) A revised Cenozoic geochronology and chronostratigraphy. In: Berggren WA, Kent DV, Hardenbol J (eds) Geochronology, time scales and global stratigraphic correlations: A unified temporal framework for an historical geology. SEPM Spec Pub 54, pp 129–212.

3. Bice DM, Montanari A (1988) Magnetic stratigraphy of the Massignano section across the Eocene-Oligocene boundary. In: Premoli Silva I, Coccioni R, Montanari A (eds) The Eocene- Oligocene Boundary in the Marche-Umbria Basin (Italy). IUGS Special Publication, F.lli Aniballi Publishers, Ancona, pp 111–117.

4. Bohor BF, Betterton WJ, Foord EE (1988) Coesite, glass, and shocked quartz and feldspar at DSDP Site 612: Evidence for nearby impact in the late Eocene [abs]. Lunar Planet Sci 19: 114–115.

5. Bottomley R, Grieve R, York D, Masaitis V (1997) The age of the Popigai impact event and its relation to events at the Eocene/Oligocene boundary. Nature 388: 365–368.

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