Russian Journal of Earth Sciences
Vol. 5, No. 6, December 2003
Global climates of the Vendian
N. M. Chumakov
Abstract
The global climate of the Vendian has been the subject of considerable
debate. In view of the difficulties of stratigraphic correlations, the absence
of reliably reconstructed positions of continents, the scarcity of climate
indicators, and the fact that Vendian outcrop areas are widely separated, it is
so far possible to identify only the most general climatic features for three
Vendian time intervals. The latest Vendian (Nemakit-Daldyn) and possibly
the early Tommotian age of the Lower Cambrian were characterized by a
glacial climate and pronounced climatic zoning. Presumably, that time was
marked by the existence of northern and southern cold climatic zones, as
well as a low-latitude and partially mid-latitude warm and hot arid zone.
Throughout the remaining part of the Late Vendian (Ediacaran or Redkino-Kotlin),
the Earth's climate was non-glacial. The warm and hot,
predominantly arid zone encompassed the low and most of middle latitudes.
In the southern high latitudes, there is evidence of warm humid climate. The
Early Vendian Laplandian (Varangian) time had a extremely pronounced
glacial climate. Glaciations of this age have been identified almost on all
large Vendian continents and on some microcontinents. According to some
paleomagnetic determinations and reconstructions for continents, these
glaciations covered the high, middle, and most of low latitudes, extending
also into equatorial regions of the Earth. These data, however, cannot be
regarded as absolutely reliable and as definitive evidence for a continuous
global glaciations lasting for millions of years ("snowball Earth''). Some
geological facts conflict with this hypothesis and agree better with the
results of numerical simulation attesting to the presence of partially ice-free
oceanic areas. This is clearly indicated by numerous glacial oscillations of
different ranks. At the same time, there are as yet no compelling arguments
to rule out the existence of low-latitude glaciations locally on land in the
Early Vendian.