Abstract
The paleolongitudinal shift of the boundaries of the Domasia-palynofacies during the Wenlockian was about 170 km along a cross-section in North America and about 90 km in West Europe. This shift probably fixes (1) the direction of drift of the reassembled Atlantic continents during the Wenlockian asN45°W± 10°to20°; and (2) the rest of continental drift as 2+ cm per year.
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