Note to users. If you're seeing this message, it means that your browser cannot find this page's style/presentation instructions -- or possibly that you are using a browser that does not support current Web standards. Find out more about why this message is appearing, and what you can do to make your experience of our site the best it can be.


Science 25 July 1997:
Vol. 277. no. 5325, pp. 541 - 545
DOI: 10.1126/science.277.5325.541

Reports

Evidence for a Large-Scale Reorganization of Early Cambrian Continental Masses by Inertial Interchange True Polar Wander

Joseph L. Kirschvink, * Robert L. Ripperdan, David A. Evans

Analysis of Vendian to Cambrian paleomagnetic data shows anomalously fast rotations and latitudinal drift for all of the major continents. These motions are consistent with an Early to Middle Cambrian inertial interchange true polar wander event, during which Earth's lithosphere and mantle rotated about 90 degrees in response to an unstable distribution of the planet's moment of inertia. The proposed event produces a longitudinally constrained Cambrian paleogeography and accounts for rapid rates of continental motion during that time.

J. L. Kirschvink and D. A. Evans, Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA.
R. L. Ripperdan, Department of Geology, University of Puerto Rico, Mayaguez, Mayaguez 00681, Puerto Rico.
*   To whom correspondence should be addressed.


Read the Full Text


THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
Late Proterozoic plate tectonics and palaeogeography: a tale of two supercontinents, Rodinia and Pannotia.
C. R. Scotese (2009)
Geological Society, London, Special Publications 326, 67-83
   Abstract »    Full Text »    PDF »
Late Neoproterozoic and Early Cambrian palaeogeography: models and problems.
S. A. Pisarevsky, J. B. Murphy, P. A. Cawood, and A. S. Collins (2008)
Geological Society, London, Special Publications 294, 9-31
   Abstract »    Full Text »    PDF »
Combined paleomagnetic, isotopic, and stratigraphic evidence for true polar wander from the Neoproterozoic Akademikerbreen Group, Svalbard, Norway.
A. C. Maloof, G. P. Halverson, J. L. Kirschvink, D. P. Schrag, B. P. Weiss, and P. F. Hoffman (2006)
Geological Society of America Bulletin 118, 1099-1124
   Abstract »    Full Text »    PDF »
Seawater chemistry and the advent of biocalcification.
S. T. Brennan, T. K. Lowenstein, and J. Horita (2004)
Geology 32, 473-476
   Abstract »    Full Text »    PDF »
A palaeomagnetic and palaeobiogeographical perspective on latest Neoproterozoic and early Cambrian tectonic events.
J. G. Meert, J.G. Meert, and B.S. Lieberman (2004)
Journal of the Geological Society 161, 477-487
   Abstract »    Full Text »    PDF »
Taking the Pulse of the Cambrian Radiation.
B. S. Lieberman (2003)
Integr. Comp. Biol. 43, 229-237
   Abstract »    Full Text »    PDF »
Supercontinents, superplumes and continental growth: the Neoproterozoic record.
K. C. Condie (2003)
Geological Society, London, Special Publications 206, 1-21
   Abstract »    PDF »
Cambrian palaeomagnetic data from Baltica: implications for true polar wander and Cambrian palaeogeography.
T. H. Torsvik, T. H. TORSVIK, and E. F. REHNSTROM (2001)
Journal of the Geological Society 158, 321-329
   Abstract »    Full Text »    PDF »
Late Cretaceous Polar Wander of the Pacific Plate: Evidence of a Rapid True Polar Wander Event.
W. W. Sager and a. A. A. Koppers (2000)
Science 287, 455-459
   Abstract »    Full Text »
Polar Wander and the Cambrian.
T. H. Torsvik, J. G. Meert, M. A. Smethurst;, D. A. Evans, R. L. Ripperdan, and J. L. Kirschvink; (1998)
Science 279, 9
   Full Text »



To Advertise     Find Products


Science. ISSN 0036-8075 (print), 1095-9203 (online)