Articles | Volume 7, issue 3
Clim. Past, 7, 757–770, 2011
https://doi.org/10.5194/cp-7-757-2011
Clim. Past, 7, 757–770, 2011
https://doi.org/10.5194/cp-7-757-2011

  19 Jul 2011

19 Jul 2011

Enhanced climate variability in the tropics: a 200 000 yr annual record of monsoon variability from Pangea's equator

R. Y. Anderson R. Y. Anderson
  • Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, NM 87131, USA

Abstract. A continuous series of 209 000 evaporite varves from the equator of arid western Pangea (age = −255 ma), as a proxy for surface temperature, has a complete suite of Milankovitch cycles and harmonics as expected for a rectified reaction to precession-modulated insolation at the equator. Included are modes of precession (23.4 kyr, 18.2 kyr), semi-precession (11.7 kyr, 9.4 kyr), and harmonics at ~7 kyr and 5.4 kyr. An oscillation of ~100 kyr, with 35 % of total variance, originates as an amplitude modulation of precession cycles. An exceptionally strong 2.3 kyr quasi-bi-millennial oscillation (QBMO) appears to have had its own source of forcing, possibly solar, with its amplitude enhanced at Milankovitch frequencies. Seasonal information in varves traces the rectifying process to asymmetrical distribution of Pangea relative to the equator, and its effect on monsoonal circulation and heat flow near the equator during summer solstices in the hemispheres.

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