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Science 23 April 1999: Vol. 284. no. 5414, pp. 616 - 618 DOI: 10.1126/science.284.5414.616
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Reports
Extensive 200-Million-Year-Old Continental Flood Basalts of the Central Atlantic Magmatic Province
Andrea Marzoli,
12*
Paul R. Renne,
13
Enzo M. Piccirillo,
2
Marcia Ernesto,
4
Giuliano Bellieni,
5
Angelo De Min
2
The Central Atlantic Magmatic Province (CAMP) is defined by
tholeiitic basalts that crop out in once-contiguous parts of North America, Europe, Africa, and South America and is associated with the
breakup of Pangea. 40Ar/39Ar and paleomagnetic
data indicate that CAMP magmatism extended over an area of 2.5 million
square kilometers in north and central Brazil, and the total aerial
extent of the magmatism exceeded 7 million square kilometers in a few
million years, with peak activity at 200 million years ago. The
magmatism coincided closely in time with a major mass extinction at the
Triassic-Jurassic boundary.
1 Berkeley Geochronology Center, 2455 Ridge
Road, Berkeley, CA 94709, USA.
2 Dipartimento di
Scienze della Terra, Universitá di Trieste, via Weiss 8, 34127 Trieste, Italy.
3 Department of Geology and
Geophysics, University of California, Berkeley, CA 94720, USA.
4 Instituto Astronómico e Geofísico,
Universidade de São Paulo, R. do Matão 1226, 015508-900 São Paulo, Brazil.
5 Dipartimento di
Mineralogia e Petrologia, Universitá di Padova, Corso Garibaldi
37, 35100 Padova, Italy.
*
Present address: Department de Minéralogie, Université de
Genève, 13 rue des Maraichers, 1211 Geneva 4, Switzerland.
To whom correspondence should be addresssed. E-mail:
prenne{at}bgc.org
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