Enhanced airborne dispersal of silicic tephras during the onset of Northern Hemisphere glaciations, from 6 to 0 Ma records of explosive volcanism and climate change in the subpolar North Atlantic
- 1Volcano Dynamics Group, Department of Earth Sciences, The Open University, Walton Hall, Milton Keynes MK7 6AA, UK
- 2Department of Volcanology and Petrology, GEOMAR Research Center for Marine Geosciences, Wischhofstrasse 1–3, D-24148 Kiel, Germany
Abstract
A 6-m.y.-long composite marine record of explosive silicic volcanism from five Ocean Drilling Program sites in the subpolar North Atlantic was compared with several marine records of global and local paleoclimate proxies (benthic δ18O and ice-rafted debris records). Coarsening and high frequency of occurrence of Icelandic tephras were recorded in 3.6–3 Ma sediments, suggesting that these tephras were dispersed farther from the source by enhanced westerly winds over the subpolar North Atlantic. The 40Ar/39Ar ages were determined by laser probe on K-feldspar and biotite phenocrysts of tephras that were erupted from the Jan Mayen volcanic system. Compared to the tuned paleomagnetic age model, the 40Ar/39Ar dating (0.618 ± 0.007 Ma to 4.90 ± 0.05 Ma) yields a new age model that postdates by 155 k.y. the inception of ice rafting on the Iceland Plateau during the cold marine isotope stage M2 (i.e., 3.3–3.14 Ma).
Footnotes
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↵GSA Data Repository item 2002066, Table DR1, Tephra database, and Table DR2, Ar/Ar database, is available from Documents Secretary, GSA, P.O. Box 9140, Boulder, CO 80301-9140, editinggeosociety.org, or at www.geosociety.org/pubs/ft2002.htm.
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↵*E-mail addresses: Lacasse—c.m.lacasseopen.ac.uk; van den Bogaard—pbogaardgeomar.de
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- Accepted April 9, 2002.
- Received November 13, 2001.
- Revision received March 19, 2002.
- Geological Society of America
