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Summary  

 

The almost continuous belts of coal beds, each one relating to specific geological periods, denote the varying positions of palaeo-equators and confirm the hypothesised land-mass configurations of my smaller Earth models. The various distributions of fossils of insects and tetrapods (most notably dinosaurs) superimpose these palaeo-equatorial belts with such confidence that it is possible to predict which range of fossils would be found in any specific area of the world.

This work suggests that until at least a 100 million years ago, the Earth was predominantly covered with ice - save for a narrow equatorial corridor within which most life was confined. Birds, insects and some plants (eg. coniferous trees) are likely to have been the first to adapt to the seasonal variations which existed beyond the confines of these corridors. Monotremes, marsupials and true mammals may have also evolved their basic characteristics in relation to these much colder conditions, beyond the corridor, in order to exploit untapped resources. These pioneers probably lived an underground existence, feeding on worms, during cold seasons, and this may explain why the first mammals were relatively small creatures.

 

More recent palaeo-equatorial lines also have deposits of evaporites and these too superimpose the fossil distribution lines for given geological periods.

 

The peripheral zones of these equatorial corridors and the extent to which glaciation intruded them can be determined by the signatures left by glaciers. These are scrape marks, till, drop-stones and terminal moraine.

 

Palaeo-magnetic data is yet another way of confirming these equatorial lines. This data independently points to their associated polar positions.

 

An insight into the sequences of evolution are revealed in these studies on palaeo-equatorial corridors. Evolution is powered predominantly by changes in environments. We can come to understand how environments changed as these corridors have moved position over time, and as the Earth got gradually warmer.

 

 

References

 

Lawrence and Hendy, Water Columns and sediments at Lake Fryxell. New Zealand Journal of Geology and Geophysics 1958.

 

Brauckman et al 1995

 

Seguira 1996

 

Milner and Seguira 1994

 

Berman et al 1994

 

Kainang Huang and Opdyke N.D., The Malay block of western Yunnan, China, Institute of Geology, Academia Sinica, Beijing, and Dept of Geology, University of Florida, Gainesville, USA. Science Direct Tectonophysics 2003.

 

Holmes A. Principles of Geology

 

Du Bois P.M. 1957 Comparisons of palaeomagnetic results for selected rocks of Great Britain and North America. Philos. Mag. Supp.v.6,p 177-186.

 

Clegg, J.A. Almond A, and Stubbs P H S, 1954, The remanent magnetism of some sedimentary rocks in Britain, Philos. Mag, ser 7, v 45 - page 483-598.

 

Konshukova 1955

Woodward 1905

Tewari 1966

Isheevo

Schmidt-Nielsen Animal Physiology

Erwin 190, 1994

 

Hargreaves R.B. and Fischer A.G.1959, Remanent magnetism in Jurassic Red limestones from the Alps. Geophys. Jour. V-2 p 750-755

 

Sander P.M et al 2006

 

Museum der Naturkinde, Berlin

 

Mateus O, Antunes, M.T., Abstracts of the Ist Symposium of European Dinosaurs, Dusseldorf, Germany.2000

 

 

THE WANDERINGS OF THE EQUATORIAL

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